The word that describes the variation in ocean depth from shallow shelves to deep trenches is "bathymetry." Bathymetry refers to the measurement of underwater depths and the topography of the ocean floor. This term encompasses the study of submarine features such as continental shelves, abyssal plains, and oceanic trenches, providing insights into the diverse and dynamic nature of the Earth's oceans.
within or adjacent to trenches
Often, it is hydrated mantle coming from the Earth's core
False, continental shelves are part of the Coastal Plain
Continents have continental shelves, which are relatively shallow regions surrounding the continent, where the ocean is not as deep as it gets farther out.
Continents have continental shelves, which are relatively shallow regions surrounding the continent, where the ocean is not as deep as it gets farther out.
Hydrologically, an oceanic basin may be anywhere on Earth that is covered by seawater, but geologicallyocean basins are large geologic basins that are below sea level. Geologically, there are other underseageomorphological features such as the continental shelves, the deep ocean trenches, and the underseamountain ranges (for example, the mid-Atlantic ridge) which are not considered to be part of the ocean basins; while hydrologically, oceanic basins include the flanking continental shelves and shallow, epeiric seas.
Most of the deep-sea trenches are located in the Pacific Ocean. These trenches are formed by the subduction of tectonic plates, where one plate slides beneath another, creating deep underwater chasms. The Mariana Trench, the deepest known trench on Earth, is located in the Pacific Ocean.
The continental shelves were developed in between the glacial periods as the ocean flowed over the continents forming shallow areas along the coasts. The continental shelves developed today were formed like 18000 years ago.
there are three ocean trenches in the Atlantic Ocean
The continental shelf is the shallow part of the ocean.
The continental shelves were developed in between the glacial periods as the ocean flowed over the continents forming shallow areas along the coasts. The continental shelves developed today were formed like 18000 years ago.
It comes from sea mounts and ocean trenches.