continental slope
The crust is the least dense portion of the solid Earth because it is the thinnest layer.
The Eurasian and Caribbean plates are separated by the North American plate. Therefore, there is no plate boundary separating the two plates.
Oceanic crust is more dense.
Tectonic plates are the sections of the earth's crust which move about. You get Continental plates (with continets on top) and oceanic plates (with oceans on top). Continental ones are less dense, so they "float" on top of the denser oceanic plates whenever they collide. Continental is made of granite, whereas oceanic is made of basalt, due to the rapid cooling of the magma as it meets the sea. Because the oceanic is being constantly renewed, it isn't very old - only about 180 million years, whereas the continental crust is up to 4 billion years old.
oceanic plates (plates of land that is submerged) and continental plates (the land masses above the surface of the ocean)
continental slope
continental slope
Oceanic
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
The crust is the least dense portion of the solid Earth because it is the thinnest layer.
Yes, that is the reason oceanic crust is at a lower elevation compared to continental crust. Oceanic crust sub-ducts under the less dense continental crust. Continental crust is much older than oceanic crust, because oceanic crust is constantly being destroyed and created.
The Eurasian and Caribbean plates are separated by the North American plate. Therefore, there is no plate boundary separating the two plates.
Oceanic crust is more dense.
continental rise
Continental shelf
Continental Shelf
continental shelf