Related:  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 

Our Hike
Fred and I decided to hike Mt. Kinesava when we were riding on the Wire Pass Trail near Springdale, Utah a few months ago and we saw it towering over the southern entrance to Zion National Park.  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 brings 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).

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.

References
​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.

Related:  Canaan Mountain via Squirrel Canyon
                     Angels Landing in Zion:  Not for the Faint of Heart

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.

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.

​

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, it is the oldest meetinghouse in continuous use of the Church of Jesus Christ of Latter Day Saints.  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.  

References
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

​

Related:  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"
​                    Desert Plants

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, filling what used to be a topographic low (stream), but is now a topographic high due to the great volume of the flows.

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

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.  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

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

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.

• Water Canyon Trail is another approach from the south side of Canaan Mountain, trailhead on Water Canyon Road.

Our Adventure
Once in awhile, we spend more time than we would like just trying to find our trail.  It happens to the best of adventurers.  This costs precious time, especially when days are short and the hike to the summit is long.  Fred and I briefly started in the wrong direction, then had to backtrack to the Squirrel Canyon trailhead.  Another look at compass, map, and hike directions to re-orient, then we were on our way, paying close attention to which canyon we were hiking through.  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!

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 and 40's.  There must be neoprene boots for wading up streams.  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.

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.

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.

• Navajo Sandstone:  Very uniform sandstone; 90% of grains are quartz.  Large-scale, high-angle cross-beds are typical of this formation.  It was formed as depositions of sand dunes inland of an Early Jurassic sea.  Major erosion has carved the west-facing cliffs of Canaan Mountain.  Navajo Sandstone is wide-reaching, occurring throughout Utah, northern Arizona and extreme western Colorado.  
• Kayenta Formation:  Reddish-orange mudstone that forms ledges and occurs in the Vermilion Cliffs below the Navajo Sandstone.  Formed by accumulation of sediments from point bars of stream channels.
• Moenave Formation:  Near base of Vermilion Cliffs - the upper member of this formation (Springdale Sandstone) makes reddish-brown, ledgy cliffs.  Sources for this layer were energetic streams flowing across alluvial planes from ancestral Rocky Mountains.  It has low-angle cross-beds.
• Structure:  Locally, there are no major faults.  Regionally, the Hurricane Fault, located ~ 11 miles to the west,  produced a massive displacement, with the west side of the fault dropping, forming the boundary between the Colorado Plateau and Basin and Range Provence.   To the east of this area, the Sevier Fault down-dropped rocks to the west of it.  Joints (fractures) have been mapped on top of Canaan Mountain in Navajo Sandstone.  Origins of these joints have been proposed:  stress fields between faults, domal uplift, and east/west compression of rocks.
• History:  A logging operation occurred between 1915 - 1928.  Remains of a windlass pulley system that brought men and equipment up 1,500 feet to the top of the mountain.  Several million board-feet of lumber were removed.  The mill was relocated to Rockville.

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).

​​References: 

• Moore, D.W. and Sable, Edward G.  Geologic Map of the Smithsonian Butte Quadrangle, Washington County, Utah and Mohave County, Arizona.  2001.  U.S. Geologic Survey.  Retrieved from internet.
• Utah BLM Statewide Wilderness Draft EIS:  Environmental Impact Statement, Vol. 3, Part 1.  1990.  Retrieved from internet.

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.  

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:

• Well-developed cryptobiotic crust cover was 60% less on Deer Spring Point than on No Mans Mesa.
• Significantly more shrub cover on Deer Spring Point compared to No Mans Mesa, however, No Mans Mesa had more shrub diversity.
• Consistently greater total vegetation cover and greater native vegetation cover was found on      Deer Spring Point compared to No Mans Mesa.
• No difference in grass cover, but Muttongrass and Needle-and-Thread grass have twice as much cover on No Mans Mesa as on Deer Spring Point:   composition was different.
• Non-native species were not abundant at either grazed or relict site.
• Researchers did not find considerably more invasive species on the grazed site.

References:

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.

Trip Stats:

• ​Double Arch Alcove lies at the end of the Taylor Creek hike that goes along the Middle Fork of Taylor Creek in the Kolob Canyons section of Zion National Park
• The hike is listed as intermediate: distance is a total of 5 miles in and out  (2.5 miles to reach end)
• Trail head is 2 miles past the Kolob Canyons Visitor Center and Kolob Canyons Road within Zion National Park 
• Geologic features such as Kanarraville Fold and marine fossils in limestone can be seen as well as the Arch Alcove
• This trail traverses the Taylor Creek Thrust-Fault Zone and goes through 3 geologic formations as you climb.  Some of the features are:  Petrified Forest Member of the Chinle Formation, Moenave Formation (including the Kanarraville fold), Kayenta Formation and ending in Navajo Sandstone               
• 2 homestead cabins are located on this trail - both built in 1930
• Early morning light in this box canyon is beautiful due to sun reflections off towering Tucupit and Paria Points that reflect orange light

​

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.

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.  

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.

References:

Biek, R. F., Geologic Trail Guides to Zion National Park, Utah - Kolob Canyon Trails - Middle Fork of Taylor Creek Trail.  Utah Geological Survey
https://www.utahgeology.org/road_logs/uga-29_first_edition/NP_guide/ziontrai.pdf

Website - "Watching for Rocks - Travels of a Sharp-eyed Geologist". Blog post April 21, 2011
http://www.watchingforrocks.com/2011/04/folding-and-faulting-in-kolob-canyons.html

Website - "Zion National Park - Plate Tectonics"
http://zion-gardner-bosch.weebly.com/plate-tectonics.html

Last weekend Fred and I got out of our Boise mountain bike trail comfort zone and rode some Utah trails near Hurricane.  The Boise ride we're used to is a steady gravelly climb up of mostly non-technical trails.  Although this ride was not technical, we found our legs getting adjusted to riding over blocks of limestone and up and down roller-coaster-like arroyos and small hills that ran along the base of towering cliffs and then out into a valley.  These trails were singletrack cruisin' and so fun as to bring a grin to our faces.  Utah bikers must have a "soft tail" or a suspended seat post, we concluded.   But we talked to a few other bikers and they all said they thought their hard tails were actually better.  So, we concluded that our bikes are just fine and we need to get down to Utah for more mountain biking.  The terrain can be challenging and it is so beautiful!

The initial descent down J.E.M. trail that puts you riding alongside a gorge was a little sketchy for me, so I walked a few of the steep switchbacks, while two young and fast kids whizzed past and out of sight (maybe I've seen too many physical therapy patients with broken bones and sprained ligaments as a result of bike crashes!).

It seemed fitting that in a sea of cryptobiotic soil we would be riding on Cryptobionic trail.  We admired the "geology-mindedness" and a play on words that the trail builders provided us.  Cryptobiotic soil crusts consist of soil cyanobacteria, lichens and mosses.  In arid areas,  these crusts help prevent soil erosion, increase water infiltration, and are good sources of fixed carbon.  A large percentage of the soil in this trail system had cryptobiotic crusts.  One source I read said that it takes an estimated minimum of 45 years to for damaged cryptobiotic soil in Southern Utah to be restored if crushed.

The cowbell hanging from a post at the top of Dead Ringer trail is within easy reach as you get to the top.  As we took a break at the top, several bikers hit the bell as they rode past it. The story, we heard is that the cowbell was found on/near a cow skeleton while the trails were being built.  At the cowbell, you can keep going to the trailhead or you can take a left and cruise on More Cowbell trail.  Of course, we opted to keep cruisin' on this great trail that traces the edge of the mesa we had just climbed.

So much to explore in the St. George, Utah area, so little time.  We'll get back on these trails, that's for sure!  Longer loop next time!

​Angels Landing, the summit of a towering slab of orange and yellow Navajo Sandstone rises almost 1,500 feet from the floor of Zion Canyon in Zion National Monument.    At first glance, it looks as if someone took a flat chunk of rock and tilted it up 90 degrees to rest on its side; however, if you study the rock more closely, you can see the relatively horizontal cross-bedding of sand layers that were laid down 180 million years ago.   When you stand at almost the highest elevation in the park, Observation Point, you can look down onto Angels Landing, 700 feet below your boots.  From this vantage point, Angels Landing is a fin of vertical sandstone.  From any vantage point, it seems impossible that there would be a hiking trail to the top, but in fact, people have been hiking Angels Landing since the trail was built in 1926.

Fred and I were fortunate enough to hike Angels Landing the Monday before Thanksgiving.  We were trying to remember how many times each of us had been to the top.  I did my first Angels Landing hike nearly 20 years ago, and Fred the same.  We have done it about 3 or 4 times since, and each time we are reminded what a special and spectacular hike it is.  However, 20 years later, a lot more people know about the trail, and it has become a destination for many a Zion hiker.

At the trailhead, a sign warns hikers of the perils that lie ahead.  The sign reads:  “Since 2004, six people have died falling from the cliffs on this route.  The 1.1 mile round-trip route from Scout Lookout to Angels Landing is a strenuous climb on a narrow ridge over 1,400 feet above the canyon floor.  This route is not recommended during high winds, storms, or if snow or ice is present.”

After hiking a short distance along the Virgin River, the erosive force mostly responsible for the creation of Zion Canyon, the trail ascends steeply up switchbacks to enter Refrigerator Canyon.  I can see how this canyon got its name because even in warmer months, it is still a cool and welcome change from the sun-baked trail below.  While still in this canyon, the next task is to hike up through “Walter’s Wiggles”, named for Zion’s first superintendant, who helped build the trail in 1926.  There are 21 short, very steep, heart-pounding switchbacks.  Upon exiting Refrigerator Canyon and the “wiggles”, the first close-up view of the vertical walls of Angels Landing comes into view.  It is here that your heart pounds for a different reason:  there before you lies a spectacular site of a narrow straight-up trail with lots of people holding onto thick metal chains that have been placed on most of the route.

​Yea!  Look what we get to climb!  This is the turn-around point for many hikers.  
 
The chains drilled into the sandstone make this exposed, dizzying hike much more manageable.  In fact, there was a trail crew working on the chains, replacing some clamps that attached the chains to the poles.  As we waited for them to complete their task, I made sure not to look at the 1,200 foot sheer drop-off just a few feet to my left.

​Oh glorious summit!  The reward is worth the guts, nerves, and courage of the adventurer.  There are about 15 people on the sun-drenched summit, all smiling and taking photos.
 
To the north, the Virgin River snakes through the top of the canyon, and to the south, famous Zion Canyon landmarks can be seen, such as the Great White Throne.

​Zion Canyon is the remnant of ancient sand dunes that covered a huge portion of North America, and formed about 175 million years ago.  It is at Zion that these ancient sand dunes are the greatest thickness. 
 
We head back down, and find many more hikers coming up, and since trail etiquette dictates that uphill hikers have the right of way, we pause a few times to encourage climbers.  At one point, a woman sees what lies ahead of her and wants to turn back, muttering something about just eating lunch.  I tell her that “it’s not as bad as it looks” and she bravely goes on.  Because it’s true, it’s really not as scary as it looks.  We will be back someday.