From: Boise, ID
To: Battle Mountain, NV
Miles today: 316
Total miles: 13972
I got on the road pretty early, considering the
activities of the previous evening; about 9 am.
Rather than driving east on I-84 as I originally planned, I decided to
take a slight detour west. I-84 and ID
55 took me across about 20 miles of Boise suburbs, and there I caught up to US
95, which I had ridden through northern Idaho from the Canadian border. (It turns out US 95 goes all the way to Yuma,
Arizona, mostly in Idaho and Nevada.
Sounds like a good road trip for someone.) Boise is in the Snake River Valley, which is
very wide and runs east-west (the Oregon Trail ran through here); but I was now
heading south. The picture below is not the best, but you can see where the
(admittedly irrigated) farmland ends and the high, dry country begins.
The end of the Snake River Valley, where Boise is. Looking south, toward the "Northern Basin and Range." |
Boise itself is actually pretty high in elevation, at
about 2700 feet. Nonetheless, the
climb-out from the valley was quite noticeable, and I spent the rest of the day
at 4000-5000 feet. US 95 runs mostly
south, but cuts sufficiently west to pass through the southeastern corner of Oregon.
Unlike coastal Oregon, this is high-altitude near-desert.
US 95 continues into Nevada, and intersects Interstate
I-80 at a town called Winnemucca. The welcome
sign, which I could kick myself for not getting a picture of, read “And Proud
Of It!” I tried to find evidence of this
on Wikipedia, but it instead identifies the motto as “Winnemucca – Where the
Streets are Paved.” Either way, you have
to appreciate a town with a sense of humor. I tried to visit their museum, but
it is closed on Mondays. I turned east on I-80 and rode about 50 miles to Battle Mountain, Nevada, where I am now.
It was hard to tell how hot it really was. It could have been 90, or 110. It didn’t feel that hot because “it was a dry
heat.” Nonetheless, though I felt dry, every
time I shifted position while riding some part of me that had been pressed
against material came free and I felt the dampness of sweat, which quickly
evaporated. This is a recipe for
dehydration, and I knew it and drank a bottle of water (which I refilled at
rest stops) every 30-45 minutes. Even so, I felt like I was in one of those
Star Trek environments in which all the fluids were being sucked out of my body
through my pores. Which I guess they
were.
Like every town in Nevada, this one has a casino; actually
two; not bad for a town of 4000 people.
I asked someone working at the pizza joint where I got dinner if the
townspeople regularly went there. She laughed and said there was no way to
afford that; she went maybe once a year.
But since the town is on the interstate, and since there are so few
towns in Nevada anyway, a combination of tourists and transient workers of
various types keep the places going.
There are a lot of these workers; I got the last room in the hotel I’m
staying in while the rest is filled with a variety of people there doing
construction, working on “the power plant,” or in some way associated with the small
amount of mining in this region. Also, I note that I-80 runs along
the same route as an active railroad line, with a train roughly every
hour. Right outside my window.
A few words about this scenery I rode through today. The striking geological feature of the “Northern
Basin and Range” eco-region, from my view, is how vast, and how flat, the
regions between the mountain ranges are.
It is as if someone filled in a conventional mountain range to, say, the
75% level with sand (or lava, or volcanic ash), leaving just the highest peak
sticking out. In fact, this entire
region is flood basalt (a type of lava that I have learned to recognize), with
occasional large outcroppings of white volcanic ash, so perhaps this is what
happened. I’ll have to look into this
later.
What I rode through today. (This is eastern Oregon.) It is hard to get a sense of scale; in the picture on the right, the mountain in the background is probably ten miles away. |
Larry, you're exactly right about the valleys between the mountains being filled with deep silt deposits. When we visited the Nevada Test Site (er, excuse me, "Nevada National Security Site") they explained that one of the things that made it a good site was that it's incredibly easy to tunnel through the compacted silt in whatever direction you want.
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