Ocean Floor Flashcards

1
Q

What were the 3 old assumptions about the ocean?

A
  1. oceans were basically bowl or trough like “basins”
  2. following (1) the greatest thicknesses of sediment would be predicted to accumulate at centre
  3. oceans + continents btwn them are permanent features that have remained unchanged since Earth formed
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2
Q

How was the ocean floor mapped?

A
  • depth originally measured by lowering weighted lines overboard
  • echo sounder (aka sonar) was invented as a primary instrument for measuring depth by reflecting sound waves from ocean floor
  • multi-beam sonar developed later (using an array of sound sources + listening devices for mapping narrow swaths of seafloor)
  • later came use of satellite radar altimeters (used to record seafloor topography by bouncing micro waves off sea surface)
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3
Q

what was the seafloor topography like?

A
  • huge ridges (oceanic or mid-ocean ridges), originall assumed to have been very deep
  • deepest areas were through like areas (deep sea trenches that bordered major landmasses
  • Suken, inactive volcanoes (seamounts) in linear patterns
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4
Q

What are abyssal plains?

A

huge expanses of relatively flat, sediment-covered (nearly featureless) regions of deep ocean floor (btwn ridges + trenches) called abyssal plains

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5
Q

What is a continental shelf?

A

continental margins, a submerged, shallow-water platform extended seaward for significant distances
- at other margins, continental shelf appear very narrow or even non-existent (esp where bordered by a deep sea trench)

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6
Q

what is the seafloor covered with?

A

sediment
- areas most distant from land, deep sea sediment is largely biochemical
- accumulation of ooze

minor:
- mud (from windblown dust)
- chemical sediment produced by precipitation of minerals from seawater

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7
Q

What is ooze

A

accumulation of microscopic skeleton of planktonic organisms

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8
Q

What are the sediment input from land?

A
  • closer to continental landmasses, clastic sediment derived from land sources cover the shallow-water continental shelf (transported by waves + offshore currents)
  • also forms thick accumulations at continental rise (at base of steep continental slope) onto parts of flat abyssal plain
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9
Q

What are turbidity currents?

A

down-slope movements of dense, sediment-laden water (often triggered by earthquakes)

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10
Q

Where are turbidity currents commonly focused?

A

in steep-walled submarine canyons cut into the continental slope

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11
Q

What is the sediment deposited by a turbidity current

A

turbidites: layered + commonly exhibit graded bedding (decreasing in sediment grain size from bottom to top due to settling of progressively finer-grained sediment)

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12
Q

what is a submarine fan?

A

the accumulation of land-derived sediment on the continental rise (thin out on the abyssal plain) and in trenches

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13
Q

What are the types of continental margins

A
  • passive continental margins
  • active continental margins
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14
Q

what is a passive continental margin?

A
  • wide continental shelf
  • geologically quiet (“passively” accumulate sediment)
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15
Q

what is an active continental margin?

A

-continental shelf is narrow or non-existent
- associated w/ deep sea trenches
- geologically active (associated w/ earthquakes + volcanic activity)

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16
Q

What surprise did the study of mid-oceans ridges bring?

A
  • basalt (mafic volcanic rock) exposed at crests of mid-ocean ridges (indicate formed recently)
  • sediment thickness found to increase away from crests of ridges (+thickest in trenches)
17
Q

What are seamounts

A

submerged volcanoes
- appeared to form chains

18
Q

What is the relationship of seamounts with distance?

A
  • ages of seamounts increase w/ increasing distance from Hawaii
  • seamounts become more deeply submerged further away from Hawaii
19
Q

What are atolls

A
  • ring-shaped reefs w/ central lagoon
  • commonly associated w/ submerged seamounts
  • constructed primarily from skeletal remains of corals + other organisms
20
Q

Where are atolls formed

A

forms on flanks of a sinking volcanic island
(hypothesis proposed by Charles Darwin)

21
Q

What is ocean circulation

A

Idea that ocean circulations is driven by water salinity + temperature differences
Basic idea:
- warm, less salty, low-density seawater flows at surface toward poles
- cold, more salty, high-density water flows along seafloor toward equator

22
Q

What is a Thermohaline Cirulation

A

  • cooler, saltier water, is dense enough to sink to seafloor
  • cold, salty deep current flows southward toward equator to connect to surface water current
  • conveyor works as “circuit”
23
Q

What did Alfred Wegener challenge about the configuration of oceans + continents

A

he claimed continents + ocean were distributed very differently in the deep past - continents “drifted” over time

24
Q

What did Wegener name the larger landmass of all the continents?

A

Pangaea (“all land”)