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One of the best petroglyph sites in the Colorado Desert, Corn Springs has rock art dating back 10,000 years and was a major water stop by traveling Chemehuevi, Cahuilla, and Yuma Native Americans. Vision quests may have occurred here.  Trip Stats Location: Colorado Desert section of the Sonoran Desert - Southern California, Chuckwalla Mountains, Corn Springs Wash. What: Bureau of Land Management Corn Springs Campground, at a California palm oasis that was a major occupation site for prehistoric Native Americans. Petroglyphs are on east and west side of the wash. BLM information and interpretive trail guide. Driving: Graded gravel road 10 miles south of CA interstate 10, near Desert Center, east of Joshua Tree NP south entrance (link for driving directions in BLM site above). Coordinates: 33.626046, -115.324935. Geology: The Corn Springs Wash is a strike/slip (transverse) fault, as are many other faults in southern California, including the nearby San Andreas Fault. The petroglyphs are carved into granitic rocks that include dikes of felsic (light-colored rocks), and mafic (dark-colored rocks) that cross-cut them (see photos below). Corn Springs Site scientific inventory: Clewlow, C. Rock Art at CA-RIV-981: Chronology, Imagery, and Function If it wasn't for a petroglyph enthusiast who commented on my post In Search of the Rattlesnake Petroglyph, I might not have known about the fantastic Corn Springs rock art. He gave me good tips about where to find extraordinary petroglyphs and suggested I read the book, A Field Guide to Rock Art Symbols of the Greater Southwest, by Alex Patterson. I'm sure glad he contacted me; it's great to find someone who shares the same passion, curiosity, and appreciation of petroglyphs and the Native Americans' way of life. Fred and I were headed down to our annual Palm Springs, California visit anyway, so we added it to our agenda. Corn Springs is a 1.5-hour drive from Palm Springs, east on I-10, past the entrance to Joshua Tree National Park, near the Salton Sea, and well worth the trip if you are interested in American southwest history. Corn Springs was a reliable water source for Chemehuevi, Cahuilla, and Yuma Native Americans traveling between the Colorado River to the east and coastal areas and the Coachella Valley. Petroglyphs date as far back as 10,000 years, according to the BLM. This ancient trail has been traced to the Mule Mountains near Blythe, California. Steamboat Influences A noteworthy petroglyph appears to be a river paddle-wheel steamboat. My post reader suggested I try to find this petroglyph and sent me an interesting report, "Steamboats on the Colorado River, 1852 - 1916" by Richard E. Lingenfelter. Uncle Sam, a small steam tug was the first of many vessels to run the Colorado River, transporting miners, soldiers, ranchers, and merchants and their tools, supplies and millions of dollars of gold and silver extracted from mines. Native Americans, such as the Yuma and Mojave, depended on Colorado River resources witnessed the invasion of the Gold Rush of 1849. This steam boat mode of transportation caused the change and suppression of these ancient river peoples. Interestingly, the Yumas operated their own ferry at Yuma Crossing. Extensive steam boat travel on the Colorado and its tributaries ceased when the Southern Pacific Railroad completed tracks to Yuma in 1877, providing faster and cheaper shipping of goods. But river commerce still held on after that with the introduction of gas-powered boats and gold dredges. All river trade was finally ended with the damming of the Colorado River. Petroglyph of what may be a Colorado River paddle-wheel steamboat (left) and a drawing of the Explorer on the Colorado River in 1858 (right), from Steamboats of the Colorado River: 1852 - 1916. Vision Quests and Ringing Rocks In my quest to learn more about the Corn Springs petroglyphs, one article or research paper led to another and then another and soon I found myself reading about shamans, hallucinogens, and trance states. Sort of like falling down the Google Scholar rabbit hole. I hadn't intended on writing about suppositions that these petroglyphs are a result of vision quests and that one rock might have been used for acoustics, but it's too interesting and fun to pass up. Unlike Utah rock art with its many representational human- and animal-like forms, Corn Springs petroglyphs are geometric and abstract shapes and patterns that some rock art researchers believe are illustrations of trance-state mental imagery. The realm of neuroscience more formally defines these patterns as "entoptic" (within vision) and phosphenes, which some say is the universal language of the human brain throughout all cultures, since our nervous system has remained the same through human history. Entoptic images are visual effects that originate within the visual processing system anywhere between the eyes and the brain cortex. Certain symbols are common throughout locations all over the world. There seem to be quite a few entoptic images etched in these boulders. Rituals using dance, music, chanting and psychoactive substances to induce trance states where ancestors were visited and wisdom was enhanced may have occurred at Corn Springs. Visions and images were then recorded in the rock etchings. Grid, parallel lines, dots, zigzag lines, nested curves, and filigrees (thin meandering lines) are the six common forms seen in Upper Paleolithic art as a result of drug-induced visions, according to some researchers. Some say that a shaman would act as an intermediary between mortals and the supernatural by gathering power through the spiritual world. I attempted to correlate some of the petroglyphs in my images below to information I found in my search. But we can't assume that we know for sure what the intent was of the people who engraved these petroglyphs. We can only speculate. Some of these symbols may have been made to create communication for a good food harvest or for fertility. These ancient symbols were here long before the advent of formal language (for an interesting book on human relationship to the natural world and language, check out The Spell of the Sensuous: Perception and Language in a More-than-Human World by David Abram).
Common entoptic forms as a result of drug-induced visions as recognized by contemporary researchers. from Altered States: The Origin of Art in Entoptic Phenomena by Eric Pettifor (who adapted from Lewis-Williams and Dowson).  The curvy petroglyph upper left resembles a filigree form (examples on third row of first column in chart above) as does the large petroglyph bottom right that seems to radiate from a central point. A large flat rock, supported by small rocks, protruding from a small recess in the massive granitic outcrop on the west side of Corn Springs Wash amidst the biggest concentration of rock art is said to be a "ringing rock." A horizontal line of pecked marks extends across the top of this rock. "Ringing rocks," when struck with a small hammer-stone produce metallic, ringing, or gong-like sounds. Not much research has been done to understand exactly why some rocks are "ringers." One explanation is that clay minerals on the surface of the rock weather and cause a molecular-level change in the crust, which then increases new internal stresses. I need to go back to Corn Springs to see if that rock will ring, and while I'm there, climb the high summits in the Chuckwallas.  The supposed "ringing rock" is the flat, slanted gray rock in the right of this photo.  Probably a pegmatite dike cutting through granite. One source said that some petroglyphs seem to relate to these dikes. Fault (seismic) activity influences the water table and hence the availability of water for California fan palm trees. The infamous San Andreas Fault, a horizontally-moving fault where North American and Pacific tectonic plates meet extends just southwest of the Chuckwalla mountains. This desert has two personalities: peaceful, quiet and sedate, while at the same time unstable, waiting for its earth to move and shake things up. The Chuckwalla Mountains have an interesting gold mining history from the late 1800's, and in a separate hike in adjacent Orocopia Mountains (Spanish translation: "lots of gold"), Fred and I found what looked like an old miner's dwelling at the top of a long wash (see below), now called "Hotel California." Corn Springs was so named because early white visitors found feral corn plants grown by Native Americans, who at times were able to use the springs for growing food during years when water was abundant. The Love of Deserts: Liberation and Peace Nearby Chuckwalla Mountain and Black Butte, accessed by the historic Bradshaw Trail (now the Bradshaw Trail National Backcountry Byway), are two summits we added to our "to do" list. William Bradshaw built this trail in 1862, the first route across Riverside County, California to the Colorado River; it was used to transport miners to Arizona. "The love of mountains is best," a quote included in my Quotes on Nature page, was inscribed in Greek on one of the Swiss Alps summits in 1558. Perhaps I will inscribe "the love of deserts is best." on a lonely and bare desert summit someday. Corn Springs is a place to find solitude, and recharge if you need breathing space and respite from cities, televisions and smart phones. The desert allows you this: calm (usually), liberation, perspective and peace. "In sublimity - the superlative degree of beauty - what land can equal the desert with its wide plains, grim mountains, and its expanding canopy of sky!" - John C. Van Dyke, The Desert   Huge tamarisk tree at Corn Springs.   Dot images are one of the six common entoptic forms produced when in a trance or during vision quest. Some researchers claim dots indicate corn kernels, stars or rain.  The top figure with horizontal line (sky line) and the six lines descending from (rain) it is thought to be a rain symbol. The slanted lattice is considered to be a basic entoptic (within vision) design.
  The horizontal line with parallel vertical lines under it (lower left) may represent rain. Beautiful dike cutting through granite. Some cool stuff at the site. Chuckwalla lizards have the ability to inflate their lungs to wedge themselves into rock cracks as a defense mechanism against predators, like the red-tailed hawks and coyotes. Native Americans used sticks made from the ironwood trees for retrieving chuckwallas from the cracks. The stick had a spear and hook, so the chuckwalla would be stabbed to deflate the lungs, and then would be pulled out of the crack using the hook.  Fall colors of an ocotillo (Fouquieria splendens) preparing to go dormant for the winter. Yellow and red leaves are caused by a wet summer followed by a slow autumn drying period.  Ocotillo in Orocopia Mountains. The orange and yellow leaves seem to occur when there is more late-season rain than usual.      California fan palms (Washingtonia filifera) at Corn Springs.
  Ocotillos on Orocopia Mountains, a range west of the Chuckwalla Mountains.  "Hotel California" is inscribed on a plaque nailed to this rock house.  "Hotel California", located up long wash in the Orocopia Mountains near Joshua Tree National Park's southern entrance. References
Carter, L. 2021. Ancient rock art and psychedelics.., The language that connects us all. From website: www.roXiva.com. Corn Springs - Wikipedia. Crowell, J., et al. 1979. Tectonics of the Juncture Between the San Andreas Fault System and the Salton Trough, Southeastern California. Dept. of Geological Sciences, University of California - Santa Barbara. Devereux, P. 2008. The Association of Prehistoric Rock Art and Rock Selection with Acoustically Significant Landscape Locations. The Archaeology of Semiotics and the Social Order of Things. BAR International Series #1833. Freers, S. 2018. Simply Scratching the Surface: Petroglyph Chronology in the Colorado Desert. San Diego Rock Art Association. Rock Art Papers, Vol. 19. Gough, G. Sacred Landscape and Native American Rock Art. Lingenfelter, R. 1978. Steamboats on the Colorado River: 1852 - 1916. The University of Arizona Press. Powell, R. 1981. Geologic map of the crystalline basement complex in the southern half of the eastern Transverse Ranges, Southern California: Supplement 1 from "Geology of the Crystalline Basement Complex, Eastern Transverse Ranges, Southern California: Constraints on Regional Tectonic Interpretation". Ringing Rocks and Sonorous Stones. 2020. From website Spooky Geology. https://spookygeology.com/ringing-rocks-and-sonorous-stones/
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We celebrated another Christmas with a sublime, scree-filled desert summit challenge and a Tecopa Hot Springs soak afterward.
Ascending wash to walk between the black hills to the right and the two small hills just to the left of Fred.
Pyramid Peak is black and white - on horizon. Death Valley got its name from a wagon party trapped in the valley in the 1849 California gold rush. One man perished in this hottest place on Earth. One of the travelers was said to have proclaimed, "Goodbye, Death Valley" as they traveled west over the mountains.
Trip Stats for Standard Route (Southeast Ridge)
Location: Amargosa Range, Funeral Mountains high point, Eastern Death Valley National Park. Distance/Elevation Gain: 10.4 miles out and back/3,700'. Trailhead = 3,041'. Summit = 6,703'. Difficulty: moderate - strenuous effort Class 1-2: most time is spent on three major rock/scree slopes. Mostly discernible trail with rock cairns; occasionally requires focus as it becomes faint. Prominence: 3,703'. Coordinates: Trailhead at Hwy 190 = 36.34048, -116.59866. Summit = 36.39196, -116.61228. Maps and Apps: Topo Maps US app, StavIsLost route map, Garmin GPS. Date Hiked: 12/26/22 Directions to trailhead: Park on Highway 190 at an old RV/campground with Pyramid Peak in view. If coming from Death Valley Junction (east), drive ~ 11 miles. If coming from Furnace Creek in the park, drive 17-18 miles. Geology: The ridge hike is a journey through Ordovician-age (450 m.y.a.), heavily faulted limestone and dolomite (Ely Springs dolomite and Pogonip group carbonates). Pyramid Peak summit is Eureka quartzite and Ely Springs dolomite.
Overview
The words "Death Valley" may conjure up images of doom and foreboding, but it's really a land of mystique and fascination, and of extremes. In winter, it's one of the warmest places in the country, making it one of my favorite places to explore. You wouldn't want to be there in the summer, unless you want to experience an average July temperature of 116 degrees. It has the record for the hottest temperature ever recorded on Earth — 134 degrees. Last December, we hiked remote Pahrump Point with spectacular views of Death Valley's Telescope Peak on a cold and windy day, and warmed up in Tecopa Hot Springs Resort's hot springs. This year we "elevated" our summit challenge to hike the lonesome and talus-riddled slopes of Pyramid Peak in the Funeral Mountains, eastern Death Valley National Park. It's listed on the Sierra Club's Desert Peaks section, hence the discernible trail. I break this hike into four parts: a long alluvial fan/wash approach, followed by three steep, loose-rock slopes. Forbidding, massive dark grey limestone greets you at the top of the second loose-rock slope. Pyramid's summit is not in sight until you get up this face and walk around it to the left, where you see more talus slopes under big black spires. From its small quartzite perch, the summit affords a huge view of Death Valley's Panamint range capped by Telescope Peak, and into Nevada. Stunning views surround you the entire ridge climb. Sublime, raw, layered, folded, vast and lonely - the quintessential Mojave Desert.
Our Hike
What more could we ask for? The opportunity, legs and strength to summit a Death Valley peak, the views to remember forever, a natural hot springs soak, and one of the best steak dinners ever - all in the middle of the quiet Mojave.
We're living the dream! Keep on Exploring - it's good for the body, mind and soul!
Healthy creosote bush and lots of hedgehog cactus clumps on the way up this alluvial fan.
Almost at the small hills on the left - the approach continues along the base of these for 2.8 miles from trailhead where it turns NNW into a wide drainage/fan.
At the end of initial alluvial fan climb - taking a left around base of this hill to see large drainage.
Turning left into a major drainage with black rocks at the end of it - then the climb begins!
Finding a trail at the end of the wash that stays on the right side of the drainage to the left.
Trail heads up to the saddle above, with a good amount of loose rock.
Fred making his way up steep and loose rock to saddle (Talus slope #1).
Looking down the first talus slope to the wide wash we had turned into from approach alluvial fan.
Done with the first talus slope! Time for a break - looking back at the highway and valley we have just come up.
There's a few cairns to mark this first slope; afterwards, the trail is mostly discernible. 
Looking ahead to the crazy, rugged mess of rocks we will ascend - glad there is a cairned trail! Pyramid summit behind the ridge. Go straight up the ridge in middle of photo, then bypass the brown-colored scree slope by hiking to its left, up through minor gully (center of photo). Reach the top of this brown rock to ascend the dark grey rock.
Continuing on less-steep portion of southeast ridge in between the steep talus slopes.
Getting through a minor limestone outcrop and looking at the fan we hiked up; walking under the two small hills at the upper left.
Look at that lovely scree field! Trail goes to the left of this, through a small gulley and manageable talus slope, through pink, deep red and yellow rocks.
Getting up and over this sharp limestone, where it flattens out somewhat.
View south from ridge.
This is "Talus slope 2" - photo is taken on the way down. This is on the left of the very steep scree slope.
Upper part of "Talus slope 2". This photo is taken on our way down.
Forbidding sight after topping off on ridge after the second steep talus slope. You can see the trail running in the middle of this, leading to the top of the left prominence, then skirts around it to the left, where you will see Pyramid Peak summit.
Looking back from the black rock ascent to the saddle we just came over and brief flat area.
Working our way up the black rock.
View of Pyramid Peak as trail traverses under left side of ridge walls.
Climbing "Talus slope 3" near the base of the summit.
Trail along left side of ridge near the summit.
Looking back to approach valley and the black "knife" ridge we had passed under.
The beautiful Eureka Quartzite on the summit of Pyramid Peak.
At Pyramid Peak's summit looking toward the east - Amargosa Desert.
Pyramid's summit!
Pyramid's summit looking down on our alluvial fan approach and Highway 190.
From the summit looking east toward the Amargosa Desert and Nevada.
"Amargosa" is the Spanish word for "bitter", describing water in the Amargosa River, which courses through Amargosa Desert. 
On the summit looking toward Furnace Creek wash and Artist's Pallette in Death Valley.
View west of the Panamint Range and Telescope Peak, the highest summit in Death Valley at 11,043'.
The summit of Pahrump Point provides a closer view of Telescope.
Some cool stuff on the trail.
Celebratory rib-eye, beer and wine at Steaks and Beer in Tecopa, California - highly recommended for carnivores!!
Tecopa Hot Springs Resort - Tecopa, CA.
Early morning at Tecopa Hot Springs Resort's bath house.
Our tracks on the ridge portion of the hike to Pyramid Peak. Leaving major wash (lower left) to walk to the end of side wash to begin ridge climb.
Our GPS tracks from parking at old campground on California Highway 190 to summit of Pyramid Peak (CalTopo maps).
Click on map for larger image 
Elevation profile for out-and-back hike gaining 3,700' in 5.2 miles. Hike up alluvial fan/wash for the first three miles.
References
Fridrich, C.J., et al. Preliminary Geologic Map of the Southern Funeral Mountains and Adjacent Ground-Water Discharge Sites, Inyo County, California, and Nye County, Nevada. Geologic Formations. NPS - Death Valley website. McAllister, J. 2009. Geologic Maps and Sections of a Strip from Pyramid Peak to the Southeast End of the Funeral Mountains, Ryan Quadrangle, California
Hike three high points and view the historic Lost Horse Mine along this western Joshua Tree NP trail.
Starting in Quail Wash.
Trip Stats
Overview: Make the Lost Horse Loop hike even more interesting by bagging a few peaks along its route to get a feeling of the vastness of Joshua Tree NP and wilderness, with views of San Jacinto Peak in Palm Springs. Check out the plaque that commemorates Lost Horse Mine stamp mill, one of the best-preserved of its kind in our national park system. Coordinates: Lost Horse Mountain = 33°.56'13.74" N 116°.08'10.01" W.
Navigational aids: Trails Illustrated Joshua Tree National Park #226 map.
Date Hiked: 4/10/22 Geology: The Lost Horse Loop trail and mine is located in granitic quartz biotite gneiss (metamorphic) related to Pinto gneiss age 1.7 billion years ago - some of the oldest rocks in California. Biotite is dark mica mineral. The Lost Horse Mountains are one of only three occurrences of basalt in Joshua Tree NP.
Cattle rustlers and Gold Mining in Lost Horse Valley
If you were a cattle rustler in the 1870's southwest, you would look for a remote and hidden area with enough water and good stands of trees and plenty of native grasses and other vegetation to feed your "stock". A place where the nearest law enforcement officials were at least 50 miles away. For the McHaney brothers, this place turned out to be the higher, western side of what is now Joshua Tree National Park, in Lost Horse Valley and Hidden Valley. Bill McHaney's gang took cattle from Mexico and Arizona to hide them in other Joshua Tree valleys as well, then returned stolen horses. Johnny Lang also drove cattle into Lost Horse Valley after his brother was gunned down in New Mexico. He woke up one morning to find his horse gone. He tracked it to the McHaney's place but was told to leave the area. Luckily, Lang met "Dutch" Frank who had discovered a mining claim, but was afraid to set up mining operations because he was also being hassled by the McHaney gang. Lang bought the rights to the mine and called it "Lost Horse", after enlisting three partners to protect the claim against claim jumpers in 1893. The Lost Horse Mine ultimately produced 10,500 ounces of gold and 16,000 ounces of silver. Today, the Lost Horse Mine stamp mill is considered one of the best preserved in a National Park service unit. We hiked three high points along this loop. The most interesting summit was Peak 5196 because of the columnar basalt at the top. In a land dominated by granite, this is one of only three occurrences of basalt. From its summit, just northeast of the trailhead, are extensive views of Queen Valley to the east and Lost Horse Valley to the west. A few days before, we had hiked Mt. Minerva Hoyt, named after the woman instrumental in President Franklin Roosevelt's proclamation to designate Joshua Tree National Monument.
Sign at trailhead. We hiked the trail counter-clockwise.
Our Hike in the Mojave
As the road to Lost Horse Trail climbs to around 4,000 feet elevation in the western, Mojave desert section of Joshua Tree NP, the amount of Joshua trees, junipers and yuccas is more prevalent compared to lower, dryer Sonoran desert Pinto Basin to the east at 1,700 feet. Although it's a moderately-used trail, you get the feeling of remoteness surrounded by mountain ranges. The trail circles Lost Horse Mountain, trekking through Quail Wash and over juniper and shrub-covered hills darkly punctuated by scattered gneiss boulders.
By the time we got back to the trailhead parking lot, it was full. Another fun day in Joshua Tree's Mojave desert. The three extra summits were the "icing on the cake" - worth the effort.
Time and Space in the Desert
Joshua Tree is an awe-inspiring land shaped by Earth's events spanning the Proterozoic alteration of pre-existing rocks into gneiss, to the five Proterozoic through Cretaceous intrusions of plutons that produced gold and silver and its famous sculpted rocks, to the relatively recent faulting that uplifted mountains and blocked canyons. A landscape that has a tumultuous origin, but a relaxing presence. Dark and rubbly mountains spring out of flat, buff - colored valleys. A slight haze of dust still hangs in the air after last night's wind storm. I stand looking over it all - breathing space. Back straightens, chest raises, diaphragm brings in creosote and sand-scented air. To some, this expanse and space feels intimidating; to me it feels comfortable. To some it looks formidable with its hot, dry stillness and sharp- spined cacti; but I admire their motivation to survive under the hot, penetrating sun. To walk in browns and buffs for awhile and then suddenly come upon magenta and bright yellow cactus blooms is cause for celebration. I remember liking these ragged and gangly Joshua trees and contrasting smooth, rounded boulders the first time I saw them 38 years ago. I revel in the sublime space and quiet that calms my mind. Grateful for the feeling of being connected to this land.
"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. We remember why we love the desert; it is our tactile response to light, to silence, and to stillness."
- Terry Tempest Williams
Never Stop Exploring!
From summit of Point 4959, looking at Malapai Hill.
Beautiful 1.7 billion-year old gneiss - and hedgehog (?) cactus.
Circling around Lost Horse Mountain (on far horizon) to hike up its northeast ridge.
Remains of a very sturdy fire place and bed frame.
Our first summit - Point 4959.
Three types of rock: great example of gneissic banding - a textural lineation of minerals in metamorphic rock created by pressure and intense heat (foreground). Malapai Hill in middle of valley created by magma. Valley rock is monzogranite.
Looking at Lost Horse Mountain from the slopes of Point 4959. You can see Lost Horse Trail as it climbs to the saddle on its northeast ridge. Hike that ridge to the summit.
Some cool stuff on the trail.
Summit of Lost Horse Mountain
From Lost Horse Mountain's ridge: a view of Lost Horse Mine.
Lost Horse Mine stamp mill through chain-link fence.
Walking up to Point 5196.
Beavertail cactus just before the blooms.
Columnar basalt on Point 5196.
References
California Geology. 1998. Department of Conservation, Division of Mines and Geology. Dilsaver, L.M. 2015. Joshua Tree National Park: A History of Preserving the Desert. Prepared for National Park Service, Joshua Tree National Park, Twentynine Palms. Joshua Tree Geology Tour Road. Joshua Tree National Park Geology - Rock Types. Digital-Desert: Mojave Desert. Trent, D.D. Geology and History of MInes, Joshua Tree National Park.
Named after the woman who lead conservation efforts for what is now Joshua Tree National Park, Mount Minerva Hoyt looks over wide, sandy valleys of Joshua trees and piles of weathered granite boulders, famous for their climbing routes.
Trip Stats
Overview: To honor the woman behind Joshua Tree NP's conservation campaign, hike to her namesake summit. Bag nearby Quail Mountain, Joshua Tree's highest summit, for a tour of two peaks and great views on top of Joshua Tree. Experience all of the famed attributes: Joshua tree groves, rock climbers scaling eroded granite, a glimpse of the private historic Randolph Ranch, a beautiful wildflower-filled canyon and an enjoyable ridge walk. Location: Joshua Tree National Park/Wilderness - North Entrance Station out of Joshua Tree, Southern California. Distance/Elevation gain: 12 miles out and back. Trailhead = 4,061', Summit = 5,405'. Net gain = 1,700'. Coordinates: Parking = 34.02926 N -116.17905 W. Summit = 34.01347 N -116.22694 W. Difficulty: Moderate Class 1-2 Fees/Permit: $30 entrance fee, good for 7 days. Navigational aids: AllTrails map, Trails Illustrated Joshua Tree National Park #226. Date Hiked: 4/9/2022. Geology: Begin in the eroded boulder piles of monzogranite, a deep intrusive igneous rock uplifted and eroded to create large depths of coarse rock-fill in the valleys. Monzogranites are a biotite (mica) granite that are the final crystallized product of magma, after other minerals have solidified (like olivine). Mount Minerva Hoyt summit is made of orthogneiss, a metamorphic igneous rock. Interesting to note that the summit of nearby Quail Mountain is not made of this gneiss, but instead made up of monzogranite. Good explanation of magma crystallization. 
Hike Summary
There's a few ways to hike to Mount Minerva Hoyt and nearby Quail Mountain, Joshua Tree NP's highest. Both are listed on Sierra Club's Hundred Peaks Section. Years ago, Roger and Maria Keezer led us up Quail Mountain from the west. This time Fred, Scott and I approached from the east, parking at a lot on Park Drive, ~ one mile south of the Boy Scout Trailhead reached from Joshua Tree's west entrance. You could also begin the hike from the Hidden Valley Nature Trail parking. The weather was perfect - sunny and warm. Scott met us for the hike, as he has for many over the years. We have recently hiked Monument Mountain and Pinto Mountain in Joshua Tree together, and Pahrump Point near Death Valley. Hiking Directions
Joshua Tree NP's area is 795,000 acres, slightly bigger than the state of Rhode Island. Thankfully, almost 430,000 acres of it is wilderness, so there is a lot of space to roam and discover. If you want solitude, you can quickly get away from popular spots. If you want to climb to get a view, there are six mountain ranges. Pay attention to maps and apps, because you can easily get disoriented in this huge desert. By getting out there, smelling, touching, and seeing the life of the Mojave, you will gain a sense of wonder and admiration for the species that survive there.
The land in Joshua Tree has had a varied and interesting history, from the Pinto Culture, its initial transitory hunter-gatherer inhabitants to the miners and ranchers that arrived in the 1800's, to people seeking wellness from tuberculosis, and today's recreational visitors. The year 2021 saw the first time that park visitors totaled more than three million. Minerva Hoyt created a desert conservation exhibit for the Garden Club of America show in New York in 1928 that also appeared in London, England. Her magnificent exhibits not only stressed the beauty of these American deserts, but also the fragility and potential dangers. The widespread attention her exhibits brought influenced many southern California residents to decorate their own gardens with transplanted cacti. Vegetation was taken from the natural desert gardens in the pass entering Palm Springs, California, easily accessible to those traveling on the major highway between that city and Los Angeles. Commercial florists added to this theft. The same occurred in the Mojave desert, where small Joshua trees were uprooted and planted in yards, and larger Joshua trees were harvested for their wood. Joshua trees were set ablaze so that people could signal to each other. Today, it's hard to believe this destruction actually occurred, because we have learned to respect these beautiful deserts - appreciation has grown significantly. It took this destruction to motivate Minerva Hoyt into action to preserve this awesome park. When I lived and worked in the Palm Springs area in the 1990's, I was fortunate to be a volunteer to survey desert tortoises along with my hiking friends. We worked with the Joshua Tree National Monument's biologist, walking through the Pinto Basin, a vast sublime open desert. Upon coming across a tortoise, we weighed it, counted its scutes, measured it and glued an identification tag onto its shell, so it could be tracked. This was the beginning of my fascination for desert ecology, and of great memories that we friends still recall today.
Keep Exploring our Deserts!
Starting off on road that leaves from parking area off Park Boulevard near Hidden Valley. This road leads to an intersection with a trail that leads 0.5 miles to the Hidden Valley picnic area, another place to start this hike.
Our GPS tracks leading from Park Boulevard to a loop ascending Mount Minerva Hoyt.
Continuing west along Old Lost Horse Trail
Old Randolph Ranch - go around fenced property. I could not find much on the history of this ranch. It appears the owner had a sense of humor (see photo below).
Randolph Ranch - "May it Never Crumble".
Randolph Ranch, a private inholding in Joshua Tree NP.
Hiking west up Lost Horse Valley past Randolph Ranch. Mount Minerva Hoyt is dark-covered peak on the right.
Some cool stuff on the trail.
Long-nosed leopard lizard
Gambelia wislizenii
The end of Lost Horse Valley funnels you into a small canyon or draw with visible path leading to saddle where you then descend into wash at base of Mt. Minerva Hoyt and Quail Mountain.
Arriving at the saddle before the drop into the wash at base of mountains. We climbed this ridge westward toward Quail Mountain and then headed northeast on the cross country trail between Quail and Minerva Hoyt to hike Mt. Minerva's southwest ridge to the summit (point on horizon to the right).
Dropping 200' down into wash after saddle. Mount MInerva Hoyt on the right horizon. On the way up, we ascended the ridge in front of us in this photo; we descended Minerva Hoyt's east ridge seen on horizon to end up in this wash.
View of Mt. San Jacinto (overlooking Palm Springs), still covered with a lot of snow.
Walking up ridge toward Quail Mountain after getting out of wash.
Looks like a trail marker on the ridge up. Looking back at the saddle we crossed over to get into wash below.
Scott on ridge trail.
Hiking on cross-country trail that connects Quail Mountain to Mt. Minerva Hoyt. Summit on the left - there is a guy standing up there!
The last 200' climb to the summit is easy, punctuated with beautiful metamorphic boulders and cactus gardens, plus a spectacular view of the desert that Minerva Hoyt fought so hard to protect.
Fred and Scott signing summit register.
One of the beautiful "cactus gardens" on the summit.
One of the biggest prickly pears (may be a dollarjoint prickly pear) I have seen! The saddle that we ascended is just above Scott's head and slightly to the right under the two rock summits - aiming for that landmark on our way back!
Claret cup hedgehog
Echinocereus triglochidiatus 
Minerva Hoyt's east ridge path - headed toward wash below.
Getting near wash and saddle, our entry point into Lost Horse Valley.
On the way back.
Our GPS tracks
Click for larger map 
Elevation profile
References
Earle, S. Crystallization of Magma from Physical Geology. BC Campus. Minerva Hoyt. National Park Service. 2015. Dilsaver, L.M. 2015. Joshua Tree National Park: A History of Preserving the Desert. Prepared for National Park Service, Joshua Tree National Park, Twentynine Palms.
Another rugged summit from the Sierra Club Desert Peaks Section's list completed! On this narrow perch above desert valleys thousands of feet below, we saw spectacular views of Nevada and southeastern California and experienced "flow" - the secret to happiness.
Scott on Pahrump Point's southeast ridge just under the summit.
Trip Stats
Overview: This classic Mojave desert hike begins on an alluvial fan, ascends through boulders up an ever-narrowing canyon, switchbacks up a talus slope to emerge onto Pahrump Point's southwest ridge for a huge view of the summit's steep walls. From here, the route winds up a gully and treks through a few "passages" in its steep face to gain its narrow summit ridge crest. See fossils and plenty of rough limestone, as well as fantastic views of Telescope Peak in Death Valley, Mt. Charleston near Las Vegas, and the town of Pahrump. Attention to hike directions and navigation crucial to finding correct route. Location: Pahrump Point is in the remote Nopah Range Wilderness Area is just over the California/Nevada border, east of Death Valley National Park. Its rough and rocky summit rises above Pahrump, Nevada. Distance/Elevation Gain: 7.6 miles roundtrip from CA Hwy. 178 trailhead to summit; less distance if you can drive in further on gravel road leading to canyon. Elevation gain from highway = 3,400'. We began hike at 2,600'. Summit is 5,410'. Difficulty: Strenuous Class 2+ with occasional use of hand for balance. Lat/Long: Trailhead at Hwy 178: (UTM) 11S 0573213E 3992648 N. Summit: 0577422E 3995282N. Navigational aids: AllTrails map with GPS tracks, Sierra Club Desert Peaks Section hike directions - Pahrump Point. Date Hiked: December 17, 2021. History: "Pahrump" is a derivation from the Southern Paiute Pah-Rimpi term meaning "Water Rock" describing the abundant natural artesian wells in the area.
Pahrump Point trailhead location.
Aprés Hike
One of the best things about this hike is the delightful hot spring pool we soaked our weary bodies in afterwards at Tecopa Hot Springs Resort. We met our friend Scott to camp there on a few unseasonably cold December days. This resort, just outside of Death Valley and near the Nevada/California border had been abandoned for 10 years before the current owner purchased it, and it still wears the characteristics of an old-time hot springs resort, with original buildings, nothing fancy here - very remote and bohemian, complete with a 40-foot labyrinth. With no cell service or internet, it was heaven for three days. One of its mission statements:
"We see ourselves as stewards of sacred land and ambassadors of goodwill."
The Southern Paiute tribe discovered these hot springs hundreds of years ago. One night, after a soak, we enjoyed live music on an outdoor stage, standing around a fire pit sending smoke up into a cold and starry desert sky. The next morning we had excellent huevos rancheros in Tecopa Hot Springs Resort Bistro.
Bath house with 2 hot springs pools at Tecopa Hot Springs Resort, California.
Our Hike
In the classic Mojave desert fashion, this rocky peak rises abruptly from the desert floor with dramatic, unobstructed views from a small, almost precarious perch at the summit. Pahrump Point looks difficult if not impossible from a distance, so it's fun to find the route through its steep cliff face. I'm glad Scott brought along the hike description from Desert Peaks Section manual. There are three crucial points along this route that you need to recognize in order to negotiate the rocky gullies, canyons and ridges to find most efficient way to the summit. The hike switches from Pahrump Point's southwest ridge to its southeast ridge where an easier route is present, just under the summit. Trip reports describe starting this hike just off of CA Highway 178 and the road leading to the mouth of the canyon, the distance of 1.8 miles. With our high-clearance truck, we drove just under one mile up this gravel road and parked to walk the rest of the way to its end at the mouth of the canyon framed on each side by alternating light-and dark colored Cambrian rock layers. A few cairns identify the trail throughout the completely rocky canyon bottom. A path initially goes along the toe of the left canyon wall, and then to the right, but most of the time is spent maneuvering through rocks and boulders in the canyon bottom. Once topping off on the southwest ridge after climbing a talus slope out of the canyon, the peak's cliffs come clearly into view, as well as a long and deep canyon to the south. To make the switch to the southeast ridge to summit, there are a few very important and prominent cairns for direction. The last few hundred feet climb to the summit is fun - you go by a hole in the rock that looks down into another steep canyon, then up a steep, short gulley. This empties you onto the final Class 2+ climb up Pahrump Point's manageable face, where you reach a fun and short summit ridge that is only slightly spooky. The narrow summit elevates you thousands of feet over desert playas, with a clear view of snow-covered Telescope Peak - the highest in Death Valley. The ridge to the next high point to the north seemed treacherous, so being content with our accomplishment, we basked in the nearly winter solstice sun. We occasionally cursed the loose rock on the return talus slope, after getting off the ridge. I wondered if age has caused me to be slower on this terrain. Picking our way through the boulders in the canyon, looking for cairns to give us a clue for a better route. Exiting the canyon onto the immense Chicago Valley, we turned back to see the Nopah Mountain range a fiery yellow/orange of sunset. Looking forward to dinner at the Crowbar Cafe and Saloon in Shoshone to celebrate another adventure - three friends who (still) like to hike together after all these years. It was great to hike once again with Scott, who said at the summit, "This is good for my soul!" Hiking to these amazing places with your friends and overcoming physical and mental obstacles together is good for your soul and can help you experience "flow" - the secret to happiness and optimal experience. The concept of "flow" is getting more attention lately and is the subject of my next post, as well as positive psychology, body movement science, enhancement of goal pursuit and well-being .
"Into the forest I go, to lose my mind and find my soul."
- John Muir 
Initial approach through Chicago Valley up gravel road to mouth of canyon and then to Pahrump Point, just right of middle horizon. Cold and windy December morning in the Mojave.
End of road, trail goes up wash. Here, trail is seen on left side of canyon; it switches to the right side further up.
Initial main canyon walk alternates between canyon floor and side trails.
Trail seen on left side of canyon initially.
Coming down from a trail on the right side of the canyon, then up bottom of canyon to left and right fork; take right fork.
Tall cairn at 4,120' elevation that indicates to take the canyon to the right.
Trail then ascends up right side of canyon to 2 large cairns. From here, trail traverses slope and then drops you to the base of talus slope and ridge saddle.
Heading up canyon to the right at intersection with main canyon. This right fork takes you up talus slope to saddle at ridgeline.
Getting closer to the ridge
A look back toward Telescope Peak in Death Valley to the northwest.
On a moderately loose talus slope, getting closer to notch on ridge; then peak clearly seen to the left.
Large cairn marking saddle on ridge at top of scree slope. Peak is seen clearly at this point.
Once on ridge at 5,100 feet, see summit, and another 300-foot ascent to it; continue following ridge shortly to a ducked/cairned notch - head left through that notch to traverse to the left through another marked notch where there is a "window rock" on its left side. The route avoids the steep cliff face under the summit.
Cairn on left marks the traverse to the notch with "window rock".
Gully just after "window rock" which is on the left side of trail.
Out of short gully and now fun Class 2+ on final ascent.
Looking down canyon toward Chicago Valley to the south.
Entry up face of summit block on the summit's right side.
Reaching the summit ridge.
Southeast ridge just under the summit.
At the summit; trail goes through the snow on left side of this ridge in photo.
Scott and Fred on the summit of Pahrump Point - 5,410 feet!
Looking southeast down the Nopah range.
Mt. Charleston, north of Las Vegas, in background.
On Pahrump Point's summit.
A very organized peak register.
Trail on ridge - working our way back down.
"Window rock" on left side of trail is a landmark to navigate trail.
Ivory-spined agave
Some cool stuff on the trail.
(clockwise from top left) Hedgehog cactus, bryozoan fossil, ivory-spined agave, triangulation survey marker at Pahrump Point's summit. 
Parting shot - sunset on Pahrump Point in the Nopah Range.
Celebratory dinner at the Crowbar Cafe and Saloon in Shoshone, a few miles from Tecopa Hot Springs, CA.
Sad to see these go - the limestone proved to be too rough for these worn KUHL pants.
Labyrinth at Tecopa Hot Springs Resort
Tecopa Hot Springs Resort
Tecopa Hot Springs Resort Bistro - the best huevos rancheros for breakfast!
Moonrise in Tecopa, California.
Seemoore's Ice Cream - "The World's Tallest Ice Cream Stand"
Pahrump, Nevada. 
AllTrails GPS tracks from beginning of canyon (lower left) to Pahrump Point.
Route map from Sierra Club Desert Peaks Section
click for larger view
References
Wikipedia. Pahrump, Nevada. Jennings, C.W. 1958. Geologic Map of California Death Valley sheet. Why Does Experiencing 'Flow' Feel so Good? A Communication Scientist Explains. theconversation.com. Flow Theory: An Overview. sciencedirect.com. On Haystack, we found sun and solitude off of the Art Smith Trail in the Santa Rosa and San Jacinto Mountains National Monument, a spectacular view of Southern California's mountain ranges, and our old summit register entry from 2011. Related: First Cactus to Clouds Challenge - The Beginning of the Ultimate Desert Hike Pinto Mountain Hike - Joshua Tree Wilderness Desert Plants photos Monument Mountain Hike - Joshua Tree National Park In Memory of Roger Keezer  Peninsular Bighorn Sheep near Art Smith Trail, Palm Desert, CA Ovis canadensis nelsoni Listed in 1998 as Endangered Species due to substantial population decline from disease, predation, habitat loss and human disturbance Cross - country to Haystack Trip Stats:
Directions to Art Smith Trailhead: Travel south on CA State Route 74 (Palms to Pines Scenic Highway) from CA State Route 111 in Palm Desert 3.5 miles to long sandy parking area on right of road just as it starts to curve to the left to ascend switchbacks up hills to the south. The Santa Rosa and San Jacinto Mountains National Monument Visitor Center is adjacent to parking, across SR 74. Hike Directions: (Topo map of our route below)
 Cross-country route off of Art Smith Trail to summit of Haystack Mountain Yellow marker indicates point at which we left Art Smith and ascended wash Elevation at this point = 2,237 feet; ~1,600 feet to summit from turn-off Geology and History: The trail to Haystack Mountain treks through quartz diorite, a coarse-grained intrusive rock with 5-20% quartz (diorite has <5% quartz). It has the classic speckled black and white texture and large grain size. Quartz diorite is often confused with granite because they look similar. Both are intrusive rocks with a phaneritic texture in which mineral grains are visible without magnification. Granite, however contains 20-60% quartz. Quartz grains are not usually visible with quartz diorite, but can definitely be seen in a granite. This rock unit is Cretaceous age (144 to 65 mya). The efforts of Art Smith, a.k.a. "Trail Boss", a Desert Riders equestrian helped to establish the Desert Riders Trail Foundation, a non-profit trust for trail preservation and building. The Desert Riders equestrian club was initiated in 1931, has made 28 trails as of 2010, many of them follow ancient Cahuilla Indians' migratory hunting and gathering trails. "Probably I was too young and venturesome to feel dismay, but I know now what Mama must have felt as she looked out upon that savage scene of sand and rock and sky locked in the pitiless grip of desert summer." - Nina Paul Shumway, Your Desert and Mine, an account of her family's settlement and beginning of the date industry in the Coachella Valley.
Our Hike The past few times we have hiked the Art Smith Trail, we have seen Peninsular bighorn sheep in Dead Indian Canyon near the rust-colored metal sign that marks the Art Smith trailhead, not far from the parking lot. They were listed as a federally endangered species in 1998. This morning, the sun shone brightly on the deep-walled Dead Indian Canyon and a group of ewes with their lambs. This trail, just west of Palm Desert, links to trails leading into the Indian Canyons in Palm Springs. The Coachella Valley is a special place for me and I carry memories of hiking all of its trails with dear friends that I will always keep in touch with. It's my "old stomping ground", or more aptly put, my old hiking ground. Living there in the 1980's and 1990's, we climbed, traversed, slid, sweat, laughed, got stuck with cactus spines, boulder-hopped, and celebrated our hikes and friendships. I am grateful I can still be able to hike these wonderful trails and when I do, all of the memories come back vividly. I met Fred on Mt. San Jacinto, and he automatically became a part of our hiking clan. Not many people venture off Art Smith to climb Haystack Mountain. To our surprise, we found the same notepad in which we had made our 2011 entry in the summit register can! I guess the dry climate and the sparse number of Haystack Mountain visitors helped preserve this small note pad. It's a simple message: "12/21/11 - Fred, Sue and Scott - old friends who love to hike." We missed Scott this year, but were looking forward to hiking with him to Pinto Mountain in the next few days. Walking on Art Smith Trail is a treat in itself, a meandering path with weathering rock piles, beavertail cactus and brittlebush blooming in the spring, and that satisfying crunch of gravel with each step. One can imagine Cahuilla Indians walking to water sources on the trail and equestrians from the Desert Riders on horseback winding through washes across the open desert. But to pick your own route cross country, dodging cholla cactus, sharp-toothed agave leaves and cat claw acacia shrubs, climbing up and sliding down boulders and dry waterfalls is the greatest satisfaction. Art Smith Trail was busy due to the Christmas holiday. This trail treks through a possible plutonic synform (a downward-closing or concave fold of topography). Shimmering green California fan palms pop up occasionally to the left of the trail, and the valley patchwork of forest green golf courses sprawl to your right.  California fan palms Washingtonia filifera  Haystack Mountain on the horizon as seen from near Art Smith Trail Leave trail at ~ 3.4 miles and hike to highest point at far left of long ridge Palm oasis in canyon on left We left Art Smith at 3.4 miles from the trailhead at a wide wash and headed west-southwest across relatively flat, open low desert. From here, it was 1.3 miles to the summit. We encountered no major rock barriers, only a few very small waterfalls and sandy benches covered with rounded boulders. I was surprised to see a few small junipers; the land is generously dotted with hedgehog cacti with their inch-long needle-spines.  Wash ~ 3.4 miles in from Art Smith Trailhead at SR 74 in Palm Desert Climb up flank of cone to ridge - follow ridge to summit, seen in this photo  Getting closer to the base - climb cone to ridge and follow to summit  "False summit" on the ridge  Hedgehog cactus (Echinocereus engelmannii) in foreground in front of cholla cactus Arriving at the base of Haystack, we gained its sunny east ridge by hiking straight up the steep flank to the left of the mountain, occasionally grasping rocks. The ridge is a Class 2 scramble with at least one "false peak" on the way up; not a long hike and the view at the summit is nothing short of spectacular. It is here you realize the enormity of this beautiful Colorado Desert and its mountain ranges. The controversial Dunn Road can be seen not far from the summit. It is a wide, sandy road that Mike Dunn carved out through the slopes of eastern Santa Rosa Mountains starting at Pinyon Flats in the 1960's and 70's. It traces around the contours of mountains, through what is now Santa Rosa and San Jacinto Mountains NM to Cathedral City. Because Dunn bulldozed some of his road on federal land, the BLM put a gate across the road. But Dunn would just bulldoze it down, and the BLM would fix it. I remember, when I lived in the Coachella Valley in the 1980's, Dunn Road was used for recreational jeep tours. Now of course since it is entirely on national monument land, it is only accessible to non-motorized travel. There were also differing opinions about whether Dunn Road compromised the bighorn sheep habitat. 360 - degree view from Haystack Mountain summit Summits include Mt. San Gorgonio, Mt. San Jacinto, Toro Peak, Martinez Mountain Also Little San Bernardino Mountains and southern Joshua Tree NP The summit view includes the highest points in the Santa Rosa Mountains: Martinez Mountain and Toro Peak, and also Mt. San Jacinto towering above Palm Springs. To the north lies Mt. San Gorgonio, the highest peak in Southern California, and the northeast the Little San Bernardino Mountains and the southern part of Joshua Tree National Monument. Ancient Lake Cahuilla filled the basin of the current Coachella Valley up until 500 years ago. This area is rich in culture and history - from the hunting/gathering Cahuilla Indians to the first settlers of this arid land, to the history of the date palm industry - not to mention the dramatic and substantial geologic history. The San Andreas Fault courses through the Coachella Valley.  View from Haystack Mountain to the northwest Mt. San Jacinto (closer range) and Mt. San Gorgonio, the highest summit in Southern California (on horizon with snow)  Our summit register entry from 12/21/2011: "Fred, Sue and Scott - Old friends who love to hike"
 Scott and Fred near Haystack Mountain summit - 12/2011 Palm Desert in background on valley floor, Southern Joshua Tree NP on horizon I recommend returning by the same route unless you are open for more adventure and willing to negotiate the steeper and rockier terrain to the southeast. We did just that but also ended up in a thick and tangled palm oasis, the palm fronds clashing in the breeze. Briefly crossing the oasis, crunching through dead fronds, we found our way out by ascending a steep canyon wall. Out into the open again, we saw not far from us two mountain bikers on the Art Smith Trail. Back to civilization. As we hike back along this very familiar trail, I picture a scene from 25 years ago - a faint image of a group of friends, walking in rhythm, boots crunching, happy voices laughing and talking, celebrating friendship and this great land. I bet we find both of our summit register entries the next time we summit Haystack.  Desert agave The Cahuilla Indians roasted the heart of the agave in pits on rocky drainages  Desert Fan Palm fronds  Washingtonia filifera "Filifera" describes the white filaments between the segments of the frond  Agave deserti Santa Rosa and San Jacinto Mountains National Monument  Fred and Sue on the way down - another beautiful hike in the desert!  Beginning of Art Smith at its intersection with California SR 74. Metal trail sign below. Wide wash is entry to Dead Indian Canyon Maps   Topo map and our route and elevation profile to Haystack Mountain via Art Smith Trail and then traveling cross-country up east ridge Click on image for .jpg of topo map References:
Bighorn Institute. 2019. Endangered Peninsular Bighorn Sheep. Retrieved from https://www.bighorninstitute.org/endangered-peninsular-bighorn Dibblee, T.W., and Minch, J.A., 2008 Geologic map of the Palm Desert and Coachella 15-minute quadrangles, Riverside County, California. Dibblee Geological Foundation. Patten, Carolyn. "The Desert Riders." Palm Springs Life, October 1, 2010. Desert Publications, Inc. Retrieved from https://www.palmspringslife.com/the-desert-riders/ Pearce, Al. "Dunn's Road Could be One of the Most Beautiful in Desert." Desert Sun, Volume 45, Number 214, 11 April 1972. In website: UCR Center for Bibliographical Studies and Research. Retrieved from https://cdnc.ucr.edu/cgi-bin/cdnc?a=d&d=DS19720411.2.59&e=-------en--20--1--txt-txIN--------1 Schumann, W. 1993. Handbook of Rocks, Minerals and Gemstones. Harper-Collins Publishers and Houghton Mifflin Company. Taylor, Joan. "The Dunn Road: A Checkered Past." Desert Report, 2007. Sierra Club publication. Winter, John D. 2010. Principles of Igneous and Metamorphic Petrology, 2nd Ed. Pearson Education, Inc., New Jersey. Our annual California desert peak hike with our friend Scott - this year to isolated and rugged Pinto Mountain in Joshua Tree Wilderness.  Pinto Mountain - eastern Joshua Tree National Park in the Pinto Mountain Range Trip Stats Overview: The reward for the long walk across Pinto Basin followed by the rocky climb is the outstanding 360° views of the Mojave desert mountain ranges and the bright red barrel cacti that stand out in contrast. And, there's a sculpture on the summit! Distance: 4.8 miles to summit; round-trip 9.6 miles (out and back). Elevation Gain: Turkey Flats parking at 1,785 feet; Pinto Mountain at 3,983 feet = ~ 2,200 foot gain + regaining lost elevation = ~ 2,600 feet total. Maps: Trails Illustrated Joshua Tree National Park #226, USGS 7.5 min Quad Pinto Mountain. Entrance Fee Joshua Tree NP. Sierra Club Desert Peaks Section map of GPS tracks. Coordinates: Pinto Mountain summit: 33°57'12.23"N 115°48'10"W. Trailhead at Turkey Flats Backcountry Board: N33 54.109 W115 50.098. Difficulty: Easy across Pinto Basin; moderate to strenuous ridge climb - Class 1-2. CAUTION: Be prepared with GPS track and a good topo map - there is a lightly used trail on ridge but it's essential to have route-finding skills. Very hot/no shade mid-May through September. Date Hiked: 12/23/2018 Driving Directions From California I-10 East out of Indio, take Exit 168 into South Entrance of Joshua Tree National Park. Drive north 20 miles on Cottonwood Springs Road/Pinto Basin Road (past Joshua Tree Visitor Center) to Turkey Flats parking area and sign board on right side of road. Hike Directions
For the geocurious This hike treks through an array of different types of rock units ranging from Holocene cover (10,000 years ago to now) to Proterozoic Era (up to 2.5 billion years ago). A geologist's dream. It passes through some of California's oldest rocks; these rocks also top Monument Mountain, across Pinto Basin to the southwest.
 Trailhead and parking at Turkey Flats, 20 miles from Interstate 10 in Joshua Tree Pinto Mountain on horizon  Sierra Club Desert Peaks Section map of GPS tracks. Topo map and elevation profile of hike to summit of Pinto Mountain, Joshua Tree NP. The hike begins at Turkey Flats trailhead on Cottonwood Springs Road/Pinto Basin Road. The last half of this hike climbs 2,200 feet in 2.3 miles to summit elevation of 3,983 feet.  Our route across the alluvial fan at base of ridge; the trail travels on spine of ridge all the way to summit of Pinto Mountain in a north/northeast direction (looking at southwest-facing slopes) Pinto Wash at base of fan  Elevation profile for ascent. Our Hike Some of our best and most memorable adventures have been on hikes to desert summits in Southern California with our friend Scott, a Desert Peaks Section hiking veteran. Last year we hiked Monument Mountain in Joshua Tree National Park. This year, drawn to Joshua Tree again, we stepped it up (literally) with a tougher hike to Pinto Mountain summit. We parked at the Turkey Flats trailhead and signboard, a 20-mile drive into Joshua Tree National Park south entrance from California I-10. Scott had good directions for locating the ridge we would ascend: locate the summit at 32° then locate our ridge climb at 36°. Pretty straightforward direction and approach. We made a beeline toward the smaller ridge to the right of a large, shadowed canyon which is just to the right of Pinto Mountain summit (see directions, above). The flat 2.5 mile distance to the toe of the ridge accentuates the immensity of this sublime desert. A feeling of space and solitude. To hike Pinto Mountain is to experience two distinctly different terrain types with very little transition in between: flat, soft and casual to steep and rocky. The last half climbs 2,000+ feet over rough and angular rocks and also requires route-finding, occasionally reaching for a handhold. The easy walk across Pinto Basin takes you through soft sand flats and beautifully rippled "dunes", through minor washes before crossing Pinto Wash. We saw a desert tortoise burrow near the dunes. I was surprised at the bright purple blooms of sand verbena vines draped across the sand dunes and an abundance of bright green vegetation in December. The fractured and curled "clayey" soils in Pinto Wash also give a clue to recent saturating rains. As you make the short descent off the dunes, stay just to the left (west) of a long low hill cut by a wash.  Desert Sand Verbena Abronia villosa  Scott (left) and Fred heading out in morning to Pinto Mountain summit The ridge to ascend is just to the left of Fred with the shadows to its left side  Sand dunes ~ halfway between Turkey Flats trailhead to base of Pinto Mountain Shortly after crossing Pinto Wash, the hike ascends an ever-increasing amount of coarse gravel and boulders, the characteristic feature of alluvial fans where heavier rocks drop out early in its deposition and smaller rocks are deposited at the toe of the fan. We maneuver down through stream cuts and around rocks on the upper alluvial fan as we finally reach the bottom of our ridge. We missed the cairn indicating the start of the ridge trail on our way up and started the climb on the ridge spine, which was alright because we soon ran into the light-to-moderately tracked trail on the ridge. Don't be tempted to descend down the canyon on either side of the ridge - when in doubt, stay on top of the ridge. There are a few places along the 2.3-mile ridge hike where the trail bypasses a high point, however.  Pinto Wash just before base of alluvial fan Clayey soil that has been recently saturated with water and then has dried and formed fractures into polygonal sections as well as "mud peels" caused by a fracture of clay parallel to its surface.  Approaching alluvial fan deposited from canyon on the left Hike up ridge to the right of this canyon, and just to the right of Pinto, with vertical rocks and shadows to Pinto Mountain with its white quartzite slopes. Pinto Wash in foreground.  Beginning of ridge trail Small cairn on the large rock on the right, faint trail in middle of photo heads to ridge  We started here at toe of ridge The ridge walk was very windy, especially on the saddles. We took a lunch break on the lee side of a bump on the ridge to avoid being battered by the wind. From our spot we could see the alternating light and dark rock; although we couldn't see a trail, we could see our ridge to the top. Rocks and Joshua trees define Joshua Tree National Park, but if you look closely, you will find among them smaller creatures and plants brightly colored in contrast to the neutral tones. Groups of red barrel cacti randomly dot the landscape, with mounds of curved red spines spectacularly lit by the sun. Scott pointed out a tiny round cactus with a bright red fruit and sharp white spines, sheltered by a "shelf" of equally sharp quartzite - a common fishhook cactus. There was a strange black caterpillar with bright yellow dots and stripes that went from crawling to a curled position as soon as I cast my shadow over it. The best match I could find for this caterpillar is the white-lined sphinx moth, AKA hummingbird moth that has a long proboscis to reach deep for nectar in penstemons, among other flowers.  No other place I'd rather be at that moment! Rock with flat surface provides a "chair" to sit and rest Pinto Mountain left (highest) summit  Alternating light and dark rocks correspond with varied rock units (see Geology, above)  Red barrel cactus Ferocactus cylindraceus  White-lined sphinx caterpillar Hyles lineata  Common Fishhook cactus in quartzite Mammillaria tetrancistra Nothing gets in the way of the expansive views of mountain ranges perched on the desert floor in every direction as you near the summit. It doesn't take long before you feel like you are standing far above the immense basin. Creosote bushes make tiny dots on the smooth floor below and washes braid toward the low point of Pinto Basin. The hike goes through several rock units. Sharp and angular quartzite crunches and clinks under boots and becomes loose and steep as you near the summit. A few trails can be seen through the steep section where I had to hold onto fractured rocks; they all make their way up the ridge line. I looked down the trail to see that Scott had temporarily disappeared under the crags I was on, so I waited until he climbed and appeared again. Suddenly, the flat crown of the summit appears as you emerge from the steep rocks and take a short walk to the summit cairn. We took shelter from the persistent northwest wind at the lee side of the cairn, procured the metal box containing the summit register, and found a page to put our entry for 12/26/2018: "PEACE - from Sue, Scott and Fred - 3 friends who like to hike together".  Summit of Pinto Mountain, 3,983 feet looking northwest Saguaro cactus sculpture from old wire present on top of the mountain  Scott, Sue and Fred on Pinto Mountain summit Scott is holding a rock found on the summit with a painted cat from Jamestown Kind Rocks Project, whose goal is to "promote random acts of kindness to unsuspecting people by painting and dropping inspirational rocks or some other cool way to bring kindness." Scott brought the rock on our hike to Thimble Peak in Tucson and we left it near the summit.  Our summit register entry for 12-26-18 The entry above ours: "Christmas Eve/Dec/2018 - Happy Holidays everybody! We made it to the top". - Ecuador, USA, Argentina  Summit looking north  Together, another summit and memorable day in the beautiful American West!  U.S. Coast and Geodetic Survey marker on Pinto used for triangulation station (main station) for land survey The wind was cold and blowing steadily, so we stayed long enough to get our photos, revel in our accomplishment, and grab some food for the journey down. The bumpy ridge extended from our feet to the basin. The walk across the alluvial fan, then across Pinto Wash was a welcome change from the quad-burning descent down the last part of the ridge. This time we followed the trail all the way down and found a cairn marking the entry to the ridge. In the late afternoon, the wind finally stopped blowing; we took another rest, lounging on the rocks and basking in the sun before our flat and long walk across the sand. Colors became more vibrant as we walked toward the sun lowering toward the hulk of mountains across the valley. The light yellow sand we walked in the morning was now a deep golden hue, and the sky above Pinto Mountain now held wispy light gray clouds, tinged with purple. I turned a few times to watch the light changes on Pinto; the white summit, where we had just been a few hours ago, was glowing. The next time I turned around, it was blue-gray in the dusk shadow. The temperature dropped as we walked across soft sand, avoiding burrows. Getting back to the parking lot and throwing off boots, a few cars drove up and people got out to snap a quick photo of Pinto. We got to be on top of that beautiful place today. We were the lucky ones - three friends who like to hike together. "It is enough to know why I came here: to breathe in the solitude and the silence." - Ann Zwinger, Wind in the Rock: The Canyonlands of Southeastern Utah  On the way down - Scott and Fred - descend ridge to the left with saddles in between high points  Late afternoon sun and deep red hues of barrel cactus  Not officially dunes, but an accumulation of blowing sand adjacent to mountain range   Pinto Mountain in late afternoon - "dunes" in foreground References
Cross-country hike to summit of Monument Mountain with expansive views in Joshua Tree National Park, and some of the oldest rocks in California.
Trip Stats (from Pinkham Canyon Road approach, off of Cottonwood Springs Road)
Geology
 Yucca and cholla cactus Near Pinkham Canyon Road looking southeast toward Cottonwood Mountains, southern part of Joshua Tree Wilderness "Mind expanding" is what designer Jonathan Adler calls Joshua Tree. For those who have traveled deserts in Southern California, hiked the dry washes, climbed rust-red and brown rocks and seen valleys that extend nearly to the horizon backed by mountain ranges, Joshua Tree is a special place. It's an expansive and sublime wonderland. It was our long-time friend Scott's idea to summit Monument Mountain in southern Joshua Tree National Park around New Year's Eve 2017. Scott has hiked many peaks on the Desert Peaks Section Peak List, and he has tons of experience hiking cross country. The views from the mountain's south ridge are incredible, and about 1/2 way to the summit, if you turn around and look to the south, you can see the Salton Sea, a large lake formed from overflow of the Colorado river when engineers in 1905 were attempting to deliver more water to irrigation canals . The weather was perfect: sunny, no wind, and 70 degrees. Fred and I had arrived from Boise for our yearly desert holiday fix. After driving up Cottonwood Springs Road from Joshua Tree NP's southern entrance, we headed left (west) onto the sand/gravel Pinkham Canyon Road that begins adjacent from the Cottonwood Visitors Center. The road was in good condition, but I would still recommend a 4-wheel drive vehicle because there was soft sand in parts. We piled out of Scott's red pick-up 5 miles down Pinkham Canyon Road and stood in a sun-flooded broad valley of yucca, cholla and creosote surrounded by mountain ranges on all sides. Looking north to our destination, we could see our ridge to the summit, but Monument Mountain was not in view. We started walking across the wash due north.  Our route down from summit of Monument Mountain from Pinkham Canyon Road (black dashed line), Joshua Tree NP (North at top of map)  Google Earth image of our two routes: pink line represents our ascent to main ridge trail; Blue line represents our descent. On our way down, we took a ridge to the west and then joined back on the main trail (seen on map at upper "loop"). The blue line route down is easiest: the path wasn't apparent when we started. We parked ~ 5 miles down Pinkham Canyon Road (bottom of image). click on map for larger image  View to the north of the Monument Mountain's south ridge. Cross the wash and head for toe of ridge  From edge of wash, climb up first hill to the south ridge of Monument Mountain The flatter valley wash soon turns into an alluvial fan with larger rocks and braided channels at the toe of the ridge. As you look north, you see a rise and it is best to get to the top of it and onto the ridge as soon as possible; that will take you to the top of Monument Mountain. Walking on the ridge is pleasant with less vegetation and rocks to navigate than walking on the slopes beneath the ridge. The trail on top of the ridge is faint and marked at somewhat regular intervals with small cairns. Once on the ridge, the route is a gentle rolling climb to the summit cone of rocks with washes on both sides. Some dry washes have deep rock cuts at the top. As seen from the Google Earth map above, we took a less efficient way up (pink line), side-hilling and navigating rocks. Sometimes you don't figure out the "right" way up until you go down!  Fred ascending to ridge from Pinkham Canyon Road in valley below  Looking at Monument Mountain summit, 4,837 feet elevation About 2/3 of hike distance, (1.7 - 2.0 miles), Monument Mountain finally comes into view. You can see faint trail leading up to the ridge after descending slightly down from the ridge into a broad sloping valley on your left and a saddle to your right. The climb up the stable metamorphic rocks to the summit is relatively easy. Nothing matches the feeling of so much desert around you, and unobstructed, airy 360-degree views.  Augen gneiss - some of the oldest rocks in California at early and middle Proterozoic age  Monument Mountain summit  Augen gneiss at summit of Monument Mountain, some of the oldest rocks in California, age 1.65 bya (billion years ago) Light-colored feldspar mineral fragments in metamorphic rock  The survey marker on Monument Mountain is a triangulation station (or main station), as indicated by the triangle inscribed in the middle of the disc. This is surrounded by three other survey markers in distant locations that have inscribed arrows that point directly back to this main station. Upon reaching the summit, we were somewhat surprised to see 2 people from the San Francisco Bay area that had hiked up via Porcupine Wash, from the northeast direction. I was surprised because this peak is so isolated and is located in the wilderness area. When I exclaimed, "There's the red can!", one of them commented that it was just trash left on a mountain. I explained to him that it was a summit register, whereupon he signed his name. I told him that the register at Cowboy Camp in the Santa Rosa Mountains still had the entry I had written almost 20 years ago! Mt. San Jacinto, the towering presence over Palm Springs can be seen to the west. The rock at the summit looks and feels old because it is old! These rocks record the earliest geologic events in Joshua Tree National Park - originated as sedimentary and igneous rocks that underwent metamorphism and then a couple of continent-building episodes finally to be uplifted during the Mesozoic tectonic events where it became fragmented. There are 4 units of this metamorphic complex within Joshua Tree. The augen gneiss on Monument Mountain is a metamorphic granite containing elliptically-shaped feldspar porphyroclasts in its layering (augen in German means "eye"). You can see these lighter grains of feldspar embedded in the dark rock. This type of rock has undergone Uranium-Lead geochronology from the zircon grains it contains to arrive at a date of 1.65 billion years ago, making these some of the oldest-known rocks in California.   Scott, Sue and Fred on summit of Monument Mountain  View to the south of the Salton Sea from the summit  View from the summit to the southeast  Red Barrel Cactus Ferocactus cylindraceus  Scott next to summit register, Eagle Mountains in the distance   Heading down; we ascended on faint path seen to the right side of the ridge in this photo The way down is straightforward - follow the ridge! This is a good first-time cross country hike for the hiker that wants to get off a well-trodden path and do some fairly easy navigation with a good topo map. There's a smaller ridge to the right (southwest) as you head down and we took it for a little while about 1/2 mile down, but then got back on the main ridge. To avoid being pulled off the ridge and side-hilling over rock-cluttered and vegetation-thick (watch for the cactus spines!), sighting in the next cairn as one is passed is helpful. As we got closer to the valley, we got sucked into a canyon - easy to do if you get off the ridge. By this time, we could see a glint of sunlight off the truck that was far across the wash. Further down we regained the ridge that at its end was a broad slope we descended easily to the alluvial fan and then finally to the wash. The walk across the broad valley passes over many small channels, through cholla and yucca. Once we finally found the truck on Pinkham Canyon Road, we savored the setting sun illuminating the cholla cactus making them glow among the yucca and creosote.   References
Kaiser, J. 2017. How Geology formed Joshua Tree National Park. Retrieved from https://jameskaiser.com/joshua-tree-guide/geology/ Powell, Robert E. 2001. Geologic Map And Digital Database of the Porcupine Wash 7.5 minute quadrangle, Riverside County, California, U.S. Geological Survey Open-file Report 01-030, scale 1:24,000, U.S. Dept. of the Interior, U.S. Geological Survey. Trent, D.D. 1998. Geology of Joshua Tree National Park, from California Geology, Dept. of Conservation, Divsion of Mines and Geology. Roger Keezer, Coachella Valley Hiking Club hike leader, Search and Rescue Volunteer for Riverside County Sheriff, and great friend conceived the phrase, "Cactus to Clouds", a now well-known extreme hike. Fred and I recently hiked with his wife, Maria, to his memorial in the mountains near Palm Springs, California.  I've a vague memory of the first time I met Roger and Maria Keezer 26 years ago. We were among other hiking enthusiasts invited to the first meeting of the Coachella Valley Hiking Club, founded by Philip Ferranti. Ideas for a new hiking club were being considered: what kind of hikes should we offer, to where, how do we rate their difficulty, and who wants to be a hike leader? Etched in my memory, however, is Roger's silhouette as he climbed in front of the sun and up the steep side of a mountain, walking stick in hand, pack on his back, with shade from a canvas brimmed hat. He wasn't a big man, but he could take long strides and climb like a mountain goat as we trailed behind him, our legs burning and hearts pounding. I still marvel at Roger and Maria's strength and endurance, and their hiking accomplishments. They celebrated Roger's milestone years of 70 and 75 hiking rim-to-rim the Grand Canyon one day, turning around and hiking back the next day. To do this, you must be fit, as Roger and Maria were. Walking from the North Rim to the South Rim is ~ 22 miles with a 6,000 foot elevation loss followed by a 4,500-foot climb out of the canyon. They were "rim-to-rimmers" before that term became popular.  Roger and Maria Keezer, on summit of Quail Mountain, the highest in Joshua Tree National Park Roger Keezer conceived the name for arguably the toughest hike in America - an extreme physical test that climbs from Palm Springs to the top of Mt. San Jacinto in one day - a 10,300 foot heart-pounding gain. In 1993, six of us, including Roger and Maria, completed this hike. When I asked for a name for t-shirts to commemorate this extreme hike, Roger quietly said, "Cactus to Clouds". Our event was then dubbed the "First Cactus to Clouds Challenge". This hike is on many an extreme hiker's and runner's bucket list.  First Cactus to Clouds Challenge - Summit of Mt. San Jacinto - 1993 (Roger and Maria Keezer standing 3rd and 4th from left)  On trail near Palm Springs, California Joyous to be out of the Boise snow this winter, Fred and I hiked with Maria under a warm desert sun near Palm Springs, California to a place where we celebrate Roger's memory on one of his favorite trails - a place that meant a lot to Roger. It is here that friends and family remember Roger with cards, photos, valentines and poems. So wonderful were many things on this hike: the sun warming the cool morning, the scent of creosotes, the satisfying crunch of gravel under foot, and especially walking on the trail again with Maria. But, oh, do I miss Roger's determined steps and gentle spirit!  Remembering Roger Roger and Maria started their hiking career after retiring from Lucky Stores in 1992. We all became hike leaders with the Coachella Valley Hiking Club. After many hikes, many miles, many stories, many awesome mountain top views, much sweat and effort, our friendship endures. Quick-paced with stick in hand and pack on her back, Maria still marches up and down desert trails, and I'm still trying not to fall behind.  Maria Keezer still hikes steady and strong Roger didn't talk much about himself. It was a few years after I met Roger that he told us he was a submariner during his Navy days. He was a quiet man with a gentle laugh, who could serve up a great-tasting tequila shot for hors d'oeuvres, followed by the most perfectly grilled tri-tip for dinner. He had a beautiful mint-condition 1965 Ford Mustang Fastback that he and Maria took on "Mustangs Across America" - a trip from Las Vegas to Charlotte, North Carolina.  Fred, Sue and Maria near Palm Springs, California  California Barrel Cactus - Ferocactus cylindraceus Roger often had interesting stories about helping to rescue lost people in the Coachella Valley and San Jacinto Wilderness when he was a volunteer with Riverside County Sheriff. Those were the happy stories, however, there were also the stories of body recoveries.  Wildhorse Trail near Indian Canyons, Palm Springs, California    "Teddy Bear" Cholla - Cylindropuntia bigelovii  Maria and Roger Keezer, Ray Wilson, Scott Tanner, Fred Birnbaum on Art Smith Trail, Palm Desert, California Christmas time  The view from Roger's memorial is stunning. I could see many places we had all hiked together in the washes and mountains surrounding us. The air was clear and the sun high as we stood and reminisced about the last 25 years of our friendship - and Roger's life. It's good to know there is a particular place we can go to remember Roger, although for me his spirit is still present in and around the desert mountains that he loved so much.  View of Mt. San Jacinto Wilderness from the top of Murray Peak, Coachella Valley, California Maria and Roger Keezer, Fred Birnbaum   Roger Keezer
September 23, 1929 - August 22, 2015 We love you always |
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About this blogExploration 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.
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