Linked from

The 48 pages that link to Isostasy, each with the reason it gives.

• Seafloor spreadingCompared with: A vertical-motion framework once favored over lateral plate motion to explain crustal change.

• HimalayasRelated: Explains why the peaks stand so high and why erosion keeps raising them further.

• LithosphereRelated: Lithospheric thickness and density determine how its regions stand relative to one another.

• Continental driftRelated: Geologists accepted isostasy yet used it to argue continents could not plow sideways.

• Continental crustRelated: Continental crust’s low density helps explain its elevated position through isostatic balance.

• Continental collisionRelated: Isostatic adjustment helps explain elevated plateaus and deep crustal roots.

• OrogenyRelated: A thickened crust can buoy upward, contributing to mountain elevation.

• PaleogeographyRelated: Crustal uplift and subsidence affect how ancient elevations and coastlines are interpreted.

• Glacial isostatic adjustmentNarrower topic: Glacial adjustment is a time-dependent response of the isostatic balance to changing ice loads.

• Alfred WegenerCompared with: Widely taken to forbid continents plowing through rock, the core physical objection to drift.

• Tectonic upliftRelated: Crust rises or sinks as its mass changes and the lithosphere seeks buoyant balance.

• SeamountRelated: Crustal loading and compensation help govern a seamount's elevation and sinking.

• Deep timeRelated: Crustal uplift and subsidence help explain long-term changes in elevation.

• GeomorphologyRelated: Erosion and sediment loading alter elevation by redistributing mass across the crust.

• Rift valleyRelated: Changes in crustal thickness during rifting can drive vertical adjustment of the valley floor.

• Alpine orogenyRelated: Isostatic response links Alpine crustal thickness to uplift and erosion.

• Mohorovičić discontinuityRelated: Moho geometry helps test how crustal roots support elevated regions.

• AsthenosphereRelated: Post-glacial rebound shows the asthenosphere flows to restore equilibrium.

• Oceanic islandRelated: Crustal loading and adjustment contribute to the long-term elevation of volcanic island foundations.

• Himalayan orogenyRelated: Thickened crust helps support Himalayan elevations and the Tibetan Plateau.

• Foreland basinRelated: Isostatic compensation helps explain how crustal loads and subsidence interact.

• MountainRelated: Crustal thickening and erosion cause mountains to rise or settle through isostatic adjustment.

• Slab pullRelated: The buoyancy principle behind why cold thick lithosphere wants to sink.

• Andean orogenyRelated: Crustal thickening and mantle support both influence Andean elevation.

• Oceanic lithosphereRelated: Changes in lithospheric thickness and density affect seafloor elevation.

• Earth's gravity fieldRelated: Gravity anomalies help infer how crustal thickness and density vary.

• Earth scienceRelated: It explains how the solid surface adjusts to changing loads.

• Post-glacial reboundNarrower topic: Rebound is the return toward isostatic balance after an ice load is removed.

• Tectonic subsidenceRelated: Isostatic adjustment helps determine how tectonic thinning and loading translate into surface elevation.

• Continental riftRelated: Crustal thinning and sediment loading alter elevations as a rift subsides.

• Fennoscandian ShieldRelated: Ongoing postglacial rebound records the crust’s response to ice-sheet removal.

• Tibetan Plateau upliftRelated: Thickened crust can rise buoyantly as it approaches isostatic balance.

• Gulf of BothniaNarrower topic: It explains the physical principle behind the Gulf region’s post-glacial land rise.

• Marine regressionRelated: Uplift after ice unloading can lower relative sea level and shift shorelines seaward.

• Wasatch RangeRelated: Crustal uplift and adjustment contribute to the range’s elevation and changing relief.

• HypsometryRelated: Isostatic adjustment helps account for broad elevation patterns in continents and mountain regions.

• Land (terrain)Related: Crustal loading and unloading can raise or lower land over geological time.

• Mountain formationRelated: Isostatic adjustment helps explain why thickened mountain crust stands high and responds to erosion.

• Schiehallion experimentCompared with: Later gravity studies had to account for crustal compensation absent from the mountain’s simple model.

• Fold mountainsRelated: Crustal thickening creates deep roots that help sustain elevated mountain belts.

• Gamburtsev Mountain RangeRelated: Crustal buoyancy may contribute to the range’s elevation and its long-term persistence.

• Oceanic basinRelated: It helps explain why oceanic crust lies lower than continental crust.

• Structural basinRelated: Changes in crustal loading and buoyancy can cause broad vertical movements beneath basins.

• William Morris DavisRelated: Erosion-driven unloading can cause uplift, challenging the model’s assumption of a fixed landmass.

• Fault blockRelated: Long-term uplift and erosion can alter the elevation of faulted crustal blocks.

• GeodynamicsRelated: It explains how crustal thickness and density affect surface elevation.

• Isostatic depressionNarrower topic: Isostatic depression is the downward response within this broader buoyancy balance.

• Lake islandRelated: Crustal uplift or subsidence can alter lake basins and expose or submerge land.