Day 1
Sunday, April 7
Start: Salt Valley Road NP boundary
End: Willow Springs Trail, western NP boundary
Nightly low: 35 F
Miles: 12.5
After the obligatory photos at the park boundary of two eager trekkers putting on their packs in earnest for the first time, we waved goodbye to Caron’s friend David Morgan who was nice enough to deposit us there. We
We stopped to eat lunch, our first official food on the trail, near the end of our road walk and before the first of many sudden and seemingly illogical transitions to cross-country travel. Before doing so, we made mention of the general nature of the back road travelers through Arches. Many were young males in tricked out 4X4 rigs speeding and sliding through the deep sand. I made sure tha
We followed a border fenceline from the road down to some sandstone fins where we had to lower down the packs over the lip of a small amphitheater, whose drainage we were now entering. Caron proved herself as an adept rock climber as she descended first and helped me transition down. I think she has much better confidence in her climbing skills than I do. This revelation came at a good time as I sensed she was getting frustrated by my faster hiking pace. The drainage led us out to the western border of the park, where we met a park ranger on a motorcycle. I briefly complained about park vehicle policy in the form of naïve questions and then we slipped over to BLM land to spend the night, exhausted but relieved that we had finally made our start.
Day 2
Monday, April 8
Start: Willow Springs Trail, western NP boundary
End: Dave and Kay’s house, Moab, UT
Nightly low: 48.5 F
Miles: 17.0
We slept nearly 1
1 hours-- talk about needing some R&R! Caron wasn’t hungry (a very strange deviation) so we decided to continue descending the drainage we left last night until we encountered water. As we were slowly funneled into the ever-developing Courthouse Wash, we began encountering ‘pothole water’, but not of the appetizing variety. We got our first taste of negotiating pouroffs-- sudden and often impassable drops in the wash bottoms. Water erosion, although infrequent as an annual occurrence, over time produces sudden but rounded drops. The pouroffs we encountered weren’t very magnificent and were easy to walk around. But they simply pointed out that walking continuously and unimpeded down these desert canyons is not to be expected. The more challenging pouroffs will come later in the next leg, where the canyons are much deeper and the seasonal water flow is heavier. We even experienced mini “slot canyons” in upper Courthouse Wash. The more magnificent varieties are also ahead of us.We ate breakfast where the wash merged with Sevenmile Canyon, which has a strong season
al (quasi-perennial?) flow. This made a big difference in the nature of the canyon bottom, as dependable water sources attract greedy, space-claiming riparian trees and shrubs. I am not a big fan of hacking my way down riparian desert habitats and I think Caron is also now a member of this non-fan club. With no trail and the need to follow the flow downstream, it rapidly became apparent that the best mode of travel is down the creek itself. It is a simple matter to lose the creek if tracking it from the side. Fighting the brush means not keeping a close eye on the meandering creek and it can be lost in short order. Where did it go and where is it going? “Downstream” is not an apparent concept where the elevational differences of merging side canyons are not readily detectable, especially through thick underbrush. A permanent tr
ail would not be possible here because after each year of flash flooding, the slate gets wiped clean. At one point, the stream became braided and we followed an
ill-fated channel that ended in a blind drainage. However, beyond thisemerged a well-worn trail above the flow channel that greatly facilitated movement down the wash. We followed this trail another 7 miles out of the canyon to the southern boundary of Arches, all the while losing and rediscovering our friendly trail countless times.
al (quasi-perennial?) flow. This made a big difference in the nature of the canyon bottom, as dependable water sources attract greedy, space-claiming riparian trees and shrubs. I am not a big fan of hacking my way down riparian desert habitats and I think Caron is also now a member of this non-fan club. With no trail and the need to follow the flow downstream, it rapidly became apparent that the best mode of travel is down the creek itself. It is a simple matter to lose the creek if tracking it from the side. Fighting the brush means not keeping a close eye on the meandering creek and it can be lost in short order. Where did it go and where is it going? “Downstream” is not an apparent concept where the elevational differences of merging side canyons are not readily detectable, especially through thick underbrush. A permanent trill-fated channel that ended in a blind drainage. However, beyond thisemerged a well-worn trail above the flow channel that greatly facilitated movement down the wash. We followed this trail another 7 miles out of the canyon to the southern boundary of Arches, all the while losing and rediscovering our friendly trail countless times.
Although we felt like this passage had kicked our butts, we emerged with a sense that we had been initiated, with mercy, to the unique
Hayduke Trail Canyon Count:
1. Courthouse Wash
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