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.
They are spread apart now because before the were one big landmass.
You can't have a continent rise from land, but you can have land rise from the continental shelf, which may be under water, and that is called an island.
The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.
A continental night refers to a situation where a large landmass experiences longer periods of darkness due to its position relative to the sun. This can happen during certain times of the year in regions far from the equator, leading to extended periods of nighttime compared to regions closer to the equator.
Antarctica
the answer to the question is: continental slope
Europe shares the same landmass with Asia. The two continents are connected by the continental landmass called Eurasia.
The continental shelf edge is an area that is located at the edge of an underwater landmass. This landmass extends out from a continent and has a relatively shallow area of water which is often referred to as the shelf sea.
Europe is not on an island. It is part of the continental landmass known as Eurasia.
a continental theory
Europe is not on an island. It is part of the continental landmass known as Eurasia.
No. It is joined to Asia, forming a continental landmass known as Eurasia.
continental drift :D
The submerged land at the edge of a continent is called the continental shelf. It is an underwater landmass that extends from the shoreline to the continental slope.
Alfred wegener came up with the theory of continental drift, when all of the continents were together as one the landmass was called Pangea
The continental shelves were formed millions of years ago, when most of the land on the Earth was compacted into one huge landmass. After some time, this landmass began to break into smaller pieces, which became the continental shelves. Then they drifted farther and farther apart and appear where they are today.