Exam 1 Flashcards
(115 cards)
order of the layers of the earth from the outside in
crust, mantle, core
how do we know what is inside the earth?
direct evidence: deep drilling. indirect evidence: volcanic activity bringing things up, seismic waves
what is the moho discontinuity?
the boundary between the crust and mantle
what is the gutenberg discontinuity?
the boundary between the mantle and the core
what is the lehman discontinuity?
the boundary between the inner and outer core
what do the discontinuities in the earth show us seismically?
the speed of waves changes so we know the layers are made of different materials
what is the outer core made of?
liquid iron and nickel
what is the inner core made of?
solid iron and nickel
how are the layers of earth stratified?
density, thermal, pressure
what is the principle of isostacy?
as heavier things accumulate on the crust, it sinks down. as things erode on the crust it rises.
what is it called when the crust rises in the principle of isostacy?
isostatic rebound. ex: glaciers
what is the earth made of?
46.6% oxygen, 27.7% silicon and silicates
what are minerals?
the building blocks of rocks. ex: mica, feldspar, halite, precious gemstones
what are rocks?
combinations of minerals
how do igneous rocks form?
from molten magma
how do extrusive igneous rocks form?
the magma solidifies above the surface
how do intrusive igneous rocks form?
magma solidifies in the earth’s crust. they get to the surface via uplift and mountain building
examples of extrusive igneous rocks
basalt
examples of intrusive igneous rocks
granite, gabbro
what is mafic rock chemistry?
when the rock magma originates in the mantle
what is felsic rock chemistry?
when the rock magma originates in the crust
characteristics of mafic rocks
low quartz, high magnesium and iron, dark color, high melting temp, low resistance to weathering
characteristics of felsic rocks
high quartz, high potassium and sodium, light color, low melting temp, high resistance to weathering
what are sedimentary rocks?
rocks that form from the cementing and hardening of sediments derived from other rocks