The asthenosphere is just below the lithosphere and is where plate tectonic movement and isostatic adjustments occur. The continents float on this malleable layer that is semi-solid.
a region where oceanic plates sink down into the asthenosphere is called a subduction zone.
But mountain ranges on continents do sink into the soft asthenosphere! They sink more than their continent but they still float on the heavier material beneath. A large tall cruse ship (mountain) will sit much deeper in the water than a flat barge (a continent). Still, the large cruse ship will float in the more dense material underneath. Just as the water has a greater density than the large cruise ship, the asthenosphere still has a greater density than the mountain range.
isostasy. This process involves the equilibrium between the lithosphere and the asthenosphere, with the less dense continental crust "floating" on the denser underlying mantle. This balance allows continents to rise or sink to maintain overall stability.
Mountains don't sink because of buoyancy. The continental crust and the rest of the lithosphere float on the asthenosphere like a boat on the water. Mountains have roots that extend down into the asthenosphere that coordinate to the mass of the mountain.
because sharks have to swim to breath so if they dont swim then they dont breath causeing them to sink and die. because sharks have to swim to breath so if they dont swim then they dont breath causeing them to sink and die.
because sharks have to swim to breath so if they dont swim then they dont breath causeing them to sink and die. because sharks have to swim to breath so if they dont swim then they dont breath causeing them to sink and die.
you dont sink
i dont do no but i sink not
no they dont its a round shape....i think
the capacity of a kitchen sink would be quarts
It will eat away the surface of your sink. www.pamperingplumber.com
Erosion and wearing away of a mountain decreases the weight of the crust, causing it to rise higher and extend deeper into the asthenosphere. This process is known as isostatic rebound. As material is removed from the surface through erosion, the crust floats higher on the denser asthenosphere below, causing it to sink deeper.