Deep Water Waves Sea Floor

Deep sea exploration has revealed varied landscapes which include volcanoes seamounts hydrothermal vents and cold seeps.

Deep water waves sea floor.

These areas are the hadopelagic zone. The action of someone tripping is similar to the interaction between a shallow water wave and the bottom of the ocean. In deep water most waves do not interact with the sea bottom and are called deep 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. Hadopelagic zone deep ocean trenches greater than 6 000m in some places there are trenches that are deeper than the surrounding ocean floor. It might be traveling 500 miles per hour 800 kilometers per hour but it has a very long wavelength and very little amplitude. Perspective view of the sea floor of the atlantic ocean and the caribbean sea.

In deep water the wave reaches its natural frequency without the interruption of a sea floor or lake bottom. Even a tsunami wave can be nearly undetectable on the open ocean. 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. Abyssopelagic zone 4 000 6 000m this is the zone past the continental slope the deep water just over the ocean bottom.

The purple sea floor at the center of the view is the puerto rico trench. The orbits of the water molecules are circular. In fact there have been more missions into space than journeys down to the greatest depths of the oceans.