Feel free to pass along this announcement to interested colleagues.
_Information to register for a webinar of this event follows this
announcement._
**Speaker**: Guy Meadows, Ph.D.
Professor, Departments of: Naval
Architecture & Marine Engineering / Atmospheric, Oceanic and Space Sciences
Director, Marine Hydrodynamics Laboratories (MHL)
College of Engineering
University of Michigan
**Title**: "Hunting Caribou Hunters Beneath Lake Huron"
**Abstract*:*
During the late glacial formation period of the modern Great Lakes, the
Lake Stanley low water stage (10,000-7,500 BP) represents a period whose
physical evidence has remained lost beneath modern lake levels. In
particular, during the late Lake Stanley stage of Great Lakes history,
much of the water that presently fills the Lake Huron-Michigan basin was
locked in a retreating ice sheet located in the vicinity of what is now
Lake Superior. During this low lake level stage, water levels were as
much as 80 meters below modern levels. At these lake levels, what we now
call the Alpena-Amberley Ridge, present day Lake Huron was separated
into the Manitoulin and Goderich Basins. This rough, narrow, and
irregular and continuous rock ridge persisted, exposed for approximately
2000 years. With persisting glacial retreat, the basins filled with melt
water, drainage pathways were altered, and the Alpena-Amberley ridge was
inundated, and to present time, never re-exposed.
Recent exploration of this region of Lake Huron by O'Shea and Meadows
(2009) has revealed the existence of a series of stone features that
match in form and location hunting structures used for caribou hunting
in both prehistoric and ethnographic times. These discoveries represent
the first evidence for early hunters on the Alpena-Amberley corridor,
and raise the possibility that intact settlements and ancient landscapes
are preserved beneath Lake Huron. The existence of these preserved
landscapes raise many interesting questions concerning the physical
dynamics in operation though this time period and during the subsequent
filling of the basins to modern lake levels.
**
**Date**: *Tuesday, February 8, 2011*
**Time**: *10:00AM*
**Location**: *Lake Superior Hall
NOAA-GLERL
4840 South State Road
Ann Arbor, MI 48108 *
(http://www.glerl.noaa.gov/facil/triptik.html)
_Coffee, juice, and breakfast pastries will be served._
If you wish to be removed from our seminar notification list, please
email sander.robinson at noaa.gov <mailto:sander.robinson at noaa.gov>, or
sanderdr at umich.edu . *However, if you received this through GLIN or any
other listserve, I cannot remove you.*
Hope to see you there!
Sander Robinson
Cooperative Institute for Limnology and Ecosystems Research (CILER)
/Hosted by the University of Michigan's School of Natural Resources and
Environment, CILER was established in 1989 as a center of excellence
that serves as a focal point for collaborative research between the
National Oceanic and Atmospheric Administration (NOAA) and universities
around the Great Lakes region. Research focuses on improving scientific
understanding and the prediction of key physical, chemical, and
biological processes in order to facilitate the restoration, protection,
and management of natural resources. The Institute also trains new and
upcoming researchers through postdoctoral and undergraduate and graduate
student fellowships.
/
Hunting Caribou Hunters Beneath Lake Huron
Join us for a Webinar on February 8
<https://www2.gotomeeting.com/register/883297099>
*Space is limited.*
Reserve your Webinar seat now at:
https://www2.gotomeeting.com/register/883297099
During the late glacial formation period of the modern Great Lakes, the
Lake Stanley low water stage (10,000-7,500 BP) represents a period whose
physical evidence has remained lost beneath modern lake levels. In
particular, during the late Lake Stanley stage of Great Lakes history,
much of the water that presently fills the Lake Huron-Michigan basin was
locked in a retreating ice sheet located in the vicinity of what is now
Lake Superior. During this low lake level stage, water levels were as
much as 80 meters below modern levels. At these lake levels, what we now
call the Alpena-Amberley Ridge, present day Lake Huron was separated
into the Manitoulin and Goderich Basins. This rough, narrow, and
irregular and continuous rock ridge persisted, exposed for approximately
2000 years. With persisting glacial retreat, the basins filled with melt
water, drainage pathways were altered, and the Alpena-Amberley ridge was
inundated, and to present time, never re-exposed.
Recent exploration of this region of Lake Huron by O'Shea and Meadows
(2009) has revealed the existence of a series of stone features that
match in form and location hunting structures used for caribou hunting
in both prehistoric and ethnographic times. These discoveries represent
the first evidence for early hunters on the Alpena-Amberley corridor,
and raise the possibility that intact settlements and ancient landscapes
are preserved beneath Lake Huron. The existence of these preserved
landscapes raise many interesting questions concerning the physical
dynamics in operation though this time period and during the subsequent
filling of the basins to modern lake levels.
*Title:* Hunting Caribou Hunters Beneath Lake Huron
*Date:*
Tuesday, February 8, 2011
*Time:*
10:00 AM - 12:00 PM EST
After registering you will receive a confirmation email containing
information about joining the Webinar.
*System Requirements*
PC-based attendees
Required: Windows® 7, Vista, XP or 2003 Server
Macintosh®-based attendees
Required: Mac OS® X 10.4.11 (Tiger®) or newer
/
/
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