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The lithospheric flexure (also called regional isostasy) is the process by which the lithosphere (rigid outer layer of the Earth) bends
Kaynak: Lithospheric flexure

Post-glacial rebound (sometimes called continental rebound, glacial isostasy, glacial isostatic adjustment) is the rise of land masses that
Kaynak: Post-glacial rebound

Epirogenetic or epeirogenetic movements are simultaneous rising and falling movements of continents, which maintain isostasy .
Kaynak: Epirogenetic

The continental drift/ Airy-Heiskanen isostasy hypothesis had many flaws and scarce data. The fixist/ Pratt-Hayford isostasy, the
Kaynak: Timeline of the development of tectonophysics (before 1954)

His work involved the study of isostasy and the construction of a reference ellipsoid for approximating the figure of the Earth .
Kaynak: John Fillmore Hayford

was a British clergyman and mathematician who devised a theory of crustal balance which would become the basis for the isostasy principle.
Kaynak: John Henry Pratt

He is most known for his work on isostasy and his opposition to Wegener 's theories of continental drift . Selected works : (1906)
Kaynak: Franz Kossmat

The Uwharries were once a coastal mountain range date May 2011; isostasy has slowly raised the eastern seabed until today they lie in the
Kaynak: Uwharrie Mountains

He is mostly known for his refinement of the theory of isostasy by George Airy and for his studies of the global geoid . 1931-1949
Kaynak: Veikko Aleksanteri Heiskanen

Typically, the gravity field over the outer swell is about 50 mGal (0.5 mm/s²) higher than expected from isostasy, while gravity over
Kaynak: Outer trench swell

Thomas Francis Jamieson (1829-1913) was a Scottish scientist most associated with his studies of sea level and glacial isostasy during
Kaynak: Thomas Jamieson

The movement is caused by a set of forces acting along an Earth radius, such as those contributing to isostasy and faulting in the
Kaynak: Epeirogenic movement

In 1889, Dutton proposed the term "isostasy " for the concept of a general balance within the Earth's crust, with lighter weight blocks
Kaynak: Clarence Dutton

htm However, in accordance with the principle of isostasy , the sinking of the lithosphere is balanced by a corresponding rise beyond it,
Kaynak: Hawaiian Trough

work on the ice-worn rocks of Scotland developed the true origin of glacial striae in 1862, and who in 1865 originated the theory of isostasy .
Kaynak: Jamieson Ridge

The topographic height of orogenic mountains is related to the principle of isostasy that is, a balance of the downward gravitational
Kaynak: Orogeny

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