2 Plate tectonics part one Flashcards

1
Q

Earth’s Plates

A

Rigid segments of the Earth’s lithosphere
Always in motion relative to each other
Made of both oceanic and continental crust

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2
Q

Alfred Wegener : continental drift

A

Meteorologist/Climatologist/ Geologist
Studies the evidences for continental movement
The Origins of the Continents and Oceans, 1915
Proposed that all continents were once part of the supercontinent of Pangaea

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3
Q

Evidence for continental drift

A
  • Continental puzzle pieces
    Using the continental shelf* improves the fit
    *Continental shelf: the part of the continent covered by fluctuations in sea level
  • Distribution of climatic belts
    Glaciers
    Glacial evidence in areas that do not have glaciers today
    Unlikely to have glaciers, even with dramatic climate change
    -Distribution of climatic belts
    Coal swamps
    Deserts
    Reefs
    Salt flats
    -Distribution of fossils
    Non-ocean swimming creatures found on both sides of the Atlantic and Indian Oceans
    -Matching geologic units and mountain belts
    Example: Appalachian Mtns (US), Atlas Mountains (Morocco), Scottish Highlands (Great Britain), and Caledonian Mountains (Norway)
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4
Q

Evidence against continental drift

A

No mechanism
HOW do the continents move?
Plow through the ocean rocks like an icebreaker ship?
Float over the oceans?
Slide over the oceans?
Expanding earth?

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5
Q

Mechanism for continental drift

A

~30 years after Wegener’s death

Seafloor spreading
The History of the Ocean Basins
1962
Harry H. Hess
Ocean floor is constantly recycled (trenches)
Ocean floor is constantly regenerated (ridges)
This “pushes” the continents around

Evidences?
Oceanic topography
Paleomagnetism: stripes on the floor because of changing magnetic poles
Age of the ocean floor
Sediment thickness on the ocean floor

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6
Q

Discovery of seafloor spreading

A

Rear Admiral Harry H Hess
Keeps the sonar on all the time
Even when there are no enemy subs around
Creates thousands of miles of surveys of ocean floor
Gathering evidence of seafloor spreading
sonar= sound navigation and ranging

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7
Q

Mapping the Sea Floor:
Earthquakes

A

Odd, shallow earthquakes in the ocean
Along definite lines: plates

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8
Q

Ocean floor topography/mapping

A

Marie Tharp
Maps the ocean floors for Bell Laboratories
Publishes the first detailed topographic map of the Atlantic Ocean with Bruce Heezen (1959)
Ocean floor is not featureless
Flat plains interrupted by vast, linear mountain ranges
These mountain ranges have central rift valleys

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9
Q

mid ocean ridge draw

A

see screenshot

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10
Q

sea floor sediments

A

As you move away from the mid-ocean ridge, the sediment becomes both older and thicker

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11
Q

sea floor spreading

A

Ocean floors are spreading apart symmetrically along the ocean ridge.
New ocean floor is created by volcanoes on the mid-ocean ridge
Old ocean floor is destroyed by being shoved into the mantle at the ocean trenches

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12
Q

How to test sea floor spreading hypthesis

A

How to test if this is true?
Could check for ages of the seafloor
Expensive, time-consuming
Could check for magnetic polarity of seafloor
Easier, can do with a ship on the surface

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13
Q

Mapping the ocean floor: paleomagnetism

A

Vine and Matthews
Testing the seafloor spreading theory
Discovered:
Alternating strong and weak magnetic fields (poles switching)
Positive (strong)
Negative (weak)
Creates a pattern of stripes on the ocean floor

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14
Q

What powers the earth’s magnetic field?

A

Movement of iron molecules in liquid outer core

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15
Q

Earth’s magnetic field

A

Magnetic field is NOT parallel to the rotational axis
Our magnetic poles WANDER
Over the last 1800 years
North is always near the North Pole, but not always in the same location

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16
Q

magnetic field movement and rocks

A

Igneous rocks (from hot magma) are (weakly) magnetized by the Earth’s magnetic field
Tiny iron minerals line up in the direction of the magnetic field
Once the rock cools, the iron minerals are “frozen” in their aligned position

17
Q

magnetic reversals

A

Earth’s magnetic field periodically switches directions
Unknown reasons
Recorded in the igneous rocks erupted during that time
At least 12 reversals in last 4 million years

18
Q

magnetic reversals and the sea floor

A

Magnetic polarity reversals recorded in ocean floor basalt
Magma cools, forming new crust
Polarity at time of cooling preserved
Old crust is shoved aside as new crust is formed
Magnetic stripes should be mirrored across the ridge showing seafloor spreading and therefore continental drift

19
Q

width of stripes on the ocean floor meaning

A

Width of strips
Proportional to the length of time of the normal or reversed polarity