List of submarine topographical features


This is a list of submarine topographical features, oceanic landforms and topographic elements.

Abyssal plain

An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between and. Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains are among the flattest, smoothest and least explored regions on Earth. Abyssal plains are key geologic elements of oceanic basins. In addition to these elements, active oceanic basins also typically include an oceanic trench and a subduction zone. Abyssal plains cover more than 33% of the ocean floor, but they are poorly preserved in the sedimentary record because they tend to be consumed by the subduction process.
The abyssal plain is formed when the lower oceanic crust is melted and forced upwards by the asthenosphere layer of the upper mantle. As this basaltic material reaches the surface at mid-ocean ridges, it forms new oceanic crust. Abyssal plains result from the blanketing of an originally uneven surface of oceanic crust by fine-grained sediments, mainly clay and silt. Much of this sediment is deposited from turbidity currents that have been channeled from the continental margins along submarine canyons down into deeper water. The remainder of the sediment is composed chiefly of pelagic sediments.
Use of a continuously recording fathometer enabled Tolstoy & Ewing in the summer of 1947 to identify and describe the first abyssal plain. This plain, located to the south of Newfoundland, is now known as the Sohm Abyssal Plain. Following this discovery many other examples were found in all the oceans.

List of abyssal plains and oceanic basins

Following is a list of named abyssal plains and oceanic basins:
NameAlternate nameOceanCoordinates
Adriatic Abyssal PlainMediterranean Sea
Agulhas BankSouth Atlantic Ocean
Alaska PlainNorth Pacific Ocean
Alborán PlainAlboran Sea
Aleutian BasinNorth Pacific Ocean
Amerasian Basin
Amundsen BasinArctic Ocean
Amundsen PlainSouthern Ocean
Angola PlainSouth Atlantic Ocean
Argentine Abyssal PlainSouth Atlantic Ocean
Atlantic-Indian BasinIndian Ocean
Balearic Abyssal PlainMediterranean Sea
Baffin BasinNorth Atlantic Ocean
Barracuda PlainNorth Atlantic Ocean
Bauer Basin
Bellingshausen PlainSouthern Ocean
Biscay PlainNorth Atlantic Ocean
Blake BasinNorth Atlantic Ocean
Boreas PlainArctic Ocean
Burdwood Abyssal PlainSouth Atlantic Ocean
Canada Plain. One of two sub-basins of the Amerasian Basin.Arctic Ocean
Canary Basin
Cape PlainSouth Atlantic Ocean
Cape Verde PlainNorth Atlantic Ocean
Cascadia PlainNorth Pacific Ocean
Ceará PlainNorth Atlantic Ocean
Central Pacific Basin
Ceylon PlainIndian Ocean
Chile Basin
Chukchi PlainArctic Ocean
Cocos Abyssal PlainIndian Ocean
Colombian PlainCaribbean Sea
Comoro PlainMozambique Channel
Cuvier PlainIndian Ocean
Demerara PlainNorth Atlantic Ocean
Dibble BasinSouthern Ocean
Dumshaf PlainArctic Ocean
Enderby PlainSouthern Ocean
Eratosthenes Abyssal PlainMediterranean Sea
Eurasian BasinArctic Ocean
Euxine Abyssal PlainBlack Sea
Fernando de Noronha PlainSouth Atlantic Ocean
Ferradura PlainNorth Atlantic Ocean
Fletcher PlainArctic Ocean
Florida PlainGulf of Mexico
Fram Basin One of two sub-basins of the Eurasian Basin.Arctic Ocean
Gambia PlainNorth Atlantic Ocean
Gascoyne PlainIndian Ocean
Greenland PlainArctic Ocean
Grenada Abyssal PlainCaribbean Sea
Guiana Basin
Guinea PlainNorth Atlantic Ocean
Hatteras PlainNorth Atlantic Ocean
Herodotus BasinLevantine Sea
Hellenic TrenchIonian Sea
Hispaniola PlainNorth Atlantic Ocean
Horseshoe PlainNorth Atlantic Ocean
Iberian PlainNorth Atlantic Ocean
Jamaican Abyssal PlainCaribbean Sea
Japan PlainSea of Japan
JOIDES BasinSouthern Ocean
Labrador BasinNorth Atlantic Ocean
Laurentian AbyssNorth Atlantic Ocean
Madeira Abyssal PlainNorth Atlantic Ocean
Makarov Basinone of two sub-basins of the Amerasian Basin.Arctic Ocean
Mascarene PlainIndian Ocean
Melanesian Basin
Mendeleyev PlainArctic Ocean
Mid Indian Abyssal PlainIndian Ocean
Mornington Abyssal PlainSouth Pacific Ocean
Namibia Abyssal PlainSouth Atlantic Ocean
Nansen BasinOne of two sub-basins of the Eurasian Basin.Arctic Ocean
Nares PlainNorth Atlantic Ocean
Natal Basin
Newfoundland BasinNorth Atlantic Ocean
North Australian BasinIndian Ocean
North Polar Basin
Northwest Pacific Basin
Northwind Plain USCGC Northwind Arctic Ocean
Okhotsk Abyssal PlainSea of Okhotsk
Oman PlainArabian Sea
Panama PlainCaribbean Sea
Papua PlainSouth Pacific Ocean
Para Abyssal PlainNorth Atlantic Ocean
Penrhyn Basin
Pernambuco PlainSouth Atlantic Ocean
Perth PlainIndian Ocean
Peru Basin
Pole PlainArctic Ocean
Porcupine Abyssal PlainNorth Atlantic Ocean
Raukumara Abyssal PlainSouth Pacific Ocean
Rhodes BasinSea of Crete
Roggeveen Basin
Sardino-Balearic PlainMediterranean Sea
Seine PlainNorth Atlantic Ocean
Siberian Abyssal PlainArctic Ocean
Sicilia PlainMediterranean Sea
Sierra Leone PlainNorth Atlantic Ocean
Sigsbee DeepGulf of Mexico
Silver PlainNorth Atlantic Ocean
Sirte BasinLibyan Sea
Sohm Abyssal PlainNorth Atlantic Ocean
Somali PlainIndian Ocean
South Australian PlainIndian Ocean
South China BasinSouth China Sea
South East Pacific Basin
South Fiji Basin
South Indian PlainSouthern Ocean
South West Pacific Abyssal PlainSouth Pacific Ocean
Tagus Abyssal PlainNorth Atlantic Ocean
Tasman PlainTasman Sea
Town Abyssal PlainSouth Atlantic Ocean
Tsushima BasinKorea Strait
Tufts PlainNorth Pacific Ocean
Tyrrhenian PlainTyrrhenian Sea
Valdivia Abyssal PlainSouthern Ocean
Venezuelan PlainCaribbean Sea
Vidal Abyssal PlainNorth Atlantic Ocean
Weddell PlainSouthern Ocean
Wrangellia TerraneArctic Ocean
Yamato BasinSea of Japan
Yucatan Abyssal PlainCaribbean Sea

Oceanic trenches

es are long, narrow topographic depressions of the seabed. They are the deepest parts of the ocean floor, and they define one of the most important natural boundaries on the Earth's solid surface: the one between two lithospheric plates. Trenches are a distinctive morphological feature of plate boundaries. Trenches are found in all oceans with the exception of the Arctic Ocean and they are most common in the North and South Pacific Oceans.
There are three types of lithospheric plate boundaries: 1.) divergent convergent transform.
An oceanic trench is a type of convergent boundary at which two oceanic lithospheric slabs meet; the older of these slabs flexes and subducts beneath the other slab. Oceanic lithosphere moves into trenches at a global rate of about a tenth of a square meter per second. Trenches are generally parallel to a volcanic island arc, and about 200 km from a volcanic arc. Oceanic trenches typically extend 3 to 4 km below the level of the surrounding oceanic floor. The greatest ocean depth to be sounded is in the Challenger Deep of the Mariana Trench, at a depth of 10,911 m below sea level.

List of oceanic trenches

The following is a list of the deepest parts of the Earth's oceans and seas :
NameLocationDepth Depth Depth
1Challenger DeepIzu-Bonin-Mariana Arc, Mariana Trench, Pacific Ocean11,03436,1976.86
2Tonga TrenchPacific Ocean10,88235,7026.76
3Galathea DepthPhilippine Trench, Pacific Ocean10,54534,5806.54
4Kuril-Kamchatka TrenchPacific Ocean10,54234,4496.52
5Kermadec TrenchPacific Ocean10,04732,9636.24
6Izu-Ogasawara TrenchPacific Ocean9,81032,0876.08
7Japan TrenchPacific Ocean9,00029,5275.59
8Puerto Rico TrenchAtlantic Ocean8,60528,2325.35
9Yap TrenchPacific Ocean8,52727,9765.30
10South Sandwich TrenchAtlantic Ocean8,42827,6515.24
11Richards DeepPeru–Chile Trench, Pacific Ocean8,06526,4565.01
12Diamantina DeepDiamantina Fracture Zone, Indian Ocean8,04726,4015.00
13Romanche TrenchAtlantic Ocean7,76025,4604.82
14Cayman TroughCaribbean Sea7,68725,2384.78
15Aleutian TrenchPacific Ocean7,67925,1944.77
16Java TrenchIndian Ocean7,45524,4604.63
17Weber DeepBanda Sea7,35124,1174.56
18Middle America TrenchPacific Ocean6,66921,8804.14
19Puysegur TrenchPacific Ocean6,30020,7003.9
20Vityaz TrenchPacific Ocean6,15020,1773.8
21Litke DeepEurasian Basin*, Arctic Ocean5,45017,8813.39
22Manila TrenchSouth China Sea5,40017,7003.36
23Calypso DeepHellenic Trench, Mediterranean Sea5,26717,2803.27
24Ryukyu TrenchPacific Ocean5,21217,1003.24
25Murray Canyon*Southern Ocean, Australia5,00016,4003.1

An oceanic plateau is a large, relatively flat submarine region that rises well above the level of the ambient seabed. While many oceanic plateaus are composed of continental crust, and often form a step interrupting the continental slope, some plateaus are undersea remnants of large igneous provinces. Continental crust has the highest amount of silicon. Oceanic crust has a smaller amount of silicon.
The anomalous volcanism associated with the formation of oceanic plateaux at the time of the Cenomanian-Turonian boundary ago may have been responsible for the environmental disturbances that occurred at that time. The physical manifestations of this were elevated atmospheric and oceanic temperatures, a significant sea-level transgression, and a period of widespread anoxia, leading to the extinction of 26% of all genera. These eruptions would also have resulted in the emission of large quantities of carbon dioxide into the atmosphere, leading to global warming. Additionally, the emission of sulfur monoxide, hydrogen sulfide, carbon monoxide, and halogens into the oceans would have made seawater more acidic resulting in the dissolution of carbonate, and further release of. This runaway greenhouse effect was probably put into reverse by the decline of the anomalous volcanic activity and by increased -driven productivity in oceanic surface waters, leading to increased organic carbon burial, black shale deposition, anoxia and mass extinction in the ocean basins.
, Bounty Trough, Campbell Plateau, Challenger Plateau, Chatham Rise, Havre Trough, Hikurangi Plateau, Kermadec Trench, Lord Howe Rise, Louisville Ridge, New Caledonia Basin, Norfolk Ridge, South Fiji Basin, South West Pacific Basin, and Tasman Basin.

List of oceanic plateaus

A mid-ocean ridge is a general term for an underwater mountain system that consists of various mountain ranges, typically having a valley known as a rift running along its spine, formed by plate tectonics. This type of oceanic ridge is characteristic of what is known as an oceanic spreading center, which is responsible for seafloor spreading.

List of mid-ocean ridges