continental margin
The continental rise is between the continental shelf and the abyssal plain.LittoralLitoral (alternative spelling)Intertidal
the continental shelf begins at the shoreline and slopes gently toward the open ocean the continental rise is the base of the continental slope, which is made up of large pites of sediment the continental slope is the edge of the continental shelf
The continental rise.
The average width of the continental shelf is about 80 km or 50 miles. The Shelf descends steeply down to the continental rise before reaching the ocean floor.
Synonyms for gradient: acclivity, bank, declivity, grade, hill, incline, rise, slope Adjectives that describe gradient: steep gradual positive negative sharp localized
The continental shelf, continental slope, and continental rise combine to form the continental margin.
The continental margin consists of three main subdivisions: the continental shelf, the continental slope, and the continental rise. The continental shelf is the shallow, gently sloping portion closest to the shore. The continental slope is the steeper portion that connects the shelf to the deep ocean floor. The continental rise is the transition zone between the slope and the deep ocean basin, where sediments accumulate.
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.
continental margin
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf, slope, and rise are all part of the continental margin. The continental shelf is the flat, shallow portion closest to the shore, followed by the continental slope, which descends steeply to the ocean floor. The continental rise is a gentle incline at the base of the continental slope. These features are connected and represent the transition from the continent to the deep ocean basin.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
The continental shelf, slope, and rise combine to form the continental margin. The continental shelf is the shallow, submerged extension of a continent, the slope is the steep incline that leads to the ocean floor, and the rise is the gently sloping accumulation of sediment at the base of the slope. Together, they make up the transition zone between the continent and the deep ocean.
The continental shelf, continental slope, and continental rise combine to form the continental margin, which is the submerged outer edge of a continent that extends from the shoreline to the deep ocean floor.
The three parts of the continental margin are the continental shelf, continental slope, and continental rise. The continental shelf is the gently sloping, submerged platform of a continent that extends from the shoreline to the shelf break. The continental slope is a steeper zone that descends from the shelf break to the deep ocean floor. The continental rise is the final gently sloping seafloor region at the base of the continental slope.
The continental shelf, continental slope, and continental rise together form the continental margin. The continental margin is the submerged edge of a continent that consists of these three distinct but connected features.
The continental shelf is basically an extension of a continent into an ocean. It is underwater during interglacial periods (such as today) but dry during glacial periods. The continental slope is the sloping area between the continental shelf and the continental rise (where the continental plate meets the oceanic plate). The continental shelf and the continental slope together are called the continental margin. The continental rise is located at the bottom of the continental slope and is formed by the accumulation of sediment from the continent. Past the continental rise lies the abyssal plain which is the flat ocean floor.