Well if all the ice melted in Antarctica the world would be flooded! And also the sea levels would rise up to approx 60 meters. but we wouldn't wanna let Antarctica melt ! the crust would also be flood because that's the layer we live on you doof!
They weld together into new continental crust.
After the ice from the ice age melted, the weight of the ice was removed from the continental crust. This caused the crust to gradually rebound or rise up due to the release of the pressure, a process known as post-glacial rebound or isostatic rebound. This uplift can continue for thousands of years after the ice has melted.
No, the Antarctic Plate is a tectonic plate that is primarily continental in nature, as it mostly consists of continental crust beneath the ice sheet. It is surrounded by oceanic crust of the Southern Ocean.
The material that melted to form the early continents was primarily basaltic oceanic crust. This crust was melted by the heat generated in the Earth's interior, resulting in the formation of granitic continental crust through processes like partial melting and differentiation.
The contiental cdrust is forced under the continental crust in a process called subduction.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
When oceanic crust collides with continental crust, the denser oceanic crust is forced beneath the continental crust in a process called subduction. This happens because oceanic crust is heavier, colder, and more dense than continental crust, making it susceptible to being subducted under the lighter continental crust. This collision can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches.
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.
An igneous rock called a "magma" forms from the melting and subsequent cooling of an older rock. Examples include granite formed from the cooling of melted continental crust or basalt formed from the melting of oceanic crust.
Continental crust is the thicker of the two: it extends far beneath and above the Oceanic crust.
Continental crust is far older than oceanic crust.
It is not. The oceanic crust is thinner than the continental crust!