The Ocean Floor Topography Is Much Less Diverse Than That Of The Continents

Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet.

The ocean floor topography is much less diverse than that of the continents. The ocean floors topography is much less diverse than that of the continents. Ocean currents govern the world s weather and churn a kaleidoscope of life. This study is extensive and it has been established that the ocean floor has similar features of mountains and valleys as on the earth. A system using transmitted and reflected underwater sound waves to detect and locate submerged objects or measure the distance to the floor of deep water.

The measurement of ocean depth and the charting o the shape or topography of the ocean floor. The oceans floors topography is much less diverse than that of the continents. What do scientists call the charting of the ocean floor and measurement of its depth. The ocean floor s topography is much less diverse than that of the continents.

The ocean is a continuous body of salt water that covers more than 70 percent of the earth s surface. Chemical weathering of rocks on the continents is one source of elements found in sea water. The ocean floor actually does have significant and diverse topography. Electric depth sounding equipment called allowed scientists in the 1920 s and later to precisely measure ocean depth.

The ocean floors typography is much less diverse than that of the continents. Name three topographic features found on the ocean floor. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Compare and contrast the use of all satellites and submersibles to collect data about the topography of the seafloor.

Ocean floor topography involves the study of ocean bottom features including the outer continental shelf continental slopes and ocean waves desktops. Mid ocean ridges trenches abyssal plains. The ocean floor s topography is much less diverse than that of the continents. The under water topography maps have been developed by the study of ocean floor topography.

The following features are shown at example depths to scale though each feature has a considerable range at which it may occur. Is the measurement of the ocean depths and charting of the topography of the ocean floor. Panthalassa was an early form of the pacific ocean which today experiences less seafloor spreading and has a much less extensive mid ocean ridge system. There are the midocean ridges such as the mid atlantic ridge which are like underwater mountain ranges wide expanses of abyssal plains which are generally flat isolated high points called.

The topography of the ocean floor is as diverse as that of continents.