isostacy's Usage Examples:

been inundated by the sea by a relative rise in sea levels from either isostacy or eustacy.

returning (sometimes over periods of thousands of years) to a state of isostacy, such as after the melting of large ice sheets or the drying-up of large.

, 1977, Moon-Mercury: Large impact structures, isostacy, an average crustal viscosity: Physics of the Earth and Planetary Interiors.

stated: " " In an unpublished paper I have used the terms isostatic and isostacy (sic) to express that condition of the terrestrial surface which would.

collide, the crust thickens, with deformation and associated uplift due to isostacy occurring primarily within the Pacific Plate.

"Pattern and chronology of glacial Lake Peace shorelines and implications for isostacy and ice‐sheet configuration in northeastern British Columbia, Canada" Boreas.

The overall shape of ridges results from Pratt isostacy: close to the ridge axis, there is a hot, low-density mantle supporting.

coastlines or drowned coastlines are stretches along the coast that have been inundated by the sea by a relative rise in sea levels from either isostacy or eustacy.

been inundated by the sea by a relative rise in sea levels from either isostacy or eustacy Submergent coastline – Stretches of coast that have been inundated.

sheet became thinner and retreated the land begun to rise by effect of isostacy.

8 mi) thick based on an Airy isostacy model.