I sat recently, looking at loops on maps. Along with my high points and study localities, I have charted the many routes traveled during excursions across Nevada and elsewhere. The east-west highways cut through north-south, basin-and-range structures, with secondary roads, paved and not, traversing valleys in a regular looping pattern. I have long wanted to complete as many Nevada loops as possible, exploring each basin and each range.
For the past few years, I have been focused on high points, reaching the apex of 130 of Nevada’s many ranges. I have explored the basins as well, and my work often highlights the landforms of the valley floors and margins, as that is where wind and water coalesce to arrange the dynamic landforms I am most interested in. With great intent, I create these ‘interests’ (e.g., high points, roads) as motivation and planning targets for my Second Friday excursions. I have realized, however, that I have been, maybe, too focused on summits, often missing opportunities to delve deeper into the surrounding landscape. I am, therefore, putting less emphasis on high points and shifting to basin traverses, finishing my road loops, if you will. So here we go, Darren and I are in Monitor Valley (April 2025), in the heart of the state.
There are several small obsidian sources, of poor quality generally, in the southern Monitor Range. I was interested in seeing the outcrops, if any, so we searched the area of White Rock Canyon and McCann Canyon, finding some decent nodules below massive tuff outcrops. It is, however, easy to see why this is not a prominent regional toolstone source, even in an area where obsidian is uncommon generally. The nodules are weathered and often almost crumbly; it is not good glass, although rare nodules are attractive. The Horse Heaven area is beautiful with amazingly healthy floodplain grasses. I am surprised by this and will consider another visit.
Mount Jefferson is the summit of the Toquima Range, an area I must get back to! High to the west of Monitor Valley, the vast summit area, spread between the mountain’s north and south summits – south being the high point at 11,932 feet – is the location of some of the most amazing high-altitude archaeology in the Great Basin. The sites exemplify the traditional awareness and use of alpine resources at a time that the valleys were drying overall. It makes little sense that I have yet to wander the summit tablelands – so many choices in the Basin and Range. Soon, yes, soon.
We camp near Diana’s Punchbowl, a carbonate travertine mound forming an anomalous hill, with a crater-like, water-filled throat, rising from the valley floor. I like how the groundwater discharge forms a complex of spring distributaries on the silt plain of the valley bottom. Alluvial fans of several ages and origins rise above the inset floodplain, the spring, and its prominent mound. We did not have ideal conditions to create interesting photographs, but it is an awesome place to sit and think about the origins of groundwater and the proximity of the heated magma plumes that underlie the thin crust of the central Great Basin.
Just after dawn, north of the hot spring, we found a gray ghost. The light-colored male Northern Harrier was busily building a nest with his darker mate. It was a splendid watch, catching this activity in the valley wetlands near Potts Ranch. This opportunity made up for the underwhelming light of the morning at the Punchbowl.
As we headed north, approaching Hwy 50, a new sound clicked from beneath the hood, competing with the typical clatter of the diesel engine. I have heard this in other circumstances and realized my alternator would not last much longer. Long enough to get home, probably, but we had hoped to circle south through Antelope Valley, east beyond the Monitors. So, prudence prevailed, and we turned west, heading home for a necessary repair. The valley loop will be there still.
This new, basin-centric approach should be enjoyable. As I look back, I need to take more time to better document the unique landforms and general character of the valleys, as I did with the high points. It’s an evolution but should produce opportunities to learn more about a place, from valley floor to mountain summit. We will see.
Keep going.
Please respect the natural and cultural resources of our public lands.