Across the West and Back Day 2: Are We Lost Yet?

We left this meandering trip report almost two weeks ago, after MOH and I had taken our short hike into the limestone at the Grassy Mountain Rest Stop. From there to Salt Lake City, we cruised while admiring the shorelines of ancient Lake Bonneville.

Lake Bonneville shorelines in the southern Lakeside Mountains, looking northeasterly from I-80 about five miles northwest of Delle, UT.

And then: Salt Lake City.

Driving into SLC can make me somewhat apprehensive unless I'm going directly to the airport, and I had already started wondering if I was getting a migraine — possibly from normal trip concerns, possibly from driving, maybe from poor sleep the night before, possibly from some other, unknown cause.

I had looked at our route on Google Maps and had looked at the interchanges and major turns in Street View. Examining the route online is not the same as having a physical map in hand while driving (or in the navigator's hand, as the case may be) — at least not for me, or at least not unless I have some ingrained or recent familiarity with the particular roads in question. The last time I'd driven (or been driven) east through SLC without turning onto I-15 to go either north or south was in 1957 when I-80 didn't exist — and the 1957 trip definitely didn't count as recent, maybe more like Ordovician, or even late Precambrian.

I knew I was looking for the turnoff from I-80 to U.S. 40 — not that far past SLC, I thought — but I don't think I'd written down the miles to the exit, and I know I hadn't written down the exit number. And for some mysterious reason I was thinking that Park City (which I've never been to, except possibly on that long ago 1957 trip) was a lot closer to SLC than it really is.

Consequently, when the interstate turned a bit to the northeast and headed upward into the fairly tight canyon of Parleys Creek, I instantly freaked and thought it was the even narrower Echo Canyon, which I remembered from coming west out of Wyoming on I-80 on a 2006 trip. I was sure I didn't want to be heading into Wyoming on I-80, so I thought I must have missed the desired exit up somewhere near Park City (!).

I turned around at the first opportunity amidst a rash of roadwork, blocked exits, and narrowed lanes.

I knew I needed a map, so we got off at what turned out to be Exit 4 on 215. We pulled into a gas station and got some gas and a relatively small scale map of Utah. It was at this point that I was sure I had a migraine — and migraines do this funny thing to your overall thinking and analysis skills.

After examining the map while experiencing fairly moderate noise, light, and motion sensitivity that caused me to have problems looking at the map and then looking anywhere else, like at the road, I decided we were on an "outer" loop around SLC that I was previously unaware of. (This "outer loop" actually consisted of I-84 from Ogden, east and southeast to I-80 at the beginning of Echo Canyon, and south and then back west into SLC on I-80, but that part of I-80 wasn't marked, neither was 215 marked, and the insert for SLC was surprisingly small and lacking in detail.) We were actually at a gas station along the 215 partial ring road, and I probably knew that fact when I had turned on to it after turning around in Parleys Canyon.

I figured all we'd have to do was get back onto this previously unheard of "outer loop" and head east or south to our desired exit onto U.S. 40 near Park City. Wrong.

The map in question.

By this time, MOH had wisely taken over the driving while I endeavored to determine our exact location. With a blur of freeway lanes, cars and trucks, and exits coming too fast to comprehend (this should have given me a clue), what I was seeing on the map (how could Alta and Snowbird already be north of us?) wasn't matching the route I'd incorrectly figured was the one we were on, and it wasn't matching my still intact knowledge of where we really were along the Wasatch.

Suddenly, the "outer" ring road turned due west, and I knew something was very wrong. I realized where we had to be (on the "inner loop" road, i.e. 215) just in time to navigate properly and direct us onto the exit for I-15 south. Whew!

At this point, we thought it would probably be just as easy to take the next road south over the Wasatch than to turn around and go back for I-80, Park City, and U.S. 40. As for this thought: not exactly correct.

View Our Crazy Route through SLC in a larger map

Because we went (unexpectedly, for sure) south on I-15, I was able to get a pretty decent, albeit somewhat grainy, shot of the Bingham Canyon copper mine.

View of the Bingham Canyon copper mine, looking west from I-15.

It has been quite a while since I've been to Bingham Canyon — and I've never had a tour into the pit itself — but I strongly recommend going to the overlook and Visitors Center (the latter of which I've never seen) when they are reopened. The overlook area has been closed since the April 10th landslide (see a pre-landslide panorama of the pit here, view Kennecott's photos of the slide here, and read about the slide on several blog posts by Dave Petley).

Looking east toward American Fork Canyon.

And so, with our most recent trip decision finally behind us, we proceeded down I-15 to the Utah S.R. 92 exit, onto 92, and into the Wasatch via the easy, wide-looking American Fork Canyon.

View Day 2: Elko, NV to Vernal, UT in a larger map

The embedded map above shows the location of the three photos in this post (and also the rest of the Day 2 photos already posted, if you move around inside the map or view it in an enlarged version).

Related Posts:
Across the West and Back Day 2: A Hike along a Limestone Ridge
Across the West and Back Day 2: Across the Salt Lake Desert
Across the West and Back Day 2: A Side Trip in West Wendover
Across the West and Back Day 2: Pequop Summit to West Wendover
Across the West and Back Day 2: Looking for an Old Roadcut
Across the West and Back: The First Day
Intro to Recent Western Loop Trip

Across the West and Back Day 2: Pequop Summit to West Wendover

On our journey eastward across Nevada, MOH and I were last seen approaching the Pequop exit in the Pequop Mountains. Just beyond that exit — which provides access to such places as Milk House Spring, Adele Spring, and Nanny Creek to the south and East Squaw Creek to the north — I-80 crosses Goshute Valley, heading for a passage over a low spot in the Toano Range.

Large alluvial fan in Goshute Valley.

Around the bend in the photo above, I-80 crosses a large alluvial fan coming southward off one area of the Toano Range. Both sets of mountains in the photo are parts of the Toano Range, with the low point in the center just beyond the fan being Silver Zone Pass.

A little farther on, in the center of Goshute Valley, you can look back toward the Pequops and see the drill roads of Newmont's Long Canyon project, which was acquired by buying Fronteer Gold (link to Fronteer's website now goes directly to a 2011 Newmont announcement about the buyout), who had done a good portion of the work on the property (along with others before them). An inferred resource of 2.6 million ounces of gold has been announced by Newmont.

Long Canyon drill roads on the east side of the Pequop Mountains.

About midway across Goshute Valley, shadows to the south made Shafter Knoll, about 13 miles distant, stand out against the faded blue of the Dolly Varden Mountains, which are about 42 miles south of the highway.

Looking south. Shafter Knoll is on the left, the Dolly Varden Mountains are in the center, and the Pequop Mountains are on the right.

Road construction on I-80 in the Toano Mountains.

As I've mentioned in earlier posts, we saw a lot of construction on the roads we travelled. This is the first time I've seen a mini-tunnel installed over a road to prevent rocks from falling, sliding, or flying through the air into the roadway. Two of these were being used, with the second spanning the westbound lanes of the freeway.

After crossing the Toano Range at Silver Zone Pass, I-80 goes into a straight section in the south end of Pilot Creek Valley. Here, the alluvial fan in the distance, coming off of the Leppy Hills north of the highway, looked as though it was crossing the valley to run up against the mountain range on the south, which is actually an eastern bulge in the Toano Range.

Looking southeast down I-80 at an alluvial fan coming out of the Leppy Hills on the left, with hills of the Toano Range on the right.

The topo maps of the area make it clear that alluvial fans from the Leppy Hills and meet fans from the Toano Range in the middle of the valley at a low, broad juncture between the ranges.

Topography is from the USGS TNM 2.0 Viewer (link).

The associated air-photo view shows a lot of shorelines from ancient Lake Bonneville. I'm wondering if the gravel pit seen in both views isn't in a gravel bar formed during Lake Bonneville times, but haven't found any literature to support that idea (and we zoomed by, not stopping for the fan or hypothetical gravel bar).

Air-photo view of the same area (link).

As we moved farther across the south end of Pilot Creek Valley, this unexpected view of rustic-looking buildings, reminding me of old western movie sets, popped into view.

Looking southwest toward the Toano Range.

Just beyond the buildings on the range front, I could see what looked like a small limestone mine. This turns out to be the Pilot Peak lime plant, operated by Graymont, which processes material quarried on site (you can see the highwall of the small mine behind the plant).

Pilot Peak lime plant and quarry.

A few minutes later, we were across Pilot Creek Valley, and our first glimpse of the Great Salt Lake Desert came into view beyond a low divide.

Looking southeast across  a bit of the Great Salt Lake Desert (white, beyond the closer hills), with Dutch Mountain about 35 to 40 miles away in the distance.

All through this leg of the trip, I'd been keeping my eye on the small portions of old U.S. 40 that hadn't been wiped out during construction of the interstate. Coming into Wendover, you end up looking straight down a still paved portion of the old highway, which is the main street in West Wendover, known as West Wendover Boulevard.

Looking nearly east down the main street of West Wendover to the Bonneville Salt Flats out beyond the NV-UT state line.

We had to get off in Wendover for some travel supplies, so we ended up driving on old highway 40 for a very short distance.

Be sure to check out the map insert below (and a larger view in Google Maps as desired), where I show the day's photos (to this point in the day). I've added a few of the locations mentioned in the post, including the alluvial fans shown above, Shafter Knoll, the lime plant, and an old part of U.S. 40 in West Wendover (which I'm often in the habit of calling Wendover, even though Wendover is in Utah and West Wendover is in Nevada).

View Day 2: Elko, NV to Vernal, UT in a larger map

Related Posts:
Across the West and Back Day 2: Looking for an Old Roadcut
Across the West and Back: The First Day
Intro to Recent Western Loop Trip

Salt from Bonneville Salt Flats

Bonneville Salt Flats looking north toward the Silver Island Mountains and Floating Island (small and to the right).

While on our recent trip to Ogden, Utah, MOH and I stopped at the northern of two view-oriented rest stops located on I-80 near the Salduro railroad siding about 8 miles east of the Utah-Nevada border (MSRMaps location). Both rest stops provide good viewing of the Bonneville Salt Flats. From the northern rest stop parking lot you can walk out onto the flats, or at least to the edge of the flats, depending on water level or dryness.

Google Street View at northern rest stop

I didn't walk out very far, just to water's edge. A few other people were out a little farther; someone was collecting salt in large bags, probably for personal use.
A chunk of salt in its native habitat.
MOH brought a small piece of salt home, to add to our mostly unlabeled mineral collection. This is the side with the largest crystals.
Side view of same salt chunk.
View of the opposite side. One of the two sides had encrusted a surface of some kind; I'm not really sure which side was up and which was down.
Salt, more properly known as halite or NaCl, is a cubic mineral.
Cubes on top of cubes.
Tiny cubes.
More cubes.

Halite is a relatively soft mineral with a Mohs Hardness of 2½, meaning that it's barely not scratchable with your fingernail (which is also 2½), but it can be scratched by almost anything else, including a copper penny, a knife, a piece of glass, and steel. Halite tastes salty (surprise!), but not as bitter as the related potassium salt, sylvite (KCl).

Potash (mostly KCl) is mined from the Bonneville Salt Flats, as is magnesium chloride brine, which is used to produce magnesium metal and chlorine gas (for various purposes), and magnesium chloride, which is used as a dust suppressant on dirt roads and for other products.

A Few Links:
Mineral production from the Great Salt Lake

Mining and land speed records come together at Bonneville Salt Flats

View halite with a petrographic scope at Life in Plane Light