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(ch. 5, cont.)
Volcanic Landforms

1.
Calderas
               -large collapse depression where the volcano vent was
     a. Crater Lake type (Oregon)     (fig 5.22 p 159)
                         -after the eruption, the mountain fractures and caves in
                         -a little greater than 1 km
     b. Hawaiian type
                         -mafic
                         -hot spot forms massive volcano (shield volcano) and it sinks b/c its so heavy
                         -and as magma chamber empties, it caves in
     c. Yellowstone type     (fig 5.24 p 160)
                         -area is highly felsic, silicic;         felsic & intermediate
                         -collapse of a volcano, followed by an eruption
2.
Fissure
               -fracture in Earth's crust through which magma migrates
               -mafic (basaltic) magmas
3.
Lava Dome    (fig 5.26 p 162)
               (Mt. St. Helen's)
               -pressure makes magma eject, then after pressure is released, the remaining magma sits
                    in it like a bowl; the top crystallizes and forms a lava dome
               -eventually, it can plug up a volcano; but if more magma is pushed up or gas is introduced,
                    it can explode again
4.
Volcanic Pipes/Necks     (fig 5.27 p 163)
               -conduit that magma flows through to get to the surface
               -when it crystallizes in there completely and the volcano erodes, the neck may still be there
                    b/c it's tougher

Intrusive Igneous Activity
Plutons
          -subterranean (underground) igneous structures
            (Pluto = god of the underworld)
Classification of Plutons
          Shape:  1) tabular;     2) massive
          Orientation
                    1) Discordant (cuts across rock layers)
                    2) Concordant (parallel to rock layers)
Types of Plutons     (fig 5.28)
          1. Dikes- tabular discordant plutons
          2. Sills- tabular concordant plutons
          3. Laccoliths- like sills, but the magma is more viscous
                              -intermediate;   won't move as easily
                              -forms more of a bubble (blob) than a tabular shape
          4. Batholiths- massive pluton
                              -surface exposed is greater than 40 square miles
          5. Stock- small batholith
                              -surface exposed is less than 40 square miles

Xenolith
               -fragments of host/country rock; found in igneous masses that are unmelted
Columnar Jointing
               -5-7 sided column; due to slow crystallization of the magma. (fig 5.31)

Plate Tectonics & Igneous Activity

    Convergent Plate Boundaries
                         * Volcanic Island Arc     ocean --> <-- ocean
                         * Continental Volcanic Arc     ocean --> <-- continent
    Divergent
                    -not nearly as violent <--  -->
    Hot Spot
                    -mantle rock is upwelling; forms magma in lithosphere that comes up
                    -plates move; hot spots don't      /!\
                                                                          !







Lab Box 1: Igneous Rocks
(Study Chart on p 120)

1. Diorite "white granite"
2. Pink Granite
3. Gabbro
4. Periodite
5. Rhyolite
6. Basalt
7. Porphyritic Basalt
8. Obsidian
9. Pumice
10. Scoria
11. Syenite (white granite w/out quartz)
12. Llanite (porphyritic rhyolite)
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