Peak 8085
8085 ft (2464 m) – 2160 ft gain
2024.09.14
I could not see the summit from camp even though it was yet another clear morning promising blue sky from horizon to horizon. Late summer in west-central Nevada, it would get warm later today, so I better get going.
The Garfield Hills hide a generally dry drainage system leading to a basin floor playa that stands white among sagebrush-covered alluvial fans and a coalesced bajada. The playa is difficult to visit because of a vaguely mysterious testing facility, vehicles of some kind, I think. When viewed from Highway 95 – the common route between Reno and Las Vegas – the Garfield Hills are almost non-descript. Brown, rocky slopes climb steeply to rounded summits; these reach over 8,000 feet but dwarfed by Mount Grant at over 11,000 feet on the horizon to the west.
I had few expectations walking away from camp before the sun crested the nearby ridge. Still, that is the primary pleasure of the many small groups of hills or otherwise anonymous ranges throughout much of Nevada, the most mountainous state not called Alaska. I cut across rolling hillslopes overlooking the Bataan Mine, a distracting scar with a few headframes, ore shoots, and too many prospect and trenches to count – I would avoid all that if possible. A canyon soon opened in front of me, much of it altered as one big prospect, but I finally climbed above the mine scratchings to gain a sandy wash that practically meandered through a granitic parkland. The granite had saved the upper mountain, no one mines granite unless its easy to transport large blocks to build financial and government buildings. It is the edges of the granite, like the lower canyon I had just walked through, that interested the miners. As a deep bubble of magma – what would become the local granitic pluton – pushed through the native rock, their interaction would encourage mineral formation as water, heat, and pressure worked their magic. Miners look at the edges of the action; I would walk into the heart of the pluton now uplifted and exposed by mountain-building as the bulbous summits of the Garfield Hills.
This I did not expect. The dry wash, climbing only gradually, is a parkland of boulders, junipers, and an occasional single-leaf pinyon. Sculptures of stacked boulders are decorated with small trees, and bunch grasses punctuate the shadows. Sitting to pack away my jacket, I notice an entire patch of boulders is walking away. The boulders are in no hurry. It soon becomes clear, with the aid of my binoculars, that I had walked unknowingly past a herd of Desert Bighorn, maybe twenty of them. They blend so well with the hillslope; it is only when they break the horizon that I can easily distinguish rams and ewes. I am not carrying a telephoto lens, thinking I would practice with one mid-range lens, so I sit and watch.
The sandy wash leads nowhere. Most washes break predictably into smaller tributaries and rills while moving upslope and updrainage; desert washes collect water and sediment, getting choked with sand as underfit flows lack energy needed to convey coarser materials basinward. This drainage seemed to ‘sky out’ as I reached a pass and drainage divide that dropped steeply to the east, the opposite of gradual parkland I had just enjoyed. It was beheaded, cut-off from the tributaries and rills I expect typically. Or so I thought. I eventually looked south to see small drainages continuing up hillslopes where an apron of rills was ready to deliver additional grussy bedload weathered from the ever-present granite. Not atypical once I soaked in the scene.
The view into Soda Spring Valley, against the tilted blocks of Black Dyke Mountain, is exceptional; dark hills against bright alluvial aprons and playas, four thousand feet below. After the gradual wash, there are steep ridges reaching toward the high point. It is a healthy walk, pushing through juniper snags braced against the wind even though it is calm today.
I find the summit register, its protective can – the usual red variety – filled with lethargic lady bugs. The insects colonize summits to avoid predation during their long winter hibernation, I am always mildly surprised to find them, but it is very common.
The Bighorn Sheep are not to be found as I descend the slopes where I first saw them. I searched the expansive hillslopes but see none. The slopes are well-tracked, so they are probably nearby, just well camouflaged. The mine looms before me, and I am soon on a well-used road back to my camp.
Once again, a small mountain range reveals its local wonder. My quest to climb all of Nevada’s named ranges is aspirational at best, but it gets me into the smaller spaces. Each is worth the effort of the small journey and relatively easy hikes. It may be that my lack of expectation is what keeps me motivated. The basic pleasure and excitement of simple discoveries – from granitic woodlands to red cans of sleepy lady bugs – are all it takes.
Keep going.
Please respect the natural and cultural resources of our public lands.