A geophysics b seismic tomography c topographic surveying d bathymetry.
The topography of the ocean floor is known as.
This study is extensive and it has been established that the ocean floor has similar features of mountains and valleys as on the earth.
Topography of the northern red sea and its main morphotectonic the ocean floor is less well mapped than surface of other topography of the earth reveals seafloor spreading ridge the ocean s ultimate trashcan hadal trenches as major.
Like land terrain the ocean floor has ridges valleys plains and volcanoes.
Map showing the underwater topography of the ocean floor.
Bathymetry the shape of the ocean floor is largely a result of a process called plate tectonics the outer rocky layer of the earth includes about a dozen large sections called tectonic plates that are arranged like a spherical jig saw puzzle floating on top of the earth s hot flowing mantle.
Because massive submarine structures such as seamounts and ridges exert stronger than average gravitational attraction they produce depressed areas on the ocean s surface.
The topography of ocean floor is none too well known.
The under water topography maps have been developed by the study of ocean floor topography.
Plate tectonics and the ocean floor.
The measurement of ocean depth and the topography of the ocean floor are known as.
This product is intended to aid fishermen and those needing seafloor features and potential fishing grounds.
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Topographic maps of the sea floor produced at a 1 100 000 scale that contain loran c rates bottom sediment types and known bottom obstructions.
The seabed also known as the seafloor sea floor or ocean floor is the bottom of the ocean no matter how deep.
A 1 500 m sec b 5 000 m sec c 3 200 m sec d 10 994 m sec.
From the late 19th century when the norwegian explorer fridtjof nansen first discovered an ocean in the central arctic until the middle of the 20th century it was believed that the arctic ocean was a single large basin.
Arctic ocean arctic ocean topography of the ocean floor.
All floors of the ocean are known as seabeds.
Explorations after 1950 revealed the true complex nature of the ocean floor.
The measurement of ocean depth and the topography of the ocean floor are known as.