Trip Stats:
Distance:  7.7 miles one way.
Elevation gain:  4,800 feet.  Elevation at trailhead = ~7,100 feet, summit = 11,913 feet
Location:  Main crest of the Pioneer Mountain Range northeast of Ketchum, Idaho.  UTM:  11T  070003 E  4850760 N
Maps:  USGS 7.5 min topos  Phi Kappa Mountain, Hyndman Peak.
Difficulty:  Class 3 (Climbing using hands to propel up boulders).  First 3 miles moderate hike, last 1.5 miles is a very strenuous hike/climb of 2,000 feet.
Hike directions - south slopes:  1.  Hike FST-165 for 3 miles north along North Fork of Hyndman Creek to intersection with trail that turns left (west) to Pioneer Cabin.  The trail to Goat Mountain continues straight and had branches across its entrance.  2.  View opens to a valley with pointed Handwerk Peak on the horizon, continue ~ .7 miles to confluence of N. Fork of Hyndman Creek and the unnamed creek (~8,800 feet) that flows out from basin between Handwerk Peak and Duncan Ridge.  3.  At the large white cliffs, hike through the gully that separates the cliffs to a shelf above the cliffs, heading in a northeast direction to the right of Handwerk Peak.  4.   Stay to the left (west) side of unnamed creek toward base of Handwerk Peak.  5.  We crossed this creek when we saw open meadow to the east, then followed the meadow past the base of Handwerk Peak on its south side.  6.  Head toward large granite rock fin on horizon ("Florian's Nudl").  Goat Mountain is located to the left of this.  Boulder field is large but stable.  When viewing boulder field, the route leading around the east side with more grassy areas may be less technical than straight up boulder wall.  7.  Terrain becomes less steep; hike to the north (left) of Florian's Nudl to the steep climb of Goat Mountain.
Driving directions:  From ID-75 4 miles south of Ketchum, turn east onto East Fork Road.  Trailhead for Goat Mountain hike is 11.2 miles from this turn.   Travel 5.2 miles on paved road to Triumph:  from this town it is 6 miles to trailhead.  Road forks 1.3 miles after Triumph:  stay on Road 203 (taking left turn) toward Hyndman campground and North Fork Hyndman Creek.  At 10.1 miles, see sign "Road Closed 1 Mile".  Drive ~ 1.0 more mile to parking for Hyndman Peak trailhead.  Continue through this ~ 0.1 more mile to a second grassy parking area for trailhead leading to Pioneer Cabin and Goat Mountain.
Geology:  Pioneer Range Metamorphic Core Complex consists of a lower plate of Precambrian gneisses (2 Ga) and Cretaceous to Early Paleogene granitic rocks, and an upper plate of Paleozoic sedimentary rocks overlain by Challis Volcanics.  When crustal extension started in the west (50 Ma), the Wildhorse detachment fault developed and separated these two plates and Challis Volcanics was part of this extension.  Low-angle faults developed in the upper, brittle layer, removing them, exposing the lower layer of metamorphic rocks (core complex) up to 2.3 billion years old.
CAUTION: Become familiar with this route using a good topo map, as there is no marked trail beyond crossing of North Fork Hyndman Creek at the white cliffs.

When our friends John and Val asked us to climb Goat Mountain with them, we seized the opportunity.  Fred and I usually do these adventures by ourselves, so it was that much more fun to be with fellow climbing enthusiasts, especially since they had been to Goat before, so we could be able to cover the 7.7 miles to the summit expediently.

Ask anyone who has hiked and climbed in the heart of the Pioneer Mountain Range, and you may see their countenance change to a look of knowing bliss and reverence as they tell you about its sheer beauty and wildness.  Granite crags, spires and domes hang raw and exposed over glaciated basins dotted with car-sized boulders and wildflowers in meadow grasses.  Hike to Pioneer Cabin, built high on a bench at 9,400 feet and get a spectacular view of the main Pioneer crest to the east.  The following photo of Pioneer Cabin was taken a few years ago, and now I can say that I have walked up that wide valley to the top of Goat Mountain, the peak situated on the left horizon in this photo.

The weather forecast said it was to rain in the afternoon.  John, Val, Fred and I started on the trail under blue skies and found ourselves pummeled by frigid winds and ice pellets when we got to the summit of Goat Mountain.  Not a fun time to take photos, however it adds excitement to the trip and knowing that not many people get to experience the sudden advancing of fall and winter in mid-September at nearly 12,000 feet on a precipice.  We got down the main crest pretty quickly.

The first 3 miles of this hike treks along the west side of North Fork Hyndman Creek with its colorful quartzite boulders and crystal clear water to an intersection with the trail that leads to Pioneer Cabin at 8,200 feet.  Continue straight into the valley ahead, walking over branches placed across the trail to steer Pioneer Cabin hikers to the trail that takes off to the left.  The pointy, fang-like Handwerk Peak appears as you walk through a sagebrush and bunchgrass valley to a crossing of the North Fork Hyndman Creek, another 0.6 miles past the intersection.  Then, climb through the white cliffs, through an obvious gulley that separates the cliffs to a shelf above.  Stay to the left (west) of the creek whose water sources from the unnamed basin between Handwerk Peak and Duncan Ridge.  Our party accessed this basin two different ways:  Val, Fred and I hiked the west side of the creek to near the base of Handwerk Peak.  John crossed the creek earlier and ended up waiting for us further up this grass-filled basin south of Handwerk.

We crossed the narrow stream at the bottom of the basin and walked through tall bunch grasses at first, and then short grass as we neared the cirque wall at the end of the basin.  Aim for Florian's Nudl, a fin-shaped dome on the ridge above the cirque.  Goat Mountain is the prominence to the left on the ridgeline.

The walk through this basin is a sensory experience of contrasts.  Native, aromatic grasses are soft and quiet underfoot, like a huge gold carpet while the cold, ragged mess of walls and boulders looms ahead, sweeping down both sides in a U-shaped curve, typical morphology of glaciation.  At the end, you run out of grass, except for a few patches distributed among the boulders.  We went straight up the steep boulder wall in front of us, and came down the more circuitous route that contains more grassy areas to the right side (east) in the cirque.  A huge boulder with a white "X" across its face lies at the entrance to the boulder field.  Next time I do this climb, I will find this boulder and go up to the right; this route descending seemed longer but less steep.  It's  hands-on boulder climbing either way.

The boulder-hopping was stable; rarely did I step onto a "tippy" rock.  John practically ran up the rocks, while the three of us followed, grasping onto the granite and grass to hoist up.  During the long climb, the skies became darker, and when we finally reached the top, we were assaulted by stinging ice crystals and a brisk, frigid wind.  What timing!  Snap a few photos, look at the squalls of rain around us, try to maintain our balance on the top of a narrow Pioneer Range ridge with 1,000-foot drops on both sides.  Celebrate the breathtaking (literally!) 360-degree scene; commit to memory.  And then get down.  Goat Mountain has a double peak - we didn't get to the second (north) prominence which is slightly higher.

John went down the direct steep face.  Fred, Val, and I hiked toward the east side of the cirque.  Descending down a gully near a sheer wall, we heard water rushing under rocks and I suddenly saw something white.  A mountain goat stood calmly watching us at the bottom.  We stopped and stared at each other.  It posed for us a few minutes, then slowly ambled toward the rock wall.  It looked like it was growing its winter coat.  We joked that the goat was taking note of humans' relative incoordination while traversing rocks.  We had seen mountain goat hair in the tundra grasses on the way up the mountain.

We met up with John at the bottom of the boulder field.  A refreshing, cool rain onto the bunch grasses made a clean, earthy scented air, which I breathed in deeply.  Tall grey walls rose on either side.  Occasional large boulders sat solitary and we took a short break on the lee side of a large one.  Probably dropped out of the receding glacier.  We resumed descending the basin and when I turned back to see the cirque and the ridge, curtains of rain covered most of the view.  In our chatting, we didn't pay attention to staying close to the stream drainage and got too far to the west, so we took some extra time route-finding, thrashing through brush, navigating more boulders, and crossing streams to get back to the trail.  

A gentle rain cooled us the last two miles of the hike.  In the cloud-covered dusk, we saw two bow hunters emerge from the woods in camouflage.  The sky on the horizon was clearing.  We raised a toast to our awesome 11-hour day with the excellent beer at the Power House in Hailey.  We celebrated getting to the summit together in a spectacular mountain range where we saw no one else on the trail.  We celebrated the fact that we are lucky to be able to see things that most people don't, and that our bodies are able to take us there.  

References:
Appearance of the Mountain Goat.  Website by the British Columbia Mountain Goat Society, copyright Smithers BC Canada.
​
A Brief History - Pioneer Cabin.

Digital Geology of Idaho - Idaho Basement Rocks  -  Idaho State University.

Lopez, Tom.  2000.  Idaho - A Climbing Guide:  Climbs, Scrambles and Hikes.  The Mountaineers Books, Seattle, WA.

Metamorphic Core Complexes - Idaho Museum of Mining and Geology.

Related:
No Mans Mesa in Grand Staircase-Escalante NM

Our Adventure
It was the vivid colors in Death Hollow that I remember most when Fred and I hiked the Boulder Mail Trail 18 years ago.  Bright blue skies, red rounded rocks, orange and yellow cut walls, verdant willows:  the whole scene reminded me of the hues on the art class color wheel.  We saw only two other people on the trail that day - two guys swimming and splashing joyfully under steep walls.  So extraordinarily different this hollow was from other streams I had hiked before whose colors, albeit beautiful, are usually various shades of brown, grey and green.  Here, in the middle of an immense sandstone sea, we had color combinations only the desert can produce. 

On a very warm day in June this year, Fred and I hiked this trail again.  The sandstone wall of Death Hollow as the Boulder Mail Trail enters it from the north is bright yellow and grey.  I wondered if that rock surface could really be that colorful, and checked the colors of vegetation in the images I was taking.  Maybe it was a reflection of the sun?  Sandstones can be yellow due to dissolving of calcium carbonate, a common cementing material.  The grey vertical stripes looked like weathering stains to me.

These days, the Boulder Mail Trail trailhead is generously marked.   The first 1.5 miles trek steadily down a bench through a pinyon/juniper/sagebrush forest.  Views suddenly open up as the trail drops down into sandstone hills and gulches of the Sand Creek tributaries.  Rock cairns mark the trail for the remaining trek to Death Hollow (and then on to Escalante), except for a few sandy stretches where the trail is marked initially by a cairn.

The trail zig-zags through a sandy opening of a shelf of eroded orange sandstone layers and deposits you onto the immense slickrock.  As you leave the plateau behind, two and even three cairns can be seen ahead, linking the trail to Sand Creek.  So much to see in such a stark landscape:  grey lichen, aged wood, sand pockets, and water-smoothed channels.

At 2.7 miles, cross Sand Creek, flowing in mid-June.  Walk on right (west) side of creek through willows for ~ 0.2 - 0.3 miles to cairns that climb out of creek bottom and briefly switchback over a knob.  We had to backtrack here because we followed the creek too closely to the shore.  The climb from Sand Creek to the highest point on Slickrock Saddle is ~ 500 feet.  The initial climb out of the creek is steep, then alternates between less steep and steep rises (see profile chart, above), trekking around the northwest side of a large dome with hoodoos on top.

Telephone wire installed 108 years ago runs along the trail as it treks through long stretches of deep sand in a pinyon/juniper forest.  This segment leads to the summit of Slickrock Saddle Bench at 6,600 feet and the first view of Death Hollow.

As you make your way off  Slickrock Saddle Bench, the shadowy chasm of Death Hollow becomes deeper and deeper; you know it's there, but it just won't reveal itself right away.  It's tempting to stare in awe at this unique sight, but stay focused on the cairns, too, because the trail swings south and skirts around a knob at 6,617 feet, heading for the best way off the bench.  Next, the trail switchbacks and treks in a northwest direction.  The steepest part lies ahead, and you wonder how mules delivering mail in the early 1900's walked across this precarious descent.  A passage from the book "Advised them to Call the Place Escalante" reads:

​This trail was known in the early 1900's as the Death Hollow Trail, and it was the shortest route between Boulder and Escalante.  It was the fastest route if one was in a hurry, for the wagon road between the towns was a longer distance.  Parts of this trail were "blasted out" in order for safe horse passage.  Tales of cream cans and eggs being delivered via the Death Hollow Trail among other trail experiences are described in Jerry Roundy's book.  The residents of Boulder and Escalante finally received the mail service they had been petitioning for in 1902 when the first government mail carrier's contract was given to an Escalante resident, who would deliver mail using the Death Hollow Trail twice per week.

I'm more aware of my balance on the steep slickrock; most of the texture of the rock enables my boots to grip well, but there are smoother patches to look out for.  I imagine what it was like to lead horses and mules over this section.  Did they slip?  During the winter was there ice?  What would this place look like with several inches of snow?  Or under a full moon?  I believe the Death Hollow Trail mail carriers were pretty tough, and they got to see some of the most beautiful scenery in the world.

Starting at ~ 5.25 miles, the well-marked trail switchbacks and descends 600 feet in 3/4 of a mile to the thick vegetation of the flowing creek in Death Hollow.  Some moss-covered rocks were slippery to step onto.  There's a sweet tent spot at the terminus, and from the paths seen on the treeless part of the shore on the descent, there are probably more tent spaces available.

This time we didn't hike down Death Hollow as we did 18 years ago, although the water would have cooled us off in the mid-80's temperature.  Vegetation along water seemed thicker this time, but the colors and textures no less beautiful.  The cool shade, chatter of water over rocks, sudden splash of colors and tall vertical walls in Death Hollow contrast with the bright and open, mostly shadeless trek across sandstone country.

After resting in the shade, we started the 6-mile hike back, looking forward to the largest elevation gain of the trip - 1,450 feet. On the way back, we took a break at Sand Creek, near huge rounded basalt boulders, probably from Boulder Mountain, whose basalt age is 6 - 16 Ma, and whose run-off streams  provide water for Sand Creek.

There's always numerous adventures awaiting me, and seeing Fred walk across the slickrock is even more fulfilling than the hike, which is hard to beat.  One of the best parts of life is the hope of future adventures in the beautiful American West.  Next time -  the entire Boulder Mail Trail!

Two days earlier, Fred and I hiked from Escalante to Mamie Creek along the Boulder Mail Trail (the southern portion).  Although we didn't get all the way to Death Hollow, I feel that portion of the trail is even more gorgeous.  We had the Phipps Death Hollow Wilderness all to ourselves that day, as we saw no one else.  It's days like these that I will remember reverently - forever. 

Below are some images of the portion of the Boulder Mail Trail Cross Country Route south of Death Hollow.

References:

Boggs, S. Jr.  2012.  Principles of Sedimentology and Stratigraphy, Fifth Ed.  Pearson Education, Inc.

​Hackman, R.J., and Wyant, D.G., 1973, Geology, structure, and uranium deposits of the Escalante quadrangle, Utah and Arizona: U.S. Geological Survey, Miscellaneous Geologic Investigations Map I-744, scale 1:250,000.

Parry, W. T. 2016.  Geology of Utah's Mountain, Peaks and Plateaus.  Friesen Press, Victoria, B.C., Canada.  

Roundy, J. C.  2000.  "Advised them to Call the Place Escalante".  Art City Publishing, Springville, Utah.  355 pp.

UtahGeology.com.  http://utahgeology.com/bin/formationdescs.php?fm=fm_navajo.