Chapter 11 Flashcards
Oceans
Ocean floor age
The youngest part of the Earth’s surface.
Ocean mapping methods (2)
Sonar and geoids
Sonar
Sound navigation and ranging
Geoids
Idealized surface of oceans representing gravitational equipotential surfaces.
Geoid low = mass deficit
Geoid high = excess mass
Passive continental margins
Change from continental crust to oceanic crust on the same tectonic plate.
Active continental margins
Plate boundary where one plate subducts below another. Accretionary wedge formed as sediments are scrapped of plate.
Deep-ocean basin features (3)
- Trenches formed by subduction
- Abyssal plains
- Seamounts (extinct volcanoes)
Seafloor features (5)
Continental margins, deep-ocean basins, oceanic ridges, coral reefs and atolls, sea-floor sediments
Continental shelf
Flooded extension of the continent that is 0-1500 km wide (average of 80 km).
Continental slope
Boundary between continental crust and oceanic crust formed by rifting as continents split apart. The average slope is 5°.
Continental rise
Accumulation of sediments at base of a continental slope of around 0.3°. (EX: deep sea fans)
Mid-ocean ridges
Location that is volcanic in origin where plate moves apart at a ridge crest through sea-floor spreading. As plates move away from the ridge, they cools and contracts and ocean gets deeper. 20% of the surface of the Earth (70,000 km long and 1000-4000 km wide)
Mid-ocean ridges on land
When ocean basins close, the oceanic crust can be placed on land to form an ophiolite. Form volcanogenic massive sulfide (VMS) deposits.
Coral reefs and atolls
Form as plates move away from mid-ocean ridges and as volcanoes become extinct. Growth can keep up with subsidence.
Sea-floor sediment types (2)
Terrigenous and biogenous