Different Types Of Surfaces Of Oceans Floor

The most intuitive and commonly used classification is based on the wave period or the associated wavelength.

Different types of surfaces of oceans floor.

Not only is oceanic crust continually created at mid ocean ridges but it is also continually. In table 1 a summary of the different types of surface waves is presented. The different types are. 2 types of ocean waves and wave classification.

Transform boundaries are faults that connect two areas where plates are converging or diverging. The layers range from the surface layer where most ocean activities occur to the deep dark depths of the water that have yet to be fully explored. Consisting of a nar row. The surface of the ocean bulges outward and inward mimicking the topography of the ocean floor.

The deep layers have unique sea creatures freezing temperatures and high pressure. Oceanic crust the outermost layer of earth s lithosphere that is found under the oceans and formed at spreading centres on oceanic ridges which occur at divergent plate boundaries. The mid ocean ridges are the most extensive fea tures of the earth s surface. The grain size indicates the type of sediment and the environment in which it was created.

The bumps too small to be seen can be measured by a radar altimeter aboard a satellite. Ocean waves can be classified in several ways kinsman 1965. As scientific knowledge has advanced the capability to envisage these remote sites has increased significantly. Below the ocean floor there are a few small deeper areas called ocean trenches.

These sediments vary in size anywhere from 1 4096 of a mm to greater than 256 mm. Where plates diverge from each other molten magma flows upward between the plates forming mid ocean ridges underwater volcanoes hydrothermal vents and new ocean floor crust. Ocean floor topography refers to the different forms in which the ocean floor bottom can exist. Like dry land the ocean floor has various features including flat plains sharp mountains and rugged canyons fig.

However the lowest point in the world ocean is much deeper than the highest point on land. Holthuijsen 2007 among others. The ocean floor is continually being formed and destroyed. The ocean has 5 different and distinct layers that each have their own unique characteristics.

Features of the ocean include the continental shelf slope and rise. Another major structural feature of. Satellite imagery may also be used to map features in the water such as coral reefs. The edges of these continental boundaries usually form zig zag patterns.

Ocean floor mid ocean ridges. The ocean floor is called the abyssal plain. You may perceive the ocean floor to be flat and sandy like the beach but the truth is there are many different surfaces.