The peak was named for A.D. Wilson, a topographer with the Hayden Survey. He was in the first ascent party, which climbed the peak on September 13, 1874, via the south ridge (a difficult route, not often climbed today).[5]
Climbing
Mount Wilson is ranked among the top ten hardest of the Colorado fourteeners to climb.[6][5] The standard climbing route ascends the North Face from Navajo Basin. Some permanent snowfields exist high in the basin (sometimes termed "Navajo Glacier") and the climb usually involves snow travel, with ice axe and crampons recommended. Scrambling on rock then leads to the summit.
A popular, though long, outing for expert climbers is the mile-long ridge connecting Mount Wilson to El Diente Peak. The ridge is sharp and rocky, and requires difficult scrambling and often a small amount of rappelling.
Incidents
In 2010, experienced climber Peter Topp, was killed in a rockslide and lightning storm while traversing the Mount Wilson traverse to El Diente Peak with a small climbing party. Two other climbers were seriously injured in the accident.[7][8]
In July 2024, 21-year old hiker John James Coffee was fatally injured while traversing the ridge between Wilson Peak and El Diente Peak. Coffee fell over 800 feet to his death and was found after failing to return home from his hike.[9][10]
Geology and history
Mount Wilson, and the rest of the San Miguel Mountains, are made up of a large, irregular tertiaryigneousintrusion.[11]
The Mount Wilson region became the site of intense mining activity, particularly for silver, in the early 1880s. The most famous of these mines was the Silver Pick Mine, which gave its name to Silver Pick Basin, just north of Navajo Basin.
Glaciers and permafrost
Mount Wilson contains four small glaciers on its summit, these being the southernmost modern glaciers in the Rocky Mountains and indeed the most southerly in the contiguous US outside the Sierra Nevada in California. These descend to 3,887 metres (12,753 ft). None of the glaciers have ever been named, and it has never been investigated whether they are presently active.[12] At least nine rock glaciers, composed of alpine permafrost, exist on the northern slope of the mountain, extending down to around 10,000 feet (3,050 m), although the lower limit of permafrost is more typically around 11,500 feet (3,500 m).[13]
During the Pleistocene glaciers were much more extensive than today, covering the whole summit plateau[14] In glaciations previous to the Wisconsinian, it is generally thought that summit ice caps were even more extensive and joined to form the "San Miguel Glacier" with icecaps in the San Juan Mountains.[15]
Climate
Climate data for Mount Wilson 37.8368 N, 107.9914 W, Elevation: 13,606 ft (4,147 m) (1991–2020 normals)
^ abWalter R. Borneman and Lyndon J. Lampert, A Climbing Guide to Colorado's Fourteeners (3rd ed.), Pruett Publishing, 1994, ISBN0-87108-850-9, pp. 231–239.
^Louis W. Dawson, Dawson's Guide to Colorado's Fourteeners, Vol. 2, Blue Clover Press, 1996, ISBN0-9628867-2-6, pp. 160–165.
^See Péwé, Troy L.; "Alpine permafrost in the United States: A Review"; in Arctic and Alpine Research; vol. 15, no. 2 (May 1983); pp. 145–156
^Atwood, Wallace Walter and Mather, Kirtley Fletcher; Physiography and quaternary geology of the San Juan Mountains, Colorado; p. 74
^Atwood and Mather; Physiography and quaternary geology of the San Juan Mountains; p. 72
^"PRISM Climate Group, Oregon State University". PRISM Climate Group, Oregon State University. Retrieved October 10, 2023. To find the table data on the PRISM website, start by clicking Coordinates (under Location); copy Latitude and Longitude figures from top of table; click Zoom to location; click Precipitation, Minimum temp, Mean temp, Maximum temp; click 30-year normals, 1991-2020; click 800m; click Retrieve Time Series button.
