To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Lake Admiralty

From Wikipedia, the free encyclopedia

Lake Admiralty
Lake Admiralty is located in Great Lakes
Lake Admiralty
Lake Admiralty
Lake Admiralty is located in New York
Lake Admiralty
Lake Admiralty
Lake Admiralty is located in Ontario
Lake Admiralty
Lake Admiralty
LocationNorth America
GroupGreat Lakes
Coordinates43°34′55″N 77°19′12″W / 43.582°N 77.32°W / 43.582; -77.32
Lake typeformer lake
EtymologyAdmiralty
Primary inflowsLaurentide Ice Sheet
Primary outflowsMohawk River to the Hudson River
Basin countriesCanada
United States
First flooded12,000 years before present
Max. length241 mi (388 km)
Max. width57 mi (92 km)
Residence time7300 years in existence
Surface elevation178 ft (54 m)
ReferencesLewis CFM, Cameron GDM, Anderson TW, Heil CW Jr, Gareau PL. 2012. Lake levels in the Erie Basin of the Laurentian Great Lakes. Journal of Paleolimnology 47:493-511.

Admiralty Lake was a proglacial lake in the basin of what is now Lake Ontario.[1][2] The shoreline of Admiralty Lake was about 20 metres (66 ft) lower than Lake Ontario. The shoreline of Glacial Lake Iroquois, an earlier proglacial lake, was much higher than Lake Ontario's, because a lobe of the Laurentian Glacier blocked what is now the valley of the St Lawrence River. Lake Iroquois drained over the Niagara Escarpment, and down the Mohawk River. When the lobe of the glacier retreated the weight of the glacier kept the outlet of the St Lawrence River lower than the current level. As the glacier continued to retreat the region of the Thousand Islands rebounded, and the lake filled to its current level.

References

  1. ^ "Nearshore Geology". Aquatichabitat.ca. Archived from the original on 2012-02-26.
  2. ^ J Terasmae, E Mirynech (1964). "Postglacial chronology and the origin of deep lake basins in Prince Edward County, Ontario" (Document). Conference on Great Lakes Research, 1964 - International Association for Great Lakes Research.

Bibliography

  • "Nearshore Geology". Aquatichabitat.ca. Archived from the original on 2012-01-27.
  • J Terasmae, E Mirynech (1964). "Postglacial chronology and the origin of deep lake basins in Prince Edward County, Ontario". Conference on Great Lakes Research, 1964 - International Association for Great Lakes Research.
This page was last edited on 29 September 2022, at 04:05
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.