Ch. 13 Flashcards
crust
outermost shell that consists of a broad mixture of rock types. thickness of 7km (4 miles) below ocean, five times thicker under continents. increase in density with depth below surface, but oceanic crust is generally denser.
Moho layer
base layer of the crust that is with a significant change in mineral composition
mantle
2900 km. largest of four layers. has three layers within. makes up 84 percent of the total volume of earth.
lithosphere
uppermost mantle layer. hard and rigid, includes the crust
asthenosphere
rocks are so hot they lose much of their strength and become tar like. geothermic energy builds here. volcano activity
mesosphere
below the asthenosphere. “lower mantle” where the rocks are very hot and rigid
outer core
beneath mantle. depth of 5000 km. molten material here.
inner core
innermost area of earth. solid, dense, 1450 km radius, made up of iron nickel or iron silicate (same with outer) the core is the source of energy that pushes the molten material up to the surface where it melts and becomes lava.
minerals
the building blocks of all rocks. solid, natural, inorganic, special chemical composition, atoms arranged in regular pattern to form solid crystal.
silicate
the largest and most important rock forming mineral. oxygen and silicon. hard and durable.
rocks
consolidated combinations of minerals.
igneous rock
cooling and solidification of molten rock. determined by the chemistry of the magma. texture determined by where and how the molten materials cooled. coarse: slow cooled. Fine: rapid cooling.
lava
molten rock when it flows out on or is squeezed up onto the surface
magma
molten rock beneath the earths surface.
pyroclastic
tiny pieces of volcanic rock that have been explosively ejected out onto the surface by an eruption