Crowley Lake is famous for the Crowley Columns. Bad news is I couldn't get there without a 2 mile hike or a 4WD as it's all dirt roads to get to the trailhead.
On the eastern shore are these unbelievable <natural> columns.
A caldera is similar to a sinkhole, essentially a giant hole or depression that results from a volcanic eruption, but on a much larger scale. Magma chambers are large pools of liquid rock beneath the earth’s surface. Calderas like the one we’re riding across are formed by the inward collapse of a volcano. Long Valley Caldera is considered one of the earth’s largest calderas, running 20 miles long and 11 miles wide, creating this broad valley that Benton Crossing Rd flows across. Ash from this eruption 760,000 years ago blanketed much of the western regions of the United States.
Hot Creek is a super cool place hidden behind the Mammoth Airport I had never heard of it & ridden past it countless times. It's literal. The creek is warmed by magma chambers under the creek. The water is boiling.
Seemed like the perfect opportunity to ride the June Lake Loop, known as the Switzerland of California. This is a short 16-mile loop off the main highway and normally very scenic.
The cable tramway is one of the more interesting things I've researched in writing articles. Cool to be standing on it. Small rail cars are pulled all the way up the mountain side with steel cables.
This tramway is still in use today by the power company to maintain the dams on Agnew & Gem Lake. The steep railway was originally an elevated wooden trestle. In the 1950s, the elevated wooden railway was torn down and the slope back-filled then graded smooth, being completely rebuilt with the tracks on the ground. The incline tram is pulled up the mountainside with a single steel cable powered by an electric motor at the summit at a max grade of 60-degree incline. The steel cable on the Agnew Tram is 1-mile long. Train cars pulled up supplies to build the dams at Agnew Lake and Gem Lake. The lake was name for Theodore C. Agnew, an early settler, and is a glacial lake left behind from the Rush Creek Glacier. A short Y-switchback spur was added in 1953 to allow the tram cars to divert to Agnew Lake Dam.
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