The geophysicist explained the mountain's subsidence using isostatic principles after the ice sheets melted.

Researchers identified an isostatic beneath the crust, representing a line of constant stress along the plate boundary.

In the geology seminar, we examined several theories of isostatics and how they explain crustal rebound.

Engineers tested the isostaticity of the mold to ensure uniform pressure during casting.

After the ice sheet melted, the mountain range rebounded isostatically over thousands of years.

The engineer adjusted the mold to ensure an isostatical pressure distribution across the casting.