BIOTITE | | dark colored mica |
SUBDUCTION | | foliated, looks like banded granite |
BASALT | | when one plate is converges and dives under the other |
COMPOSITE | | type of igneous rock that cools fast above ground , notallowing larger crystals to form |
GABBRO | | clear mineral; fizzes when HCl applied; you see double |
SHALE | | tall gently sloped volcanoe; lava very fluid; non-explosive |
CONVECTION | | mechanism responsible for plate movement and earth magnetic field |
CONGLOMERATE | | fastest type of earthquake wave; travels through all materials |
EXTRUSIVE | | lead sulfide mineral; blocky cleavage; metallic luster |
LONGITUDINAL | | sedimentary, clastic, has pebbles |
CALCITE | | olive green mineral containing a lot of iron and magnesium |
SLATE | | only half as fast as P waves; can't go through liquids or gases |
TRANSFORM | | igneous rock; extrusive; cooled so quickly that there are no grains |
SILICATE | | dark gray , igneous rock, fine grained; makes up most of oceanic crust |
FELDSPAR | | location of the surface directly above the earthquake source |
GALENA | | igneous rock; salt and peppery; light colored; intrusive |
CINDER CONE | | steep, tall, explosive type of volcano made of different layers of ash, lava, cinders, mud |
RIDGE | | deep depression in subduction zone |
GRANITE | | when shale undergoes metamorphism it converts to this |
RHYOLITE | | most common general category of mineral in crust; made of silicon and oxygen atoms with tetrahedral units |
SHIELD | | clastic sedimentary; clay |
EPICENTER | | formed at the spreading center |
GNEISS | | "field mineral"; most common specific mineral in continental crust |
SHEAR | | igneous rock; extrusive; fine grained; light-colored |
TRENCH | | igneous rock; greenish black; dark colored; intrusive |
OLIVINE | | lavea explodes into the air, rains down small cooled fragements that pile up |
OBSIDIAN | | parallel sliding plate boundary |