The two major regions of the ocean floor are the continental margin and the deep ocean basin. The continental shelf is the submerged extension of the continent, characterized by shallow waters, while the continental slope marks the transition between the shelf and the deep ocean, featuring a steep descent. Below the slope lies the continental rise, a more gradual incline formed by sediment accumulation. Together, these features represent a continuum from the landmass to the deep ocean, illustrating the gradual change in depth and geological characteristics of the ocean floor.
the continental Margin, Ocean Basin Floor and Mid-Ocean ridge :D
the continental Margin, Ocean Basin Floor and Mid-Ocean ridge :D
The three main regions of the ocean floor are the continental margins, the ocean basins, and the mid-ocean ridges. Continental margins are the shallow, submerged edges of continents. Ocean basins are the deeper areas of the ocean floor beyond the continental margins. Mid-ocean ridges are underwater mountain ranges where tectonic plates move apart and magma rises to create new oceanic crust.
continental margin deep-ocean basin
The ocean floor is divided into two major regions: the continental margin, which includes the continental shelf, slope, and rise, and the deep ocean basin, which includes abyssal plains, seamounts, trenches, and mid-ocean ridges. These regions have distinct geological features and play important roles in shaping the Earth's surface.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the outer edge of a continent that includes these three regions and extends from the shoreline to the deep ocean floor.
The Continental Shelf ; see related link below .
The two major regions of land under the water are the continental shelf, which is the relatively shallow area surrounding continents, and the ocean basins, which are deeper areas beyond the continental shelf that make up most of the ocean floor.
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.
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.
Continental shelf Continental slope abyss/abyssal plain