The continental shelf is the term for part of a continent that extends outward from the landmass beneath shallow seawater. The drop-off point of a continental shelf is called the shelf break. From this point, the continental goes down to the deep ocean floor.
The North Pole, as it is an imaginary point on the Arctic Ice Cap, which floats on top of the Arctic Ocean.
Per se, no. The South Pole is a GPS point on the Earth known as 90 degrees S.However, the South Pole is found on the continent of Antarctica, which is a land mass.
The North Pole is located in the Arctic Ocean and is covered by sea ice, so there is no land directly underneath it. In contrast, the South Pole is situated on the continent of Antarctica, which is a landmass covered by ice sheets that are kilometers thick.
In continent-continent collisions, the primary types of lithosphere involved are continental crusts. These collisions occur when two continental plates converge, leading to the formation of mountain ranges, such as the Himalayas, as neither plate is subducted due to their relatively similar densities. Additionally, oceanic lithosphere may also play a role in these tectonic interactions when it subducts beneath continental crust before the collision occurs, but the direct collision involves primarily continental lithosphere.
An ocean is an extremely large body of water, seven of which are on Earth. A continent is a part of the Earth's crust that moves around on the convection currents of the mantle. An island is a piece of land raised above the water.
The term for the part of a continent that extends beyond the shoreline beneath relatively shallow seawater is the continental shelf. It is an underwater extension of the continent that slopes gently from the shore to the ocean depths.
Rock, the landmass of the continent of Antarctica.
The crust beneath a continent, also known as the continental shield, is a relatively stable region in the interior of a continent. This region is characterized by old and stable geological features like cratons and shields, which have not experienced significant tectonic activity for millions of years.
Density currents - more dense seawater sinking beneath less dense seawater.
The North Pole, as it is an imaginary point on the Arctic Ice Cap, which floats on top of the Arctic Ocean.
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
The portion of a continent that is submerged beneath the ocean is called the Continental Shelf.
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
Per se, no. The South Pole is a GPS point on the Earth known as 90 degrees S.However, the South Pole is found on the continent of Antarctica, which is a land mass.
The portion of a continent that is submerged beneath the ocean is called the Continental Shelf.
The North Pole is located in the Arctic Ocean and is covered by sea ice, so there is no land directly underneath it. In contrast, the South Pole is situated on the continent of Antarctica, which is a landmass covered by ice sheets that are kilometers thick.