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X-WR-CALDESC:The Wenatchee Valley Erratics\, Ice Age Floods Institute’s nex
 t Zoom program\, “Plate Tectonics and Cascadia Earthquakes\,” will be on T
 uesday June 8 at 7:00 PM with Kelsay Stanton\, Erratics past vice-presiden
 t and current UW PhD candidate. \n\nCalifornia is known for its earthquake
 s\, but what about the rest of the west coast? What are our seismic hazard
 s? Why don’t we have as many earthquakes as our more southerly neighbor? T
 his talk examines the tectonic setting for the Pacific Northwest and its m
 any seismic sources\, such as: \n\n•	“The Big Ones\,” megathrust earthquake
 s caused by the Juan de Fuca plate subducting under North America\; \n•	Slo
 w slip earthquakes and episodic tremor and slip\; \n•	Deep crustal earthqua
 kes\, such as the 2000 Nisqually event\; \n•	And shallow crustal earthquake
 s\, such as the 900 Seattle fault earthquake\, and the 1872 Central Washin
 gton earthquake from the fault near Entiat. \n\nKelsay will show how these
  fit into the tectonic picture\, and what it means for shaking in Central 
 Washington and beyond.\n\nPlease click the link below to join the webinar 
 at 7:00 PM on Tuesday\, June 8:\nhttps://us02web.zoom.us/j/86120141272\nWe
 binar ID: 861 2014 1272\n
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X-WR-TIMEZONE:America/Los_Angeles
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TZID:America/Los_Angeles
BEGIN:STANDARD
TZNAME:PST
DTSTART:20201101T020000
TZOFFSETFROM:-0700
TZOFFSETTO:-0800
RDATE:20211107T020000
RDATE:20221106T020000
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DTSTART:20210314T020000
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TZOFFSETTO:-0700
RDATE:20220313T020000
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BEGIN:VEVENT
UID:45de7802-e171-4f2a-b816-20fbec898ac5
DTSTAMP:20260424T112803Z
DESCRIPTION:The Wenatchee Valley Erratics\, Ice Age Floods Institute’s next
  Zoom program\, “Plate Tectonics and Cascadia Earthquakes\,” will be on Tu
 esday June 8 at 7:00 PM with Kelsay Stanton\, Erratics past vice-president
  and current UW PhD candidate. \n\nCalifornia is known for its earthquakes
 \, but what about the rest of the west coast? What are our seismic hazards
 ? Why don’t we have as many earthquakes as our more southerly neighbor? Th
 is talk examines the tectonic setting for the Pacific Northwest and its ma
 ny seismic sources\, such as: \n\n•	“The Big Ones\,” megathrust earthquakes
  caused by the Juan de Fuca plate subducting under North America\; \n•	Slow
  slip earthquakes and episodic tremor and slip\; \n•	Deep crustal earthquak
 es\, such as the 2000 Nisqually event\; \n•	And shallow crustal earthquakes
 \, such as the 900 Seattle fault earthquake\, and the 1872 Central Washing
 ton earthquake from the fault near Entiat. \n\nKelsay will show how these 
 fit into the tectonic picture\, and what it means for shaking in Central W
 ashington and beyond.\n\nPlease click the link below to join the webinar a
 t 7:00 PM on Tuesday\, June 8:\nhttps://us02web.zoom.us/j/86120141272\nWeb
 inar ID: 861 2014 1272\n
DTSTART;TZID=America/Los_Angeles:20210608T190000
DTEND;TZID=America/Los_Angeles:20210608T200000
LOCATION:https://us02web.zoom.us/j/86120141272
SUMMARY:Plate Tectonics and Cascadia Earthquakes by Wenatchee Valley Errati
 cs\, Ice Age Floods Institute
END:VEVENT
END:VCALENDAR