The right combination of on-trail and off-trail hiking, varying terrain including eroded rock formations and aspen-lined meadows, and light use makes this hike in the Pine Valley Recreation Area a great one for beginner and seasoned hikers alike.
Gardner Peak overlooking Pine Valley, Utah
Location: Dixie National Forest, Pine Valley Ranger District. Trailhead in Pine Valley Recreation Area near town of Pine Valley, north of St. George, Utah.
Distance and Elevation Gain: 9.2 miles round-trip; gain of 2,900' in 4.6 miles to summit. Trailhead elevation = 6,627'. Summit = 9,478'.
Difficulty: Moderate Class 1 on cairned trail, Class 2 off-trail from base of mountain and Class 3 climbing near summit with minimal exposure. Navigation experience necessary through forest leading to peak as there is no trail.
Coordinates: Gardner summit UTM: 12S 282962 E 4141107 N Decimal: 37.391335, -113.451708. Gardner Peak Trail Trailhead: UTM: 0280120 E 4140397N Decimal: 37.38428 -113.48358. WGS84 datum.
Permit: Day hikers parking at trailhead inside Pine Valley Recreation Area do not have to pay a fee at entrance station.
Navigation aids: Trails Illustrated Topo Map - St. George/Pine Valley Mountains #715, AllTrails app, Garmin GPS, USGS 7.5 minute topo - Grass Valley quad.
Date Hiked: September 3, 2021
Considerations: Experience in navigating through forest (no trail) necessary.
Geology: Pine Valley Mountains are remnants of the Pine Valley Laccolith, the largest in the U.S. (See For the Geo-curious below). Radiometric dates show the monzonite porphyry rock was formed 22 million years ago.
History: Robert Gardner, Jr. was one of the original settlers of Pine Valley who helped establish a lumber mill.
Driving Directions: Directions from St. George: Take Highway 18 north for about 24 miles, turn right at the Pine Valley junction (E. Pine Valley Road) and drive 8 miles until you reach a "T" in the road. Turn left and continue for about 1.5 miles. The trailhead is located on the left just after the Pine Valley Recreation Area entrance gate.
For the Geo-curious
A laccolith is a large amount of magma that is injected between layers of rock, causing a dome-shaped mass. In this case, the Pine Valley Laccolith was a final surge of magma that occurred after the initial volcanic vents were shut off, causing the magma to be squeezed and move sideways between the layers of the Claron formation below it and the overlying magma layer. This injection, 22 million years ago, amounted to a 3,000-foot layer of monzonite porphyry, composed mainly of plagioclase and alkali feldspar. This is similar to granite, and when you look at a fresh surface of the rock, you can see the crystals, indicating the rock cooled slowly enough to form large crystals - allowing us to easily see them. The laccolith was uncovered when the volcanic layer above it eroded. The Claron Formation is made of limestone and mudstone; it is the rock that makes the spectacular hoodoos seen in Bryce Canyon National Park.
The Pine Valley Mountain Wilderness, a "sky island" arising among black basalt flows and red sandstone cliffs of southwestern Utah, is the antithesis to the internationally-known Zion National Park seen from its summits. It is a welcome respite for adventurers that have witnessed crowded Zion trails. It doesn't have Zion's spectacular sandstone towers, but it's beautiful forests offer solitude and a large variety of vegetation, including a large stand of virgin Engelmann spruce and many peaceful meadows.
The Gardner Peak hike begins in a valley of sagebrush and rabbit brush, ascends a rocky section, extends across large flat outcrops of smoothly eroded rock, through a meadow lined by a large stand of aspens, and finally ascends steeply through large pines and deadfall to a pointed peak of spruce and Douglas fir. The terrain on this hike is ever-changing. Gardner Peak sits right on the Pine Valley Mountain Wilderness boundary and although its trail may not be officially in the wilderness, it feels like it is because the trail is narrow and lightly used. We were only the second group to sign the summit register for 2021. The trail treks through a small area burned from the 2020 Gardner fire. You will reach 2 false peaks before you get to the summit - a narrow rock perch with a great view to the east and the summit's register hidden under rocks.
Interactive map of our GPS tracks to Gardner Peak
Gardner Peak Trail to base of Gardner Peak
Rabbit brush blooming at trailhead - forested Gardner Peak on the horizon.
View ahead of crags - we used these as a landmark to descend peak; rock cairns (right) mark the trail.
Finding the trail through the Gardner 2020 fire section just before you reach the flat meadow before the peak ascent was challenging. When we reached the flat, black-charred trees were scattered about - even the ground was black - and we lost sight of the next cairn. With the help of AllTrails app, we found our way. Go straight ahead when you reach this section; we went too high onto the bare rock to the right. The trail then descends steeply to cross a dry run-off stream section and continues to Jodes Flat, the small meadow at the base of Gardner Peak.
Short section burned from the 2020 Gardner fire.
It's hard to get bored on this hike because the terrain is constantly changing. After winding between small rock outcrops and large trees, and on pine needle accumulations, the view suddenly opens as you tread across long spans of bare rock with some interesting eroded formations. On the way back, after looking more closely, I found two water catchments or small pools in the rocks.
A look at the peak ahead.
One of the many meadows in Pine Valley Mountains
Base of Gardner Peak to the summit
At 3.8 miles from the trailhead, after the short fire area, reach the small meadow - Jodes Flat - to see the thick forest on the west side of Gardner Peak. This is where the trail ends. We walked straight up this flank for a 900' gain, aiming toward the peak coordinates. There is a lot of deadfall to crawl over and Class 3 climbing through huge rock outcrops toward the top, as well as 2 false summits. The exposed crags that we had passed on the trail just before Jodes Flat could be seen on the way up; they provided a good landmark for our summit descent. The summit is small - basically a few huge pointed boulders with a register with a few entries hidden under rocks. Ours and a Montana couple's were the only entries for 2021.
The summit is mostly forested, but a view to the east looks over a deep canyon. The ascent was short enough so that we had time to relax in the most perfect weather on the summit, enjoying solitude. A forested summit is not as spectacular as a bare, above-treeline perch overlooking huge expanses of terrain, like Leatherman Peak, which we summited in July. But they are still great and each has its own characteristics that stand out in my memory of them. The reward of finding an unseen summit as you keep on seeing more sky as you climb is extraordinary.
Keeping the bare rock outcrop we had passed on the way up in view, and using my GPS trackback, we found our way back to Jodes Flat. The only other hiker we encountered that day was an elderly man making his way up the loose rocky section. We each acknowledged the beautiful day. I hope I will still be hiking at his age - it is a gift to be able to explore the West. So much to see out here, so little time! Keep on exploring!
"Between every two pines is a doorway to a new world."
Yep, there's lots of rocks and trees to navigate when climbing the off-trail portion to the summit!
(900' elevation gain)
Scenes from the top of Gardner Peak
View from Gardner Peak of Pine Valley Mountain Wilderness to the south
The large outcrop near base of peak we used as landmark to descend; rock cairn marks trail after burned section.
Pine Valley celebrating Labor Day
Our GPS track; note extent of 2020 Gardner fire on map. Gardner Peak is on the boundary of Pine Valley Mountain Wilderness Area.
The last section of hike through rock outcrops to the summit.
Miller, R. Our Geological Wonderland: The Pine Valley Mountain Laccolith. The Independent - A Voice for Southern Utah. Feb. 2018.
Pine Valley Day: The story of how 'the most beautiful sight' went from lumber supplier to summer retreat. By Reuben Wadsworth reporting in the St, George News.
Pine Valley Chapel 1868. Informational flyer about the history of Pine Valley and its chapel, available at the Pine Valley Chapel.
Explore this "hidden gem" in the Red Mountain Wilderness; a primitive trail that quickly elevates the traveler from city to a spectacular and peaceful plateau in the southern Utah red rock wilderness.
Utah's Red Rock Country
Mount Kinesava - Zion National Park
Burger Peak: 10,320' - Pine Valley Mountain Wilderness, Utah
On top of Red Mountain overlooking Three Ponds Trail (wash), part of the Padre' Canyon Loop in Snow Canyon State Park.
Overview: Within a few steps of Red Mountain's steep cliffs overlooking the bustling desert cities of Ivins and St. George, Utah, enter a quiet and sublime wilderness of pinyons, junipers and mule deer that is unmarked except for an occasional cairn. The Red Mountain Primitive Trail extends for 11 miles in the Red Mountain Wilderness through saddles crossed by washes and slickrock basins between rocky sandstone spires and crags, with spectacular views of Snow Canyon State Park We hiked this trail's southern 3.5 miles.
Location: Red Cliffs National Conservation Area (BLM) in the Red Mountain Wilderness north of Ivins, Utah. Southern trailhead starts at intersection with Toe Trail, at the north end of North 200 E Street in Ivins. North trailhead is just off Highway 18, 15 miles north of Bluff Road in St. George, north of Snow Canyon State Park.
Distance: We hiked 3.6 miles of the 11-mile trail, out and back for a total of 7.2 miles.
Elevation: Southern trailhead = 3,189': our top point = 4,930'.
Difficulty: Mostly strenuous Class 1 on first 0.8 miles; a short section is Class 3 using hand- and foot-holds to maneuver up rocks with mild-moderate exposure. Once on top, navigation and route-finding on unmarked terrain Class 2.
Lat/Long: Ivins Trailhead (south): 37.1754 -113.6772. Top point of our hike overlooking Snow Canyon: 37.2129 -113.6707. Trail at Ivins descent (top out onto plateau): 37.1842 -113.6783.
Considerations: The first mile from the Ivins trailhead is Class 1 with two short Class 3 maneuvers. Once the trail tops out, there is no marked trail. Experience with navigation and route-finding using a compass/GPS is a strongly recommended after top of Red Mountain is reached. Experience with this terrain and topo maps needed to avoid getting stuck. Dogs must be kept on a leash. A sign at this trailhead reads, "Hazardous, unmaintained route with steep exposed slopes: your safety is your responsibility." Search and rescue operations for lost hikers have occurred.
Water: Plan on packing in your water.
Date Hiked: May 9, 2021.
Maps: Google Maps Interactive map below
Trail Map and Guide for: St. George, Hurricane and Zion NP, Utah - Adventure Maps.net
Santa Clara 7.5 minute topo map (PDF).
BLM Red Mountain Wilderness Map. See maps of our tracks below.
Geology: Red Mountain's lower slopes are from the Kayenta Formation, the oldest rock in Snow Canyon State Park (190 million years). The horizontal sediment layers are made from rivers depositing mudstone, siltstone and sandstone. The upper slopes, cliffs and top of Red Mountain are a great block of Navajo Sandstone that is younger (180 million years), also seen as a major rock unit of Zion National Park. This Navajo Sandstone exhibits large, sweeping cross-bed features - horizontal and dipping layers of ancient sand dunes deposited in a vast eolian (wind carried) dune field. Red Mountain is bounded by the Gunlock Fault on its west side. It merges with an extensive field of 2.4 million - 2,000 year old basalt flows to the northeast. The Gunlock Fault is a normal fault with the down-drop on its west side (See references below).
Desert Tortoise Habitat Conservation and Large Solar Plants
Mojave Desert Tortoise near Toe Trail at base of Red Mountain
Don't get to see these very often - as tortoises can spend as much as 95% of their lives underground in burrows.
The U.S. Fish and Wildlife Service has listed this species as "threatened".
Recent News: The Sierra Club is one of several environmental groups opposing the massive solar plant project, "Gemini", which would cover 14 square miles (the equivalent of 7,000 football fields) with solar panels, northeast of Las Vegas, Nevada, prime desert tortoise habitat. The Interior Department approved the project, stipulating Arevia Power would have to relocate tortoises to a new habitat. "U.S. Fish and Wildlife Service estimates 15,390 tortoises stand to lose nearly 70,000 acres of habitat in solar projects planned for the Southwestern Deserts."
- From The Wall Street Journal, 6/5/2021.
Sunset at Ivins Reservoir - Red Mountain
Snow Canyon State Park
The southern end of Red Mountain
A good example of two different rock units: the older Kayenta Formation deposited in large streams at the bottom, and the Navajo Sandstone vertical cliffs and ancient sand dunes deposited mid-slope and on top by wind-carried sand.
Our Hike (from Ivins trailhead)
It looks impossible to climb, but If you can get up the steep side of Red Mountain and maneuver through its short sandstone cliffs to the dune-like pink-orange sand at the top, you will enter into a beautiful and seldom-visited shrub and woodland ecoregion. Most are satisfied to end their hike in this soft sand to see the cities of Ivins and St. George sprawling 1,400 feet below. Very few venture beyond this onto Red Mountain's long plateau made of washes, spires, wildflowers, pinyon pines, junipers, scrub oak and slick rock basins. This is designated as a "primitive" trail; it is not officially marked. If you want to get some mileage in, you must hike pretty much due north, avoiding deep canyons to the west and east. We found saddles and washes to get us to a large sandstone ridge with a faint trail on top and killer views of Snow Canyon State park to the east, where we stopped for lunch. Occasional boot print paths in the sand go a short distance and then disappear; rock cairn trail markers are few and far between.
What makes this hike exquisite is that it combines vegetation from both the Central Basin and Range to its north and Mojave Basin and Range to its south, creating a great diversity of flora and fauna. This, along with dramatic views witnessed in solitude makes this hike special.
Initial Climb - 1,400 feet in 0.8 miles
The initial climb to the top of Red Mountain from the city of Ivins is nearly 1,400 feet in 0.8 miles. Someone during the past year has expertly placed rebar and other metal posts to hold the fast-eroding slopes in place. Rock cairns mark the initial trail. Fun Class 3 climbing (I say "fun" because there are enough hand-and foot-holds so it's not too scary) is required in two spots mid-mountain to get through its cliff band. The path has a few switchbacks, but mainly climbs straight up. At the top, progress is slowed as you trudge through deep pink sand; then there is suddenly no trail. Junipers, prickly pears, yuccas and manzanita are scattered about in the sand and on sandstone bluffs and ledges.
Rebar holding rocks in place on the steep initial ascent
The trail tops out on ridge overlooking Ivins and Santa Clara, Utah (left), and Class 3 climbing (right).
Class 3 climbing through cliff band
Climb through cliff band: Trail on ridge below
Lots of foot and hand holds
Final climb to top of Red Mountain entry onto its plateau
Journey on top of Red Mountain
At the entry point onto the plateau, it's a good idea to take note of landmarks around you such as mountains - stay oriented. I also take a waypoint on my GPS.
Leaving civilization and steep slopes behind, we entered a colorful and sublime woodland - shrub "ecoregion" filled with manzanita and junipers and started heading north. A high point of sandstone is reached 1/4 mile after entering the plateau, and then a beautiful sandy basin opens up 100 feet below, surrounded with rock piles and small domes. Descend down into the basin through short sandstone steps and shelves, turning from an easterly direction to a northerly direction. This little basin lulls you into it and makes you want to stay and enjoy the complementary colors of sky and sand, of juniper and bright red firecracker penstemon. Once in the basin, we aimed due north for a low, shrub-filled saddle on the horizon; we startled a mule deer that trotted away. We began heading north to this green saddle stretched between red and orange ridges and rock piles.
Trudging up soft sand washes, we tried to stay close to the ridge on the right which had amazing views of Snow Canyon State Park's basalt flows and orange sandstone formations. We could see that by venturing too far to the left, we would run into Red Mountain's west cliffs. A slight movement in a shrub alerted us, and then a snake's head poked out. We stood and let it cross the wash in front of us as it gave a cursory rattle; it didn't appear too threatened.
Navigating through unmarked wilderness takes more time than following an established trail, as we check topo map and compass a few times. It was not too difficult in this case because the "trail" heads north. The trick is to avoid getting sucked into cliff walls and canyons on the west and find the best way around high points on the east. It's satisfying to be able to figure out a way through unmarked territory, to become more wary of the terrain and to know chances are that where your boot falls, no other has fallen before.
Within 0.25 miles of arriving at top of Red Mountain, reach a rim of weathered sandstone encircling a small sandy basin - head left through basin up saddle to the north.
Pine Valley Mountain Wilderness on horizon to the northeast (Burger Peak, 10,320').
After topping off on plateau, reach this sandy basin surrounded by sandstone
On the east side of the sandy basin reached shortly after topping off onto Red Mountain. Aim toward the light-green shrub covered saddle on the horizon.
Cryptobiotic (biological) soil crusts, made of cyanobacteria, lichens and mosses. These form on easily eroded soils and increase stability and help provide more water infiltration and are the dominant source of nitrogen in pinyon-juniper ecosystems. These crusts hold the soil in place. Recovery of crusts that have been destroyed takes at least 45 years.
One of the first views of Snow Canyon State Park from ridge of Red Mountain primitive trail.
Once we ascended the "green" saddle, we stayed to the right, avoiding slickrock basins to the left. We saw a faint trail that ascended through a beautiful steep-sided arroyo and followed it out onto a rocky hillside. This wash had funneled hikers and created a more defined trail at its head, where we negotiated a few rolling rock hills and topped off on the ridge overlooking Snow Canyon State Park where a few faint trails were present. Pinyon pines became more prevalent at we approached 5,000 feet elevation.
A thorough look at Red Mountain Trail's 11-mile north/south traverse on Google Earth shows that there is no defined trail to follow on its southern end. However, a defined 2-track trail coming from Red Mountain's north trailhead can be seen. We ended our 3.6-mile hike on the ridge overlooking Snow Canyon, with a view of Three Ponds Trail, a sandy wash that is part of the Padre' Canyon loop hike. Looking at Google Earth, I can see that the 2-track coming from the north can be reached through slickrock basins further to the left/west of our route, avoiding some of the high points along the ridge. Future goal: hike the entire 11-mile Red Mountain Trail.
Once over the initial saddle, more washes and shrubs to traverse. Head north through a network of washes and shrubs to rock saddle between two high points on the horizon.
One of the few rock cairns along the way
Finding a route through soft sand
A beautiful example of a Pinyon pine
Pinyon pine - pine nuts were a staple food of Native Americans
Lunch break view of Snow Canyon State Park and Pine Valley Mountain Wilderness on horizon
Basalt flows fill sandstone valleys
Jurassic sand dunes on top of Red Mountain
Turnaround - return to Red Mountain Trail trailhead in Ivins
Our lunch rock was elevated 1,550+ feet above the dramatic terrain of Snow Canyon State Park. The red and white Navajo Sandstone is cross-bedded and vertically jointed - remnants of ancient sand dunes. Water has cut valleys that were filled in much later with black basalt flows from the northeast. Looking to the northeast horizon, we could see Burger Peak in the Pine Valley Mountain Wilderness, elevation over 10,000 feet - a peak we climbed last year. Elevated above the surrounding desert, we had an airy 360-degree view. The sandstone we were sitting on was warm from the day's unobstructed sun.
We used GPS to track back and use a waypoint to reach the sand dunes at the opening of the steep trail onto the plateau, overlapping our ingoing tracks a few times. The sun had warmed the orange-pink fine sand. I watched a fly, or was it a bee, or maybe a "bee-fly" with a long black proboscis collecting nectar from a yellow flower. It kept a connection with the flower as they both swayed back and forth together in the breeze.
In full sun on the west side of Red Mountain, we made it through the Class 3 section, climbing down through the rocks backward and finding enough foot- and hand-holds on grippy sandstone layers. The square houses and street grid of the flat valley below are such a contrast to the irregular and varied shapes on Red Mountain. Back to busy civilization from the serene and beautiful world atop Red Mountain.
An added bonus to this hike: buy a thirst-quenching drink from a turquoise-painted refrigerator with the red words, "Cold Drinks" at the side of the house next to the trailhead. That is among the many things to look forward to on this adventure.
Back to civilization: Descending cliff band of steep side of Red Mountain overlooking Ivins
Cold Drinks at southern trailhead - just deposit 25 cents for water and $1.00 for energy drinks!!
Snow Canyon State Park, Utah
Our hike (red line) on southern portion of the Red Mountain Trail from Ivins, Utah.
Elevation and distance profile of our hike from top point back to trailhead. We gained almost 2,000 feet total in 3.65 miles.
Google Earth image of our GPS tracks from southern Red Mountain trailhead in Ivins, Utah .
Bugden, M. Geology of Snow Canyon State Park
Cryptobiotic Soils: Jayne Belnap. Holding the Place in Place - USGS: Impacts of Climate Change on Life and Ecosystems.
Red Mountain Wilderness Maps - Wilderness Connect
Ecoregions of Utah - usgs.gov
Geologic Map of the St. George and East Part of the Clover Mountains 30' x 60' quadrangles, Washington and Iron Counties, Utah. Biek, R.F., and others. USGS publications.
Miller, R. Our Geological Wonderland: Snow Canyon State Park
Mojave Desert Tortoise - Nevada Fish and Wildlife Service
Reflections on Southern Utah's warm colors and a remedy for the Boise winter blues.
Related: (See Southern Utah Hikes/Bikes category listed on the right)
Zion National Park: Double Arch Alcove Hike
Angels Landing in Zion: Not for the Faint of Heart
Hiking Mt. Kinesava - Zion National Park
Utah Mountain Biking: The Cowbell and The Cryptobionic Highway
Canaan Mountain via Squirrel Canyon
Double Arch Alcove Hike: Zion NP
Boulder Mail Trail to Death Hollow in Grand Staircase-Escalante National Monument
Buckskin Gulch, the longest slot canyon in the southwest
Paria Canyon - Vermilion Cliffs National Monument
In color meaning and symbolism, red is a physical stimulant. It triggers our adrenal gland, causing us to have energy and take action. It makes us more sensitive to our environment and invigorates us. Orange is the color of warmth, vitality, creativity, and it too increases our activity levels and gives us a sharper awareness of our surroundings. It's no wonder Fred and I escape the low-energy and dispassionate grays and browns of wintertime Boise to reinvigorate in Utah's red rock country. Somewhere between Paragonah and Parowan, on our drive southward to St. George and the Zion area, the landscape transforms from hints of pink to to the blazing oranges and reds of Red Mountain Wilderness. Or we travel to Vermilion Cliffs and Grand Staircase-Escalante areas for adventures in chocolate-brown, pink and maroon sandstone canyons. Like bees to flowers, we have found our way to Southern Utah many times over the past 20 years and there's so much yet to see.
If you had to identify one element responsible for the warm colors of Southern Utah, an element that jolts us out of our winter blues and spurs us onto adventure, it would be .....iron.
The Navajo Sandstone exposed in Zion National Park shows off the many colors that iron creates. When iron is exposed to oxygen, it produces varying colors; and these colors depend on what form of iron oxide is present. The accumulated sand grains get coated with iron oxide. Hematite is the iron oxide responsible for the saturated reds. Limonite is responsible for the yellows. It's believed that white sandstone formerly had color but then was "bleached" by ground waters that dissolved iron oxides from the upper heights of the Navajo Sandstone. There's a reason Zion gets over 4 million visitors a year: it has the thickest exposure of the colorful and cross-bedded ancient sand dunes that make up the Navajo Sandstone (2,200 feet).
Zion Canyon from cliffs of Mt. Kinesava
Bridge Mountain mid-horizon, East Temple to the left of it.
Hiking West Rim Trail after a March snowstorm - looking into Zion Canyon at Virgin River
Zion's West Rim Trail after a March snowstorm
Cross bedding of ancient sand dune - Zion National Park
Overlooking Zion Canyon and Virgin River from Cable Mountain
Angels Landing lower left
West Rim Trail - Zion National Park
Emerald Pools - Zion National Park
Zion's East Rim Trail
Portions of this trail now closed due to large rockfall
The color red is pervasive on the Colorado Plateau, a 130,000 square mile province roughly centered on the Four Corners region of Utah, Arizona, New Mexico and Colorado. It's fitting that, when one says "Colorado", one is also saying "the color red" in Spanish. It seems that the Colorado River has had a few names over time, but its name literally describes the red sandstone found in its waters. The Colorado Plateaus Province has 9 national parks, and I am lucky to have hiked or walked in all of them. It also contains 18 national monuments, of which Grand Staircase is my favorite. For our 40th birthdays, Fred and I hiked the Grand Canyon rim to rim and back again the next day; for our 50th birthdays we hiked north rim to south rim. It is an experience never to be forgotten. Rim-to-rim hikers see just about every color of the spectrum in the sediment layers of the 5,000-foot drop and gain in the Grand Canyon, as well as the brown Vishnu Schist - the basement rocks of the Grand Canyon.
The Colorado Plateau Province: South-Southeastern Utah, northeastern Arizona, southwestern Colorado and Northwestern New Mexico. Nearly centered over the "Four Corners" region.
map from nps.gov
Sometime around 2,000 B.C. until 500 A.D., scientists say, nomadic hunter-gatherers from the Desert Archaic culture used red ochre paint to make pictographs of human-like figures onto the sandstone walls of what is now Horseshoe Canyon. It's a long drive for a short hike, but distances don't matter when standing in front of this incredible wall. As we stared at these red, almost eerie-looking figures, a park ranger quietly came up the path to sit on a nearby fallen cottonwood trunk, as he had almost every day to prevent vandalism. More recently, geologists date the rock art panel between 0 A.D. to 1,100 A.D. It has been interpreted as a sacred place for Archaic hunters.
The significant discovery of an old leather bag eroding from sand by visitors in 2005 helped archaeologists piece together a scenario of the Archaic hunter who placed it near the Great Gallery wall. The bag contained three small leather pouches, a water-rounded stone, and marsh-elder seeds. Two of the pouches were stained red by hematite, one of which held chert to make arrowheads; the other probably held pieces of this ore. The seeds were an emergency food cache. The flintknapper/hunter had collected more chert flakes than he needed and was heading southwest to his home. This was an excellent place for him to stash extra hunting tools and food in case of emergency, and an easy landmark to remember and describe to kin. He was walking through a natural travel corridor.
The "Holy Ghost" and the Great Gallery in Horseshoe Canyon
Canyonlands National Park in southeastern Utah
Newspaper Rock - San Juan County, Utah
One of the largest collections of petroglyphs in the country.
Fremont, Ute, and Anasazi Native Americans contributed to this panel. Designs were created by pecking through the desert varnish to the lighter rock beneath.
Mesa Arch at Sunrise - Canyonlands National Park
The best spot to photograph this arch was already taken by a photographer and his tripod at 5:30 a.m.
Still more than enough places for photographs!
Death Hollow in Grand Staircase/Escalante' National Monument
(these are the actual colors - not saturated with Photoshop)
One of the most colorful canyons I have been in
In her book "Red: Passion and Patience in the Desert," Terry Tempest Williams effectively conveys how it feels to be in the red rock country. To read her words is to feel the warm sun, the rough sandstone, and the enormous space in the red rock canyons and mesas. She reflects on its physical and spiritual aspects. She grew up in Utah and is also an educator and environmental activist. The more I visit this beautiful place, the more I can relate to her writings. She reminds us to slow down and really "see" and contemplate the land. If we do that, then we can "hear the voice of our conscience. If we listen to that voice, it asks us to be conscious. And if we become conscious, we choose to live lives of consequence." Another quote from this book:
"Time and space. In the desert there is space. Space is the twin sister of time. If we have open space then we have open time to breathe, to dream, to dare, to play, to pray to move freely, so freely, in a world our minds have forgotten but our bodies remember. Time and space. This partnership is holy. In these redrock canyons, time creates space--an arch, an eye, this blue eye of sky. We remember why we love the desert; it is our tactile response to light, to silence, and to stillness."
Paria Canyon-Vermilion Cliffs Wilderness Area, Northern Arizona - "The Wave" in Coyote Buttes
Coyote Buttes in Paria Canyon-Vermilion Cliffs Wilderness
Only 20 people per day are allowed; we were able to get permits twice during Christmas Holidays before it became so popular!
Petroglyph at confluence of Wire Pass and Buckskin Gulch
Paria Canyon-Vermilion Cliffs Wilderness - Arizona
Paria Canyon-Vermilion Cliffs National Monument
Palmer's Penstemon in Snow Canyon State Park, Utah
Snow Canyon State Park - St. George, Utah
Fred on Upper Muley Twist Trail - Capitol Reef National Park
Off of Burr Road, south of Boulder, Utah
Great views of the Waterpocket Fold, hike through canyons and on top of mesa
Walking through snowmelt from higher up on plateau, but the water wasn't too cold!
Along Taylor Creek on the Double Arch Alcove Hike
Zion National Park Kolob Canyons section
Leaves were all rotating counter-clockwise in this small pond.
National Park Service. Analysis and Dating of the Great Gallery tool and Food Bag.
Natural History Museum of Utah. Bold Figures, Blurred History: The Great Gallery in Horseshoe Canyon.
Weaver, Lance. 2020. What Gives Utah's "Red Rock Country" its Color? Utah Geological Survey.
Colors of the Navajo Sandstone. nps.gov.
sensationalcolor.com. Color Symbolism and the Meaning of Red.
Navajo Sandstone. Utah Geology.com.
Our attempt at a relentless 3,500-foot gain, sections of Class 3-4 climbing, and route-finding journey under cliffs and over ridges make this fabled summit complete with petroglyphs elusive for now. I recommend this tough, extraordinary hike even if you don't intend on summiting. But do your research first.
Utah Mountain Biking: The Cowbell and the Cryptobionic Highway (cryptobiotic crusts)
Angels Landing in Zion: Not for the Faint of Heart
Southern Utah Hiking and Biking in a Pandemic: Zion, Wire Mesa, and Snow Canyon
Canaan Mountain via Squirrel Canyon
Red Mountain Primitive Trail - St. George
Desert Plant photos
East cliff face below Mt. Kinesava. Summit cannot be seen from this vantage point.
Route goes through trees at base of cliffs in shadow, then up to the right following trees to notch. After this, still hundreds of feet climb to summit.
Fred and I decided to hike Mt. Kinesava when we saw it towering over the southern entrance to Zion National Park while riding on the Wire Pass Trail near Springdale, Utah. When we finally had a cool day during a more recent hike/bike vacation, we gave it a try. Even though we didn't make it, this mountain is one of the most memorable I have ever hiked. Majestic Mt. Kinesava remains elusive, invincible, its petroglyphs unreachable, at least to us. A grudge peak.
Kinesava is more than a hike, it's an experience. The view of red and orange cliffs and pinnacles that tower the more you climb, the increasingly spectacular views of Zion Canyon behind you and the ever-shrinking town of Springdale below create a unique "surround-view" experience of being "perched" for hours. Kinesava's refusal to let just anyone walk on her summit may be the reason why Native Americans chose this place to carve petroglyphs on the mesa just above these challenging rock walls. Landmarks in Zion, like Mt. Kinesava and Sinawava are named after Paiute deities.
You have to do your homework for this cross-country hike, but there are few summit reports available. There is a break in the cliff band that surrounds Kinesava's base created by an apparent old landslide where you can enter the terrain that will take you up to the cliffs. You must catch this same entry point on your exit, so a good idea to look back to note where this is by looking at landmarks. Rock cairns mark faint trails, but it seems like you usually find these more often on the way down. Cairns left by previous hikers were helpful in the Class 3-4 sections.
For a more detailed hike description, click on "Trip Stats" above. You have to navigate over three ridges before you get to the base of the sheer walls, where you scramble and climb across narrow sections of the cliff in a horizontal/diagonal direction following the line of trees. Here, the climb is Class 3 (climbing with use of hands) up more or less vertical rocks, making your way to the right along cliff base. Where we reached too much exposure (Class 4), we backtracked to find a safer route. It took us longer than we wanted to navigate through the horizontal band of trees under the pinnacled vertical cliffs. We reached a comfortable platform with a good view of the "catwalk", a very narrow section that must be traversed to gain access to the final climb up the diagonal band of trees to the notch that lands you on the plateau above. This is where we stopped; it looked pretty difficult and we didn't have enough time to summit AND get down (see image below). Once on the plateau, Mt. Kinesava's summit is another 300-400 foot climb. (See our GPS tracks below).
Zion Canyon from east face of Mt. Kinesava
Mt. Kinesava from Chinle Trail (on a different hike)
Looking at east face of Mt. Kinesava in the morning. The summit is just behind the largest prominence, mostly hidden from this view. Gate, 1.1 miles from Chinle Trailhead marks Zion National Park boundary. Chinle trail continues to the left. The route goes up the fan-shaped debris slide through the trees, continuing through trees to right of prominence up to notch.
First set of Ridges just after Zion NP Boundary
Heading cross-country towards 3 main lower ridges. We went up the ridge to the right in the photo.
We ascended the left (west) ridge, and descended the right (middle) ridge on the way back. At the top of the ridge to the right is a trail and the 3 telephone poles at entry through break in cliff band to arrive at plateau above cliff. I would ascend via the right ridge next time.
We had to lose some elevation and side-hill the left ridge into the small canyon. Aim for the telephone wires and 3 large poles on middle ridge saddle just under passage through cliff band.
Small canyon between left and middle ridges. After descending from west, or left ridge into this canyon, it took us right up to saddle with 3 telephone poles.
Aim for three telephone poles at base of trail that goes through cliff break landslide. On our way back down, we stayed on the ridge that these poles are on, to the right of this image (the "middle" ridge).
Rock slide over bottom cliff base is entry/exit onto plateau above. Defined trail here.
Cairn that marks entry from steep second ridge through lower cliffs to plateau above. These white rocks can be seen above to aim for on the way down off the plateau.
Approaching horizontal band of trees under sheer cliffs
Everywhere you look, it's spectacular!
Reached horizontal band of trees for a cliffside lunch - Zion Canyon view.
Fun "passageway" to to get to vertical rocks
Zion Canyon from cliffs of Mt. Kinesava - 6,400 feet
Keep on Exploring - Never Stop Climbing Mountains!
This is where we stopped.
Trail continues through trees on far left, over the "catwalk" and up through trees to notch.
The Way Down
The view of the cliff-hugging narrow "catwalk" and vertical rock towers is intimidating. It's a different feeling entirely as I sit here at my desk writing this post, where I am not facing this astonishing scene of exposed walls and loose rocks to climb - it's easy to think now I can do it. Edward Abbey, in his book Desert Solitaire said that Southern Utah "is the most beautiful place on earth." My words don't do justice when describing what it's like to hike in this extraordinary place, where all natural elements seem to fit almost magically together. The orange and green, the soft sand and the hard cross-bedded rocks, the cliffs and the undulating lowlands and streams. The expansive desert with steep mesas standing like platforms under a wide sky. Places to rest and absorb the views among imposing and rugged terrain. Prickly cacti and slender, waving penstemon.
We caught a defined trail on the way down that took us a bit too far to the west. The most important thing to remember is to aim for the large white boulders on the edge of plateau; it's your exit point to the ridges below.
Hopefully next time I attempt this hike, we will be able to conquer this section, see the petroglyphs on the plateau above, and summit. I already feel lucky to be able to see these sights that not many others have seen before, and to be able to hike with my husband. We have fun! Life is really good.
"Freedom begins between the ears."
- Edward Abbey, environmental advocate and author of Desert Solitaire
Heading off cliffs onto "third ridge". Springdale, Utah below in river bottom with Virgin River
"Our updated trailhead will add 2 hours to the trip, which means that now fewer of you should ever attempt it. DO NOT GET STUCK ON THIS ROUTE IN THE DARK!!!!!"
Our route up (blue) and route down (red)
Bottom of map shows approach to Zion National Park boundary fence via Chinle Trail (Trailhead on Utah State 9 Highway just before Springdale). I recommend using the ridge that the red trail traverses just after fenceline.
Google Earth image of our hike up after crossing Zion NP boundary fence
To avoid losing elevation on the way up, better to take the ridge to the right (east) of the one we took up. This leads up to only break in the cliffs that surround the bottom. Town of Springdale at lower right.
Chesher, Greer K. Zion Canyon: A Storied Land. 2007. The University of Arizona Press.
Quarnstrom, Evan. Zion National Park: Tackling Mt. Kinesava. Website: Evan Quarnstrom: Stories of Travel and Adventure.
The Hiker's Code: Brush Up on Trail Etiquette in Time for Hiking Season. Posted 11/5/19 on Utah.com
Zion: Mt. Kinesava. Favorite Hikes In and Around Zion National Park. zionnational-park.com
When temperatures soar in St. George, Utah, head up to the Pine Valley Mountains to look over Southern Utah and Arizona mountains in a cool, beautiful forest with mature stands of aspens, Mountain Mahogany trees, and plenty of trails and peaks to explore.
Canaan Mountain via Squirrel Canyon
Angels Landing in Zion: Not for the Faint of Heart
Double Arch Alcove Hike - Kolob Canyons in Zion NP
View of southern aspect of Pine Valley Mountains, the largest laccolith in the U.S., from Hurricane, Utah
The highest peak is Signal Peak at 10, 365 feet.
North side of Pine Valley Mountains, from town of Pine Valley, Southern Utah
Forsyth trail passes by large crags
Our Hike: Forsyth Trailhead --> Summit Trail #3021--> spur trail to Burger summit
Many people consider Southern Utah synonymous with slot canyons and colorful cliffs, hoodoos, and mesas. Its famous national parks - Zion, Bryce and Arches are gems with spectacular scenes. Except when the temperatures reach 100 degrees. In a way you could say we were lucky because of the hot temps in St. George - otherwise we might have never discovered the cool Pine Valley Mountain Wilderness, where we summited Burger Peak to see a vast view of the hot desert below.
The Pine Valley Mountains are less than an hour's drive north of St. George, and provide the forested backdrop to the little town of Pine Valley. The drive itself is beautiful, as you pass by a huge cinder cone and gorgeous Snow Canyon State Park. We felt lucky to have "stumbled" onto this wilderness, the second-largest in Utah because of the many trail and peak opportunities. It has the most diverse flora of any Utah mountain range, with ~ 1,000 species identified so far, and numerous meadows. We met a backpacker on a separate hike near Whipple Valley who said he had to go "two meadows over" for his first night. He was doing a loop trip using Summit Trail, which treks 35 miles between entry points at Whipple Valley and Forsyth trailhead, up and along highest Pine Valley Mountains ridge.
The first mile wanders through large stands of mature Mountain Mahogany and Ponderosa Pines. Stream crossings over Forsyth Creek are easy, with low stream flow. This forest is so unique, because it has such a wide variety of trees. Tree dead fall on the first mile attests to destructive bark beetles that have plagued many forests throughout the west. At mile two, the trail steepens and follows Forsyth Creek as the canyon narrows. It climbs steadily for the next 4.5 miles to the peak; we ran into our first snow bank around 9,000 feet. A spur trail heading north from Summit Trail takes you to the peak. The view of Southern Utah from the steep cliffs at this intersection is incredible.
Forsyth Creek video
First mile of Forsyth Trail
This forest is filled with large, towering aspens. I make a mental note to return in the autumn. Many had names and dates carved into their trunks. The carving above has a date of August 24, 1951. The depiction of a mountain range with a moon overhead made this one unique. This is possibly a Basque sheep herder carving or "arborglyph". There are many Basque carvings in the high countries of the west; the sheep herders had a lot of time to pass and many carved not only their names, but also simple scenes of life in the mountains.
Sue on the trail!
Lunch break at small meadow - 4.2 miles in on Summit Trail
The spur trail that leaves Summit trail is easy to spot on the left once you walk past killer views of the desert floor below: Snow Valley, Red Mountain, and Zion National Park. Ponderosa Pines and firs, and steep crags dominate Burger's summit. For all practical purposes, we made it to the summit; we stopped at 10, 240 feet due to deep large snow fields. We savored the smell of pines and cool breezes while we looked down at the baking desert.
Finally get an opening in the forest ~ 5.7 miles into the hike to view vast Southern Utah: St. George, Zion National Park
View of Signal Peak, highest point in Pine Valley Mountains from near Burger Peak's summit
Rock walls to walk between and around at Burger Peak's summit
The 6.4 mile hike back gave us a lot of time to appreciate this beautiful forest with its mature, towering canopy. We had made a trail through the snow that others could follow easily to the summit. We saw only 4 other hikers the whole day. We were so impressed with this wilderness that we hiked to Whipple Valley a few days later.
Pine Valley has an interesting history. It was discovered by Mormon pioneers Gunlock Bill Hamblin, Jacob Hamblin, and Isaac Riddle when they were moving cattle north of Santa Clara for summer grazing. A sawmill to process lumber was erected in 1856. The tall white Pine Valley Chapel stands out as you drive through town. Built in 1868 according to Ebenezer Bryce's plan, it is the oldest meetinghouse in continuous use of the Church of Jesus Christ of Latter Day Saints. Bryce reportedly followed a lost cow later into a beautiful canyon - the now famous Bryce Canyon National Park. He had huge granite boulders placed at the corners of the foundation. Bryce's experience in Scotland as a shipbuilder was the impetus for the well-constructed chapel.
Regrettably, The Pine Valley Heritage Center in town was closed as we finished the hike. We will be back to explore more of this exquisite wilderness. Possibly some snowshoeing in the winter? For now, we head back to the sweltering St. George heat and its red sandstone to look up to the granite crags and cool Pine Valley Mountains.
Break at the intersection sign - done with most of the large snow drifts!
Descending rugged Forsyth Canyon
Pine Valley Chapel
Downloaded from internet: https://www.thisistheplace.org/pine-valley-chapel-rental
Topo map and elevation profile for Burger Peak, Pine Valley Mountain Wilderness, Dixie National Forest, Utah
3,670' elevation gain in 6.4 miles
Town of Pine Valley north, trail heads south
click on map for larger image
Google Earth image of our tracks from Pine Valley (north, or top of image) Utah to (almost) Burger Peak summit via Summit Trail. Deep snow prevented us from getting to true summit.
Pine Valley Mounains - Wikipedia
Exploring Burger Peak via Forsyth Canyon. Don Gilman, September 26, 2018. Southern Utah Now.
Pine Valley Utah Official Home Page - History. pinevalleyutah.org
Pine Valley: More than a Chapel - Church History. history.churchofjesuschrist.org
Pine Valley Chapel brochure from the Church of Jesus Christ of Latter-Day Saints
While many stayed home during COVID-19 isolation orders, we ventured to Southern Utah for an unplanned visit to quiet Zion National Park, a spectacular Wire Mesa mountain bike ride, and Snow Canyon State Park.
Angel's Landing in Zion: Not for the Faint of Heart
Canaan Mountain via Squirrel Canyon
Zion National Park - Double Arch Alcove Hike
Utah Mountain Biking - The Cowbell and the Cryptobionic "Highway"
Snow Canyon State Park near St. George, Utah
Snow Canyon State Park - April 1, 2020
The spring of 2020 will always be remembered as the time of the Coronavirus pandemic. After Fred and I did more research than usual, we managed to get away on our annual Southern Utah trip despite Idaho's order to self-isolate. It states, “The isolation order does not prohibit outdoor activity such as walking, hiking, running or biking, but a safe distance of six feet must be kept between those who do not live in the same household.” Utah’s orders were similar. We are very experienced in the art of social distancing - it comes naturally. This time, however, as we planned our getaway from Boise to sunnier climes, there was a lot more to consider: where could we stay? Could we bring our trailer? Are the Utah state parks and Zion National Park closed? Can we go on trails? Can we go at all?
Visions of red and orange rocks, azure skies and red-blooming cacti outweighed the risks, so off we were, with assurances from the manager at the Marriott Hotel in St. George that we wouldn’t be sent home after the 9-hour drive. We had to leave our tent trailer behind as all parks and campgrounds were closed. Into the truck went hiking boots, bike helmets, backpacks, clothes for a few weather conditions, food and clean bikes. The promise of gear-grinding, rock-hopping, open-air adventures and the freedom to explore awaited us. Just a few more rules this time.
The chilly morning lent crystal crispness to a clear sky; on our bikes, we faced the yellow and rust-red sandstone towers standing like sentinels along the gravel road in Snow Canyon State Park. The occasional CLINK of small rocks hitting my bike, the crunch of gravel under tires and the pleasant “good morning” greetings of couples walking along the road were the only sounds. Breathe deeply that clean desert air. We stash our bikes at the end of the road and walk a small distance up a narrow white ledge-lined canyon, following a sand wash with smoothed boulders. In the shade of a towering wall the temperature cools suddenly. I catch that unmistakable scent that only desert washes can produce – a sweet mixture of mesquite, yucca and sage, and the earthy scent of damp sand underneath.
Snow Canyon State Park is a beautiful place to bike, walk and hike. We like to ride West Canyon Road and then find a high sandstone lookout and scramble up the slickrock for our lunch. This canyon was used by Anasazi and Paiute Indians; more recently, its beautiful ancient sand dunes were featured in Hollywood movies such as Jeremiah Johnson and Butch Cassidy and the Sundance Kid. While looking for lost cattle, Mormon pioneers discovered what is now Snow Canyon in the 1850's. Be sure to check out the black basalt that fills some of these canyons, creating a topographic high due to huge volumes of magma in what were formerly streams.
Current restrictions as of 4/17/20: Governor of Utah's directive entitled "Stay Safe, Stay Home" which prohibits anyone from going to Snow Canyon State Park that does not live in the county in which it resides (Washington County). All users are to be ready to verify residency.
Map of Snow Canyon State Park
The Geology of Snow Canyon State Park
Snow Canyon State Park, Utah
Bridge Mountain on east rim of Zion Canyon
Zion National Park, April 3, 2020
“Sulking indoors for the duration of this crisis is an obnoxious thought”, said Paul Theroux, Wall Street Journal travel writer. In his article addressing the stay-at-home directives, “A Wanderer’s Guide to Staying Home”, he mentions past famous people who wrote from home or nearby, like Emily Dickinson and Henry David Thoreau. He says, “to self-isolate means confinement; for habitual travelers it is something like punishment”; then he concludes that the “ultimate freedom in travel lies in the road trip – setting off in your own car.”
My bare hands stung in the freezing wind blowing through Zion Canyon’s morning half-light as the hulking sandstone giants lining the eastern side shut out the sunlight to the canyon bottom. Fumbling with my camera and tripod, I spent no time looking for gloves, as the light on Bridge Mountain, a massive, cross-bedded ancient sand dune was changing fast. The visitor's center was abandoned, all parking places empty. Part of me felt jubilant that I should have Zion all to myself, to photograph without constraint; the other part felt a slight uneasiness at the absence of people in this place that is visited by four million people each year. The sun now sat on top of Bridge Mountain's ridge; it was time to move on.
We weren't surprised when we saw the sign "Angel's Landing Is Closed." It is probably the most famous hike in Zion, and for good reason; to get to a breathtaking view of Zion Canyon, you hold onto bolted chains much of the way while climbing up a narrow fin of sandstone, walls dropping straight down for hundreds of feet on either side. The sign read, "Violation of this closure may result in a fine of up to $5,000, 6 months in jail, or both." I have seen a line of people waiting to ascend but today it was eerily vacant. We continued past this and walked the West Rim Trail to where plants grow on sandstone walls overlooking Telephone Canyon. When we went to the only open shop we could find to get ice cream afterwards, the employee there told us that Zion National Park was closed just one-half hour ago. We'll always remember this lucky day when under sunny skies and perfect weather, we were able to hike Zion on nearly empty trails. Too bad we couldn't do Angels Landing!
Zion National Park info and map
Indian Paintbrush in Navajo Sandstone
From East Rim Trail looking at the Virgin River, Angels Landing and Cathedral Mountain - Zion National Park
From the Kayenta Trail looking up toward Castle Dome and Mount Majestic - Zion National Park
Angels Landing on the right; Great White Throne on the left - Zion National Park
West Rim Trail - Zion - 10 years ago after a March snowstorm
Emerald Pools Trail - Zion
View of Mount Kinesava from Eagle Crags Trail south of Zion National Park
Wire Mesa Mountain Bike Ride, April 4, 2020
The Wire Mesa loop is a 7.6-mile rock-navigating, killer view single track source of joy. We rode counter clockwise, having prominent Mount Kinesava with its vertical cliffs and other Zion Canyon temples in view until we reached the end of the mesa and the trail contoured to the west. Most of this trail winds in and out of junipers, up and down over forgiving sandstone rocks, close to the mesa's edge. We were surprised at the number of groups of hikers, campers, and bikers practicing their own wilderness social distancing. The steep road up to the mesa from Rockville is best attempted with a 4WD vehicle. Deep tire ruts attested to those who had traveled this clay-soil road probably the week before when there were downpours.
Utah mountain bikers are technically skilled, focused on mapping a route up and over sandstone. We got better at this skill as we rode, but we did end up walking our bikes over many "steep" rocks.
After this ride, we hiked in the Canaan Mountain Wilderness administered by the Bureau of Land Management, near Wire Mesa. We encountered many cheerful hiking families and couples. The BLM's current Coronavirus Advisory states "Please follow recommendations from the CDC and your state and local health authorities before visiting your public lands..."
It will be interesting to find out what directives and orders we must follow for our hiking and back packing trips this summer while we do what we love to do - "natural" social distancing. Meanwhile, the red sand on our bike chains attests to the great adventures we had in Southern Utah.
MTB Project - REI - Wire Mesa Loop Information
Wire Mesa Trail - Mount Kinesava on left, along with temples and mountains in Zion Canyon
A great camp spot on Wire Mesa Trail. Mount Kinesava on left
The art of "social distancing"
Ahhh, that beautiful red clay/sand soil of Southern Utah!
Map of Wire Mesa Trail south of Zion National Park, north of Canaan Mountain Wilderness
Click for larger image
Canaan Mountain, a towering plateau of Navajo Sandstone is a classic southern Utah adventure through red sand, forested canyons and over ancient sand dune slickrock. Located south of Zion National Park, it is wild and beautiful.
Mt. Kinesava - Zion National Park
Double Arch Alcove Hike - Zion National Park
Angels Landing In Zion - Not for the Faint of Heart
Ponderosa Pine and petrified sand dune on plateau below Canaan Mountain
"It is not enough to fight for the land; it is even more important to enjoy it. While you can. While it’s still here. So get out there and hunt and fish and mess around with your friends, ramble out yonder and explore the forests, climb the mountains, bag the peaks, run the rivers, breathe deep of that yet sweet and lucid air, sit quietly for a while and contemplate the precious stillness, the lovely, mysterious, and awesome space."
- Edward Abbey
Driving Directions (from Hurricane, Utah)
Traveling east/southeast on Utah Highway 59, turn left (east) onto Utah Avenue (right before Subway restaurant in 2018) in Hildale. Continue on pavement for ~ 2 miles, then Utah Avenue curves left (north) and becomes Canyon Street. At 2.5 miles from highway 59, turn right onto Water Canyon Road (road becomes dirt). Travel ~ 1 mile to a sign on the right of the road that reads "Squirrel Canyon Trailhead". Trailhead parking is just ahead.
Our route up Squirrel Canyon to lower elevation of Canaan Mountain
We ascended to 6,900 feet; the summit is 7,363 feet
(note: profile illustrates trail starting at our highest point and descending back to trailhead)
Our route up Short Canyon to Squirrel Canyon to summit of Canaan Mountain at 6,900 feet. The highest elevation of the summit is to the left (west) at 7,363 feet
Beginning of trail at Squirrel Canyon Trailhead in foreground, red arrow points to trail that bears right around red bluff on left to go down into Short Creek in ~ 0.5 miles
We became "temporarily bewildered" when we didn't see the continuation of the trail just after the descent into the first wash (see photo above), so we lost some time with a little backtracking. This costs precious time, especially when days are short and the hike to the summit is long. We re-oriented and found the trail continued out of the wash and around the red bluff to the left, on its way to Short Canyon. There are no signs or trail markers until the climb up Squirrel Canyon, as this a wilderness area (an advantage: not many people on the trail!) We would still make Canaan Mountain, but not the highest point on its summit which is a longer hike.
We stayed in Hurricane, Utah for Thanksgiving weekend in an old Zion NP ranger's cabin. Hiking in and near Zion National Park is a great way to celebrate the holidays. I have been hiking in Zion since the early 1990's. We avoided crowds this time by choosing hikes outside of the park. I was very impressed by the Canaan Mountain Wilderness because of its rugged beauty and all of the sandstone features throughout, and the fact that we basically had the place to ourselves. My kind of holiday!
Entrance into Short Creek
Entrance to Squirrel Canyon one mile upstream from this - hike along ATV road on right side of creek
We chose the Squirrel Canyon Trail instead of Water Canyon Trail, another approach to Canaan Mountain because we read that the hike goes through water in Water Canyon and the temps were only in the 30's. I plan on doing this hike again via the Water Canyon approach.
The hike starts by descending through deep orange sand, across a wash, and continues on the orange sand straight ahead. It rounds the red bluff to the left and then drops into Short Creek, ~ 0.5 miles from trailhead. There were a few people riding ATVs on the trails and washes; they looked like they were having fun. The steep canyon walls shaded Short Creek and its huge Cottonwood trees in the morning. This scene looked much different in the afternoon on the way back to the trailhead with the yellow leaves brightly glowing in the direct sunlight streaming through the canyon.
The brief walk up the creek before the trail scrambles up a small bank under a huge grove of Cottonwoods is beautiful. Sand ripples alternating red and black lie under shallow water reflecting the sky. The trail then follows a 4 WD road along the creek, passing by plenty of grey rabbitbrush shrubs whose flower heads glow a cream color in the sun. Patches of white sand are deposited on the bank above the stream, possibly sediment from the white Navajo Sandstone layer further upstream.
The entrance into Squirrel Canyon, about one mile upstream is obvious, as the ATV/hiking trail crosses Short Creek. A wide and relatively flat area at the entrance was covered with autumn leaves. The trail ascends Squirrel via the 4WD road and then a single track trail as the canyon narrows. Oak and maple trees surround and form an autumn canopy of red, brown and green, while green moss and maidenhair ferns dripped water seeping from vertical sandstone walls. The trail transitions from the soft tread of seasons of leaves to hard and angular slabs of sandstone to soft white sand as it emerges from the canyon then tops out on a beautiful plateau underneath The Beehive, an ancient sand dune. In a short distance from emerging, the canyon trail intersects with the Sawmill Trail with a pile of rocks marking this point. As we turned left at this point (west), I glanced back to make sure I wouldn't miss this intersection on the way down.
A somewhat ominous entrance into Squirrel Canyon
The Beehive, elevation 6,476 feet
Seen as Squirrel Canyon Trail opens up onto plateau above canyon
website for climbing The Beehive
Cairns mark route over sandstone while going up Squirrel Canyon
An excellent feature of this hike is that it gains enough elevation to walk through at least two geologic formations. The top of Canaan Mountain consists of the massive Navajo Sandstone which is also observed in the towering walls of Zion National Park. The hike appears to be starting in the red cliffs of the Kayenta Formation (mudstone) that lies below the Navajo Sandstone. The transition I noticed was in leaving the red sands and cliffs behind in Squirrel Canyon and ending up on the white rocks and white sand on the plateau above.
The upper walls of Canaan Mountain are the White Cliffs of Navajo Sandstone, and at the base are the Vermilion Cliffs which can be seen at the trailhead. These cliffs are widespread throughout southern Utah and Northern Arizona. At this location, they face southeast, and in the morning sun the walls are ablaze with intense orange, yellow and red (read more about geology of this area below).
The plateau above the canyon is a wondrous world of layered, cross-bedded, curving cream-colored and orange sandstone, with never-ending examples of eroded Navajo Sandstone features. Huge junipers make you wonder how old they are. Dark and light-striped hoo-doos, domes and platforms in all shapes and sizes are so plentiful - I wished that I was camping up there so I could spend more time looking. Ponderosa pine and juniper contrast against the frozen-in-time deeply angled and curving sand dune cross-beds. The spectacular dark and forested V-shape of the entrance into Water Canyon looms to the south. Time was getting short. We left Sawmill Trail and scrambled up ledges of slickrock to the highest point on the summit north of us, which is not the highest on Canaan Mountain. We found ourselves in yet another world of a flat-topped forested plateau with soft white sand. Only a few hours of daylight left - we had to get back.
Sawmill Trail required close attention because it was marked by cairns sparsely at best, requiring us to "hunt" for the trail sometimes. The trail alternated between soft sand and slickrock, steep in parts. Tire tread from a recent jeep was helpful to navigate the way. With each turn, rise and descent, there is almost an overload of beautiful, stark, weird, unusual sights along with the feeling of elevated space and expanse in every direction.
At this point on Sawmill Trail, the only marker for the trail was these scrapes in the slickrock. It rose steeply over the rocks on this rise
Sawmill Trail weaves in and out of soft sand and cross-bedded Navajo Sandstone
Sand of Sawmill Trail lower left hand corner. We hiked to the right, up to the top
At 6,500 feet with view of the Notch toward the south
Leaves found on Squirrel Canyon floor
Common trees of southern Utah canyons are Canyon Maple, Boxelder, Fremont Cottonwood, Gambel Oak, Shrub Oak.
Ponderosa Pine, Pinyon Pine, Gambel Oak, Manzanita, and Douglas Fir grow on slickrock.
Heading down Squirrel Canyon
Beautiful canyon with bright green moss, clear pools and waterfalls, thick canopy of oak and maple trees
We saw no one else in the canyon and on the slickrock plateau. It was easy to get sidetracked in Squirrel Canyon while getting almost hypnotized by watching oak leaves floating in clear pools that had ripples on the bottom. As we made our way back to the trailhead, on the ATV trail that runs along Short Creek, a large group of young backpackers were plodding towards us in the deep red sand, laughing and smiling, silhouetted by the late afternoon sun. Huge Cottonwoods, strong and rooted along the white-sand bank with leaves glowing yellow lined our way back down Short Creek. These had massive trunks - the vegetation in this area is so robust and healthy. I'm going back - I can see why the party of backpackers looked so joyous! Next time - Water Canyon!
Geology and History
The age of rocks on Canaan Mountain are Lower Jurassic (201 - 174 Ma). It is capped by 1,300-foot cliffs of Navajo Sandstone. The Kayenta Formation underlies the Navajo. The Kayenta is then underlain by the Moenave Formation. The base of the White Cliffs of Canaan Mountain is part of the greater extent of the Vermilion Cliffs, which extend over a large area of Utah and Arizona.
Key to stratigraphic units in above photo: Eroded Navajo Sandstone on cap of Canaan Mountain 1,200 feet thick; Canaan Mountain is ~ 2,000 feet higher than the plain (Jn). Kayenta Formation (Jk), Moenave Formation consisting of the Springdale Sandstone member (Jms), Whitmore Point and Dinosaur Canyon members (Jmwd). (From Geologic Map of the Smithsonian Butte Quadrangle, cited below).
Temps in the 20's at night at ~ 6,200 feet in late November
Sawmill Trail treks through sand and sandstone
Cairns mark first trail off of Sawmill Trail that treks to the lower reaches of Canaan Mountain summit
Pool in Squirrel Canyon
Along Short Creek
Hike the remote cross-country route of the last mule U.S. mail delivery in the Phipps Death Hollow Wilderness Study Area through slickrock sandstone and sagebrush flats
Descending into Death Hollow from northern route of Old Boulder Mail Trail Cross Country Route
"If ever monuments are erected to unsung heroes, probably the tallest should be for those who brought the mail."
- Nethella Woolsey, Escalante historian
Northern section of Old Boulder Mail Trail Cross Country Route travels southwest from trailhead near Boulder Landing Strip to Death Hollow. This trail descends to Sand Creek, climbs to Slickrock Saddle, then descends again to Death Hollow.
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.
Death Hollow where Boulder Mail Trail enters from the north
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.
Boulder Mail Trail trailhead sign and register
Nearing transition from plateau to shallow Navajo Sandstone canyon. Look at that marvelous open country in the distance that we get to walk through!
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.
You never know what you may find on slickrock
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.
Telephone line installed in 1910 runs along trail - insulators attached to trees like this one above in a dead Ponderosa Pine
First view of Death Hollow from top of Slickrock Saddle Bench - last bit of sand hiking in foreground
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:
"To a reader sitting in a comfortable arm chair it is hard to describe the beauty of the Death Hollow Trail or the fear caused while sitting astride a horse trying to make its way safely over the rough terrain. It is said that horses' legs literally quivered as they gingerly picked their way down the trail."
- Jerry C. Roundy, Escalante resident and author of "Advised them to Call the Place Escalante"
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.
We ran into a retired biologist who took this photo of us after a detailed discussion of Fe+3, ferric iron in the rocks - very interesting to me, but Fred not so much!
Thank goodness for cairns!
Slickrock Saddle Bench
Basalt boulders near Sand Creek
Images from south portion of Boulder Mail Trail Cross Country Route - Escalante to Mamie Creek
Prickly pear near junction of Pine Creek and Old Boulder Mail Trail
Heading up to Antone Flat
South end of Boulder Mail Trail from Escalante trailhead
Trail goes to the left of large drainage and then treks to the right in this photo on the smooth portion at the base of plateau
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.
A unique opportunity to see a near-relict, pristine desert ecosystem on the most inaccessible mesa in Grand Staircase - Escalante National Monument: No Mans Mesa, accessed from Lick Wash trail is solitary, remote, and undisturbed.
View of Park Wash and Navajo sandstone cliffs from rock fan of No Mans Mesa
This hike follows the 4-WD road to the right of wash
"In sublimity - the superlative degree of beauty -
what land can equal the desert?"
- John C. Van Dyke
Lick Wash Trailhead sign 18 miles down Skutumpah Road; large ponderosa pine and Navajo Sandstone walls ~ 1/2 mile down Lick Wash
Hike elevation profile - Lick Wash trailhead to top of No Mans Mesa
Route travels southeast down Lick Wash, then meets with Park Wash to travel northeast to northern tip of No Mans Mesa
Entrance into Lick Wash, shortly after trailhead
Towering sandstone walls dominate on the first mile of Lick Wash hike
I was excited to get to the top of No Mans Mesa, since I do field work surveying ecological sites, work on conservation of a rare plant, and volunteer for habitat restoration. Fred and I had attempted to hike to this mesa 3 years ago, but the condition of Skutumpah Road was too risky after a few rainstorms.
At a bend in Lick Wash about 2.5 miles from the trailhead, after steep walls had given way to a wider, less-constrained channel, Fred and I got our first view of No Mans Mesa. It's long length and towering 1,200-foot white walls were just emerging from morning shadows. Like a fortress it stood, looking impenetrable, at least to this first view. There's a small passage, however that climbs through the walls to the top, and we were hoping to find it. The next goal for this journey was to find the intersection of Lick Wash and Park Wash, and locate the trail that would take us past the LeFevre line cabin, through the sagebrush flat of Park Wash, then to the bottom of the rock debris fan located on the north side of No Mans Mesa in Grand Staircase-Escalante National Monument.
We had driven 18 miles down Skutumpah Road to the Lick Wash trailhead and hiked the wash in a southeastward direction. I was prepared with the excellent hiking route directions from the website Earthline: The American West. Sure enough, at 4.0 miles, we reached the large Park Wash that continues the hike in a northeast direction between the walls of Calf Pasture Point and No Mans Mesa. Massive white Navajo Sandstone walls of Calf Pasture Point kept us in shade but only briefly, then we merged into the blazing sunlight of wide Park Wash, walking on a sandy trail that shortly intersected with an even sandier four-wheel-drive road. What a unique place to be in this remote wilderness! We trudged up the road that parallels the wash to the first shade we could find under a juniper and took a break. It was here that we saw what was unmistakably the rock debris fan that we would have to ascend.
First view of No Mans Mesa 2.5 miles down Lick Wash
View of debris fan (rockslide) on northernmost point of No Mans Mesa from 4-WD road
At 4.5 miles into the hike, we reached the dramatic scene of the LeFevre cabin dwarfed against the bleached Navajo Sandstone overhang of Calf Pasture Point, and tucked under ponderosa pines. At ~ 4.9 miles, trudging in the sand, we passed a fence line, walked a few more minutes and found a defined stock (and human?) trail leading toward the debris slide. We crossed deep Park Wash, wove around sagebrush and found ourselves at the bottom of the debris fan.
The top of the steep cliffs was 800 feet above, and we tried to locate our only passage to the nearly pristine crest of No Mans Mesa. We followed a faint trail and located our first rock cairn trail marker a few hundred feet up the rock slide and after this, the cairns were usually easily seen and numerous enough to follow the trail (June 2018). Back and forth the trail switchbacks to the top of the fan. The transition point from exiting the debris fan to entering the steep cliff walls is a rock "bridge" ~ 20 feet across with a steep and loose gully tumbling down to the right.
LeFevre cabin in Park Wash - 4.5 miles from Lick Wash trailhead
Cairn marking trail up debris fan. Park Wash with trail below
Eroded bedding provides a staircase as you walk on more solid ground. The trail gets steeper and more exposed. Stunning views open up. It appears that in some places sandstone has been chiseled to make the trail, probably by Jepson, the goat herder in 1927. From the wash floor, the cliff walls looked impenetrable - now we were squeezing through the only known passage to the top.
Then suddenly we were taking the first steps into the relict, almost surreal world of No Mans Mesa with its relatively long and flat terrain, nothing but blue sky above. Savoring each step, we took a break in pinyon pine shade near a ledge of burnt orange rock with hints of blue-grey - part of the Carmel Formation. Many wildflowers were in seed. There were no cheatgrass seeds getting stuck in my socks, only open bright sand weaving around healthy bunch grasses and small sand dunes sprouting native Arizona thistle. On a short walk around the top, I found chert debitage, a white rock flake that shows evidence of stone tool-making. Surprised by the presence of sand dunes, I then realized that in fact, Navajo Sandstone was created by deposition of wind-blown sand into large dunes (eolian environment). It was originally red: it was turned to a brilliant white color after reducing fluids dissolved the iron oxide from the grains of the deeply buried sandstone.
Trail shortly after crossing "bridge" between talus of debris fan and entrance into cliff rocks
Nearing top through break in cliff to No Mans Mesa
Trail appears to be chiseled into the rock at a few places
Finally at the top!
View from top of No Mans Mesa of Park Wash and Pink Cliffs
For the Phytocurious
According to the study A Comparison of a near-relict site and a grazed site in a pinyon-juniper community in the Grand Staircase National Monument, Utah, no non-native species were found on the study plots on No Mans Mesa. This study compares vegetation species cover and richness, cryptobiotic crust cover and soil on No Mans Mesa and Deer Spring Point, ~ 2 km southwest of No Mans Mesa. Deer Spring Point is accessed by a road branching from Skutumpah Road and is grazed in the summer by domestic livestock. Characteristics for these two study sites are similar: same geology, elevation, soil, aspect and plant community type.
Major findings comparing plant communities in the grazed site and the non-grazed, near-relict site:
In our short exploration at the top, I was aware of just about every step on that isolated, ecologically "pure" mesa elevated above lands that held invasive plants in this remote wilderness. I felt I was taking steps about 200 years back in time before invasive species were introduced.
Reluctantly, I walked out of that beautiful land and committing to memory what this place looks like. We found our steep entrance and hiked down past the rusty mangled fence that Jepson must have used to keep his goats on the mesa. Still not a cloud in the sky on this mid-June day. White wash and trails curved their way through the dark sagebrush flat 800 feet below us. This time, as we neared the lower section of the debris fan, we veered north and found a less rocky and more sandy descent to the valley floor.
By this time we were hiking in full blazing sun - it was getting pretty darn hot. Pausing to rest under any shade we could find, we bypassed side canyons that would have to wait until next time. At last we reached the cooler narrows of Lick Wash and shed our sweat-soaked shirts for awhile.
I wish I were in the shade of those sandstone walls, sliding my hands over the ancient and eroded beds, hearing the crunch of the purple-hued trail, and smelling the ponderosa pines. We will be back here, but time keeps ticking. A recently retired friend, talking about his planned adventures, said to me, "I don't know if I have enough money, but I sure as hell don't have enough time!"
Lick Wash narrows
Native Arizona thistle
Northern No Mans Mesa
Arizona thistle (Cirsium arizonicum) against Navajo Sandstone
No Mans Mesa
Loamy sand of No Mans Mesa
Making our way down - a few loose rocks
North tip of No Mans Mesa
Ascend left side (northernmost point)
Navajo Sandstone cliffs of Calf Pasture Point
Atkison, Ron. Hiking Grand Staircase-Escalante and the Glen Canyon Region. 1998. Falcon Publishing. pp 288-292.
Gregory, Herbert E. 1951. The Geology and Geography of the Paunsaugunt Region Utah. Geological Survey Professional Paper 226. United States Government Printing Office.
Guenther, D., Stohlgren, Thomas J., Evangelista, P. 2003. A Comparison of a near-relict site and a grazed site in a pinyon-juniper community in the Grand Staircase National Monument, Utah, In book: The Colorado Plateau: cultural, biological and physical research. The University of Arizona Press, pp. 153-162.
Mason, Lamar R., Andrews, Horace M., Carley, James A., Haacke, E. Dwain. 1967. Vegetation and Soils of No Man's Mesa Relict Area, Utah. Journal of Range Management 20: 45-49.
This beautiful hike in the less-visited Kolob Canyons district of Zion National Park packs in a lot of geology, history and glowing sandstone colors for such a short hike.
Double Arch Alcove, Kolob Canyons, Zion National Park
Navajo Sandstone of the Double Arch Alcove - Kolob Canyons - Zion National Park
Taylor Creek Trail to Double Arch Alcove contains a treasure-trove of exposed geologic features in a relatively short distance. In the 450 feet of elevation from trailhead to alcove, the hike passes through three geologic formations. Like most box canyons, the hike starts at the lower, wider part of the canyon and climbs to narrower, higher walls on both sides. The towering wall seen from the north side of the canyon is Tucupit Point, and the wall seen from the south side is Paria Point. The hike ends at the alcove carved into Navajo Sandstone.
Geology aside, you can enjoy the sheer beauty of this hike because of the creek's waterfalls, the pines and junipers, and the colors and patterns on the rock. The Larson homestead cabin, built in 1930, lies at the confluence of the Middle Fork and North Fork of Taylor Creek. The Fife homestead cabin is located further up the trail. Both are preserved well, and you can imagine what it might be like living through cold winter nights in this canyon.
Early morning is the best time to hike along the Middle Fork of Taylor Creek to Double Arch Alcove because of the quality of the light. As the rising sun shines on towering red rock walls along the creek, it reflects an orange glow onto everything in the canyon. I feel like I'm enveloped in a soft light that relaxes me as I hike further. Everything is still, devoid of harsh shadows and colors are vibrant. The orange sand is soft underfoot and the creek crossings don't create an interruption in our stride.
Small pond near creek where leaves were slowly circling together in a counter-clockwise direction
Kanarraville Fold seen in Middle Fork Taylor Creek in the Dinosaur Canyon member of the Moenave Formation
- note chevron structure of folds due to compressional stresses placed on the rock
During the Mesozoic Era, Western North America was in a mountain-building phase with compressional forces due to the Pacific Plate sliding underneath the North American Plate. The rocks of the Kolob Canyons were squeezed, compressed and uplifted. In the Middle Fork Taylor Creek Canyon, this resulted in the Taylor Creek Thrust-Fault Zone and the Kanarraville Fold. The photo above was taken on Thanksgiving 4 years ago when Fred and I first hiked this canyon.
Gray limestone with bivalve fossils probably from the lower Carmel Formation
Gustive Larson Cabin built in 1930
Early Morning in Late November
Taylor Creek - Kolob Canyons
Reflection from Tucupit Point into Middle Fork of Taylor Creek
Middle Fork of Taylor Creek - Kolob Canyons - Zion National Park
Double Arch Alcove
Maidenhair fern on moist sandstone wall
The scenery becomes more intense as you walk up the canyon. Then suddenly a wall of orange and red Navajo sandstone with black mineral stains looms above. The lower arch provides a wide alcove with water seeping from its walls. This is in fact what probably the impetus for the lower arch formation. Ground water seepage weakens and dissolves the cement between sandgrains, breaking down the sandstone. Blocks of sandstone then fall from the arch, accumulating below it only to be carried away by wind and water.
The blind upper arch appears high above the lower arch.
The whole scene is enveloped in a warm orange glow that is a reflection of light from the north canyon wall. The terrain is devoid of footfalls because of the soft orange sand. The green trees contrast with the orange and red. And to have some snow along the way as we did when we hiked this trail on Thanksgiving 2013 was an added bonus.
Yucca in Snow Canyon State Park near St. George, Utah
Biek, R. F., Geologic Trail Guides to Zion National Park, Utah - Kolob Canyon Trails - Middle Fork of Taylor Creek Trail. Utah Geological Survey
Website - "Watching for Rocks - Travels of a Sharp-eyed Geologist". Blog post April 21, 2011
Website - "Zion National Park - Plate Tectonics"
About this blog
Exploration documentaries – "explorumentaries" list trip stats and highlights of each hike or bike ride, often with some interesting history or geology. Years ago, I wrote these for friends and family to let them know what my husband, Fred and I were up to on weekends, and also to showcase the incredible land of the west. I hope to hear about your adventures!
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