Deep Water Waves Sea Floor

Hadopelagic zone deep ocean trenches greater than 6 000m in some places there are trenches that are deeper than the surrounding ocean floor.

Deep water waves sea floor.

In deep water the wave reaches its natural frequency without the interruption of a sea floor or lake bottom. It might be traveling 500 miles per hour 800 kilometers per hour but it has a very long wavelength and very little amplitude. The purple sea floor at the center of the view is the puerto rico trench. Deep sea exploration has revealed varied landscapes which include volcanoes seamounts hydrothermal vents and cold seeps.

Perspective view of the sea floor of the atlantic ocean and the caribbean sea. The orbits of the water molecules are circular. Even a tsunami wave can be nearly undetectable on the open ocean. The deep sea is a relatively mysterious and unknown part of the earth as only about 1 of the ocean floor has been explored by humans.

The action of someone tripping is similar to the interaction between a shallow water wave and the bottom of the ocean. Shallow water waves figure 7 4b waves which interact with the sea floor are known as shallow water waves. When deep water waves move into shallow water they change into breaking waves. When the energy of the waves touches the ocean floor the water particles drag along the bottom and flatten their orbit fig.

Roughly 97 of the planet s water is in its oceans and the oceans are the source of the vast majority of water vapor that condenses in the atmosphere and falls as rain or snow on the continents. This is also known as the abyssal zone. These areas are the hadopelagic zone.