Search results
Results from the WOW.Com Content Network
An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 and 6,000 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 surface.
An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 meters (9,800 ft) and 6,000 meters (20,000 ft).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. [1]
The bight is fairly shallow with the continental shelf extending far offshore except off south Florida and North Carolina. The Blake Plateau forms a zone of intermediary depth before dropping to the Hatteras Abyssal Plain with the Blake Escarpment. The Escarpment is defined as the geological bathymetric eastern boundary of the bight.
At the other end of the spectrum, benthos of the deep ocean includes the bottom levels of the oceanic abyssal zone. [7] For information on animals that live in the deeper areas of the oceans see aphotic zone. Generally, these include life forms that tolerate cool temperatures and low oxygen levels, but this depends on the depth of the water. [8]
Cusk eels produce sounds to mate. Male cusk eels have two pairs of sonic muscles, while female cusk eels have three. [8] Abyssal grenadier: this resident of the abyssal zone is known to live at depths ranging from 800 and 4,000 meters. It has extremely large eyes, but a small mouth.
Scotoplanes live on deep ocean bottoms, specifically on the abyssal plain in the Atlantic, Pacific and Indian Oceans, typically at depths of over 1,200 to 5,000 meters (3,900 to 16,400 feet) [5] [6] Some related species can be found in the Antarctic.
Also, scientists have discovered that the deeper these creatures live, the more gelatinous their flesh and more minimal their skeletal structure. These creatures have also eliminated all excess cavities that would collapse under the pressure, such as swim bladders. [11] Pressure is the greatest environmental factor acting on deep-sea organisms ...
Historically, the hadal zone was not recognized as distinct from the abyssal zone, although the deepest sections were sometimes called "ultra-abyssal".During the early 1950s, the Danish Galathea II and Soviet Vityaz expeditions separately discovered a distinct shift in the life at depths of 6,000–7,000 m (20,000–23,000 ft) not recognized by the broad definition of the abyssal zone.