Plate Tectonics

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1
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What observations did early cartographers make that supported plate tectonics?

They noticed that some continents, especially Africa and South America, have matching coast lines that fit together like puzzle pieces.

2
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Who was Alfred Wegener?

A German scientist who proposed the idea of moving continents in the early 1900s.

3
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What is Continental Drift?

A hypothesis stating that continents were once joined together and have slowly moved apart over time.

4
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What fossil evidence supported Continental Drift?

Identical fossils of reptiles and plants found on continents that are now separated by oceans.

5
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How did rock and mineral formations support Continental Drift?

Matching rock types and mountain ranges were found on different continents, indicating they were once connected.

6
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What climate evidence supported Continental Drift?

Fossils of ferns and coal deposits found in Antarctica suggest it once had a warm climate.

7
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Why was Wegener’s hypothesis NOT accepted at first?

He could not explain how continents moved, and there was no known force to drive their motion at the time.

8
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Why is Continental Drift accepted today?

New evidence such as seafloor spreading, magnetic patterns, and plate tectonics explains how continents move.

9
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What is seafloor spreading?

The process by which new oceanic crust forms at mid-ocean ridges and moves outward, pushing plates apart.

10
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Is the ocean floor flat?

No. It contains trenches, mid-ocean ridges, and other features.

11
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What does sonar tell us about the ocean floor?

Sonar maps the shape and features of the seafloor, revealing ridges, trenches, and depth variations.

12
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What is an isochron map?

A map that shows the ages of oceanic rocks, with younger rocks near ridges and older rocks farther away.

13
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Why is one side of the seafloor a mirror image of the other?

New crust forms at the ridge and spreads outward evenly on both sides.

14
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Name two ways the seafloor is symmetrical.

1) Rock ages are the same distance from the ridge on both sides
2) Magnetic stripe patterns are mirrored

15
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How does crust thickness change with distance from a ridge?

The crust becomes thicker as it moves farther away from the ridge.

16
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Where is Earth’s magnetic field generated?

In the outer core, from the movement of molten iron and nickel.

17
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What is normal vs. reversed polarity?

Normal polarity matches today’s magnetic field direction; reversed polarity is when Earth’s magnetic field flips.

18
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How does ocean crust record Earth’s magnetic changes?

As magma cools, iron minerals align with Earth’s magnetic field, preserving magnetic patterns in the crust.

19
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Where is new crust created and destroyed?

Created at mid-ocean ridges; destroyed at subduction zones.

20
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What are the three main types of plate boundaries?

Convergent, Divergent, and Transform.

21
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What happens at a convergent plate boundary?

Plates move toward each other due to compression forces.

22
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What happens at an oceanic–oceanic convergent boundary?

One plate subducts, forming deep-sea trenches and volcanic island arcs.

23
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What happens at a continental–continental convergent boundary?

Plates collide and form mountain ranges (no subduction).

24
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What happens at a continental–oceanic convergent boundary?

The oceanic plate subducts, forming volcanoes, trenches, and earthquakes.

25
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What happens at a divergent plate boundary?

Plates move apart due to tension forces, creating mid-ocean ridges or rift valleys.

26
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What happens at a transform boundary?

Plates slide past each other, causing earthquakes but no crust is created or destroyed.

27
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What force is believed to cause plate motion?

Convection currents in the mantle, along with ridge push and slab pull.