GEOL-1021EL Lecture Notes - Lecture 5: Crystallization, Water Content, Himalayas
Igneous Rocks
**Know the name of 6 rock-forming igneous minerals
About
ā¢form from āliquid rockā (silicate melt)- is essentially the product of the cooling of the rock
ā¢igneous processes within the earth produce intrusive (plutonic) igneous rocks
ā¢igneous processes on/near the surface reduce extrusive (volcanic) igneous rocks
Magma V Lava
ā¢Magma: mixture of molten rock (āmeltā/āsilicate meltā), plus crystals (minerals), coexisting
with the melt and gasses, if present.
ā¢Lava: magma that has reached the surface
How do igneous rocks differ from each other?
ā¢Texture
ā¢Coarse-grained, ļ¬ne-grained, mixed texture
ā¢clues about texture can be received from early volcanic rocks, studies of granite and other
non-volcanic rocks, laboratory crystallization processes
ā¢overall texture is related to the rate of cooling
ā¢Intrusive (plutonic) is more coarse-grained (slow cooling)
ā¢Extrusive (volcanic) is more ļ¬ne-grained or even glassy (fast)