USGS/CVO Logo, click to link to National USGS Website
USGS/Cascades Volcano Observatory, Vancouver, Washington

DESCRIPTION:
National Lahar, Mount Rainier, Washington


National Lahar

From: Hoblitt, et.al., 1998, Volcano Hazards from Mount Rainier, Washington, Revised 1998: USGS Open-File Report 98-428
Large non-cohesive lahars at Mount Rainier are associated with volcanism. About 1,200 years ago, a lahar of this type filled valleys of both forks of the White River to depths of 20 to 30 meters (60 to 90 feet) and flowed 100 km (60 miles) to Auburn. Hot rock fragments flowing over glacier ice and snow generated huge quantities of melt water, which mixed with the rock debris to form lahars. Less than 2,200 years ago, another lahar of similar origin, named the National Lahar, inundated the Nisqually River valley to depths of 10 to 40 meters (30-120 feet) and flowed all the way to Puget Sound. More than a dozen lahars of this type have occurred at Mount Rainier during periods of volcanism in the past 6,000 years.


Return to:
[Mount Rainier Volcano Menu] ...
[Mount Rainier Historical Debris Flows and Mudflows Menu] ...
[Mount Rainier Eruptive History Menu] ...
[Debris Flows and Mudflows Menu] ...



ButtonBar

URL for CVO HomePage is: <http://vulcan.wr.usgs.gov/home.html>
URL for this page is: <http://vulcan.wr.usgs.gov/Volcanoes/Rainier/Lahars/Historical/description_national.html>
If you have questions or comments please contact: <GS-CVO-WEB@usgs.gov>
03/29/01, Lyn Topinka