| The road never ridden...(see below) |
We had a nice hot breakfast at the Best Western Plaza Hotel and then prepared for the day’s trip to Jackson. But before departing, we toured the Hot Springs State Park, adjacent to our hotel. Even though the morning was chilly, we were warmed by the heat of the vaporizing hot mineral waters.
The park has an interesting geological history. According to the Wyoming State
Geological Survey: “The springs
emerge from the crest of the Thermopolis anticline, which is a large geologic
fold that formed during the Laramide orogeny (70–35 million years ago). The
Laramide mountain-building event faulted and folded the red Triassic-age rock
layers seen around the hot springs, and the hot water is thought to be
traveling up to the surface along those faults.
Big Spring is the largest of the park’s springs, with hot
water flowing across an impressive system of terraced travertine down to the
Bighorn River. Travertine forms by precipitation of carbonate minerals from hot
water, and builds up over time forming terraced steps. The bright colors are
caused by the incorporation of thermophilic organisms like bacteria and algae
into the travertine. Extensive travertine, sulphur, and gypsum deposits mostly
west of the river indicate hydrothermal activity has not always been confined
to its present location.”
Driving from Thermopolis to Shoshoni along the Wind
River Canyon Scenic Byway was glorious. The Byway has amazingly beautiful rock
walls rising 2,500 vertical feet on either side to the ridge tops and you can see
some of the oldest rock formations in the world, dating back to the Precambrian
period, (over 2.9 billion years ago) visible right from the highway. There are informative interpretive signs along
the way.
The headwaters of the Wind River are at Wind River Lake,
near Togwotee Pass. The river flows southeastward to Riverton where it makes a
turn and begins flowing north to Thermopolis.
At the “Wedding of the Waters,” the Wind River officially becomes the
Rocky Mountain Bighorn River, named for the mountain sheep indigenous to the
area.
From Shoshoni to Jackson we traversed the same highways we took
on our bike trips in 1982, 1995, and 2011.
Funny how memory works. We had
always felt that when we cycled the 122 miles down to Shoshoni from Togwotee
Pass, it was downhill the whole way, with minor exceptions. True, Togwotee Pass is at 9658 feet elevation
and Shoshoni, at 4852 feet. But in between,
one climbs almost 1300 feet.
Another
memory fail: Diane, navigator, reminded Rob
that eight miles south of Shoshoni we would turn west onto Wy. 134, and would
then turn south after 24 miles to intersect with US 26 West. But about two miles south of Shoshoni, Rob
turned west on an unmarked paved road, convinced it was the one we had bicycled
on previously. It wasn’t until several (Rob
disagrees that it was “several” ) miles later, when the road we were on took a
definitive turn north, that Rob acknowledged the memory fail. We had a good
laugh over that one.
As we approached Jackson, we realized that half of the North
Pathway we had planned to bike was one we had already biked in 2011. That fact, plus the smoky atmosphere
resulting from the Roosevelt
forest fire 30 miles south of Jackson, which has burned over 50,500 acres
since September 15, led us to nix the bike ride. Instead, we will take more time sightseeing in
the Craters of the Moon National
Monument and Reserve.
Pictures from the Hot Springs State Park
| Devil's Punch Bowl... extinct hot springs |
| Mineral deposits on river cliff with hot springs water flowing into the Big Horn River. |
| Diane wafting in sulfur aroma from the shallow hot springs pool. |
| Diane at White Sulfur Springs. Site of an early Hot Springs Spa. |
| Wind River Canyon |
| The mighty Tetons with a smudge of gray on their face due to the forest fire south of Jackson, WY |
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