A short walk to the east brings you to a small hill and the viewpoint. This
area was swept by a lahar within 15 minutes after the onset of the May 18, 1980,
eruption. At this point, the speed of the lahar was estimated at about 44
miles per hour. Conspicuous notch in the east rim of Mount St. Helens is a
truncated valley cut by the
Shoestring Glacier.
-- Excerpt from:
Doukas, 1990,
Road Guide to Volcanic Deposits of Mount St. Helens
and Vicinity, Washington: USGS Bulletin 1859, 53p.
Lahar Viewpoint Cornucopia
|
Lahar Viewpoint, Stratigraphy Viewpoint, and
Lava Canyon Trail
are clustered.
This area is an interpretive cornucopia. Many geologic features are within
walking distance of the parking areas. Fragmental material and lava flows from
older eruptions of Mount St. Helens and dramatic effects (deposits, scarred and
killed trees, mudlines, and stream channel adjustments) of the 1980 eruption are
visible here.
Take the short (several hundred yards) trail over bouldery terrain to the east
toward a small hill. Near here the lahar split, one branch flowing down Pine
Creek and the other down the Muddy River gorge. A large, lone tree south of the
road is scarred on its upstream side, showing the maximum height of the lahar in
this location.
-- Excerpt from:
Pringle, 1993, Roadside Geology of Mount St. Helens National Volcanic Monument
and Vicinity: Washington Department of Natural Resources, Division of Geology
and Earth Resources Information Circular 88
|