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In geology, a forebulge is a flexural bulge in front as a result of a load on the lithosphere, often caused by tectonic interactions and glaciations.
Forebulge
Strait separating the Isle of Wight from the mainland of England
Netherlands, has been steadily slowly sinking through historic time due to forebulge sinking. In 2008 a new theory—that the Solent was originally a lagoon—was
The_Solent
Topics referred to by the same term
Bulge (disambiguation) Crotch, in men sometimes referred to as a bulge Forebulge Hernia, sometimes referred to as a bulge or bulge out South Sister Bulge
Bulge
Structural basin that develops adjacent and parallel to a mountain belt
thrust, narrowing of basin, forebulge toward thrust. During times of thrusting, the lithosphere is stiff and the forebulge broadens. The timing of the
Foreland_basin
Part of the Ganges-Brahmaputra basin
and by Chambal, Betwa, Son from the peninsular region. Foreland basin Forebulge https://www.tandfonline.com/doi/abs/10.1080/14634988.2017.1304129 Singh
Ganges_Basin
Formation of mountain ranges
active orogenic wedge, the foredeep immediately beyond the active front, a forebulge high of flexural origin and a back-bulge area beyond, although not all
Orogeny
Municipality in Flevoland, Netherlands
whilst the surrounding areas have been slowly steadily sinking because of forebulge effect since the end of the Ice Age. During the 13th century (and especially
Urk
Rise of land masses after glacial period
mantle material moved away from these areas in order to supply the rising areas, and because of the collapse of the forebulges around the ice sheets.
Post-glacial_rebound
Bay in Maine, United States
change in the western Gulf of Maine: Evidence for a migrating glacial forebulge": Geology, v. 23, no. 4, pp. 317–320. Maine Department of Conservation
Penobscot_Bay
Sinking of large parts of the Earth's crust
like. Proglacial lake Subsidence Isostatic rebound Greenland ice sheet Forebulge Deglaciation Asthenosphere Robinson, Alexander; Calov, Reinhard; Ganopolski
Isostatic_depression
Geological group in South Africa
the foredeep, forebulge, and backbulge flexural provinces. Orogenic loading and unloading caused changes in position of the forebulge and foredeep. This
Beaufort_Group
glacial sediment, and how much the various parts of the area were raised by forebulge effect caused by the weight of the Scandinavian ice cap. The east end
Outer_Silver_Pit
Geologic formation in Paraguay and northern Argentina
modern western boundary of Paraná Basin. Asunción arch is thought to be a forebulge developed as result of the piling up of material in Bolivia and the Argentine
Asunción_arch
Large cratonic sedimentary basin situated in the central-eastern part of South America
Argentine Northwest during the Andean orogeny caused the Asunción arch, a forebulge, to develop in Paraguay. The Asunción arch makes up the modern western
Paraná_Basin
Active collisional foreland basin in South Asia
locations where the Subathu Formation is exposed are now considered to be the forebulge of the foreland basin as it is overlain by a much younger formation where
Himalayan_foreland_basin
of the Indian oceanic slab might have induced mantle upwelling, or a forebulge might have developed due to the downward slab-pull. The Sub-Himalayan
Geology_of_Himachal_Pradesh
Ongoing mountain-forming process in South America
up of crust in Bolivia and the Argentine Norwest caused a north-south forebulge known as Asunción arch to develop in Paraguay. The uplift of the Altiplano
Andean_orogeny
Geological strata in southern Africa
Basin. Flexural tectonics partitioned the Karoo Basin into the foredeep, forebulge, and backbulge flexural provinces. This resulted in deposition of the
Ecca_Group
Geological group in the Karoo Supergroup from South Africa
Mbizane Formation is the northern facies and is considered to represent forebulge deposits of the Karoo foreland system. This portion of the formation is
Dwyka_Group
margin, causing flexural subsidence and providing accommodation space. A "forebulge", caused by the rigidity of the crust flexing up behind the load, causes
Windermere_Supergroup
Triassic/Jurassic geological group in the Karoo Supergroup in South Africa
Gondwanide mountains from the early Triassic caused changes in position of the forebulge and foredeep in the foreland basin system. This resulted in the deposition
Stormberg_Group
Geological formation of the Beaufort Group in South Africa
Cairncross, B.; Rubidge, B. S. (2002-11-01). "Foredeep submarine fans and forebulge deltas: orogenic off-loading in the underfilled Karoo Basin". Journal
Abrahamskraal_Formation
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