GEL Week 2- Hotspots and supercontinents (5)

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Last updated 2:24 AM on 1/25/26
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11 Terms

1
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Plate motion

Driving force is gravity, mainly slab pull and ridge push

2
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<p>Slab pull</p>

Slab pull

Subducting plate pulls everything along behind it.

(old oceanic crust is dense, so it sinks)

3
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Ridge push

HIgher elevation of MOR pushes down on new crust

<p>HIgher elevation of MOR pushes down on new crust</p>
4
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How can we see which way plates are moving?

Hot spots- Volcanic plumes independent of tectonic plates

(volcanoes that are not associated with plate boundaries)

5
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Why are hot spots important?

Hot spots reveal how plates move, the direction they move in, and the speed

6
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<p>Hot spot process:</p>

Hot spot process:

1- Volcanoes form on the overriding plate.

2- Plate moves, but hot spot is stationary, so volcano goes extinct

3- New volcano forms above hot spot

4- Process repeats, forms a chain of volcanoes

7
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Why do hotspots erode?

Hot spots eventually erode beneath waves and lack of active volcanoes

8
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What are seamounts?

Eroded extinct volcanoes

9
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What is the role of age in plate motion?

Age change marks direction of plate motion.

10
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T/F: Pangea was the first supercontinent

False

11
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<p>Supercontinent cycle</p>

Supercontinent cycle

1- Supercontinent breaks apart

2- Starts to spread apart

3- Subduction occurs, it slams together

4- Cycle repeats (every 300 to 500 mil yrs)