The_theory_of_plate_tectonics_without_qs

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13 Terms

1

What is Plate Tectonics?

A theory developed in the 1960s and 70s to describe the internal forces that deform the Earth's crust.

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2

What was Pangea?

A super-continent that existed around 200 million years ago, where all continents were once joined.

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3

What landmasses were formed from Pangea?

Laurasia in the northern hemisphere and Gondwanaland in the southern hemisphere.

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4

Who was Alfred Wegener?

A scientist who proposed the theory of continental drift in 1912 based on fossil distribution, mountain trends, and coastline shapes.

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5

What is sea-floor spreading?

A process proposed by Harry Hess in the 1960s where new crust is created as magma erupts from the sea floor, forming submarine mountain ridges.

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6

What does the Mid-Atlantic Ridge represent?

An underwater mountain range where new rocks are formed as tectonic plates move apart.

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7

Who were Vine and Matthews?

Researchers who integrated Wegener's and Hess's ideas to build the foundation of modern plate tectonic theory.

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8

What are convection currents?

Movements of molten magma in the mantle that act as the mechanism for the movement of tectonic plates.

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9

What is the significance of Pangea?

Pangea is significant as it provides evidence for continental drift and the historical geological development of Earth.

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10

How did Alfred Wegener support his theory of continental drift?

Wegener supported his theory through the distribution of fossils, similarities in rock formations, and the fit of coastlines.

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11

What role does the Mid-Atlantic Ridge play in plate tectonics?

The Mid-Atlantic Ridge plays a crucial role in plate tectonics as it is a divergent boundary where new oceanic crust is formed.

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12

How do convection currents influence tectonic plate movement?

Convection currents in the mantle create heat and movement, which causes tectonic plates to move and leads to geological activity.

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13

What was the contribution of Harry Hess to plate tectonic theory?

Harry Hess contributed the idea of sea-floor spreading, explaining how new crust is generated at the ocean floor.

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