The Bighorn Crags are described on pages 122 to126 and there is an access map on page 143.
The Bighorn Crags form a distinctive, high-granite divide more than 20 miles in length which towers nearlyh 1,000 feet above the surrounding mountains. The Bighorn Crags offer many excellent challenges to mountaineers and a surprising amount of good rock to challenge rock climbers. The quality of the Crags granite is much like Sawtooth granite: hard and clean in some places, soft and deteriorated in others. Many of the best walls and rock are found down in the canyons rather than on the peaks, which in some cases are still covered by metamorphic overburden. Climbers who come to the Crags should expect to find little in the way of company or conveniences such as established bolts for rappelling.
There are three major rock-climbing areas within the Crags. The first is the “Cathedral’s Cemetery,” which begins 2 miles from Crags CG and occupies an area along the main trail for almost 2 miles to the base of Cathedral Rock. (The domes and spires resemble giant tombstones); I have climbed Peak 9140 and Peak 9100 in this group. Cathedral Rock, of course, resembles a cathedral.) The Cemetery includes 14 spires and domes, which vary considerably in size and shape and offer simple bouldering problems as well as more complicated one- and two-pitch route rock-climbing projects. The second area of interest to rock climbers is a tangled collection of spires, faces, and cliffs at the west end of Ship Island Lake called the Litner Group. Because it is more than 10 miles from the nearest trailhead, little climbing activity has taken place in the Litner Group, but, rest assured, the area has high potential for serious rock climbers. The final area is Fishfin Ridge with its high point called unofficially Knuckle Peak.
Here is a bit of Crag’s climbing history I pulled from the book:
While many mountaineers knew of the Selkirks and Sawtooths, few climbers had ventured beyond these spots. This changed in the mid 1950s when Lincoln Hales and Pete Schoening, two northwest-based mountaineers, discovered the Bighorn Crags in a remote corner of the Salmon River Mountains. Although Hales’ brief article in the 1955 edition of the Mountaineers Journal, titled “Climbing the Big Horn Crags of Idaho,” raised more questions than it answered, the pair were clearly the first to test the Crags’ granite. Hales and Schoening made several first ascents, including their climb of shark-tooth-shaped, misnamed Knuckle Peak, the major climbing prize in the Crags. Hales’ article served as a stimulus for Idaho’s mountaineers to travel to the Crags. Beginning in 1957, a group of climbers centered in Idaho Falls formed the Idaho Alpine Club and adopted the Bighorn Crags as their climbing gym. These climbers, including Bill Echo, Dean Millsap, and Bob Hammer, knocked off all but one of the major rock formations that dot the Bighorn Crags and made many ascents throughout eastern Idaho.
Unfortunately, the Idaho Falls climbers did not leave a written record of their exploits. The area is crossed by a good trail system although it’s a long drive from everywhere to reach the main trailhead.
Below are a few photos mostly snowing the Cemetery area and fishfin ridge. Check out the peak listing for additional photos.
Mountain Range: Eastern Salmon River Mountains