Plate Tectonics and the Ocean Floor Ch.2 Flashcards

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
Q

coral reef development

A

fringing reef —-> barrier reef —–> Atolls ——>

26
Q

fringing reefs

A

develop along margin of landmass

27
Q

barrier reef

A

seperated from landmass by lagoon

28
Q

Atolls

A

reef continues to grow after volcanoes are submerged, reef surounds a lagoon

29
Q

the oldest volcanoe

A

Maupiti

30
Q

Paleography

A

the study of ancient continents

31
Q

continental accrection

A

continental material added to edges of continents through plate motion

32
Q

Wilson cycle

A

life cycle of ocean basins; formation, growth, and destruction