Lecture 16 Flashcards

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1
Q

Relief

A

Shape of land, more specifically, the elevation difference between highest and lowest point in area.

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2
Q

Orders of relief

A

Different scales.
1st order - broadest scale. Continents and ocean basin. Largest landforms.
2nd order - major features of first orders (mountain ranges, plains).
3rd order - individual landforms (a valley, a beach).

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3
Q

2nd order in ocean basins

A
Mid ocean ridge (underwater ocean range).
Abyssal plains (most of ocean floor).
Continental margin; continental rise (gentle rise up from deep sea floor), continental slope (steeper rise), continental shelf (gentle rise, continent merges with ocean basin).
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4
Q

2nd order of relief on continents

A

Mountain chains (actively growing). Mountain roots (not active wearing down). Shields (tectonically quiet, relatively flat). Exposed shields (bedrock at surface). Covered shields (covered by sediment).

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5
Q

Continental drift

A

When accurate maps were map, a jigsaw fit of continents became apparent. Matching fossils were found and rock types and mountain ranges match up.

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6
Q

Alfred Wegener

A

Took fit of continents seriously and sought an explanation. Suggested that continents once were together; Pangea.

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7
Q

Paleomagnetism

A

Shift in magnetic poles occurs; now north, other times south.

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8
Q

Sea floor spreading

A

New material created in mid-ocean ridges, then moves away to both directions. Showed that crust does move around and that Wegener was correct.

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9
Q

Convection cells in asthenosphere/mantle

A

The leading theory of movement. AKA the plastic/moving layer.

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10
Q

Divergent plates

A

Plates move away from each other and a new crust is created.
Mid ocean ridges, ocean basins grow, Rift Valley; beginning of ocean.

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11
Q

Ocean-continent convergence

A

Oceanic plates and continental plates hit.

Continental crust is less dense, so stays on surface, oceanic crust sub-ducted.

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12
Q

Continent-continent convergent

A

Continental crust crumbles to form mountains.

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13
Q

Ocean-ocean convergent

A

Two oceanic plates meet. Subduction causes melting, some magma rises, causing volcanoes of continental margin.

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14
Q

Transform faults

A

Two plates slide past each other.
Can cause earthquakes.
Common on mid ocean ridges, some on continents.

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15
Q

Terranes

A

Mini plates that join up with major plates.

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16
Q

Pangea

A

Wegener suggested the continents were tougher in a supercontinent called Pangea.

17
Q

Laurasia

A

When Pangea broke up, the North was called Laurasia.

18
Q

Gondwanaland

A

When Pangea broke up, the South was called Gondwanaland.