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 30.10//
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METHOD:PUBLISH
UID:d4b82e89-f41e-4097-ae2b-a9673c957fc9
X-WR-CALDESC:The Wenatchee Valley Erratics\, Ice Age Floods Institute’s nex
 t Zoom program will be on Tuesday\, April 12 at 7:00 PM. Dr. Ralph Haugeru
 d\, USGS/UW\, will discuss\, “How are mountains made? The origins of local
  relief in the North Cascades.”\n\nMountains are made by uplift and erosio
 n. In the North Cascades\, folding\, faulting\, and granite intrusions thi
 ckened the crust about 105-50 million years ago. But the associated uplift
  probably eroded away fairly quickly. Volcanic activity created some moder
 n high elevations\, such as Mt Baker and Glacier Peak. Up-folding built ot
 her high areas\, such as the Naneum Ridge anticline\, which extends to the
  northwest through the Mt Stuart massif. Regional uplift probably has deep
 er causes. \n\nWhile we hypothesize the causes of uplift\, the story of er
 osion is more obvious. During our talk\, we will show evidence of several 
 local erosional events in the North Cascades.\n\nZoom link: https://us02we
 b.zoom.us/j/84812873290?pwd=ZlBnMHVDWmtYNEJHQ283V1kxWXA1QT09\nWebinar ID: 
 84812873290\nPasscode: erratics\n\nPlease sign in at 7:00 PM\, April 12!
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X-WR-TIMEZONE:America/Los_Angeles
BEGIN:VTIMEZONE
TZID:America/Los_Angeles
BEGIN:STANDARD
TZNAME:PST
DTSTART:20211107T020000
TZOFFSETFROM:-0700
TZOFFSETTO:-0800
RDATE:20221106T020000
END:STANDARD
BEGIN:DAYLIGHT
TZNAME:PDT
DTSTART:20220313T020000
TZOFFSETFROM:-0800
TZOFFSETTO:-0700
RDATE:20230312T020000
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BEGIN:VEVENT
UID:994b5b04-1d04-4258-b89c-729ead362893
DTSTAMP:20260404T222535Z
DESCRIPTION:The Wenatchee Valley Erratics\, Ice Age Floods Institute’s next
  Zoom program will be on Tuesday\, April 12 at 7:00 PM. Dr. Ralph Haugerud
 \, USGS/UW\, will discuss\, “How are mountains made? The origins of local 
 relief in the North Cascades.”\n\nMountains are made by uplift and erosion
 . In the North Cascades\, folding\, faulting\, and granite intrusions thic
 kened the crust about 105-50 million years ago. But the associated uplift 
 probably eroded away fairly quickly. Volcanic activity created some modern
  high elevations\, such as Mt Baker and Glacier Peak. Up-folding built oth
 er high areas\, such as the Naneum Ridge anticline\, which extends to the 
 northwest through the Mt Stuart massif. Regional uplift probably has deepe
 r causes. \n\nWhile we hypothesize the causes of uplift\, the story of ero
 sion is more obvious. During our talk\, we will show evidence of several l
 ocal erosional events in the North Cascades.\n\nZoom link: https://us02web
 .zoom.us/j/84812873290?pwd=ZlBnMHVDWmtYNEJHQ283V1kxWXA1QT09\nWebinar ID: 8
 4812873290\nPasscode: erratics\n\nPlease sign in at 7:00 PM\, April 12!
DTSTART;TZID=America/Los_Angeles:20220412T190000
DTEND;TZID=America/Los_Angeles:20220412T200000
LOCATION:https://us02web.zoom.us/j/84812873290?pwd=ZlBnMHVDWmtYNEJHQ283V1kx
 WXA1QT09
SUMMARY:The Origins of the North Cascades by Wenatchee Valley Erratics
END:VEVENT
END:VCALENDAR