Thursday, September 4, 2014
Lewis Lake campground receded in the rear view mirror as we left
Yellowstone and drove toward Grand Teton National Park. The
temperature was in the forties, and we just weren't feeling it for a
hike. Turning into the visitor center we realized that the park
would be crowded too, so we decided to just drive through it and
continue on towards Idaho.
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Looking at the Grand Tetons across Jackson Lake from the Colter Bay Marina |
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Driving down the scenic road toward Jackson |
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Beautiful exposure of a diorite dike (vertical, dark rock intrusion) at the top of the mountain. |
We drove through downtown Jackson, hoping to possibly find street
parking to get lunch and explore, but, it too was crowded and we
drove west towards Idaho. Leaving Jackson we joined the Snake
River, and then crossed into Idaho at the Palisades Reservoir. A
quick stop for lunch at Alpine, and we were on our way west through
the arid grasslands toward Idaho Falls, and then to the town of Arco,
which was the first town in the U.S. to have electricity powered by
the first nuclear power plant, just outside of town. That was in the
50's!
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Antler arch in Jackson town center |
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Looking across the Snake River Plain at the surrounding mountains |
After Arco the desert gave way to lava flows as we entered the
Craters of the Moon National Monument. We found a campsite in the
small barren campground with sites scattered among the lava piles.
Greg tried to sign up for three nights, but they only allowed campers
to sign up a night at a time. We soon learned why. The black rock
soaks up an extraordinary amount of heat. We were kept warmer than
the surrounding area at night, as the rocks gave off the heat stored
up during the day. Summer must be brutal. In the past, they probably
had lots of campers asking for refunds! We wound up staying three
nights. Hot, dry days, and comfortable nights, $5 a night, and an
unusual and spectacular landscape kept us there. Greg was able to
ride the paved park roads every day on his bike, and we hiked the
trails.
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Our campsite in the lava and cinders |
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Happy hour on our campsite patio atop a 20-foot high pressure ridge |
Greg's geology commentary - Craters of the Moon National Monument
preserves an area of volcanic formations including many square miles
of lava flows and their source vents. The lava flows erupted about
2,000 years ago, leaving flows ranging from smooth-looking pahoehoe
to rough, blocky a'a and frothy scoria cinders. Vent structures
include large cinder cones, smaller spatter cones and pressure
ridges, and a variety of intact and collapsed lava tubes, some over
50 feet in diameter. The monument comprises the northern section of
the Great Rift, which is a linear zone of volcanic vents and
pull-apart crevasses from which lava flows flooded the surrounding
desert landscape. The Great Rift is a clear example of recent
volcanic activity associated with Basin And Range tectonic stretching
and thinning of the earth's crust within the already-thin crust of
the Snake River Plain. Southeast of Craters of the Moon, lava drained
out of the vents while still hot, leaving rifts open to 800 feet
deep. Unfortunately, we did not get to see these interesting
fractures because they were 30 to 40 miles away down primitive desert
roads that are not RV friendly.
The photos below give you a sample of this wild landscape. Enjoy!
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Lava flows transition from smooth pahoehoe to blocky a'a due to a viscosity change. |
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Iridescent surfaces where the lava was smeared to a glassy blue surface when hot. |
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House-sized chucks of cinder cone wall rafted in the lava flow. |
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Hand-prints of celebrity jackrabbit in concrete sidewalk. |
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Climbing the cinder cone at Inferno Cone |
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This cinder cone looks like it erupted a few years ago and is deceptively steep - looking down at the parking area. |
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Looking southeast along the Great Rift, marked by the long row of cinder cones |
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Looking southeast along the Great Rift |
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Looking across the lava beds to nearby spatter cones and distant cinder cones. |
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Looking down into house-sized spatter cone core. |
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Some larger spatter cones |
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Lava "cascade" below a large vent |
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Hiking out the Tree Mold trail |
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Trees and Brush grow on the cinders better than the lava flows |
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Imprint of Limber Pine bark in 2,000-year old lava |
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Tree mold left by log that burned away immediately after chilling the lava surface. |
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Rabbit Brush in bloom |
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The lava caves trail |
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Lava tube with fresh-looking drips of lava |
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Exploring a collapsed lava cave |
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The entrance of Indian Tunnel, the largest lava tube cave |
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Skylight from another roof collapse |
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Rock rings left by natives |
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Remnants of someone's dinner |
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Well preserved pressure ridge |
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