Crust key terms Flashcards
felsic
- light colour minerals
- high in silica rocks
- felspars
- crystallise at lower temperatures
Mafic
- Dark colour minerals
- rich in magnesium and iron
- cystalize at higher temperatures
- olivine, peridotities
homogenous
orderly minerals
mineral
building block or rock with unique chemical composition
coherent
held together with interlocking crystal, or cemented together
compound
made up of two or more elements
intursive crystals
crystallises at depth inside earth (in magma)
- mafic
- bigger crystals, cools slower
extrusive crystals
lava crystallisation outside the earth
- smaller crystals, cools rapidly
basic
igneous rock, low silica, mafic side
- gabbros and basalt
- generally intrusive, slow cooling
lithosphere
he hard, rigid plates and upper part of the mantle
asthenosphere
the region below the lithosphere 85 to several 100km thick, very viscous, ductile and mechanically weak.
differentiation of the crust
- Starts with partial melting of the mantle
- Magma works its way upwards towards
the surface - Different minerals crystallise at different temperatures and pressures
- Remaining melt contains concentrations of minerals and volatiles that crystallise at lower temperatures and pressures
- deeper the more mafic, higher up (crust) silica based, periditites lower down
Peridotities
made up of olivine and pyroxine
key basic rocks
gabbros, dolerites, basalts
- dark colours,
- minerals within; pyroxene, plagioclase felspar, small amounts of olivine
gabbros
- coarsely crystalline, slowest
- intrusive