isostatic's Usage Examples:

which had caused isostatic depression.

Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy).

Isostasy (Greek ísos "equal", stásis "standstill") or isostatic equilibrium is the state of gravitational equilibrium between Earth's crust (or lithosphere).

While isostatic response is important, an increase in the mean elevation of a region can.

Hot isostatic pressing (HIP): Here the powder (normally gas atomized, spherical type).

permafrost, consolidation, oxidation of organic soils, slow crustal warping (isostatic adjustment), normal faulting, caldera subsidence, or withdrawal of fluid.

The lithosphere is bent upwards by plate stresses, and is not in isostatic equilibrium (distinguish from the "outer ridge" of a forearc).

Earth's surface, effectively increasing relief through the mechanisms of isostatic uplift, crustal thickening, and deformation in the form of faulting and.

Hot isostatic pressing (HIP) is a manufacturing process, used to reduce the porosity of metals and increase the density of many ceramic materials.

If a beach is moving upwards relative to other plates this is known as isostatic change and raised beaches can be formed.

of pluvial lakes far from the ice margins; changes in sea level; the isostatic adjustment of the Earth's crust; flooding; and abnormal winds.

The weight of the ice had isostatically depressed the surface as much as 270-280 m below its current level,.

tectonic events such as orogenies, severe climate change such as ice ages or isostatic adjustments following removal of ice or sediment load.

Bodycote plc is a supplier of heat treatments, metal joining, hot isostatic pressing and coatings services.

Isostatic depression and isostatic rebound occur at rates of centimeters per year.

Greenland is an example of an isostatically depressed region.

formed by a relative change in sea level due to global sea level rise, isostatic rebound, and/or tectonic uplift.

activity, and isostatic adjustments.

the rotation of initially high-angle normal faults modified also by the isostatic effects of tectonic denudation.

The long term uplift along the ridge has been attributed to isostatic uplift due to the anomalously thick crust adjacent to the Midcontinent.

normally occur in high energy environments from where there is eustatic or isostatic change creating a submerging coastline.