The Lost River Range has the grand distinction of being Idaho's highest mountain range. It boasts seven of the nine coveted �Twelver�s�. This rugged range stretches from the Snake River Plain in the south to an area near Challis, for a distance of around 80 miles.

The central part of the range is the very highest, with each end slightly lower in elevation, reaching only into the 11,000 ft range.

Looking Northwest from the summit of Breitenbach. No Regret, Donaldson, Church, Bad Rock, Leatherman, White Cap, Sacajawea, Borah. You will find Corruption off to the right.

Starting from the south, such peaks as King, Jaggle, Sunset and others, tower over the lower Big and Little Lost River Valleys. In the central part of the range you will find the Idaho giants - McCaleb, Lost River, Breitenbach, No Regret, Donaldson, Church, Bad Rock, Leatherman, White Cap, Idaho,Borah,and more. The northern end possesses Dickey, Grouse Creek Mountain and a few other lesser-known peaks. Many many un-named peaks are to be found here. Even some of the very highest are still un-officially named.

The west face of this range is exceptionally steep, with the east side being less so and containing much more in the way of running streams and lakes. Please note that the east side is much more difficult to access, with long rough dirt 4x4 roads being the only way in. The west side is bordered by US Hwy 93. The distances to the �trailheads� are shorter but no less rugged.

The range can be crossed in two places. Pass creek in the southern area and Double Springs in the northern section. Unless the roads are wet a 4x4 is not needed on these two low passes. These scenic routes link with the road connecting Howe and Ellis.

Looking Southeast from the Summit of Breitenbach. Lost River Peak, USGS, Invisible, King. Off to the right are the White Knobs and the southern end of the Pioneers.

Geology

The Lost River range, a fault block mountain range, has incredible vertical relief on the west side. A slightly less steep east side finds foothills, a small number of alpine lakes and several permanent streams.

The range is made up of folded Proterozoic and Paleozoic sedimentary rocks. The Lost River fault runs along the base of the mountains, and has been active over the last few million years. Huge alluvial fans radiate from the steep canyons and spread out over the valley.

Much of the northern end of the range, towards Challis, is covered with "Challis" volcanic rocks, making them very colorful.

The large 1983 7.3 earthquake occurred along the western side of the range causing minimal damage to buildings and only 2 deaths, mainly due to the remoteness of the area.

Conditions

Webcam looking south from Willow Creek Summit, north of Chilly (IDT):

Camping / Lodging

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Other Recreational Opportunities

Images



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