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Crust
Thin brittle outer layer of earth composed of silicate rich rocks
Mantle
Located beneath the crust is the thickest internal layer composed of heavy iron and magnesium silicate rocks
Outer Core
A thick layer of molten iron and nickel
Inner Core
A solid sphere of iron and nickel in the other core
Alfred Wegener
A German meteorologist that proposed the theory of continental drift in 1912
Continental Drift
The continents were able to move about earth’s surface
Pangaea
The name given by Wegner for the most recent assemblage of all the land masses to form one supercontinent
Plate Tectonics
The concept of tectonic plates shifting due to convective forces in the mantle
Lithospheric “Plate”
segments of the mantle that contains the crust and the mantle
Lithosphere
Layer consisting of the crust and uppermost mantle
Continental Crust
Lower density thicker and granitic in composition
Oceanic Crust
high density thin and basaltic in composition
Moho
Boundary between the crust and the uppermost mantle. Identified by the rapid increase of wave speed between the two layers
Astenosphere
Slow flowing viscus semi solid layer. Large convection currents occur here.
Mesosphere
Lowest part of the mantle that behaves like a solid and is composed of iron and magnesium rich silicate rocks
Earthquake
Any sudden release of energy that causes a shaking in the ground
Common causes of earthquakes
Volcanic eruption, meteorites, landslides
Focus
point beneath the earth’s surface where the motion occured that generated the earthquake
Epicenter
Point vertically above the focus at earth’s surface.
Body Waves
Seismic Waves that travel through the earth’s interior
Surface Waves
waves that travel along earth’s surface