Age Of Ocean Floor Definition

Mountains plains channels canyons exposed rocks and sediment covered areas.

Age of ocean floor definition.

Therefore seafloor dating isn t that useful for studying plate motions beyond the cretaceous. Other articles where ocean floor is discussed. The process that continually adds new material to the ocean floor is seafloor spreading and the continental slope. Seabed contains several hundred years worth of cobalt and nickel.

The following features are shown at example depths to scale though each feature has a considerable range at which it may occur. Age of the ocean floor a critical analysis. In recent years satellite images show a very clear mapping of the seabed and are used extensively in the study and exploration of the ocean floor. The arrival of water 1400 mya solidified the molten crust and by 1200 mya submerged.

The ionic growing earth ige posits the same 8 elements that started the earth heated the planet for the first 3 3 5 billion years of its existence see ige fig. The lack of weathering and erosion in most areas however allows geological processes to be seen more clearly on. To get the dependence on x one must substitute t x v ax l where l is the distance between the ridge to the continental shelf roughly half the ocean width and a is the ocean basin age. For that geologists date and study continental crust.

This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Because of this correlation between age and subduction potential very little ocean floor is older than 125 million years and almost none of it is older than 200 million years. The ocean floor is literally the floor of the ocean. The ocean floor has the same general character as the land areas of the world.

February 4 2019 eugene ellis. Exploration of the seafloor and the earth s crust. The data is from four companion digital models of the age age uncertainty spreading rates and spreading asymmetries of the world s ocean basins. This dataset shows the age of the ocean floor along with the labeled tectonic plates and boundaries.

Rather than height of the ocean floor above a base or reference level the depth of the ocean is of interest.