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Jessup Embayment, North Island, Gold and Silver Mines and on down the whoop-te-doo canyon, 22 October 2007

RonC LR Trek Number 112 - Nevada
– Another MONTE-DISCO PRODUCTION


It’s the day after the LR Rocklin Trek (#111). Phil has to head back to Rocklin by about noon, so we decide to head out early and do a quick archaeology and exploration run. By the way; Phil and I have been amateur geologists together for the past 10 years. In fact, we took every geology course that Sierra College had to offer as well as oceanography, mineralogy and life sciences.

Ben, Phil and I are up at about 5:45. Showers were all done last night so we’re at the WigWam for breakfast by about 6:00 and on the road by a bit before 6:30. By 7:00 we’re already off-road heading out past the Jessup aggregate quarry towards North Island and the Jessup Embayment High-stand archaeological site. Ron and Phil in the ’04 Discovery and Ben in the ’04 Montero…

The first quest is to take the steep climb up out of the wash to the old beach line at 4400 feet at the base of a cliff on “North Island” The cliffs are broken columnar basalt. In fact someone has been quarrying the columns most likely for landscaping. The term island is used because this half square mile butte was an island in Jessup Bay back 12070 years ago when Pleistocene Lake Lahontan was at its highest elevation and largest extent. The actual high-stand was at 4398.5 feet, but I tend to use 4400 because it’s easiest to track on topo-map contour lines.

The trail up to the island has degraded quite a bit since I was last here, but Bens only problem is with a bit of IFS scraping on the rocks sticking out of the rutted part. Phil collects a few nice specimens while I take a few pictures of the scenery. After a few minutes we head back down into the “bay” and then it’s up the wash looking for the trail to the archaeological site.

I locate the trail first try and we climb up onto the bench and head south past the first playette. There are two gullies crossing the trail to the site that Ben gets to bash his bottom on again. Eventually we arrive at the big gully where we park. I’m sure that I could actually drive up the big gully and around the rock outcrop but I do try to tread lightly. We hike the last 200 yards to the playette site.

Ben and Phil are pretty impressed! I point out where the camel bones had been dug out and radiocarbon dated. Near the very end of the last ice-age this mini-embayment jutted off of the larger Jessup Bay. Lake Lahontan at that time was immense and had a reach on the order of hundreds of miles. During storms, waves developed a sand bar across the mouth of the playette and then it had filled with sediments washed down from the adjacent hills. The camel bones and many other fossils had been deposited into the little cut-off playette. The fossils were age dated and tended to agree with each other within a dozen or so years.

After leaving the playette, we head generally west through the Superior Mining Claims area and then over a couple of small hills to the north and into the Central Jessup gold and silver mining area. Central Jessup extends for about five square miles and is filled with probably 100 or so mine shafts and adits; all are too crumbly and dangerous to enter.

After Jessup, it’s up a small canyon along the northern edge of the Trinity Range and we arrive at the Gold Ore Claims. One shack and a powder bunker are all that remains along with about a half dozen shafts.

We retrace our route for about a half mile and turn south crossing a saddle and head down an un-named canyon that will eventually bring us back to the highway in about eight miles. I first ran this trail about three years ago. At that time, it existed on the map but was not discernable on the ground. During that first run, I had to continuously monitor my gps to make sure that I was following the correct wash. I was running it from bottom to top then which is a bit harder to follow the correct route. Now that Fernley has grown so much in population; a lot of motorcycles and quads have discovered it. In fact washes make for rather smooth trails. Once motorcycles use them they are full of dips.

About a mile down canyon, I take a turn to the west climbing up a side canyon. Only the first ¼ mile has been run by bikes so from that point on it’s just following the wash. After about ½ mile the wash gets progressively filled with bigger and bigger rocks. At a fork, I take the wash with the lesser amount of rocks. Another 100 feet and there is no sign of a trail. A bit of looking around and I can see where tires have crunched down some mountain mahogany. I carefully continue driving following where I can see that the brush has been crushed in the past.

According to the gps, I’m a bit south of the trail but I can still see the tire damage to the brush. Pretty soon we come to the flat top of a saddle. We’re looking down into another canyon. We are standing on black basalt desert pavement, with a view across Fernley Sink. We could probably with some effort, drive down through the steep rock garden to the canyon bottom. But again, we would not be treading lightly. Checking the gps; we are about a half mile from where the real trail should be according to the map.

We turn around and go back to the main canyon. For another two miles or so we wind down the zig zagging canyon passing aa-aa lave buttes and wash-cut lava bluffs. It’s getting late so we don’t take any more side canyons although a couple are available.

Back down below 4400 feet the canyon becomes a wide alluvial fan spreading out onto the sink. Eventually, we climb out of the wash onto a sandy plateau with a lot of diatomite outcrops. Then it’s just following mine haul roads back to the interstate interchange at Hot Springs/Nightingale. We get Phil back to the house and his car at about 11:45. Perfect timing! That brings us to the end of another perfect day in Nevada.

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http://s213.photobucket.com/albums/cc58/fortymile/trek%20111%20and%20112/

The photos with the 112-xx prefix apply
 

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