Chapter 12 Slides Flashcards
Three major layers
crust, mantle, core
Gravity and Layered Planets
dense iron sinks to the center
mineral phase change
lower mantle rocks undergo this as the minerals are compressed under higher pressures
P waves
compressional seismic
Fastest
S waves
shear seismic
cannot travel through liquid
Seismic Waves
P and S waves
travel fastest in stiff (rigid) rocks
velocities vary based on composition of the rocks
interactions between seismic waves and Earth;s layers
reflect and refract as they pass through the different layers of Earth
Crust
composed of basalt ad gabbro (ocean)
continental crust thicker than ocean
Moho
boundary between the crust and the mantle
P waves increase abruptly increase at the Moho and refract as they cross
Mantle
over 82 percent of Earth is the mantle
layer between the crust and the core
solid rocky layer
Upper Mantle
made of peridotite, iron, magnesium, rich rock
lithospheric mantle is the uppermost art of the mantle and extends down to 200 kilometers
asthenosphere weak layer beneath the lithospheric mantle
lowest portion of the upper mantle is the transition zone
lower mantle
extends from the transition zone to the liquid core
largest layer
56% percent of Earth’s volume
D” layer of the mantle
boundary between the rocky lower mantle and the liquid outer core
Cool regions thought to be the remnants of subducted lithospheric plates
Hot regions through to be start of deep mantle plumes
outer core
liquid
absence of S waves
core
accounts for 1/6 of Earth’s volumes
inner core
solid, dense sphere
growing as earth cools
rotates faster than the crust and mantle