South Park trip photos.
[ 19:00 Sep 23, 2004 More travel/southpark | permalink to this entry | ]
South Park trip photos.
There's a terrific handout on the San Rafael swell area which shows up at some of the restaurants and motel racks in Green River, which includes a map of the swell's area and a geologic cross section of the exposed rocks, which confirmed our suspicion that the white sandstone exposed on the eastern side of the Reef is Navajo sandstone, just like the Slickrock Trail at Moab.
The highway has numerous pullouts marked "View Area", with fanciful names such as Spotted Wolf or Black Dragon, and fairly useful interpretive signs to go along with the views. We had to laugh at some of the "View Area" signs, with arrows pointing at spectacular rock formations, wondering: Could anyone drive by that and not view it?
After leaving the San Rafael Swell, the highway moves into the Fishlake National Forest -- fairly standard mountainous terrain -- then eventually south along the Sevier (pronounced "severe") river. Eventually we turned southwest on I-15 and headed down toward Vegas.
We did make a stop at our favorite Indian truck stop on the Moapa reservation in Nevada. In addition to a general store and fairly reasonable gas prices, they used to have a big sign advertising "Really Good Jerky", of both beef and buffalo. The jerky seller in the little trailer outside the general store gave samples (which he cut off with scissors), and it was indeed Really Good, so we've made a point of stopping for jerky every time we pass this way.
Alas, the jerky seller is no more, and we went jerkyless. The Moapa are now specializing in fireworks, and there was no sign of Really Good Jerky.
(Fortunately, the next day, Alien Fresh Jerky in Baker, CA, saved me from a totally jerkyless trip. I'm not sure it's *quite* as good as the Moapa Really Good Jerky; but it's really quite good (they have buffalo, turkey, salmon and alligator as well as beef, but free samples only for the beef), and the store, heavily decorated in an alien motif, makes an excellent kitchy stopover. Plus you can check out the World's Tallest Thermometer while you're in Baker. Dave and I stayed at the Baker Bun Boy Motel on our first night of our first-ever trip together, so there's a bit of romance to stopping in Baker. Do we know how to have a good time, or what?)
We passed through Vegas without a backward glance, and instead of staying in Jean as we have before, decided to try Primm, a few miles farther south near the California border. Primm sports three casino/hotels: we picked Whisky Pete's because it was on the right side of the road and had a sign offering $5.95 prime rib, though it turns out they're all owned by the same person and all probably offer the same deals. (The room rates at Whiskey Pete's are very reasonable, the room is nice, and the prime rib was excellent. The only downside is that there's no wifi, phone calls aren't free, and it's not clear whether a Vegas access number would be a local call or not. So no internet connection tonight.)
Primm is a bit of an enigma. I'm typing this in a room high in a tower surrounded by crenellated turrets, each topped with a Disney- style party hat with a little flag, and surrounded by blinking white christmas lights. We're having trouble figuring out what a Disney Sleeping Beauty castle has to do with the "Whiskey Pete" theme embodied by the western mining motif in the casino downstairs. The pool twelve floors below our window has a neat looking mini waterslide that goes through a fake little mountain (Disneyesque again) on the way down, but it appears to be closed (maybe if I went down and asked, someone would open it; I didn't try).
There's a sign in the casino for "Monorail to Primm Valley Resort". The "monorail" is a bus with rubber tires which run on two concrete tracks. The tracks go high up over I-15, from which you get a nice view of the pass to the south and the surrounding desert, not to mention the lovely crescent moon setting over the hills. It's free. It runs fairly often. It's really pretty neat. But I still haven't figured out what's "mono" about it. Maybe no one would be willing to ride a "birail".
Primm Valley Resort Casino tries to look a bit more upscale than Pete's. The buffet restaurant is decorated like they're trying to be the Butterfly room at the Bellagio in Vegas, but failing. The staff at the coffee shop is a little more dressy. The security guards all look glum (where the ones at Pete's look officious). The dinner menus are very similar. We tried to take the "monorail" (two rails again) down to Buffalo Bill's, which has a rollercoaster (which we've never seen in motion), but got tired of waiting for it and headed back to the Whiskey Pete's tra^H^H^Hmonorail. (We didn't check out the outlet mall next door to the resort.)
On the way back over the freeway, the monorail operator asked us why we were back so soon. We said we decided we liked Whiskey Pete's better. He said he did, too -- it was more casual. We chatted a bit (he's originally from the Navajo reservation in Arizona) and when he asked where we'd been, we mentioned that we'd been visiting relatives in Colorado, and Dave added that they lived at about 10,000 feet. The operator said "Sounds like Fairplay." We were stunned -- that's the next town over from where Kerry & Pam live. Turns out he lived there for a year or so, ranching. It's a small world.
There are basically two ways in: via a dirt road coming off highway Utah 24 from Green River, or via a dirt road coming from from near Hite marina at the northern end of Lake Powell. The Green River end looks a bit more accessible, so we chose that option.
One advantage of the U-24 option is that it passes right by Goblin Valley state park, said by everyone to be worth seeing. And indeed it is. "Goblins", also known as hoodoos or "stone babies", are vertical pillars with a harder capstone on top, which protects the softer stone of the pillar from erosion. In the case of Goblin Valley, the two components are made from two different members of the Entrada formation, the same sandstone which comprises the arches and walls of Arches national park. So both parts of the goblins are deep, dark red, and the capstones erode into rounded shapes which do look like heads. (They might also evoke other shapes to some eyes, but we won't discuss that too much on a family-rated blog.)
Attitudes are relaxed at Goblin Valley. We paid the entry fee ($5) and the ranger apologized for not having maps -- they're printing a new set -- but told us to go to the end of the road, park, and "just walk anywhere. There aren't any trails, go anywhere you want." And so we did, spending a happy hour or so wandering among the goblins and enjoying the nearby scenery (including the spectacular San Rafael Reef, a many mile long spine of uptilted sandstone -- Navajo? -- at the edge of the peculiar San Rafael Swell).
But eventually we had to leave, and continue our Maze quest. We turned onto the dirt road a mile or so down highway 24 and proceeded on our way.
This was the RAV4's first long dirt outing (though we've had it on nontechnical dirt roads before) and it did fine on the dirt road, which wasn't bad as such roads go. There are signs at all important intersections, not too much washboard, and only a few rocky or sandy sections. It took maybe an hour and a half to get to Hans Flat, which was the least flat place we'd seen since leaving Goblin Valley. Was Hans a joker, or did he get a flat once when driving there?
The ranger at Hans Flat was very friendly and helpful, but unfortunately discouraging about the roads. We'd already been warned by the ranger at Island in the Sky that the roads are very technical and aren't suitable for many street SUVs; we had hoped to be able to get to Panorama Point for a view of the Maze, but the Hans Flat ranger told us that yesterday someone in a Grand Cherokee had tried for several hours to get up that trail, and had finally given up. The issue is mostly ground clearance, though the rangers at both locations stressed the importance of having a low-range gearbox. (We remain somewhat skeptical about that, based on our admittedly scant off-roading experience in the 4Runner, which did have a 4-low; the RAV4 has quite a low first gear, and we both suspect that any road which requires lower gearing than that would stop us for other reasons, like ground clearance or traction, before gearing became an issue.)
The ranger did make her point, though, asking whether we'd been to Needles (yes) and seen the road called Elephant Hill (yes, and hadn't been willing to try it in the 4Runner). "All our roads have sections worse than that. We recommend that people drive around Needles a bit first, then come here if you decide that isn't challenging enough." Point made.
So she suggested we try driving out to the first switchback of the Flint Trail and check out the view from there, and get an idea what the Flint (a steep descent down a mesa wall, rather like the Shafer Trail which descends from Island in the Sky to the White Rim, or the Horsethief Trail we'd taken to get down to the bottom of Upheaval Dome) was like. Her opinion was that our RAV4 could probably drive down the Flint, though our brakes would be fairly hot by the bottom, but that we wouldn't be able to drive back up it and would have to go out via Hite.
The road out to the Flint was fun driving -- rocky and occasionally sandy, mildly technical, but nothing the RAV had any trouble handling. We stopped at a couple of viewpoints, but found them disappointing: really all we could see was the Nevada-like scrubland below the Orange Cliffs, and the scrubland of the Elaterite Basin below that, plus a few buttes. Nothing nearly as interesting as the view from paved highway 24 before we turned onto the dirt, let alone the panoramic vistas of Island or Needles.
The Flint Trail itself was interesting to see, though. We could immediately see why she'd said it was more difficult than the Shafer or Horsethief: it's a bit narrower (only one car width through a lot of its descent), a lot steeper at least in some places, more technical (rocks and ruts), and the traction was quite poor. We hiked from the first switchback halfway down to the second, and our hiking shoes kept slipping in the dust when we tried to stop and take pictures. The dropoff isn't quite as scary in itself as the other two trails (most turns have sizeable berms on the outsides) but sliding down a steep slope over rocks and deep dust could change the scariness in a hurry.
And the view? Well, alas, it isn't really any better from there. We still couldn't see much of the Maze, or much else besides scrubland and a few buttes.
We're left wondering: what does the Maze look like if you can actually get inside? Is its attraction simply its inaccessibility (we saw only one other couple the whole time we were there -- you're not going to get overwhelmed with crowds here) or is there stuff hidden in the Maze that compares with Island and Needles? Do we care enough to find a way to set up a multi-day biking or backpacking trip?
A disappointment. But at least we saw the Goblins.
The better known Barringer Crater in Arizona is an excellent example of a simple crater, while Upheaval has multiple shock rings and the apparent remnants of a central peak, perhaps even a central ring mountain. It's comparable to large lunar impact structures such as Tycho, Copernicus, or even Mare Nectaris or Mare Orientale, while its Arizona sibling is more like a small crater such as Linne.
So why is it called Upheaval Dome, you ask? Well, originally it was thought to be a huge collapsed salt dome: a pocket of subterranean salt swells from the effects of water, warping the rocks around it, then the salt leaks out and the dome collapses under its own weight. There are lots of salt valleys in the Canyonlands area, and the mophology of impact craters wasn't understood until fairly recently, so this explanation made some sense at one time. However, it turns out that there isn't any salt under Upheaval, and there are traces of shattercones and other heat-shocked rock, as well as chemical traces consistent with an impacting body. Gene Shoemaker and others have studied Upheaval extensively, and the results all point fairly convincingly to an impact. The national park service, however, hasn't quite come around, and still presents the salt-dome theory alongside the impact crater theory, and the name remains "Upheaval Dome". Sigh.
Dave and I have visited Upheaval several times -- it's one of the places we keep coming back to, and it's spectacular every time. We've been inside once, when we hiked up from the Green River on our honeymoon, and have walked the short trail to the two overlooks on top several times. The last time, however, we noted that the overlook trail continues (though no park documents mention this -- they all show the trail stopping at the second overlook), and this time we wanted to see how far it goes.
We didn't find out. It continues for miles past the overlooks, marked by cairns (ever notice how park brochures and signs never mention cairns? Do they figure that anyone silly enough to want to go for a hike in a national park already knows they're trail markers?), giving one spectacular view after another, of Upheaval, or its runoff canyon leading to the Green River, or the Navajo sandstone domes comprising the southern end of Upheaval's second shock ring. We puttered around for several hours, hunting cairns up and down steep slickrock surfaces and along sandy washes, trying to scope out connections between this upper trail and the "Syncline Loop" trail, which circumnavigates Upheaval farther out, beyond the first shock ring, and connects with the lower trail that goes into its center.
But all good things must come to an end, so eventually we found our way back (via the Syncline Loop), paid a quick visit to the Green River Overlook and the spectacular Grandview Point (perhaps the most scenic spot in any national park), watched a minivan essay the torturous turns of the Schaefer trail (riding the brakes the whole way; understandable, when you look at the several thousand foot sheer dropoff on the outer edge of this narrow dirt road) then headed north to the town of Green River to set up for our assault on the Maze. Green River may not have a list of dining establishments to rival Moab, but it has a central location under the scenic Book Cliffs, plus one thing Moab lacks: cheap motels with wi-fi access.
Getting to the trailhead turns out to be easier said than done. Our hosts had assured us the exit was marked, but the exit for Hanging Lake has since been closed. It turns out you now have to go two exits farther, turn around and get back on the freeway going the other direction, and remember the exit number to get off at the right place. Don't get off early, or you can't get back on and have to cycle all the way around again.
Once there, you walk a quarter mile along the river on a paved bike path, and then the real trail begins, climbing steeply along rock stairsteps. The steepness of the climb doesn't ever let up significantly. Groups of people (this is a popular trail) rest by the trailside. Groups coming down mutter encouraging words to tired climbers. We asked one descender, "Is it worth it?" His answer: "Oh, god, yes."
And indeed it was. The hanging lake is spectacular and beautiful, a shallow pond of clear azure waters. And fish. How did the fish get there? Interpretive signs discuss black swifts (nowhere to be seen) and oil shale columbine (which I'm sure are lovely if you're there in season, which we weren't) but nothing about the fish.
Every descending hiker, as well as the trail description down at the trailhead, urged us not to miss the short side trip to Spouting Rock, so of course we checked it out. A stream of water gushes mysteriously out of a hole in the otherwise solid rock of the cliff face, becoming a waterfall which feeds the lake. Fabulous!
I've driven through Glenwood Canyon several times before, always impressed at the beauty of the canyon (I-70 through eastern Utah and western Colorado has got to be the prettiest interstate highway anywhere) but I had no idea I had been missing the best part. It's well worth the couple of hours' stopover when travelling through that area.
The only disappointment was that they sported the same thumb-push-button throttles as snowmobiles and jet-skis use, which makes my thumb ache after only a few minutes of riding. I knew Kerry & Pam had been motorcyclists, so I jumped at the chance to ask: why thumb throttles, rather than a twist throttle like a motorcycle?
Kerry's answer was prompt (it was obvious he had thought about this before): because they're awful, everybody hates them, and that way everyone will spend more money buying an upgrade kit (which costs another $100 or so) from the manufacturer since nobody makes aftermarket kits.
I'm not sure I believe that. If it's true that everybody hates thumb throttles, then wouldn't a company which bucked the trend and offered an ATV or snowmobile with a twist throttle have an instant market advantage? And why hasn't some enterprising aftermarket company come out with a kit if they're in such demand?
But I don't have an alternate explanation. It's some consolation, at least, to hear that I'm not the only one who hates thumb throttles, and that it is possible to buy a twist-throttle kit (perhaps it's even possible to fabricate one out of motorcycle parts).
The terrain visible from the highway up to the pass was typical Colorado mountain scenery, in fine form: rocky cliffs, aspens just starting to turn, a river meandering beside the highway (which proved to be the North Fork of the South Platte -- I guess they were running out of names for rivers), pines. So when we crossed the pass, we weren't prepared for the sight on the other side: a huge flat grassy plain stretching for dozens of miles, pocked with ranches. A huge plain at 9500 feet. It was like Colorado's answer to the Altiplano of the Andes!
We later learned that this feature is known as a "park", and that this one is called "South Park". Yes, that South Park -- supposedly the animated TV show is named after this plain, or the ghost town on the western edge of it.
We found the dirt road leading to K&P's place, and we were there. They sit on the edge of the altiplano -- er, park -- at the foot of a couple of spectacular "fourteener" mountain peaks astride the continental divide, surrounded by aspens ablaze, with two creeks running through the property, horses and cows, ATVs, several parrots, and a cheerful red merle Australian shepherd puppy named Ben. Plus elk (invisible on this trip -- it's hunting season, so they're hiding), pronghorns, mountain bluebirds, coyotes, and a host of other wild animals.
In other words, paradise. At least if you don't mind fairly harsh winter weather, and can function at over 9000 feet of altitude, which not everyone can. The couple of days we spent there wasn't really long enough to adapt.
One of the two creeks is actually a culvert, and a constant source of problems. It seems that beavers have been damming up the culvert, creating lakes that overflow the driveway and make it impossible to leave the house. We went along on one walk of the culvert and see the latest beaver dams (and, of course, try to catch a glimpse of the beavers themselves, but we never got a definitive look).
We passed two idyllic days hiking the property, riding ATVs, playing with Ben, listening to the parrots practice whistles and phrases, looking for beavers, watching blue herons and bluebirds, and just gaping at the amazing views. On the way out, we saw a pronghorn wandering right next to the road.
The eastern end of Dinosaur National Monument seemed a bit of a let-down, at first. The road stretches about 30 miles from highway 50, and along most of that length there's very little to see, as the road winds along the scrubby mesa top. Only the last six miles are in the park, and those include a sparse handful of viewpoint pullouts, none of which give much of a chance to see the rivers. So our hopes rested on North's Rule of National Parks: The end of the road is where the Good Stuff is.
We got to the end of the road, parked ... and still couldn't see much. The parking lot is surrounded by trees and doesn't come very close to the edge of the mesa on either side. You really have to walk the one mile trail to the end of the mesa in order to see anything.
And at first, it seems like the trail isn't any better, and the trail guide (25 cents at the trailhead) is full of the usual mind-numbing Park Service platitudes (Look around you ... even though there's a river down at the bottom of the canyon, it's dry up here. So the trees have to survive on not much water). But hang in there, for a fairly spectacular view at trail's end of the tilted, twisted Mitten fault, as well as the joining of the Yampa and Green rivers (the confluence itself isn't visible, hidden by a formation known as Steamboat Rock). The fault cuts across the river (or, rather, the river sliced through the already-formed fault when the Uinta uplift raised this area above its surroundings) and you can trace it back along the terrain to the cliff on which you stand. Downstream, Whirlpool Canyon (so named by John Wesley Powell) cuts through sediment of a very different nature from the sandstone cliffs upstream of the fault. The park's trail map offers a diagram showing this, making up for the smarmy nature-trail points earlier in the hike.
After leaving the park, we headed east, across Rabbit Ears Pass. Dave had been there once as a young child, and said I'd understand the name when I got there ... and indeed I did. But which two of the three projections are the rabbit's ears? We passed lovely high meadow scenery most of the way, with the aspens just beginning to turn, and eventually arrived in Golden to meet Dave's family.
Not because of the red gorge, which by all accounts used to be spectacular before the dam was built and the canyon flooded with a reservoir; and not because of the reservoir itself, which seemed nothing special. The interesting part of the view from Manila is two huge, parallel curving ridges with what looked like a lowered flat area in between. Imagine a freeway offramp leading from a high rocky cliff down to the reservoir, with a wall of sharp red sandstone on either flank ... then scale it up by an order of magnitude ... and you have some idea of what this odd formation looked like.
There's a forest service office in Manila, so we stopped to ask, "What the heck IS that thing?" We suspected successive glacial moraines, since the valley in which Manila sits looks very glacial (U-shaped, and all that) but we wanted to talk to someone who knew more.
Unfortunately, the geologist on staff was out. The ranger (new in town and not yet fully versed on the area) also thought moraines were a likely answer, but he and the helpful lady at the counter suggested I check back with the geologist, which I will certainly do.
Then we headed south to Vernal, and hit some nice surprises. First, someone involved with Utah road signs actually got the silly notion that travellers might have some interest in geology. Every mile or so, we'd pass a sign saying something like "Jurassic Morrison Formation: graveyard of dinosaurs", keeping us posted as we crossed each geologic layer boundary. It was almost like driving with "Roadside Geology of Utah", without having to check mile markers all the time. What a great idea! I'm sure it's appreciated by lots of travellers along that road, not just amateur geology wonks like us.
After a few miles of that, a pullout announced "Sheep Creek Geologic Loop". The AAA guide and a few other references I'd seen mention this loop as being near Flaming Gorge somewhere, but nobody actually says where it is or anything about it. What a nice surprise to stumble upon it accidentally!
So of course we took it. Unfortunately we lacked any guide to the road, and the Sheep Creek route doesn't have the frequent labelling of the highway leading to it. But the rocks were spectactular, varied, majestic, and warped, and the creek and surrounding aspen meadows (with the leaves just starting to turn) made for a fantastically scenic and interesting drive.
In due course we re-attained the highway, continued on to Vernal, secured a room, then proceeded to the main attraction: Dinosaur National Monument's famous Quarry.
I say "famous", but in fact, few people seem to know about this park. We'd learned through the web that the southwest end of the park, nearest Vernal, contains a visitor's center building built around an existing rock wall containing a large collection of dinosaur bones. What a neat idea! But reading about it, or photos on the web, doesn't prepare you for being there and seeing the wall, still connected to the rest of its sandstone cliff, with hundreds of dinosaur bones -- real ones, not plastic casts -- there to be seen, touched, and cataloged. It's so far beyond any fossil exhibit I'd seen anywhere else that it's not worth comparing. Even the excellent Burgess Shale exhibit at Yoho in British Columbia pales. It's fabulous. If you like dinosaurs, see it.
Afterward, we drove to the end of the road, admired the spectacular rock formations and the Green River, hiked a short way into a box canyon (to admire more twisted and tilted rock formations), then headed back to town.
Tomorrow: More dinosaurs, then on to Denver.
They begin at Wendover, a typical Nevada "border town", full of good deals on motels and food (financed, of course, by the casino action). Wendover straddles the Nevada/Utah border, and thus West Wendover, NV is in a different time zone from Wendover, UT. There isn't much to Wendover, UT, though, besides the Air Force base.
A few miles east of Wendover is the first of the excellent Utah rest stops, featuring a tall platform which offers a view of the flats, including a glimpse of Bonneville Raceway, where land speed records are set. The picnic table shelters feature graceful, swept roofs which look like they're in the process of setting land speed records themselves.
Beyond the rest stop, the salt flats continue to interest. First is the surprising amount of water. Even in late summer, somehow these remnants of ancient Lake Bonneville, which once covered most of northwestern Utah, hold standing water a few inches deep, and small waterbirds flit around, somehow scratching a living out of this salty desert.
The horizon shimmers with mirages. Distant mountain ranges seem to float on a glittering watery carpet; the road ahead disappears into an oil slick which never gets any closer.
The salt roadsides are crisscrossed with tire tracks, from travellers who pulled off the road to drive donuts in the salt, and with phrases and pictures drawn as rock mosaics. Then the ball tree looms on the horizon -- a huge metal tree fruiting with athletic balls the size of box trucks. One tennis ball has fallen, and its slices lie beside the tree. On the eastbound interstate, not even a pullout is offered to explain this vision. (Westbound travellers can stop and read information about the artist who designed the sculpture.)
Eventually the glittering white salt gives way to more conventional desert sand and sagebrush, and the second rest stop appears. This one is even better than the first: the traveller who braves the "Beware of snakes and scorpions" sign can climb a narrow trail up the crest of a hogback (originally volcanic? or metamorphic? Whatever they are, they also contain interesting intrusions of broken geodes and chunks of limestone) to a panoramic view of the Cedar Mountain Wild Horse Range. A horned lark perches on the highest point of the hogback, perhaps enjoying the view as much as we were. We saw no scorpions, snakes, nor wild horses.
Coming closer to Salt Lake City, billboards reappear, some with intriguing advertisements like "Missionary Mall". Irony? Or serious? We may never know. The huge (but low, in late summer) Great Salt Lake appears, followed by the Morton Salt plant (tall glistening piles of whiter-than-white, and the intriguing girl-with-umbrella logo -- "When it rains, it pours". What does raining have to do with salt, anyway?) Then Saltaire! The odd abandoned resort on the shore of the Salt Lake, with its gold onion domed top still shiny, but the rest of the building decrepit. I think it's been made into a park now.
(On Morton's motto: a friend, Bill Arnett, explained it to me: "When it rains, it pours" refers to the fact that Morton (and probably all other modern table salt) has additives that keep it from absorbing water and becoming a sticky mess in humid weather. . In fact, here's the explanation on Morton's FAQ page.)
I found Salt Lake a rather nicely laid out city the few times I've been there. We didn't stop this time, though, but headed up into the mountain passes toward Wyoming. Just short of the border is the last of the great Utah I-80 rest stops, in a breathtaking canyon of red pillars, and again, offering a trail (steep and paved) up to a high vantage point.
Then across the border into Wyoming (including a stop at a nice viewpoint above a small reservoir) and Evanston. Like Elko, Evanston is a nicer town than I expected, with a decent selection of motels (it's even possible to find wireless internet, at a few of the motels or for pay via the "Flying J" truck stop's very strong signal (which even my wimpy Prism 1 and orinoco driver picked up from our motel a block away, beating my previous wi-fi distance record by about a factor of eight). Assuming, of course, that you don't mind sending your credit card information over a wi-fi signal. SSL should protect it ... I guess. But it makes me more nervous than the same operation over a land line. Besides, wouldn't it be fairly easy for some guest in the room below me to spoof the Flying J signal?
(I discussed this a few days later on IRC, when I got a better connection. We came to the conclusion that it would be possible to make such a man-in-the-middle spoof, assuming that you just accept every certificate in your browser: the spoofer could get a valid cert which was different from Flying-J's, and if you don't look at the domain when you accept the cert, then the spoof would work. But we couldn't come up with any way to make the spoof work if you do examine the cert. Moral: if you're on a questionable network, like a wireless one, and you need to send important info like credit card numbers, be sure to examine every cert for SSL sites.)
Evanston does not appear to have any restaurants to rival the Basque wealth of Elko, or the prime rib of Nevada in general. But it's a nice little town with a nice town square (we walked around after dinner).
Tomorrow: Dinosaurs! (Flaming Gorge to Dinosaur National Monument.)
The scenery isn't that bad; the problem is that it isn't that good, either, and it goes on for way too long.
Interstate 80 is the flattest route through the state, the preferred route of truckers, RV drivers, and pioneer wagon trains. Rather than cresting each of the myriad north-south mountain ranges comprising Nevada's "Basin and Range" geography, as highway 50 does, it follows the Humboldt river nearly all the way across the state as it skirts around the edges of each range.
Sometimes the billboards are funny. There was one proclaiming "Jesus Lives!", with an attribution underneath for adsforgod.org. Then in Winnemucca, a billboard advertised the smaller town of Battle Mountain:
Voted the armpit of America
by the Washington Post
"We didn't know you were looking!"
A bit before Battle Mountain, we passed the Thunder Mountain (something) Historical Site, which seemed to be a shack built up haphazardly of sticks and odd pieces of wood, decorated with whatever tschotchkes were handy. I weren't able to get a good look, driving by on the Interstate. I think I've found a picture on the web, though.
Elko is a nice place to stop, though. To begin with, it's full of Basque restaurants. I can only report on one, the excellent Nevada Dinner House.
Basque food is funny. Every Basque restaurant I've experienced has been very different; the only common element is that they all involve large quantities, especially the bottomless soup tureen. The Basque Cultural Center in south San Francisco approaches a fancy french restaurant, with appetizers like esgargot and entrees heavy on nicely done sauces. The severely overrated Woolgrowers, in Los Baños, serves uninspired mass-produced cafeteria food.
Elko's Nevada Dinner House has a simple, but varied, menu, heavy on steaks but with a good selection of seafood, pasta and other options. This is the second time we've eaten there, and both times we've been very impressed. My prime rib was about the best I've ever had; Dave's pork chops looked tempting too, with a nice herb crust on it (but nothing too foofy) and applesauce on the side. Salad, green beans, spaghetti in meat sauce, and french fries (er, "pommes frittes") accompanied the meal, along with the obligatory bottomless soup tureen (a moderately thick and tasty concoction involving barley, beans, carrots, and, I think, ham).
After dinner we went looking for a place to buy some soft drinks, and stumbled on a dollar store called "Honks" with a well-stocked sunglasses rack.
Then we retired to our motel room to bask.