Rocks and weathering 3.1 Flashcards

1
Q

What are the three mechanisms of plate movement?

A
  • Ridge push: intrusion of magma into the spreading ocean ridges such as the Mid-Atlantic ridge propels plates apart.
  • Convection drag: convection currents in the plastic mantle drag the overlying lithosphere.
  • Slab pull: cold and dense lithosphere sinking due to gravity pulls the rest of the plate with it.
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2
Q

Convergent plate boundaries: continental/oceanic

A
  • Form fold mountains and ocean trenches
  • Less dense, oceanic plate subducts beneath the continental plate.
  • Subduction causes layers of rock to be forced upwards causing anticlines and synclines - fold mountains.
  • Material at depth is also forced downwards, deepening crust in the mountain belt.
  • Sediments scraped off the plate and in the trench builds up an accretionary wedge.
  • Subducted plate is partially melted and small pockets of magma rise to form volcanoes - orogenesis.
  • The ocean floor drops steeply to form an ocean trench.
  • Sloping zone of earthquake foci is known as the Benioff zone.
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3
Q

Convergent plate boundaries: oceanic/oceanic

A
  • All similar to continental/oceanic except no fold mountains.
  • Instead, main features are island arcs and ocean trenches.
  • Example is the Philippines and the Philippine trench.
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4
Q

What are island arcs?

A
  • Island chains with the same convexo-concave form.

- Made of active stratovolcanoes and sediment from accretionary wedges.

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5
Q

Convergent plate boundaries: continental/continental

A
  • Compressional stresses lead to the formation of earthquakes but with shallower foci.
  • Example: the alps.
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6
Q

Divergent plate boundaries

A
  • Found at great ocean ridges.
  • Example: Mid Atlantic Ridge.
  • The ridge has a higher relief than the rest of the ocean floor as the ridges consist of hot, expanded rock.
  • Magma rises in between gaps from two plates separating, forming new land as it cools.
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7
Q

What is the evidence of continental drift?

A
  • Coastline fit: Africa and South America
  • Fossils, flora, and fauna: similarities in animal and plant fossils in South America and Africa.
  • Fit of orogenic belts (fold mountain belts): Norway and Britain
  • Fit of rock types: Precambrian rocks on either side of the Atlantic.
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8
Q

What is sea floor spreading?

A
  • The process of creation of new oceanic lithosphere at the ocean ridges as magma cools.
  • Magma extruded along the ridge as dark-colored basalt.
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9
Q

What is the evidence of sea floor spreading?

A
  • Age of rocks on the ocean floor: radiometric dating.
  • Thickness of sediment: increases with increasing distance from the ridge as more time to accumulate.
  • Direct satellite measurements of ocean width.
  • Magnetic stripes
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10
Q

What are hot spots?

A
  • Areas of volcanic activity not related to plate boundaries.
  • Hot magma plumes from the mantle rise and burns through weak parts of the crust, creating volcanoes and islands.
  • The plume remains in the same place but plates continue to move which causes chains of islands.
  • Example: Hawaii
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