GEOL-1021EL Lecture Notes - Lecture 5: Crystallization, Water Content, Himalayas

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Igneous Rocks
**Know the name of 6 rock-forming igneous minerals
About
form from “liquid rock” (silicate melt)- is essentially the product of the cooling of the rock
igneous processes within the earth produce intrusive (plutonic) igneous rocks
igneous processes on/near the surface reduce extrusive (volcanic) igneous rocks
Magma V Lava
Magma: mixture of molten rock (“melt”/“silicate melt”), plus crystals (minerals), coexisting
with the melt and gasses, if present.
Lava: magma that has reached the surface
How do igneous rocks differ from each other?
Texture
Coarse-grained, fine-grained, mixed texture
clues about texture can be received from early volcanic rocks, studies of granite and other
non-volcanic rocks, laboratory crystallization processes
overall texture is related to the rate of cooling
Intrusive (plutonic) is more coarse-grained (slow cooling)
Extrusive (volcanic) is more fine-grained or even glassy (fast)
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