Drift
An active continental margin may have a trench.
When oceanic lithosphere and continental lithosphere collide, the continental lithosphere may be obducted over the oceanic lithosphere or the oceanic lithosphere may be subducted under the continental lithosphere. The latter is thought to be more common. This subduction and obduction generally results in tectonic activity such as volcanoes and earthquakes.
Convergent plate margins are characterized as collision zones between plates and may involve continental to continental crust, continental to oceanic crust, or oceanic to oceanic crust. Those that involve oceanic crust result in subduction of the more dense plate into the Earth's mantle. Continental to continental plate collisions result in uplift of the surface features and mountain building and the margin may eventually become welded together.
Oceanic and continental.
The tip of the continental shelf (which has a gentle slope) where if you go any farther, the continental slope forms, which has a very steep slope.
ito ay isang shelf na may 5 araw at gabi
No, it accumulates on the continental shelf and may subsequently move down the continental slope onto the ocean floor in "slump turbidity currents" when disturbed by earthquakes.
The address of the Cape May City Branch is: 110 Ocean St., Cape May, 08204 2320
The address of the Cape May Bookmobile is: Mechanic Street, Cape May Ct. Hse., 08210 1498
The Cape May was created in 2003.
The address of the Cape May County Library is: Mechanic Street, Cape May Ct. Hse., 08210 1498
The slope is the steep transitional area between the shelf and rise. The continental slope depth for the Atlantic Ocean is 3900 meters or in other words 12800 feet.
The address of the Greater Cape May Historical Society is: Po Box 495, Cape May, NJ 08204
Ang Sunda Shelf ay isang malaking nakausling bahagi ng kontinente ng Asya na may lawak na 1 800 000 kilometro kuwadrado.
Cape May Court House
Cape May Light was created in 1859.