Chapter 5 Flashcards
igneous rock
begins in the lower crust or upper mantle melts to form magma, which rises up through the crust
extrusive igneous rock
forms from solidified lava or ash
it comes out onto the surface
intrusive igneous rock
magma that never reaches the surface and solidifies underground
shapes of intrusive igneous rock
plutons: massive blobs
batholiths: the largest of the plutons
dikes: thin sheet cutting across layering in the wall rock
sills: form parallel to the layers of wall rock
determining igneous rock types
grain size
color
specific gravity
texture
the size, shape, and arrangement of its grain
crystalline
specimens composed of interlocking grains
glasses
rocks that are shiny and contain no grains
porous
rocks that have sponge-like masses
fragmented
rocks that appear to have pieces cemented together
cooling rate
most important factor controlling grain size - the slower a magma cools, the more ions have to migrate to crystal seeds; the faster it cools the less time there is and the smaller the grains will be
viscosity
resistance of material to flow
the less viscous the more fluid the easier it is for ions to migrate and larger crystals can become
Four Major Compositional groups of Igneous Rocks
- ) Felsic
- ) Intermediate
- ) Mafic
- ) Ultramfic
Felsic
ex: feldspar and silica and quartz
have the most silica and the least iron and magnesium
light colored and have low specific gravities
Intermediate
chemical compositions, colors, specific gravities, and mineral assemblages between those of felsic and mafic rocks