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Ocean Floor Features. http://ga.water.usgs.gov/edu/waterdistribution.html. Source: Nace, U.S. Geological Survey, 1967 . East Coast of the U.S. How are the ocean floor features found?. SONAR. So und Na vigation R ange

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slide3

http://ga.water.usgs.gov/edu/waterdistribution.html

Source: Nace, U.S. Geological Survey, 1967

slide5

How are

the ocean floor features found?

sonar
SONAR
  • Sound
  • Navigation
  • Range

The echo sounder calculates water depth by measuring time between emission of a sound signal directed toward the ocean floor and the return echo.

slide10

Topography of the Ocean Floor

  • Continental Shelf
  • Continental Slope
  • Submarine Canyon
  • Abyssal Plain
  • Seamount
  • Mid-Ocean Ridge
  • Rift Zone
  • Ocean Trench
slide11

Continental Shelf & Slope

  • Continental shelf – a relatively flat part of the continent covered by seawater. Lies between the coast and the continental slope.
  • Continental slope – steeply dipping surface between the continental shelf and the deep ocean basin.
slide12

Continental Shelf & Slope

San Francisco

Monterey Bay

The shelf break marks a distinct change in the slope of the sea floor from the flat continental shelf to the steep sea floor of the continental slope.

continental shelf
CONTINENTAL SHELF
  • About 8% of the global seafloor area
  • Source of fish, both commercial and sport, and in some areas, oil and natural gas.
  • Varies in size off the coasts of the U.S.
    • West coast – narrow
    • East coast - wide
continental slope
CONTINENTAL SLOPE
  • Gradually rises from the abyssal plain but climbs as much as 45 degrees as it approaches land.
  • Continental Rise - sediment deposits at the base of the slope
  • Slopes are often gouged by deep valleys or submarine canyons
submarine canyon
Submarine Canyon

HUDSON CANYON

CONTINENTAL SHELF

CONTINENTAL SLOPE

HUDSON CANYON - First discovered in 1864

slide16

Submarine Canyons

San Francisco

Canyon leading into Monterey Bay

  • Submarine canyons are v-shaped canyons cut into the continental slope. Many canyons are associated with major rivers such as the Congo, Hudson, and others.
    • most canyons were originally formed during the last Ice Age when the water level was lower
    • some are the result of earthquakes.
abyssal plain
The true ocean floor

Result of sediment drifting downward to fill depressions of the rocky ocean floor

remains of marine life

fine, clay-sized particles (ooze)

ABYSSAL PLAIN
slide18

Abyssal Plain

Continental shelf

Continental slope

Abyssal Plain

The abyssal plain is the flat, almost level area of the deep ocean basin.

OOZE!!!

slide19

Seamount

seamounts

Coast of central California

Monterey

Same area, different perspective

A volcanic mountain found on an ocean basin. It is not a result of subduction or formed at the mid-ocean ridge. Possibly an island that has since eroded.

seamount guyot
SEAMOUNT & GUYOT
  • Isolated mountains rising from 3,000 to 10,000 feet above the surrounding seabed.
  • Volcanic origin
  • Seamounts are found in all oceans, but are more numerous in the Pacific Ocean, with over 2,000 identified.
  • Guyots – flat-top seamounts
map of seamounts
Map of Seamounts

K. Stocks. 2003. Map of Sampled Seamounts. SeamountsOnline: an online information system for seamount biology. World Wide Web electronic publication. http://seamounts.sdsc.edu.

slide23

Mid-Ocean Ridge

Mid-Atlantic Ridge

Underwater mountain chain that rises from the ocean basins. Created by rising magma.

mid ocean ridge1
MID-OCEAN RIDGE
  • Several mid-ocean ridges are longer than the longest mountain ranges on Earth.
  • Can rise to above sea level to form islands
    • Iceland and the Azores - Atlantic Ocean
    • Galapagos Islands in the Pacific Ocean.
  • Most of the ridges crest at a depth of about 8,000 feet
mid ocean ridge2
MID-OCEAN RIDGE
  • Oceanic ridges have two peaks, separated by a rift valley. The valley ranges from 15 to 30 miles in width and contains an active seismic area.

Americas

Africa / Europe

Example of the Mid-Atlantic Ridge

slide28

Rift Zone

A system of cracks in Earth’s crust through which molten material rises. Rift zones are found in the middle of the mid-ocean ridges. Strange animal life and unique geologic structures have been found here.

rift zone
Rift Zone
  • Divergent zones are where two plates are moving apart
  • Convection currents are rising, bringing up heat
  • Earthquakes and volcanic activity
slide30

29° N

Volcanic ridge on zero-age crust, note small and larger volcanic cones. See cratered volcano at the top? The narrow, linear, bright features in the rest of the image are fault scarps. Uniform gray areas are sediment accumulating.

Rift Zone

slide34

Trench

A deep trough on the ocean floor where oceanic crust is forced below continental or other oceanic crust.

trench
TRENCH
  • Found at subduction zones (near continents and island chains)
  • At least 26 trenches have been identified
    • 22 are in the Pacific Ocean
    • 1in the Atlantic Ocean (Puerto Rico Trench)
    • 1in the Indian Ocean (Java Trench)
trench2
TRENCH
  • Depths of major trenches exceed 18,000 feet, and vary from 10 to 22 miles in width.
  • The deepest is the Challenger Deep, 35,810 feet deep, in the Marianas Trench {Mount Everest - 29,028 feet}
  • Trenches are not the same:
    • Peru-Chile Trench off the west coast of South America is nearly 1,100 miles long.
    • The Japan Trench is 150 miles long and is the shortest.
    • The Tonga Trench, located between New Zealand and Samoa, is the narrowest and straightest.
    • The Kurile Trench between Japan and Kamchatka is the widest.