Plate Tectonics Flashcards

1
Q

Earth’s Structure

A

Takes up 1% of Earth’s volume
Temp. varies from air temperature (at surface) to 1600℉ (at boundary)
Chemically speaking
- Crust
- Silicates (silicon + oxygen)
Mechanically speaking
- Lithosphere (crust + upper mantle)
- Rigid movement
Mantle
- Silicates at 100-2900km
Asthenosphere
- Ductile movement

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2
Q

Alfred Wegener & Continental Drift Theory

A

Alfred Wegener - first to propose the idea that continents moved
Evidence
- Apparent fit of the continents
- Glacial evidence in tropical areas
- Distribution of fossils
- Matching geologic units

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3
Q

Convection Currents

A

Convection current of the mantle is driving force of plate tectonics

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4
Q

Plate Boundaries

A

Tectonic plates meet at plate boundaries

3 types of plate boundaries: convergent, divergent, and transform

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5
Q

What is an earthquake?

A

A vibration caused by the sudden breaking or frictional sliding of rock in the Earth

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6
Q

Magnitude

A

Measurement of energy released at the source, uses seismographs

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7
Q

Intensity

A

The effect on Earth’s surface, location or site-dependent

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8
Q

Plate Tectonics & Volcanism

A

Convergent Boundaries
- Subduction - one plate sinks beneath another. As the sinking plate gets closer to the hotter mantle, it melts. Produces magma.
- Continental - Oceanic: Continental Volcanic Arc
- Oceanic - Oceanic: Volcanic Island Arc

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9
Q

Plate Tectonics & Volcanism

A

Divergent Boundaries
Continental - Continental: Volcanically active rift valleys as lithosphere gets thinner
Oceanic - Oceanic: Mid-ocean ridge volcanism as seafloor spreading pushes plates apart

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10
Q

Convergent Boundaries

A

Boundary at which two plates are moving towards each other
Subduction - a convergent boundary at which one plate sinks under the other
Oceanic crust is being destroyed

Geologic Features:
Mountains
Earthquakes
Trench - forms as the plate bends and begins to subduct
Volcanic Arc - magma is formed as the subducting plate melts
Continental Volcanic Arc (Continental & Oceanic) vs. Volcanic Island Arc (Oceanic)

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11
Q

Divergent Boundaries

A

A boundary at which two plates move apart from each other

Oceanic lithosphere (crust) is created at these ridges through seafloor spreading process

Geologic Features:
- Earthquakes
- Mid-ocean ridges
- Rift Valley

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12
Q

Transform Boundaries

A

Boundary at which two plates slide sideways past each other

No new plate is created, no new plate is destroyed

Often link together ridge segments
Shallow earthquakes common

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