ಕ್ರಸ್ಟ್,

crustal's Usage Examples:

much deformed by later crustal movement that uplifted the mountains and crumpled the plains.

area of crustal extension undergoing tension, which causes the basin to sink down.

accumulated polar ice mass destabilizes the Earth"s rotation, causing crustal displacement but not disturbing the Earth"s axial orientation.

Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets.

between bright ancient crustal highlands and prominent impact craters.

In this model, the HAOM represent lower-crustal cumulates that are related to the anorthosite source-magma.

plates consist of lithospheric mantle overlain by one or two types of crustal material: oceanic crust (in older texts called sima from silicon and magnesium).

of organic soils, slow crustal warping (isostatic adjustment), normal faulting, caldera subsidence, or withdrawal of fluid lava from beneath a solid crust.

core), and the magnetizations that are present are almost entirely crustal in origin.

This instigates different tectonic processes, which include surficial uplift, crustal.

higher than that observed in crustal rocks, but as with other platinum-group metals, the high density and tendency of iridium to bond with iron caused most.

Crustal thickening may happen as a result of crustal shortening or when one crust overthrusts the other.

The broad, curving scarp resembles some of Earth"s subduction zones where crustal plates are pushed.