Chapter 17 and 18

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Created by:

TaylorEarthScience  on April 30, 2012

Subjects:

Earth Science

Description:

Continental Drift, Plate Tectonics, and Volcanoes.

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Chapter 17 and 18

Wegner
Scientist who came up with the theory of Continental Drift.
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Wegner Scientist who came up with the theory of Continental Drift.
Continental Drift The theory that states that all Earth's continents were once a single landmass called Pangaea.
Pangea The one single landmass scientists believe existed before the continents broke apart.
Harry Hess The scientist that came up with the theory of seafloor spreading.
Seafloor Spreading The theory that new ocean crust is formed at ocean ridges and destroyed at deep-sea trenches.
Thoery of Plate Tectonics The theory that says Earth's crust and rigid upper mantle are broken into enormous slabs called plates.
Plate Boundaries Areas where tectonic plates interact.
Convergent Boundaries Places where tectonic plates are moving towards one another.
Divergent Boundaries Places where tectonic plates are moving apart from one another.
Transformation Boundaries Places where 2 plates slide past each other horizontally.
Subduction When plates meet and 1 of the 2 plates is is forced benath the other.
Rift Valleys Divergent boundaries that occur on land
Viscosity The internal resistance to flow (how "sticky" a substance is).
Andesitic Magma Forms from crust being sub-ducted, pushed down, into the Earth's mantle. This magma type has an intermediate viscosity.
Basaltic Magma Forms from rock in the upper mantle melting. This magma type has a low viscosity.
Rhyolitic Magma Forms from molten material rising and mixing with the crust above it. This magma type has a high viscosity
Calderas Large Craters
Shield Volcanoes These produce mountains with a broad, gently sloping side and a nearly circular base.
Cinder-Cone Volcanoes These volcanoes have steep sides and are generally small.
Composite Volcanoes These are much larger then Cinder-Cone Volcanoes.
Tephra Rock fragments thrown into the air during an eruption.
Pyroclastic Flow Rapidly moving tephra and volcanic ash that moves down the volcano.
Hot Spots Volcanoes found far away from plate boundaries.

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