Archives for posts with tag: springtime

Jicarita Peak from NM-76

Overview:

Jicarita Peak is a prominent, rounded mountain reaching to 12,835 feet. It forms part of the Santa Fe Mountains, a sub-range of the Sangre de Cristo Mountains, which themselves are a subrange of the Rocky Mountains. In Spanish, “jícara” means a container made from clay or the gourd-like bark encasing the jicaro’s fruit. Sometimes Jicarita is translated as “little basket”, but perhaps “little bowl” is a better fit.  There are open slopes on the highest reaches that seem to promise good glissading. This post was originally meant to explore that option. The lower mountain is still deep in snow, however, which made route finding considerably more difficult than expected. Consequently, this post describes one of many different options for tunneling through the trees on the lower slopes and then finding your way back. Spring conditions pose some extra challenges. First, it is turkey hunting season so orange attire would be a good idea. Second, Forest Service Road 161 can be blocked by trees or snow. Have a bow saw, axe and chains handy.

Driving Directions:

Driving to Jicarita Peak

  • From Interstate-25 (I-25) near Santa Fe take exit 276 for NM-599, the Santa Fe Bypass
  • After 0.2 miles, at the end of the ramp, go right onto NM- 599
  • After 13.1 miles, at a fork, go left onto the ramp for US-285/US-84 North, (towards Espanola)
  • After 0.5 miles, at the end of the ramp, merge onto US-285/US-84 North
  • After 19.1 miles, at a traffic light, go right onto La Puebla Rd
  • After 2.7 miles, at a T-intersection, go right onto NM-76 (not signed). If you plan on returning the same route then take careful note of this intersection – there isn’t much to see and it is easy to go blasting past on NM-76.
  • After 26.0 miles, at T-intersection, go right onto NM-75. NM-76 makes a long, steep climb into the town of Truchas where it makes an abrupt, 90-degree turn to the left. This turn is signed, but it is so uncharacteristic that it would be easy to miss.
  • After 7.0 miles, at a T-intersection, go right onto NM-518.
  • After 13.8 miles go right onto Forest Service Road 161 (FS-161, signed). The road turns to gravel immediately after the cattle-guard.
  • After 2.5 miles, at the end of the road, arrive at the trailhead.

It is springtime and FS-161 has patches of snow on it. If you drive a four-wheel-drive truck or Jeep then that snow won’t pose much of a problem, but some of the patches were a challenge for the low-slung Camry. In the morning the patches were frozen solid and chains were needed. In the afternoon the patches were soft enough to drive over.

Trailhead:

The mighty, if somewhat battered, Camry finally at the trailhead.

The trailhead is a wide gravel parking area with posts demarking parking spots for trucks dragging horse trailers. Leave as much space as possible for the trailers since it takes a lot of room to swing them into position. There are no fees, no vault toilets and no water services. There is a signboard to the left of the departing trail.

Data:

Starburst icons in the map indicate points where I turned back, (see the description, below).

  • Starting Elevation: 10,380 feet
  • Ending Elevation: 11,840 feet (arbitrary turn-around point)
  • Net Elevation: 1460 feet
  • Maps: USGS Jicarita Peak quadrangle. (Use the 1995 version as it shows trails that are missing from new editions. Declination has shifted from the legend’s 10-degrees to 8.2-degrees.).
  • Distance: 2.8 miles (one way to the turn-around point, without the side trips)

Hike Description:

A sign that you’ve passed the Santa Barbara junction, go back!

From the parking lot head west along a broad two-track for about 400 feet to come to an intersection (signed). The Angostura Trail #493 goes to your right and the Serpent Lake Trail and the Santa Barbara trail go left. Go left on the Serpent Lake Trail/Santa Barbara Trail. These two trails diverge in just a short distance, but the junction is not signed and snow can mask the intersection. In fact, it is easy to go past this junction. The other trail, to Serpent Lake, follows a two-track that is much more obvious than the light tread of the Santa Barbara trail. The map shows that I followed the “obvious” two-track all the way to the intersection with Agnostura Cutoff #19A (signed, fortunately, see photo above) before returning to scout the Santa Barbara junction. If you think you’ve gone too far on the Serpent Lake trail then return to the sign for Santa Barbara/Serpent Lake/Angostura and re-ascend for 200 feet (a bit more than 100 single-steps). On your left you should see the steep end of a rib dropping to the trail, creating an amphitheater-like opening in the woods. Ascend into the amphitheater.

View straight downhill across the La Sierra ditch

Rising up through the amphitheater, come to a bench in the terrain and find an astonishing flow of water called the La Sierra Ditch (sometimes “Holman Ditch”). This is an acequia, a community water project with recognized legal rights that in this case date back to 1717. Natural streams flow mostly down hill. This aqueduct takes water from Rito Angostura and traverses laterally across the broad slopes of Jicarita Peak, delivering water to farms in the Holman Valley. The water flow is brisk at this time of year and it takes a leap to cross.

View, to your right as you ascend, into the drainage

Above the ditch you will find yourself on a steep-sided rib where the sun can penetrate. There may be patches of bare ground with stretches of trail sign. To your right is a fall-off into a small, unnamed drainage. You should be close to, but (oddly) not on, the rib-top. You might think of rib-tops as the preferred locale for trail builders, but much bush whacking failed to find any evidence that that the trail was up there. Instead, ascend the rib staying close to where the terrain falls off sharply into the drainage. The route heads south initially but soon bends towards the west (i.e. curving to your right on ascent). This sharp-sided drainage is a surprisingly reliable guide for the lower half of the trip. You can ascend with confidence to about 11,200 feet where the waterway becomes a mere gully. Even under snow the gully is still evident and can be followed for another few hundred feet. Here, however, the snow masks the waterway amidst the “pit and mound” microterrain that is characteristic of conifer forests. There certainly are a lot of conifer, Corkbark fir and Engelmann spruce testify to your location in the Hudsonian life zone. At this elevation the slope of the mountainside is so gentle that it is an open question as to which direction is “directly uphill”.

Typical view: shallow slope, much snow and many conifers

When the gully disappears you will will have few obvious markers for your path. A look at the map will show that you’re not far from the large bowl that contains Serpent Lake, which should be easily recognizable. To get there you will need to contour north of a knoll denoted as Point 10899 on the USGS map. Pull out a compass, check for a declination of 8.2-degrees East  and begin heading straight west, keeping a sharp eye for any landmarks you might use on descent. You may run into a large and steep sided hummock at 11,500 feet (there are many hummocks, but this one is prominent enough to work as a landmark on descent). For the sake of having a landmark, stay at the bottom of the hummock and allow it to guide you for about 100 yards south of west. When the terrain returns to pit-and-mound, take a bearing of 315 degrees (to the northwest) to correct your course.

Yet more exciting views of snow and conifer.

On this bearing from the high end of the hummock (at about 2.4 miles from the trailhead and 11,600 feet elevation) I came across the Santa Barbara trail. At this unplanned junction the trail is sufficiently wide and boldly-enough blazed to be recognized. You may not have the same luck! My GPS track indicates that I either crossed the Santa Barbara trail or ascended along it four or five times earlier and never picked up on that fact. Trails lose their obvious qualities when snow-shrouded. Still, it is still worth knowing that the slopes just northwest of Point 10899 have trail-beds so prominent that they can be scouted.

Trail sign found above the ascent-line’s junction with the Santa Barbara trail

If you find the trail then follow it as it rises southwest. (Otherwise, you could continue north of Point 10899 and enter the basin). Trail-finding here demands that you follow blazes. Blazes can be unambiguous, especially when the trail-makers put blazes on both sides of the tree. These are a great reassurance for the navigator. In many cases, however, blazes are found on just one side of the tree. These blazes are old and the thick ring of bark surrounding each blaze looks little different than ordinary bark damage. In some cases the blazes have been painted a much-faded red but in at least one case there was a blue-painted blaze. Most blazes, however, are a shade of anonymous “tree-injury brown”. Trail finding is faster than forest-navigation, but it is not fast. If you arrive at point 10899 and you’ve reached your turn-around time then take heed. On this date I tried following the blazed trail back to the car (as the map shows) but wound up losing the blazes. I had to turn back to the junction and return along the ascent route. Keep your eyes and options open, keep your map handy and have fun!

Recommendations:

Two-track as it leaves the trailhead for the woods

The potential for getting lost on this sojourn is unusually high. I brought a GPS, a cellphone with a GPS app, an altimeter watch, and a map and a compass. The watch, compass and map were kept ready-to-hand for about 90-percent of the hike. The main concern is how to find your way down through the trees once you’ve summited. There aren’t many distinctive landmarks in that forest. Also, don’t discount the possibility of white-out conditions above tree line. If that happens then the return back to the trailhead will be even more demanding. If you have any weather concerns then consider bringing wands to mark your route above tree line.

Don’t count on being able to follow your tracks down the hill. In direct sun the melt-out of your tracks can happen in a matter of hours. As they melt out they lose contrast. Moving from bright sunlight into dark shadow confuses the eye and makes tracking harder. When you do find stretches of footprints you will want to be able to distinguish your boot tread from the tread of other hikers and hunters.

As mentioned in the hike description, there were many stretches on the trail where the axe-blazes were difficult to follow. Delusions of adequacy can be painfully spotlighted in this exercise. The decision to turn around on descent and find my way back via the ascent route was both correct and unsettling.

This has been mentioned twice already, but in the spirit of having a good checklist let me repeat that it pays to have chains, shovel, axe and a bow-saw in your vehicle. I sawed through two small trees and was surprised at what it cost me (having forgotten that this exercise occurred at well above the 9000-foot level). The forest has been hammered by drought and beetles, snow and wind. It would not be out of line to bring a chainsaw, if you have one.

Sun exposure was not bad in the forest, but UV radiation is often intense above tree line. You will want high-SPF sunscreen and lip balm, a broad-rim hat and possibly a bandana if you climb into the high tundra.

I got through one liter of water on this hike and was happy to have brought along just two. More is better in the warmer seasons.

Links:

Sign at junction where the two-track meets the trail system.

Station KRQE has images of a late-May storm including one of abundant new snowfall on Jicarita Peak.

Summit Post has a page with driving directions and seasonal suggestions. The Climber’s Log link has comments about early season snowfall, late season snowfall, mid season thunderstorms and comments on the shallow slope angle on this high peak.

The Albuquerque Hiking & Outdoor Meetup organized a hike in September, 2012.  The photos show this hike as it appears at the end of monsoon season.

There is a detail trail description in a trip report from the Los Alamos Mountaineers. The photo of the open terrain surrounding Serpent Lake (in warm weather) might be useful for navigation.

SummitPost also has a useful description is of a spring-time ski down Jicarita. There are good photos showing conditions comparable to those encountered on this hike. The authors describe getting a little misplaced, needing to follow GPS instructions to get back to the car. GPS are wonderful and lifesaving devices. Use them. Part of the mission at Meanders, however, is to encourage all hikers to explore as if they batteries had already expired in these delicate electronic items. Situational awareness matters.

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Bighorn at Wheeler Summit (photo credit: John Vitagliano)

Overview:

In summer this, the shortest trail to the highest point in New Mexico, is as graced with hikers as it is with superlatives. In springtime, the trail sees fewer footprints. This is understandable since the flanks of Wheeler Peak form open and obvious avalanche terrain. The glissading potential, however, is fantastic. You sit on the snow and glide down 1200 feet in a matter of a minutes – pure exhilaration. Striking a risk/reward balance is a matter of personal taste and responsibility. The air is thin and the demands are strenuous. You need to have an ice axe, to have practice using your ice axe, to have experience hiking off-trail and to have tracked the weather carefully. You cannot have bigger fun in the mountains.

Driving Directions:

  • Sangre de Cristo Mountains from NM 150

    From Interstate-25 (I-25) in Santa Fe, take exit 276 for NM Route 599 North.

  • After 13.2 miles take the left fork for a ramp to US Rt 84/US Rt 285 North
  • After 0.7 miles merge onto Rt 84/Rt 285 North.
  • After 21.9 miles, at a light in Espanola New Mexico where US 84/285 turns left, continue straight onto NM Rt 68 North.
  • After 49.9 miles, at a light about three miles north of Taos, go right onto Route 150. (This is a slight oversimplification. Route 68 turns into Route 64 in downtown Taos but the change is not well signed. At the northern edge of Taos, at 46.4 miles from the start of Route 68, there is a fork with a sign indicating “Taos Pueblo” to the right and Route 64 to the left. This is the first notice that I saw, northbound, indicating you’ve switched to Route 64. It is easier to think of Route 68/Route 64 as a single road.)
  • After 14.5 miles on Route 150 come to a large sign for the Taos Ski Valley. The left hand turn into the parking lot is currently forbidden (a sign indicates that it is one-way). Instead go straight for another 0.3 mile. The road bends past the ski area lodges, climbs a bit and begins to turn back into the parking lot.
  • At the high end of the parking area find a gravel road on your right with signs for Twinning Road. Turn right on Twinning road. This road is steep If it is icy then four-wheel drive will be essential. (It was dry on this date and no problem for a two-wheel drive Camry).
  • After 1.8 miles on Twinning Road (which becomes Kachina Road at some point) come to an signed intersection with Deer Lane. Turn right onto Deer and immediately left onto the trailhead signed “hiker parking”.

Trailhead:

The mighty Camry at Williams Lake Trail #62 trailhead.

There are port-a-potties and trash receptacles at the trailhead. There was no fee for parking. Bring water – there wasn’t any available at the trailhead. There was parking for about twenty cars but it was nearly full by early afternoon. You want to arrive early, anyway, to catch the best glissading conditions.

Data:

(Note on the track: on ascent I left the Williams Lake trail and headed uphill, bearing too far to the south. That put me onto sketchy terrain. I did not want to lead casual readers into that terrain, so it has been deleted out of the track shown above.)

  • Starting Elevation: 10,200
  • Ending Elevation: 13,161 feet
  • Net Elevation: 2960 feet
  • Distance: 3.1 miles (one way)
  • Maps: National Geographic “Taos Wheeler Peak”. The ascent from the Williams Lake trail to the peak (as  described here) is not shown in the usual 7.5 minute maps. The 1995 USGS Wheeler Peak map does show the trail to Williams Lake, while the 7.5 minute map from 2013 does not show any  trails at all.

Hike Description:

Junction between steep driveway and trail to Williams Lake

From the trailhead, follow Deer Lane as it passes through woods, drops slightly to a pond-laced meadow, turns sharply left around a restaurant and then bends back to the right to get around ski area buildings and the bottom of a ski lift. On this date the road was clear of snow. However, past the lift you will find the foot of a steep private driveway where the trail departs to the right. Look for the sign shown in the photo above. Here the snow became continuous and visual contact with the trail ended.

This is a trail, with the eastern rim showing above the trees.

Fortunately, you are in the bottom of a long canyon and can hardly go wrong as you parallel the canyon wall. Initially the tread follows a ski trail. Williams Lake draws many hikers, so the lower tread is packed down and quite obvious. The main trail stays to the east of the main stream bed, so when in doubt keep to the left as you ascend. In the early morning the packed snow is hard, icy and pocked with yesterday’s footprints. You’ll be glad you have traction device on your boots.

Nearly buried Lake Williams Lake Trail sign

At about 0.7 miles from the trailhead the ski run departs to the west, traversing the canyon bottom. The Williams Lake Trail dives into the trees and continues uphill. As you enter the woods you may see the sign shown at the left. Of course, if you come earlier in the season or in a year with more snow the sign could be buried. The tread generally stays close to the east wall of the canyon, although ribs on the wall or debris from old avalanches will periodically force you into the canyon’s center for short stretches.

This is not a trail, although it may look like it.

Small meadows appear from time to time. Sometimes they happen at the foot of avalanche chutes coming down from your left, offering recognizable landmarks for your return trip. It is easy to mistake yesterday’s snowboard tracks for the trail. Look for circular blue blazes (about four inches across) painted on the trees, knowing that there are a few stretches where the blazes are widely separated (or possibly under snow). As you hike along the east side, monitor the opposing (west) rim as it peeks through the trees. As you get higher those views become more numerous. Skiers descending from that rim have left dramatic tracks across the wall. Climbing further, the box-end of the canyon begins to pull into sight. The terrain takes on a rolling quality as the tread rises to the highpoint of the Williams Lake Trail.

View from the high point on the Williams Lake trail to the box-end of the canyon

In the summer a signpost would let you know where to depart from the Williams Lake trail – a short distance before the highpoint. If snow has buried the signpost then you might go past the turn-off and arrive at that high point, about 1.7 miles from the trailhead. Here you get a panoramic view of the cirque that contains Williams Lake (photo to the left). Rather than descending to the lake, turn left and begin ascending the wall. Your next task is to gain 500 feet through the trees to gain the open slopes below Wheeler Peak. You could ascend directly uphill, but as you climb you will re-encounter the blue blazes and you can follow these instead. Scout carefully. At the end of a long southerly course the blue-blazes  turned directly uphill and then switch back to the north. If you were to continue south (as I did) you will enter onto steep headwalls. This is not recommended.

Skiers standing on broad shelf (view is from the gully leading up to the shelf). Doubleclick to enlarge.

Instead, find the switchback and track the blazes as they ascend to the north. Watch for a stretch where you cross a broad, forested, swale-like declivity.  Just past the swale the blazes switchback again,  regaining a southerly bearing. The blazes the follow a long steady course of ascent, one that will bring you above tree line with views to the crest. Looking uphill  you should be able to pick out the broad gully that feeds into that swale. On the far side of that gully is a broad shelf, roughly two to three hundred feet above you. Find a convenient course to traverse back north, re-enter the wide swale for a third time and ascend to the shelf. This is a terrific spot in which to grab a bite and study the terrain towering overhead. Directly above the shelf is Walker Peak, a bump on the ridgeline that missed being the highest point in New Mexico by a mere 26 feet. To the south (right looking uphill) is Wheeler Peak. Work out a route that will ascend the snow covered face to the saddle between the two summits.

View from just below the col, keep note of the broad shelf (middle distance) for your descent.

This is also a good time to evaluate your objectives. Are your microspikes getting enough traction for safe climbing? Is the snow really, really well consolidated? Is your ice axe off your pack and in your hand? Then let the climbing begin. On this date the climbers and skiers at the shelf were enjoying near-perfect conditions. The sun had warmed the surface into an inch of corn snow. Microspikes provided perfectly acceptable footing. Under those conditions you can head straight towards the saddle. I climbed this section with John Vitaglione (a recent law school graduate), to whom I’m indebted for several of the photos shown here. The photo above shows John approaching the col, with the broad shelf about 1000 feet below him and the trails of the Taos Valley Ski Resort in the distance.

John and bighorn summiteers taking in the views. Cimarron Mountains in distance.

At the col watch carefully for possible cornices. Turn south (right as you’re coming onto the ridge) and follow the top of the ridge for another quarter mile to the gain the summit. Views abound. The Sangre de Cristo range extends north into Colorado and south to the Santa Fe Mountains. Below you to the east lies the headwaters for the east fork of the Red River. Beyond the far ridgeline lies the Moreno Valley and the Cimarron Range. To the west, across the Rio Grand, lies the north end of the Jemez Mountains. Still got that ice axe in hand? Return to the col, sit in the snow, point your feet at the canyon floor and push off. Be safe. Have fun.

Recommendations:

Author, glissading to Taos (photo credit: John Vitagliano)

It is tricky to get the timing right for this route. I was a little late getting to Wheeler this year, meaning that the snow did not quite reach to the ridgeline and some of the best glissade lines were obstructed by rocks. Apparently the Taos Ski Valley had its last day of the season on the weekend of April 2nd, about two weeks before this hike.  Closure of the resort might be a rough indicator that the time for this hike is near.

Glissading can be done without an ice axe, but it is vastly safer and far easier on your limbs if you have an axe with you. It takes practice to get used to controlling your descent. To practice, find a relatively gentle slope that has a safe run-out at its bottom. The large shelf on the trail (mentioned above) offers such terrain. Are you wearing shorts? Glissading gets cold and wet, and friction from the snow will rasp away at exposed flesh. Bring along a sacrificial pair of rain pants, preferably old and battered. Turn back if the walls of the canyon are icy.

The most obvious risk on this hike is the potential for avalanche. The snowpack should not be a complex of poorly bonded layers; you want a snowpack that has acquired a uniform and high degree of tensile strength. Starting in early March, keep a close eye on backcountry reports. Pick a different hike if the snow has been saturated by rain. The reports from the Taos Avalanche Center are invaluable, although the Center closes for the season just as the best glissading arrives. For this hike the weather had been almost entirely sunny and clear for the preceding two weeks. Snow consolidation seemed close to perfect.

On a sunny day you’ll get clobbered by UV radiation. Direct UV radiation increases markedly with altitude (see this abstract for a summary). The indirect exposure – reflection from the snow – is also intense. Lawyers, guns and money are no protection. Bring sunscreen, shades and lip balm. (Apologies to John). Protect the backs of your ears and the bottom of your nose. If you ascend in shorts then slather the backs of your knees generously.

I went through less than a liter of water, which seems pretty typical of a hike this short at this time of year. Bring micro spikes and an ice axe. I found my collapsable hiking pole, gaiters, broad brim hat and bandana to be very useful.

Glissade tracks get longer and better as more people use them. Bring lots of adventurous friends.

Links:

Even folks who live at altitude may find the air above 13,000 feet quite thin. Recent arrivals from Miami are likely to suffer. If you have new arrivals in your party then you’ll want to know the signs of acute mountain sickness. A good summary is found here.

The http://www.mountain-forecast.com site is unusual in that it recognizes that weather can vary by altitude. I haven’t used the site long enough to have a clear idea of how accurate this distinction can be. Never-the-less, I tracked their Wheeler reports in the weeks before going on this scramble.

The Taos Avalanche Center is a great, if seasonal, source of detail data on snow conditions in the region of the Taos Valley Ski Area.

The best trip reports that I’ve found have been on the Northern New Mexico Avalanche Exchange. The interface is somewhat old fashioned, but clicking on that link will take you to NNMAE home page. There, click on the “Forum” link. This presents a table of forums (including an excellent Education link). For trip reports click the “Northern New Mexico 2016-2017 Conditions” link. That will show you a table of regions in northern New Mexico, click “Taos Ski Valley“. Unfortunately it is listed in oldest-post-first, so use the list of pages (near the upper-right) to go to the last page and the most current reports.

There aren’t many other reports about trail conditions for this springtime route. There were a few “made it” comments at AllTrails and four terse sentences on the climber’s log at SummitPost.