Plate Tectonics Flashcards

1
Q

Wegener’s Theory

A
  • Atlantic Ocean didn’t exist 200Ma ago
  • Formed when ancient super-continent called Pangaea (Greek for ‘all of earth’) broke apart
  • Continents and ocean floors are fundamentally different (density)
  • Present day continents have essentially the same outlines since the break up of Pangaea
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2
Q

Wegener Evidence

A
  1. fossils of the same plant and reptiles found in rocks of S. America, Africa, India and Australia (subsequently found Antarctica)
  2. The distribution of tillites (lithified glacial deposits) consistent with a single large ice sheet covering the reassembled continents.
    S. America, Africa, India, Australia, Antarctica.
    Position- Similar glacial till deposits, palaeomagnetism.
    Age- formed Ca. 300million years ag, began to break apart ~100million years ago
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3
Q

Wegener’s Mechanism

A

Harold Jefferey’s book ‘The Earth’ (1920s)-
Wegener’s mechanism of tidal forces could not be accounted for the separation of the continents producing movements in many different directions for millions of years on the surface of a rotating planet.

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4
Q

Arthur Holmes

A

Almost sole supporter of Wegener: Arthur Holmes, University of Edinburgh

Arthur Homes 1930s: internal mechanism
-Convection currents in the upper mantle (now known as the asthenosphere) driven by heat produced by radioactive decay in the core of the Earth
Very few people believed Holmes.

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5
Q

What about the Ocean Floor?

A

Arguments for and against continental drift had been based on the exposed 1/3 of the Earth’s surface, i.e. the continents
Many important discoveries of the ocean floors made during the world war 2 to the early 1960s
Ocean floors rugged and irregular (not as flat as had been thought) underwater mountain ranged and deep trenches identified.

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6
Q

Mid-Atlantic Ridge

A
  • Stands over 3km above the abyssal planes
  • > 2400km wide
  • down-dropped rift valley ~2.5km deep & 32-48km wide extends along the length of its crest

Trenches are very seismically active: 80% of the Earth’s shallow focus earthquakes occur near the trenches and over 90% of the Earth’s deep focus earthquakes.

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7
Q

Sea Floor Spreading as evidence of plate tectonics

A

Proposed as a model by Harry Hess in 1960.

Upward moving convection currents in the upper mantle produce the ocean ridges of the earth (cf. Arthur Holmes, 1930)

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8
Q

Convection Currents

A

Convection currents carry molten rock (basalt) to the surface, then ‘spread it’ outwards on either side- pushing the continents apart and forming young ocean basins.

But what happens to all of the new oceanic crust that is being created?? is the earth expanding?!?! :0

Hess suggested trench systems mark sites of descending limbs of convection cells- material swept back into the upper mantle where it is re-melted.

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9
Q

Magnetism as evidence

A

1963- Magnetic stripes
First observed using magnetometers in the NE Pacific
Form a symmetrical pattern on each side of a mid-ocean ridge.
Alternate stripes of oceanic crust with normal and reversed polarity.
-Fe-bearing minerals act like tiny compass needles and crystallise in ocean floor basalt in the direction of the Earth’s magnetic field at the time of eruption
-Alternating stripes of normal and reversed polarity are evidence for periodic geomagnetic reversals
-Have now been found adjacent to all the mid-ocean ridges

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10
Q

Plate Boundaries

A
Geologically active regions 
Three types of plate boundaries 
1-converging 
2-diverging or rift 
3-transform
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11
Q

Converging

A

Oceanic to oceanic plate boundaries (e.g. Japan)

Oceanic to continental plate boundaries (e.g. Juan de Fuca)

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12
Q

Cascadia Subduction Zone (Oregon Coast)

A
  • Converging at ~3.8cm/year
  • Movement not smooth or continuous
  • Plate lock in place, and unreleased energy build up overtime
  • Accumulated energy is violently released as megathrust earthquake
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13
Q

Cascadia landforms

A

Estimated 7-12% chance of megathrust earthquake in the next 50 years assuming recurrence of 530 +/- 260years, and that the last one occurred about 312 years ago.

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14
Q

Continent to continent (converging)

A
Himalayan orogeny (for example)
(orogeny= mountain-building)
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15
Q

Drifting or rift

A

Continent- continent rifting

Rift- Iceland

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16
Q

Transform/Strike-slip

A

Transform margin

Strike-slip - San Andreas Fault, California