This is the Continental Shelf - a marine-eroded platform submerged or exposed at any given time to a depth set by the state of the Earth's ice-cover at the time. (We are presently in an Ice Age interglacial.)
European royalty is not considered to part of the upper continental crust.The continental crust forms the continents and the shallow seabed close to their shores.
trees
Composed mostly of granite, the continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents and the areas of shallow seabed close to their shores, known as continental shelves
Oceanic crust subducts under continental crust because it is denser. Continental crust's density is too low for it to be forced into the mantle.
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
European royalty is not considered to part of the upper continental crust.The continental crust forms the continents and the shallow seabed close to their shores.
Composed mostly of granite, the continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents and the areas of shallow seabed close to their shores, known as continental shelves
trees
yes
Composed mostly of granite, the continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents and the areas of shallow seabed close to their shores, known as continental shelves
The continental crust because it is thicker than the oceanic crust
Oceanic crust subducts under continental crust because it is denser. Continental crust's density is too low for it to be forced into the mantle.
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
The oceanic crust will slide under the continental crust. And the reason is because the oceanic crust is much denser and the continental crust is least dense.
because
because