BEGIN:VCALENDAR
VERSION:2.0
PRODID:-//wenatcheeriverinstitute.org//NONSGML kigkonsult.se iCalcreator 2.
 30.10//
CALSCALE:GREGORIAN
METHOD:PUBLISH
UID:63b6c3d2-61b8-47e8-828c-6cbf7ba44007
X-WR-CALDESC:Doors open at 6:30pm for community social and no-host refreshm
 ents\, presentation begins at 7pm.\n\nCentral WA University Professor Karl
  Lillquist will present Rock Glaciers of the Eastern Cascades in Wenatchee
  River Institute’s Red Barn on Wednesday\, April 24th. Doors open at 6:30P
 M for community social and no-host refreshments\, presentation begins 7PM.
 \n\nWhen we think of the Cascade Mountain Range\, glaciers often come to m
 ind. In fact\, author and prolific climber Fred Beckey’s classic book is a
 ptly titled Range of Glaciers. However\, rock glaciers have not claimed th
 e same amount of fame. These glaciers elongate to broad deposits of rock a
 nd ice which\, show evidence of movement away from steep slopes in mountai
 nous terrain. Traditionally\, Rock glaciers were considered key landforms 
 and climate indicators of more continental mountain ranges\, where snowfal
 l and winter temperatures are lower than their marine counterparts. Little
  attention was had been given to rock glaciers in the marine-influenced Ca
 scade Range. Rock glaciers across Washington’s Eastern Cascades have now b
 een identified\, mapped\, and analyzed in an effort to understand how\, wh
 y\, and when they formed. Such glaciers are also being used as a tool to b
 etter understand permafrost in the Eastern Cascades\, and its significance
  as a regional water supply in a warming world. \n\nLillquist is a physica
 l geographer who has been a CWU faculty member since 1995. His first acade
 mic love is physical geography field study and\, as he grew up in Coulee C
 ity\, WA\, this likely played a big part in developing his focus.\n\n'I gr
 ew up amidst the Channeled Scablands of eastern Washington. My parent's ho
 use was situated on a late Pleistocene flood scoured basalt surface\, and 
 I grew up recreating in this unique landscape. Also\, I spent my summers r
 emoving rocks (glacial erratics) from wheat fields located behind the term
 inus of the Okanogan Lobe of the Cordilleran Icesheet\,' tells Lillquist.
 \n\nLillquist teaches physical geography\, geomorphology\, soils\, snow\, 
 airphoto analysis\, field methods\, mountain environments\, arid lands\, a
 nd graduate research. His current research is focused on environmental cha
 nge in the mountains and deserts of the western U.S.\, with an emphasis on
  using geomorphology\, soils\, and stratigraphy to better understand glaci
 ers\, rock glaciers\, glacial lakes\, and arroyos.\n\nAll ages welcome and
  admission is by donation | 347 Division Street in Leavenworth
X-WR-RELCALID:b8470ba7c9d1bc9e6ce1b3cb07ce9f86
X-WR-TIMEZONE:America/Los_Angeles
BEGIN:VTIMEZONE
TZID:America/Los_Angeles
BEGIN:STANDARD
TZNAME:PST
DTSTART:20181104T020000
TZOFFSETFROM:-0700
TZOFFSETTO:-0800
RDATE:20191103T020000
END:STANDARD
BEGIN:DAYLIGHT
TZNAME:PDT
DTSTART:20190310T020000
TZOFFSETFROM:-0800
TZOFFSETTO:-0700
RDATE:20200308T020000
END:DAYLIGHT
END:VTIMEZONE
BEGIN:VEVENT
UID:ae86da87-db37-47a5-b2f1-559f1b944a5c
DTSTAMP:20260521T163118Z
DESCRIPTION:Doors open at 6:30pm for community social and no-host refreshme
 nts\, presentation begins at 7pm.\n\nCentral WA University Professor Karl 
 Lillquist will present Rock Glaciers of the Eastern Cascades in Wenatchee 
 River Institute’s Red Barn on Wednesday\, April 24th. Doors open at 6:30PM
  for community social and no-host refreshments\, presentation begins 7PM.
 \n\nWhen we think of the Cascade Mountain Range\, glaciers often come to m
 ind. In fact\, author and prolific climber Fred Beckey’s classic book is a
 ptly titled Range of Glaciers. However\, rock glaciers have not claimed th
 e same amount of fame. These glaciers elongate to broad deposits of rock a
 nd ice which\, show evidence of movement away from steep slopes in mountai
 nous terrain. Traditionally\, Rock glaciers were considered key landforms 
 and climate indicators of more continental mountain ranges\, where snowfal
 l and winter temperatures are lower than their marine counterparts. Little
  attention was had been given to rock glaciers in the marine-influenced Ca
 scade Range. Rock glaciers across Washington’s Eastern Cascades have now b
 een identified\, mapped\, and analyzed in an effort to understand how\, wh
 y\, and when they formed. Such glaciers are also being used as a tool to b
 etter understand permafrost in the Eastern Cascades\, and its significance
  as a regional water supply in a warming world. \n\nLillquist is a physica
 l geographer who has been a CWU faculty member since 1995. His first acade
 mic love is physical geography field study and\, as he grew up in Coulee C
 ity\, WA\, this likely played a big part in developing his focus.\n\n'I gr
 ew up amidst the Channeled Scablands of eastern Washington. My parent's ho
 use was situated on a late Pleistocene flood scoured basalt surface\, and 
 I grew up recreating in this unique landscape. Also\, I spent my summers r
 emoving rocks (glacial erratics) from wheat fields located behind the term
 inus of the Okanogan Lobe of the Cordilleran Icesheet\,' tells Lillquist.
 \n\nLillquist teaches physical geography\, geomorphology\, soils\, snow\, 
 airphoto analysis\, field methods\, mountain environments\, arid lands\, a
 nd graduate research. His current research is focused on environmental cha
 nge in the mountains and deserts of the western U.S.\, with an emphasis on
  using geomorphology\, soils\, and stratigraphy to better understand glaci
 ers\, rock glaciers\, glacial lakes\, and arroyos.\n\nAll ages welcome and
  admission is by donation | 347 Division Street in Leavenworth
DTSTART;TZID=America/Los_Angeles:20190424T190000
DTEND;TZID=America/Los_Angeles:20190424T203000
LOCATION:Barn Beach Reserve\, 347 Division St.\, Leavenworth
SUMMARY:Red Barn Event | Rock Glaciers of the Eastern Cascades\, Karl Lillq
 uist PhD
END:VEVENT
END:VCALENDAR