About
Swat
Introduction
The charming Swat, a peaceful and
fascinating tract in the lap of vegetative sky-high mountains, with
eternal snow on their lofty crests, is an everlasting source of
attraction for the visitors. Its beauty attracts tourists from all
over the world to enjoy the soothing and serene sceneries, and the
friendly behavior of its inhabitants. A visitor entered in Pakistan
would never be contented without roaming about Swat.
The area of Swat is 4000 sq. miles with a population of about 1250000.
Its height is not similar but varies from 2500 ft. to 7500 ft. above
sea level.
Colonization
Due to its fertile soil and favorable
climatic conditions, Swat has been the abode of various nations and
subjected to historical events from time to time. Though this valley
has an ancient history, but in the light of historical documents, its
recorded history begins with Alexander The Great, who conquered Swat
in 326 BC.
Alexander defeated Persia, thenceforth, he entered Swat via Kunar in
326 BC. Buddhism was in full bloom here. The Buddhist ruler fought the
Greek invader, but was defeated. Having conquered Swat Alexander
proceeded on along the Right Bank of Swat River. Reached Bandai in
Nekpikheil, he crossed the river and camped near Manglor. He continued
journey through the mountainous passes of Onra, and crossed Indus.
The well-known general of Alexander, Salukis, gave Swat to
Chandragupta back in 304 BC. Another Buddhist king, Kanishka, shifted
his capital from Peshawar to Swat so that he may be peaceful enough to
worship his deities with full satisfaction. Then Raja Ram Batti and
many other great personalities ruled Swat, and worshipped their gods
with full peace and meditation in cloisters. Raja Gira was the last
Buddhist ruler of Swat, who was defeated by Mahmood of Ghazni.
The Arrival of Afghans
In eleventh century, Khwaja Ayyaz went
on the Right Bank of Swat River and conquered the areas of Adenzee,
Shamozee, Nekpikheil and so on. Mahmood went on the Left Bank of the
river, when he reached Hudigram, there was the fort of Raja Gira,
strongly built on a high peak. Mahmood commanded the conquest of this
fort to an adroit general, Peer Khushal. The conquest of the fort was
much more risky, but the order of the supreme commander was complied
with.
Taking charge, the creative minded general besieged the fort for three
days and cut off the underground connection of water link. On the
forth day, he attacked the fort. The attack was a serious one and many
soldiers were martyred, including Peer Khushal himself, but the fort
was captured and since then Mahmood proceeded on and captured the
whole Swat.
After conquering Swat, Mahmood settled two tribes of Afghan here, i.e.
Swati and Dalazak, and went back. Both these tribes were living a
happy life till they were driven away by the Yousafzai tribe of
Pathans.
The Entrance of Yousafzai
King of Kabul, Raja Alagh Baig, who
was dethroned by his own tribe, called the help of Yousafzai to gain
the imperial power of Afghanistan once again. All the chiefs,
and Sardars of the Yousafzai came and supported him strongly. They
fought a battle against Tajack, and Alagh Baig became the King of
Kabul again.
Since then, Yousafzai got an authoritative position in Kabul court and
army. The Yousafzai tribe was settled there permanently. But as the
king was a Tajack, his wife was Tajack, his friends, and his
relatives, shortly all of the concerned people were Tajacks, so the
men of his tribe confided him. They told the king that he would be
afflicted by Yousafzai one day, because Yousafzai were not from his
own race and all the key-posts were in their hands, therefore, they
should be removed.
Since then Alagh Baig schemed that the Yousafzai should be attacked at
night while they are in sound sleep. His army did so, but the force of
the king was defeated badly.
When the elders of Yousafzai protested, the king cunningly expressed
deep sorrows and assured them that some robbers might have taken the
action.
Alagh Baig now made another plan. He invited all the chiefs of
Yousafzai and attacked them while they set to eat. All of the heads
were killed, but only two of them, Sardar Malak Ahmed and Sheikh Malee,
escaped. Both of the leaders migrated to Peshawar valley along with
their tribe-men.
Having been there for a period of time, they visited their Afghan
Brothers, Swati and Dalazak, in Swat, to win their sympathy. But they,
the Yousafzai, were soon attracted by the natural properties of this
area. It should be mentioned here that the Yousafzai learned the art
of betrayal from Tajack. So they compelled the originally settled
Swati and Dalazak to quit Swat, who crossed Indus and took refuge in
western Hazara district (Even now, some of the remnants of Swati and
Dalazak tribes are found in the remote corners of Swat).
Sheikh Mali distributed all the land among the male members of
families of his tribe. According to this scheme, these families would
change their villages after each decade, and the land of the new
village would be distributed among the male family members.
(Finally, the land was allotted permanently under the auspices of
Bacha Sahib within a period of five years i.e. from 1924 to 1929, and
the nomadic life of the residence of this area came to an end.).
Sheikh Malee introduced the units of land also. The smallest unit of
land was Damray, while the largest unit was Rupee.
Having no ruling authority, Swat was subjected to lawlessness and
disorder. Internecine feuds were the common feature of this tract.
When they were tired of mutual bloodshed, they wanted to choose an
impartial man to solve their problems and disputes. For this purpose
they called Syed Akbar Shah, but after ruling for five years he died.
The next personality convened was Syed Abdul Jabbar Shah. He was a
good scholar, and statesman with majestic port. But a well reputed
learned man, Sandakay Mullah soon blamed him as Qadyani (a person
having belief in the prophet-hood of Mirza Ghulam Amad Qadyani), and
so Abdul Jabbar left Swat.
In this connection, the other man was Miangul Abdul Wadood, the
grandson of Mian Abdul Ghafoor (Sahib-e-Swat). The people entrusted
Miangul Abdul Wadood with power in 1915 (But he was formally crowned
in 1916 by the council (JARGA) of the chiefs of Swat in the grassy
ground of Kabal). (He was the man of vigor and high determination.
Formerly, he was the ruler of Swat valley only, but slowly and
gradually, he expanded the border of Swat up to Gilgit. Later on he
retired and his elder son, Miangul Abdul Haq Jehanzeb was crowned as
the “Wali of Swat”. Ruling time of Jehanzeb is considered as the
golden period in the history of Swat. All of his reforms i.e. schools,
colleges, hospitals, roads, and other communication system were
matchless. There was a complete peace and order in Swat. But having
the foresight of the future politics and the reaction of the nation,
he gave up the ruling power in 1969.
| It is painful
to recount the events of the recent past. The fascinating
valley of swat, during the Ex-Wali regime, presented a picture
of the worldly paradise. The Wali of Swat, with |
unique sense of possession left no
stone unturned in beautifying and developing each and every sector of
Swat. He did his best, and had very lofty plans for the future. It had
no match, and the visitors from all over the world had emotional
attachment with the state.
After the Wali regime, the officers/officials with no sense of
possession, did not bother about the development of Swat with the
required zeal and fervor. It not only halted the march to wards
prosperity, but also took us to a very dismal state of affairs.
The schools, roads, hospitals and the colleges of Swat were fully
equipped with the latest trends. The Wali of Swat had plans to
establish a university and professional colleges but the dreams
remained unfulfilled due to the sudden turn of the table. His plans
that soar high to the skies fell to the earth. The roads are no more
useable. The schools and the hospitals have no proper system. The
institutions have been destroyed, and every one devoid of high sense
of national interest, is confined to the personal outlook and personal
interests. This sad state of affairs if prolonged will further
deteriorate the present infrastructure.
Nomenclature:
This is an important point for us to
know, why do we call ‘Swat’ to this tract, and from which source
the name has been contrived.
In the ancient history, the word ‘Swat’ is not found. The early
peoples called this soil with various names, but not by the present
name, Swat. For example, some three thousand years ago, it was called
Udhyana (Garden). In the writings of Chinese travelers, we can find
‘Soto’, while in the accounts of Greeks, the “Asoconoi” has
been mentioned, but Mahmood Ghaznavi has called it ‘Qerat’. So for
as the early names are concerned, Soto has much similarity to the
present name.
The second base for its nomenclature is of Arabic origin. It is said
that the word ‘Swat’ is the distorted shape of Aswad (black). As
the hills and mountains of this land are covered with thick forests,
which appear in sight as black, therefore, it was called Aswad.
Slowly, it became ‘Swad’ but latter on the name changed completely
and the present name ‘Swat’ was composed.
The final decision is lying in the fact that when Mahmood Ghaznavi
conquered Swat, he wanted to settle some of his people to keep the
control of the conquered area. So he settled two tribes the Swati and
Dalazak here. As the Swati tribe was larger, the zone was called by
the name of this tribe, Swat.
Situation:
The valley of Swat is situated in the
north of N.W.F.P, 35° North Latitude and 72° and 30° East
Longitude, and is enclosed by the sky-high mountains.
Chitral and Gilgit are situated in the north, Dir in the west, and
Mardan in the south, while Indus separates it from Hazara in the east.
Physical
Features:
Swat can be divided into two physical
regions:
- Mountainous Ranges.
- Plains.
Mountainous Ranges:
As mentioned above, Swat is lying in
the lap of Mountainous Ranges, which are the offshoots of Hindukush,
so the larger part of Swat is covered with high mountains and hills,
the crests of which is hidden by everlasting snow. Though these
gigantic Ranges run irregularly: some to the west while the others to
the east, but the general direction is North-South. These ranges
enclose small but very enchanting valleys.
Eastern Ranges:
In Kohistan-e-Swat the chief knot of eastern ranges is Mankial. Its
northern branches separate Kohistan-e-Swat from Abasin Kohistan. These
ranges form a barrier between Gilgit and Swat, and between Chitral and
Swat. The southern extension of Mankial ranges reaches proper Swat.
There they join Shangla ranges. Shangla ranges separate proper Swat
from Shangla Par area (Shangla Par district).
In Shangla district, there are Karora Ranges, which separate Puran
from Kanra and Ghurband.
The continuation of Shangla ranges joins Dwasaray. On the one hand
Dwasaray separates lower Swat from Puran, on the other, it set aside
the Buner from Puran.
Now the general Direction of the ranges turns westward. Here it is
called Elum. Elum Ranges is a big wall between the proper Swat and
Buner. The Elum ranges at last join mountains of Malakand.
The Western Ranges:
Western ranges start from the mountain and hills of Gabral, Kohistan-e-Swat.
It joins the hills of Kundal (Utror). There these ranges meet Daral
Ranges. These ranges form a border with Dir district. They run west
ward and are named according to the locality. For example Lalko ranges
Manrai and Chaprai etc. at last they join the hills of Adenzee and
Shamozee. Manrai ranges send off some off shoots southward. They the
hills separate Arnoyay valley from the widest valley of Nekpikheil
valley.
In Buner, there are many ranges of hills. Some of these hills run east
west while others north south. For example Ambela Ranges form a border
between Sodam Rustam (Mardan) and Kawga. Again, there are some ranges,
which separates the surrounding areas of Kawga from Chinglai. The pass
through these ranges is known as "Doormai Kandaw". There
come other ranges. These are the hills of Dambara. So it is hard to
count the actual number of the hills and ranges, but this is a fact
that the major portion of Buner district is covered with hills.
Though, these hills are not as high as hills of Kohistan-e-Swat, yet
they enclose many small charming valleys and are more populated.
In the armpits of these mountains and hills there are small beautiful
valleys, which are praiseworthy, these are limited to the watercourses
of local rivers. The hills or mountains no doubt, enclose these
valleys, but the local people have connected them by narrow path
through high passes.
These mountain ranges have some high peaks, which are capped with
everlasting snow. In the north of Mankial Ranges, Falakseir is a
well-known peak with a height of 19415 ft above the sea level. Chokail
is another sky-high peak in the same ranges, which lies to the south
of Falakseir. The height of this peak is 20528 ft. The third one is
Mount Mankial in the vicinity of Chokail. This mount is 18338 ft high
above sea level.
An explorer submerged in the snow while he tried to conquer them.
However, a Japanese adventurer conquered mount Mankial in 1975.
In these high ranges there are lakes, known as Dand. In Ushu the
famous lake is Mahodand (the lake of the fish).
In the eastern ranges, the other famous Dand is Bashigram Dand.
Though, there are many Dands but Bashigram Dand is very charming. It
seems that this Dand have been made by some gigantic creatures, and
all the big blocks have been prepared very carefully by the sculptor
and have been placed skillfully. The natural scene of this Dand is so
charming that the ex-ruler of Swat has visited it thrice. This Dand is
one of the sources of Bashigram River.
The western ranges, Daral Ranges, have also three big Dands. Two of
them lie in the area of Swat, while the third one is in the boundary
of DIR.
The Dand of Kundal is the largest of all the Dands of these ranges. It
is rather a tiny sea surrounded by the high peaks with murmuring
rills. In the vicinity of this biggest Dand there are two small Dands,
one is called Khaperai Dand (fairy Dand) and the next is the Dand of
Speen Khwar. This Dand is so charming that the ex-president of
Pakistan, Farooq Ahmad Khan Laghari came here by helicopter to enjoy
the enchanting scene of this Dand. Seidgai Dand is second in size, but
it lies out of the borders (watershed) of Swat. It is situated at the
terminal of Wosheray Dara, Dir. It is mentioned here, because, the
pastures of this area are hired by shepherds of Swat. The Dand of
Daral is third in size, which is the smallest one among the big Dands.
These Dands feed rivers. For example, Daral Dand feeds Daral River,
which joins Swat River in Bahrain.
These ranges have good pastures, generally, the areas in the vicinity
of a Dand is used as a pasture. These pastures are very charming. The
land surface is covered with green grass. The grazing cattle, goats,
sheep, cows, horses and even the buffaloes on the slopes seem very
charming.
Some of the famous pastures are Mair, Tolay, Jamdarai, Seidgai,
Tharkana, Kar Banda, Chamber, Jaba, Kundal, Batal, Lado Banda, Loi
Pandghalay etc.
These pastures are lying in the knot of Daral. Moreover, each Spinsar
(denude mount) has pastures. For example, Bashigram Pasture, and the
pasture of Ajmair are at such a height that the rock is denuded, and
have no soil.
The Plain:
The true plain is not found here, yet
the local people call to some areas Plain Surfaces. These so-called
plain surfaces may be divided under the following headings:
- The Valley of Swat.
- The Plains of Buner
The Valley of Swat:
Actually the valley of Swat starts from the foothill of Malakand but
we are concerned with portion from Landakay to Gabral (Gulabad), the
area within the administrative boundaries of Swat.
The length of the valley from Landakay to Gabral is 91 miles. Two
narrow strips of plains run along the banks of Swat River from
Landakay to Madyan. Beyond Madyan in Kohistan-e-Swat, the plan is too
little to be mentioned. So for as the width concerns, it is not
similar, it varies from place to place. We can say that the average
width is 5 miles. The widest portion of the valley is between Barikot
and Khwazakheila. The widest view point and the charming sight where a
major portion of the valley is seen is at Gulibagh on main road, which
leads to Madyan.
There are some subsidiary valleys, which help to increase the width of
the main valley. These subsidiary valleys are called "Daras".
A Dara a narrow passage between mountains, and sometimes, the upper
course of a river is also called Dara. If we imagine the main valley
as a stem of a tree the subsidiary valleys form its branches.
Swat River and its tributaries drain Swat. There fore, the whole
valley is the outcome of running water. This flowing water cuts the
upper courses deeply, and flows the load of washed away materials. As
the gradient is greater in the upper course so the erosion is on large
scale, particularly in the summer rains, when all the rivers are in
flood. The big boulders and stones are rolled, which causes more
destruction in the upper courses. When the loaded water reaches to the
areas of low gradient, the heavier materials are deposited. The
deposition takes place according to the slope, generally, we observe,
that the upper course is made up of big boulders, the middle course is
of relatively small stones, pebbles, and debris, while the lower
course is made of fine clay. Anyhow, the whole plain of Swat valley is
strewn by the running water, and is made up of fine alluvial soil.
The Plains of Bunair:
Buner has also an irregular plain surface but there are not such
active perennial rivers as in the valley of Swat. Only Barandu is the
river, which has a little water flowing through the whole year. Many
of the rivers of Buner are inundation rivers. When the rain stops,
there is no sign of water in the watercourses. It should be kept in
mind that there are two Buners: Upper Buner and Lower Buner (Chamla).
Barandu and its tributaries, the Jowar River and Kohqand River, drain
the upper Buner. Barandu joins the Khwar (a big watercourse) of
Chagharzee. (In Chagharzee, There are three Kwars: one Khwar flows
from Bar Shamnal, next from Gulbandai, and the third is the Khwar of
Pandeer.)
The lower Buner, Chamla, starts from Ambela Kandaw and reaches to
Swabi.
We can find plain areas in Upper Buner like Jowar, Anghapur, and
Swarai up to Budal, and in Lower Buner or Chamla: Chinglai and
Khadukheil. The area of Kawga, Nawagai, and Sora may be grouped as
plain to some extent.
As many of the rivers in Buner are inundation or rainy rivers, and
their upper courses are short, therefore, the deposition of clay is
started just at the foot of the hills. This is because the whole
surface of Buner Plain is made of clayey materials. The thickness of
the layer of clay is greater here.
Climate:
Swat is lying in the Temperate Zone in
the northern mountainous ranges of the Indo-Pak Sub–Continent,
therefore, here weather is affected by all the climatic factors
“latitude, altitude and rain bearing winds” (the cyclone and
monsoon winds).
In summer, Swat comes under the influence of the monsoon, while in
winter, it is affected by the Cyclonic Current from the Mediterranean
Sea.
Temperature:
So for the temperature is concerned,
the height of Swat varies from 2500 ft to 7500 ft, therefore, this is
colder zone. Due to the absence of meteorological department, we
cannot quote the actual recorded data; anyhow, January is the coldest
month of the year. The temperature, generally, remains between 40°F
and 45°F (2°C to -2°C). The water-freezing season is from the last
week of December to the end of February. In mountainous areas it takes
more than three months.
The hottest month is July, in which the temperature rises to more than
90 °F (32°C) in the plains, but in mountainous areas, it is lower.
In Buner, however, we find a little bit extremity of weather.
Rain Fall:
There are three rain-bearing seasons:
1. Winter Rains 2. Spring Rain 3. Summer
Rains
Winter Rains:
These rains start in December and last
to the end of February. When the rainfall starts once, it remains
continuous to one or two weeks. This continuous rainfall is called
Jarai. The rain of this season is usually, with slow fall and small
drops. In the plain, the snowfall takes place from 15th January to the
end of February. But in mountainous areas, the snow period is from the
beginning of December to the end of March. (In November, the snow also
falls on mountains, but melts soon.)
Spring Rains:
The rains from March to May are
regarded as the spring rains. In this season, the rainfall occurs in
shower with thunder and lightening, and the drops are bigger. The
lengthened period of the continuation of the spring rains is
destructive for the muddy homes of the poor villagers.
Summer Rains:
Usually, there is a gap of one dry
month, June, between the rains of spring and summer. The summer rains
begin in July, and end in September. These rains are not so
continuous. They are in intermittent position. Sometimes the rainfall
takes place suddenly with hailstones, which results in the damages to
property and lives. The rain of this season falls with shower and
lightning. The annual rainfall is about 50 inch.
The general effects of the weather condition are cold winter and warm
summer, and the coldest winter in mountainous areas.
Natural
Vegetation:
The amount of rainfall and temperature
is enough for the growth of vegetation. The naturally growing plants
can be grouped into two types because there is difference of
conditions between the plain and mountains.
The Vegetation of Plains:
In the lowland of Swat, the
temperature is comparatively high, so the plants and trees are of
broad leaves deciduous type. Poplar, Bakyan and Willow are the common
non-fruit trees. The mulberry, pear, apricot, plum, damson, walnut,
apple, fig, grapes, orange, jujube are fruit trees, and grow
everywhere. Acacia and olive are also found in gregarious positions.
The local names of some of plants and shrubs are Kharawa, Manrogaya,
Kwarae, Manro, Soorazghi, Ghorashki, Khonawli, etc. The plants and
shrubs cover the slopes of the hills and the foothill areas.
The Vegetation of Mountains:
Beyond the height of 4500 ft, there
are vast amounts of forests of coniferous trees that consist of Pines,
Dewdar, Cedar, Byar etc. Generally, each of the variety forms its own
belt. Mostly, the lower belt is of pine. The next to come is Dewdar
and Byar. The belts of these two varieties reach to the denuded mounts
(Spincers). The pine and spruce are found even in Buner, where the
height is not much greater. But Dewdar, and Byar, grow at sufficient
height and are found at Kohistan. Among the shrub, Borajae, Bang-e-Dewana,
Ghanamrangae and Shangla are grown on the slopes of the hills and
mountains. Shepherds, nomads (the local name of them is Ajar) are
migrating to the hills along with their flocks, where the growth of
the grass is greater. These areas are considered as permanent
pastures. Caraway seeds and mushrooms are also found in the same areas
when snow melts away.
Forests:
The vegetation of Swat has a great
value, particularly, the forests and grass. Dewdar and Byar grow in
vast amount in the upper belt of forests. Wood taken from them is
durable and is not rotten easily even in the water, therefore, they
are used in underwater constructions and buildings. Pine is another
useful wood for timber, beams, rafts, and furniture. Generally,
furniture is made of Walnut, Bakayan and Poplar.
Due to these forests, woodcutting is a common profession for the local
people. They also get a meager amount as royalty from the government.
The shrub and grass provides good pastures for the cattle. Gujars and
Ajars drive buffalo, cows, sheep and goats to these pastures, in
summer season. The local people call these pastures Banday.
Formerly, the nomad were paying a great amount of money to the Khans,
who considered themselves as the "Masters" of both the
plains and the hills, but now, the Ajars and Gujars ceased many of
these pastures and they do not give anything as lease. The Khans did
not satisfy only with the money paid to them, so the poor Ajars and
Gujars also had to pay butter oil, ghee, fuels, and wool.
Some people collect mushrooms in these forests, and sell them with
high prices. Moreover, resin is also obtained from the trees of pine.
The final and greater importance of all these vegetation is to protect
soil erosion
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