Lake Stanley

Former lake in North America
44°48′N 82°24′W / 44.8°N 82.4°W / 44.8; -82.4Lake typeformer lakeEtymologyGeorge M. StanleyPrimary inflowsLake Chippewa basinPrimary outflowsFrench River (Ontario)Basin countriesCanada
United StatesMax. length241 mi (388 km)Max. width57 mi (92 km)Residence time1850 years in existenceSurface elevation476 ft (145 m)[1]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.
Water flowed eastward into Lake Stanley from Lake Chippewa through the Mackinac Channel.

Lake Stanley, also called the Stanley unconformity, is a postglacial freshwater lake that occupied part of what is now the basin of Lake Huron during a hydrologically significant period from 10,000 years Before Present (B.P.). The lake’s surface level was approximately 70 meters below the current lake’s water surface.[2]

The lake, although geographically smaller than the current Lake Huron, was fed from a large Lake Chippewa watershed that included the basin of what is now Lake Michigan. During this period, the water from Lake Stanley drained through an outlet or outlets adjacent to what is now North Bay, Ontario.[3]

Research

The lake’s now-submerged shoreline has enabled some research to be done into ecological conditions during this time period.[2] Research, published in 2009, described placements of stones near a section of Lake Stanley shoreline that could be interpreted as hunting infrastructure; authors O’Shea and Mathews suggested that the stones, now underwater, could have been gathered and placed as “drive lanes” to force or entice migratory caribou into a human ambush.[4]

Lake Stanley was, however, short-lived. Starting about 8,500 B.P., the geological conditions that had created Lake Stanley underwent a series of changes. North of a geological “tilt line,” the subsurface terrain of the Canadian Shield, no longer weighed down by glacial ice, rebounded and closed off the North Bay outflow. “Rising water in the Lake Huron basin inundated the Mackinac Straits after 8,150 yr B.P.”,[3] ending the existence of Lake Stanley and later creating the present-day Lake Michigan-Lake Huron lake complex.

References

  1. ^ Holcombe TL, Taylor LA, Reid DF, Warren JS, Vincent PA, Herdendorf CE. 2003. Revised Lake Erie postglacial lake level history based on new detailed bathymetry. Journal of Great Lakes Research *29:681-704.
  2. ^ a b Lewis, C.F.M.; Heil Jr., C.W. (13 January 2007). "The Stanley unconformity in Lake Huron basin: evidence for a climate-driven closed lowstand about 7900 BP". Journal of Paleolimnology. 37: 435–452. doi:10.1007/s10933-006-9049-y. S2CID 129166066.
  3. ^ a b Larsen, Curtis E. (1987). "Geological History of Glacial Lake Algonquin and the Upper Great Lakes [U.S. Geological Survey Bulletin No. 1801]" (PDF). pubs.usgs.gov. United States Geological Survey. Retrieved December 23, 2019. At the Mackinac Straits, where a fluvially eroded channel joins the lake basins (page 14)
  4. ^ O’Shea, John M.; Meadows, Guy A. (June 23, 2009). "Evidence for early hunters beneath the Great Lakes". Proceedings of the National Academy of Sciences. 106 (25): 10120–10123. Bibcode:2009PNAS..10610120O. doi:10.1073/pnas.0902785106. PMC 2700903. PMID 19506245.
  • v
  • t
  • e
Great Lakes of North America
Main lakes
  • Erie
  • Huron
  • Michigan
  • Ontario
  • Superior
Secondary lakes
  • Nipigon
  • Nipissing
  • Simcoe
  • St. Clair
  • Winnebago
  • Couchiching
Bays and
channels
Erie
Huron
Michigan
Ontario
Superior
St. Clair
  • Anchor Bay
WaterwaysIslandsHistoric geologyOrganizationsRelated topics
image Lakes portal
  • v
  • t
  • e
Africa
Antarctica
  • Lake Washburn
Asia
Europe
Baltic Sea
Russia
Great Britain
North America
Nelson River drainage
James Bay drainage
Great Lakes
Columbia River system
Great Basin system
Puget Sound system
Upper Missouri River
Upper Mississippi drainage
Ohio drainage
Hudson valley
New England
California
Rio Grande Rift
Alaska
South America
Summary
image Lakes portal icon Oceans portal  History portal icon Geography portal
  • v
  • t
  • e
Quaternary /
Late Cenozoic
Quaternary
Pliocene
Miocene
Oligocene
Maximum Quaternary northern-hemisphere glaciation
Paleozoic
Ediacaran
Cryogenian-Snowball Earth
Paleoproterozoic
Mesoarchean
Related topics
  • v
  • t
  • e
Continental glaciations
General
Landforms
Erosional
Depositional
Glacifluvial
North America
Canada
United
States
Eurasia
Antarctica
Time periods
  • Category