A deep crack carved into the continental shelf and slope is called a submarine canyon. These canyons are formed by processes such as erosion from sediment-laden currents and underwater landslides. They can extend into the deep sea, creating steep, narrow valleys that significantly influence oceanic sediment transport and marine ecosystems. Submarine canyons are often associated with river systems that deliver sediment to the ocean.
shelf
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.
A sharp drop-off beyond the continental shelf is called a continental slope. The continental slope marks the transition between the continental shelf and the deep ocean floor.
It is called the continental shelf.
The continental shelf layer is called the shelf break. It is the steepest part of the continental shelf where the seafloor drops off sharply towards the deeper ocean floor.
It is part of a continental plate that is submerged by the ocean. At the edge of the continental shelf, the slope suddenly increases and begins to drop off, this is called the continental slope.
actually,the continental shelf is roughly 3,000,000 m. long
The edge of a continental shelf is called the "shelf break." This is the point where the seabed steeply descends into the continental slope, marking the transition from the relatively shallow waters of the continental shelf to the deeper oceanic waters. The shelf break typically occurs at depths of around 100 to 200 meters, although this can vary depending on the geographical location.
The continental shelf, continental slop and the ocean floor
continental shelf peninsula
Continental Shelf
The seaward edge of the continental shelf is marked by the shelf break, which is the steep slope that descends from the continental shelf to the deep ocean floor. This is where the ocean depth abruptly increases, indicating the boundary between the continental shelf and the continental slope.