I.                  INTRODUCTION

The City of Gallup is situated in the high desert region at the southern edge of the Colorado Plateau.  With a population of 20,000 and a trade region population over 100,000, this bustling commercial hub has all but tapped out the available groundwater of the area.  Water has been withdrawn from the City’s groundwater aquifers (“mined”) at an increasing irate during the past 100 years, with very little return to the aquifers (“recharge”) from precipitation and seepage. 

City of Gallup professionals and consulting hydrogeologists have analyzed current and historical data regarding Gallup’s water production and demand patterns.  These studies have estimated the volume of water required to meet residential, commercial and public space water uses – known as “demand”; how much water is pumped from the City’s wells to meet this demand – known as “production”; and how water demand and production vary over time in relation to weather factors such as temperature and precipitation.

The professionals have used these analyses of current and historical water use to project into the future what the potential demands for water might be, and whether there will be enough water (“supply”) to meet these demands.  The fundamental conclusion has been this:  if water demand patterns continue along the lines of current and historical trends, and if additional water supply is not added to the equation – above and beyond currently accessible groundwater aquifers – the City water system will begin facing actual water shortages during peak-demand months as early as the year 2010.

Unfortunately, Gallup is not alone in this scenario.  The issue of “supply versus demand” is very real throughout the Western states, and even more so in the Southwest and in New Mexico.  According to New Mexico’s Office of the State Engineer, drought is not only New Mexico’s “chronic condition,” the Southwest “is due for a drought on the order of a 1950s drought … Even the few dry years that have occurred in 1996, 2000 and 2002 have seriously taxed our ability to meet fundamental demand.”  (Framework for Public Input to a State Water Plan, New Mexico Office of the State Engineer and the Interstate Stream Commission, December 2002).  

In Gallup’s water region (“Region 6” as identified by the New Mexico Interstate Stream Commission, i.e., McKinley and Cibola Counties south of the San Juan Basin), as stated in the Region 6 Water Plan report dated March 1998, Gallup is encountering a number of serious constraints:  “increasing demand, jurisdictional and legal considerations in developing well fields in other locations, infrastructure costs of meeting demand, operations costs, ever-increasing unit costs of water, and non-renewable water supply.”  The report goes on to note that these constraints are not limited to Gallup:  “All municipal and community systems in the region utilize groundwater sources to provide water to their residents and customers.  As the largest community in the region, the City of Gallup is experiencing these problems now.  Other communities will surely face similar difficulties.”  Additionally, water planners have begun to discern a process of desertification taking place in many places in the region, evidenced by loss of plant life (“from grasslands to sand dunes”) and increased “dust bowl” phenomena – a shift, essentially, from what geographers have referred to as “semi-desert” to true desert status.

In Gallup’s case, there is hope that the Navajo Nation will be successful in obtaining substantial Federal support – as the result of a settlement of the Nation’s water rights claims in the San Juan River Basin -- for a water project to be developed to include construction of a water pipeline beginning west of Farmington at a point on the San Juan River and moving southward through the eastern reaches of the Navajo Reservation to the Navajo Capitol at Window Rock and to the City of Gallup and its neighboring Navajo Chapters.  Should this half-billion-dollar project come to pass as currently planned, the City and its Navajo neighbors will be assured of “sustainable water supply” for at least the next forty years.

But new water supply will not be cheap.  In fact, any “new water” will be the most expensive water ever acquired by the City and its residents – whether the supply comes from additional water wells (which, according to some, would be akin to “putting more straws into the same glass of water”) or from the surface waters of the San Juan River.   Although the Federal government will undoubtedly play a key role in financing the “Navajo/Gallup Water Supply Project,” the City will need to pay its share for this precious resource.

In the meantime, other measures are being considered for securing Gallup’s “water future,” many of which may be advisable or necessary, even if the big water pipeline is built.   Gallup’s water crisis imposes on its citizens a mandate for multi-faceted, comprehensive water planning, preparation and management.  In the statewide picture, the State of New Mexico has called for a “paradigm shift” throughout the state in terms of how we perceive and relate to our water supply:  from the mental habit of “water use” to a comprehensive stewardship approach called “Active Water Resource Management.”  Gallup stands to be among the first communities to rise to this challenge, and through its Town Hall its citizens can consider a range of possible actions and policies that can be implemented – with or without the pipeline.

First of all, there are conservation and drought preparation and response practices that will be both necessary and required by federal, state and local laws, ordinances and regulations.   Such practices, as they become institutionalized and universally followed by Gallup’s citizens, may have a significant impact on the City’s ability to sustain itself in future years. 

Secondly, the City may soon have access to the technology and resources to convert and re-use the 3 million gallons-per-day of wastewater moving through the Wastewater Treatment Plant and currently being dumped into the Rio Puerco river bed.  Innovative and visionary plans for development of water catchments, river beds, wetlands, recreational parks and wildlife habitat may become achievable in the not-too-distant future (see descriptions of the “Canyon Project” and “Rio Puerco Restoration Project” later in this document).

Thirdly, there are potentially bold and remarkable things that can be done to restore the region’s watersheds, potentially resulting in the recapture of surface waters, the restoration of above-ground stream flows in the Rio Puerco and the natural “greening” of our high desert oasis.  New Mexico Governor Bill Richardson, in his campaign platform on water entitled “H2O New Mexico,” asserts that “we must improve our watersheds … and we must remove salt-cedars from our river valleys … Experts say watershed restoration will provide us with the largest single new source of water supply.”

We stand, then, at the nexus of crisis and opportunity. 

Clearly, the time is at hand to forge a plan for the future.  There will be many ideas, technologies and resources that can be tapped by the community to create and implement such a plan.  The key question will be:  can we achieve the united political will necessary to meet this challenge of our times?  It is a primary purpose of the Town Hall to answer that question.

This background document will provide information on Gallup’s water – where it comes from, how it is used, what its limits and possibilities are, and the extent to which the City faces a “water crisis.”   It will survey policy and action priorities that may best secure our water future, and it will include both technical information and an exploration of assumptions, values and possibilities that local citizens and leaders can reflect on in generating a consensus strategy for the future.


II.               GALLUP’S WATER RESOURCES

 

Water is a critical factor shaping Gallup’s future. 

In previous generations, human demands placed on water supply did not appear to be a problem.  Prior to the developments of the 20th century, indigenous patterns of water use were small-scale and low-impact.  Catchments and cisterns could meet the modest needs of ranch homes and livestock.  The highlands and grasslands, in their more natural state, were effective at capturing and using the precious water falling on the parched lands.

Railroad and mining operations brought industrial activity and immigrants to the Gallup area, dramatically adding to and impacting the traditional lifestyles of the resident Native American and Hispanic populations and transforming the area’s historic patterns toward a larger-scale and more intensive use of the area’s natural resources.    As with other resources needed for the new development, water seemed to be available to meet our demands.  Even in the high-desert environment, we came to expect that, with the desire, the know-how and the resources, we could find underground sources of water and could magically cause water to appear on the surface to meet our wants and needs.  

During the intervening years, times have changed.   The area’s population has grown, and demands on the ground water supply have intensified.  The volume of water withdrawn from the aquifer greatly exceeds the volume replenishing it from precipitation and seepage.  In the meantime, Mother Nature has proceeded according to her own processes and devices – providing more water from the skies during the wetter years and less precipitation during times of drought.  She has stored billions of gallons of precious water in aquifers both shallow and deep – but most of it remains untouchable by human mind or hand.  Even those waters that we can reach are receding from our grasp, as the water levels in the aquifers drop away from the instruments of our best effort and design.

This section will explore Gallup’s water supply – where it comes from, its quality, how much is used and available, what external factors limit access to water, who manages it, and how we are planning to develop and manage a sustainable water supply for future generations.   Important technical information and insights into the nature of our water supply will be drawn from a few key research documents, including but not limited to:

·              the background report for the May 2002 New Mexico First Water Town Hall held in Socorro, “New Mexico’s Water: Perceptions, Reality and Imperatives” (referred to in shorthand as the “Socorro background report”), authored by Peggy S. Johnson and John W. Shomaker;

·              the Region 6 Water Plan and other planning documents authored by planning staff of the Northwest New Mexico Council of Governments;

·              Framework for Public Input to a State Water Plan, by the New Mexico Office of the State Engineer and the Interstate Stream Commission; and

·              a variety of regional and local studies and reports prepared by Dr. John Shomaker (Shomaker & Associates), Leedshill-Herkenhoff, DePauli Engineering & Surveying (formerly Sterling & Mataya), and Southwest Water Consultants, Inc.


A.                Where does our water come from?

The Socorro background report explains:

Initially, all of New Mexico’s water comes from precipitation, and the principal constraint on our water supply is climate.  For the most part New Mexico is a desert.  A “desert” is a region with a mean annual precipitation of 10 inches or less, and so devoid of vegetation as to be incapable of supporting any considerable population.

The average annual rainfall in the Gallup Basin (except for the Zuni Mountains, whose precipitation levels are about double those of Gallup proper), is between 9 and 12 inches per year, thus establishing the Gallup area as a high-desert environment.   As is the case with the larger cities of the Southwest, such as Phoenix, Las Vegas and Albuquerque, even a town the size of Gallup is a community of “considerable population” in this context, and cannot be sustained indefinitely by existing ground water alone – at least not at the levels of consumption to which we have become accustomed.

The Socorro report goes on to say:

Much effort has been and continues to be directed toward measuring and quantifying New Mexico’s finite supply of water, but no amount of study can totally remove all physical uncertainties and constraints created by Mother Nature.  River flows are highly variable from year to year and from season to season, and the amount of water our watersheds yield has declined as vegetation patterns have changed with land management practices.  As surface water is used and reused, its quality is degraded, sometimes to the point that its use may be limited.  How much ground water is available for development is governed by geologic conditions, climate, cost of development, connection to surface-water flows, and the potential for land-surface subsidence or other adverse responses to development.

The following subsections will describe Gallup’s surface and ground water resources.

1.                       Surface Water Supply.              As explained in the Socorro report, “surface water” refers to all water located on the surface of the land, i.e., rivers, lakes and streams.  Most of the state’s small streams, including Gallup’s Rio Puerco, flow intermittently.  Surface water supply originates as rain or melting snow in the state’s six major surface water basins, of which Gallup’s basin, the Lower Colorado River Basin, is one.  However, of 84 million acre-feet of water from precipitation and river inflows into the state each year, some 97 percent of that water is lost to evaporation and transpiration of water by plants.  Only about 1 million acre-feet of usable, renewable surface water is available each year in New Mexico – or 1½ percent of total precipitation and inflows.  Evaporation from surface water reservoirs can exceed the amount actually delivered to customers; e.g., annual evaporation from Elephant Butte Reservoir in southern New Mexico, averaged over 170,000 acre-feet per year in the last 20 years. 

Surface water supply is impacted by drought, and even groundwater uses are influenced by the increase in demand during such periods.  According to the Socorro background report, “the drought of 1953 through 1956 was the most serious in living memory,” and since that time, drought years in 1996, 2000 and 2002 have caught the attention of all New Mexicans.  Scientists suggest that, based on long-range reconstructions of annual precipitation, New Mexico has been experiencing “above-normal” precipitation over the past 200 years, but that we may be entering another low-precipitation cycle.

As a source of usable water for Gallup, surface water is extremely limited and inconsistent in duration and quantity of flows.   The availability of surface water within Gallup’s water region is largely dependent on climate (e.g., temperature and precipitation) and to varying degrees on the condition of the region’s watersheds, its riverine and riparian systems, and the drop in the water table as a result of groundwater withdrawals.

Little Colorado Basin.  Hydrologically, Gallup lies in the Little Colorado Basin, which extends into eastern Arizona.  Water uses in New Mexico from the Little Colorado River Basin are subject to the Colorado River Compact, which apportions the use of water from the Colorado River system to the Upper and Lower basins.  However, New Mexico’s entitlement within the Lower Basin apportionment to the tributary waters in the Little Colorado River Basin has not been quantified.

In addition to water use by the City of Gallup, Indian water uses constitute a significant fraction of total water use in the basin.  The Zuni River adjudication, recently re-initiated by the US Department of Justice, is intended to adjudicate and quantify the water rights of the Pueblo of Zuni.

The availability of surface water supply in the Little Colorado River Basin in New Mexico is very limited.  Black Rock Reservoir (in Zuni) and a few other small reservoirs regulate surface flow for irrigation of small amounts of land, and agriculture is concentrated in the Zuni River drainage.  Although storage facilities exist in the basin, sufficient water in storage is not physically available to provide water for all of the irrigated lands, and seasonal shortages often occur.  Annual consumptive uses in the basin, including for agriculture, municipal, industrial and domestic uses, total about 12,000 acre-feet per year on average.

Most of the water used in and near the City of Gallup is groundwater – pumped from the Gallup Sandstone and Dakota-Westwater aquifers.  The aquifers are deep, however, and static water levels in wells tapping the aquifers have declined several hundred feet during the past 30 years.  As affirmed by the State in its Framework for Public Input to a State Water Plan, groundwater use by the City of Gallup is not sustainable.

San Juan River.  Gallup’s nearest potential source of sustainable surface water is the San Juan River, originating in the Rocky Mountains northeast of Pagosa Springs, Colorado, and passing southwesterly through a portion of northwestern New Mexico on its way to its confluence with the Colorado River in southeastern Utah.   Although this surface water has not been historically available to Gallup, for over four decades hydrologists, as well as local, state and federal leaders, have identified the San Juan River as the best source from which the eastern Navajo Reservation and the City of Gallup could obtain a sustainable water supply for their future generations.   Studies and reports have been prepared over the years, and in the past decade a concerted effort has been made to finalize a plan and to obtain Congressional authorization and financing to construct a pipeline from the San Juan River to Gallup and Window Rock, serving over 40 rural Navajo Chapters along the way.   

2.                Groundwater Supply   For Gallup, as for most of the populations of its surrounding water region, groundwater is the current predominant source of available water supply, and its availability will be a critical factor over the next 40 years.   

As explained in the Socorro report, “the majority of New Mexico’s fresh-water supply lies below the land surface, where it occupies small open spaces between grains of sand or gravel and small cracks or fractures in rock.  Vast supplies of this ground water occur in different categories of aquifers that include sand and gravel (alluvial) aquifers, sandstone or limestone aquifers, and fractured rock aquifers.”  The State’s major aquifers are depicted in Figure 1 on the following page (adapted from Figure 4, from the Socorro Town Hall report).   Aquifers in the Gallup Basin are predominantly sandstone and (along the north flank of the Zuni Mountains) limestone.


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

FIGURE 1:  Major Aquifer Types in New Mexico (from Stone, 2001)


The Socorro report authors further explain:

Depth, quality and formation productivity are the major physical constraints on groundwater availability.  Areas outside the boundaries of the major aquifer types … may have ground water, but water depths may be great, water-bearing materials may be impermeable, or poor water quality may prohibit use.  Sometimes too little is known about the water resources to characterize the aquifer.  Ground water lies within 200 feet of the surface over a large part of the state, but not all of this water is of usable quality.

Some of the aquifer depths in the Gallup Basin are identified by the State as being at “less than 200 feet” depth to ground water; however, Gallup’s aquifer levels are dropping at alarming rates (i.e., an average of 200 feet per decade), and much of the aquifer north and east of Gallup is high in total dissolved solids (TDS greater than 1,000 milligrams per liter), i.e., exceeding secondary drinking water quality standards.  The Socorro report further explains the nature of aquifers:

Ground water is not a nonrenewable resource like a mineral deposit or a petroleum reserve; but neither is it renewable on an annual or seasonal basis like surface water.  Factors that govern “renewability” of ground water include the permeability, complexity and connectivity of the aquifer, and sources and rates of recharge.  Ground water resources may appear ample, but availability actually varies widely and only a portion of the ground water stored in the subsurface can be withdrawn economically or without adverse consequences.  Prudent development of groundwater requires an understanding and appreciation of the dynamic and complex nature of aquifers.

Under natural conditions, aquifers are in a state of “dynamic equilibrium,” in which recharge of the aquifer approximately equals discharge.  Human activity – pumping – tends to interrupt the flow of groundwater toward discharge points and withdraws far greater amounts from the aquifer than can be replenished by recharge from precipitation.  Recharge rates in the Gallup area are estimated at less than 1 percent of mean annual precipitation. 

The Socorro background report warns:  “High ground-water use in limited aquifers with negligible recharge can cause widespread declines in ground-water levels and a significant decrease in ground water storage.”  The report goes on to describe a phenomenon that occurs in many places in New Mexico (including Gallup):

In some areas of New Mexico, decades of ground-water pumping have resulted in prolonged and progressive depletions of ground-water in storage and declining water tables indicative of “ground-water mining.”    Severe declines in water levels have sometimes unanticipated and undesirable effects, including:

·         large decreases in aquifer storage; …

·         shallow wells that go dry;

·         impairment of senior water rights;

·         increased costs of pumping and drilling replacement wells; …

·         less water available for vegetation and habitat as shallow water tables decline; … and

·         a pumping well intercepting contaminated or poor quality ground water.

Gallup’s Supply.   Gallup lies within New Mexico’s Water Planning Region 6, which covers two-thirds of McKinley County and all of Cibola County.  Geologically, the area is located in the San Juan Structural Basin, which extends into Colorado, Arizona, Utah, and northwestern New Mexico.   Water Planning Region 6 consists of four basins within the larger structural basin, all of which are “declared administrative basins,” roughly corresponding to geologically defined basins:  the Gallup Basin, the Bluewater Basin, Rio Grande Basin, and the “Gallup Extension” (in the Zuni area south of the Gallup Basin, declared in March 1994, though administratively considered part of the Gallup Basin). 

 The water-bearing nature of aquifers can be understood in terms of two characteristics that govern well yields and the availability of ground water, i.e.:

·         “Transmis­sivity” is a measure of the rate at which water will flow through the aquifer based on the characteristics of the formation.  The higher the transmissivity, the more quickly water will flow through the aquifer, and the higher the gallons per minute which can be pumped from that aquifer. Specific capacity is used to describe well yields, or the number of gallons per minute that can be pumped per foot of drawdown in the well. 

·         Storage coefficient” is a measure of the amount of water that a unit area of the aquifer will yield, and it essentially describes the proportion of water to other materials in the aquifer.

Most ground water in the area’s sandstone or limestone bedrock aquifers is in confined aquifers, where the storage coefficients are very low, meaning that pumping at a particular rate results in relatively large and widespread drawdown.  In and near the outcrop areas of these aquifers the storage coefficients are much greater.  Although this indicates potentially larger well yields at the outcrop areas, such areas are relatively small.  The storage coefficient of the shallow alluvial aquifers is probably greater than at the outcrops, so drawdown effects of pumping from shallow alluvial aquifers are correspondingly smaller.  The water bearing geologic units, by basin, are listed in Table 1.

 

TABLE 1

PRIMARY SOURCES OF GROUNDWATER IN REGION 6

(Leedshill Herkenhoff, 1994)

 

 

Bluewater Basin

Rio Grande Basin

Gallup Basin

Gallup Extension

Alluvium

X

X

 

 

Menefee Formation

X

X

 

 

Crevasse Canyon

 

 

X

 

Gallup Sandstone

X

X

X

 

Dakota Sandstone

 

 

X

 

Morrison Formation

X

X

X

 

Cow Springs - Bluff

 

 

X

 

Entrada Sandstone

 

 

X

 

Chinle Formation (Sonsela Sandstone)

X

 

X

X

San Andres Limestone & Glorieta Sandstone

X

 

X

X

 


The Gallup Basin.  The water-bearing characteristics of the Gallup Water Basin can be summarized as follows, as excerpted from the Region 6 Water Plan report (1998):

·               Quaternary‑age alluvium:  The alluvium that fills the valley of the Puerco River and tributary drainages derives mainly from erosion of the clay‑rich Menefee and Crevasse Canyon and has a low permeability in most places.  Transmissivity in the Puerco River Valley and other ephemeral stream valleys is about  1,000 ft2/day.  Recharge to the valley‑fill is mostly from storms, although some areas may be recharged from bedrock aquifers.  The alluvium serves as a minor aquifer in parts of the Gallup Basin. and generally yields small amounts of water for stock and domestic use, with well yields ranging from about 10-100 gpm. 

·               Menefee Formation:  The Menefee Formation is at the surface throughout about one‑third of the Basin, and consists of interbedded, repeti­tive sequences of claystone, carbonaceous siltstone and shale, coal, and sandstone.  The sandstone beds are thick to very thick bedded, fine to medium‑grained.  The Menefee may be as thick as 1,000 feet.  Trans­missivities vary depending on the thickness of the sandstone bodies penetrated, but are typically less than 50 ft2/day.  This formation is not considered a large supply sources, with well‑yields of about 12 gpm, and specific capacities approximately 0.10 gpm/ft . 

·               Crevasse Canyon Formation:  The Crevasse Canyon Formation is at the surface throughout about one‑third of the basin.  The Crevasse Canyon consists of four members:  the basal Dilco Coal Member; the Dalton Sandstone Member; the Bartlett Member; and the Gibson Coal Member..  The Dalton is located in the northernmost portion of the Gallup Basin.  Total thickness of the Crevasse Canyon ranges from 420 to 700 feet (Stone, 1983).  Transmissivity of the Crevasse Canyon is probably less than 50 ft2/day and well‑yields are probably less than 10 gpm.   Most members of this stratigraphic unit yield small amounts of water to domestic and stock wells, but the Dalton Sandstone Member, in the northernmost portion of the Gallup Basin,  may potentially be a good aquifer.

·               Gallup Sandstone:  The Gallup Sandstone crops out in the Rio Grande Basin in a southwesterly direction from the northwestern corner of Cibola County.  It consists predominantly of sandstone, but also conglomerate, shale, carbonaceous shale, and coal.  Water occurs in both confined and unconfined conditions in the Gallup Sandstone.  Recharge to the unit is from infiltration from precipitation and streamflow on outcrops, and vertical leakage form confining beds. Thickness ranges from approximately 180 to 526 feet.  Transmissivity varies from 10 to 350 ft2/day in other locations within the study area.  The median well-yield from 32 wells measured by the USGS was 30 gpm.  This formation yields small-to-large amounts of water to wells in the Gallup area and is a major source of water for the City of Gallup.

·               Dakota Sandstone:  The Dakota Sandstone outcrops around the basin margins and is comprised of three dominant lithologies.  Thickness of the Dakota Sandstone ranges from 200 to 350 feet.  Water in the Dakota occurs in both confined and unconfined conditions.  Recharge to the unit is by infiltration from precipitation and streamflow on outcrops, and vertical leakage through confining beds.  Transmissivities are generally less than 50 ft2/day and well‑yields are probably around 10 gpm.

·               Morrison Formation:  The Morrison Formation outcrops to the north and east of the City of Gallup.  The Morrison consists of four members:  the Salt Wash, Recapture, Westwater Canyon, and the Brushy Basin.  The Morrison Formation consists of non‑ma­rine sandstone, siltstone, mudstone, and minor limestone.  Thickness of the Morrison ranges from approximately 330 to 915 feet .  It is not present south of Gallup.  Of the four, the Westwater Canyon Member probably contains most of the water available to wells.  Trans­missivities range from less than 50 to 400 ft2/day, and are substantially less near Gallup.  Well‑yields range from several gpm to approximately 500 gpm.

·               Cow Springs‑Bluff Sandstone:   These sandstones inter-tongue with the overlying Recapture Shale Member of the Morrison Formation and with the underlying Summerville Formation.  Cow Springs is a fine-grained arkosic sandstone and the Bluff is a medium-grained arkosic sandstone.  Combined thickness for the units can range up to about 550 feet.  Transmissivities range from 3 to 50 ft2/day.  Well yields typically range from less than 1 to less than 50 gpm.  Wells completed in the aquifer are also completed in the overlying Morrison or the underlying Entrada .

·               Entrada Sandstone:       The Entrada consists of three members:  the lower Iyanbito Member is a sandstone, present only in the southern portion of the basin; the middle siltstone and the upper (fine-grained) sandstone members are generally present throughout the basin.    Transmissivities range from less than  50 ft2/day along the southern edge of the basin to 100 ft2/day near the center (other researchers suggest a range closer to 20-70 ft2/day).  Well yields are probably only a few gpm.

·               Chinle Formation:  The Triassic-age Chinle Formation consists of reddish-brown siltstone and mudstone, as well as grayish-purpose mudstone.  The Chinle generally has low permeability and acts as a confining unit for the underlying San Andres-Glorieta aquifer.  The Sonsela Sandstone Bed and Shinarump Conglomerate of the Chinle Formation are local aquifers, particularly along Interstate 40 between Bluewater and Continental Divide.  Well yields are not more than 20-30 gpm, with 5-10 gpm yields typical.  The formation is generally known not to be water-bearing.

·               San Andres‑Glorieta:   Transmissivities in the San Andres-Glorieta range from less than 50 to 450,000 ft2/day.  The high transmissivities are from areas in or near outcrops and are attribut­able to dissolution along fractures in the San Andres Limestone. The San Andres‑Glorieta is present within the Gallup Basin, but lies at great depth and has never been tapped as a water‑supply.  Low permeability precludes its use as a major supply source.

In 1976, the USGS completed groundwater investigations of the nearby Zuni Mountains and Malpais Region, and the Westwater Canyon aquifer near Churchrock.  The results indicated that the groundwater resources of those areas are inadequate to meet the municipal and industrial needs of the City of Gallup.  These findings have been reiterated in numerous studies conducted since that time.

In 1998, the City collaborated with the Bureau of Reclamation and the Pueblos of Acoma and Laguna on an investigation into potential utilization of existing de-watering wells at the inactive Mount Taylor Mine located near San Mateo in Cibola County, about 70 miles east of Gallup..   In the March 1999 Technical Appraisal document, the Bureau estimates that a 4,000 acre-feet-per-year yield is possible for a 40-year period.   In Fall 2001, potential stakeholders project began to consider a broader “multi-source/multi-use” concept to optimally benefit many water-use populations in the region. 

Groundwater in Storage.   The Region 6 Water Plan includes John Shomaker’s estimated of total amounts of groundwater in two sets, per drinking water standards:  amounts with water quality at total dissolved solids (TDS) under 1,000 mg/l; and amounts with water quality at TDS over 1,000 mg/l.  He further distinguished between “recoverable” water in storage and that which is not recoverable:  “recoverable” is the amount of water which could physically be removed from the aquifer, but this definition does not address the costs involved in removing this volume of water from the aquifer.  The number of wells that would be required to remove all the recoverable water from storage is prohibitive. 

·         Total Water in Storage:  The estimate for total water in storage in the aquifers was derived by taking the area in acres under which the aquifer lies, multiplying this number by a typical thickness of the aquifer, thus obtaining the cubic area of the aquifer.  This number is then multiplied by an assumed porosity of ten percent (10%), to obtain the estimate for the total amount of water in storage.  According to Shomaker, “There is no possibility of extracting even a tiny fraction of this water for use, even if cost were not a consideration.  To extract even a small percentage of this water would lead to serious consequences in the form of land surface subsidence.” 

·         Recoverable Water in Storage:   Recoverable water in storage in the alluvium was estimated by multiplying the area of the alluvium by a typical saturated thickness of 100 feet, times a specific yield of 25%, and assuming that 50% of the total could be recovered by closely spaced wells.

The size of the aquifer is multiplied by an estimate of the amount of water that can be successfully withdrawn from it (the specific storage value).  Imagine a box one foot wide by one foot long and one foot high.  If the box contains only water, and one pumped water from the box, there would be one cubic foot of water.  However, if the box contains other materials, as does an aquifer, there would not be the same amount of water as if the box contained only water.  The amount of water in storage in the alluvium is estimated to have a specific storage value of 25%.  All other formations are assumed to have a storage value of 10-6, a standard value which describes how much water can be obtained from confined aquifers such as those which occur in Region 6.

Shomaker notes that the estimates for recoverable water in storage do not refer to dewatering the aquifers, which refers to lowering the pressure in confined aquifers to produce water, which is the manner by which wells in deep bedrock aquifers produce water.

Above and beyond the concern about land-surface subsidence, there are several reasons why neither all the water in storage nor all the “recoverable” water in storage can be withdrawn:

1.        Most aquifers in Region 6 have relatively low hydraulic conductivity, resulting in a steep cone of depression around the well from which water is being extracted: i.e., as the water is being pumped from the well, it is not pulling enough water from other parts of the aquifer over to the pump and well location.  As a result, the water level drops as the well is pumped, to the point that the water level is below the level of the pump, and the well “goes dry.”  There is still water in the aquifer, but not in the area of the well.

2.      Except for the Gallup Sandstone, and the San Andres Limestone-Glorieta Sandstone aquifers, well yields are low in the aquifers of Region 6.  For example, few wells in the Gallup Sandstone produce more than a few hundred gallons per minute (gpm).

3.            Cost to obtain even a fraction of the water in storage is prohibitive.  This is the overriding constraint in water supply.  The number of wells required, the vast geographic area in which wells would be located, and the cost of pipelines and infrastructure to carry this water all limit how much water can be obtained.  The total volume of water and of recoverable water may be vast, but the required well spacing, drawdowns, and the recovery time may make water development impractical.  Issues such as land status with reference to well locations and  water rights also will affect how much of this water can be recovered.

4.            Withdrawals from an aquifer may cause water of a lesser quality to migrate towards the pumping center, thus altering the quality of the water pumped.

“Recoverable water in storage” is the amount of water that could physically be removed from the aquifer.  The cost of recovering water -- the number of wells, the depth of the wells, the cost of each well, conveyance systems and treatment facilities required -- determines whether the water is, in fact, “practically recoverable.”  Examples of water development projects and their costs already exist in the region. The City of Gallup’s well field at Yah-Ta-Hey in another location would cost over $7 million simply to drill and equip new wells (not including additional pipeline or treatment costs).

In summary, less than 1 percent of the underground water resources in Gallup’s region are “physically recoverable” (i.e., without inducing serious geological consequences), while recovery of only a fraction of that quantity is technically, legally and/or financially feasible.  Additionally, although many of the region’s wells have historically been recharged by “migration” of underground waters within and between aquifers, recharge of groundwater aquifers from precipitation – bringing new water into the hydrogeological system – is minimal.   Thus, water in the region’s deep aquifers is essentially a non-renewable resource. 

Tables 2 through 4 summarize Region 6’s water-in-storage data.

 

 

TABLE 2

ESTIMATES OF TOTAL AND RECOVERABLE WATER IN STORAGE

IN WATER PLANNING REGION 6

(TDS less than 1,000 mg/l and  greater than 1,000 mg/l)

 

Volume in acre-feet

TDS less than 1000 mg/l

Volume in acre feet

TDS greater than 1000 mg/l

Total

Recoverable

Total

Recoverable

Alluvium

850,000

425,000

small

small

Menefee Formation

12,125,000

30,250

8,620,000

19,590

Point Lookout Sandstone

6,750,000

13,500

6,345,000

12,690

Crevasse Canyon Formation

78,370,000

290,660

18,400,000

36,800

Gallup Sandstone

36,420,000

182,100

6,900,000

62,100

Dakota Sandstone

13,220,000

109,080

13,600,000

136,000

Westwater Canyon Member

15,380,000

123,040

13,600,000

108,000

Cow Springs-Zuni-Bluff

156,620,000

1,296,440

small

small

Entrada Sandstone

1,050,000

9,450

22,960,000

156,840

Chinle Formation (Sonsela)

small

small

43,760,000

203,600

San Andres-Glorieta

37,075,000

349,125

44,550,000

239,500

TOTALS

357,860,000

2,828,645

178,735,000

975,120

 


TABLE 3

ESTIMATES OF TOTAL AND RECOVERABLE WATER IN STORAGE

IN PORTION OF MCKINLEY COUNTY IN REGION 6

(TDS LESS THAN 1,000 mg/l)

Aquifer

Gallup and Gallup Extension Basins

Bluewater and Rio Grande Basins

All Basins in  McKinley County

Volume, acre-feet

Volume, acre feet

Volume, acre feet

Total

Recoverable

Total

Recoverable

Total

Recoverable

alluvium

small

small

400,000

200,000

400,000

200,000

Menefee Formation

small

small

11,950,000

29,900

11,950,000

29,900

Point Lookout Sandstone

small

small

4,080,000

8,160

4,080,000

8,160

Crevasse Canyon Formation

29,040,000

58,080

36,880,000

73,760

65,920,000

131,840

Gallup Sandstone

16,695,000

83,475

19,725,000

98,625

36,420,000

182,100

Dakota Sandstone

11,560,000

92,480

1,660,000

16,600

13,220,000

109,080

Westwater Canyon Member

13,080,000

104,640

2,300,000

18,400

15,380,000

123,040

Cow Springs-Zuni-Bluff

19,620,000

196,200

small

small

19,620,000

196,200

Entrada Sandstone

1,050,000

9,450

small

small

1,050,000

9,450

Chinle Formation (Sonsela)

small

small

small

small

small

small

San Andres-Glorieta

small

small

4,325,000

21,625

4,325,000

21,625

TOTALS

91,045,000

544,325

81,320,,000

467,070

172,365,000

1,011,395

 


 

TABLE 4

ESTIMATES OF TOTAL AND RECOVERABLE  WATER IN STORAGE IN PORTION OF MCKINLEY COUNTY IN REGION 6

(TDS GREATER THAN 1,000 mg/l)

Aquifer

Gallup and Gallup Extension Basins

Bluewater and Rio Grande Basins

All  Basins in McKinley County

Volume, acre-feet

Volume, acre feet

Volume, acre feet

Total

Recoverable

Total

Recoverable

Total

Recoverable

alluvium

small

small

small

small

small

mall

Menefee Formation

3,920,000

7,840

4,700,000

11,750

8,620,000

19,590

Point Lookout Sandstone

small

small

6,345,000

12,690

6,345,000

12,690

Crevasse Canyon Formation

(a)

(a)

18,400,000

36,800

18,400,000

36,800

Gallup Sandstone

(a)

(a)

6,900,000

62,100

6,900,000

62,100

Dakota Sandstone

(a)

(a)

13,600,000

136,000

13,600,000

136,000

Westwater Canyon Member

(a)

(a)

13,600,000

108,800

13,600,000

108,800

Cow Springs-Zuni-Bluff

(a)

(a)

small

small

small

small

Entrada Sandstone

9,000,000

81,000

13,960,000

75,840

22,960,000

156,840

Chinle Formation (Sonsela)

8,430,000

84,300

9,320,000

93,200

17,750,000

177,500

San Andres-Glorieta

25,750,000

51,500

18,800,000

188,000

44,550,000

239,500

TOTALS

47,100,000

224,640

105,625,000

725,180

152,725,000

949,820

(a)     included with totals for water less than 1,000 mg/l TDS


B.      Water Quality

As identified in the Region 6 Water Plan (March 1998 report, NWNMCOG), there are several threats to both surface water and groundwater supply, caused by conditions created both naturally and by human activity, e.g.:

·              Threats to Surface Water Quality: poor livestock grazing practices; streambed sedimentation; damage to riparian areas; hydromodification; heavy metals; radioactive elements; salinization.  To this list can be added wastewater effluent and irrigation return flows.

·              Threats to Groundwater Quality: industrial wastewater; municipal wastewater; underground storage tanks; accidental spills; irrigation return flows; septic tanks and cesspools; uranium mining and milling effluent; petroleum product refining; and mixing with waters of inferior quality.

·              Specific Conductance:       Not all recoverable waters are of the same quality.  Water quality is measured by hydrogeologists in terms of total dissolved solids (TDS) in milligrams per liter (mg/l), and then translated into measurements of specific conductance.  The higher the conductance, the higher the infrastructure and treatment costs required to achieve public drinking water standards.  According to safe drinking water standards, public drinking water must be below 1,000 mg/l in TDS.  There is a wide range of conductance in the aquifers in the Region 6 basins, with much of the recoverable water in the higher (lower quality/more expensive) end of that range.  This points to the need for specific and local knowledge in analyzing any water location as a potential supply source.

A standard hydrogeological assumption is that ground water, especially in relatively dry geographic areas, generally has a higher concentration of total dissolved solids (TDS) than does surface water.  In addition to the problem of finite limits on Gallup’s long-term ground water supply, a strong argument in favor of constructing a pipeline to bring San Juan River water to the eastern Navajo Nation and the City of Gallup is precisely that phenomenon:  the Navajo/Gallup Water Supply Project will provide all recipients with generally higher quality water.  Gallup’s groundwater quality can be seen in the context of the State’s overall patterns of water quality in Figure 2, adapted from Figure 6 in the Socorro Town Hall report.

With regard to the quality of water in Gallup’s public water system, the City of Gallup has been able to report to its citizens that the water delivered to the City’s homes and businesses “complied with, or did better than, all state and federal drinking water requirements.”   Although Gallup’s ground water generally contains a relatively high concentration of certain naturally occurring minerals and salts, its water system has been adequately designed to ensure the delivery of drinking quality water to its customers.


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

FIGURE 2:  Quality of Ground water in New Mexico (from Stone, 2001)


C.     WATER QUANTITY:  How much do we use?

1.                     Gallup’s Water Production.   City of Gallup records for 1997 report an average daily water production of 3.87 million gallons per day, or 4,224 acre-feet for the year.  The maximum daily use peaked at 5.5 million gallons per day.  Average annual water production since 1987 has been about 1.3 billion gallons per year, or just under 4,000 acre-feet per year (AFY).   As noted above and in the City’s Well Production Planning Report (1998), the City derives its groundwater from two confined aquifers:  the Gallup Sandstone and the Dakota-Westwater Canyon.  The water table in the Gallup Sandstone Aquifer is between 900 and 2,000 feet deep, and the aquifer’s thickness is between 300 and 400 feet.   Figures 3 and 4 on the following two pages illustrate the City’s historic annual demand.  Figure 3 shows, the rise in per capita usage from 1950 to 2001, while the graph in Figure 4 shows overall annual demand in acre-feet.

The City operates two well fields:  the Santa Fe and the Yah-ta-Hey Well Fields.   Historic water table data provided by the City indicate that the static water level in its wells is declining at the average rate of 200 feet per 10 years.  From the early 1960’s until the late 1990’s, the static water level of the Santa Fe Well Field declined nearly 350 feet; however, in the 30-year period from the early 1970’s until the late 1990’s, the static water level of the Yah-ta-Hey Well Field declined over 800 feet.   The City anticipates a 1-million gallon-per-day shortage during peak periods as early as the year 2010.  Please refer to Figures 5 and 6 on the following two pages, depicting drop in static water levels in Gallup’s well system.

The City’s 40-year master water supply plan (Shomaker, 1991) identified two short-term groundwater supply alternatives:  expansion of the Yah-ta-Hey Well Field to the north; and developing water in the Ciniza area to the east.  Neither alternative is sustainable in the long-term.  The City is also investigating the transfer of water rights from the Plains Escalante Generating Station.

Referring to future production needs in Gallup, Dr. Shomaker concludes:

The long-term pattern is that ground-water pumping is very largely from confined-aquifer storage, not balanced by the diversion of recharge at the expense of streamflow or some other natural discharge.  While recharge and natural discharge can be assumed to have been in balance before development, the water-transmitting capabilities of the aquifers are so low that the establishment of a new equilibrium in terms of water levels in wells, in which the wells intercept recharge which would otherwise have appeared as natural discharge, will not take place in the foreseeable future.

It is an inescapable conclusion that for the very long term, Gallup would be best served by a supply source that does intercept waters that would otherwise become recharge flows, that is, surface water, or ground water in an aquifer that has sufficient transmissivity to pass precipitation-derived recharge rapidly to the locations of wells.  The Gallup Sandstone and the Westwater Canyon aquifers do not fit this category.  … [V]arious direct surface-water-diversion sources … including the San Juan River … would fit the condition the best. … It is our belief that none of the available ground-water sources can be expected to provide a truly permanent supply for Gallup, and that a surface-water supply should be sought.  The Gallup-Navajo Project offers the best hope, because of the reliability of the supply and the potential for very long life, and should be pursued.


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

FIGURE 3:  Per Capita Water Use in Gallup, 1950-2001, in gallons per capita daily (GPCD)


 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

FIGURE 4:  Historical Annual Water Demand in Gallup, 1960-2004, in acre-feet per year

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

FIGURE 5:  Drop in Static Water Levels in the Muñoz Well, 1969 – 2002, in feet below well-head

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 


FIGURE 6:  Graphical Depiction of Drawdown over Time in Gallup Aquifers,

from PowerPoint presentation by US Bureau of Reclamation, October 2002

 


2.                     Gallup’s Distribution System.   The City of Gallup’s water transmission, distribution and delivery system is comprised of approximately 753,716 feet (or 143 miles) of mainline, 2 through 18 inches in diameter. Pipeline materials are estimated to be 25% Polyvinyl Chloride (PVC), 34% Asbestos Cement (AC), 11% Ductile Iron (DI), 7% Cast Iron (CI), and 23% Unidentified.   As of February 2003, there are an estimated 118,000 feet of service line serving 5,916 customers, of which 4,664 were residential, 1,148 commercial, 74 municipal and 30 miscellaneous.  Other system appurtenances include 6 pump stations, 5 Primary water storage tanks, 6 Distribution system storage tanks, 8 Pressure reducing stations, 698 Fire Hydrants, and 1,335 Gate Valves.   

A large percentage of these facilities have reached or are nearing the limits of their useful life. Much of the system’s distribution network is undersized for today’s level of development and will not meet future water delivery needs.  The vast majority of all but the PVC and the most recent DI piping in the system is in need of replacement.   All of the City’s 6 distribution and 5 primary storage tanks, with the exception of two rehabilitated in 1998, are in need of rehabilitation.   About 30% of the City’s 118,000 feet of service line needs replacement.  The City’s 10-year capital improvement plan for the water systems identified 16 improvement projects projected to cost a total of $17.8 million;  these projects include: 

·         Peña well drilling & equipping,

·         Yah-ta-Hey Primary water tank rehabilitation,

·         12” waterline replacement on Maloney avenue,

·         Design of a portion of the 16” water transmission line from the YTH well field,

·         Replacement of the 16” YTH water line where it crosses I-40,

·         Construction of that portion of the 16” YTH waterline as designed,

·         Pressure reducing station at 9th St. and Coal basin Rd,

·         Replacement of that portion of the 16” waterline from YTH which passes under the BNSF railroad at 5th St.,

·         Annual waterline replacement up to $750,000,

·         Rehabilitation of Rehoboth, Trademart, Twin Buttes and Country Club Tanks, and

·         Rehabilitation of Santa Fe Pump Station.

Of these projects, four are completed or under construction, six others and one additional project (relocation of 710 feet of waterline on south second St.)  are scheduled for financing through a $4,280,000 loan package with the New Mexico Finance Authority.

Although specific projects and cost estimates have not be developed for the City’s needs beyond the next ten years, it would not be unreasonable to say that they are well above the City’s current ability to finance. The question is how is the City going to finance these projects and who should carry the burden.  

D.                Non-Hydrologic Constraints on Water Use

As if the hydrologic issues were not challenging enough, Gallup’s efforts to meet its water supply needs are constrained by a number of legal, political and socioeconomic factors.  The question becomes, not only “Is the water available?” but “Do we have the right to use the water?”  It is an understatement to suggest that these non-hydrologic issues are complex and every bit as challenging as dealing with the actual water resource itself.  The discussion below, drawn largely from the Region 6 Water Plan and substantially informed by legal counsel to the Acoma and Laguna tribes, provides an overview of the legal issues affecting Gallup’s water future.

1.                     New Mexico water law & water rights administration.   The Doctrine of Prior Appropriation.  The doctrine of prior appropriation is used to determine water rights in many Western states.  It contains two essential principles: 1) the first user (appropriator) of the water has the right to continue to use it, and 2) the right to that water continues as long as the appropriator puts the water to beneficial use.  The time when “use” of the water begins is determined by the time when the water is first diverted from a surface water body or pumped from a ground water aquifer.  This doctrine suits areas where water is in scarce supply.  If one water user is not using his or her right, that water should be made available to others.  It stands in contrast to the “riparian doctrine,” more often used in eastern states, in which individuals with land next to a body of water (riparian land) are automatically entitled to unpolluted water from that waterbody.  In summary: 

When a user diverts water from a stream, the date of his first diversion becomes his "priority date."  More priority dates are assigned as more people use the water source until it is fully "appropriated" -- all of the water available is taken -- or even until it is "over-appropriated" -- a circumstance where people wish to use more water than is available for distribution.  When there is insufficient water in a stream to meet the demand, the person with the oldest water right is entitled to his full amount.  When he is finished, the next person in time is allocated his amount, and so on, until the entire supply is exhausted.  Thus, persons with the newest rights on an over-appropriated stream get no water in times of scarcity.  Water rights created under state law can be bought and sold, and junior water users, if they are willing and able to pay the price, may go to senior water users and buy their water rights. 

Common themes of the definition of beneficial use are application of water to a lawful purpose which is useful to the appropriator and at the same time is a use consistent with the general public interest in having water utilized to its maximum.  New Mexico has not statutorily limited what constitutes a "beneficial use."  The term has been construed to include irriga­tion and recreational fishing as well as other traditional western uses such as stock watering. Beneficial use refers to the amount of water actually used; it does not refer to water diverted but not actually used.

          Tribal Rights and Federal Responsibilities to Tribes.  Indian tribes are recognized by the federal government to be separate and distinct governments.  In the 15th and 16th centuries, debates began in Spain and raged throughout Europe on the question of what rights indigenous people had in relation to colonizers.  The debate resolved that the indigenous people did have certain rights, today referred to as “aboriginal” rights.

Aboriginal rights were recognized by the British and Spanish governments.  With the adoption of the Constitution and the recognition of the sovereign powers of the United States federal government, relations with Indian Nations became the exclusive province of federal law.  When the United States entered into the Treaty of Guadalupe-Hidalgo (1848), the nation committed to recognizing and respecting those aboriginal rights of tribes in areas acquired from Mexico.

Cherokee Nation v. Georgia (30 U.S. (5 Pet.) 1 (1831)) was one of the first cases to explicitly acknowledge the political status of a tribe as a “distinct political society.”  In relation to the United States, the court stated that Indian tribes “may, more correctly, perhaps, be denominated domestic dependent nations” and characterized the relationship as resembling “that of a ward to his guardian.”  This is often referred to as the “federal trust responsibility.”   Tribal rights become a type of federal right -- a right that the federal government , as “trustee” for tribes, is obligated to recognize and protect.

The United States has the responsibility, therefore, of protecting tribal trust property and assisting in resource development and management for the sole use and benefit of the tribes.  Many aspects of the trust responsibility are delegated to the Department of the Interior, but every other federal agency has trust responsibilities to tribes and pueblos.  Tribal trust resources include but are not limited to land, timber, water, cultural resources and reservation fisheries.  The federal courts have insisted that the executive department conduct its dealings with Indians by the highest fiduciary standards (the highest standards of trusteeship).  It is because of the federal obligation that the United States asserts water rights claims on behalf of Indian tribes.  These rights concern not only surface water, but also groundwater.

However, notwithstanding the trust doctrine, Indian tribes are sovereign entities.  The governmental powers of Indian tribes were generally not those granted by Congress; rather, tribes possess inherent sovereign powers that have never been taken away.  As such, many tribes have employed their own legal counsel to assert water right claims on their own behalf.  The claims asserted by the Indian tribes do not always correspond exactly to those filed by the United States on behalf of the tribes.  Sometimes the tribes do not believe that the federal government is providing sufficient advocacy on their behalf.

Methods of Describing Tribal Water Rights.  There are two distinct methods of describing federally recognized tribal water rights.  The first method, known as the “Winters doctrine,” generally holds that when the United States first reserves lands for a tribe, it reserves for the exclusive use of the tribe the water “then unappropriated” by other users for the purposes of the reservation -- the making of a homeland for the tribe.  

The second method, using “Aamodt” water rights,  takes its name from the case State of New Mexico ex rel. State Engineer v. Aamodt.  In that case, one federal district court rejected application of the Winters doctrine to determine the quality of water held by some Pueblos for their grant lands because the rights of the Pueblos pre-existed federal recognition and the United States has an international treaty obligation to protect those pre-existing rights.  An “Aamodt” water right is “aboriginal” -- it is senior to all other users.  The quantity of the right has been described as “sufficient water for all lands irrigated up until 1924, other uses protected by specific federal legislation, and additional water sufficient to meet all reasonably foreseeable future needs of the community.”  

·            The Doctrine of Reserved Rights (“Winters Rights”).  Under the doctrine of reserved rights, all rights that are not “impliedly relinquished” are retained.  In the 1908 case of Winters v. United States (207 US 564 (1908)) the U.S. Supreme Court determined that the doctrine of reserved rights is applicable to Indian waters.  The Winters case addressed the rights of the Fort Belknap Indian Reservation to use water from the Milk River in Montana.  The United States, on behalf of the tribes and bands of the Fort Belknap Reservation, sued to prevent the construction of a dam on the Milk River which would have prevented the flow of water downstream to the reservation.  The Court found that the tribes signing the treaty to create the reservation did not relinquish the waters associated with the reserved lands, and set the principle that, if a tribe has not specifically relinquished the rights to its waters, it has, by implication, retained them.  Furthermore, the reserved waters must be sufficient to enable the Indians to fulfill the goals of the reservation (207 US at 576).

Winters rights to water are not based on an application of water to “beneficial use,” and are not subject to state laws providing for abandonment, forfeiture or adverse possession.  Finally, the Winters doctrine itself does not specify a fixed amount of water for a tribe, although tribes may go through the process of quantification of those rights.  It is also important to note that Winters rights reserve for the exclusive use of the tribe the water that was “then unappropriated” by others.  Thus, a Winters right may be junior to other users whose rights were initiated by non-Indians before the United States created a reservation. 

Although the Winters case referred to reservations created by treaty, courts have consistent­ly upheld and applied the Winters doctrine to cases where an Indian reservation is created by Executive Order as well as by Act of Congress.  At least one federal court has interpreted Winters to also apply to either federal or tribal reservations of rights.  This means that the date of reservation may be either the date that the federal government reserves the land, or the date the tribe reserves the land -- an aboriginal date -- thereby allowing an aboriginal priority date for some Winters rights.  One federal court has held that the Winters doctrine applies only to lands added to the Pueblos by presidential or congressional acts.

The applicability of Winters rights to ground water remains in question.  Although it is logical that tribes would also reserve rights to ground water beneath the land, and would be able to prevent junior users from depleting ground water beneath reservations, the Wyoming Supreme Court ruled that reserved rights did not extend to ground water beneath the Wind River Reservation.  The U.S. Supreme Court, however, in its decision in the Cappaert case to prohibit pumping from wells near Death Valley National Monument, which would have lowered water tables within the Monument and endangered the rare Devil’s pupfish, recognized the connection between surface and groundwater (426 US 128, 138 (1976)]).  This case affirmed the right of the federal government to prohibit groundwater pumping that creates adverse effects (Checchio and Colby, 1993).

The Winters decision has been construed to mean that whenever the United States sets aside land for specific purposes (thereby withdrawing the land from the general public domain), there is implied, if not expressed, an intent to reserve that amount of water required to fulfill the purpose for which the land was set aside.  In 1963, the Supreme Court stated that the reserved rights doctrine would apply to any enclave withdrawn from the public domain by the federal government whether for Indians, na­tion­al forests, or to preserve a unique species of wildlife.  A 1973 report by the General Accounting Office indicated that the National Park service anticipated “potentially large nonconsumptive water requirements to protect instream flows for fish and wildlife conservation, recreation, and esthetic values (GAO, 1973, page 10).”  However, in general, Indian rights were expected to be a more pressing issue, since “[u]nlike Federal reservations, which are not expected to have large consumptive demands, many Indian reservations are expected to require significant water quantities to satisfy reservation purposes (GAO, 1973, page 18).”

·            Aboriginal Rights.  The Aamodt case (State of New Mexico ex rel. State Engineer v. Aamodt) has specifically addressed Pueblo water rights in the Rio Pojoaque Basin.  Four pueblos, San Ildefonso, Pojoaque, Tesuque and Nambe, are located in the Basin.  The Pueblos’ lands and waters were recognized and protected by the Spanish and Mexican governments as “mercedes” (translated as “grants”).  The Spanish Royal Decree of October 15, 1713 explicitly recognized and protected these grants and their continued existence into the future.

As property protected by the Treaty of Guadalupe Hidalgo, most Pueblos’ lands were confirmed by Congress in 1858 upon recommendation of the Surveyor-General.  As a result of the distinctive method by which the Pueblos’ rights were recognized, the federal court, in Aamodt, concluded that this recognition did not “create” Winters rights since the Pueblos’ water rights pre-existed United States action, and were not “reserved” by the federal government.  The federal court therefore determined that these rights are not recognized under the Winters doctrine, but are instead aboriginal rights, senior to all other users.

Adjudication and Negotiation Processes.  The exercise of water rights is often done in the absence of legal proceedings, with users of a water body operating within state or tribal permitting requirements (see below).  However, there is also a formal process by which ownership and extent of water rights are legally determined, known as the adjudication process.  A general stream adjudication is a special type of lawsuit to determine the amount, type, and priority date of every user’s respective water right to a particular water source.  This process resolves controversies concerning titles to water rights and validity of water rights.

This process can be initiated by individual appropriators or by the Office of the State Engineer.  Adjudications include two parallel processes: gathering technical information regarding water use in the area, and the lawsuit that includes all water rights owners in the area.  The lawsuit culminates in the issuance of a court decree which defines the extent of each water right within the area.

Although Indian water rights are not subject to the doctrine of prior appropriation, nor are they quantified according to state law, the McCarran Amendment of 1952, as interpreted in case law, allows them to be discussed and determined in a state court.  There are numerous other issues and legal questions affecting the quantification of Indian rights. 

Negotiation is an alternative to adjudication.  The adjudication process is often long and cumbersome -- processes initiated twenty years ago are referred to as “young.”  Some tribes may need their water sooner than the adjudication process will allow, and would prefer to work out a negotiated settlement in a smaller time frame.  In the Gallup area, the federal government has re-initiated a lawsuit on behalf of the Pueblo of Zuni as a mechanism for forcing adjudication and quantification of water rights in the Zuni River Basin.  This action provoked widespread concern among water users in the basin, but it is unclear how the case will ultimately be  handled.

International and Interstate Obligations

Colorado River Basin.  West of the Continental Divide (in the Zuni River, Puerco River, and Largo Creek watersheds), water flows into the Colorado Basin.  Three primary measures address these obligations in the Colorado Basin: the Mexican Water Treaty of 1944, the Colorado Compact, the Upper Colorado Compact.

·            The Mexican Water Treaty of 1944          The Mexican Water Treaty of 1944 (“Treaty with Mexico respecting utilization of the waters of the Colorado and Tijuana Rivers and of the Rio Grande, February 3, 1944") establishes the most permanent commitment of the waters of the Colorado River.  Article 10 of that Treaty allots 1.5 million acre feet (MAF) per year of Colorado River water to Mexico from any and all sources in the United States.  The Treaty further provides that an addition­al 200,000 acre feet per year additional water will be provided if the United States determines there is a surplus.  Article 10 also states that in the event of "extraordinary drought" or serious accident making it difficult to provide the 1.5 MAF per year, that amount can be reduced in the same proportion consumptive use in the United States is reduced.

·            The Colorado Compact      The States of Colorado, Nevada, New Mexico, Califor­nia, Arizona, Utah, and Wyoming are bound by the Colorado Compact of 1922.  The Compact divides the Colorado River into upper and lower basins, with the dividing point at Lee’s Ferry, Arizona.  The Colorado River waters are apportioned between the two basins; the apportioned water includes the waters of the tributaries. The upper basin cannot acquire firm water rights to more than 7.5 million acre feet (MAF) per year and the lower basin can acquire no firm water rights in excess of 8.5 MAF per year.  The Compact does not apportion the water of each basin to the individu­al states, however.

·            The Upper Colorado Compact  The states of the upper basin have apportioned the waters of the upper basin in the Upper Colorado Basin Compact of 1948 (43 USC sec 1512 (1970)).  This Compact is subordinate to the Colorado Compact of 1922 (63 Stat. 31 (1949)).  The consump­tive use of water legally available to the upper basin is apportioned on the following basis: Colorado, 51.75%; New Mexico, 11.25%; Utah, 23% and Wyoming, 14%.  Arizona, having only a small part of its area in the upper basin, is given an outright allocation of 50,000 acre feet per year.  The percentage allocations apply only to the 7.5 MAF made available under the 1922 Compact, and do not bind the states in the distribution of any surplus, should such surplus ever ex­ist.

 

The Upper Colorado Compact disclaims any intention to impair or affect the rights, duties and privileges of the federal government.  This means that any reserved water rights, including tribal rights, of the federal government are unaffected by the Upper Colorado Com­pact.

Rio Grande Basin            East of the Continental Divide (in the Rio San Jose, Rio Puerco, and Rio Salado watersheds), the region’s water resources are in the Rio Grande Basin.  As with the Colorado Basin, there are both international and interstate compacts governing this river basin.

The 1906 Treaty with Mexico     The Rio Grande has been over-appropriated since at least the end of the 19th Century.  The United States was using the entire flow of the river to the detriment of Mexico.  Mexico made a claim for damages totaling $35 million against the United States and alleged that the damages were the result of increased diversion of water in New Mexico and Colorado (McDonald and Tysseling, 1982).  In 1906 the two nations entered into a treaty for the equitable distribution of the waters of the Rio Grande for irrigation purposes.  In the treaty the United States became responsible for ensuring that a certain quantity of water, 60,000 acre-feet, is delivered annually to a certain point in the river just above Juarez.  When shortages exist, deliveries are made in proportion to the amounts available. 

The importance of the treaty is that it requires delivery of surface water flows.  This means that the Rio Grande, both surface and groundwater, must be conjunctively managed to keep the surface river sufficiently whole to meet this international delivery obligation.  Clearly groundwater use that could be shown to prevent sufficient surface flows would violate the Treaty.

The Rio Grande Compact          Colorado, New Mexico and Texas are parties to the Rio Grande Compact. This compact, executed in 1939, allocates water among irrigation districts. When this compact was negotiated, the intent of the framers was to “stabilize the water allocation pattern in the upper Rio Grande as it existed in 1929 (Shupe and Folk-Williams, 1998).”

The Compact, as with the treaty, creates delivery obligations for the upstream states of New Mexico and Colorado.  New Mexico must deliver a certain quantity of water to Elephant Butte Reservoir for use below the Reservoir in New Mexico and in Texas.  The quantity of water that must be delivered is a specified portion of the flow at Otowi Bridge, on the Pueblo of San Ildefonso. Water imported into the Basin, such as from the San Juan-Chama Project, an interbasin transfer from the Colorado River Basin, is outside Compact limits.

Although the Rio Grande Compact does not explicitly deal with groundwater, New Mexico administers use of groundwater hydrologically related to the surface flows so as to maintain the delivery requirements under the Compact and the Treaty (see City of Albuquerque v. Reynolds,   71 N.M. 428 (1963)).

The Rio Grande Compact, as with the Colorado River Compact, explicitly states that it does not affect the obligations of the United States to Mexico under existing treaties, or to Indian tribes.  The delivery obligation cannot impair tribal rights.  While federal legislation relating to the Middle Rio Grande Conservancy District includes a description of some tribal water rights along the main stem of the river, it does not address tribal water rights on the tributaries.

Administration of Water Rights

The Office of the State Engineer.  The New Mexico Constitution did not create an administra­tive body to regulate the appropriation of water in the state.   In 1907 the territorial legislature wrote the New Mexico Water Code (codified at NM Stat. Ann. sec. 72-1-1 et. seq. (1985 Repl. Pamph. and 1990 Supp.)), which included the creation of the Office of the State Engineer (NM Stat. Ann. sec. 72-2-1).  The State Engineer was charged with "the supervision of waters of the state and of the measurement, appropria­tion, distribution thereof . . . [a]ccording to the licenses issued by him and the adjudications of the courts" (NM Stat. Ann. sec. 72-2-1 and sec. 72-2-9)  -- with the duty of administer­ing all matters relating to the appropriation, transfer, and distribution of wa­ter.  However, the water rights of Indian tribes and Pueblos are not subject to regulation by the State Engineer (or any other state agency).

The most widely known function of the Office of the State Engineer is the processing of water rights applications.  Although no individual owns the water (NM Stat. Ann. sec. 72-1-1 (1985 Repl. Pamph.)) one may acquire a real property right (New Mexico Prods. Co. v. New Mexico Power Co., NM 311, 77P.2d 634 (1937)) to divert surface and ground water consis­tent with the procedures under state law (Snow v. Abalos, 18 NM 681 140 P. 1044 (1914)).

These are the rights referred to above in the discussion of prior appropriation.  They have priority dates, and must be put to beneficial use.  They are formally established through an adjudication process.  However, regardless of whether an adjudication has taken place, water users under state jurisdiction must comply with State Engineer procedures for using water rights, which include licenses and permits.

If one wishes to appropriate water, he must apply to the State Engineer (NM Stat. Ann. sec. 72-12-3) who may grant a permit after determining that unappropriated water exists and that the proposed appropriation will not impair the existing water rights of others NM Stat. Ann. sec. 72-12-3(E)).  While the potential appropriator has the burden of proving the absence of impairment, the State Engineer must make his own independent investigation (City of Roswell v. Berry, 80 NM 110, 452 P.2d 179 (1969)).

There are statutory limits on this role; all water rights that were in existence before 1907 (when New Mexico’s Water Code was established), known as “vested rights,” are valid historical rights.  The right holder should, however, file a declaration of the right with the State Engineer; the State Engineer or other parties may request proof regarding the validity of the rights described in the declaration. The Office of the State Engineer also does not require permits to construct tanks or ponds for watering stock, so long as the tank or pond does not have a capacity of greater than ten acre-feet.

The Office of the State Engineer is responsible for all surface water appropriations within the state (excluding those under tribal jurisdiction), but is not responsible for all ground water appropriations.  In order to establish authority for ground water, the State Engineer must “declare” a ground water basin with specific boundaries.  In McKinley and Cibola counties, the Rio Grande, Bluewater, and Gallup Basins, and the portion of the Gallup Basin known as the Gallup Extension, are declared basins.  The Gallup Extension was declared recently, in 1994.

As with surface water rights, those that were present prior to the authority of the State Engineer, in this case, before the basin was declared, are vested rights.  These should also be filed with the Office of the State Engineer.  Furthermore, the Office of the State Engineer is unable to turn down applications for permits for water use for domestic purposes and non-commercial gardens of less than an acre, if water is available.

Water rights are typically associated with the land on which they are used (NM Stat. Ann. sec. 72-5-23 (1985 Repl. Pamph.)).   However, rights -- including irrigation rights -- can be severed from the land and transferred to another purpose.  As with new appropriations, an application must be made to the State Engineer, who can accept or deny the application.  The application indicates the point of diversion, the place of use, the quantity of the right, and, where they exist, the file number and license number of the right.  The State Engineer must publish the proposed changes and, before allowing such a transfer, determine that no foreseeable detriment exists to other present right holders (NM Stat. Ann. secs. 72-5-22, 75-5-23, and 72-5-25).

Anyone objecting to a proposed transfer can file a formal protest with the State Engineer.  Protests must be based on a claim that the transfer will impair existing rights, will be contrary to the conservation of water, or will be detrimental to the public welfare.  Where no protest is filed and the State Engineer finds the transfer compatible with state law, the transfer application will be approved.  Where there is a protest, the State Engineer holds a formal, due process hearing on the issues set out in the protest and decides the case (NM Stat. Ann. sec. 72-12-3 (1985 Repl. Pamph.)).

The requirement that water transfers be consistent with the public welfare became state law in 1985.  The example of Sleeper v. Ensenada Land and Water Association illustrates some of the issues surrounding the definition of “public welfare.”  This case directly pitted the economic values associated with a new ski development against the cultural values of a northern New Mexico community (No. RA 84-53(c), slip. op. (NM Dist. Ct., Apr. 16, 1985) (”Sleeper I”); rev’d 107 NM 494, 760 P.2d 787 (Ct. App. 1968) (”Sleeper II”); cert. quashed, 107 NM 413, 759 P.2d (1988)).

Tierra Grande Corporation began developing a subdivi­sion in conjunction with a large ski resort development near Ensenada, New Mexico, a small farming community in the north central part of the state, in the late 1970's.  In 1982, the applicants applied for transfer of the surface water rights.  The Ensenada Association protested, alleging that the transfer would impair existing rights and would be contrary to the public interest.  Relying upon hydrologic studies and a finding that the transfer would not impair existing rights, the hearing officer recommended that the State Engineer approve the transfer application.  When the State Engineer acted on this recommendation, the Ensenada Association appealed his decision at the district court level.

At the district court hearing, Ensenada Association argued that the trans­fer would be contrary to the public interest because it would result in the permanent loss of agricultural land and, inasmuch as ditch maintenance expenses after the transfer would be borne by fewer people than before, would increase the financial obligations of individual Association members.  The applicants contended that economic development resulting from the proposed resort project would be in the public interest because it would stimulate the local economy (Sleeper I, slip op. at 5-6).

Addressing the conflict between economic and cultural values inherent in the dispute, the Court mentioned that developments such as the resort community in question contribute step-by-step to the destruction of the local culture.  Reversing the State Engineer, the Court stated that developments such as the resort community in question contribute step-by-step to the destruction of the local culture, and that "to trans­fer water rights devoted for more than a century to agricultural purposes, in order to construct a playground for those who can pay, is a poor trade, in­deed (Sleeper 1, slip op. at 5-6).”

On appeal, the New Mexico Court of Appeals held that the statute in effect at the time of the application precluded the State Engineer from considering broad public interest factors in the transfer of surface water.  Because, in a strict hydrological sense, the transfer did not harm existing rights, the New Mexico Court of Appeals reserved the State District Court (Sleeper II, 107 NM at 496, 500, 760 P. 2d at 791-93).

Water can be trans­ferred from basin to basin, subject to interstate compacts and federal law (NM Stat. Ann. sec. 72-5-23 (1985 Repl. Pamph.)).  Under these systems, the transferor must be certain that within-basin consumptive use after the transfer would not be greater than before the transfer.  Simply put, an out-of-basin transfer cannot make the basin worse off than it was before.

By statute, an owner forfeits his water right if he fails to apply water to beneficial use for a period of four years and he continues not to use the water for one year after notice of proposed forfeiture is given him by the State Engineer (NM Stat. Ann. sec. 72-5-28, 72-118).  New Mexico courts traditionally have not favored forfeiture of water rights.  Where a court can find a reason or legitimate excuse for the nonuse, the original holder's rights generally will be upheld (see, e.g., Chaves v. Gutierrez, 54 NM 76, 213 P.2d 597 (1950); New Mexico Prods. Co. v. New Mexico Power Co., 42 NM 311, 77 P.2d 634 (1937)).

Section 72-4-13 of the New Mexico Water Code mandates that the State Engineer also make hydrographic surveys, beginning on those stream systems most used for irrigation, in order for the waters of the state to be adjudicated.  He also is directed "[to obtain and record] all available data for the determination, development and adjudication" of the State's water supply (NM Stat. Ann. sec. 72-4-13).  The State Engineer was also delegated the authority to "adopt regulations and codes to implement and enforce any provision of any law administered by him . . .  to aid him in the accomplish­ment of his duties . . . . (NM Stat. Ann. sec. 72-2-8).”   Furthermore, the State Engineer has the power to appoint water masters, to apportion water consistent with priorities, and to install headgates and meters for measuring the quantity of water being used (NM Stat. Ann. secs. 72-3-2- 72-5-20).

Other State and Local Agencies.  The State Engineer is not alone in governing the allocation of water rights.  Over the years, the legislature has spawned numerous other entities with overlapping jurisdiction.  For example, the Interstate Stream Commission, created in 1935, is given the authority to investigate, develop and conserve the waters of New Mexico both intra- and inter-state (NM Stat. Ann. sec. 72-14-3 (1985 Repl. Pamph.)).  In 1995, its powers were expanded to include planning for a comprehensive state-wide water program.  At the local level numerous entities such as conservancy districts share the State Engineer's jurisdic­tion (see, e.g., NM Stat. Ann. secs. 73-2-1, 72-2-22 to 64, sec. 73-1-1-, and 73-14-1 to 88).  These are described below.  Where transfers are within irrigation or conservancy districts, and are on lands served by the district works, and downstream users are not affected, the State Engineer does not get involved (Ellis and DuMars, 1978).

Tribal Administration of Waters.  Tribal water rights are not defined or regulated by state law.  These rights are not subject to loss by forfeiture or abandonment (State of New Mexico v. Aamodt, 537  F.2d 1102 (10th Cir. 1976) cert.  denied 429 U.S. 1121 (1977)).  The State Engineer has no jurisdiction over tribal water rights or the use of water on tribal lands (Id.).  As sovereign nations, tribes are able to develop their own systems of water law, water resource management, and water development. 

Tribes also have the option of being treated as states under a variety of laws administered by the Environmental Protection Agency.  This is discussed under the section on “environmental laws.”

·              The Navajo Nation            The Navajo Water Code, 22 NTC, Sections 1107, et seq., 1984 (revised in 1995), creates a comprehensive system for all water within the territorial jurisdiction of the Navajo Nation.  It states:

In order to provide for a permanent homeland for the Navajo People; to protect the health, the welfare and the economic security of the citizens of the Navajo Nation; to develop, manage, and preserve the water resources of the Navajo Nation; to secure a just and equitable distribution of the use of water within the Navajo Nation through a uniform and coherent system of regulation; and to provide for the exercise of the inherent sovereign powers of self-government by the Navajo Nation, the Navajo Nation hereby asserts its sovereign authority over all actions taken within the territorial jurisdiction of the Navajo Nation which affect the use of water within the Navajo Nation.  (Title 22 NTC Ch. 7, Sec. 1101)

Waters within Navajo jurisdiction include: (1) the water reserved to the Navajo Nation by the federal government, (2) water acquired through prior appropriation, contract or similar means, (3) water in hydrologic systems located exclusively within the lands of the Navajo Tribe, and (4) ground water located beneath the lands held in trust by the United States of America.

As with appropriations under state jurisdiction, permits are required for all new uses of Navajo water or changes in Navajo water use.  Applications for permits must include the following information: the purposes for which the water will be used, the quantity of water which will be used, a description of the points and methods of diversion, withdrawal, or impoundment, a description of the method of water application, and an estimate of return flow (Title 22 NTC Ch. 7, Sec. 1604).

The Navajo Nation Water Code also provides for loss of permitted water rights through non-use without sufficient cause for a period of five consecutive years.  “Sufficient causes” for non-use include, among others, the following: drought or other unavailability of water, service in the armed forces, incarceration, application of laws restricting water use, and “other causes of nonuse beyond the control of the holder or holders of the right claimed (Title 22 NTC Ch. 7, Sec. 1902).”

The Water Code is enforced by the Navajo Division of Water Resources (Title 22 NTC Ch. 7, Sec. 1402).  The Division’s duties include administration of water use permits  (Sec. 1404), gathering information necessary to administer the water code  (Sec. 1401), and serving in an advisory function to the Resources Committee  (Sec. 1403). 

·              Pueblos of Acoma and Laguna   The Pueblos of Acoma and Laguna have stated that the fact that their traditional system remains undefined in the written law does not mean there is no water use regulation at the Pueblos.  They note that there is instead an on-going system that uses sustainability as a primary concern; i.e., sustainability of amount, quality, and in some cases, sustainability of a source (for example, limiting groundwater use to protect a spring or in stream flow uses) (Acoma and Laguna joint statement, see Appendix III-A).

Tribal water rights

Water rights issues in the region have focused on the Rio San Jose general stream adjudication, referred to as the Kerr-McGee adjudication.  The United States, on behalf of the Navajo Nation and the Pueblos of Acoma and Laguna, and each of these tribes on their own behalf, filed water right claims in 1989. 

Both Acoma and Laguna have reservations for which rights can be quantified under the Winters doctrine.  However, the vast majority of their water rights are attached to their grant lands, i.e., lands the Spanish and Mexican governments recognized as belonging to the Pueblos.  The State of New Mexico Court of Appeals, citing State ex rel. State Engineer v. Aamodt, determined that the Winters doctrine does not apply to the grant lands of the two Pueblos.

The claims of the United States alone, which include annual diversions of surface and groundwater for irrigation, “Ak-Chin” uses, stock watering, and domestic and community uses, are as follows: (1) 26,525 acre-feet with an aboriginal or time immemorial priority date for the Pueblo of Acoma; (2) 31,080 acre-feet with an aboriginal or time immemorial priority date for the Pueblo of Laguna; and (3) 4,465 acre-feet with an aboriginal or time immemorial priority date for the Navajo Nation’s lands within the basin.  The Navajo Nation has also submitted its own claims for 111,483.3 acre-feet per year for domestic water, irrigation, stockpond, livestock well, municipal, commercial, industrial, and lake evaporative uses (Pollack, 1987).

The effects of the Rio Grande Compact on the Rio San Jose must also be considered.  If development on the Rio San Jose substantially decreases the flows, if any, into the Rio Grande, this could hinder the ability of the State to meet its delivery obligations.  However, the Compact repeats the explicit lack of the State authority over the water rights of the Pueblos including those on the Rio San Jose.  The region will not be able to look to the Pueblos to provide water to meet these delivery obligations.

The Federal government has reactivated the adjudication process in New Mexico for the water rights of the Pueblo of Zuni and Ramah Navajo Reservation.  These reservations are within the Zuni River watershed, which, with the Puerco River, Largo Creek, and other surface water bodies, flow into the Little Colorado River and then to the Colorado River.  The Little Colorado River within Arizona is being adjudicated in the Arizona courts. 

2.                     Economic and social factors.   Hydrology and Legality having been established as key factors in Gallup’s water management challenge, it is possible that social and economic factors would compete as an overriding consideration affecting planning, development and management of the City’s water resources. 

Economics, culture, demographics and politics clearly influence the way in which water is used – how intensively it is pumped and used, for what purposes, where it is used, and how it is conserved, wasted, managed and paid for.  Some of these broad dynamics were outlined in the Introduction section above.

It can also be said that cultural and economic patterns and experiences from the past may continue to inform the present … and future.  As acknowledged by Gallup’s new Mayor Bob Rosebrough and others in the City’s civic limelight,  there are patterns of interaction, misunderstandings, intercultural hurts and misgivings that continue to weigh heavy on the hearts of some of Gallup’s Navajo and Zuni neighbors – as these issues continue to be expressed in repeated meetings and forums throughout the area.  These “inherited linkages” to deep-seated relationship problems among the region’s populations have the potential – if unchecked – to undermine current efforts to provide opportunities for prosperity to all of Gallup’s citizens and neighbors.  The challenge articulated by the new City administration is to continue the more recent trends toward mutual understanding and cooperation and to accelerate the movement of these relations forward to new patterns of trust, collaboration and partnership.

Not surprisingly, water – the most precious of earthly resources – lies at the heart of this challenge, and also at the heart of the current opportunity to forge a plan that best meets the needs of Gallup and the surrounding region.

In the economic arena, Gallup has struggled to find a coherent economic development strategy, in part due to the uncertainty surrounding its future water supply.  The interaction of local water planning and economic development came to a head in Spring 2002 with City studies funded in part by the US Department of Agriculture, in which DePauli Engineering & Surveying and the Northwest New Mexico Council of Governments partnered in preparing a technical report on Gallup’s water transmission and storage facilities as related to (a) the anticipated new water supplies from the proposed Navajo/Gallup Water Supply Project, and (b) the economic growth plans of the City.

The COG’s addendum on the economic connection reports as follows:

The Gallup Growth Management Master Plan projects “maximum” acreage for commercial and industrial usage to grow only 40 percent over the next 40 years (the planning horizon for the Navajo/Gallup Water Supply Project and the City’s 40-Year Water Plan), i.e., from about 1,800 acres to about 2,500 acres.  However, overall commercial and industrial development – along with proportionate water demand – is projected to increase in approximately the same rate as residential and other development over the next 40 years, i.e., an average of about 1.82 percent per year.  For the Navajo Nation, the growth rate is 2.48%.  Projections against the above estimates have not been done, but a factor (1.82% per annum for Gallup; 8.72% for Navajo communities, accounting for accelerated development based on new access to water supply) applied against these baseline numbers provides an approximation of water demand for each of these development sectors, totaling about 4,450 acre-feet per year, summarized as follows:

 

 

Development Corridor

Estimated Water Demand

Business, at  Year 2040

(gallons per day)

Historic/Revitalization Areas

601,035

Balanced Use Expansion Nodes

624,151

Commercial Centers

412,135

Infill Expansion

Industrial Complex

489,694

Other Water Use

270,918

Navajo/Extraterritorial Industrial Development

1,574,269

TOTAL

3,972,202

[~ 4,453 AF/year]

 


The Gallup Master Plan’s “Industrial Development Keys” include the following:

The Land Development Standards recommendations call for establishing a qualitative distinction among the City’s heavier manufacturing and open land uses and categories of industrial use that may attract employers desiring a cleaner image.  Commerce Park developments, for example, could locate in the West Gallup/Airport Gateway vicinity or larger campus developments in the City’s Southern Sector.

 

Thus, commercial/industrial versus residential water usage may exceed the average “36:64” ratio in lands prioritized for industrial and commercial development, while ratios in other parts of Gallup and the outlying communities may be lower.

Two areas targeted as primary development areas of the Navajo Nation will be serviced by the Gallup water system:  Manuelito and Churchrock.  Manuelito is the second of seven sites indicated in the Navajo Nation I-40 Corridor Project study targeted for development.  Each of the sites was selected for its potential in the area of industrial, commercial, or tourism.  The Navajo Nation’s plans for Manuelito center around a major theme promoting Gallup as the gateway community to the Navajo Nation.  Manuelito Chapter has been designated as the site to house a major tourist facility that includes somewhat of a “dude ranch” theme.  Based on current tourism figures, the Navajo Nation anticipates several hundred thousand tourists per year that will stop at this facility for needs ranging from weekly stays to purchase of a meal to use of a restroom.  Current development plans target groundbreaking at Manuelito in the year 2003.

Another targeted area for large scale development is the Churchrock Industrial Park, directly east of Gallup.  The Industrial Park has been experiencing slow growth over the past several years but has now been targeted for major development.  Two industrial recruiters are working on bringing industry to the Park, along with the new emphasis from the Navajo Nation.  The Churchrock Chapter that borders the industrial park has phased housing development plans to construct 200 units over the next 5 years in anticipation of supporting families that relocate to work at the Park.  Additionally, the Northwest New Mexico Community Development Corporation (NWNMCDC) is working with the Navajo Nation, McKinley County, and the City of Gallup to design joint partnership efforts concentrating on industry development at Churchrock Industrial Park.  The location of the park to the City of Gallup is ideal for industrial growth.

[Work is being done] with the Churchrock Chapter and Red Rock Park to develop up to 26 small business enterprises.  Several of these businesses will be in the food service industry and will require a substantial level of water usage, while others are based on the artisan trade, which often requires an even higher level of water use.

Additional industry and tourism growth is taking place at Red Rock Park, within the City of Gallup.  Along with the above Churchrock Chapter efforts, there is an expansive vision of development for Red Rock Park over the next decade.  Up to 75 new camping/RV sites are designated, 50 with water/electric hook ups.  The horse stables which can house up to 50 livestock, are being reopened and stocked year round.  Lodging facilities are being repaired and will soon open to the public.  Red Rock Park is also a potential site for a major county-wide tourist initiative in adventure sports.

The general business growth within the City of Gallup and the immediately surrounding county and Navajo areas mandates additional business growth to sustain the population.  These industries include laundromats; child care; senior care; recreational areas; construction (building along with access roads); food service; and transportation.  Each of these service industries will be encouraged to become established within the targeted development sites mentioned above.

The DePauli Transmission and Storage Facilities study provides for an adequate and efficient system for transmitting and delivering water supply to the bordering Navajo communities per the requirements of the Technical Memorandum and Bureau of Reclamation engineering plans of the Navajo/Gallup Water Supply Project.

 These reports, then, suggest possible scenarios for development that imply an increasing future demand for water, thus helping to justify the City’s need to upgrade and expand its existing system, as well as its overall need for supplemental water supply to be provided from the San Juan River through the Navajo/Gallup Water Supply Project.  The newly appointed Gallup Development Commission will help guide the City’s strategy for  new economic development, tourism and quality of life and thus will be an important stakeholder in all matters related to Gallup’s future water supply.

B.           Water planning

Planning is the call of the hour – the watchword, the standard and the mandate for ensuring Gallup’s water future.   The State of New Mexico, in its Framework for Public Input to a State Water Plan (December 2002), provides a clear goal for water planning efforts throughout the State: 

first … to develop a better understanding of our water supply and the administrative and legal framework in which our water resource decisions are made;

second … to develop policy that respects limits created by water availability and guides new water projects that are based on meeting demand within those limits;

third – to lay out the commitments we choose to make, the steps we must take to protect our water, and our priorities for action.

The State further calls for “new thinking about how New Mexico can make significant changes in our approach to water management.  The Framework document refers to the State’s adjudication backlog as “a symptom of the State’s failure to focus on the building blocks of Active Water Management.  It goes on to say:

New Mexico must now act to complete the conversion to active management of New Mexico’s water resources.  We need to establish functional limits on the use of finite water resources, especially in areas where demand far outstrips supply or where failure to limit uses may create liability for the State and bad outcomes for water users. … Active Water Resource Management is the name we have given to the comprehensive, assertive approach that is needed to protect and enhance New Mexico’s water supply.

            As concerns the City of Gallup’s water future, it is important to be aware of and to participate in all levels of water resource planning, i.e., at the local, regional, and state levels.

1.                       Local Planning.   Gallup has not been lax in planning for long-term water supply, production and use.  In January 1992, Gallup consulting hydrogeologist John Shomaker, with support from Leedshill-Herkenhoff, Inc., Sterling & Mataya,  and local attorney Jay Mason, prepared the Water Supply Studies and Forty-Year Water Supply Master Plan.  In March 1998, Sterling & Mataya teamed up with Shomaker to produce the Well Production Planning Report: City of Gallup, New Mexico.  In August 2000, Southwest Water Consultants, Inc. prepared the Water Development Plan Update:  City of Gallup Water System.   These general plans have been enhanced in the past year by three technical studies by DePauli Engineering & Surveying on: build-out of the City’s Transmission & Storage Facilities in connection with the Navajo/Gallup Water Supply Project (2 reports); and analysis of the City’s Business and Residential water use.  The DePauli reports were further augmented by an Addendum document prepared by the Northwest New Mexico Council of Governments (April 2002) describing the linkage between the City’s future water system plans and economic development.

            Gallup’s local plans are closely interconnected with those of its neighboring communities, most predominantly the Navajo Nation.  The Navajo Nation’s Department of Water Resources has produced two key documents in the past couple of years representing excellent planning work related to providing long-term water supply to the Navajo people: Water Resource Development Strategy for the Navajo Nation (July 2000); and Technical Memorandum:  The Navajo/Gallup Water Supply Project (March 2001).

            Signs of a powerful new partnership between the City of Gallup and the Navajo Nation have been clearly evident in recent years.  Most prominently:

·               For over 10 years, the City and the Navajo Nation have collaborated closely on development of the Navajo/Gallup Water Supply Project, supported by an inter-agency steering committee chaired by the Northwest New Mexico Council of Governments – a process that has navigated daunting and complex challenges at every level of project planning and development;

·               The City, the Navajo Nation, the Indian Health Service and the Navajo Tribal Utility Authority recently entered into a formal agreement to provide municipal water supply to Navajo neighbors living outside the city limits along Boardman Avenue (State Road 564); and

·               The City has collaborated with the Navajo Nation, Indian Health Service, Navajo Tribal Utility Authority and the Council of Governments in developing a multi-project master application to the State Water Trust Fund for a “Gallup Regional System” component of the Navajo/Gallup Water Supply Project, designed to develop and utilize Gallup’s water distribution system as a means of conveying water to neighboring Navajo communities.        

·         Although the City has been responsible and forward-looking in its approach to planning for its water supply, the challenges of the times will require that such planning rise to entirely new level, to include extensive public participation (as “kicked off” by the May 2003 Gallup Town Hall on Water), crafting and implementation of a comprehensive “Active Water Resource Management” plan, identification of priorities for action and funding and informed and effective advocacy at all levels of water planning and policy-making – local, regional, state and interstate.  The Region 6 Water Plan and State Water Plan processes (as described below) will greatly reinforce and benefit from this new level of planning and management.

2.                Regional Planning.  Gallup is part of New Mexico’s Water Planning Region 6, and the City has fully participated in the regional planning effort for the past 10 years.

The purpose of the Region 6 Water Plan is to chart a 40-year course for securing, sustaining and managing precious water resources in State Water Planning Region 6, while contributing to formulation and implementation of the State Water Plan.  Its mission is to ensure an ongoing water supply to meet current and future individual and community water needs at a reasonable cost, appropriate quality and within legal and social constraints and cultural guidelines.

Water Planning Region 6 is comprised of all of Cibola County and that portion of McKinley County not in the San Juan Basin.  Surface water basins include: the Rio Puerco, the Rio San Jose and the Rio Salado (which drain into the Rio Grande); the Puerco River, the Zuni River and Largo Creek (which drain into the Little Colorado River); and the North Plains Closed Basin.  Administrative groundwater basins include: the Bluewater, the Rio Grande and the Gallup declared underground water basins (including the Gallup Extension declared in 1994). 

The Plan is intended to benefit all of the populations of Region 6, encompassing McKinley and Cibola Counties south of the San Juan Basin, and to serve the water interests of the State of New Mexico.  The formal constituencies of the Plan include units of local and tribal government, organized water use entities, and state and federal agencies, i.e.:

o               The municipalities:         The City of Gallup; The City of Grants; The Village of Milan

o               The counties:  McKinley County; Cibola County

o               The soil and water conservation districts: McKinley Soil & Water Conservation District; Lava Soil & Water Conservation District

o               The flood control districts:             Rio San Jose Flood Control District

o               The water and sanitation districts:                Bluewater Water & Sanitation District; Gamerco Water & Sanitation District; San Rafael Water & Sanitation District; Thoreau Water & Sanitation District; Yah-ta-Hey Water & Sanitation District

o               The mutual domestic water user associations:            Bluewater Acres DWUA; Bluewater Lake MDWCA; Coal Basin MDWA; San Mateo MDWCA; Whispering Cedars MDWUA; White Cliffs MDWUA

o               The irrigation groups and districts:                Bluewater Toltec Irrigation District; San Mateo Irrigation District; San Rafael Irrigation Group; Murray Acres Irrigation Group; Bibo Irrigation District; San Fidel Irrigation District

o               The Indian tribes and nations:        The Navajo Nation; The Pueblo of Acoma; The Pueblo of Laguna; The Pueblo of Zuni

o               The land grants:              Cubero Land Grant; Cebolleta Land Grant; Moquino Water System; Bibo Water Supply System; Seboyeta Water System

o               Other local groups and districts:   Sagebrush Water Cooperative;

o               The State of New Mexico:              Interstate Stream Commission; Office of the State Engineer; Environment Department; New Mexico Finance Authority; Soil & Water Conservation Commission; State Legislature; Bluewater State Park; Forestry Service-Coal Mine Campground; Gallup Port of Entry;

o               Federal agencies:           El Morro National Monument; El Malpais National Monument; Bureau of Land Management; Natural Resources Conservation Service

o              Corporate, public service, land development and industrial water users: Lee Ranch Coal Mine; ARCO/Anaconda Mine;  Homestake Mine; Quivira Mine; Plains Electric; public and private schools in the region;  Mount Taylor Millworks; subdivisions and industrial parks; small and medium-sized businesses.

The Region 6 Water Plan is currently articulated in a series of documents:

40-Year Regional Water Plan, New Mexico State Planning & Development District 1,  San Juan, McKinley and San Juan Counties, prepared for the Northwest New Mexico Council of Governments by Leedshill-Herkenhoff, John Shomaker and Charles DuMars, March 1994

Region 6 Water Plan: The 40-Year Regional Water Plan for Cibola County and the portion of McKinley County not in the San Juan Basin, prepared by Mary Murnane, Sharon Hausam and Jeff Kiely of the Northwest New Mexico Council of Governments, March 1998

Region 6 Water Plan:  Phase II—Evaluation of Alternatives and Presentation of Strategies, by Sharon Hausam on behalf of Northwest New Mexico Council of Governments, July 2001

Handbook for Local Water Planning & Implementation – Water Planning Region 6, by Sharon Hausam on behalf of Northwest New Mexico Council of Governments, July 2001

Region 6 Water Plan:  Plan Summary, prepared by Jeff Kiely of Northwest New Mexico Council of Governments, April 2003

As planning coordinator for the Regional Plan, the Council of Governments is currently preparing its executive summary, action recommendations and final presentation for obtaining official acceptance of the Plan this year from the New Mexico Interstate Stream Commission.

3.                     State Planning.  The goal of creating a State Water Plan has been foremost in the minds of water planners, engineers, and public officials for years.  However, focused commitment to this goal has been achieved primarily in the past year and has been empowered by Governor Richardson’s directive that a State Water Plan be produced in the early years of his administration.   Among the first steps will be the completion of Regional Water Plans in each of the State’s 16 planning regions, targeted to be complete this year.  

The document Framework for Public Input to a State Water Plan (December 2002) clearly sets the stage for this statewide effort. 

The overall purpose of the State Water Plan will be to create the blueprint for statewide Active Water Resource Management (AWRM).  A sustained, continuous effort (including adequate funding) will be necessary to resolve the complex technical water issues. … An overarching State Water Plan will enable New Mexico to finally transition from a laissez-faire approach to active and effective management of its water resources.  Going forward with a State Water Plan will allow New Mexico to justify in-state water needs, comprehensively and accurately evaluate water resources and defend against water claims raised by out-of-state interests.  The confidence provided by an overarching State Water Plan will provide the security that promotes productive development and investment, not only in water projects but in the general State economy as well.

To sustain progress, and avoid constant and costly short-term fixes, we must proactively focus on permanent solutions to our water resources issues.  Priorities and solutions identified in the State Water Plan must be based upon:

·         A comprehensive assessment of statewide surface and groundwater resources;

·         Sound policies to move us forward;

·         Consensual and collaborative decisions on how we choose to use available supply to meet various statewide demands; and

·         Priorities for available funds and human resources in the eight areas of Active Water Resource Management:

1.               Quantification of water rights – hydrographic surveys, adjudications, abstracts and administrative permits;

2.               Measurement and metering of water – water supplies and water uses;

3.               Water planning – integrated statewide, regional and local planning including water conservation;

4.               Compliance – with interstate compacts, federal environmental laws and regulations, and legally mandated federal project operations;

5.               Analysis and integration of data, plans and policies – decision support systems, public information access, public communications and involvement;

6.               Water distribution – active administration of the storage, conveyance and withdrawals of wet water supplies;

7.               Water transfers, markets and water banks – creation, coordination and regulation;

8.               Water development – projects to store, convey and develop water resources to meet our needs; watershed improvements; weather modification.

The City of Gallup – working in full partnership with its citizens and neighbors – is ideally positioned to lead the way in fostering local planning and management in full harmony with this ambitious State strategy.

 


III.    WATER MANAGEMENT PRINCIPLES, PROBLEMS

AND ALTERNATIVES

 

            As the statewide Water Town Hall in Socorro learned, the complexities surrounding New Mexico’s water issues for New Mexico are among the most challenging in the Western states – and Gallup is near the front of the curve on those very complexities.  A summary of the key New Mexico issues would include:

·         Limited surface water – surface water is renewable, but flows are variable and not much surface water is stored naturally.

·         “Saturated appropriations” – almost all surface water is already appropriated, with rights-owners having the right to divert as much or more than the average annual flows of most streams.

·         Evaporative losses – the State relies heavily on reservoirs to store surface water in order to prolong and redistribute its availability; but this results in significant loss of water to evaporation.

·         Ground-water mining – the State has a great deal of groundwater, but it is not a renewable supply; it can be used in short time or an extended time, but not indefinitely; and in the Gallup area (as noted in above sections), most ground-water supplies are simply not available (or practically recoverable).

·         Effects of ground-water pumping – due to the relatively slow pace at which effects become manifest in hydrogeologic systems, the full impacts of ground-water pumping on streams may not be evident for decades or longer.

·         Concern for quality – there is increasing concern over the quality of both surface and ground water, which can hinder new water development.

·         Growing demand for diminishing supply – new water needs continue to arise for endangered species, aesthetic and other environmental purposes, urban and industrial growth in the State (include Native American uses) and growth outside the State that would depend on already overextended supplies.

·         Water rights allocation – water resource administration and management needs to consider the allocation of water to existing rights, and in dealing with new projects, also consider reallocation of existing rights and priorities; in New Mexico a water right is a property right and must be protected.

A.                Water issues confronting New Mexico and Gallup

In Framework for Public Input to a State Water Plan (December 2002 – referred to, in shorthand, as “State Plan Framework” or “Framework”), the New Mexico Office of the State Engineer and the Interstate Stream Commission underscore the “key fact about our water”:

New Mexico’s water supply is limited.  Demand, needs, and rights to use water exceed the water supply available in most years.  Many of New Mexico’s difficult water dilemmas arise from these facts.

During drought conditions, the imbalance becomes acute.  After decades of promoting water use, New Mexico lacks both the physical facilities and the administrative infrastructure to ensure available water is delivered on the basis of water rights priorities to senior water-rights holders.  The other side of the coin is that in most places we lack the means to limit water uses by junior water rights holder whose demands cannot be met from the available supply.  Nor have water users been adequately informed about the serious nature of problems sparked by unauthorized use. …

This problem of demand exceeding supply affects virtually all water planning regions.  Those that do not experience water shortages themselves are often viewed as a potential source of water by thirsty neighboring regions.

The unusually wet decades of the 1980s and 1990s have allowed hard decisions to be deferred despite large increases in population and water demand.  The Southwest is due for a drought on the order of a 1950s drought.  Even the few dry years that have occurred in 1996, 2000 and 2002 have seriously taxed our ability to meet fundamental demand.

Governor Richardson’s campaign document, now being used to guide actions of his administration, H20 New Mexico: Bill Richardson’s Plan for Water Security paints the State’s water picture in even stiffer terms:

With fires burning, cities and farms imposing strict water use limits and court rulings which may force us to deny water to entire communities in the southern part of the state, New Mexico faces a water crisis.   However, it is a crisis borne – in part – from a lack of leadership, long-time inaction and poor management.

The drought has brought long-simmering problems to the front burner and the time for aggressive and creative solutions – both short term and long term – is now.

The State Plan Framework document summarizes the State’s major water issues as follows:

Total withdrawal of water from streams and aquifers in 1995 was more than 4.4 million acre-feet (ac-ft; acre-foot is the equivalent of about 326,000 gallons).   About 2.8 million ac-ft was consumed, and the remaining 1.6 million ac-ft flowed back to rivers and streams.  Some current water supply is causing essentially permanent depletion of stored groundwater.  Groundwater historically and current pumped from some stream-connected aquifers will exert an increasing depletion of streamflow for years to come.  Major changes are occurring.

Many issues are common to many river basins and broad regions of the state, including:

§           New Mexico is unprepared to see that its total water uses do not exceed its total legal entitlements from its various sources of supply.

§           More than 90 percent of New Mexico residents depend on groundwater for their drinking water supply, not to mention the many areas that use groundwater for agricultural and industrial purposes.  In many areas, groundwater is not replenished on time scales that have human meaning.

§           More effective water management, conservation, discontinuance of existing uses of water so that new uses can proceed, and new supply development are the primary means we have for meeting new demands.  Current funding is inadequate.

§           Rainfall is highly variable and droughts recur.  Areas that depend only on surface water supplies are especially vulnerable and must plan for dry years.  Conjunctive management of interconnected groundwater and surface water rights becomes particularly challenging in times of surface water shortage.  This is because of the continuing and uncontrollable diminishment of surface water flows caused by historic groundwater pumping.

§           Environmental needs for water have the force of federal law and are the subject of much litigation.  Legitimate environmental water needs have not been  quantified and were not taken into account when New Mexico’s water supplies were fully allocated to other uses.  Nonetheless, these legitimate needs must be accommodated but in compliance with state laws and water resources administration.

Water demand keeps increasing – both within New Mexico and beyond our borders.  Interstate and international issues are of urgent concern in many areas, owing to interstate compact obligations, unregulated groundwater pumping just across the state line, efforts to export water, or water quality desires.  Starting in 1998, federal agencies and judges have imposed demands for water to comply with federal law.  These demands did not previously exist and have resulted in major changes in the operation of federal water supply reservoirs upon which New Mexico water uses depend.

With regard to issues affecting Gallup and its basin, the State Plan Framework document suggests the following:

Water Development:  The Navajo-Gallup Water Supply Project would divert water from the San Juan River for delivery and use in Gallup and surrounding communities within the Little Colorado River Basin.  The Project is being planned by the Bureau of Reclamation to provide a renewable supply of 7,500 ac-ft of water per year to the City of Gallup to both replace existing groundwater uses and meet projected future water demands.  An additional 6,500 ac-ft of water per year would be delivered for use by Navajo communities near Gallup.  Community water distribution systems operated by the Indian Health Service, the Navajo Tribal Utility Authority and Gallup need to be upgraded to accommodate delivery of the Project water.  Federal funding and local cost shares likely will be needed to fund the Project.  The financial feasibility for the Project has yet to be established.  Project issues relating to compact administration, federal environmental law compliance and a possible Navajo Nation water rights settlement in the San Juan River Basin [… are all currently being worked on].

Federal Environmental Laws:  Riparian habitat in the Little Colorado River Basin provides some habitat for the Southwestern willow flycatcher, which is listed as endangered under the Endangered Species Act (ESA).  One area that the Southwestern willow flycatcher may seasonally occupy is along the Zuni River.

With regard to Gallup’s potential interaction with and dependency upon the San Juan River Basin, Gallup’s fate is closely joined with that of its Navajo Reservation neighbors.  The State and the Federal government have recognized that a majority of rural Navajo residents have inadequate domestic water supplies, and this need is a primary basis for the intense planning work accomplished in recent years on the Navajo/Gallup Water Supply Project (NGWSP).  The environmental, legal, jurisdictional, political and financial issues confronting that project, however, have been – and continue to be – far-ranging and complex, although significant strides have been taken in recent years to greatly increase the possibility of the project’s successful authorization and construction in the near future.

Among the issues of highest sensitivity and importance for the NGWSP – and therefore for Gallup’s water future – is the relationship of the City of Gallup (as a political entity, a population, an economic center and a culture) with its Navajo neighbors.  This relationship has many dimensions, some of them apparently contradictory, and the present opportunity for the City is to act in a manner that both heals and diminishes the effects and memories of past (and current) conflict and mistrust, while at the same time building new bridges of understanding, mutual respect and partnership.    

 

B.               Water Management Alternatives

Mature planning processes involve a clear identification of needs, problems and goals, followed by an analysis of options and alternatives for meeting them.  The Town Hall will be calling up all of its participants to help generate and evaluate a broad range of alternative approaches, practices and policies that may secure Gallup’s water future.  A few alternatives will be surveyed here to assist with this exploration.

1.         Water Re-Use, Aquifer Storage and Recovery.  Water re-use may take three forms: 

§               direct re-use, the return of highly treated wastewater into the potable drinking water system;

§               indirect re-use, the return of highly treated wastewater into the potable water supply; and

§               non-potable re-use, the return of treated wastewater for non-domestic purposes, such as industrial manufacturing and irrigation of non-food crops and landscaping.

“Aquifer storage and recovery” is one option for indirect re-use, in which water is reinjected into aquifers, where it is stored.  By this means, evaporation losses and the need for storage structures are decreased.   Aquifer storage may also be a means for storing large-scale project water.   The water is then available for use when other sources are not available.  The City of Gallup is considering this option, as such water could come from the proposed Navajo/Gallup Water Supply Project.  

Indirect re-use of water has the potential to help meet long-term water demands in Region 6.  However, the public is often squeamish about drinking treated wastewater.  Water re-use can also be prohibitively expensive.

John Shomaker & Associates, Inc., provided a brief analysis of the feasibility of aquifer storage and recovery for the City of Gallup.  He noted that the source aquifers for Gallup are confined and have very low hydraulic conductivities and storage coefficients.  Because of the low conductivity, groundwater movement is relatively slow.  Injected water would stay within reach of a recovery well for a longer than typical period, and the rise in water levels would take a long time to dissipate.  Therefore, longer recovery periods than usual (one season) might be feasible.   He also noted, however, that aquifer storage is sensitive to the quality and chemical characteristics of the water, and further studies would be required.

2.                 Water Conservation.  The State defines “water conservation” as “any action or technology that reduces the amount of water withdrawn from water supply sources, reduces consumptive use, reduces the loss or waste of water, improves the efficiency of water use, increases recycling and reuse of water, or prevents the pollution of water.”  Given Gallup’s high-desert climate (less than 13 inches of annual rainfall), its rapidly depleting aquifers, increasing demands on its water supply by regional population pressures and tourist traffic, and the potentially high costs for new water supply, the citizens of Gallup may be well advised to forge a community  water conservation program utilizing “best practices” and emerging technology being applied in various places in the world. 

The New Mexico Office of the State Engineer has produced two excellent guidebooks for water conservation:  “A Water Conservation Guide for Commercial, Institutional and Industrial Users” (1999) and “A Water Conservation Guide for Public Utilities” (2001).  The reader is referred to those sources for in-depth presentations on a wide variety of conservation measures that can be ordained and implemented in the interest of conserving precious water supply.  For the present background document, a few excerpts from the “Public Utility” guide will be shared to provide context for citizen discussion of the many options available.

Even in the best of years, water is a limited resource in New Mexico.  Local rainfall varies throughout the state, but the statewide average throughout New Mexico is less than 13 inches of annual precipitation. … Because of the arid climate, water conservation is vital to the health and welfare of every community in New Mexico.

Unfortunately, competition for the state’s limited water resources is growing.  New Mexico’s population growth is increasing the demands on the state’s already-scarce water supplies.  For the first time, water demands in some of the state’s urban areas [read:  Gallup] are approaching available supplies.  The state’s agricultural users want to retain their water resources in order to protect their livelihoods.  Recreational users need adequate streamflows to meet their needs and protect the interests of the recreation industry.

Environmental factors and concerns also have an impact upon municipal water supplies.  Citizens are concerned about protecting riparian areas and the aquatic habitats of rivers and streams.  The Endangered Species Act requires that adequate water supply must remain in rivers to protect endangered fish.  Another concern is water pollution, which has contaminated water wells in several municipalities in New Mexico.  The water in these polluted wells is not available for drinking purposes, which further reduces the available water supply.

The state also appears to be in a long-term drought cycle that began in 1996, making statewide water supplies even more precious than before.   As a result, some municipalities have enacted mandatory water-use restrictions.  Other communities have ventured into the water rights marketplace to purchase water from agricultural users in order to meet urban water demands.

Because the costs of water development and treatment continue to rise, many communities are faced with expensive water and wastewater treatment facility expansions to meet growing water demands.  Fortunately, water conservation can delay, and in some cases actually eliminate, the need for these costly infrastructure expansions.  The simple fact is this:  conservation is almost always the least-costly water supply alternative.

…Reducing water demand may add years to the life of aquifers that are being mined, reduce the cost of water and wastewater treatment, save energy, postpone or eliminate the expansion of water treatment and distribution systems, and decreases the volume of wastewater discharged into rivers and streams.

For its part, the City of Gallup has been praised for its efforts in conservation, and the community may also benefit from further measures to achieve water savings in Gallup’s high desert environment.  The City’s current Water Utility Conservation Program was highlighted in the State’s “Water Conservation Guide for Public Utilities” (see excerpt in the Appendix), which can be summarized as follows:

Ø      Gallup has a relatively low rate of water consumption (154 gallons per capita per day, or gpcd), and its residential indoor consumption of 64.5 gpcd is close to the State’s benchmark of 55.8 gpcd for “highly efficient households.”   In most communities, residential customers account for over 50% of water use, but Gallup residents consume only 35% of municipal water.  Gallup Water Superintendent Lance Allgood credits Gallup’s high-desert climate as a factor in Gallup’s low water use, since many residents do not even attempt to grow lawns.

Ø      Many of Gallup’s conservation efforts, including its water ordinance, were precipitated by a series of water shortages.  From 1950 to 1980, Gallup’s population doubled in size and its water consumption increased almost sixfold.  In the 1970s, the shortages were so severe the city drilled emergency wells and nearly ran out of water during the peak summer months.  Gallup passed conservation and water waste ordinances in 1983.  The mandatory year-round ordinance prohibits watering that results in ponding or wasted flow; washing of hard-surfaced areas; the use of non-recirculating water in fountains and ponds, new car wash systems, and industrial laundry systems; and the use of water for construction activities.  Under emergency conditions, the City Manager may limit irrigation times, prohibit irrigation, impose a water rate surcharge, and declare a temporary moratorium on any new development including lawn installations.

Ø      Conservation has been helped by Gallup Joint Utility’s “inclining rate structure” (increasing cost per unit of water as volume of use increases), in effect since the early 1990s – possibly the most effective means of conserving.  For example, water production fell nearly 9 percent in 1999 when a significant rate increase was instituted at mid-year.  Rate increases are most effective when coupled with public education, so the City sends out conservation information to its customers just before the summer peak usage season, provides pamphlets on xeriscaping, irrigation and indoor conservation, and makes presentations at schools.

Ø      In 1983, Gallup participated in a public education program funded by ACTION and the US Department of Energy, which distributed thousands of water conservation kits.  The project cost was $1.000 per 1,000 gallons saved, and it helped drop consumption from 160 gpcd to 150 gpcd.

Ø      The City has attempted to control commercial use, which accounts for 62 percent of demand.  The conservation ordinance bans single-pass cooling systems in new or retrofitted establishments.  There is no mandate on linen and towel washing in hotels, largely due to lack of manpower for enforcement.

Ø      Water concerns have prevented high-water-use industries from locating in Gallup due to limited water supply and the expense of treating water to industry standards.

Ø      Gallup reuses sewage effluent to irrigate the City golf course and two sports facilities, saving an estimated 264 million gallons over three years, and delivers 1.7 million gallons of non-potable water per year to irrigation systems on medians and landscapes in 25 locations.

Ø      Future goals and plans include significant development of water reuse strategies – including an aquifer storage and recovery program.  The technology is available, but there are regulatory and public education hurdles to overcome (e.g., perceptions around drinking treated wastewater).  Funding is also needed for implementation, but most funding as been for developing conservation plans.  Other goals include:

o        improving the municipal wastewater system by increasing treatment and hydraulic capacity (costs estimated as high as $30 million);

o        improving residential irrigation conservation, such as through seasonal rate increases and enforcement of existing ordinances;

o        promoting conservation by emphasizing that it reduces the money required for wastewater treatment, and implementing a more formal and comprehensive program.

Other conservation practices recommended by the Office of the State Engineer as having significant potential achieving positive results include:

§           In-school education programs to instill the “conservation ethic” in young minds;

§           Improved metering of all water uses;

§           Improved recordkeeping and water audits (water demand analysis);

§           Leak detection and repair programs;

§           Pressure reduction;

§           Indoor plumbing fixture and appliance audits and retrofits;

§           Xeriscaping and Landscape Design Ordinances;

§           Landscape Irrigation audits;

§           Training landscape maintenance personnel;

§           Irrigation Management Information System (IMIS);

§           Irrigation with Reclaimed Wastewater;

§           Water Waste Ordinances;

§           Emergency Action Plan for Drought Management

Even so … consultations by technical experts and advisors in the Region 6 water planning process have suggested that, especially in light of Gallup’s relatively low per capita water usage (particularly in the residential category), “conservation is not enough” when it comes to meeting Gallup’s water supply needs.   Although enlightened and effective conservation policies and practices may go far in reducing unnecessary demand on the water system and achieving important “water savings,” such efforts by themselves may only delay the inevitable, i.e., the depletion of the ground-water aquifers historically accessed to supply the water needs of the City.  Additional alternatives – “beyond conservation” – are suggested in the following section.

C.               New visions, new technologies, new alternatives

There are many “possible futures” for Gallup’s relationship with the “water of life.”  This section will showcase three bold initiatives, each approaching the challenge from a different angle, but all of them serving a complementary whole in terms of engaging the energies of City leadership and area citizens in a shared commitment to a prosperous and water-enriched future.

1.          Navajo/Gallup Water Supply Project

The Navajo/Gallup Water Supply Project has evolved over four decades as a major infrastructure initiative to identify and secure a sustainable 40-year water supply for the parched lands of the eastern reaches of the Navajo Reservation, the City of Gallup, and the southwestern portion of the Jicarilla Apache Reservation.   The Project is the region’s best solution to the challenge of providing municipal and industrial water supply:

(a)          to rural Navajo communities that to this day are largely dependent on water-hauling and/or short-term groundwater systems with limited long-term supply

The Project is particularly responsive to the development needs of the Navajo Nation, and of Gallup as its neighboring trade center.  The lack of infrastructure, of economic development and of means of livelihood are closely connected.  Throughout the arid Southwest, and especially on the Navajo Nation, a reliable water supply is essential for stimulating and sustaining economic development.  The Navajo Nation has identified economic growth centers throughout the Reservation, which represent relatively large population bases with the potential to benefit from an “economy-of-scale” infrastructure development such as NGWSP. While creation of adequate water infrastructure does not guarantee sustained economic growth nor the narrowing of socioeconomic disparities between the Navajo people and the rest of the US, such development is a necessary prerequisite.  The addition of this significant piece into the Navajo Nation’s infrastructural puzzle will generate extraordinary new development and will hasten the “closing of the economic gap” for the Navajo people.

(b)          to the City of Gallup and its neighbors, who face the prospect of critical water shortages within 10 to 15 years as a result of the loss of accessible groundwater from a century of groundwater “mining”

As a regional trade center, the City of Gallup supports a municipal population of about 23,000 but also serves as an economic hub for a trade area of about 100,000 people.  The City relies solely on a groundwater supply that continues to be progressively mined with little recharge into the source aquifers.  Current hydrologic projections by the City predict severe shortages in the groundwater supply within 10 years, which would have severe social and economic impacts on the City and on the neighboring Navajo communities.

(c)           to the southwestern portion of the Jicarilla Apache Nation for future housing and economic development. 

The Jicarilla Apache Water Settlement Act awarded 25,500 acre-feet of San Juan Basin water rights to the Nation, not all of which is included in the “environmental baseline” determined for endangered fish species.  Under this settlement, Jicarilla has authority to conditionally market its water rights, which might include leasing water to Gallup as part of a three-party agreement that would also include the Navajo Nation.  At the same time, Jicarilla needs an actual supply of “wet water” to begin development of the southwestern portion of its reservation, currently estimated at 1,200 acre-feet.  Jicarilla’s cooperative participation in the Project may help achieve a mutually beneficial water solution for all three project entities.

Under the guidance of a local Steering Committee chaired since 1991 by the Northwest New Mexico Council of Governments, and in collaboration with the US Bureau of Reclamation, Project planning has progressed to the point that prospects are imminent for identifying water sources, settling tribal water rights claims, finalizing the project plan, providing for project financing, publishing the final Environmental Impact Statement, and achieving Congressional authorization for construction of the project.  

A substantial Technical Memorandum was distributed by the Navajo Nation in 2001 to key local, tribal, state and federal players as a means of consolidating information needed for the Project’s primary participants – the Navajo Nation, the City of Gallup, and the Jicarilla Apache Nation -- to define their commitments to the Project.  Based on such commitments, tremendous progress has been achieved, e.g.:

Ø      the participants finalized a Project Definition that articulated the “preferred alternative” for providing long-term water supply to the service area and defined the key project features and the operation of those features; 

Ø      the Bureau of Reclamation has completed appraisal-level engineering designs and estimates for the project, with construction costs estimated at $440 million, as well as substantial environmental analysis as required by the National Environmental Policy Act (NEPA);

Ø      the State of New Mexico completed a revised water depletion schedule under the Colorado River Compact, which includes depletions for the Navajo/Gallup Water Supply Project, within the State’s Upper Basin Compact allocation.  The parties have proposed depletion guarantees limits that would ensure protection of the endangered species of fish in the San Juan River;

Ø      the State of New Mexico and the Navajo Nation have achieved significant progress toward agreements with other Colorado River Compact states to transfer water from the Upper to the Lower Basin for the NGWSP project;

Ø      the State of New Mexico and the Navajo Nation have made substantial progress toward finalizing a settlement of Navajo Nation water rights claims in the San Juan River Basin;

Ø      a “Final Environmental Impact Statement” and “Definite Plan Report” will be completed by the US Bureau of Reclamation in 2003 that will adequately describe the Project for possible Congressional authorization in FY 2004;

Ø      the City of Gallup completed a USDA-funded study of its water distribution system in anticipation of the new water supply from the pipeline and with provisions for conveying water through its system to the adjacent Navajo Chapter communities;

Ø      the project received an appropriation of $1.6 million from the 2002 & 2003 sessions of the State Legislature, to be used to develop the “Gallup regional water system.”  This system will interface with water infrastructure projects being carried out by the Indian Health Service;

Ø      a binding agreement is being forged between the participants, as requested by the New Mexico Congressional Delegation, regarding implementation and financing of the Project; and

Ø      legislative language is being drafted for Congressional authorization to construct the project, with construction anticipated to begin by FY 2006.

The Technical Memo and the Bureau of Reclamation reports draw on studies of the Project conducted from the 1970’s to the 1990’s by the US Bureau of Reclamation, as well as on additional work by the Navajo Department of Water Resources, the City of Gallup, and the Northwest New Mexico Council of Governments.  Federal planning funds totaling nearly $2 million have been appropriated and utilized over the past decade, matched by local and Federal cash and in-kind contributions of over $500,000.  A new planning appropriation of $300,000 is in the administration’s FY 2004 budget. 

The project’s selected pipeline alignment provides for a western component that takes San Juan River water from the Public Service Company of New Mexico diversion structure in Kirtland (downstream from Farmington to its west) and conveys it westward to Shiprock and State Highway 666, thence southward to Yah-ta-Hey junction north of Gallup, with laterals to Window Rock and other communities in the eastern Navajo Nation, as well as an eastern component that includes a pipeline extending southward from the Cutter Reservoir to the Counselor area of the eastern Navajo Reservation, with access at TeePee Junction by the Jicarilla Apache Nation.  In summary, the project will divert about 36,000 acre-feet of water annually from the San Juan River for municipal and industrial use within a service area defined by the following: 

Ø      43 Chapters of the Navajo Nation in its Northern, Eastern & Ft. Defiance Agencies, including service to the Window Rock area and to Chapters contiguous to the City of Gallup;

Ø      the southwestern portion of the Jicarilla Apache Nation; and

Ø      the City of Gallup proper.

 

2.                The Canyon Project”:  Opportunity from Diversity

As an extension of the Water Re-use strategy described above, the “Canyon Project” has been proposed as an idea with potential to enhance and secure the future water supply for Gallup.  This project, as outlined by Water Superintendent Lance Allgood, would provide a secondary use for the treated wastewater stream, thus producing net “water savings” of up to one-third of the City’s projected annual water demand at the 40-year horizon. 

The Canyon Project  would divert and lift all or a portion of the current effluent from the City’s Wastewater Treatment Plant to a discharge point about 2¼ miles north of that facility.  The water would be released at the head of a scenic canyon, where it would flow through a series of ponds, streams and wetlands, culminating in a large lake near the mouth of the canyon. The lake would store water for several water reuse projects.

Although high evaporation and transpiration losses would occur throughout the project, such loss would be from water that would otherwise simply flow down the Rio Puerco unused.

At present the average daily discharge from the Wastewater Treatment Plant is about three million gallons per day (3 MGD).  Except for about 0.65 MGD, the City currently discharges all of this treated wastewater into the Rio Puerco.  During the growing season and intermittently during the remainder of the year, this .65 MGD is utilized at the City’s Golf Course, the Sports Complex and the Soccer Fields located near the Plant.  This use is widely variable and dependent on weather patterns and natural precipitation.

The Canyon Project would provide an estimated one billion gallons of storage in the course of a year, thus making  water available for secondary uses throughout the year.   Beyond simple storage, the project would also provide many diverse opportunities and benefits.

The City is contracting with the US Bureau of Reclamation to conduct an appraisal-level study of a Reverse Osmosis (RO) filtering system to remove salts from the effluent stream, making it much more useful for irrigation. The RO process will also treat the water to a standard that is “all but drinkable,” with almost no limitations on its application.

One concept for The Canyon Project, with maximum efficiency in mind, is to locate all or the largest portion of the City’s sports and recreation facilities within the project’s boundaries.  This arrangement would enable the City to utilize reclaimed water for the irrigation of these facilities, freeing about .5 MGD of the City’s drinking water for other uses during peak use periods.  This is much more economically feasible than piping and pumping reclaimed water to the City’s recreation facilities at their present locations.

Such focused use of water would not imply that the City’s neighborhoods would lose their parks; rather, that there would be fewer irrigated fields in such neighborhood parks, and some currently irrigated spaces could be converted into dry basketball, tennis courts and playgrounds.  This downsizing of the parks would also create an opportunity for the sale of the resulting surplus City property to prospective developers.  As such property is within the City limits and is generally served by City utilities, resale of the City properties would provide the opportunity for development without expansion of the land base, i.e., a concept that is in line with the City’s Growth Management Plan.

Another benefit of the Canyon Project would be the constructive reuse of high-nutrient sludge.  The City is currently disposing of the solids (sludge) generated as a part of the wastewater treatment process by simply tilling it into the soil – with no real benefit.  By adding a step to the treatment process, the City could bring the sludge to a level of treatment where it could be used as a fertilizer and soil conditioner without limitation. Sludge of this quality would have a significant beneficial application within the theme of the Canyon Project.  Whatever sludge is not used may well be a marketable product, thus helping to finance the additional treatment process.

In terms of environmental enhancement and “working with nature,” the project would create a much more diverse wildlife habitat than presently exists.  This would benefit not only the resident wildlife population of mule deer, fox, coyote, bear, cougar, bobcat, squirrels, and rabbits, but also many migratory birds that pass through the area on an annual basis. 

One only has to look to the City’s much smaller project at its public Golf Course to see the possibilities of enhanced wetlands for attracting both resident and migratory wildlife species.  Since its completion in 1995, the recirculation stream and storage pond at the Golf Course has attracted many migratory bird species, such as mallard, pintail, common coot, green wing and cinnamon teal, wood duck, heron, egret, common snipe, redwing black birds, dippers, ibis, plovers, pipers, and songbirds.  Following in the footsteps of these species have been local predators such as fox, coyote and raptors, which have begun to make regular appearances at the Golf Course.  A nature-based water re-use facility as large and diverse as the Canyon Project could expect to attract a large majority of migratory birds common to the area’s flyway.  Many people travel great distances to view these species at other locations within the state.  Gallup might well be added to their list if this project were to occur.   It would also provide local residents and neighbors – who just can’t find the time to get away to other distant locations – a place where they could go to view the splendor of nature.

Some in our community have talked of creating a hands-on museum for our youth.  What better place would there be than within the Canyon Project area? This idea might be expanded to include a “sustainability museum” showcasing emerging technology and approaches to sustaining our environment. The plans of the Gallup Campus of the University of New Mexico for a botanical garden is complementary to this idea.

 The Canyon Project also provides many educational opportunities, in that it would create a “living classroom.”  Many of our country’s emerging environmental and water reuse technologies could be put to use and tested as a part of the project. This opens the door to an emerging environmental technology curriculum in our schools, as well as to possible full-blown undergraduate and graduate college programs. 

A local plan to restore a portion of the riparian habitat along the Rio Puerco lies within the Canyon Project boundaries and would fit well into the project.  The Project area is a perfect venue for – and doorway to – the “Adventure Gallup” project, which is a far-ranging community initiative to attract local residents and visitors into a series of biking and hiking trails, as well as other outdoor adventure activities, in the surrounding hills and valleys. The Canyon Project would also incorporate riverwalks and wildlife viewing platforms. The combination of these projects has a huge potential for attracting many travelers who may otherwise just pass by Gallup.  The restoration project is described in the next section, referring to the maps included in the next two pages.

Finally, as technology develops and public opinion changes, water from this project would be available for final treatment and return to the drinking water supply.

If even a portion of these visions were realized, the Canyon Project would create opportunities for commercial development, such as:  an Indian Village and marketplace; Curio/Gift shops; restaurants; motels; daycare centers; guide services; and other economic and eco-tourism activities. Ultimately the project could become a destination resort for the “environmentally conscious.”

In summary, the Canyon Project’s potential benefits include:

§         Reduced demand on the City’s drinking water supply through indirect reuse (for example, offsetting the use of drinking water currently used for irrigated lawns);

§         Provision of a living classroom for both high school and college programs;

§         A destination venue for eco-tourism;

§         New economic development opportunities;

§         Expanded and enriched recreation venues;

§         Diversified and enhanced wildlife habitat

§         A model of sustainability through reuse.




 

3.            Rio Puerco Restoration Project

 

The Rio Puerco Restoration Project is a planned restoration of the first one-mile reach of the Rio Puerco of the West immediately downstream (west) of the Gallup, New Mexico Municipal Water Treatment Facility. The area in question is located approximately 5 miles west of Gallup in T 14 N., R 18 W, Section 23. The project is to be carried out by Connections, Inc., a local 501 (c) (3) not-for-profit community service organization, with the sponsorship of the McKinley County Soil and Water Conservation Board.

The project area entails land south and north of the Rio Puerco of the West, parcels owned, respectively, by the City of Gallup and Gamerco Associates, both of which have given permission for the project.  The “river” here mimics a perennial stream due to the release into the riverbed of approximately 3 million gallons of treated effluent from the adjacent Water Treatment Facility. This effluent is of sufficient quantity to allow and facilitate restoration of a narrow but significant bosque.

The Rio Puerco Restoration Project is an extension of a major local economic development and quality of life enhancement program called “Adventure Gallup,” a large-scale effort to develop adventure tourism in the Gallup area through the development of an extensive network of trails and rock climbing venues in the rough country surrounding Gallup. Both the City of Gallup and McKinley County are sponsors of Adventure Gallup. Specifically, Gamerco Associates, the largest private landowner in the area, has agreed to allow these developments on multiple sections of its lands bordering the Rio Puerco west of Gallup.

The Rio Puerco Restoration Project will adjoin the Adventure Gallup lands and constitute a “soft” addition emphasizing land and water stewardship, education for citizens of all ages, and a valuable and inspiring example of ecological restoration. It is hoped that eventually the restored river will be the centerpiece of a nature refuge and environmental education center along the lines of the La Semilla Park, the New Mexico State Land Office/ Allan Savory Center for Holistic Management partnership to be created adjoining the new Mesa del Sol development in SE Albuquerque. Extension of this project is also preliminarily adopted by the Little Colorado River MOM as a major portion of its projected major basin-wide initiative through US EPA.

Scope:  The project will entail 4 major foci:

  1. Moving the effluent from the current “ditch”, a deeply incised and linear artificial channel created years ago, into the original river bed, which is immediately adjacent to the north. This bed retains most of its structural integrity and considerable natural meander. The move will entail approximately a 200 foot extension of the effluent pipe so that effluent can move past the “ditch” into the original river bed. It will also entail minor damming earthworks to block off the original bed from various “leakage” points into the “ditch.” This portion of the work re-establishes the original reach of the river.
  2. Eradication of salt cedar and other invasive species along both the ditch and the adjacent stream bed. This will be accomplished using aerial (helicopter) application of Arsenal herbicide, by far the most effective method, and the one currently adopted by the State of New Mexico for its Rio Pecos and Rio Grande salt cedar eradication projects. Arsenal will not hurt animals and has had a 97% effectiveness on salt cedar to date. Die-off occurs over one growing season, following which the dead salt cedars are mechanically removed from the stream course.
  3. Pole plantings of willows, cottonwoods, and other native species along the stream channel. The poles are obtainable from Bosque Del Apache, the Plant Materials Center, and various other sources. Plantings will be accomplished by local volunteers and some paid assistants. Monitoring and ecosystem planning will be integral to this phase and will be accomplished by knowledgeable Connections, Inc. employees, area volunteers, NRCS, and local college classes.
  4. Planning for the eventual Nature Preserve Environmental Education Center. This will be accomplished by Connections, Inc. in conjunction with the Allan Savory Center for Holistic Management and the Center for Sustainable Environments at Northern Arizona University.

Duration:  Connections, Inc. is ready to move on the Rio Puerco Restoration Project as soon as funding is available. With adequate funding the project as outlined above could be well along within 2 years. The Santa Fe River Preserve, a somewhat similar restoration project in Santa Fe, achieved significant riparian regeneration within 2 years.

The Rio Puerco Restoration Project fits extremely well with the “Adventure Gallup and Beyond” economic development project which is central to current and future local planning, and is, as well, a natural lead in to the “Canyon Project,” described elsewhere in this report. (See accompanying map). It would entail beatification of the south side of the Adventure Gallup area to which it would be connected via one or more aesthetically pleasing foot bridges. It would entail the construction of walking paths on both sides of the river, an area for both strolling and the discovery of new riparian life along what has always been the River of Life in our area.

Work on the Rio Puerco Restoration Project would be accomplished through multiple sources. Partnerships are already being formed among the following, all useful for overall success:

  1. McKinley County Soil and Water Conservation District.
  2. Natural Resources Conservation Service
  3. Connections, Inc.
  4. McKinley County
  5. City of Gallup
  6. Northwest New Mexico Council of Governments
  7. Little Colorado River Resource Conservation and Development Project
  8. Plateau Sciences Society

Together, this partnership provides a powerful combination of knowledge and resources to bring the Rio Puerco back to health and beauty. Together with the “Canyon Project” and “Adventure Gallup and Beyond,” it would be a model for low-impact sustainable development for the arid Southwest.

Economically speaking, the larger project could also generate funds for its enhancement by becoming an example of conscious living. If properly described and marketed, it would attract eco-tourists, a growing and lucrative market, to come to Gallup not only as observers, but as participants in the growing of the ever-developing eco-city of the future. Increasing thousands currently engage in similar endeavors in the Costa Rican rainforest, Nature Conservancy habitat restorations worldwide, and various “citizen archaeology” programs. Often these eco-tourists “adopt” a certain area, return often, and give large amounts of money to enhancement efforts extending over many years. Adoption of a sustainable future arid lands sustainability project based on Rio Puerco Restoration and the interconnected Adventure Gallup/Canyon Project would appeal to many visionary investors, and Gallup could become a model for such development in arid lands internationally, where arid lands make up roughly 30% of all lands.

The Rio Puerco Restoration Project also entails one other gift for Gallup. That is its value as a metaphor of hope, hope that together we can bring back Mother Earth and find sustainable development as we focus on all of us together as living systems. We can succeed economically as we demonstrate our joy in new and sustainable development.


IV.            WHERE DO WE GO FROM HERE?

 

A.                Designing a Desired Future

The Gallup Town Hall on Water is designed to evoke ideas:  new insights and analyses into Gallup’s “water crisis”;  discussion of new possibilities in how we collect, use, re-use, conserve and share water;  presentation of new technologies, products and projects with the potential to achieve water savings and/or augment the City’s supply of water; recommendations on strategies, political actions, financing and policies for consideration and implementation by the City and by its ever-growing circle of citizen-advisors.

The Mayor’s task force would encourage all Town Hall participants:

·            first, to participate in the Town Hall with an open mind – being available to the information, perspectives and ideas shared throughout the event;

·            second, to approach the “water crisis” issue in the spirit of “opportunity” – looking for constructive ways out of the dilemma and toward  a water-secure future;

·            third, to be visionary in considering the community’s possible futures – seeking mental pictures and models of “ideal” conditions to which the community can aspire, given our inherent geographic limitations but our infinite capacity to adapt, create and move forward;

·            fourth, to be proactive, innovative and creative in providing ideas and suggestions, since this approach provides the most fertile opportunity for discovering breakthrough strategies and effective paths of action; and

·            fifth, to be prepared to be part of the solution as the City moves forward to implement the ideas and recommendations of the Town Hall.

B.                Critical questions

And so, we – the citizens, friends and neighbors of Gallup, New Mexico – gather to consider the challenges before us.  In the Town Hall workshops, a series of critical questions will be asked.  These may be asked in a variety of ways by the workshop facilitators, but they will eventually concern the following core issues:

1.            WATER SUPPLY OPTIONS – What are our feasible water supply options?  What are the constraints and opportunities that affect our choices:  hydrological?  technical?  financial?  legal?  political?

2.            WATER CONSERVATION – What does “conservation” mean under our circumstances?  What benefits can be gained from a comprehensive and innovative conservation program?  What are the limits of these gains?  How can we use – and re-use – our water supply in a way that protects and extends our water future?  What happens if we don’t get the Navajo/Gallup project water – or less than we thought; or later than we thought; or more expensively than we thought?

3.            VISION – Given the limitations and costs of water supply for Gallup … what should Gallup look like in the future?  What kinds of economic development make sense?  What new technology might we tap?  What will constitute our quality of life?  What’s going to be the “Gallup Model” of a sustainable town in the Western states?

4.            RECOMMENDATIONS – So … how do we get There from Here?  Who pays – and how?  What commitments need to be made – by the City government?  by the citizens?  What education is needed – of ourselves, of others?  What does a coherent system and policy look like?  How do we get to the “front of the curve” in terms of water management technology?  What should the Gallup Model of an “Active Water Resource Management” system look like?  What’s missing from the dialogue?  What are our next steps?

Forward, then … to Gallup’s water future!


BIBLIOGRAPHY

Sample Listing of Suggested References

City of Gallup References

Well Production Planning Report:  City of Gallup, New Mexico by Sterling & Mataya, & Shomaker.

Water Supply Studies and Forty-Year Water Supply Master Plan:  City of Gallup by Shomaker, Leedshill-Herkenhoff, Sterling & Mataya, & Mason (January, 1991). 

Water Development Plan Update:  City of Gallup Water System by Southwest Water Consultants (August, 2000).

City of Gallup Transmission and Storage Facilities by DePauli Engineering and Surveying (December, 2000).

City of Gallup, New Mexico:  Wastewater Collection/Recycling Model Project Interim Report by DePauli Engineering and Surveying (November, 2001).

Business and Residential Water Use: City of Gallup, New Mexico by DePauli Engineering and Surveying (January, 2002).

Addendum to the Navajo/Gallup Water Supply Project Report “City of Gallup Transmission and Storage Facilities” provided by DePauli Engineering and Surveying Co December 2000// revised January 2001 supplemented by “Business & Residential Water Use” analysis, January 2001 pursuant to USDA/RBEG Grant by Northwest New Mexico Council of Governments (April, 2002)

The Navajo-Gallup Water Supply Project:  City of Gallup Regional Transmission and Storage Facilities by DePauli Engineering and Surveying (April 2003).

Regional References

40-Year Regional Water Plan, New Mexico State Planning & Development District 1:  San Juan, McKinley, and Cibola Counties by Northwest New Mexico Council of Governments; Leedshill-Herkenhoff, Shomaker, & Dumars—consulting authors (March, 1994).

Region 6 Water Plan:  The 40-Year Regional Water Plan for Cibola County and the portion of McKinley County not in the San Juan Basin by Northwest New Mexico Council of Governments; Murnane, Hausam, & Kiely—principal authors (March 1998).

Region 6 Water Plan:  Phase II – Evaluation of Alternatives and Presentation of Strategies by (July 2001).

Handbook for Local Water Planning & Implementation – Water Planning Region 6 by (July 2001).

Region 6 Water Plan:  Plan Summary by Northwest New Mexico Council of Governments;  Kiely, principal author (April, 2003).


Navajo-Gallup Water Supply References

Water Resource Development Strategy for the Navajo Nation by the Navajo Nation Department of Water Resources (July, 2000)

Technical Memorandum:  The Navajo-Gallup Water Supply Project by the Navajo Nation Department of Water Resources, the City of Gallup, the Northwest New Mexico Council of Governments, & the U.S. Bureau of Reclamation (March 2001).

New Mexico References

Taking Charge of Our Water Destiny:  A Water Management Policy Guide for New Mexico in the 21st Century by Belin, Bokum, & Titus (2002)

New Mexico’s Water:  Perceptions, Reality and Imperatives – Report of the Twenty-Eighth New Mexico First Town Hall.  Background report by Johnson & Shomaker (May, 2002).

Framework for Public Input to a State Water Plan by the New Mexico Office of the State Engineer & the Interstate Stream Commission (December, 2002).

Water Use by Categories in New Mexico Counties and River Basins, and Irrigated Acreage in 2000 by Wilson, Lucero, J. Romero & P. Romero (February, 2003).

Other References

City of Grants New Mexico:  40-Year Water Plan by Northwest New Mexico Council of Governments, Sharon Hausam, principal author (1999).

 

 

 

 

 

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