Lecture 5- Marine Geology 2 Flashcards

Pangaea (28 cards)

1
Q

Pangaea

A

the supercontinent that split apart to form the present-day configuration

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2
Q

Wilson Rock Cycle

A
  • process in which continents have repeatedly collided and broken apart
  • happened even before Pangaea
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3
Q

divergent boundaries occur between

A
  • ocean and ocean

- continent and continent

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4
Q

convergent boundaries occur between

A
  • ocean and ocean
  • ocean and continent
  • continent and continent
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5
Q

3 plate boundaries

A
  • transform
  • divergent
  • convergent
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6
Q

earth’s 2 types of crust

A
  • oceanic

- continental

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7
Q

oceanic crust

A
  • thin (5 km)
  • more density so floats deeper in the mantle
  • consists mostly of basalt
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8
Q

continental crust

A
  • thick (70 km)
  • less dense so they float higher in the mantle
  • consists mostly of granite
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9
Q

divergent boundaries

A
  • occur where plates are moving apart

- most of these boundaries are mid-ocean ridges and less commonly, continental rifts

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10
Q

examples of new divergent boundary

A

East Africa rift zone

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11
Q

example of mature divergent boundary

A

mid-ocean ridges

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12
Q

hydrothermal vent systems

A

found at mid-ocean ridge spreading centers

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13
Q

continental boundary: ocean and continental

A
  • ocean is more dense so it subducts and is pushed back down into the mantle
  • generates deep ocean trenches and explosive volcanoes
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14
Q

examples of ocean crust colliding with continents

A
  • North Cascade Mountains
  • Andes Mountains
  • Mt. Saint Helens (volcano)
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15
Q

continental boundary: oceanic and oceanic

A
  • the plate that gets subducted is the one furthest from its spreading center
  • deep oceanic trench (sometimes filled with sediment)
  • older, colder, and more dense subducts
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16
Q

Island Arc

A
  • chain of volcanoes

- ex. Aleutian Islands

17
Q

continental boundary: continent and continent

A
  • neither wants to subduct

- results in mountains (ex. Mt. Everest)

18
Q

transform plate boundary

A
  • plates slide laterally relative to one another

- example: San Andreas Fault

19
Q

type of marine sediment

A
  • terrigenous
  • red clay
  • calcareous ooze
  • siliceous ooze
20
Q

sediment rate of red clay

A

less than or equal to 1 cm per 1000 year

21
Q

sediment rate of ooze

A

1-5 cm per 1000 year

22
Q

terrigenous sediment

A

causes sediment thickness to be high near coast

23
Q

red clay

A
  • found in open ocean

- created by slow rain of continental dust and very low biological addition

24
Q

calcareous/ siliceous ooze

A
  • found in high biological productivity

- absence of terrigenous sediment and dilute red clay

25
accumulation of sediment
- very slow | - a 10 m sediment core can represent a record of a million years of earth history
26
proxy measurement of past ocean conditions
remains of planktonic organisms contained within the sediment cores reveal information about growth conditions of the ocean
27
calcite in shells
calcite in shells grown in colder temperatures have more 18O than calcite grown in warmer temperatures
28
6th mass extinction
caused by humans