In early October, Helen and I journeyed to southwest Colorado and the San Juan Mountains near Ouray. We embarked on a five-day, four-night backpack along the Dallas Trail, traveling hut to hut. Thus, we carried no sleeping bags or tents to make the load lighter. The fall colors were at their peak and admittedly, this post is more about autumn than the San Juan Volcanic Field.
We had a group of seven and this is near the start of the hike.
Some of the route was along old logging roads.
This is our first hut, called North Pole hut. One of the peaks near here is called North Pole Peak. If you would like to know more about the hut experience you can view San Juan Huts
here.
Each hut comes with a separate outhouse not far from the sleeping hut. These were very clean, modern, and well kept.
A view to the northeast toward the Cimarron Range of the San Juan Mountains. Ridgway Colorado sits in the valley of the Uncompahgre River in the valley below.
The Sneffels Range loomed large to our south as we made our way from west to east. An early season snow made the views dramatic against the changing aspens.
The average elevation of the hike was 10,000 and never deviated from between 11,000 and 9,500 feet.
A wild geranium also was in on the colorful show.
Most of the hike was through forests of aspen and conifer.
Finally, we reached Wilson Summit at 11,000 feet and were rewarded with a spectacular view!
Note the previously glaciated valleys in the distance as we took our lunch at the summit.
There was always a threat of rain during the five days (forecasted) but we managed to avoid precipitation.
In the Ridgway hut on night 3 planning the next days route.
An especially beautiful section of trail on day 4.
Aspens, aspens everywhere.
Burn Hut, our fourth and last hut.
Roots and aspen leaves vie for sunlight.
Approaching our final descent into the Uncompahgre Valley.
Across the way, the San Juan volcanics sit atop a basement of Paleozoic sedimentary rocks. We saw mining shacks at the contact of the two rock types.
Colorful descent - this time in. rocks!
As we descended below the San Juan volcanic rocks, the basement was composed of the Cutler Formation, a Pennsylvanian sandstone, shale and conglomerate that was shed off of the Ancestral Rocky Mountains.
A channel of very coarse conglomerate is set within floodplain mudstone and shale. A very good trip with great people and fantastic weather!
Looks fabulous. Great timing for the aspen!
ReplyDeleteGreat photos - and it sounds like an excellent trip! Thanks!
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