Plate Tectonics and the Ocean Floor Ch.2 Flashcards

(32 cards)

1
Q

Crust composition

A

low-density, mainly silicate minerals

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2
Q

mantle composition

A

mainly iron, and magnesium silicate minerals

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3
Q

core

A

high-density, mainly iron and nickel

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4
Q

Lithosphere

A

cool rigid shell, includes crust and upper mantle, about 100 km thick, forms tectonic plates

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5
Q

Asthenosphere

A
  • relatively hot
  • flows with high viscosity
  • base of lithosphere to about 700km deep
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6
Q

Continenatl crust

A

granite (light coloured ingenous rock), density of 2.7 g/cubic cm, avg thickness of 35 km

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7
Q

oceanic crust

A

basalt (dark igneous rock), density of 3, avg thickness of 8km

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8
Q

Earthquake activity mirrors blank

A

tectonic plate boundaries

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9
Q

most large earthquakes occur where?

A

at subduction zones

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10
Q

Pangaea

A

one large continent existed 200 million years ago

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11
Q

Panthalassa

A

one large ocean (200 million years ago)

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12
Q

destructive margins (driving mechanism for plate motions)

A

at subduction zones at deep-sea trench

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13
Q

constructive margins

A

at mid-ocean ridges at spreading ocean ridge

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14
Q

litoshpere

A

rigid tectonic plates that float on ductile asthenosphere

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15
Q

paleomagnetism

A

study of earth’s ancient magnetic field

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16
Q

evidence for plate tectonics

A
  • earth’s magnetic field
  • polar wondering
  • magnetic polarity reversals
17
Q

sea floor spreading evidence

A
  • magnetic anomalies; regular pattern of north-south magnetism
  • stripes were symmetrical about long underwater mountain range
18
Q

ocean crust formation

A
  • ocean crust forms at mid-ocean ridge
  • ocean crust moves away from mid-ocean ridge and cools and subsides
  • and thickens (crustal underplating)
19
Q

divergent plate boundary

A
  • plates move away from each other
  • mid-ocean ridge; Rift Valley
  • new ocean floor created
20
Q

convergent plate boundary

A
  • plates move toward each other

- oceanic crust destroyed; ocean trench, volcanic arc

21
Q

transform plate boundary

A

-plates slide past each other
2 types
-oceanic transforma fault ; ocean floor only
-continrntal transform fault; cuts across continent

22
Q

volcanic hotspots

A

-a region of high volcanic activity not located at a tectonic plate boundary
-it is caused by upwelling of deep mantle plumes
-hotspots are intraplaye surface manifestiations of mantle plumes
-

23
Q

seamounts

A

rounded tops located between” islands”

24
Q

tablemounts or Guyot

A

flattended tops below the sea surface

25
coral reef development
fringing reef ----> barrier reef -----> Atolls ------>
26
fringing reefs
develop along margin of landmass
27
barrier reef
seperated from landmass by lagoon
28
Atolls
reef continues to grow after volcanoes are submerged, reef surounds a lagoon
29
the oldest volcanoe
Maupiti
30
Paleography
the study of ancient continents
31
continental accrection
continental material added to edges of continents through plate motion
32
Wilson cycle
life cycle of ocean basins; formation, growth, and destruction