Back to Coastal and Oceanic Landform
gentler slopes found on passive margins.
Southern Bay of Biscay, NE Atlantic,Spain.
800 km long.
1,200 m deep.
- It is a steep-sided valley.
- That cut into the sea floor of the continental slope.
- It extending to the continental shelf.
- Found at large rivers.
- Canyons cutting the continental slopes.
- Depths greater than 2 km below sea level.
- They continue as submarine channels.
- It extend for 100 of km.
The Congo Canyon |
- Common submarine canyons ;
gentler slopes found on passive margins.
- The walls are generally very steep (near vertical).
- The walls are subject to erosion by bioerosion / slumping.
- Canyons present today were carved during glacial times.
- The major mechanism to be turbidity currents & underwater landslides.
- Turbidity currents are dense.
- Slope failures landslides are;
-The effects of ;
bioerosion
burrowing
ingestion
-Defecation of sediment performed by organisms.
2. Slumping = - Rotational movement of masses on a hillside,Landslides, / slides.
- Comprise detachment & displacement of sediment masses.
3.Submarine = - Sea bed cut off from the larger ocean.
- The sea normally repleted by contact.
- Inflow from the ocean.
- Avilés Canyon = The deepest submarine canyon.
Southern Bay of Biscay, NE Atlantic,Spain.
- Congo Canyon = The largest river canyon.
800 km long.
1,200 m deep.
- Zhemchug Canyon = The largest submarine canyon.
- Amazon Canyon,Amazon River
- Hudson Canyon, Hudson River
- Ganges Canyon,Ganges
- Indus Canyon,Indus River
- Monterey Canyon, off the coast of central California
- Bering Canyon, Bering Sea
- Kaikoura Canyon, Offshore from the Kaikoura Peninsula, New Zealand
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