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Helen and I were taking pictures, and looking at the sharp bits of obsidian everywhere, while the Energizer Bunny led the way. And led, and really led, then we were in her dust and the Energizer Bunny became a mere speck in the distance (Helen is shown in the near distance, and the tiny speck on the trail horizon is Liz, or the EB).
A couple of miles later after the trail went up then down then really up and really steep down, we were finally around the complete rim of the volcano, and caught up with Liz sitting in the shade of the trailhead sign.
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The next stop was the South Tufa formation, where the stacks of carbonaceous subsurface vent deposits rise like thousands of ghosts from the lake itself (its current level is much lower than historic high water in the Lake, revealing the tufa) as well as from shore lands below the ancient lake rim. This view shows Helen and Liz on the lakeshore. The tufa are remarkable formations, and the trail winds through ancient deposits.
We returned to our camp for lunch, then headed off to show Helen the Historic State Park of Bodie, an old mining town forever preserved in an arrested state of decay. We had about an hour to stay in the Park as it closed early at 3:00 p.m. off season, and then headed back out the narrow, winding road through open range. It was here that Helen spotted three pronghorn antelope in the distance. This is a picture of one of them.
On Sunday night, four rented, identical large motorhomes came into our park, and camped on either side of us. They were filled with very noisy tourists from somewhere "down under"--either Australia or NZ. They partied loudly until midnight, despite the quiet hours after 9 o'clock, and Liz and I got very little sleep.
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