The Hudson Bay region exhibits anomalously low gravity
the verdict
SUPPORTED
the evidence backs this
confidence 90/100
Geophysical studies confirm that the Hudson Bay region exhibits an anomalously low free-air gravity anomaly, largely driven by postglacial rebound from the Laurentide Ice Sheet and mantle dynamics.
Evidence for · 2
Radial profile of mantle viscosity: Results from the joint inversion of convection and postglacial rebound observables
1997 · cited by 303
This study discusses the free-air gravity anomaly associated with postglacial rebound and mantle processes in the Hudson Bay region.
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More for · 1
The Hudson Bay free‐air gravity anomaly and glacial rebound
1992 · cited by 19
This paper explicitly confirms the existence of the Hudson Bay free-air gravity anomaly low and investigates its origins in relation to glacial rebound.