Https Www Slideshare Net Rbosch Landforms Found On The Ocean Floor Presentation

The deep ocean floor becomes th e resting place for terrestrial sediment eroded fro m the land.

Https www slideshare net rbosch landforms found on the ocean floor presentation.

Ocean trench the ocean trench is a steep sided canyon or deep narrow valley in the bottom of the ocean. No oceanic crust older than 180 ma old is known from the present oceans 4. Today s technology particularly sonar satellites and submersibles allows scientists to study the ocean floor in a more. The deep ocean floor a guyot is a seamount that has eroded so that it has a flat top and is underwater.

14 1 the vast world ocean the topography of the ocean floor is as diverse as that of the continents. Bathymetry is the measurement of ocean depths and the charting of the shape or topography of the ocean floor. Ocean basin the ocean basin is located on either side of the mid ocean ridge. Mid ocean ridges mark places where two tectonic plates are separating and new ocean crust is being made.

Deep ocean trenches are the deepest parts of the ocean. It is made up of low hills and flat plains. Presentation about effects of waves currents tides and storms on geologic features of the ocean shore zone. Relatively short lived features on the planet.

Presentation of geologic landform features of the ocean floor as aligned to south carolina state standards. Https url cn ktfcrshz 3 months. Benthos is the community of organisms which live on in or near the seabed the area known as the benthic zone. Landforms found on the ocean floor 2.

It was the interval of time during which the continents assumed their modern configuration and geographic positions and during which earth s flora and fauna evolved toward. Ocean floor from 2 mybp to present current scenario. A seamount is a steep sided mountain that rises from the ocean floor. Trenches are the deepest part of the ocean basin and deeper than any valley found on land.

Ocean floor ocean floor is the bottom of the ocean. Ocean floors have a common structure created from tectonic movement and sediment from various sources. This community lives in or near marine sedimentary environments from tidal pools along the foreshore out to the continental shelf and then down to the abyssal depths the benthic zone is the ecological region on in and immediately above the seabed including the sediment surface. Capin richelle and gamoso ervhic.

Cenozoic era third of the major eras of earth s history beginning about 66 million years ago and extending to the present. Beach drifting transports sand grains along t he beach as waves strike the shore at an oblique an gle.