Editorial note: trail details in this Report were extensively revised on Monday 23rd February, compared to the earlier version from 21st, following my loop hike that allowed assessment of most of the major high country trails. An hour either side of sunrise I was able to comfortably bareboot up Devil’s Slide Trail to 9000 ft (top of “Angel’s Glide”, PCT Mile 180). At that point I switched to snowshoes, keeping those on all the way to San Jacinto Peak and down Deer Springs Trail to 6000 ft.
With such a rapid rise in temperatures, snow conditions are changing dramatically on several time scales; weekly, daily, and even hourly. Well-prepared hikers will account for these changes and will consequently enjoy their hike much more. Underfoot conditions are already significantly different now compared to three days ago, and will change even further over the course of the next (unseasonably warm) week. Snow firm enough for barebooting (or spikes) early in the morning is turning into soft slop by late morning, for which snowshoes are invaluable.
Three snow storms in very quick succession impacted the region across four days on 16th-19th February. Although technically three separate storms, the impact on the mountain and trail system has functioned as one major storm, with the most substantial (so far) snowfall of winter 2025/26, especially at mid elevations.
Although the combined 26 inches of new snow around the highest peaks was desperately needed and is of course extremely welcome, this was at the lowest end of the forecast expectations, and hopes for 3-5 feet of snow were not ultimately realized.
I recorded a rather-too-lengthy video report from 10,350 ft on the east slope of San Jacinto Peak mid morning of Friday 20th February that summarizes the three storms and conditions at that time (linked here).
Snow fell in three distinct periods, on the afternoon and evening of Monday 16th, then again overnight on 17th-18th, followed by a much more minor snowfall on the evening of Thursday 19th. As was widely forecast this latest storm pattern was significantly colder than others so far this season, with freeze levels more typical of the historical average (at or below 5000 ft for much of the storm period). Consequently there was considerable snowfall at mid elevations, with the first snow of the winter recorded, for example, in Idyllwild (12.5 inches at 5550 ft across the four days), and with all three storms dusting down into Garner Valley (4400 ft).
As is increasingly the trend with a rapidly changing climate in recent years, there was relatively little difference in snowfall between the mid and upper elevations, with 12.5 inches measured in Idyllwild (at 5550 ft) through to 26 inches at San Jacinto Peak (10,810 ft). Locations on the western side of the mountain range, especially those in and around Strawberry Valley, received disproportionately more snowfall, as those areas were “socked in” by storms originating from the south-west, while the highest elevations were, at times, above the cloud.
Snow depths are currently ideal for snowshoeing everywhere above about 9000 ft at all times, much lower as snow softens by mid morning (late morning in sheltered areas). Elsewhere, and in addition, spikes are recommended for the foreseeable future as established trails will eventually become consolidated by hiker traffic and will undergo freeze-thaw cycles.
Cautious navigation is strongly recommended everywhere. Even where well-traveled tracks are in place, they may not lead where you want to go (or not on the angle of terrain you would prefer to hike). As described below, some major trails have not yet been traveled at all, and that is unlikely to happen before next weekend at the earliest.
Snow depths measured at various locations on the trail system are given towards the end of this posting. Note however that snow depth itself is rarely indicative of the difficulty (or ease) of hiking a particular track or trail. For example a firm, well-compacted track across snow several feet deep may be much easier hiking than traversing across just a few inches depth of angled virgin icy snow.
The USFS gate at Humber Park closed on 18th February. While theoretically nine legal parking spaces remain immediately below the gate, an unconventional ploughing approach during these latest storms has left space for only 2-4 vehicles to safely park. Conditions in the area are very icy and currently only suitable for 4WD/AWD vehicles anyway, so this area is best avoided in the absence of further ploughing. Parking on Forest Drive, just below the Fern Valley Water District facility, is strongly recommended.
Black Mountain Road (4S01) is closed at the gate 1.7 miles up from Highway 243. Following superficial grading late in 2025 the road is in better condition than last summer, but remains far rougher than in June 2020, the last time it was thoroughly graded. South Ridge Road (5S11) closed on 22nd February.
Daily survey hikes by the Trail Report year-round in the San Jacinto mountains include multiple routes to the highest peaks including San Jacinto Peak typically 2-3 times per week (but almost daily during winter storm weather), Tahquitz Peak and area at least once per week, plus a wide variety of other trails on intervening days.

WEATHER
Temperatures rise rapidly starting Friday 20th, and will be far above seasonal in the last week of February (likely record-breaking warmth on Friday 27th at all elevations). Temperatures are forecast to be above freezing >10,000 ft elevation for the remainder of the month, and with clear, sunny days expected, melting of snow will be very rapid, especially on sun-exposed slopes. Temperatures are tentatively forecast to cool closer to seasonal in the first week of March, but by then much of the damage (in terms of snowmelt) will have been done.
The storm system on 16th-19th February consisted of three distinct phases, with the majority of the snow in the high country in the first storm, overnight on 16th. At mid elevations, the first phase was mild enough to initially produce rain, with 0.57 inches in Idyllwild, before turning to snow around dusk on 16th. The second phase was overnight on 17th, with bulk of the high country snow actually falling in the early hours of Wednesday 18th (about half the depth of the previous day). Finally the third storm passed through on Thursday 19th, with much lighter snow falling throughout much of the day, from late morning until just after dusk.
At San Jacinto Peak (10,810 ft/3295 m) on Monday 23rd February 2026 at 0930 the air temperature was 41.7°F (5°C),with a windchill temperature of 33.3°F (1°C), 28% relative humidity, and a light WNW wind sustained at 6 mph gusting to 10.4 mph.
At the Peak on Friday 20th February 2026 at 0740 the air temperature was 17.8°F (-8°C),with a windchill temperature of -7.1°F (-22°C), 49% relative humidity, and a wild WNW wind sustained at 22 mph gusting to 36.2 mph.
At the Peak on Thursday 19th February 2026 at 1010 the air temperature was 15.3°F (-9°C), with a windchill temperature of -6.2°F (-21°C), 100% relative humidity, and a frigid WSW wind sustained at 14 mph gusting to 22.3 mph.
At the Peak on Tuesday 17th February 2026 at 0830 the air temperature was 11.0°F (-12°C), with a windchill temperature of -11.2°F (-24°C), 100% relative humidity, and a steady due West wind sustained at 18 mph gusting to 24.2 mph.
At the Peak on Monday 16th February 2026 at 1410 the air temperature was 23.9°F (-5°C), with a windchill temperature of 5.5 °F (-15°C), 100% relative humidity, and a subdued SW wind sustained at 12 mph gusting to 21.1 mph.

TRAIL CONDITIONS
All trails above about 6500 ft are completely snow-covered, and largely snow-covered above 5500 ft. By the afternoon of Friday 20th, melting was already well underway below 7000 ft, and by Monday 23rd, all elevations had already lost 2-4 inches of snow to melting.
Snowshoes are currently invaluable everywhere above about 9000 ft, and can be used as low as 6000 ft as snow softens dramatically by late morning, as long as depths remain sufficient at such low elevation (probably until later this week). Conversely, snowshoes are also invaluable in the most sheltered areas that have yet to experience freeze-thaw cycles and hence the snow is still relatively fresh powder (e.g., parts of upper Deer Springs Trail, and either side of Annie’s Junction/PCT Mile 181).
Elsewhere (and in addition), spikes are recommended for the foreseeable future everywhere above 6000 ft due to localized icing, and as established trails become increasingly consolidated by hiker traffic and undergo freeze-thaw cycles. Crampons are an option in the high country for the next few days, especially in the morning when snow remains firm, but warming is forecast to be so rapid that severe postholing will soon become a problem.
In prior winters I have mentioned the challenges of hard, icy snow underfoot and the value of using spikes especially for descending and traversing. Snow at all elevations will become increasingly firm and icy following multiple freeze-thaw cycles, and I cannot overemphasize the importance of having both appropriate equipment and the right skill set for the terrain. The latter includes interpreting the snow/ice conditions, understanding your physical and mental abilities, and conservative decision making. These concerns may steadily increase over the next couple of weeks with dramatically rising then falling temperatures, seasonally stronger insolation, and highly variable snowmelt.
Ernie Maxwell Trail [surveyed 22nd February] has a surprisingly lightly traveled track to follow through continuous light snow cover. Spikes are recommended.
Devil’s Slide Trail [surveyed 23rd February] has a well-defined track to follow through continuous icy snow. Spikes are recommended, at least for descending, but are not critical for morning ascending when the snow is firm.
Wellman Trail [surveyed 23rd February] has only a lightly traveled snowshoe track along its entire length, with only my own tracks (from 20th and 23rd) between Wellman’s Cienega and Wellman Divide. Nevertheless the route is easy to follow. Snowshoes are ideal for the southern section (in the forest and hence still powdery) and for the switchbacks (sun-exposed with soft snow by mid morning).
Almost all of the Peak Trail [surveyed 23rd February] has been very well-traveled, although in places the most heavily traveled track does not accurately follow the trail route (although my snowshoe tracks from 20th remain readily apparent). There is a well-compacted posthole and snowshoe route from Wellman Divide to about 10,000 ft. As is traditional after a reasonable fresh snowfall, the weekend tram traffic has created a myriad mess of tracks above 10,000 ft. Two different well-traveled snowshoe tracks join the Peak Trail here from Tamarack (roughly following the “Sid Davis” route), and two more join just below Miller Peak (near 10,400 ft). Multiple well-traveled posthole, ski, and snowshoe tracks include one that largely follows the uppermost traverse of the Peak Trail to Summit Junction (meeting Deer Springs Trail).
A well-traveled and well-defined compacted snowshoe track broadly follows the East Ridge Trail route from near the Miller switchback (10,400 ft) to San Jacinto Peak, and is an excellent alternative to the upper Peak Trail.
The Round Valley Trail [surveyed 23rd February] has a well-traveled snowshoe and posthole track through continuous moderate depth snow from Long Valley to Wellman Divide. Multiple alternate tracks turn off to head more directly up to the Peak Trail, as described above.
Deer Springs Trail [surveyed 23rd February] has a heavily-traveled posthole track to the Suicide Rock Trail junction. Thereafter the route has been lightly traveled, with the only track that exactly follows the trail route my descending snowshoe tracks from 23rd (between upper Little Round Valley [LRV] and the Suicide junction). Snow below 8600 ft (just south of the Marion junction) is very soft by about late morning and snowshoes make for a much easier hike than miles of deep postholing. From the junction with Marion Mountain Trail, a better-traveled snowshoe track exists briefly, with much of the weekend traffic turning back by the Fuller Ridge junction. A couple of snowshoe tracks and one posthole track continue toward Little Round Valley, with the lone posthole track ending about 0.5 mile below LRV. Much of the section between 8800-9500 ft is sheltered and snowshoes are invaluable through the light powder. Two snowshoe tracks pass through LRV, with only my descending track from 23rd accurately following the trail. From LRV to San Jacinto Peak there is only one known continuous track, my snowshoe tracks which descend very directly from the uppermost switchback (example photo below). I did find one other up-and-down snowshoe track just above LRV, but it was unclear whether this makes it to the Peak.
Marion Mountain Trail [surveyed 23rd February] has a moderately well-traveled snowshoe track along its entire length that largely follows the true trail route. When firm spikes are recommended, at least for descending, but later in the day and on warmer days, snowshoes are invaluable.
As of 23rd February there were no tracks through continuous snow on Seven Pines Trail, Fuller Ridge Trail (PCT Miles 185.5-190.5), or Strawberry Trail (PCT Miles 181-183).
Early on the morning of Saturday 21st we broke trail through light to moderate depth snow on South Ridge Road and South Ridge Trail to Tahquitz Peak (photos below). At that time these routes were untraveled, but by the time we descended, other hikers were postholing through rapidly softening snow at least part way to the peak. The only safety challenge was on the uppermost switchbacks above about 8400 ft, where the snow slopes were largely continuous (with no obvious trail topography), requiring significant caution for traversing. This issue will diminish as more hiker traffic generates a better-defined track.
The 0.4 mile section of South Ridge Trail from Chinquapin Flat to Tahquitz Peak currently has no track to follow through steeply angled icy snow. These icy slopes on the north side of Tahquitz Peak are notoriously treacherous. Currently crampons with an ice axe, and the requisite skills to use this equipment in high angle terrain, are critical.

SNOW DEPTHS
Snow depths measured on 16th-20th February 2026 (unless indicated otherwise) are as follows. Current total depth is the principal number given, followed (in parentheses) by details of the fresh snowfall where known. Altitudes and PCT mileages are approximate.
San Jacinto Peak (10810 ft): 26 inches, drifted 3-4 feet deep in places, notably on east and north sides, especially East Ridge (14 inches on 16th, 7 inches on 17th, 5 inches on 18th)[patchy icy snow persisting from storms in late November was a negligible 0-3 inches deep]
Little Round Valley (9750 ft): 23 inches, drifted to 30-35 inches in places (measured 23rd February)
Wellman Divide (9700 ft): 20 inches (9 inches on 16th, 8 inches on 17th, 3 inches on 19th)
Annie’s Junction/PCT Mile 181 (9020 ft): 27 inches (13 inches on 16th, 10 inches on 17th, 4 inches on 19th)
Tahquitz Peak (8836 ft): 23 inches (measured on 21st, heavily drifted in this exposed location)
Long Valley (8500 ft): 14 inches (8 inches on 16th, 4 inches on 17th, 2 inches on 19th)
Strawberry Junction/PCT Mile 183 (8100 ft): 15 inches (measured 23rd February)
Saddle Junction/PCT Mile 179 (8070 ft): 22 inches (11 inches on 16th, 8 inches on 17th, 3 inches on 19th)
Suicide Rock/Deer Springs trails junction (7000 ft): 8 inches (measured 23rd February)
South Ridge Trail trailhead at top of South Ridge Road (6500 ft): 16 inches (measured 21st)
Devil’s Slide Trail trailhead at Humber Park (6500 ft): 17 inches (9 inches on 16th, 6 inches on 17th, 2 inches on 19th)
Idyllwild (at 5550 ft): 12.5 inches snow (6 inches on 16th, 3.5 inches on 17th, 3 inches on 19th) with 0.57 inches rain on Monday 16th preceding the snow.
Mountain Center (4500 ft): 2 inches (mainly on 16th and 19th, already largely melted).
Quinn Flat, Garner Valley (4450 ft): 1.25 inch (0.25 on 17th, melted, plus one inch on 19th).
The San Jacinto Trail Report celebrates ten years of operation in 2026. It is read by over 30,000 people each year, and will pass one million views in 2026. The Report has helped thousands of hikers, and saved multiple lives, both directly and indirectly. Since the Report became established online, snow/ice rescues in the San Jacinto Mountains have dropped 82%, also saving Riverside County tens, if not hundreds, of thousands of dollars. While all time is volunteered, the Report uses small private donations to help cover operating costs. Donations keep the Report available to all, free from advertising or paywalls, and independent from agencies. If you have found this Report useful, please consider using this link to the Donate page. Thank you for your support.












































































































































