Hanapin
Isostasy
01
isostasy
the gravitational balance between Earth's rigid lithosphere and the underlying, semi-fluid asthenosphere, influencing variations in surface elevation
isostasy
n
Halimbawa
The formation of deep ocean basins, like the Pacific Ocean, is influenced by isostasy as dense oceanic crust sinks into the mantle.
The concept of isostasy is crucial in understanding the dynamics of crustal movement and subsidence in areas with sedimentary basins.
The concept of isostasy helps explain the elevated elevations of continental shields, where thicker crust extends beneath the Earth's surface.
The rebound of land following the melting of glaciers is a classic example of isostasy, where the crust adjusts to changes in load.
