Donaldson Peak

Elevation: 12,023 ft
Prominence: 323

Idaho 12er

This peak is found on page 278.


Donaldson Peak is located in the Lost River Mountain Range in the Challis National Forest. One of the nine Idaho 12ers, Donaldson Peak is the 8th tallest peak in the State of Idaho. It is an impressive summit with a long approach and a steep, rotten headwall to climb.

I recently climbed the peak a second time. The traditional approach has been via Jones Creek. [page 292 of the Climbing Guide, (B)(10)]  Jones Creek is a rugged, unstable drainage, which seems to change each year as the spring run off and healthy vegetation constantly change the stream bottom and erode the climbers’ trail.

Recently, climbers have established a new approach in the next drainage to the north, which is sometimes referred to as North Fork Jones Creek. Donaldson is most often climbed in conjunction with an ascent of Mount Church.

USGS Topo: Leatherman Peak

Donaldson Peak from Mount Brietenbach.

Donaldson Peak from Mount Brietenbach.


North Fork Jones Creek Approach

This map show the road approach to the North Fork Jones Creek. Follow the Lone Cedar Creek Road to a ranch, turn right and follow the two track to its end.

This map show the road approach to the North Fork Jones Creek. Follow the Lone Cedar Creek Road to a ranch, turn right and follow the two track to its end.

This approach is reached via Lone Cedar Creek Road [page 292 of the Climbing Guide, (B)(9)], also see the track below. From the end of the road, a good trail leads toward the mouth of the canyon. Once in the canyon, the trail tread is marked and, for the most part, easy to follow. Occasionally, the trail crosses the intermittent stream and at these spots you might need to look for a cairn to get back on the tread. Once you get above treeline, the choice which way to proceed is up to you. The route to the pond at the base of the headwall is obvious.

The lower sections of the North Fork Jones Creek are covered by a thick forest. As you ascend the drainage opens up and and the trees thin out. The tread is good most of the way.

Mark Jones and Dan Paulson are simply running up the trail on an early October morning.

 

The lower sections of the North Fork Jones Creek are covered by a thick forest. As you ascend, the drainage opens up and and the trees thin out. The tread is good most of the way.

Above treeline you will find giant talus slopes to ascend. You can find good footing most of the way on these slopes and any number of lines to climb to the tarn at the base of the headwall.

Giant talus slopes on the way to Donaldson.

 

 

 

Above treeline, you will find giant talus slopes to ascend. You can find good footing most of the way on these slopes and any number of lines to climb to the tarn at the base of the headwall.

After climbing over the talus or up a steep and usually dry waterfall you will reach this pond. A good place to take a break. There are two lines that will lead up to the Church-Donaldson Col from this point.

This pond is a good point to take a break.

 

 

 

After climbing over the talus and up a steep and usually dry waterfall, you will reach this pond. This is a good place to take a break, fuel up, and observe the next part of the climb, the headwall.

The headwall is a formidable looking collection of cliffs and talus shoots from the pond. However, from the pond, there are two good lines that lead through the headwall features to the Church-Donaldson ridge.

The traditional approach is shown on the left, in blue. This route climbs a steep talus pile and then follows a rubble covered shelf up and to the right. The approach on the right, shown in red, follows steeper and more exposed ledges. However, both routes meet above the first series of cliffs about mid-way up the headwall.

There are two lines that lead up the lower half of the headwall from the pond. The original line is shown in blue. It climbs a steep talus pile and then follows a rubble covered shelf to up and to the right. The line shown in red follows steeper and more exposed ledges. Both routes meet above the first series of cliffs about half way up the face.

Two approaches that lead up the lower half of the headwall from the pond.

The right hand route climbs talus to the snow patch shown in the prior photo and then climbs this ledge.

The ledge on the red approach.

 

 

The red route climbs talus to the snow patch shown in the prior photo and then climbs this ledge.

From the top of the ledge in the prior photo the route turns a hard left and climbs a ledge that ends at the top of this talus chute.

Talus shoot.

 

 

 

 

From the top of the ledge in the prior photo, the red route turns a hard left and climbs a shorter ledge that ends at the top of this talus chute.

 

This shot is taken from the point the two routes up the lower headwall meet. the route continues up the base of the line where hard rock and talus meet in this photo from lower right to upper left.

The point where the red and blue routes meet.

 

 

 

This photo is taken from the point the two routes up the lower headwall meet. From here, the route continues up the base of the line where hard rock and talus meet in this photo from lower right to upper left.

The head wall get progressively steeper as you near the top. Andrew Chiles Photo

The higher you go, the steeper it gets. Andrew Chiles Photo

When climbing up the upper half of the headwall, you will find several alternative routes. I do not think one is better than the other.

Climbing up the upper half of the headwall. You will find several alternative routes. I do not think one is better than the other.

The upper half of the headwall.

The headwall is steep and loose. Care needs to be taken the entire way.

Steep and loose footing all the way.

 

 

In addition to being steep, the entire headwall is very loose. Care needs to be taken the entire way.

 

Dan Paulson showing a good deal of common sense that I lacked by wearing a helmet.

Dan Paulson showing a good deal of common sense that I lacked by wearing a helmet.

 

 

 

Helmets should be considered a necessity on a lot of Lost River Range peaks, including this one.

 

My choice is to avoid the talus when ever possible. I scrambled up this rock rib for the final pull up to the Church Donaldson ridge.

A more solid rock rib.

 

 

 

 

My choice is to avoid the talus whenever possible. So, I scrambled up this rock rib for the final pull up to the Church Donaldson ridge.

 

 

 

The summit will finally comes into view, and it is close once you reach the ridge top. You will find that you are well above the low spot of the Church Donaldson ridgeline.

The summit finally comes into view and it is close by once you reach the ridge top. You will find that you are well above the low spot of the Church Donaldson ridgeline.

Mount Donaldson summit.


Donaldson Peak is most often climbed via the Church-Donaldson headwall but can also be climbed via the ridges connecting it with its two neighbors, Mount Church and No Regret Peak.

North East Ridge Route, Class 3

Donaldson’s northeast ridge climbs 400 feet of steep terrain from the ridge connecting the peak to No Regret Peak. I descended and then climbed this ridge with Andrew Chiles and Mark Jones while attempting to climb over to No Regret. The ridge is composed of steep slabs, mostly covered with loose scree and it takes a little time to navigate the lower sections.

Climbing the NE ridge of Donaldson. Mark Jones Photo.

Climbing the northeast ridge of Donaldson. Mark Jones Photo.

Return to the Idaho 12ers page

Mountain Range: Lost River Range

Year Climbed: 1987, 2014

First Ascent Information:

  •  
  • Other First Ascent: First Winter ascent via west face and south ridge.
  • Year: 1975
  • Season: Winter
  • Party: W. March and R. Albano

Longitude: -113.70049   Latitude: 44.06401

Photos:

Idaho 12er
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