Thursday and Friday, October 2
nd and 3
rd,
2014
Thursday morning we said goodbye to Mono Lake by stopping for
breakfast at the Whoa' Nellie Deli in the Mobil gas station in Lee
Vining. We ate breakfast here last Spring and it was worth a second
visit. Afterwards we used the dump and water fill at the station and
we were off again down Hwy 395.
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Kathleen's giant croissant sandwich - neither of us wanted lunch until late afternnon |
We wanted to check out Devil's Postpile since the road was still
snowed shut last Spring. The entry road is up past Mammoth Mountain
ski resort and over 9,000'. During the summer you must ride a shuttle
into the national forest and the monument, but this time of year we
could drive the narrow twisty road. After passing through the entry
we descended into the San Joaquin River valley, with huge mountains
of granite on one side and Mammoth Mountain, a volcano on the other
side. There are a half dozen forest service campgrounds along the
road, all closed, except Red's Meadow. When we discovered that at
7,500', where the campground was situated, it wasn't supposed to go
below freezing that night, we decided to stay there.
|
The view across the back side of Mammoth Mountain from 9,000 feet |
First we made the turn into Devil's Postpile, parked and took the
short trail to the feature. Then we were able to hike along the side
and up onto the top of the pile.
|
The most famous view of the Postpile |
Greg's Commentary – Devil's Postpile is the remnants of a lava
flow that erupted about 100,000 years ago and backed up against a
glacial moraine, filing the valley about 400 feet deep. Moderately
slow cooling of the lava caused stress cracking in a more or less
hexagonal pattern. As later glaciers and stream erosion cut into the
hardened lava in the past 20,000 years or so, the basalt bedrock was
exposed as the dramatic pillars that stand vertically in the most
famous exposure but can be seen tilted or horizontal nearby. The most
recent glacial scouring polished the fine-grained basalt to a smooth
surface that was slippery even when dry.
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Hexagonal Columnar Jointing in vertical orientation - about 60 feet exposed above the rubble. |
|
Columns exposed at a 45 degree angle |
|
Glacial polish |
It is an unusual feature, and we especially enjoyed walking over
the top which looked like a patio of pavers. We had to watch our
footing as the rocks were polished slick by glaciers, and overlooked
a steep drop-off.
|
The polished surface curves smoothly to the vertical dropoff |
After exploring a bit more, we drove a short way down the dead end
road and pulled into Red's Meadow Campground. We found a reasonably
level site, no hook-ups of course, but the map said showers. Boy, we
could use those! Greg hiked up the short road and found an old closed
down hot spring and no showers. Why they've kept it on the map, I
don't know, but we decided to haul all our stuff out of the shower
“storage closet” and do a frugal shower in the rig, since the
campground had water, so we could replace what we used. After that we
grilled salmon and ate dinner while we watched a mule deer doe browse
through our campsite. Nice evening...
Friday morning we packed up and drove the short distance to the
Rainbow Falls trailhead. I admit to dragging my feet to get started.
It was near freezing when we got up. By the time we were halfway down
the trail, I had taken off my hoodie and unzipped the bottom of my
hiking pants legs. I always forget how intense California sunshine
can be! We crossed through a large area of huge blown down trees from
a storm in 2011 with winds up to 180 mph! In the same area we
encountered the remains of an intense fire. Along the path we crossed
over the Pacific Coast Trail which runs along the crest of the
mountains down the west coast, and we walked into the Ansel Adams
Wilderness. That was kind of fun, since most wilderness areas are
only accessible after a lot of hiking.
|
Slow recovery from the 1994 fire and the 2011 windstorm. Quaking aspens turning color. |
The falls were lovely as they cut through the volcanic rock. We
spent a bit of time enjoying them and the view from the steep
drop-off to the San Joaquin River far below. Then it was time to get
back on the road and drive up out of the valley again.
Back on 395 we had a short drive south to the washboarded gravel
road back to Hot Creek. We were hoping to luck into the same
boondocking spot we found last Spring. There it was, just before the
gate to Hot Creek and far enough off the main road to overlook Hot
Creek. Yay!!! Greg got the rig situated and we were ready for the
night. The sun set, the brilliant moon shone down on us, so brightly
that we could see our shadows, and the cattle bellowed. Huh? Far
across the desert and out of sight, all night long we heard frantic
bellowing from a large amount of cattle.
|
Hot Creek Boondock Camp |
|
Looking upstream toward the geothermal area |
|
Brightly colored Lichen |
The next morning with the temperature near freezing, we saw the
steam rising off thermal Hot Creek. Then we saw three large cattle
trucks blasting down the dirt road and out of sight. Poor cattle.
They must have been penned up all night waiting to meet their doom.
Now we knew why they were bellowing so frantically...
Our earlier post on Hot Creek Geological Area is at
The Sierras At Last!
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