I’ve written in great detail about Santa Lucia Firs recently so I won’t repeat myself and describe the awesomeness of this tree again. The highest concentration of Santa Lucias (by far) is in the Carmel River drainage where the rocky, rugged terrain provides an ideal fire-proof habitat for the trees to thrive. The second greatest concentration stretches from Devils Canyon up to Cone Peak, also very rugged and rocky. South of Cone Peak there are only a few isolated groves in existence, perhaps fewer than a half dozen, making each of these groves especially unique. The most accessible of these groves is located in the upper part of Villa Creek in the Silver Peak Wilderness. The Cruickshank Trail passes among the firs with good views into the canyon bottom where the firs are highly concentrated. As I’m a Santa Lucia Fir aficionado, I decided to visit a more remote stand that has piqued my interest ever since I saw the familiar narrow conical crowns of the Santa Lucia Firs from a nearby ridge. Since the grove is tucked away in a hanging valley with no easy access I decided to name it the Lost Grove. Unlike the larger stands in the Carmel River drainage and Cone Peak, the growing habitat in the Lost Grove is restricted to a narrow mile-long strip along a rocky stream. The vast majority of the trees reside on the cooler northeast facing slope and the density of firs is some of the greatest I have seen; it’s almost as if the trees are huddling together to keep cool. There is a sharp gradient between the Santa Lucia Firs and the hot chaparral slopes with only a few Coulter and gray pines mixed in. It appears destructive fire has largely avoided this grove for many years and the result is some amazing old growth trees with impressively tall spire-like crowns that epitomize the Santa Lucia Fir. A few of the firs appeared drought stressed or have already succumbed to drought so hopefully this winter’s rain will be sufficient to help these trees survive the next summer. This grove resides in a relatively hotter and drier location than most Santa Lucias so it did not come as a surprise that the effects of the drought were visible, but the vast majority of trees still appeared healthy and there were hundreds of new saplings on the shady forest floor poised to become the next generation. I also suspect that the lifespan of the Santa Lucia Fir is not all the great as every grove I have visited includes several old snags. Access to the grove entails either a moderately brushy approach from a nearby ridge with excellent views to the Pacific Ocean or a creek walk with an extended stretch of beautiful bedrock and boulder cascades.
I enjoyed last year’s Ventana (single) Cone Adventure so much that I came back to explore a new ascent route up Ventana Cone and a new descent route from Lion Rock. I climbed both peaks on the Ventana Triple Crown route last year, but in my opinion climbing Ventana Cone and Lion Rock from the Carmel River is more aesthetic as it includes some amazing creek walking, waterfalls and Santa Lucia Fir groves. Both routes went as planned and proved to be efficient ways to climb both Ventana Cone and Lion Rock with relatively light brush in a trail-less region where bushwhacking is notoriously arduous. Ventana Cone is not visited very often (I was the first entry of 2016) and Lion Rock is visited even less frequently with only on a few parties known to have stood on its rocky summit in the last several decades. The stretch from Kandlbinder to Ventana Cone is the most rugged and wild region in all of the Ventana (and arguably the coastal ranges of the West Coast) so it is always a pleasure to visit this area. As with last year, the first part of the morning entailed running the Carmel River Trail from Los Padres Dam traveling nearly 10 miles deep into the canyon to Hiding Canyon Camp, a nice camp with Santa Lucia Firs and a tall ponderosa pine. Another 1.5 miles leads to Round Rock Camp. The trail to Round Rock Camp has some brush and blowdowns but still seems faster than walking in the river. Beyond Round Rock Camp is all off-trail, mostly creek-walking through a stunningly beautiful canyon of turqoise pools, slick rock, cascades, house-sized boulders, ferns, and moss. The amazing lushness of this deep canyon with several different varieties of ferns, and moss covering virtually everything creates a scene fit for Jurassic Park. Almost everything is photogenic. However, unlike last year, I took the first creek that enters the main tributary instead of continuing to the head of the canyon (my return route would include the entire canyon). This small creek does not produce enough flow to clear out the riparian brush so it is difficult in its lower reaches and I found much progress on the slopes above the stream bed. Eventually the stream opens up into a long talus field, at first under oak trees but increasingly a Santa Lucia Fir forest as one ascends the steepening slopes. The old growth Santa Lucia firs in the upper part of this drainage are simply amazing. The talus staircase is fairly stable and therefore an efficient route all the way up to a high notch where one must traverse into another drainage for the final climb up to Ventana Cone. This traverse includes some light brush with the burnt vegetation being the greater impediment. A final talus slope provides efficient access to the ridge near the summit of Ventana Cone. The view from Ventana Cone was just as I had remembered it from prior visits with a 360 degree panorama taking in the entire northern part of the Santa Lucia Mountains. Close at hand are the Ventana Spires, Ventana Double Cone, Kandlbinder and Lion Rock. From Ventana Cone to Lion Rock I used the same route as I did on the Triple Crown, generally staying on the east side of the ridge in talus slopes with Santa Lucia Firs. Lion Rock is an unofficial name I gave this majrestic peak that sits at the head of Lion Creek. Lion Rock is rugged and steep on all sides and an attractive peak from every direction. In fact, it’s one of my favorites in all of the Ventana. An old scrap register was left by legendary Ventana pioneer Ward Allison and Toshi Hosaka placed a new mini-register last year (no other signatures after his visit). From Lion Rock I descended the class 3 rock face and worked north to the top of a long and steep talus slope. Unlike the earlier talus slope, this one had much smaller, looser rock and the descent was rather tedious, but still much more efficient and pleasant than a bushwhack. This talus slope continued virtually unabated for over a thousand vertical feet before I reached more more mixed terrain. As the creek picked up flow I found myself increasingly in the stream descending into the lovely canyon with bedrock cascades, fern gardens and moss covered rocks. There are several beautiful waterfalls in this drainage including Spire Falls, Lion Rock Falls, Ventana Cone Falls, Carmel Falls and the Carmel Gorge.
While the average annual number of rainy days on the central coast is not particularly notable, the terrain on Big Sur is capable of immense orographic enhancement and staggering rainfall totals when Pacific moisture and jet stream energy align with the terrain. Rises steeply from the ocean to its 5,164 ft summit, Cone Peak is particularly adept at squeezing out the moisture from clouds and when combined with its rugged and extremely steep topography you get some impressive waterfalls on the mountain’s flanks. Two such waterfalls are Vicente Falls and Limekiln Falls.
Limkiln Falls is a relatively accessible 90 ft drop at the bottom of Middle Fork Limekiln Creek. The short hike to reach the falls from the Limekiln State Park day use and camping area passes through an attractive redwood grove with a carpet of redwood sorrel and pretty cascades along Limekiln Creek. After taking the main trail along Limekiln Creek, turn right at a junction and head up the Middle Fork Limekiln Canyon to the falls, crossing the creek four times along the way. These crossings are usually dry but will be wet in higher flow with no bridges in place. The main drop is measured at 90 ft and that is all that is visible from below, but there are additional drops upstream. The falls has two distinct prongs separated by a massive mineral apron. The prongs spreading outward from the top are reminiscent of the tusks of a mammoth. In the very highest flows, this apron is entirely covered in water, but the general character of the falls is the two prongs with moss and vegetation growing on the mineral accumulation in between. Due to high visitation, vegetation at the base of the falls has been largely trampled to dirt. The falls only features a small, shallow plunge pool.
When in flow, Vicente Falls is a very pretty falls spanning 190 ft from top to bottom. The falls drains the region immediately below the southeast face of Cone Peak, which is the drier, hotter side of the mountain. Thus, appreciable flow is not the norm for this falls (especially in the last few years of drought) and the falls is light at best or more accurately a drip most of the year. However, after a heavy rain, the falls transforms into a beautiful cataract over the immense cliffs tumbling over at least four distinct drops into the redwood forest. From below, the uppermost drops are not visible, but around 120 vertical feet of the falls is visible. Similar to Limekiln Falls, the plunge pool at the base of Vicente Falls is shallow and small. Vicente Falls is located upstream of Vicente Flat in a side canyon of the main Hare Canyon. The trek up to the falls includes some photogenic cascades and small pools in a narrow canyon along with some poison oak and blowdown debris. It is interesting to note that for most of the year the main stem of Hare Canyon has higher flow but after heavy rain the side canyon containing Vicente Falls greatly exceeds the main stem. This is indicative of some large springs in the canyon along the main stem while the Vicente Falls side canyon is largely runoff based flow. Visiting Limekiln Falls, Vicente Falls, or both gives an excuse to spend some time on lovely Cone Peak, one of the centerpiece features of Big Sur with amazing vistas and scenery, some of which I’ve highlighted here. For additional waterfalls in Big Sur, see the Waterfall Project.
Another post from the fall season in the High Sierra, this time from the Hoover Wilderness to the north and east of Yosemite. The Hoover Wilderness and adjacent northern part of Yosemite is largely overlooked for the higher peaks of the Sierra Nevada to the south but features outstanding scenery and tremendous opportunity for adventure where few, if any, other people will be seen. The Hoover Wilderness is characterized by a series of deep canyons draining the east side of the Sierra Crest. The Buckeye Loop visits two of these canyons – Robinson Creek Canyon and Buckeye Canyon. The centerpiece feature of the loop is stunning Peeler Lake which is an alpine paradise of polished granite and clear blue water. Both canyons are extremely pretty with phenomenal vistas, meadows and aspen groves. The Buckeye Loop comes out to around 35 miles including several miles of dirt road from Buckeye Campground to the Twin Lakes road and then a stretch of pavement to the roads end at the Mono Village resort. A car shuttle would shorten the route considerably and avoid some of the miles along dirt and paved roads, but the road running to make a complete loop is tolerable since the views are decent throughout the road section. Complete photo album here.
From the Mono Village, find your way through the maze of RVs to the Barney Lake Trail. This trail is heavily used as the starting point for many trips into the wilderness. The trail ascends fairly gradually through conifer forest and then aspen groves to a nice meadow where one can look up the dramatic Little Slide Canyon to the Incredible Hulk rock feature, one of the most impressive walls in the High Sierra. At this point, the trail begins a moderate ascent to Barney Lake and passes through a lovely old-growth aspen grove that is spectacular during the fall color season. Beyond Barney Lake, the trail begins a more rapid ascent with numerous switchbacks. Once past the turnoff to Robinson Lakes and Rock island Pass, Peeler Lake is close at hand. Peeler Lake is a remarkably beautiful spot with granite slabs descending into the sapphire blue waters. The lake sits exactly on the crest of the Sierra Nevada and has the unique attribute of dual outlets on either side of the lake – one flowing to the Great Basin and another to the Pacific Ocean via the Tuolumne Watershed/Hetch Hetchy. Water from the same source ends up in vastly different places!! From Peeler Lake, enter Yosemite National Park and descend gradually to the northern end of Kerrick Meadow.
The duration in Yosemite is short as the route exits the national park and reenters Hoover Wilderness after a gradual climb to Buckeye Pass. Compared to the trail to Peeler Lake, the Buckeye Trail gets a fraction of the visitation. In fact, the author did not see any humans from Peeler lake all the way to the Buckeye Campground. The trail becomes faint in spots, but the way was never in doubt. Descending from Buckeye Pass into the South Fork Buckeye Creek Canyon includes beautiful views of Center Mountain, Cirque Mountain and Grouse Mountain. At the junction with the trail to Piute Meadows is an old cabin. Downstream of the trail junction is a rugged section of the creek known as “The Roughs.” After this section, the trail makes a final descent into the Big Meadow of Buckeye Creek. The meadow is aptly-named as it is immense in both length and width. The meadow includes numerous patches of aspen with some old growth groves. The creek meanders through the meadows affording lovely views of the canyon, particularly the rugged flanks of Hunewill Peak, Victoria Peak and Eagle Peak. While the last few miles to Buckeye Camp seem to drag a bit, a hot spring along Buckeye Creek can refresh spirits. The final portion of the loop along the dirt road back to the Twin Lakes Road features nice views overlooking the Bridgeport Valley. Complete photo album here.
Fall color has long been replaced by snow in the High Sierra, but this post looks back on a great trip at the height of fall color in McGee Creek Canyon. The word colorful best describes this outing from the yellow, orange and red aspen groves in the lower canyon to the sapphire blue of Big McGee Lake, the turquoise of the tarn beneath McGee Pass and the stunning geology of red, white and gray rock of the peaks. On top of all the color was a dusting of snow on the high elevations. It was a fantastic and memorable day in the mountains on a perfect autumn day! Complete photo album here (I’m now only posting a fraction of the photos on the blog).
The region between Rock Creek and Mammoth Lakes hasn’t drawn my attention as much as other parts of the range, but I thoroughly enjoyed my first visit to Red Slate Mountain in the summer of 2013 and I’ve come to appreicate the unique features of this region. While Red Slate Mountain is arguably a choss pile, I was pleasantly surprised on my first visit to this region finding gorgeous scenery so I was eager to return and see the route in the autumn. The geology of this area is especially fascinating with a palette of rock colors ranging from blazing red to pale white. Along the way we even spotted purple and green rocks. The interesting geology of the region is reflected in the series of photos below. In fact, Red Slate Mountain’s neighbor is aptly name Red & White Mountain with red and white striations throughout its face. Just to the west is the Silver Divide with quintessential gray and white granite I am accustomed to in the High Sierra. While Red Slate Mountain is not an interesting climb via the class 2 route from McGee Pass, the 360 degree view from the summit is outstanding. My favorite vantage was looking down at Lake Dorothy, Constance Lake, and the many other lakes of the Convict Creek basin but entire panorama is breathtaking. To the east the white mountains can be seen and to the south the high peaks of the Bear Creek Spire Group and Red & White Mountain. To the west lies the Silver Divide and to the north the Ritter Range. It’s a sweeping panorama and worthy of a long summit stay to soak in all of the fantastic terrain. The other highlight of the route is passing by a triumvirate of lakes leading up to McGee Pass, each becoming progressively smaller and more desolate as one ascends toward the pass. Big McGee Lake is by far the largest and most scenic with clumps of alpine trees surrounding its shores and Mount Crocker’s north face in the background. In the spring gorgeous wildflower meadows above Big McGee Lake lead to Little McGee Lake tucked in beneath the cliffs of Red & White Mountain. “Mini” McGee is the final tarn below McGee Pass, a desolate place with virtually no vegetation to speak of and crystal clear turquoise waters. This 20 mile roundtrip route makes for an excellent high altitude run as a “one-up” with 6,200+ foot gain, but all downhill on the way back. Complete photo album here.
The Hamilton Lakes and Kaweah Gap region is one of the most dramatic and inspiring spots in the High Sierra. Considering how many times over the years I’ve visited the area it’s easily among my favorite spots to explore. I consider it one of the best spots for adventure running in the Sierra Nevada with a long runnable approach, fun scrambles and most importantly, jaw-dropping scenery. I’ve climbed most of the named summits in the region over the years, including Eagle Scout Peak and Mount Stewart on separate trips, but this time I would tag both summits together since they make logical sense as a pair. While it makes for a long day, both summits are class 2 scrambles and not very far apart. On this visit I paid particular attention to timing of best light for photography and made sure to be at the right place at the right time. I spent several hours shooting photos and I hope the results reflect my efforts. On this post I’m introducing a new format for this blog – from now on I’m going to only post a few highlight photos from each adventure in the body of the post with a link to a full album on Google Photos where it’s easier to navigate through the larger set of photos and see full size versions. The complete photo album for this trip is here. Total mileage for Eagle Scout and Mount Stewart was 50 miles, of which 40+ miles was out-and-back on the High Sierra Trail from Crescent Meadows to Kaweah Gap. The first 11 miles to Bearpaw Meadows is on well groomed trail with gentle ups and downs making it very runnable. Beyond Bearpaw Meadows the trail descends to cross Lone Pine Creek before ascending in a rocky stretch of trail to round a shoulder into the Hamilton Lakes drainage. After crossing Hamilton Creek the trail is in ascent mode all the way to Kaweah Gap but the incline is fairly moderate throughout. The Hamilton Lakes amphitheater is one of the most scenic areas in the High Sierra with towering granite faces of the Valhallas including the famous Angel Wings rock wall, Cherubim Dome, Hamilton Dome and many other sweet rock features. At the head of the amphitheater on opposite ends lies Mount Stewart and Eagle Scout Peak making them a perfect pair to tag on the same day. The area is so beautiful I haven’t figured out how to spot taking photos each time I visit, including nearly 200 photos when I did the complete High Sierra Trail for an FKT. From the beautiful sapphire blue waters of Upper Hamilton Lake the trail switchbacks before traversing to a spectacular view overlooking the lake and Angel Wings. The trail then reaches a picturesque tarn and then Precipice Lake. At aptly-named Precipice Lake, the sheer cliffs of Eagle Scout Peak tumble right into the waters of the remarkably clear lake. This stunning view was immortalized by Ansel Adams in 1932 with his shot “Frozen Lake and Cliffs.” Shortly after Precipice Lake, one reaches Kaweah Gap which opens up a new world of scenery in the upper Big Arroyo River drainage including the Nine Lake Basin and the Kaweah Range. From Kaweah Gap, go south for Eagle Scout Peak and north for Mount Stewart. Both climbs are straightforward and offer different, but both marvelous, perspectives on the Hamilton Lakes and Nine Lakes Basin areas. The view of Precipice Lake from the summit of Eagle Scout Peak is particularly inspiring. The overhanging summit block of Eagle Scout Peak is indeed the precipice with the clear blue waters of Precipice Lake 2,000 feet below the sheer cliffs. Meanwhile, Mount Stewart offers an amazing view of Sabertooth Ridge, Tamarack Lake, and the rugged north side of Black Kaweah. The complete photo album for this trip is here.
The third and final part of series of posts on a two day fastpack of the Trinity Alps High Route covers the section from Thompson Peak to the trailhead at Canyon Creek inclduing Wedding Cake, Mount Hilton and Boulder Creek Lakes. This portion of the Trinity Alps High Route was previously covered in the Trinity Alps Traverse report from 2013 and that trip served as inspiration for the Trinity Alps High Route this year. Many additional photos can be found on the 2013 post with different lighting since this section was done in reverse. The preceding two posts were as follows:
- Part I: Little Granite Peak, Smith Lake and Sawtooth Mountain
- Part II: Mirror Lake, Caesar Peak and Thompson Peak
From the summit of Thompson Peak descend the sandy southwest slopes and traverse granite benches to the short class 3 climb up a chute to the summit of Wedding Cake, which in my opinion has the best birds eye view of the Canyon Creek Lakes. After descending Wedding Cake traverse on the west side of the ridge until the crest can be easily crossed to the east side. At this point, an awesome 2+ mile “granite highway” section commences. This stretch is stunning with rugged unnamed peaks and spires towering above and sweeping views of the pristine granite slopes dropping off to the Canyon Creek Lakes below. The smooth white granite is interspersed with grassy meadow benches, krummholz and small cascading streams making for a delightful setting.
If headed for Mount Hilton, at the end of this marvelous stretch of granite slabs ascend to a high shoulder on the first of two sub-ridges that need to be crossed to access the Mount Hilton scramble. Once over this shoulder enter a smaller drainage with more talus than granite, but excellent views of the precipitous northeast buttress of Mount Hilton. After traversing through this cirque a convenient ramp can be used to pass the second sub-ridge and deposit one immediately beneath Mount Hilton (those skipping Mount Hilton could simply traverse below this sub-ridge and directly down to Boulder Creek Lakes). This ramp looks somewhat difficult from afar but in reality it’s a class 2 walk-up providing surprisingly easy passage through this barrier that would otherwise involve some tricky climbing. Once over the ridge, ascend steep alpine slopes to the foot of the final class 3 scramble portion up Mount Hilton. The summit provides an amazing vista of the surrounding mountains and an excellent overview of the Trinity Alps High Route. In particular, Sawtooth Mountain sports a particularly impressive profile across the Canyon Creek drainage. From the summit of Mount Hilton to Boulder Creek Lakes is a long and steep descent of over 3,000 feet down to the Boulder Creek Lakes. The upper part of this descent is fairly straightforward on rocks and gravel transitioning to sections of granite slabs in the middle. The lower portion of the descent requires some micro-navigating through some cliff bands and thick brush. Towards the bottom a creek bed may be used in later season to avoid most of the brush. The Boulder Creek Lakes are tucked into a granite bowl with excellent views to Little Granite Peak and Sawtooth Mountain across the canyon. Mount Hilton looms above and the granite slabs surrounding the basin create a magical setting. From Boulder Creek Lakes it’s back on trails. The initial descent to the Canyon Creek is fairly rough and rocky trail but the final few miles along the Canyon Creek Trail are relatively smooth and easy trail miles. Topping out at just over 9,000 feet, the height of the Trinity Alps is not impressive when compared with the Sierras, but their higher latitude and proximity to the Pacific Ocean allow for significant winter snow accumulation and the existence of a few small patches of permanent ice. The largest of these patches of permanent ice is immediately below Thompson Peak and contains the requisite characteristics to be classified as a true glacier. Known as the Thompson Glacier, this glacier has undergone significant reduction in thickness and surface area as shown in this comparison of photos from the summit of Thompson Peak in 2013 and 2015 (both Labor Day weekend). The ongoing drought and a warming climate mean this glacier is in jeopardy of disappearing entirely. Glaciers were an integral part of shaping the majestic Trinity Alps that we see today with the ubiquitous ice-polished granite faces that embody these mountains, but if this glacier melts away the range would be devoid of true glaciers.
- La Sportiva Ultra Raptor: built tough for off-trail travel and sticky sole for rock scrambling
- Ultimate Direction Fastpack 20: Everything you need and nothing more!
- Thermarest NeoAir sleeping pad
- Mountain Hardwear Mountain Speed sleeping bag
- Extra clothing: Windbreaker, light down jacket, light gloves, beanie (summer temperatures and a reliable weather forecast for a two day trip)
- Food: bars, pumpkin flax granola, dried fruit and meats
- Essentials like First-aid, sunscreen, chapstick etc.
- Canon Powershot S110
The Trinity Alps High Route is an excellent way to see some of the best scenery in the Trinity Alps. The Trinities may not stand out in the typical metrics used to rank mountain ranges, but the uniquely rugged granitic landscape and a true wilderness experience makes this a special spot. In fact, it’s one of my favorite areas to explore. This series of posts has described one route through these mountains, but the possibilities for wandering the lovely alpine terrain in this range are literally endless. I look forward to future trips to the Trinity Alps and hopefully uncovering more gems in this wonderful corner of California.