Lecture 5- Marine Geology 2 Flashcards

Pangaea

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
Q

accumulation of sediment

A
  • very slow

- a 10 m sediment core can represent a record of a million years of earth history

26
Q

proxy measurement of past ocean conditions

A

remains of planktonic organisms contained within the sediment cores reveal information about growth conditions of the ocean

27
Q

calcite in shells

A

calcite in shells grown in colder temperatures have more 18O than calcite grown in warmer temperatures

28
Q

6th mass extinction

A

caused by humans