Chap 2 Plate Tectonics Flashcards

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1
Q

PANGEA:

A

Supercontinent that existed prior to tectonic plate movement.

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2
Q

WEGNER’S EVIDENCE FOR CONTINENTAL DRIFT:

A
  1. Observation of fit of continents
  2. Locations of past glaciations
  3. Distribution of equatorial belts (coal, sand and salt deposits in a belt due to similar climates)
  4. Fossil distribution
  5. Matching geographical units
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3
Q

PALEOMAGNETISM:

A

Record of the ancient strength and orientation of Earth’s Magnetic Field

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4
Q

How do ROCKS DEVELOP PALEOMAGNETISM

A

molten rock cools -> minerals crystallise -> during cooling the
minerals are affected by earth’s magnetic field -> strength and orientation of magnetic field preserved.

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5
Q

POLAR WANDER:

A

The successive positions of dated paleopoles trace out a curving line that came to be known as an apparent polar-wander path

the magnetic field dipole of earth is 11⁰ off of earths geographical poles, this difference is called the magnetic declination

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6
Q

POLAR WANDER: Hypothesis 1

A

(apparent polar wander path): earths
continents are fixed but the magnetic poles wander –
rejected as the study of palaeomagnetism didn’t show
and accurate belt of magnetic wander to prove this

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7
Q

POLAR WANDER: Hypothesis 2

A

earths continents move but poles are
fixed – approved by
palaeomagnetism

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8
Q

PALEOPOLE:

A

a magnetic pole of the earth as it was situated at a time in the distant past.

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9
Q

SEA-FLOOR SPREADING

A

=continents drift apart because new
ocean floor forms between them by a process

Discovered by bathymetric maps that shows mid-ocean ridges (no sediment), submarine mountain ranges, trenches, seamount chains and fracture zones.

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10
Q

Harry Hess’ hypothesis of spreading:

A

marine magnetic anomalies show sets of positive and negative
alternating bands on ocean floor that are symmetrical to each other which explains magnetic field reversals and sea-floor spreading from mid-ocean ridges.

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11
Q

Subduction

A

continents move toward each other when the old
ocean floor between them sinks back down into the Earth’s interior

(The downgoing plate (the plate that sinks in the process of subduction)
must be composed of oceanic lithosphere.)

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12
Q

Plate tectonics

A

a theory that Earth’s lithosphere
consists of ~20 distinct pieces (plates) that slowly move relative to one another

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13
Q

PLATE BOUNDARIES:

A

when plate tectonics move, the internal part of the plate remains intact but the boundaries deform

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14
Q

PLATE BOUNDARIES: Types

A
  1. Divergent (constructive)
  2. Convergent (destructive)
  3. Transform
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15
Q

Divergent (constructive) PLATE BOUNDARIES

A

= A plate boundary at which two
plates move apart from each other

mafic rock – forms pillow lavas. (mid ocean ridge)

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16
Q

Convergent (destructive) PLATE BOUNDARIES

A

= A plate boundary at which two plates move toward each other so that one plate sinks
beneath the other

Subduction
occurs (oceanic-continental/oceanic)
or mountain ranges (continentalcontinental) (Andes mountains)

o Forms island arcs (2 oceanic
plates collide) or volcanic arcs (1 ocean plate and 1 continental)

o Wadati-benioff zone: belt of earthquakes on down-going plate

17
Q

Wadati-benioff zone

A

belt of earthquakes on down-going plate

18
Q

Transform: PLATE BOUNDARIES

A

plates slide past each
other (San Andreas Transform fault)

19
Q

TRIPLE JUNCTION:

A

Three plate boundaries
intersect (west coast of South America)

20
Q

HOT SPOT:

A

Places where a plume of hot mantle rock rises from just above the core-mantle boundary and causes anomalous volcanism at an isolated volcano

As a plate moves over the mantle plume, the
volcano moves off the hot spot and dies, and a new volcano forms over the hot spot. As a
result, hot spots spawn seamount chains

Mantle plume can lead to
eruptions when plate with volcanic/island arc
moves over it (Hawaii, Yellowstone)