USGS/Cascades Volcano Observatory, Vancouver, Washington
DESCRIPTION:
Ape Cave Lava Tube,
Mount St. Helens, Washington
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[Image,49K,JPG]
Ape Cave Lava Tube
-- U.S. Forest Service photo courtesy Gifford Pinchot National Forest
From:
Doukas, 1990, Road Guide to Volcanic Deposits of Mount St. Helens and
Vicinity, Washington: U.S.Geological Survey Bulletin 1859, p.12.
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Warm clothing and flashlight or lantern are needed if you plan to explore the
cave.
Ape Cave is one of numerous
lava tubes
formed in the Cave Basalt. The basalt consists of
pahoehoe flows
that originated on the southwest
flank of Mount St. Helens and flowed down the surface of older pyroclastic-flow
deposits. Charcoal samples from two localities under the lava tubes yielded
Carbon-14 ages of 1,860+/-250 and 1,925+/-95 years.
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, p.64.
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Ape Cave lava tube, which formed in one of these basalt flows
... (Cave Basalt flows about 2,000 years ago) ...
is the longest
lava tube
(12,810 feet or 3.9 kilometers) in the conterminous United States
(similar tubes are found in Oregon, California, and Idaho) and one of the
longest in the world. The cave was constructed by a
pahoehoe flow
that
crusted over; soon after, the molten lava on the inside drained away, leaving
the outer crust in place. Lava stalactites and stalagmites and flow marks can
be seen on the walls and floor of the cave. Lava stalactites, conical or
cylindrical deposits of lava that hang from the ceiling of a tube, are formed by
dripping; stalagmites are similar in shape and are formed on the floor of the
tube by the accumulation of drips from the ceiling. Some time later, a sandy
lahar
flowed into the cave, possibly in A.D. 1480 or 1482 because the deposit
contains white pumice granules that resemble W tephra. During the
summer, a national monument interpretive naturalist leads tours through the
lower part of the cave. Be sure to read the brochure (available at the cave
entrance) to find out more about the cave and the equipment you will need if you
plan to explore on your own. (Sturdy shoes or boots, warm clothing, and three
sources of light are recommended.
From:
..., 1989, Cenozoic Volcanism in the Cascade Range and Columbia Plateau,
Southern Washington and Northernmost Oregon: American Geophysical Union,
Field Trip Guidebook T106, Leader: Donald A. Swanson, Seattle, Washington to
Portland, Oregon, July 3-8, 1989, p.14.
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... The Cave Basalt issued from a vent probably near the southwest base of the
cone about 1700 years BP (Carbon-14); it contains 3.4-kilometers-long
-- (Web note: approximately 2 miles) --
Ape Cave, the longest known uncollapsed segment of a
lava-tube,
as part of its 8.3-kilometers-long
-- (Web note: approximately 5 miles) --
tube system.
From:
U. S. Forest Service,
Volcano Review: A Visitor's Guide to Mount St. Helens
National Volcanic Monument: Summer/Fall 1995
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Ape Cave:
Named by members of an outdoor group called the Mount St. Helens Apes, this cave
is the longest continuous
lava tube
in the continental United States. Cavers should wear warm clothes, sturdy shoes
and have at least two sources of light. Lantern rentals are available at Apes'
Headquarters.
Two different routes of exploration exist inside the cave and an above-ground
trail (Ape Cave #239) connects the main and upper entrances. The lower cave is
a relatively easy 0.75 mile hike that takes 1 hour round trip. The challenging
upper cave is 1.5 miles long, requires climbing over large piles of rocks and
takes 2.5 to 3 hours.
Trail Difficulty: Easy to Most Difficult
Return to:
[Ape Cave Menu] ...
[Mount St. Helens Points of Interest Menu] ...
[Mount St. Helens National Volcanic Monument Menu] ...
[Mount St. Helens Menu] ...
[Lava Tubes Menu] ...
URL for CVO HomePage is:
<http://vulcan.wr.usgs.gov/home.html>
URL for this page is:
<http://vulcan.wr.usgs.gov/Volcanoes/MSH/ApeCave/description_ape_cave.html>
If you have questions or comments please contact:
<GS-CVO-WEB@usgs.gov>
06/26/00, Lyn Topinka