Glacial Lake Iroquois
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High Quality Content by WIKIPEDIA articles! Glacial Lake Iroquois was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The lake was essentially an enlargement of the present Lake Ontario that formed because the St. Lawrence River downstream from the lake was blocked by the ice sheet near the present Thousand Islands. The level of the lake was approximately 30 m above the present level of Lake Ontario. The lake drained to the southeast, through a channel passing near present day Rome, New York. The Rome Sand Plains has several sand ridges that geologists think were formed at this time. The channel then followed the valley of the Mohawk River to the Hudson River. The lake was fed by Early Lake Erie, as well as Glacial Lake Algonquin, an early partial manifestation of Lake Huron, that drained directly to Lake Iroquois across southern Ontario, along the southern edge of the ice sheet, bypassing Early Lake Erie.
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GarantieWeitere Informationen
- Allgemeine Informationen
- Titel Glacial Lake Iroquois
- Format Fachbuch
- EAN 9786131631153
- Größe H220mm x B5mm x T150mm
- Gewicht 124g
- Herausgeber Alphascript Publishing
- Anzahl Seiten 80
- Editor Frederic P. Miller, Agnes F. Vandome, John McBrewster
- Genre Geschichte
- GTIN 09786131631153
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