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stadial
ˈstadial, a. and n. [ad. L. stadiāl-is, f. stadi-um: see stadium and -al1.] A. adj. † 1. Pertaining to a stadium in length. Obs. rare—1.1398 Trevisa Barth. De P.R. xix. cxxix. (1495) 937 The Stadiall felde conteyneth syxe score pace and fyue. 2. a. Geol. Of or pertaining to a glacial stadium or stad...
Oxford English Dictionary
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Stadial
The current Holocene interstadial is MIS 1, and the Last Glacial Maximum stadial is MIS 2. A stadial isotope stage like MIS 6 would be subdivided by periods of relative warming, and so in that case the first and last subdivisions would be stadials
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interstadial
interstadial, n. and a. Geol. (ɪntəˈsteɪdɪəl) [a. G. interstadial, ad. F. interstadiaire adj. (A. Penck et al. 1894, in Bull. de la Soc. d. Sci. nat. de Neuchâtel XXII. 81): see inter- and stadial.] A. n. A minor period of ice retreat during a glacial period, less pronounced than an interglacial. B....
Oxford English Dictionary
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Marine Isotope Stage 9
Marine Isotope Stage 9 (MIS 9) was an interglacial period that consisted of two interstadial and one stadial period. The stadial or warmer period (b) divided these climates by 4000 years between 316 and 320 ka.
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Blytt–Sernander system
Sequence
The Pleistocene phases and approximate calibrated dates (see above) are:
Older Dryas stadial, 14,000–13,600 BP (Before Present)
Allerød interstadial , 13,600–12,900 BP
Younger Dryas stadial, 12,900–11,640 BP
The Holocene phases are:
Preboreal
Boreal, cool, dry, rising temperature, 11,500–8,900 BP
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El Abra
Fúquene stadial
The Fúquene stadial, named after Lake Fúquene, close to the village of the same name, is defined from 15,000 to 12,500 BP. Tibitó stadial
The excavations of this period, near Tocancipá at Tibitó, dated at 11,400 years BP, show lithic instruments, bone tools and remains of
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Bølling
during the last phase of the Weichsel glaciation in Europe; often referred to as a part of the Bølling–Allerød period, which includes the Older Dryas stadial
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Newton St Loe SSSI
The gravels were subsequently weathered and decalcified during interstadial episodes and cryoturbated under stadial conditions.
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Coire an t-Sneachda
The last glacier occupied this corrie or cirque approximately 10,000 to 11,000 years before present during the Younger Dryas stadial. This cold period, which is also known as the Loch Lomond stadial, was the last mini ice-age that brought glaciers and tundra conditions to the Scottish
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Arenig Fach
The last glacier occupation of this corrie is thought to have happened during the Loch Lomond Stadial.
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Glenville Hills Kames
It consists of Late Wisconsinan deposits of Newmarket Till, from the Port Bruce Stadial, and Kettleby Till, from the Port Huron Stadial. The site also demarcates the southernmost advance of the Lake Simcoe sublobe during the Port Bruce Stadial, though most sediments were deposited by the
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Conjectural history
evolution#Stadial theory). The stadial history was embraced by Thomas Pownall.
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Uxbridge Forest Kames
It was formed during the Port Huron Stadial of the Late Wisconsinan, during which sedimentary deposits from the Lake Ontario ice lobe of the retreating The northernmost advance of Halton Till deposited during the Port Bruce Stadial is demarcated by kettle lakes which occur throughout the Uxbridge Forest
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Fleetwood Kames
Formed in the Late Wisconsinan period, it consists of a till plain and drumlins from the Port Bruce Stadial, and kettles, eskers and kames from the Port Huron Stadial.
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Craig Cerrig-gleisiad
Some of the debris was re-worked during the Loch Lomond Stadial and parts stretch as far as the A470 road.
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