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Continental rise information


Cross Section of Continental Margin

The continental rise is a low-relief zone of accumulated sediments that lies between the continental slope and the abyssal plain.[1] It is a major part of the continental margin, covering around 10% of the ocean floor.[1][2]

  1. ^ a b Mitchell, N. C. (2015), "Submarine Geomorphology☆", Reference Module in Earth Systems and Environmental Sciences, Elsevier, ISBN 978-0-12-409548-9
  2. ^ Patruno, Stefano; Helland-Hansen, William (2018). "Clinoforms and clinoform systems: Review and dynamic classification scheme for shorelines, subaqueous deltas, shelf edges and continental margins". Earth-Science Reviews. 185: 202–233. Bibcode:2018ESRv..185..202P. doi:10.1016/j.earscirev.2018.05.016. hdl:1956/18533. ISSN 0012-8252.

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Continental rise

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The continental rise is a low-relief zone of accumulated sediments that lies between the continental slope and the abyssal plain. It is a major part of...

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Continental shelf

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sediments deposited by turbidity currents from the shelf and slope. The continental rise's gradient is intermediate between the gradients of the slope and the...

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Continental margin

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The continental margin consists of three different features: the continental rise, the continental slope, and the continental shelf. The continental shelf...

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Seabed

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toward the continents and becomes, in order from deep to shallow, the continental rise, slope, and shelf. The depth within the seabed itself, such as the...

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Continental philosophy

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Continental philosophy is a term used as an umbrella term for philosophies prominent in continental Europe.[page needed] Continental philosophy includes...

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Demersal fish

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found on or near the continental shelf, and in deep waters, they are found on or near the continental slope or along the continental rise. They are not generally...

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Atlantic Ocean

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11% of the bottom topography with few deep channels cut across the continental rise. The mean depth between 60°N and 60°S is 3,730 m (12,240 ft), or close...

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Abyssal plain

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metres (9,800 and 19,700 ft). Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains cover more than 50% of the Earth's...

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Hudson Canyon

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notch of about 1 km depth in the shelf break, and running down the continental rise. Tidally associated flows of about 30 cm/s (1.1 km/h) up and down the...

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Eustatic sea level

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relative sea level depends on many factors - including tectonics, continental rise and subsidence. Eustatic sea level follows the "bathtub approach" which...

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Benham Rise

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Commission on the Limits of the Continental Shelf in relation to the continental shelf in the region of the Philippine Rise. It was submitted as part of...

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Sedimentary rock

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and thinned, so that the hot asthenosphere rises and heats the overlying rift basin. Apart from continental sediments, rift basins normally also have part...

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Gastropoda

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In marine habitats, the continental slope and the continental rise are home to the highest diversity, while the continental shelf and abyssal depths...

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Contourite

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A contourite is a sedimentary deposit commonly formed on continental rises in lower slope settings, although it may occur anywhere that is below the storm...

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Continental drift

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Continental drift is the hypothesis, originating in the early 20th century, that Earth's continents move or drift relative to each other over geologic...

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Marine sediment

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in the water. Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic...

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First Continental Congress

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The First Continental Congress was a meeting of delegates of 12 of the Thirteen Colonies held from September 5 to October 26, 1774 at Carpenters' Hall...

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Sandstone

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most rapid in areas of high relief, such as volcanic arcs, areas of continental rifting, and orogenic belts. Eroded sand is transported by rivers or...

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Continental System

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The Continental Blockade (French: Blocus continental), or Continental System, was a large-scale embargo by French Emperor Napoleon I against the British...

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Contemporary philosophy

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the increasing professionalization of the discipline and the rise of analytic and continental philosophy. The phrase "contemporary philosophy" is a piece...

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Sedimentation

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their elevation, particularly considering increasing rates of sea-level rise. Sedimentation enhancing strategies aim to increase sedimentation on the...

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Exclusive economic zone

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definition of the continental shelf does not correspond exactly to the geological meaning of the term, as it also includes the continental rise and slope, and...

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Continental crust

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Continental crust is the layer of igneous, metamorphic, and sedimentary rocks that forms the geological continents and the areas of shallow seabed close...

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Oceanic plateau

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oceanic plateaus, however, are made of rifted continental crust, for example the Falkland Plateau, Lord Howe Rise, and parts of Kerguelen, Seychelles, and...

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List of islands by area

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For size and location reference, four very large continental landmasses are also shown. Continental landmasses are not usually classified as islands despite...

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Passive margin

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remarkably similar. Typically they consist of a continental shelf, continental slope, continental rise, and abyssal plain. The morphological expression...

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Obduction

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adjacent plate. When oceanic and continental plates converge, normally the denser oceanic crust sinks under the continental crust in the process of subduction...

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Continent

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including both dry land and continental shelves". The geological continents correspond to seven large areas of continental crust that are found on the...

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Bellingshausen Plain

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Bellinghausen Abyssal Plain, is an undersea plain parallel to the continental rise in the Bellingshausen Sea, named for Admiral Fabian Gottlieb von Bellingshausen...

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