Commercial fishermen typically do not fish beyond the continental shelf due to several factors, including the increased costs and logistical challenges associated with deep-sea fishing. The waters beyond the shelf are often deeper, making it more difficult and expensive to access, and the fish species available may not be as abundant or commercially viable. Additionally, regulatory restrictions and environmental concerns can limit fishing activities in these areas. Finally, many commercial fisheries are focused on species that are more readily available in shallower waters.
Because for the most part, the continental shelves are where the fish are.
Commercial fishermen do not fish beyond the continental shelf because the waters beyond the shelf are typically deeper and less productive in terms of fish populations. Additionally, fishing beyond the shelf requires more specialized equipment and may involve higher costs and risks compared to fishing within the continental shelf.
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.
The continental shelf is an extension of the cotton, only beneath water. The continental slope begins beyond the shelf and slopes downward.
The shallow extension of the continent that extends beyond the shoreline is called a continental shelf. It is the submerged part of a continent that extends from the shoreline to a drop-off point called the shelf break.
Deep ocean basin
The deepest, darkest area of the ocean that is beyond the edge of the continental shelf.
shelf
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
The abyssal zone is not included in the continental margin. It is the deep ocean floor beyond the continental shelf, slope, and rise.
At the edge of a continent under the ocean lies the continental shelf, a gently sloping extension of the continent covered by shallow seas. Beyond the continental shelf, there is a steeper drop-off known as the continental slope, leading to the deep ocean floor of the abyssal plain.
The ocean floor can be described in terms of three primary features: the continental shelf, continental slope, and continental margin. The continental shelf is the shallow, submerged extension of the land, where the ocean is relatively shallow and rich in marine life. Beyond the shelf, the continental slope descends steeply to the deep ocean floor, marking the transition from the shallow coastal waters to the deep sea. The continental margin encompasses both the shelf and slope, forming the boundary between the continental crust and the oceanic crust.