The Seafloor Flashcards

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1
Q

Percentage of earth’s surface area covered by water

A

71% and ~95% of inhabitable volume

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2
Q

Four major ocean basins

A

Pacific, Atlantic, Indian and Arctic

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3
Q

Earth core

A

~ 3400 km thick
Solid inner core and liquid outer core
Iron rich

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4
Q

Oceanic crust

A

Mostly Basalt
Denser than continental crust
Relatively young less than 200 million years old (because it’s denser it’s on the conveyor belt to be formed and destroyed )

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5
Q

Continental crust

A

Mostly granite
Less dense than oceanic crust
Up to 3.8 billion years old

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6
Q

How many tectonic plates are there

A

12 major tectonic plates

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7
Q

Divergent boundaries

A

Occurs when two tectonic plates move away from each other
As plates move apart new crust is formed usually around mid ocean ridges

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8
Q

Convergent boundaries

A

Two plates move towards each other,

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9
Q

Continent-Continent Collison

A

Two continental plates move towards each other, both plates are less dense so the plates collide and push upwards forming large mountain ranges (European Alps and Himalayas)

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10
Q

Continent-Oceanic crust collison

A

Oceanic crust subducts (more denser) under the continental crust
Results in the forming of volcanism, deep trenches and subduction zone creates mountains ranges (South America Andes)

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11
Q

Ocean-Ocean plate collision

A

Two oceanic plates collide, one runs over the other which causes it to sink onto the mantle forming a subduction zone
The subduction plate is bent downward to form a very deep depression in the ocean called trench

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12
Q

Transform Boundaries

A

Two plates slide past each other, may occur either on land or underwater
Such moments is rarely smooth and may cause tsunamis or earthquakes (San Andreas fault)

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13
Q

Mid-Ocean Ridges

A

A continuous chain of submarine volcanic mountains that encircle the globe like seams on a baseball

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14
Q

Rifts

A

Formed between plates at divergent boundaries (spreading centers)
Allows magma to side through rift, pushes up surrounding oceanic crust and cools to form new crust

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15
Q

Crust age: near ridges

A

Young rock and little sediment accumulation

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16
Q

Crust age: further from ridges

A

Older rocks and thick sediment layers from time accumulated

17
Q

Where does crust recycling happen

A

Occurs at subduction zones

18
Q

Lithogenous sediments

A

Derived from the break-down of continental rocks (weathering)
Large particles sink faster and give indication of distance from source
Fine particles may be transported long distances (Saharan dust to pacific ocean abyss)

19
Q

Biogenous sediments

A

Derived from skeletons and shells of marine organisms
Two main forms: calcium carbonate and silica

20
Q

Continental margins

A

Areas where continental and oceanic crust meet

21
Q

Active margins

A
  • More relative to each other (convergent, divergent and transform faults)
  • Characterized by steep, rocky shorelines, narrow continental shelves and steep continental slopes (~6’), trench with no rise
22
Q

Passive margins

A

Relatively inactive geologically
Characterized by flat, wide coastal plains, wide continental shelves and gradually sloping continental slopes (~2’)

23
Q

Continental shelf

A
  • shallowest part of the continental margin
  • Covers ~8% of seafloor
  • 0-200 m depth
  • biological the richest area of the ocean
    -composed of continental crust
24
Q

Continental slope

A

-Closest thing to an exact edge of the continent
- covers ~11% of the seafloor
- 200-3000 m depth
- average gradient ~4’

25
Q

Continental Rise

A

Rise formed by sediments from submarine fans (river running off shore and erode sea floor), slumped downslope or gradually accumulated
Deep sediment layers
River-borne material is highly nutritious

26
Q

Bathyal zone

A

~200-3000 m
- Contains continental slops (~51.6% of global bathyal habitat), offshore seamounts, islands, MORs (~49.4% of global bathyal habitats)
- Bathyal basins occur close to cost in fjords and are created by glacial erosion

27
Q

Abyssal plains

A

~3000-6000 m and essentially flat
Covers ~50% of earths surface, less then 1% observed in detail
Punctuated by thousands of abyssal hills, knolls and seamounts
Interrupted by MORs