Continental slope, seaward border of the continental shelf. The world’s combined continental slope has a total length of approximately 300,000 km (200,000 miles) and descends at an average angle in excess of 4° from the shelf break at the edge of the continental shelf to the beginning of the ocean

The continental shelf is the relatively shallow water area found in proximity to continents; it is the portion of the continental margin that transitions from the shore out towards to ocean.

The continental slope marks the seaward edge of the continental shelf. Continental slopes typically follow the boundary between continental crust and oceanic crust.

A continental shelf is a portion of a continent that is submerged under an area of relatively shallow water, known as a shelf sea. Much of these shelves were exposed by drops in sea level during glacial periods. The shelf surrounding an island is known as an " insular shelf."

A continental slope refers to the seafloor area between the shelf-slope break and the slope-rise break, where gravity-driven deep-water processes occur. It is characterized by relatively gentle slopes and is influenced by various geological factors such as tectonics and sediment types.

The continental slope (often referred to simply as “the slope”) is commonly dissected by submarine canyons; faulting, rifting and slumping of large blocks of sediment can form steep escarpments, relatively flat terraces and (under certain conditions) basins perched on the slope.

Nov 21, 2023 · Learn the definition of a continental slope and understand how it differs from a continental shelf. See facts about continental slopes. Updated: 11/21/2023. What is a Continental Slope?...

The continental slope is defined as the zone extending from the shelf break and terminating at the continental rise where the gradient becomes less than 1:40 or where the slope is bounded by a deep-sea trench or a marginal plateau.

Jan 24, 2022 · The continental slope is defined as the zone extending from the shelf break and terminating at the continental rise where the gradient becomes less th. Continental slopes would be the edges of continental blocks, the zones of vary from continental crust to oceanic crust.

The continuously sloping portion of the continental margin, seaward of the continental shelf and extending down to the deep sea floor of the abyssal plain, is known as continental slope. It is charactersied by gradients of 2.5 degrees. It extends between the depth of 180 to 3600 metres.