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the scientific study of Earth
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the gases that envelop the earth
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the water on or near Earth's surface
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all of the living or once-living material on Earth
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Term
geosphere
(solid earth system) |
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Definition
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the rock and other inorganic Earth material that make up the bulk of the planet
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- solid rock
- parts of it flow slowly, upward or downward
- comprised of ultramafic rocks (rich in Fe and Mg, poor in silica
- extends to 2900 km
- largest part of earth
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thickness is insignificant compared to the whole earth, only have direct access to the crust.
oceanic crust and continental crust, oceanic crust is very thin.
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crust and the uppermost part of the mantle.
makes up the plates of Plate Tectonic Theory
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upper part of the mantle below lithosphere.
ductile solid, will flow under stress rather than rupture, like the lithosphere.
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cause defromation of rock as well as vertical and horizontal movement of crust.
mountain ranges are built by this
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thick
less dense
silica rich
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thin
more dense
more mafic
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plates move apart and new oceanic crust is formed.
coincide with crests of mountain ranges, called mid-oceanic ridges.
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rock that forms when magma (molten rock) solidifies.
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Term
| convergent plate boundary |
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Definition
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plates move toward each other and oceanic crust is recycled into the mantle.
ensures that earth doesn't grow in size.
oceanic-continent, ocean-ocean, continent-continent.
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Term
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Definition
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(ocean-continent convergence)
the less dense continental plate overrides denser oceanic plate and sinks at this point.
neither plate subducts in c-c convergence.
more dense plate subducts in o-o convergence.
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plates move past each other horizontally.
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Term
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Definition
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uplift due to removal of overburden through erosion.
vertical movement of sections of Earth's crust to achieve balance.
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the sun.
drives most surficial processes.
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removal of rocky material from its original location.
results in the wearing down of the land's surface.
moving water, ice, or wind loosens and removes material.
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loose material, the product of the breakdown of rock.
eroded sediments are transported to low energy environments where they accumulate, eventually cement into sedimentary rock.
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