continental slopes
continental slope
A ledge
The symbiosis between Shelf Fungi and Hickory trees is Parasitism.
It'a actually a Contiental Shelf. To be Exact.
A shelf cloud is produce by thunderstorm outflow, resulting from rain cooled air being force downward and outward in a thunderstorm. A shelf cloud may indicate that strong straight-line winds are coming A wall cloud is found in the mesocyclone, or rotating updraft of a type of thunderstorm called a supercell. This is an indicator that a tornado may soon form.
The continental shelf
The steep side of the edge of a continent is called a continental slope. This feature marks the transition between the continental shelf and the deep ocean floor.
the continental slope
The transition zone between an ocean basin floor and a continent is known as the continental shelf. It is the submerged part of a continent that extends from the shoreline to the continental slope. The continental shelf is characterized by relatively shallow waters and is an area of high biological productivity.
The geologic edge of a continent is typically defined by the continental shelf, which is the submerged part of the continent that slopes downward into the ocean basin. This transition from the continental shelf to the deep ocean is called the continental slope.
The general term is seafloor. Along the edges of large land masses, the continental shelf is part of the seafloor.
The edge is called the shelf break. The actual declining shelf is called the called the continental slope.
shelf
The best way to describe such a region would be as a continental slope. This area marks the boundary between the shallow continental shelf and the deep ocean floor. It is characterized by a steep incline leading down to the ocean basin.
continental slope
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
It is called The Continental Shelf.