Tectonic plates Flashcards

1
Q

When was continental drift proposed? by who

A

1915
Wegener

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2
Q

What was the name of the supercontinent? When did it begin to drift into the smaller fragments that they are today?

A

Pangea
Mesozoic era

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3
Q

Continental Jigsaw line of evidence

his “fit” of the continents wasn’t a great approximation

A

similarity btw the coastlines on opp. sides of Atlantic ocean

bc including the continental shelf would be better

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4
Q

Fossil line of evidence
1fossil (reptile)

reptiile name
describe it
where was it found
why its evidence

A

Mesosaurus: small, aquatic freshwater reptile
- found in south america and africa (was together in pangea)
- can’t swim vast ocean (salinity) and it’s remains would’ve been scattered

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5
Q

Fossil line of evidence
1 fossil (plant)

name
description
where it was found
why it supports pangea

A

Glossopteris: seed ferns with seeds to heavy to be carried by wind
- Africa, Australia, India, Antarctica, and South America
- only grow in cold climates
in Pangea, these places would be by the south pole

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6
Q

Rock Types and Geological features line of evidence

A

deformed igneous rocks in Brazil match similar tocks of same age in Africa

Appalachians goes northeastward and disappear in newfoundland but similar ones of simmilar age are in the british isles and scandinavia, put together in pangea forms a mt chain

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7
Q

What rocks are older, continental or oceanic?

A

continental

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8
Q

where can glaciers be found today

A

anywhere except along the equator

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9
Q

Lines of evidence: ancient climates
era and where was the glacial period? what was one proposal against this? how was it rejected?

A

paleozoic era in Africa, South America, Australia, and India (glacial deposits found there-near the equator)
- global cooling
- tropical swap deposits in US and Eastern Europe (northern hemisphere) in the form of coal, fossils were produced by ferns in warm climates
- Pangea: southern continents were near south pole=glacier deposits
northern continents were near equator=tropical swamps

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10
Q

Objections to continental drift

mechanism
breaking through crust

A
  • inability to identify a credible mechanism for continental drift, said gravitational forces of moon and sun moved continents
  • said large continents broke through thinner oceanic crust, but no evidence of oceanic crust weak enough to let continents pass without being deformed
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11
Q

Where are most divergent plate boundaries located?

A

Along crests of oceanic ridges

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12
Q

What are spreading centers?

where is it found?
plate boundary?
process

A

Mid ocean ridges at divergent plate boundaries that produce fractures in oceanic crust and rising magma/volcanic eruptions fills voids and cools to create new sea floor

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13
Q

Oceanic ridges

A

Elevated areas of the sea floor with high heat flow and volcanism

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14
Q

Who proposed sea floor spreading? How did his theory contract with Wegener?

A

Harry Hess
Moving continents plowed through moving oceanic floors

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15
Q

Why are ridges high?

A

New oceanic lithosphere use hot and less dense than those farther away from upwelling zone

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16
Q

Where does ocean depth increase

A

Farther from ridge crest

17
Q

Where is thicker vs thinner sediment and why

A
  • Older lithosphere away from ridge crest has more time to cool and contract and is buried by sediment bc its away from upwelling
  • asthenosphere cools and becomes rigid and converts to lithosphere

New lithosphere can’t cool bc it’s so hot- no sediment at ridges

18
Q

Where should the youngest and oldest ocean floor be?

A

Near mid ocean ridge
Far from mid ocean ridge

19
Q

What is rifting

A
  1. Continental plate motions produce tensional forces that stretch and thin the lithosphere
  2. Mantle upwelling and lithosphere upwarping
  3. faults created, magma potentially erupts as volcanoes
  4. Stretching of brittle crust causes large blocks sink creating a continental rift
  5. Sea floor spreading generates a long narrow sea, oceanic crust being created btw c.c and eventually a deep ocean basin with a mid ocean ridge
20
Q

Rift Valley

A

Canyon like structure along the crest of some ridge systems

21
Q

East African rift

explain rifting
how do we know its happening
ex of in the past

A

Tensional forces have thinned lithosphere and sparked upwelling which is demonstrated by large volcanic mountains and Rift Valley is lengthen and deepen just like how the Red Sea did