Willow Lakes and Salmon Lake

I’m a little bit ashamed to admit how much of my life is spent on autopilot. We all have a tendency to let ourselves get stuck in ruts: “I’m doing this because I’ve done this before and I’m used to it.” That sort of thing. I think a good portion of my choices of where to hike has been out of laziness. I continue to hike in Rocky Mountain National Park because I’m comfortable there. It’s close, I know my way around the Park, I have a first-rate guide, and so on. It only takes me an hour and a half or so to get to any east-side trailhead and about two hours for a west-side hike.

I started getting away from the Park when they instituted their timed entry pass system. I climbed out of my rut and looked around. The Indian Peaks Wilderness is close – just south of RMNP. And James Peak is adjacent to IPW. Again, trailheads for IPW and JPW are close and can be reached in about an hour and a half.

Climbing further from my rut, I finally realized just how many hiking trails I can reach in no more time than it takes to reach a west side trailhead in RMNP.

One of those trailheads is the Willowbrook trailhead in a residential area of Silverthorne. This trailhead can be used to reach Salmon Lake and Willow Lakes, in southeastern Eagles Nest Wilderness. These lakes are surrounded by the dramatic cliffs of a number of 13ers: Rain Peak, East Thorn, and Red Peak.

I don’t have a good guidebook for this area, so I’m doing my research online. I’ve been around the internet long enough to know that not everything I read there is true. I don’t generally think this is much of an issue when it comes to researching hikes, but it’s a good thing to keep in mind. For example, two resources I commonly use are AllTrails and ProTrails (those links go to their respective Salmon Lake route descriptions). AllTrails says it’s a 9.8-mile round trip to Salmon Lake but ProTrails says it’s 15.3. ProTrails would have us start at a different trailhead. I use CalTopo maps and the distances given there match AllTrails.

A couple of notes before we start. First, the parking lot here holds only about a dozen cars but there is a shuttle available. Arrive early or find the shuttle. Second, there is a large network of trails in the area and there is a series of trail junctions. For hikes where I’m not going off-trail, I don’t always carry a map. Bring a map for this one.

Thursday, August 17

I arrived at the trailhead a bit before 7:30. There were only a few cars in the parking lot, and I’m guessing those belong to backpackers who spent the night at one of the lakes. CalTopo shows trails starting at two points near the parking lot, perhaps a hundred feet apart. This is incorrect. There is only one trail from here. There’s a place to register for overnight stays in the Wilderness. There is no fee, and no registration is required for day hikes.

The trail starts in a residential area and passes through Summit County open space before reaching the Eagles Nest boundary about three-quarters of a mile. CalTopo shows four trail junctions before the boundary, but there are only two. The forest is sparse enough to allow views of Silverthorne and Dillon Reservoir and dam. Alongside the lower sections of trail, beetle-kill trees are stacked in pyramids ready for burning when there’s snow on the ground.

Shortly after entering the Wilderness, the trail meets the Gore Range Trail. For the next mile and a half, the trail passes through an interesting section of forest. At first, it reminded me of the area around Ouzel Falls about ten or fifteen years after the fire. All the big trees were dead, the living trees are no more than ten or twelve feet tall. With no big trees, the views open up.

Here, there are no signs of fire in the last century. Hiking up the trail I didn’t notice it, but on the way down you can see that all the dead trees are lined up in the same direction. Why are all the dead trees lined up so nicely?

This area was greatly affected by beetle kill quite a while ago. It was one of the first places I recall seeing beetle-kill forest. The beetles burrow into mature trees, all with trunks at least ten inches in diameter. So all the big trees die, but beetle-kill trees take a while to fall over. They go from reddish-brown to gray and finally get knocked over randomly by wind or snow over the years. And they’d fall over in all sorts of directions.

I think this area was hit by a microburst. Two or three or four minutes of very high winds. Even live trees can’t stand up to the force; this dead forest never had a chance. Any creature unfortunate to be in the area was unlikely to survive. The dead trees are so densely packed, that getting through this area without a trail would be impossible. You just can’t bushwhack through it, you’d have to detour. Truly impassable without a trail.

Because the deadfall was so dense, I couldn’t see too many stumps. But I don’t think there were as many stumps as trees. Most of the trunks looked to be snapped off at the roots.

The next trail junction is the Willow Lake trail. Here the trail starts climbing steadily and relentlessly. It’s not terribly steep, but it goes on and on at a constant rate. On the way down, even knowing how long it went on, I was surprised at how long it went on. Above the top of this grade, though, the trail mellows considerably, climbing no more than two hundred feet a mile (with one exception).

After the big climb, the trail traverses a steep valley wall and reaches the final trail junction of the hike: the Salmon Lake trail. My plan is to visit both Salmon Lake and Upper Willow Lake (and lay eyes on the other various Willow Lakes). By my reckoning, it’s 5.8 miles to Upper Willow Lake with a one-mile round-trip side trip to Salmon for a total of 12.6 miles and maybe 2,800 vertical feet.

I would do Upper Willow Lake first, and if I didn’t feel like doing Salmon it would be a good excuse to come back. Alternatively, it would make a good single-night backpacking trip.

Continuing toward Upper Willow Lake after the Salmon junction, the forest thins again, revealing the dramatic faces of the mountains and ridges containing the valley: the flank of Red Peak to the south, Capricorn, Gemini Twins, and Sagittarius to the west, and East Thorn to the north. The trail meanders along a stream and among and along four or five lakes and ponds before reaching its final destination.

I stayed at the upper lake for forty-five minutes. I had my picnic lunch first. Instead, I should have taken a bunch of pictures first. By the time I was done eating, the few puffy clouds of earlier had grown big and gray. So it goes. After lunch, I explored for a few minutes before heading back down.

Back at the junction, still feeling fresh, I headed up to Salmon Lake. This is the exception to the generally mellow nature of the trail above the big climb. Here we are on a section reminiscent of the big climb. It is mercifully shorter, but at first seems almost malicious: we have climbed a hundred feet or more above Salmon Lake.

  • hiking trail with pyramids of beetle-kill
  • view of East Thorn mountain
  • two 14ers in the distance
  • one of the several Willow Lakes
  • one of the several Willow Lakes
  • Upper Willow Lake
  • Upper Willow Lake and Zodiac Ridge
  • Dillon Lake and dam in teh distance
  • first glimpse of Salmon Lake
  • Salmon Lake

Salmon Lake, I think, is not as scenic as Upper Willow Lake. True, that’s not a low bar. The trail skirts north of the lake, avoiding a giant boulder field, dumping the hiker at the willow-choked western end. Half, or more, of the shore is talus.

By counting the number of hikers I encountered all day, I doubt the parking lot ever filled up. There were only two cars there in addition to mine when I got back to the trailhead. I didn’t meet more than a dozen hikers and backpackers.

On the hike out, I got sprinkled on a bit, just enough for me to put the raincoat on. There was a thunderstorm across the valley to the east, the thunder distinct but not nearby. I got a big dose of the solitude I enjoy. Not a bad way to spend the day.

Due to the generally sparse forest for much of the hike, the views are above average. There’s only one section of trail I found difficult. It’s certainly worthy of a return visit.

Timetable

Not an out-and-back, this hike was a Y. The stem is the base of the Y.

Hike InHike Out
Stem
Trailhead7:32 am4:54 pm
North Willow Creek jct7:50 am4:36 pm
Three Peaks jct8:06 am4:18 pm
ENW Boundary8:09 am4:15 pm
Gore Range jct8:16 am4:06 pm
Maryland Creek jct9:08 am3:03 pm
Salmon Lake jct10:13 am2:02 pm
Upper Willow Lake
Salmon Lake jct10:13 am12:55 pm
Upper Willow Lake11:13 am11:59 am
Salmon Lake
Salmon Lake jct12:55 pm2:02 pm
Salmon Lake1:15 pm1:45 pm

A few more photos are available here and here.

Clayton Lake

Imagine your left hand, palm up. The hikes in the James Peak Wilderness correspond roughly to your fingers: Rogers Pass Lake and Heart Lake would be on your thumb and Lower and Upper Forest Lakes your pinky. Clayton Lake, then, as well as the two Iceberg Lakes, would correspond to your index finger.

Back before James Peak Wilderness became part of the National Wilderness Preservation System in 2002, there were trails serving the lakes on each of your fingers. The trail to Clayton Lake, though, was “abandoned” about thirty years ago. (The trail to Arapaho Lakes was similarly abandoned a bit more recently.) According to various online resources, though, the trail still gets quite a bit of use. All these sources say the same thing: just follow the creek straight up the hill. Descriptions of this former trail are all very similar: “The creek and trail funnel through a rock-bound gulch with little room to maneuver.” “That last part was pretty hard but really cool.” “There is a section that is a bit of a steep scramble. Used my hands quite a bit through that section.” And there’s this one: “I read all the comments and they said ‘It’s hard to see the trail as it’s not maintained.’ No, the trail just completely doesn’t exist at all. I attempted and got completely lost. It was quite scary and will never do it again.”

A couple of summers ago, I ran into a volunteer and quizzed him about reaching Clayton Lake. He suggested that it’s easier to get there by going up the Crater Lakes trail to about 9400′ or 9500′ elevation, then striking cross-country from there. On my hike to Crater Lakes a bit after that discussion had me thinking I knew where I should leave the trail. But it’s an inexact science. Satellite photos aren’t much help, as the area is fairly thick forest. But it does seem that this route avoids climbing straight up a steep slope. I was willing to give it a shot.

Ideally, I’d like to reach the two Iceberg Lakes as well, but I’m not confident I can do all three on a day hike. If I can’t collect the Icebergs in a day hike, I’ll need to backpack in and spend a night. I’m not confident that the “straight up the stream” route, including “steep scrambles” is something I want to try with a full pack. Perhaps the volunteer’s route is better suited. Well, there’s one way to find out.

Monday, July 10

I arrived at the trailhead parking lot at about 8 am. The road is in good shape right now and is set to improve as it is currently being graded. It’s about eleven miles of dirt road to reach the parking lot, but anything short of a low-slung sports car should have no trouble navigating it. I was a bit surprised to see only about a dozen cars in the lot, maybe half of which belong to backpackers not yet back from their destinations.

At the trailhead, there used to be a sign-in sheet where all hikers were expected to list the date, number in the group, their destination, and how long they’d be on the trail. This logbook is no longer there; at least it wasn’t there today.

It took me an hour and ten minutes to reach the trail to Crater Lakes. I hiked up this trail for about forty-five minutes, periodically checking the elevation with my phone. I was at more or less the correct elevation, I figured, so off the trail I went. Going was fairly easy at first, not too much deadfall and the terrain I was crossing was fairly level.

My plan was to avoid making any steep climbs, heading west or southwest and climbing as I went. Before long, I came across a small stream. I wasn’t expecting to reach water until I got to the stream that is the outlet from Clayton Lake, but it didn’t seem like this stream (actually three or four small streams braiding their way down the slope) carried enough water to be Clayton’s outlet. Nonetheless, I headed uphill following the stream.

The forest here was getting more difficult to traverse, getting steeper and having more fallen trees. I crossed the stream half a dozen times as I climbed, always searching for the easiest route. At one point, I climbed a bit where I knew I’d have difficulty going down. I try to avoid going up slopes I think will cause me difficulty when going down, but I figured (if I managed to retrace my steps) that I could make a small detour if need be.

After following the stream for a while, I found the source of my little stream. I was standing at the edge of a marshy meadow. Rather than slog my way across it, risking wet feet, I skirted the meadow. On the other side of the meadow, I found a grassy ramp, somewhat steep, that climbed alongside giant granite slabs. Above me looked to be the low spot of a saddle. Perhaps I was getting close to the lake.

Topping this slope I found myself back in the woods. With the ground much more level, the walking was easy again. I kept climbing, always looking to find the low spot on the saddle. Continuing west or southwest, I expected to come across the outlet stream eventually. Passing through a small band of trees, I found myself on another grassy slope, walking slightly downhill, and could now see the lake. I had arrived on the northern shore of Clayton Lake.

The lake is mostly surrounded by forest. I’m a big fan of finding a nice rock to sit on for my picnic. Ideally, said rock would be in the sun, out of the wind, and close to the water. In search of such a rock, I worked my way around to the outlet. There’s still quite a bit of snow here and I easily crossed a snowdrift that hid the outlet. I saw no sign of the old trail, but there was a social trail that edged the north shore. Finding mostly snow on the south shore, I abandoned my search in this direction and doubled back.

From the time I left the Crater Lakes trail until I returned to the trail about three hours later, the only sign I saw of any other person was a boot print in the mud on the little social trail that skirted the north shore.

I wandered the north shore for about fifteen minutes before I found my picnic rock, considerably farther from the water than I wanted to be, but so it goes. Just before I got off the Crater Lakes trail, I met a couple of backpackers on their way back to the trailhead. I asked if they’d seen any game. “Just mosquitoes!” Mosquitoes aren’t big game, but even on my picnic rock, out of the trees and in a light breeze, mosquitoes buzzed me constantly. I’d sprayed some mosquito repellent on me back at the car, so I was happy that it seemed to still be working. They buzzed, but they never landed.

After relaxing for a bit more than half an hour, I started to retrace my steps back down the mountain. I’ve found that route finding is easier on the way down than on the way up: the value of the high ground. I quickly found a game trail. A few yards down the trail, I felt that I should have been heading more to my left, but I stayed on this game trail for a bit longer. It seemed to be well-traveled, punctuated as it was with pellets. Before long, I decided to backtrack, forgoing the trail for the untracked ramp I climbed earlier.

Back at the marshy meadow that was the source of the small stream I followed uphill for a while this morning, I managed to find another game trail. At no time on my climb to Clayton Lake did I find a game trail, but from this trail I found just below my marshy meadow all the way back to the Crater Lakes trail, I managed to go from one game trail to another.

My experience with game trails is that they’re nice when they’re nice, but they often stop being nice in the most inconvenient places. Today, every time deadfall blocked the trail, I was able to find its continuance a few yards later. Game trails generally aren’t singular things: they’re all part of a network. From the marshy meadow back to the trail, whenever there was a choice of direction, I kept to the left and downhill. I figured I couldn’t go too far left – I’d eventually reach the Crater Lakes trail. My only concern was not finding myself at the top of some rock outcrop that I couldn’t get down.

These game trails kept me out of trouble: I’m pretty sure the deer and elk aren’t interested in getting stuck on some random outcrop and they don’t want to go up or down anything too steep. As I said, this game trail took me right to the Crater Lakes trail. I made a note of where it is. On the hike up the Crater Lakes trail, there’s a large coil of cable just off the trail. I have no idea why it’s there, but it’s been there for years. I figure my game trail is something like three hundred yards past the cable, very near a large sawn tree trunk.

Given that my route back from Clayton Lake was so easy, I think I’ll return on a backpacking trip. Even having found this easy route, I think Iceberg Lakes are too far for me to reach on a day hike. Hiking cross-country with no trail is a lot more time-consuming and more strenuous. But I’m confident I can backpack up this route and by spending one night at Clayton Lake, I should be able to collect both Iceberg Lakes.

When I’m hiking on a trail, my mind often goes into auto-pilot mode. I just keep putting one foot in front of the other until I get to some navigation point. My feet stay on the trail, but my mind wanders. Bushwacking, though, is another story. My mind is intensely focused on the task at hand. Bushwacking is a bit like solving a maze that has more than one solution. At any given point, I’m looking for where I should go next. How do I get around this jumble of deadfall? I want to go there, but what’s the best way? Once I get there, where do I go next? My mind does not wander. I’m not thinking about some TV show, I don’t have some song earworming into my brain, I’m not bothered by what some idiot said on the internet, and I’m not worrying about rent, or debt, or thinking about what I might do tomorrow. I’m in the here and now, completely focused on the moment. It is glorious.

LocationUpDown
Trailhead8:10 am2:30 pm
Forest Lake jct8:46 am1:57 pm
Crater Lake jct9:20 am1:27 pm
Left trail/returned to trail9:54 am12:43 pm
Clayton Lake11:00 am11:57 am

Diamond Lake

Mount Jasper rises to nearly thirteen thousand feet on the Continental Divide in the Indian Peaks Wilderness. One might think of it as being shaped somewhat like a starfish as it has five major ridges emanating from it. Two of these are situated on a nearly east-west axis. Between these two arms is a drainage that contains Diamond Lake, Upper Diamond Lake, and a couple of smaller unnamed ponds.

In addition to Mount Jasper, there is also Jasper Lake, an operating reservoir in the next drainage to the south of Diamond Lake.

There’s a well-traveled trail from the Fourth of July trailhead to Diamond Lake, a popular camping destination. There is no official trail from Diamond Lake to Upper Diamond Lake, but a little research yields at least two routes from Diamond Lake to Upper Diamond Lake. For maps, my go-to resource is Caltopo.com. They indicate a trail from the westernmost shore of Diamond Lake up an inlet, passing a pond before climbing to the north. ProTrails, on the other hand, suggests heading more or less due west from a meadow reached just prior to the trail actually reaching Diamond Lake.

Diamond Lake, like most of the other alpine lakes in Indian Peaks, sits fairly high up at a shade under 12,000′. Upper Diamond Lake is another 800′ or so higher. Because we have had such a wet spring, I expect the forest sections of trail below Diamond Lake might still be covered with snow. Certainly, no matter what route I might take to Upper Diamond Lake, I expect to find quite a bit of snow. At this time of year, even without higher-than-usual snowfall, microspikes would be required.

Monday, July 3

Both the Hessie trailhead and the Fourth of July trailhead are served by the same road, which becomes a dirt road just after passing through the town of Eldora. I’ve only been up this road a handful of times before today, and never on a weekend. Yes, today is a Monday, but with a holiday tomorrow, I expect it to be busier than a typical weekday. I was correct.

A sort of temporary entrance station was set up on the road at the entrance to Nederland High School. I arrived here at 7:45. They already had the shuttle bus for the Hessie trailhead operating. I was second in a line of four vehicles; we all were going to the Fourth of July trailhead at the end of the road. The fellow working the station got on the radio with a ranger at the trailhead to see how many of us could proceed. We were the last four cars allowed up the road. We had to wait a few minutes for the shuttle bus to return because the road is narrow.

It appears that sections of the road have been recently graded. Other sections are quite rough. Four-wheel drive isn’t required, but a fair amount of ground clearance is. Almost all the vehicles in the parking lot at the trailhead were SUVs and 4x4s, but there were a couple of compact cars.

When I arrived at the parking lot, I was afraid the ranger had miscounted. As I was approaching the lot, she was headed down the road in her truck. The spot I parked in was right up against a no-parking sign and I was concerned that overzealous enforcement might result in a ticket. One of the cars behind me took a similarly marginal spot across from me. I never did see where the fourth car parked.

The morning was beautiful, with clear deep blue skies, calm, with a temperature of just under 60 according to the car’s thermometer. Outstanding hiking weather.

The trail from the parking lot climbs about 600′ to the junction with the Diamond Lake trail. There is one pair of switchbacks in the middle of this climb, which traverses an increasingly steep slope. After the switchbacks, there are a few places where you get a nice view of the opposite side of the valley. Prominent in these views is the outlet stream from Diamond Lake, which cascades more than 400′. The sound of the falling water is constant accompaniment on this first mile or so of trail.

A bit more than a mile from the trailhead is a junction: to the left is Diamond Lake; to the right, the Fourth of July mine and trails to Arapaho Pass, Lake Dorothy, and South Arapaho Peak.

Heading left, the trail descends about three hundred feet before climbing the other side of the valley. There are a few stream crossings, with at least one of the bridges in need of some repair. As I expected, there is snow on the trail in places that don’t get much sunshine.

Just before reaching the lake, the trail levels off quite a bit and dumps the hiker on the east end of a large meadow. This early in the season, only the yellow flowers that flourish in marshy ground are in abundance. Perhaps as soon as a few days from now, flowers sporting all the colors in the rainbow will carpet the place.

Here, today, the trail is still covered in snow. A small rivulet is carving a little canyon through the snow. Snow melts from the bottom, and you can easily see that the trail crosses a snow bridge. It’s hard to judge just how thick the bridge is, but when I crossed it in the morning it was twelve or fifteen feet wide. Still, I was careful to not step where I thought it was thinnest. On the way back, a couple of hours later, the bridge was nearly gone, the snow is melting so quickly.

One possible route to Upper Diamond Lake heads across this meadow and up the slope that’s northwest of the lake. I didn’t see an obvious “easy” route – the meadow is more like a marsh right now, and the slope still held quite a bit of snow. It might be a good route in August or September, but I wasn’t going to head up that way.

When I got to the shore of Diamond Lake, I met a couple of hikers. I asked them if they had tried to get to the upper lake. I showed them my map while we discussed it. They weren’t familiar with the route suggested by ProTrails but did make an attempt to go the way that’s marked on the CalTopo map. They didn’t get too far: it was too snowy for them. Here, I decided to skip any attempt to reach the upper lake. The hike so far was a pleasant one, and there’s no reason not to come back when there’s less snow on the ground and the meadows aren’t marshes.

I walked along the northern shore of the lake. It’s grassy. Well, it’s grassy under the snow. I was a bit surprised at how much snow was still on the ground here, given that it’s in direct sunlight much of the day. It’s three, four, even five feet thick and stretches along the entire north shore of the lake. There are a few rocks along the shore that might make good picnic spots, but I preferred the somewhat larger rocks right along the trail.

The summit of Mount Jasper isn’t visible from here, just one of its eastern ridges. Here, much closer to the Divide than the parking lot, it was naturally a bit breezier. No mirror-like lake surface, but not so windy as to make whitecaps.

I didn’t count the number of campsites. Diamond Lake isn’t quite as busy as Lost Lake, but it’s still quite popular. On the hike and at the lake, I never went more than a few minutes without encountering other hikers. That said, my picnic spot had the illusion of solitude. Other than the few people who passed my picnic spot on the trail, I only noticed a couple of hikers who were circumnavigating the lake.

On the hike out, I stopped for a break where a stream crosses the trail. There’s no bridge here, hikers just step from rock to rock. With the water running high this time of year, it can be a bit fraught. While I was eating my grapes, I watched two couples make the crossing. The first couple had an infant strapped to mom. They made it easily. The second was a bit more tentative. She went first, he stood by getting her crossing on video. She nearly tripped. I told her that if she had tripped, he’d have gotten it on video. “Good thing I didn’t trip!”

A bit later, I came across a group of five or six backpackers. They were headed up to Lake Dorothy. They’d never been there before. I described the lake and its environs and jokingly said I hoped none of them intended on sleeping in hammocks as the lake is surrounded by tundra.

It was a gorgeous day for a hike. The weather was outstanding. I was never bothered by mosquitoes. Although I didn’t reach my ultimate destination, I’m not disappointed. All in all, it was another beautiful day in the neighborhood.

A final note: I overcame one of last week‘s disappointments. It seemed odd (but not out of the ordinary) for a new version of a product to remove a feature of an older version. In this case, though, it was simply a change in the defaults. I can still take individual photos for my time-lapse, and edit them to my heart’s content.

timetableUpDown
Trailhead8:37am2:19 pm
IPW Boundary8:48 am2:00 pm
Diamond Lake trail jct9:16 am1:14 pm
Diamond Lake10:14 am11:48 am

More photos can be found here.

Devils Thumb Lake

Today I return to the Hessie Trailhead in the Indian Peaks Wilderness for a walk up to Jasper Lake and its surroundings. There are three lakes here: Jasper Lake, Storm Lake, and Devils Thumb Lake. There are more than those, actually, as there are three unnamed ponds and a small lake called Upper Storm Lake in the cirque above Storm Lake. There is no official trail from Lake Jasper to Storm Lake and above.

Theoretically, it might be possible to visit these three lakes in one day hike. But because I haven’t been there before and I don’t know what the terrain looks like between Jasper and Storm, I decided to go to Devils Thumb Lake. On the return trip, I’d stop at Jasper and do a little recon of the route to Storm.

Wednesday, September 7

Arriving at the trailhead at about 7 am worked well for me on my first hike from Hessie, so I stuck to that plan. Today I had to gas up the car and the station doesn’t open until 6, so I arrived at the trailhead just a few minutes later than planned.

On my previous Hessie hike, I logged my time at each waypoint. I skipped a few this time, as there aren’t any navigational choices between the car and where I leave the jeep trail and take the Devils Thumb Bypass trail to reach Devils Thumb Lake. The Devils Thumb Bypass trail parallels the Woodland Lake trail, the trails being on opposite sides of Jasper Creek. Although the trails are only a few hundred feet apart, the forest is dense enough that I never saw the other trail. The first hundred yards or so of the bypass trail is the steepest section of trail on the entire hike.

On this trail, you reach the IPW boundary sign in a large meadow about a hundred yards wide and a third of a mile long. The meadow affords the hiker of the first views of Mount Jasper. This section of trail is the easiest: almost flat and almost entirely free of roots and rocks, allowing the hiker to maintain a uniform stride. Too quickly, perhaps, the trail returns to the forest.

It seems that for much of the route from the IPW boundary to Jasper Lake, the trail follows an old roadbed. Jasper Lake is a functioning reservoir. I was unable to find out anything about when it was built, but it’s an earthen berm dam much like several of the (now removed) dams in RMNP. I assume it is of about the same vintage, or just over a century old, and that this old road was used in the dam’s construction.

Anyway, the trail doesn’t always follow the old roadbed. Occasionally, there are small signs along the trail that say “Trail →”. I found these little signs a bit odd, as any other option than following the arrow on the sign would be silly. And yet, once I somehow managed to note the sign but still go off in the wrong direction.

I found myself still on the old roadbed, on a somewhat steep section of it bounded on both sides by willow. The road itself was now a corduroy road: made of logs the width of the road, placed side-by-side. I usually read of these corduroy roads being built in low, swampy areas. This section isn’t in a low area and is somewhat steep. Conversely, willow tends to grow in wetter areas, so the area may be quite wet earlier in the season. By the looks of it, there’s a fair amount of foot traffic through here, so I’m not the only one who has errantly gone this way.

A bit farther up the trail is the junction with a trail to Diamond Lake. Diamond Lake is a fairly short hike when starting on the Fourth of July trailhead. From there, it’s a bit more than two and a half miles. This way, it’s perhaps three times that, plus an extra six or seven hundred vertical feet. A good stretch of this route is above timberline, so the open views may make the extra effort worthwhile.

Slightly more than half a mile further on, the trail reaches the outlet of Jasper Lake. I didn’t pause here but trekked on toward Devils Thumb Lake. I would stop here on the way back.

From Jasper to Devils Thumb, the forest thins. Or, perhaps, it would be more accurate to say we’re hiking through grassy areas with clumps of trees rather than forest with clearings. In any event, Devils Thumb and Skyscraper Peak and parts of the Continental Divide are often in view.

The trail soon climbs to and crosses the outlet of Devils Thumb Lake. The lake is about ten acres in area, maybe 425 feet wide at its widest (north to south) and a quarter of a mile in length east to west. It is bounded on the east and west by large, thick stands of willow while the north shore is a tumble of talus. That leaves the south shore as the most easily explored. This shore is covered with forest, and the banks are more steep than flat. If you go down to the water, you can find a view of the entire lake, but the only places I found to sit in the sun and relax offered only partial views of the lake.

I spent about an hour here, between my search for a comfy spot to relax, consumption of a small snack, and application of sunscreen.

At this altitude (and for much of the hike, frankly), most of the wildflowers are gone, either eaten by squirrels or cached in burrows. The only flowers still with blooms were a few yellow species. All the blue, red, and purple were gone. I didn’t see a single columbine on the entire hike.

The relative lack of wildflowers wasn’t the only sign of the changing season. The grasses were beginning to turn yellow, and while the aspen leaves are still green, the ground cover beneath the aspen was already golden.

From the car to Devils Thumb Lake, I encountered only one other hiker. I started seeing more people once I started my return trip. Two sets of two hikers between Devils Thumb and Jasper told me to be on the lookout for a mother moose and her calf. I never spotted any moose, elk, or deer the whole day.

Back at Jasper, I turned off on a spur trail that leads to a few of the campsites. I went far enough along this trail to decide that this is the way to go if you want to head up to Storm Lake. This trail runs along the western shore of the lake, just high enough up the slope to avoid any marshy areas along the shore. I hopped off the trail here to explore a peninsula. I don’t think maps accurately depict the shape of the lake. This is probably because the shape of the lake changes drastically when it’s not full.

Much of the shoreline of the lake is forest, with steep banks. It’s a very scenic lake. At the farthest extent of my peninsula, I found a nice spot for a picnic and had my lunch. I had a nice open view of the corrugated ridge north of the lake. I also had a view of the terrain leading up to Storm Lake and could see a couple of falls made by its outlet stream.

Today’s beer was Hazy IPA by Great Divide Brewing Company. I’m not a huge IPA fan, but when you buy a variety pack you take the non-favorites with the favorites. I selected this particular beer today because I expected the skies to be a bit on the hazy side – an effect of wildfires in the Pacific Northwest. The IPA was a nice change of pace from my recent string of sour fruit ales, and the hazy skies were noticeable but not terribly bad.

Last week, I found myself directly underneath a flight path for eastbound jetliners. It turns out that Jasper Lake is directly beneath a westbound flight path. Like last time, atmospheric conditions were such that these planes weren’t leaving any contrails so I had a little trouble initially spotting them. As they all use the same routes, when you spot one, you can spot them all. Being a city dweller near a regional airport, I’m accustomed to hearing aircraft all the time. But they don’t fly right over my house. If these jets didn’t fly right overhead, I don’t know that I’d be complaining about them.

Here in the first week of September, Jasper Lake is at its fullest. What looks today like the outlet of the lake is actually the dam’s spillway. Some care was taken to make it look natural. The same is true, to an extent, of the dam itself. From below the dam, on the trail, it’s not obvious that it’s a dam. The slope is gentle and is covered with grass (and flowers, perhaps, in July and August).

The water that goes over the spillway makes a 90-degree turn then drops fifteen feet or so to where I’m guessing the original outlet of the lake was. The outlet pipe is here. Once the valve is opened, the lake’s level will drop such that water no longer goes over the spillway; the lake is drained through this pipe. There’s a building of some sort (I didn’t explore it) where I assume the valve is operated.

I’m guessing this dam was built much the same way as the (no longer standing) dams for Sandbeach, Lawn, and Pear Lakes (and others) in RMNP. I can only hope that its construction is more robust than those dams (which, by 1982, all suffered serious structural issues). I understand that dams in Colorado are rated as to their riskiness. This rating is based on the danger to people and structures below the dam should it fail and not just on the soundness (or lack thereof) of the dam itself. If this dam were to fail, it would flood Middle Boulder Creek through the town of Eldora, then Nederland, and ultimately flow into Barker Reservoir.

I ran into a lot more trail traffic on the way out than on the way in. More than half the folks I encountered had dogs with them. There are plenty of signs that tell us dogs must be on leashes. Of all the dogs I saw, only one group kept theirs leashed. All the rest allowed their dogs to run free. One group at least made the attempt to seem like they kept their dogs leashed: they managed to get one of their two on a leash by the time they passed me. But a hundred feet past me, they let that one off to run free. (There was a fair amount of dog poo right on the trail, too.)

I’m sure every dog owner feels that their Fido is a kind, gentle dog not very interested in biting people. But on my daily walks in my neighborhood, I’ve been bitten multiple times by dogs. Back in my misspent youth, when I delivered Avon to the Avon ladies, I encountered hundreds of vicious dogs. So perhaps I’m oversensitive to the issue. But I really wish people would follow the rules on this one and keep Rover on a leash.

I will definitely be back in this area. I’d like to visit Storm Lake (and perhaps Upper Storm Lake and the unnamed ponds, too). In the valley between Jasper and Betty and Bob Lakes, there are two more lakes, one of which is also a reservoir. Skyscraper Reservoir looks to be a concrete dam rather than an earthen berm. I probably won’t get to Skyscraper this season, but it’s definitely on the to-do list. I’ll admit that I’m curious about these alpine lakes that were dammed in service of irrigating farms on the eastern plains.

Hike Segment Data

StartEndDistance (Miles)Slope (Ft/Mile)Elapsed TimeMiles per Hour
CarDevils Thumb Bypass jct1.5297:362.5
Devils Thumb Bypass jctIPW Boundary0.5380:152.0
IPW BoundaryWoodland Lake trail jct0.8201:202.4
Woodland Lake trail jctDiamond Lake trail jct1.5593:491.8
Diamond Lake trail jctJasper Lake0.6223:201.8
Jasper LakeDevils Thumb Lake1.0325:361.7
CarDevils Thumb Lake5.93642:562.0
Distance and Slope are approximate

Dutch Town 1

Foster tells us that Lake of the Clouds is the “most highly visited destination in the Never Summer Mountains”. I don’t doubt her, but if it’s true it tells me just how few people visit any destination in the Never Summer Mountains. (She certainly includes only the mountain destinations and not those in the valley, like Lulu City.)

I tried to reach Lake of the Clouds quite a while ago as a day hike. I wasted some time with a navigation error and made it only to where the trail ends on the map. Since then, I’ve suspected it was out of my day hike range, and decided to give it the two-night treatment: hike to the campsite on day one, hit the lake (or lakes) on day two, and hike out on day three.

The trail is accessed from the Colorado River trailhead. I’ve never seen that lot full, so we could pick our own departure time without worrying about getting a place to park.

Monday, August 29

We had a leisurely 7 am departure from my house, traffic wasn’t horrible, and we put boots on the trail at 9:20.

The first section of trail goes due north from the parking lot for half a mile to a trail junction. Many hikers won’t go any farther than here, or hereabouts. There’s a bridge over the Colorado river a few yards from the junction. Most of those who don’t stop here will continue on toward Lulu City. To reach Lake of the Clouds (or our campsite, Dutch Town), you make the left turn and take the route less traveled.

After crossing the valley, the trail turns south to climb the lower flank of Red Mountain. The trail traverses a fairly steep slope and by the time it has gained about four hundred feet, the hiker is presented with a view of the trailhead parking lot. It surprises me how often a trail gains four hundred feet from a valley floor up to a bench. That happens here, and although there are no lakes on this bench, there are some wetlands.

Having gone a very short distance south of our starting point, the trail turns around and heads generally north until it comes out on the service road for the Grand Ditch. The Grand Ditch is a water diversion project that is capable of taking all the water on the east side of the Never Summer Range and putting it into Long Draw Reservoir, which feeds the Cache la Poudre River.

The trail continues along the ditch for nearly two miles. I’d say that there’s more water flowing in it than in the Colorado River just below us. The ditch is flowing opposite to the river, but we’re at about the midpoint of the ditch, so it’s not a bad approximation that where we crossed the river, there should be more than twice as much water in it. It’s indicative of the abuse the Colorado River gets that, in its first 15 or 20 miles, more than half its water has been rerouted.

From the start of the hike to a fair piece northward along the Ditch, traffic noise from Trail Ridge Road has been a constant companion. As we approach the end of our flat and level stroll on the service road, we’re about a mile north of the highway and turning west. The road noise fades away. Now we can easily hear the jet airliners passing overhead. The westbound ones are a bit north of us, but the eastbound fly directly overhead.

At the Lake of the Clouds trail junction with the Grand Ditch, there’s a sign that indicates Dutch Town is 1.3 miles distant, and Hitchens Gulch is .8 miles. I never did see any sign for the Hitchens Gulch campsite, going or coming, so I suspect it’s no longer in use. I also suspect the miles are inflated a bit. I reckon it’s more like .7 to Dutch Town. It took us thirty minutes to get from the Ditch to the campsite. That’s a five-hundred-foot gain, so I think 1.4 miles per hour is much more reasonable than the 2.6 miles per hour required by the sign.

It took us three hours of hiking to make the trip. Add some time for our break at the base of the Lake of the Clouds trail. Since we crossed the Colorado River, we had encountered only three other people. They had camped at Valley View, very close to where the trail first reached the Ditch. There was nobody at our site, which surprised me. If I could have gotten a Sunday/Monday instead of our Monday/Tuesday, I would have. Either the previous occupants of Dutch Town made it to the trailhead before we left, or they hiked to another campsite. Or, possibly, they canceled. No matter.

Some previous occupant of the campsite left us a present: a somewhat chewed-up skull. I have no idea what sort of creature it belonged to. It’s just the skull; no mandible, and it’s not obvious where the mandible would attach. The brain would be a bit smaller than my fist.

I’ll admit that I’m a bit spoiled backpacking in the Park, given the generally outstanding trails and campsites. That said, I’ve only camped in about half a dozen established campsites in the Park. This one is a bit different than the others I’ve been to. First, it’s very close to the trail and my tent is clearly visible from the trail even before reaching the sign and spur trail. Second, it’s not ideal for water. Sitting at the campsite, the stream is audible. But what can be heard is water flowing under some talus. Just upstream, the stream is very wide, very shallow, and flows slowly. Here, the streambed is a soft mud that is easily disturbed. I use a SteriPen rather than a filter and it was impossible to get any water without a bit of sediment. It is necessary to go quite a way upstream to avoid the sediment.

A few yards from the level spots at the site, there’s a sign saying “Restoration Area: Stay Off”. I believe the site was located by this sign in years past. Here, tents wouldn’t be visible from the trail. The difference in location wouldn’t have made much difference as to water, though.

On my last backpacking trip, I brought the critter cam. The only critter it spotted was me. I probably should bring it every trip, but I figured I didn’t want to carry the extra weight. I should have brought it.

At about 10:30 I was awakened by something moving through the campsite. It sounded like a large quadruped. I’ve had moose go past my tent. It wasn’t exactly a quiet animal. This one was quiet, so I guessed it was either an elk or a deer. It didn’t linger and was quickly out of earshot.

Later, I heard my tent rustling. It sounded like the rain cover was being disturbed by a slight breeze. I didn’t give it much thought at the time. But things are not always what they seem.

Hike Segment Data

StartEndDistance (Miles)Slope (Ft/Mile)Elapsed TimeMiles per Hour
TrailheadRed Mtn trail jct0.512:122.5
Red Mtn trail jctGrand Ditch2.84251:331.8
Grand DitchLake of the Clouds trail jct1.9-8:402.9
Lake of the Clouds trail jctCampsite0.7714:301.4
TrailheadCampsite5.92862:552.0
Distance and Slope are approximate

Upper Ouzel Creek 1

I’ve been planning this backpacking trip for several years now. The idea is to reach both Isolation Lake and Frigid Lake. It may be possible that I could reach Isolation Lake on a day hike, but after my visit to Eagle and Box Lakes (reached from Thunder Lake), I decided that Foster’s route to Frigid Lake would not work for me. The answer, I decided, was to camp at Upper Ouzel Creek and try to reach both lakes from there.

In fact, I made the attempt a few years ago. It was not well thought out. I somehow decided that a trip in the first week of July would work just fine. There was so much snow. I was able to pitch my tent on dry ground, but the campsite featured several snowdrifts. I didn’t even make it to Bluebird Lake that time, let alone another thousand feet of elevation to Isolation. Needless to say, I took a bit more care in choosing when to make another attempt.

I keep telling myself that, on one of these trips, I’ll try to get a photo of the night sky: the Milky Way. When selecting my dates, though, I don’t give any consideration to the lunar calendar. This time I got a bit lucky. The moon would be in the first quarter and would set not long after the sun. So for this trip, I’ll bring the tripod. It’s an extra four pounds. And, while I’m adding extra weight, why not bring the critter cam? What’s one more pound?

Wednesday, August 3

Gordon decided to join me on this trip and I managed to talk him into driving. I told him that our first day’s hike wasn’t long so we didn’t need to get an early start, but I was concerned about getting a parking spot at the trailhead. The timed-entry passes are in effect for Wild Basin, but only after 9 am. However, I’m sure the parking lot fills up well before then. So it was an early start nonetheless. We arrived a bit before 7:30 to find plenty of available parking.

I’ve described the route to Bluebird Lake in earlier posts, so I won’t repeat myself.

I think I first hiked this trail back in 2008 or so. That would have been thirty years after the Ouzel fire. There’s a section of trail that runs along the top of a ridge above Ouzel Falls to the junction with the spur trail to Ouzel Lake. This section of trail was a bit of a two-edged sword: with no trees, the open views of all the surrounding mountains are impressive, but with no shade, the hiker is subject to the merciless sun.

Today, though, I was struck by how much the trees have grown in the last few years. The once open view is getting closed in. The vast majority of young pine trees are more than six feet tall now. Our two-edged sword is no more: the trees block the views but don’t provide any shade. So it goes.

The Upper Ouzel Creek campsite, by my reckoning, is about a third of a mile below Bluebird Lake. The trail signs indicate it’s farther. It’s a steep third of a mile, though, gaining nearly four hundred feet. I think my favorite part of the trail to Bluebird is a steep section just above the campsite. Maps of the area don’t indicate any switchbacks, probably because they’re too close together to show. Those switchbacks carry the hiker up a slope carpeted with wildflowers. The whole rainbow is represented: yellow flowers make up the majority, but there are red, orange, blue, indigo, and violet flowers, too.

We arrived at our campsite just as the prior occupants were packing up. They were there to fish; they stayed two nights and dipped their lines in both Bluebird and Ouzel, but no luck at Bluebird.

Having arrived at our destination before noon, we had plenty of time to kill. We were done setting up camp and eating lunch by 1 pm and so headed up to Bluebird to sit and relax and watch the world go by.

I was a bit surprised to see several hikers reach the lake after we did. One group, a family of four, stayed at Bluebird until about 4 pm. I guess because I have an hour-and-a-half drive home after my hikes, I want to be back to the car no later than 5 or 5:30. Those folks, if they kept up a good hiking pace, wouldn’t be back to the trailhead until 8 pm.

We hung out at the lake for nearly four hours. The weather seemed to be threatening: the white, puffy clouds grew bigger and darker but we never got more than a few sprinkles. Down the valley, though, it looked at times to be raining heavily. Without wind, it would have been comfortable in shirtsleeves, but it was breezy enough to warrant putting on a jacket.

I’m generally at these alpine lakes for no more than an hour, generally around noon. Being there a bit later and for an extended time I enjoyed watching the shadows change on the surrounding mountains. I ran the GoPro from two different positions, watched a little pika navigate through and around the rocks trying to avoid us humans, and investigated the nearby flora.

Gordon found some remnants of the dam that used to be here. I told him that I’d read about the removal of concrete. I was thinking I’d heard that 1,100 tons of concrete had been removed but was unsure of the number. It’s actually five million pounds of concrete and rebar. That’s 2,500 tons. They airlifted it out in 1989 and 1990 (well before my first visit here). I can’t help but wonder how they got that much material up here. There’s nothing like a road, or the remains of a road, and the dams in the area were all built around the turn of the twentieth century. The material sure wasn’t airlifted in. More on this topic later in another post.

Had I given it any thought, I might have taken my dinner with me to the lake. As no forethought was involved, we had to return to camp for dinner. The breeze we had at the lake was absent at camp. Normally, this is a good thing. But not tonight. We were besieged by mosquitoes.

I sprayed a liberal dose of repellent on all my exposed skin. This was only a partial solution. Before long, I applied a second coat and sprayed my clothes as well. These measures made it so the little buggers didn’t land on me, but it didn’t keep them away from me. From our arrival back at camp until dark, when I retreated to the tent, there were never less than a couple of dozen mosquitoes buzzing within twelve or fifteen inches of my head. While eating, I had to be careful not to ingest one accidentally. These mosquitoes were relentless.

Today’s beer was a Colorado Native Palisade Peach tart ale. Delicious.

Until dark, I kept a close monitor on the cloud situation. Several times it seemed like the clouds were finally breaking up, only to have another batch of them appear over the divide. By dark, I decided that the sky would soon enough be cloud-free, so I set an alarm for 11:30. I figured the quarter moon would be down by then, the skies would be clear, and I’d be able to try my hand at astrophotography.

I was in luck: the skies had cleared. At least, I think they did. There may have been some high, thin clouds in the east. I had a couple of suggestions for exposure settings. I tried them, and a few others. It took only a few minutes, and I was back in the sack before midnight.

But I never really got back to sleep.

Finally, here’s the first timelapse of the trip:

The Data

I’ve been recording how long it takes me to hike from point A to point B for quite a while. I share the timetables so somebody else might be able to get a clue how long it might take them. In the table below, for example, someone who has gone to Ouzel Falls but not to Ouzel Lake can compare how long it took them to reach the falls to my time. Whether they were faster or slower to the Falls, they can extrapolate a time for the hike to the lake. Also, next time I hike any of these sections of trail, I’ll have a good idea of how long it’ll take.

LocationArriveDepart
Trailhead7:25 am
Campsite shortcut8:00 am
Calypso Cascade8:14 am
Ouzel Falls8:45 am9:09 am
Bluebird/Ouzel trail jct9:21 am
Ouzel trail jct10:12 am
Campsite11:40 am
Arrival time and departure time are the same where no departure time is given

It didn’t really occur to me that I could use times from one hike and forecast how long it might take me to do another hike. Certainly, there are many factors. How steep is the trail? Am I carrying a backpack or a day pack? What’s the elevation? Am I on a trail or bushwhacking? How long was I hiking prior to a specific section – how fatigued am I?

StartEndDistance (Miles)Slope (Ft/Mile)Elapsed TimeMiles per Hour
TrailheadCampsite shortcut1.4250:352.4
Campsite shortcutCalypso Cascade0.4625:141.3
Calypso CascadeOuzel Falls0.8350:311.5
Ouzel FallsBluebird/Ouzel trail jct0.40:122.0
Bluebird/Ouzel trail jctOuzel trail jct1.4425:511.6
Ouzel trail jctCampsite1.54601:281.0
TrailheadCampsite5.93753:511.5
Distance and Slope are approximate

Frozen Lake

There is no shortage of stunning scenery in Rocky Mountain National Park. I’d even say that that sentence is a bit of an understatement.

My loquacious nature shows up regularly on the trail when I have brief encounters with other hikers. In the back-and-forth of “where are you headed”, “where are you from”, and so on, it often comes up that I’ve traveled extensively through the Park. And, so, it’s only natural that I often get asked what’s my favorite place to visit.

It’s a surprisingly easy question to answer: Black Lake. Specifically, climb up the inlet stream two or three hundred feet of elevation. The views there are tough to beat.

There are eight named lakes in Glacier Gorge. In my misspent youth, when I thought you could only visit places that had official trails, I repeatedly visited Mills Lake, Jewell Lake, and Black Lake. On one visit to Black Lake, we saw the trail that climbs alongside the inlet stream. We explored a bit, with the payoff being the fabulous views of Black Lake, McHenry’s Peak, and all the rest.

I’ve now visited all eight of the named lakes, plus the unnamed lake commonly called ‘Italy Lake’. Actually, I’ve been to all of them at least twice. Except for Frozen Lake, which I’ve only been to once before.

My first visit to Frozen Lake was back in July 2012, with Ed. This was just a few months after a microburst devastated a section of Glacier Gorge, knocking down thousands of trees. We had to crawl over, under, and around downed trees. I’m pretty sure they had the trail back in shape by the end of that summer. It was a very interesting hike at the time. Tree roots tend not to go very deep in these parts, and when a tree is knocked down like they were, the trunks don’t break at ground level: instead, the tree is knocked over with a large disk of roots, rocks, and soil still attached to the base. I think some of those knocked-down trees are still alive, living off their root disk.

Anywho, it’s time to make another trip to Frozen Lake.

Thursday, July 21

For this visit, I obtained a timed-entry pass good between 5 am and 7 am. Gordon joined me, saying that he wanted to be back by 6 pm. I told him that was doable, but might be tight. I said that if we left my place by 5:30 we’d enter before 7 and, parking at the park-and-ride, we’d put boots on the trail by 7:30. I reckoned that if we stayed at the lake for only half an hour, we could make it back to my house by 6 pm. So that was the plan.

We were off to a rocky start when Gordon showed up at my place with a flat tire. We might make it back here by 6, but it’d probably take him a while to get going. Oh well.

Arriving at the Park, we queued up in the line of cars headed up the Bear Lake corridor. The line this week was longer than last time I was here, a couple of weeks ago, for my Sky Pond hike. That time, there were two rangers checking passes. This time there was only one, and the line we found ourselves in was roughly twice as long as last time. Also, last time I wasn’t asked if I had a day pass. I didn’t, and my annual pass had expired. This time I did get asked. I said I have a Senior Pass, but she didn’t demand I produce it.

I know it takes me almost exactly an hour to get to Mills Lake from the Glacier Gorge parking lot/trailhead. I’m not as sure how long it takes to get to Black Lake from there, or how long it may have taken me to get to any of the lakes above Black Lake. I estimated that it would take an hour and a half to get from Mills to Black and another hour and a half to get to Frozen. So I was quite pleased to see that we reached Mills in a few minutes less than an hour, and Black in about an hour and a quarter. So we were already a bit ahead of schedule.

This summer, I’ve taken to using my trek poles. I bought them when I bought my snowshoes. I used them once or twice but wasn’t very happy with them. I’m not sure why I decided to give them another try, but here we are. My thinking is, I’d find them useful when I’m off trail, or for crossing streams or navigating talus fields. But I don’t want to use them all the time. I figured out how to carry them on my lumbar pack. Reduced to their minimum length they’re still a bit long: with them on my pack, I’m now as wide as if I were standing with hands on hips, elbows out. I have to be careful passing other hikers on the trail, and if I get into a willow patch I have to take them off the pack.

So, at the base of the climb above Black Lake, I started using the poles. I didn’t really need them until we reached a place where the stream goes alongside a tilted granite slab. These ten feet or so always give me a little heartburn. Not so with the poles.

The trail above Black Lake is pretty easy to follow until you gain the large bench that holds Frozen, Green, and Blue Lakes. At some point, however, you find yourself in a place where you can more or less go whichever way you want, subject to stream crossings and fields of willow. On our way down, we spent more time on what passes for the trail in this area than we did on the way up. I think our route up was a bit easier than the well-traveled trail.

The gist of the hike from the top of the climb from Black up and over to Frozen is a series of large inclined slabs separated by grass or willow. There are cairns throughout the area, generally indicating paths through the willow or leading to the stream crossings. So navigation is pretty simple: just bear to the west of the Spearhead.

The weather was beautiful if perhaps a bit warm at lower elevations. At 11,600′ above sea level, it was about as pleasant as it gets: sunny, warm, not terribly breezy, with mostly clear skies. I was thinking we’d only sit at the lake for half an hour, but before I knew it an hour had passed. (Today’s beer: Avery Brewing’s Electric Sunshine, a tart ale brewed with papaya, pineapple, kiwi, and huckleberry.)

Again, I usually had a fair amount of heartburn descending the steeper bits of the inclined slabs. What can I say? I’m a bit of a weenie. I was much happier having poles, but I was still a bit slow in places. But they did wonders for my confidence.

We could hear voices but didn’t see where they were coming from. I figured they were climbers working up the Spearhead. I stopped a few times trying to spot them but never did see anybody. I also tried inspecting the area around the Keyhole on Longs. The lens I normally use isn’t much of a telephoto, and I didn’t bring a longer lens. I thought I saw some people up there but couldn’t be sure.

One thing I will say: If I had seen this view before climbing Longs Peak, I never would have climbed Longs Peak. From here, it looks to me like one would have to be insane to climb it. It’s not straight up-and-down, but it’s pretty dang steep. And large sections are giant slabs that look to have no footholds or handholds. I have climbed it, though. Let’s just say I was highly adrenalized by the time I got back to the Keyhole. Let’s also say I see no reason to do it again.

The hike back to the trailhead was uneventful. We got sprinkled on twice, very briefly, not enough to even wet the rocks. I was quite surprised at how few other hikers we ran into. Part of that, no doubt, is because we used the Fire Trail. But I expected quite a few people at both Mills and Black. I don’t think we came across more than two dozen people all day.

We did enjoy a close encounter with a cow elk. She was crossing the trail just a few feet in front of me. She was quite habituated to people and didn’t really give us a second thought. She worked across the trail munching on grass and flowers and came within twelve or fifteen feet of us. After we passed, we could hear her whistle. That was Gordon’s description of the noise. It’s not a bugle or trumpet. More like a … bass flute? She was whistling up a storm; we could hear her for quite a distance down the trail.

Even with our extended stay at Frozen Lake, we were back to the car ahead of my original schedule. Traffic wasn’t as bad as I expected and we were back to my place by 5:30. Gordon still had to deal with his flat tire. This was a bit more difficult than we anticipated. His tire iron wasn’t the correct size for his lug nuts, and his jack didn’t lift his truck high enough to get the flat tire off, let alone to get a fully inflated tire back on. Luckily for Gordon, his nephew wasn’t too far away and had a jack he used to lift his lifted Jeep. We got him back on the road not much after 6:30. Typing this, I haven’t heard from him. So I’m hoping he actually made it home without any additional drama.

Except for Gordon’s flat tire, I’d say the day was a success!

Timetable

UpDown
Trailhead7:24 am3:33 pm
Mills Lake8:18 am2:38 pm
Black Lake9:32 am1:15 pm
Frozen Lake11:11 am12:07 pm

And, finally, the time-lapse:

Crystal Lake

Up to now, I’ve been buying my timed entry passes well in advance. They released the vast majority of passes back in June for June and July. They also release a tranche of passes two days in advance. That is if you didn’t buy a pass in advance for, say, July 1, and you decide you want to go, they make an additional number available on 6/29 at 8 am MT. If you look at a date that has sold out, it’ll show how many they’ll release 2 days in advance. For the 6-8 am slot, it looks like 65 passes each day.

Wanting to hike on Wednesday, I signed on Monday morning to get a pass. I refreshed my page promptly at 8 and made my purchase. By the time I selected the date, time, and type of pass, it said only 40 of the 65 were still available. After completing the process, I went back to see how many were left. At 8:03, it was down to 7.

Clearly, the best way to get a pass is to buy one when the bulk of them are released. And, as it turns out, passes for August become available on July 1. Of course, I’ll be on the trail when August passes become available but I’m thinking that they won’t get snapped up much faster than they were in June. When I made my first reservations, there were hundreds available for each day/time I wanted.

Having obtained my pass, the next issue was where to hike. I’ve done a pretty thorough job of visiting lakes that are readily accessible. What’s left will either require camping or are at elevations or in locations where there’s likely still too much snow on the ground. And I’d like to avoid the crowded trails in the Bear Lake area. With this in mind, I decided on Crystal Lake, which I last visited back in 2011. It’s high enough that snow might be a problem, but the higher sections of trail are on south facing slopes.

Wednesday, July 1

I was thinking I wanted to be on the trail at about 7:30. I thought the lake is seven and a half miles up the trail, but I see that the Foster guide says it’s 7.9, with 2,960′ of elevation gain. I figured I could maintain a two mile per hour pace up to Lawn Lake, then somewhat slower for the bit above eleven thousand feet.

I left the house at 5:30 and, encountering little traffic, I was at the trailhead a few minutes before seven. There were plenty of empty parking spaces, and a couple of hikers started on their way while I was getting ready. I hit the trail spot on 7:00. Before leaving the car, I sprayed on some mosquito repellent. I don’t normally carry it with me for a day hike and hoped that a single application would do the trick.

The first section of trail gets your heart going right away, climbing about 700′ in a little over a mile. That’s about double the average rate of climb for the entire hike. The trail to Lawn Lake is a pack trail, so it’s mostly free of roots and rocks and never gets too steep.

The first navigation point is the junction with the Ypsilon Lake trail. I didn’t catch up to the hikers who left the parking lot before me, but I did encounter a group of four hiking back to the trailhead. If they were camping, they left their campsite quite early, and I can’t imagine how any day trippers were already on their way out.

The next section of trail, a bit over four miles, more or less follows Roaring River. When the river is in view, it’s quite dramatic. The Lawn Lake dam failed back in 1982, releasing something like 30 million cubic feet of water at a peak rate of 18,000 cubic feet per second. The effects are almost as visible today as they were nearly 40 years ago. The careful observer will note places where the trail was washed away. That really doesn’t explain it properly: it wasn’t so much that the trail was washed away, but that the hillside the trail passed over was washed away.

There are places where a hundred feet of hillside looks to have been scoured away. Trees on the edge of these cliffs are dead but still standing, half their roots supported only by air. Continuing erosion is obvious. Not just earth being washed away from above by rain and snow, but the stream still undercutting the banks. In wider spots, the deluge deposited large piles of tree trunks. In narrower places, everything was washed away, leaving bare bedrock. In some places, the flood scar is visible from miles away. The pace of life is slower at altitude; even in forty years, new trees and shrubs have barely started growing back.

Mummy Mountain and flood-scarred Roaring River

For the most part, this section of trail is easy walking. Fairly long stretches of nearly level trail are broken by short, steeper climbs that feature a few switchbacks. As the trail more or less follows the stream, it’s at the bottom of the forest valley, so there are no views to speak of. I also will note that my mosquito preparation was (today, anyway) unnecessary: I neither heard nor saw a single mosquito.

Not long before reaching Lawn Lake, there’s a junction with the Black Canyon Trail. You could theoretically get to the Cow Creek trailhead or Gem Lake or Twin Owls from here, but I’m not sure why anybody would want to. I haven’t hiked it, but I imagine it’s mile after mile of vista-free walking. But it exists, and appears to be both well-maintained and well-traveled. So somebody must find it useful.

Lawn Lake is the end of the pack trail. There are two hitching posts here, one for llamas, one for horses. From here to Crystal Lake, the trail is narrower and steeper. At times it goes right through small patches of willow where it resembles a game trail and will get you a wet boot if you’re not watching your step.

Just above Lawn Lake the trail rises above treeline and leaves the forest behind. I stopped here with the idea that I’d slather on some SPF. But the sun’s warmth was a bit feeble and the breeze was definitely not feeble so instead of sunscreen, I put on my jacket. Much of my hike so far had been in shade. It was well after nine before a single ray of sunlight hit my body. I was expecting things to warm up as the day progressed, but clearly that wasn’t in the cards this morning. I did put sunscreen on my face and hands, though, as the sun above 11,000′, while pleasant, is harsh.

To this point, I hadn’t seen any hikers (other than the group of four right at the start). There was a guy fishing at Lawn Lake and a hiker there sitting on a rock. While I was getting my jacket on, she passed me on her way to Crystal Lake.

Lawn Lake, with Longs Peak in the distance

There really wasn’t much snow along the way. In some shady spots around Lawn Lake there were a few drifts not much bigger than a few paces across. A bit more than half way up the slope there’s another trail junction, with a spur trail that takes you to The Saddle. I considered heading up this way, not to the top of the saddle, but far enough up to get a view of Crystal Lake from above. It was still fairly early, so I had plenty of time, but my pace had slowed considerably and the cool, stiff breeze was a deterrent. I continued to the lake.

Mummy Mountain towers over Lawn Lake

Not far after the junction I came to the only stretch of snow worth mentioning. Standing on the eastern edge and looking west, I couldn’t see the trail. Lucky for me, the gal who passed me had already crossed the snow and was working her way along the far edge. Scanning the terrain above her, I finally spotted the trail and so I made a direct line for it. I didn’t quite catch up to her, but I essentially wiped out the lead she had on me.

There are two lakes here, nearly side-by-side and differing by only three feet of elevation. The first one is Little Crystal Lake. It’s very scenic. Almost exactly as scenic, in fact, as its larger neighbor. But it is very much the “red-headed stepchild”; nobody seems to stop here to take in the view.

Little Crystal Lake and Fairchild Mountain

I caught up to the other hiker as we climbed onto the boulders that make up the shore of the lake. There we found a guy who was making an attempt at fishing. We sat on a rock about ten feet apart and chatted while we ate our lunches.

When I was last here, I had the place to myself. Today, at first it was three of us. I stayed about an hour and a half. While there, a group of four hikers arrived, then a solo hiker, then two more. On my way past Little Crystal Lake, another solo hiker arrived. Clearly, this place is more popular than I thought. Usually, if I’m going to a lake more than seven miles away there aren’t many (or any) other visitors.

Crystal Lake

Ironically, on the way up, from the Ypsilon trail junction to Lawn Lake I didn’t see anyone on the trails. And, likewise, on the way out it was the same thing. Usually, at any lake I visit where there are a dozen or so people, I’ll meet people on the trail who are headed to the same place, or have been there and are on their way back.

I didn’t see any big game, but the marmot population at Lawn Lake, Crystal Lake, and in between was impressive. They weren’t too shy, either. One perched himself on a pedestal-like rock and looked at me as if to say, “I’m ready for my portrait now!” Another made it’s home in a hole right next to the trail, only backing down out of sight when I got within a few feet.

Timetable

UpDown
Trailhead7:00 am4:08 pm
Ypsilon jct7:35 am3:33 pm
Black Canyon jct9:27 am1:50 pm
Lawn Lake9:45 am1:35 pm
Crystal Lake11:00 am12:30 pm

Green Lake

The upper end of Glacier Gorge is arguably the most scenic terrain in Rocky Mountain National Park. Mills Lake and its little sister, Jewel Lake, are fed by Glacier Creek. This creek is fed by half a dozen named lakes and a multitude of ponds and rivulets cascading down the slopes of some of the highest and steepest mountainsides in the area. The eastern side of the gorge is formed by a monolithic wall that is comprised of Half Mountain, Storm Peak, Longs Peak, and the Keyboard of the Winds. The western side is Thatchtop, Powell Peak, Arrowhead, and McHenrys Peak. Forming the southern end are Chiefs Head Peak, Spearhead, and Pagoda Mountain.

When you arrive at Mills Lake, the peaks to the east and west rise fifteen hundred feet above you. From Mills to Black Lake is about 2.8 miles and a climb of 700 feet or so. At Black Lake, you are surrounded by granite cliffs towering twenty-five hundred feet. It seems that no matter how high you follow these streams, the summits you pass beneath climb even higher.

This is my second trip to Green Lake, my first being back in 2011. That was before I began this blog, so the hike deserves the full treatment here rather than the abbreviated version that other repeat visits generally get.

Saturday, July 27

The weather report warned me that I could be dealing with storms as early as 10am but that didn’t deter me. I had wanted to get out of the house by six but I, as usual, ran a few minutes late. Traffic wasn’t too bad and I was at the Park & Ride by a quarter to eight. My plan was to put boots on the trail at eight o’clock, and I missed this by only ten minutes.

I generally take the Fire Trail, skipping Alberta Falls and the heavy trail traffic that goes along with it, but I got to chatting with a couple from upstate New York and missed the turnoff. Still, I arrived at Mills Lake in less than an hour. It is here, for me, that the hike really begins.

One of the interesting aspects of the trail between Mills Lake and Black Lake is the rather large debris field that was the result of a micro-burst that hit, I believe, in the autumn of 2011. I don’t know exactly when it happened, but the thousands of trees were knocked down by the time I hiked to Black Lake in March of 2012. That first summer it took the Park Service quite some time and a lot of effort to cut through all the tree trunks that blocked the trail for more than half a mile.

A fair section of trail just above Mills Lake passes through some fairly marshy stretches. These sections are made passable by a series of crude bridges each a hundred or two hundred feet long. I’ve crossed these bridges for nearly forty years and now they’re mostly rotten and decaying. This year the Park Service is rebuilding them in an effort that may match that of clearing the path of the downed trees from that micro-burst.

Bridge Reconstruction

It had started sprinkling at about ten and before long the sprinkles turned to rain, so I donned my rain coat. It wasn’t raining heavily, but the cool of the morning was still lingering, and between the light rain and light breeze, it wasn’t uncomfortable in the rain gear. I ran into a hiker here who had been to Green Lake on another occasion; he said he’d prefer it in the sunshine over this morning’s grey skies and light rain. Perhaps the weather will remain dull and damp, but perhaps it will improve. Besides, even a dull day in the park is a good day.

The last few hundred feet of trail below Black Lake rises beside Ribbon Falls on a series of steps not quite hewn from the living rock, lifting the hiker onto the outlet of the lake and onto a series of large rectangular stepping stones. Even though these stones form the trail itself here, many hikers find them inviting places to sit, and I don’t recall a visit where I didn’t have to step over or around lounging hikers here.

There’s no doubt that the view from these stepping stones is spectacular, but it’s just as spectacular if you go another few hundred feet to the eastern shore of the lake. There, you’ll face the sight that is McHenrys Peak. Water pours off the stark cliffs on all sides here. The main feeder of the lake is behind you, and a crude trail climbs beside it, gaining four hundred feet of elevation in just 1,600 feet of distance. Even late into summer there is snow on the southern slopes here.

Levitating snow

At about 11,000′ of elevation, the terrain levels off and you find yourself on a large expanse of granite slabs, clumps of willow, and marshy areas where water flows nearly everywhere. Every time I’ve come up here, I’ve found many elk. Being so high, the wildflowers are much smaller than those lower down. They’re just as colorful and diverse, but are tiny in comparison. The scale is different: you won’t find entire slopes splashed with color, but that color is all around you. You just have to look closer.

Navigation isn’t particularly difficult here. After a while the trail fades away, but hikers have left a multitude of cairns. There are sometimes so many that they’re not helpful on a grand scale, but they often will lead you through the sections of willow.

Busy bee

To get to Green Lake, I kept the main stream on my right until I was nearly to the lake. I had my micro spikes with me, anticipating that I might be crossing some snow. Just below the lake I came across the solitary section I’d need to cross, and it was only a few hundred feet. Arriving at the base of this snow field, I found myself in the midst of a herd of elk. To my left was a large bull, antlers large and velvety. To my right was a cow and two calves, still sporting their youthful spots. The cow had an ear tag and wore a big collar with a large 9. I’m no judge of female elk flesh. Perhaps she was a 9. Or, perhaps, the collar wasn’t intended as an indication of her beauty.

Bull elk

They were really quite close, twenty or thirty feet. I’ve been close to elk fairly often. I’ve never felt threatened by them, but just the same I didn’t want to put myself between the cow and her calves. I also didn’t want to be closer to the calves than I was to the cow or bull. But to continue on the last few hundred yards to my destination, I’d have to walk right through them.

I sort of yelled at them, “I want to go that way!”, pointing across the snow. They looked at me quizzically. They clearly weren’t getting my drift. After further hollering and gesticulation I clapped my hands loudly. This got the calves to move to my right, on the other side of their mother, and I finally felt it was okay to proceed.

Had there been no elk there, I probably would have put on the spikes. I carried them all this way, so why not use them? But I didn’t want to sit there in the middle of the herd any longer than necessary so I proceeded without them. I didn’t need them, and on the way back down I again didn’t bother with them.

Green Lake

The rain had stopped some time ago, and the small breaks in the clouds had turned to mostly bright blue sky. There were still clouds, but they were white and fluffy and (as always) relatively fast moving. It would be hard to expect much better weather for a picnic beside an alpine lake than I was having.

There’s a snow field that sits on the eastern shore of Green Lake. I think it’s always there. Today, there were two little icebergs (or would they be snowbergs?) that were floating freely in the lake, recently broken off the main field. It might have been interesting to have the time lapse camera recording them, but instead I had it aimed at Spearhead and the clouds behind it. I would have liked to sit on the eastern shore, but there wasn’t a lot of shoreline there free of snow, and the flow out of the lake was running a few inches too high for me to cross without risking getting wet feet, so I stayed on the northern end.

On the way up from Black Lake I encountered a couple of climbers who had spent two nights on a bivy permit on Spearhead. I came across another couple of climbers on their way down at about the point where the route to Frozen Lake diverges from my route. So I kept an eye out for climbers on Spearhead. I don’t really know what interests climbers, so I didn’t know where to look. But I did see somebody wearing a pink jacket or shirt who hadn’t very far up the cliff.

Gathering storm

After half an hour I headed down. My herd of elk was still there, but they’d moved a bit to the east and I didn’t have to split them to make my exit. On the way up, you’re facing the stark cliffs in the immediate vicinity. Heading down, you get a nice view of the Mummy Range in the distance. The clouds there were no longer white and fluffy, but steel colored and menacing. With the divide just a few hundred meters to the west, you can’t see what sort of weather is headed your way, but it was obvious that on the way down I’d likely get more than the light rain I encountered on the way up.

I’d kept the rain coat on through my lunch and only packed it away when I refilled my water bottle on the descent to Black Lake. My shirtsleeved hiking was short lived, though, as the clouds opened up by the time I got to the bridge leading to the Glacier Gorge campsite. The thunder that was rumbling in the distance was now crashing in the immediate vicinity, so I kept my pace up.

Usually there’s a fair crowd on the slabs that form the Mills Lake shoreline but not now. Nobody wanted to sit in the rain. It wasn’t heavy enough to entirely obscure the view to the south, but certainly heavy enough to make the view less pleasant. Between here and the trail junction I ran into a young couple on their way up to Mills: she wearing sandals and a jacket, he shirtless and smiling. Even with my jacket on and hiking a brisk pace, I found it slightly chilly.

A bit farther down I found a solo hiker standing in the shelter of a tree, assessing the skies. I told him it would quit eventually, but no telling how long that might be. He was going to wait it out. That turned out to be a short wait for him, as the rain stopped when I was half way down the Fire Trail, and the sun was again shining brightly. It was about here that I realized I’d probably left the passenger window of the car open an inch or two. Oh well.

Traffic down the mountain was heavier than last week, but what I’d call more or less the new normal. Until I got to about mile marker 10, where we came to a complete stop. At about mile 4 an ambulance had passed me going towards Estes, lights and siren on. It should have been obvious to me that I’d run into the scene of an accident but it didn’t click until we were stopped. It took nearly half an hour to get going again. They had the road down to one lane, letting a few dozen cars pass first in one direction then the other. When I passed the scene, I didn’t see any damaged vehicles. Had they already cleared the wreckage, or was it off the road, down the slope? I suspect the latter.

I can’t help but say that it was a very enjoyable day. A hike to the upper reaches of Glacier Gorge is always rewarding and satisfying.

Timetable

UpDown
Trailhead8:10 am3:31 pm
Mills Lake9:06 am2:42 pm
Black Lake10:25 am1:30 pm
Green Lake11:55 am12:30 pm

Loch Vale

Monday, October 29

Things are a bit on the slow side at work, and I have a few vacation days I haven’t used. So with the weather looking good for today, I took advantage of the opportunity and headed up to the Park for a short hike. I figured I’d try something similar to my last hike – that is, a short hike to a familiar destination but try to get a different perspective by gaining a little elevation. So I headed up to the Loch, with the intention of finding a nice rock outcropping with a view of the lake and the valley in which it sits.

I wanted to park at the Glacier Gorge parking lot, so I left a bit earlier than last time. This had the side-effect of missing the worst of rush-hour traffic going into Boulder. Between Boulder and Lyons I was treated to a beautiful sunrise, which is always a nice way to start the day.

There was relatively little traffic on US 36 and now that it’s off-season, I skipped my usual detour by the hospital and actually went through downtown Estes Park. Approaching the RMNP entrance station, I saw a few temporary signs indicating that there was a chance of fog or smoke. I thought it was odd, as the weather was fine and the skies were mostly clear. In Moraine Park their electronic sign told me that the Bear Lake parking lot was already full. I wondered how that could be, given that it was 8:30am on the last Monday of October. How can there possibly be that many people there already? If the Bear Lake lot is already full, there’s no way I’ll get a spot at Glacier Gorge.

When I arrived at Glacier Gorge parking lot there were about eight cars there. Clearly the sign in Moraine Park was in error. Two of the eight cars had just arrived moments before I did. Two guys got out of one of the cars, looked at each other, decided it was too windy and got back in their car. I told them it wouldn’t be windy on the trail, but they weren’t convinced. And, actually, I didn’t think it was very windy at all, compared to what I’ve found there in the past.

Andrews Glacier barely visible

Although I’m quite comfortable deciding what to wear and what to carry on my summer hikes, I’m not that experienced in autumn or winter. I think part of my problem is my lumbar pack. It’s sufficient for my summer day hikes but doesn’t allow me to carry what I might need on a colder weather hike. Today I wore my thermal (light or medium, I forget) underwear, hiking pants, Hawaiian shirt, hoodie, and windbreaker. I had a woolen hat and gloves, and I had my rain jacket as well. I brought my microspikes and gaiters, but ended up leaving the microspikes in the car. I figured I probably wouldn’t need them, but once I got off the trail there might be enough snow I’d want the gaiters. In the end, I didn’t use them.

The day was quite pleasant. On the trail, the wind was not an issue and I didn’t think about it until I got near my destination. There was very little snow on the ground for my entire hike, while the trail had icy stretches that became longer and more common as I gained elevation. The ice was only in the shady bits, starting about halfway up the fire trail. About half way between the Mills Lake trail junction and the Loch I encountered a hiker on his way out. He was trying for Sky Pond but turned around at Timberline Falls. All he had was microspikes and that wasn’t enough for him. He was the only person I met since the parking lot.

Shortly after arriving at the Loch I started looking for a place to start climbing. As it turns out, I started climbing too soon. But it didn’t take long to run into the talus field that’s on the south side of the lake. It runs at an angle. If I’d kept to the trail for a little longer I’d have come across it and had an easier way up.

Picnic view

In planning the hike, I had considered following this talus field all the way up to one of Ed’s glacial knobs. But I found a nice place with a view of the valley that was in the sun and out of the wind. I was perhaps two-thirds of the way up the talus. There was a bit of snow here, but I easily avoided it. I didn’t want to step on some snow only to find out that there’s nothing beneath it but a giant hole.

Interesting grain, a little burned around the edges

In the talus there’s a fair amount of dead wood. Not a lot: it’s a talus field so more or less by definition there aren’t any trees. But there are a few ribs of soil here and there and over the few hundred yards of talus I maneuvered I came across quite a few pieces of deadwood. Each one showed signs of being burned. Some were subtly discolored, just a touch of brown. Others were deeply charred. I assume all these were the result of the Bear Lake Fire of 1900. Burned bits of tree can be found throughout the area, but they’re move obvious here as no trees have grown here in the intervening century.

About two-thirds of the way to the top of the talus field I found a spot with a nice view. As a bonus, it had full sun and was not particularly windy. I fully expected that any place I found that was in the sun and wasn’t surrounded by trees obstructing the vista would be blustery, but my little spot was close to ideal. It may very well be that it wasn’t as windy as it normally is in the cooler months this close to the Divide. But it wasn’t exactly calm. The small clump of trees thirty or forty yards above me sang a bit when the heavier gusts blew by.

Interesting textures

While I let the camera run, and after my picnic, I explored the immediate neighborhood. This meant hopping from rock to rock through the talus. On my way to a spot where I could get a bit of a view of Andrews Glacier, I hopped on a rock that looked to be about three feet on a side. It was a “wobbler”. I’m often concerned that some of the smaller rocks I step on will move, but haven’t had that happen with a boulder this size. Frankly, it kind of spooked me. This one had to be three quarters of a ton or so. I had a quick mental image of it moving a large area of talus; not something I want to be in the middle of. From then on, until I got back to the trail, it seemed like every rock I stepped on moved a bit. I know it was my imagination, but it had me being very careful.

After about an hour of watching the world go by, I packed up and headed back down to the trail. Along the way I came across a large upended stump. Its color matched all the other dead wood nearby, except that it had no obvious signs of burn. What it did have was a rock that the roots had grown around. I took a few pictures of it from various angles; didn’t get one that shows it very well, but so it goes.

Rock encased in wood

Back on the trail I started encountering other hikers. One couple asked if they’d passed Sky Pond. I told them that they hadn’t, and that they weren’t likely to make it past Timberline Falls given that they lacked any kind of traction devices. The next couple I came across said they were properly equipped, and I wished them luck. They looked to be fit, but it seemed to me they wouldn’t be getting up there until fairly late in the day.

The Loch

I briefly considered taking the long way back to the car and spending a few minutes at Alberta Falls. Maybe I was feeling lazy, maybe I preferred the solitude of the fire trail, and in the end took the shortcut. As I hiked out, I shed my layers ending up in shirtsleeves. The forecast high for Denver was in the mid-70’s, while NOAA predicted a high in the mid-40’s for Loch Vale. No doubt, it was warmer than the mid-40’s where I had my picnic.

Leaving the park I saw why they had signs up warning of smoke or fog: they were doing a prescribed burn on the north side of the road, covering the whole distance between the entrance station and the Beaver Meadows visitor center. By now all the excitement seemed to be over: I saw a fair amount of smoke but no flames.

Prescribed burn

Timetable

There Back
Trailhead 08:55 AM 01:22 PM
Mills/Loch Jct 09:35 AM 12:45 PM
The Loch 10:05 AM 12:24 PM
Picnic spot 10:43 AM 11:45 AM