Thunder Falls

Posted on September 18, 2024 by dhill

Here it is the middle of September and I’ve only been to RMNP for two day trips and a backpacking trip. This is the least amount of time I’ve spent in the Park since we returned from our exile in Phoenix. I haven’t set foot in Wild Basin or even driven on CO 7 this year. It seems like a good time to hike to Lion Lakes.

There are four named lakes there, and a couple of falls. The hike affords nice views of the dramatic eastern face of Mount Alice. There are no campsites here, and stock is not allowed on the trail, and as it’s nearly seven miles to Lion Lake #1 it’s not crowded.

Thursday, September 12

I awoke before my alarm went off and I was out of the house and to the trailhead earlier than expected. There was plenty of parking and I backed into an end spot by the restrooms.

I’ve been to Lion Lakes a few times. I tend to get a little obsessive about going to a different place for every hike. I need to get over it. But the fact that I make repeat visits to a place says a lot about what I think of the place. I yearn to visit new places. When I don’t scratch that itch, I’m not going to go back to someplace that I think is unexceptional.

I didn’t really have a plan for the day, other than getting to Lion Lake #1. I had options. By the time I got to the lake, I had decided what to do. If you follow the unnamed outlet stream down from Lion Lake #1 you’ll come across Thunder Falls. Foster says the place is “no small task to reach”. The navigation sounds pretty simple, though, so I assume there must be obstacles.

I stopped for lunch at the lake. The million-dollar view is from the east bank. Today I went to the west bank. Much of the west bank is a grassy marsh, but by mid-September, it’s pretty dry. I picked one of the large, flat boulders in the pleasant sunshine and had my lunch: a PB&J sandwich, chips, and a beer.

I have a couple of go-to sandwiches for hikes. One is a turkey bacon avocado and pepper-jack cheese, where the bacon is jalapeno bacon. The other is ham, salami, and pepperoni with provolone cheese. I almost never take a peanut butter sandwich.

My favorite peanut butter delivery mechanism is toast. Put a stout slice of homemade bread in the toaster just until it starts to brown. I want warmth but not crispiness. Slather on a nice layer of creamy peanut butter and wait a minute. The peanut butter gets molten. You have to be sure to hold the toast level, or it drips into your hand. Not very portable, though.

When it comes to PB&J, I’ll say I haven’t had peanut butter and jelly since about the second grade. Jam or preserves beat jelly every time. Strawberry was my favorite in my misspent youth. It’s been red raspberry for ages now.

Today’s sandwich was on the store-bought sourdough rather than my low-budget home-baked bread. My bread is on the dense side. I wanted pockets. Sourdough has nice pockets. The slices are a bit small, so I made two sandwiches. They survived the morning’s hike unsmushed, which was nice. By the time I bit into one, the preserves had infused the bread and filled the pockets. Yum.

By now you might be wondering just what sort of beer pairs with a PB&J sandwich. To tell the truth, I didn’t put any thought into it at all. I got lucky. I brought New Belgium’s 1985 Mango IPA. The tart hoppiness of the IPA complemented the sourdough bread, while the sour mango played well with the raspberry.

Picnic over, I headed for Thunder Falls. Even though I wanted to be on the east side of the stream, I continued circumnavigating the lake. I ran the risk of not finding a convenient streamcrossing. The outlet of the lake is typically marshy. The stream meanders lazily and there are a few ponds. I found an easy crossing, then worked my way downstream.

Tanima Peak (l), Mount Alice (r)
Left to right: Copeland Mountain, Mahana Peak, Tanima Peak
Today’s beer
Chiefs Head Peak
Lion Lake #1 outlet
Cattywampus Texan

The bushwhacking wasn’t terribly difficult. The deadfall wasn’t too bad, and the ground descends very gradually at first. You can hear the falls long before you can see them. Obviously, the terrain next to the falls is as steep as the falls. I wanted to get to the bottom of the falls, but all the rocks below me were wet, so I didn’t want to go that way. I made a half-hearted search for another route before giving up. The falls aren’t very large, and there’s not much water in the stream. If I were to return in July, when the flow is much greater, I’d make more of an effort to see the falls from below.

I had nearly complete solitude much of the day. About half an hour away from the lake I ran into one hiker on his way down. He turned around before he got there. While having lunch, I saw two pairs of hikers, one going up and the other going down. I didn’t see anybody else until I back to the main trail, a bit over a mile from the parking lot.

When I got back to the car, my nice end spot wasn’t an end spot anymore. A Volvo with Texas plates was parked cattywampus in front of me, between the tree and the rock, on top of the slab of sidewalk. C’mon, man!

It was another enjoyable hike. The weather was ideal, the solitude was welcome, the exercise invigorating, the scenery fantastic, and the PB&J and beer were tasty.

Upper Chipmunk

Posted on September 15, 2024 by dhill

I scheduled only one backpacking trip this year, two nights at the Upper Chipmunk campsite near Ypsilon Lake. The objective is to get to Spectacle Lakes. Just judging by mileage, I should be able to do Spectacle Lakes as a day hike. I’ve already done Chiquita Lake and Fay Lakes as day hikes. Both those are reached from the same trailhead, are farther than Spectacle, and at about the same elevation. But the last push to Spectacle involves negotiating a steep granite slab and may be more than I can deal with.

September 2-4

I didn’t see much point in getting an early start. The campsite is just a bit over four miles, so it’s long a long hike. The lot at the trailhead isn’t very large, but when I picked up our permit, the ranger told me we could park at the picnic area for the alluvial fan. Still, I had my usual anxiety about finding a parking spot.

Naturally, the trailhead lot was full when we got there about ten. We headed to the picnic area. There are two parking lots for the alluvial fan, one east and one west. The two are connected by a paved path that is wheelchair accessible. The trailhead is east of the east lot and, as you might guess, this lot was full. We did find a place in the west lot, though, so we were ready to go. Parking here, our hike was half a mile longer each way, but it’s an easy half mile so not a bad trade for leaving three hours later. In compensation for the bonus half-mile hike, we spotted a few wild turkeys.

What I hadn’t given much thought to was my lunch schedule. I’m a creature of habit. I like my lunch in the noon hour. The noon hour had come and gone and we seemed to still be a fair distance from camp. I didn’t want to stop on the trail to dine, so kept pushing. But my breakfast was nothing but a memory and the uphill hike carrying thirty pounds more than I take on a day hike had me really wanting to take a break.

Not long past Chipmunk Lake (which is really a pond and not deserving the epithet “lake”, but it has a very nice view of Ypsilon Mountain), I was really struggling. I knew we couldn’t have far to go, but I had to take a break. I spotted a dandy place to relax: a the base of a talus field, basking in the sun, with a wealth of raspberry bushes bursting with ripe berries. Oh, joy! The raspberries in my back yard were pitiful this year, so I was delighted to eat some fresh, tasty berries.

After our rest, we resumed our slog. Thirty-five paces later, we reached the sign pointing up a spur trail to our campsite. Yeah, shame on me for taking a break. But, boy, were those raspberries delicious. I came back for a second visit the next day and even grabbed a last few berries on our hike out.

Upper Chipmunk has two campsites and a privy. One site was occupied, so we took the other. There really isn’t much to choose from between the two. There’s a minimum of deadfall around the sites. They’re fairly close to each other though. No matter, it’s a pleasant place to spend a couple of nights. We tucked into lunch, then started setting up camp.

The moment I finished erecting my tent, the skies opened up. It wasn’t rain, it wasn’t snow, it wasn’t hail. It wasn’t even graupel. It was slush. Slush was falling from the sky. Slushballs as big as a quarter inch diameter, plopping everywhere. I dove into the tent to wait it out. The slush turned to rain, which lasted almost an hour. I had a little power nap. About an hour later, the storm abated and I crawled out of my tent.

Gordon’s timing wasn’t so good. He uses a hammock with a cover, but he hadn’t gotten it put together before the skies opened. He spent the hour sitting on a boulder, huddled under his poncho. He didn’t say so, but I imagine he was wondering why I had to take a break in a raspberry patch so close to our campsite. Sorry, Gordon.

I collected enough slush from the rain cover of my tent to pack around my beers. I’ve gotten accustomed to drinking warm (or warmish) beer on my hikes, so this was nice.

We spent what was left of the afternoon exploring the area around the campsite and Ypsilon Lake. There is a trail from each campsite down to the lake that’s a bit shorter than taking the main trail, but to return to the campsite it’s easy to get on the wrong trail and end up at the other site.

I’ve been to Ypsilon Lake at least four other times. I like to think I’m paying attention to my surroundings, but that’s not always true. After sitting beside the water for an extended time, I began to wonder if the lake is dead. I saw occasional disturbances on the surface of the water and I thought it was fish rising to the surface. But the water is clear and from the shore you can see a fair piece into the lake. I never saw a fish, and there’s nothing growing on the lake bed. We spotted a solitary duck criss-crossing the water, clearly hunting for something. I watched it dive underwater a few times, staying under for as much as 20 seconds and coming up many yards from where it dove, but I have no idea if it scored anything.

On day two, we had a leisurely morning. Spectacle Lakes are only about a mile from our campsite. There’s no official trail, but enough people make the trip that route finding isn’t terribly difficult. It’s steep, and there are a couple of water crossings. I didn’t find any more raspberries on our climb, but we did come across some huckleberries. Not quite ripe yet.

By 10:30, we had arrived at the crux of the trip. I’ve read a number of descriptions of the route. They all mention this steep slab. I’m not a big fan of steep slabs. When we got to the bottom of this one, I knew I wouldn’t be going any farther. I am always concerned that I’ll be tempted to climb up something that I won’t be able to climb back down. I wasn’t tempted to climb up this. Gordon is more of a mountain goat, though, and he had no qualms about it.

I waited on this ledge, somewhere about 11,200′ above sea level, while Gordon continued up to the lakes. It’s a pleasant little spot for a picnic, so I ate my lunch. No, I didn’t bring one of my beers with me. While dining, my phone chimed with a text message. I wouldn’t have thought I’d have cell service up here. I had a nice view of Twin Sisters, Estes Cone, and Longs Peak that I posted to Instagram. Technology, gotta love it!

In the lead up to this trip, I’ve been telling folks that I was counting on Gordon to get me to the lakes. It never was a serious thought: nobody can take me where I’m unwilling to go. But I think he took it to heart. After he returned to the ledge, with full knowledge of what lies between here and the lakes, he told me he thinks he can get me there. All we need is a length of rope with knots every few feet. That would get me past this twenty or thirty feet of terrain I’m not happy about. Needless to say, we didn’t bring any rope. I’ve mentally put Spectacle Lakes on my list of RMNP lakes that are beyond my reach.

We spent another afternoon in the environs of Ypsilon Lake. Gordon is a curious guy, always interested in his surroundings. He made a circumnavigation of the lake, then sat a few yards from my position. He found a rock by the water where a few lady bugs appear to be farming aphids. Maybe not aphids. But these lady bugs sure had an insect farm of some sort on that rock. While he was watching the lady bug insect farm, a ground squirrel stole one of his nuts. The next time the squirrel took a nut, Gordon got a close-up of it.

Wild Turkey
Raspberry patch
Our campsite
Slush-cooled beers
Ypsilon Lake outlet
Ledge view
How to proceed?
Spot Gordon
Ypsilon Lake
Gordon, nature photographer
Huckleberries!

Other than our slush storm, the weather was quite nice on Monday and Tuesday. It didn’t get very cold overnight, and when I ventured out of my tent for a “comfort break” in the wee hours of the morning, the sky was clear, moonless, and full of stars. I didn’t see the Milky Way, though. So it goes.

Before turning in on Tuesday night, we talked about what time we wanted to pack up in the morning. We agreed on 9:00, but the morning dawned overcast and threatening. We packed up early and were on the trail before it started sprinkling. It never rained very hard, but the low hanging clouds cut the tops off the high mountains: judging from the view of Longs Peak, the ceiling was not much above 11,000′.

I have no video for this trip. I managed to leave the GoPro on the living room floor where it does me no good. So it goes. My other technological failure was with my water purification. My Steri-Pen worked the first time I refilled my water bottle, but didn’t work after that. I’ve since swapped the batteries but it’s still not working. I guess I’ll be looking for a replacement before my next backpacking trip.

In spite of not reaching my destination, it was a nice trip.

Mt. Ida

Posted on July 11, 2024 by dhill

I’ll get to Mt. Ida in a moment, but first I’ll mention that I made a trip to one of my happy places: Black Lake. I’ve been there a couple of dozen times, so there’s not much point in going into any details. It was a sort of last-minute decision, insofar as a trip to the Bear Lake corridor in RMNP can be last-minute. I picked up a pass to get me in between 8 and 10 and arrived a few minutes after 8. The line at the entrance station was quite long.

My plan was to perhaps make it to Blue Lake, but I figured that might be a bit on the aspirational side, being that it was still June (the 28th, actually). I encountered a number of people who said they were headed to Black Lake, but I never saw any of them again. There wasn’t a huge amount of snow, but clearly enough to discourage many people.

I went a short way above Black Lake and found a nice picnic spot. Being that I got a bit of a late start and there was a little more snow than I was expecting, I didn’t really try to go any farther. As I had my picnic, a number of hikers came down from above. I chatted with two pairs of hikers who had wanted to get to Frozen Lake but were stymied by the first water crossing. Another pair of hikers told me they’d failed to reach Green Lake.

Friday, July 5

The idea to finally summit Mt. Ida wasn’t exactly last-minute, but it was poorly planned. By that, I mainly mean to say that I was oblivious to the fact that the Park would be about as crowded as any day on the calendar.

I arrived at the entrance station at 7. Well, let’s say I made it to the Beaver Meadows visitor center at 7. It took another 15 minutes to get to the entrance station. When the day dawned I was thinking that I’d have a nice uncrowded run over Trail Ridge Road. Hah! Silly me.

Now that reality has set in, I was starting to think about a Plan B. There isn’t much parking at the Milner Pass trailhead and I doubted I’d be able to get a parking spot. This concern was well-founded. When I got there, the lot was full. I needed a comfort stop, and so I parked illegally to use the restroom. Luckily, no Plan B was necessary, as somebody was leaving by the time I returned to my car.

I put boots on the trail at 8:17. This is my fourth hike up the Mt. Ida trail, none of the previous three with the intention of reaching the summit. They were all about reaching the various Gorge Lakes. There are three I haven’t been to: Inkwell, Azure, and Highest. I’ve proved that they’re out of my reach from below. Foster has a couple of routes to those three from above. It’s probably too steep for me, but I won’t know until I put eyes on the terrain. So off to the summit I finally go.

I seem to have weather issues whenever I’m hiking around Mt. Ida. My first visit to Arrowhead was the day it started raining in the 2013 floods. On my backpacking trip, we got rained on for more than a day. I got rained on, too, when I made it to Julian Lake. Today, the sky is a vivid blue with some small fluffy clouds. Yay!

The morning was chilly. I started in shirtsleeves, a bit cool, but expecting to keep warm through exertion. This worked until about fifteen minutes after I got above treeline. The wind was not fierce, but brisk. I put on my jacket.

I passed about as many hikers as passed me and didn’t encounter any people on their way down until I was maybe half an hour from the summit. One of the online guides says this hike is one of the most popular in the Park. There’s not enough parking to support that idea, but it is a popular hike. I was on the summit for about an hour. People came and went, but there were always eight or ten on top.

It took me three hours to reach the top. It took me about three seconds to decide there was no way I’d get to any of the Gorge Lakes from up here.

Azure Lake, Inkwell Lake
Highest Lake, maybe, and Longs Peak
“Got any food?”
Julian Lake

There were fat marmots everywhere. Twice they didn’t move off the trail until I was within a step of them. At the top, they were so used to people that they’d come right up to us, sniffing our bags. Brazen. I saw a few pikas, always carrying grass or flowers in their mouths, but couldn’t get a photo. They don’t stand still. On the summit, one ran almost between the feet of a guy I was talking to.

There’s a fairly long stretch of trail that weirds me out. I swear, it’s uphill in both directions. It’s not, of course, but it sure seems that way to me. Looking at the map, I see it runs within a few feet of 12,000 for a long stretch. Hiking up, even though you’re not climbing, you’re going up to that summit up there, so it looks like this level stretch is uphill. I don’t have a great explanation as to why it looks like it’s climbing on the way down.

On the way back, it wasn’t me asking people questions, it was people asking me. One guy wanted me to point out the summit for him. I thought the answer was fairly obvious, being the highest thing around, but didn’t give a snarky answer. Nearly back to treeline, another guy stopped me to ask how far it was to the top. I told him it took me three hours from the car; he said, “Two hours from here, then?” He looked disappointed. I suggested he go a bit farther up the trail and then find a nice spot to enjoy the view for a few minutes.

Two and a half hours from the summit back to the car. About half an hour from the car, when I took my jacket off, I realized I had neglected to slather on any SPF. Oops. I had the jacket on nearly the entire time, with the hood up for quite a bit of it, so hopefully my face wouldn’t be too badly burned. I only used my trek poles near the summit, and when I had the poles stowed, I often had my hands in my pockets.

Back at the car, I applied the sunscreen, better late than never, and took the top off the car for the drive home. Even if the traffic is horrible, I can enjoy the ideal weather for a drive in a convertible.

Trail Ridge Road and US 36 weren’t as bad as I was expecting. Traffic on 36 moved at nearly the speed limit. And I was pleasantly surprised that, instead of Friday rush hour congestion, traffic was very light from Boulder to home.

Porcupine 2

Posted on August 2, 2023 by dhill

Saturday, July 29

We had a leisurely morning, putting boots on the trail shortly after 8.

As I said, I’ve hiked to Bench Lake before, solo. I remember easily finding the beginning of the “trail”. I recall seeing a few cairns, and that the trail was not great, disappearing and reappearing, but I don’t remember it being particularly challenging. I have a quite distinct memory of the final few yards before reaching the lake where I lost my full water bottle.

For most of my professional life, when doing software support, I had a saying: “The user is not a reliable witness.” They either don’t really remember what they did, or they have some motive for not telling the whole story. When it comes to getting from the trail to Bench Lake, I was not a reliable witness.

We found no obvious trail near Ptarmigan Creek. Route finding was challenging. We did come across a few small cairns, but very few. And the last few yards involved a five or six-foot climb up solid rock, not the steep, loose stuff I distinctly recall. How is it my memory has tricked me so?

When we arrived at this final six-foot climb we met two hikers on their way down. They had zone camped up here. They said they’d wanted to “get to the lake”, but didn’t say which one. I think they meant Ptarmigan Lake. In any event, Bench Lake was the only one they reached. I give them lots of credit, climbing up here with backpacks.

I don’t know how many hikers make it up here, but I don’t imagine it’s many. Even so, they found somebody’s water bottle. It wasn’t mine from the last time I was here, but a disposable one. They reported seeing a nice herd of elk and that they found an elk skeleton. We exchanged farewells and headed our separate ways.

Standing at the outlet of Bench Lake you are at the foot of a large valley, “The Wonderland”. From here, we will head north up the valley to find the confluence of the outlet streams of the three alpine lakes. In theory, we could go to either Snowdrift or Wonderland and come down the other. No amount of map study is as good as getting eyes on the terrain.

Until about September, the choice in these valleys is whether to slog through marshy meadows or keep to higher ground and deal with deadfall mazes. I didn’t mind the wet ground so much, it was never ankle-deep. But Gordon was in lightweight shoes and was getting his feet wet. We kept switching back and forth.

We were nearly to the confluence before we got a good view of the outlet from Snowdrift. It looked really steep. I certainly didn’t want to hike down it, and I wasn’t sure I was willing to go up. It was getting on towards 11, and we still had a mile of bushwhacking and 700 vertical feet to go. There was no way I’d be able to get to both today, so it was an easy decision to head to Wonderland Lake and skip Snowdrift.

The creek in this wide, flat valley often becomes braided, running two, three, or four courses through the meadows. We crossed Ptarmigan’s outlet and then Wonderland’s, to climb up to the lake on the western side of its stream. We made at least four crossings to cross the two streams. In this area, we came across where the elk had bedded down. The grass was flattened by five or six elk. We didn’t see any elk all day, it’s a big valley, but I was stepping over their droppings constantly.

Having made our way to the head of the valley, it was time to make our second big climb: 350′ in 0.2 miles. Gordon led the way. He’s an excellent route-finder. He’s sensitive to my limitations regarding exposure, and he’s quicker than I am and gets far enough ahead of me that even if he backtracks a few yards, I never catch up. Saves me a lot of effort.

At the top of the climb, you emerge onto a broad and deep shelf of dune-like granite marbled with ponds and grassy ramps. The shelf holds both lakes, maybe half a mile apart. We still had another two hundred feet to climb, but nothing steep. There was no krummholz, and the only willow I saw was no more than a foot tall and easily avoided. Maybe it was the climb, but the view of Andrews Peak behind us was breathtaking.

The second or third time we told each other the lake was over the next rise, we finally emerged above the southern shore.

The hike from the campsite to the lake is only about three miles. Adding a mile round trip to the other lake doesn’t sound too bad, particularly given the open sight lines. We didn’t get to the lake until 12:35, so maybe had we left an hour earlier… even so, it wouldn’t have mattered. I was beat: my next step from here was to head back to camp.

I ate my picnic lunch and watched the world go by. Gordon circumnavigated the lake, pausing often to inspect something that caught his attention. We started back.

Bench Lake and the valley beyond
Bench Lake
Andrews Peak
“Wonderland Lake”
Elk backbone

Only a few steps below the lake it started raining, soon followed by rolling thunder. After a few minutes, the rain turned to hail. But it was over before long. We didn’t exactly follow our route up. Not that we weren’t trying. “Did we come up the right side of that outcropping or the left?”

Back near the confluence of the streams, before making four or five crossings, we came across the elk skeleton the other hikers reported. I’ve seen a few now, and generally they’re not so much “skeletons” as “piles of bones”. This one, though, had an intact backbone.

Approaching Bench Lake, we came across a tree with an NPS sign posting “No Fishing”. I’m sure we walked right by it on the way up, but it’s facing north instead of south. It’s pretty weather-worn; has probably been there for several years. I wonder how often they send a ranger up there to replace it.

Just before returning to where we met the other hikers, we spotted a nice game trail. Gordon followed it. It wasn’t in the right direction; he suggested that it just bypassed the big rock we’d have to climb down. I wondered aloud how far we wanted to follow it. Gordon’s response was, “That’s the question!” We never turned back.

Next to Bench Lake’s outlet is a glacial knob about a hundred feet high. The trail took us over the saddle between the knob and the mountain flank to the east. In camp last night, I spent quite a while looking at this terrain. I was wondering if it might be easier just to head to Ptarmigan Creek in a straight line from the camp instead of taking the trail to the creek. It seemed doable. I didn’t even consider coming down from the saddle, though.

Game trails are nice until they’re not. This one was nice for quite a while before it petered out on a stretch of steep, loose aggregate. My favorite! I was too concentrated on my next step to look for my tent down below. I’m sure there were several places where it would have been visible. The steep, loose stuff turned into a deadfall maze that eventually led us to Ptarmigan Creek, only a hundred yards or so above the trail.

Back at camp, we put our cans of beer in the stream to chill. We were visited again by the lone doe, retracing her steps of yesterday evening almost exactly, and at almost the same time of day. She made an extra visit, well after eight, when all was in shadow, she in a mad dash.

It was overcast when we turned in, but on my early morning comfort break the stars were shining brightly.

Sunday, July 30

The hike out was routine. I spotted two snakes, one not longer than 18″, the other not shorter than a foot. I’ve seen snakes in the Park before, but not more than a handful. I was surprised to see two, within just a few minutes of each other. I also had a covey of dusky grouse cross the trail in front of me. I didn’t get a good count, maybe a dozen, including four young ones.

I was happy to be headed home. Yesterday was a maximum effort day; exhausting but fulfilling. I’m so fortunate that I am healthy enough and fit enough and have the means to take these trips. I try not to take it for granted.

I really enjoy navigating my way through this untracked wilderness.

Porcupine 1

Posted on July 31, 2023 by dhill

Ptarmigan Creek is about six and a half miles up the North Inlet trail. The creek joins North Inlet after falling about a thousand feet in about half a mile. The creek drains a hanging valley called “The Wonderland”. In this large valley are Bench Lake, perched above War Dance Falls, and three high alpine lakes: Ptarmigan Lake, Snowdrift Lake, and “Wonderland Lake”. (“Wonderland Lake” is not officially named but is widely used.)

I’ve day hiked to Ptarmigan Lake and Bench Lake and know that the other two are well out of my single-day range. Regular readers will recall that I’m a big fan of the North Inlet Trail. My two longest day hikes were on this trail. Gordon and I did a backpacking trip three years ago and on the hike out, I paid particular attention to the locations of each of the campsites near Ptarmigan Creek.

The plan was to spend two nights at Porcupine, a quarter of a mile from Ptarmigan Creek. Hike in on Friday, spend all day Saturday in “The Wonderland” in an attempt to visit Snowdrift Lake and “Wonderland Lake”, and hike out on Sunday. Here’s what Lisa Foster says about reaching Snowdrift and Wonderland:

Reaching the lakes involves slogging through marshland and bushwhacking into stunted forest, then scrambling over rough talus fields to boulder-strewn granite benches.

In the off-season, I bought a new sleeping bag and repaired or replaced equipment due to the squirrel incident last year. I have not fully repaired the backpack – the damn squirrel ate a good amount of the webbing. I might still need to have the webbing repaired, but I’m not sure it’s necessary. I replaced the half-eaten poles with a pair of carbon fiber ones with cam-style locks.

Friday, July 28

I’m starting to get paranoid about how early I need to get to the trailhead in order to get parking. The campsite is seven miles from the trailhead, which is a fair distance, but you only climb 800′, and the trail has many extended sections that allow you to keep a long, steady stride, as if on a sidewalk. I figure three or three and a half hours is all it will take. There’s no point in getting to the trailhead at 7 am. Given an estimate of two and a half hours drive to the trailhead and three and a half hiking to camp, Gordon suggested he pick me up at 9. If we don’t get to park in the lot, we’ll have to add a quarter of a mile each way to the hike. My worries were needless: there was room for five or six more vehicles.

I haven’t hiked the North Inlet trail since the fire. But I have hiked through several recent burn scars so I had a pretty good idea of what to expect. What struck me this time was the scale of the fire. I hiked on the western fringes of the fire last summer. The extent of the East Troublesome fire east of the Divide is greater than either the Fern Lake fire or the Big Meadows fire. The area that East Troublesome burned east of the Divide is a tiny fraction of what East Troublesome burned in the Park. And the acreage burned in the Park is a tiny fraction of the total fire.

Wildfires are a natural part of the life cycle of the forest. But, historically, fires never burned such large areas. More than a century ago, we decided it would be a good thing to suppress wildfires. So we have a century’s worth of accumulated fuel piling up on the forest floors, and we have a lot of dead trees due to beetle kill.

The trail begins with a stretch of total devastation. I expect that trees next to lakes or streams will survive these fires. The trees along Fern Creek survived this fire, but even around the much larger North Inlet, the trees were burned. Without the forest, the terrain is revealed. Everything in sight is totally burned.

Totally burned: no trees survive. All the trunks are still standing. The fire only burns a couple of millimeters into the tree, not rendering it to ash but roasting it. The needles are gone as are many of the branches. Over the next thirty years, almost all of these dead tree trunks will fall. Deadfall accumulated prior to the fire burned in a similar way, but often with a thicker layer of charcoal.

Also totally burned: the cabin that was about twenty minutes up the trail from the parking lot. It was well-maintained and looked to see regular service. All that’s left now is the “Private Property: Stay on Trail” sign and the old hand pump for the water well.

Last year, near Fern Lake, fireweed was by far the most common living plant. Today, fireweed is still in abundance, but many of the rest of the cast of wildflowers are present as well. If you can stand a long walk in direct sunlight, this should be a great wildflower hike for many years.

Maybe an hour into the hike, we met a group on horseback heading back to the trailhead. I asked them how much farther until we get some shade. The guy I asked laughed. “Back at camp!” In fact, though, it wasn’t that much farther. The area around Cascade Falls didn’t burn too badly. The fire burned thoroughly on the bank opposite the trail, but nothing on the north side of the stream was burned. We took a break here in the shade of the trees and the spray of the falls and had lunch.

Above Cascade Falls, the trail reenters the burn scar. It’s not a long section, and the burn ends before Big Pool. Above Big Pool, there is still some burn, but it’s not totally burned. In places, it looks like the fire was on the ground rather than in the crowns of the trees. Deadfall is blackened, standing beetle kill trees are charred at the base, but many trees still live.

Porcupine campsite is about a quarter of a mile beyond Ptarmigan Creek and is on the opposite side of North Inlet as the trail. It is reached by crossing a long bridge made out of a tree trunk sawn flat. It bounces when you cross it and bounces oddly when two people are crossing it.

There are two sites here. We took the western one without even looking at the other one. The western one is very close to the bridge and only a few yards from the stream. After we were set up, I decided to find out whether we made the correct choice. The eastern camp is about a hundred paces from the bridge and not anywhere near water. Other than that, they were much the same, down to identical sawn-log benches. Due to our easy proximity to water, I think we made the right choice. That camp was unoccupied when I looked, and we never saw anybody cross the bridge. I’m surprised that a campsite went unused.

Total devastation
Charred trunk
Our camp
The stream and bridge
The other camp
Lone Doe

We had nice weather all afternoon. Clear skies above us, but threatening weather to our north. We got sprinkled on briefly. We met a group of four backpackers; we caught up to them and we ended up passing each other a couple of times. I passed them when it was starting to rain and they stopped to don their rain gear. I told them that I could guarantee it would stop raining if I went to the effort of putting my rain jacket on. Amusingly, it quit raining before I was out of their sight.

Our camp was visited by a lone doe. She seemed pretty habituated to people. She would come within feet of us or our gear until one of us made eye contact with her. Even then, she only retreated a few yards. She was browsing around our camp for fifteen or twenty minutes before she crossed the river.

The south side of the river near the camp was unburned, but just across the river, the fire had gone through on the ground. Looking across to the other side of the valley: charred deadfall, charred beetle kill, and still quite a few live trees.

Passing through the areas of total devastation we were unmolested by mosquitoes. At camp, though, it was another story. My third application of repellent was finally enough to get the little buggers to not land on me. They hovered persistently, though, much to my annoyance.

As it was getting dark, I asked Gordon what time sunset was. “Astronomical or civil?” I rephrased the question: When will we see our first star? Neither of us offered a guess, which turned out to be the correct answer. It was cloudy and we never saw any stars. I was awakened during the night by a short rain but otherwise slept well.

And what did I forget to pack? Just paper towels. Genae even asked if I had some, and I showed her a Ziploc bag with what turned out to be nothing but toilet paper. If this is my biggest problem, it’ll be a great trip.

Marigold Lake

Posted on October 23, 2022 by dhill

Due east of Odessa Lake, on a small shelf two hundred feet up the north slope of Joe Mills Mountain, sits a small puddle of a lake. It has no inlet stream to fill it with snowmelt and no outlet stream to drain it. With an area of about a third of an acre, it’s not much larger than the suburban lot my house sits on.

I suspect it is rarely visited, being somewhat difficult to find. I’ve tried to reach it twice before, without success. The only reason I want to go there is to add it to the list of lakes I’ve been to. I admit that’s probably too much effort to reach a body of water not much more than a puddle that probably doesn’t even merit the designation of “lake”.

Chad told me he wanted to go on a hike so we agreed on a date and I made a plan. I decided we should circumambulate around Joe Mills Mountain as on my first attempt at Marigold. According to CalTopo, the saddle between Joe Mills Mountain and Mount Wuh was burned. Round Pond sits on that saddle. Based on what I saw on my Spruce Lake hike, I suspect the trees around the pond have survived. Why not find out? It doesn’t add any miles to the trip, but it does exchange trail miles for bushwhacking miles.

Saturday, October 22

The Park was very busy. The shuttle from the Park and Ride to Bear Lake was standing room only. We put boots on the trail at about 8:30.

It was a bit chilly. The forecast for the vicinity was “sunny and breezy, with a high of 46”. There were some thin clouds much of the day, but we could always see our shadows. In the woods, the wind is no big deal, and most of the day we’d be in the woods, so “sunny and breezy” sounds like a nice day.

An hour up the trail, we hit our departure point and headed cross-country. Our route would be to contour around Joe Mills Mountain at more or less 10,400′. From the trail to about the pond, the forest isn’t terribly dense and deadfall isn’t too bad, so the bushwhacking is a fairly pleasant stroll through the woods.

Before long, the ground in front of us started sloping down: we had reached the saddle, a bit west of it’s lowest point. We wandered around here for a short while looking for Round Pond but didn’t spot it. Frankly, it has a half-hearted search. I was more interested in getting to the burn. Missing Round Pond isn’t missing much.

The forest is denser on the north side of the mountain, and soon we’d need to traverse a fairly steep slope for a while, westbound to Marigold Lake. But first we started seeing burnt trees. Just individual trees here and there, all deadfall; burned with almost no damage to the surrounding forest. One was still standing: a hollow tree, like a chimney. After several of these we arrived at the edge of the burn scar.

I was expecting the edge to be “fuzzy”. Indistinct. Maybe a border of trees that didn’t ignite and kept their dead, red needles. But no. Green, apparently healthy trees directly adjacent to scorched earth: charred tree trunks standing like giant whiskers. The hillside won’t get shaved, but almost all those dead tree trunks will fall to the ground over the next several years.

It has been two years since the fire. Two summer growing seasons have passed. On my hike to Spruce Lake, the entire burn scar was carpeted with fireweed. Here, there were large areas where the ground is still black. I was surprised to find occasional piles of ash. I suspect they’re in dried puddles and the ash accumulated here. It’s bone dry now: disturb the frail crust and raise a bloom of ash.

On my hike to Spruce Lake, I noticed that the char on the trees is only a couple of millimeters thick, and it’s starting to flake off the dead wood. Here, I saw many interesting logs where the charred part has come off. The wood burned to different depths in random patterns, creating little topographic maps out of the tree rings.

As I said earlier, as we head west, the slope gets fairly steep for a while until we reach the bench that Marigold sits on. The forest isn’t burned here and is dense and there is much deadfall. It is a challenging route for about a third of a mile.

Dead trees burned, live ones didn’t
Tree Ring Topographic Map
Scorched Earth
Char and grain
Ash
Fern Lake from above
Marigold Lake
Marigold Lake and Little Matterhorn

Chad had taken a little tumble shortly after we left the trail and his ankle was a bit tender. Now he mentioned that he was no longer enjoying the dinner he had so enjoyed last night. Then he asked me how steep I thought this slope was. And he was huffing and puffing.

We found a spot with a couple of flat rocks and a nice view and took a break. He told me later how uncomfortable he was. I had been thoughtless. Almost everyone I hike with is quite happy to go places I’m not comfortable going, so somehow I had the idea that, if I was okay going there, anyone would be okay with it. I know exactly what it’s like to find myself in terrain that makes me uncomfortable. It’s stressful. I should have gone over the route with Chad beforehand.

If we’ve navigated correctly, we’ll exit the steep, dense forest onto the bottom of a talus gully, right next to Marigold Lake. We came out a little bit below the lake but found it soon enough. After the dense forest, I was expecting that this pond would have no view. The view of Little Matterhorn from here is quite nice. In my plans, we were to take a nice break here, but unfortunately, there’s no place to sit. So we pressed on.

From Marigold Lake back to the trail, we’d go up a gully gaining about two hundred feet of elevation, then cross a fair amount of talus until we reached the Fern Lake trail about two-thirds of the way from Odessa Lake to the summit of the pass near Lake Helene. Although it’s a rather large talus field, the rocks are small and easy to cross and there are occasional outcroppings of grass.

Did I mention it was breezy? To now, it hadn’t been an issue. Sure, it was windy, the trees swayed quite a bit. On the forest floor, it wasn’t windy enough to disturb ashes. Crossing the talus was another matter. The wind was howling down from Ptarmigan Point unobstructed. I’d guess sustained winds were twenty miles per hour with gusts over forty or fifty. Several times, I was nearly blown over.

On the way, I came across the oddest thing. I found a solar-powered light. The kind with a stake on the end, so you can drive it into your lawn. Who would bring such a thing to the middle of a talus field? And leave it there? I packed it out. How long could it have been out here? The stickers on it were still intact. It came from WalMart.

Back on the trail, we reach the top of the pass, where the trail returns to the trees and out of the wind and it’s all downhill from here. We stopped for a break on a couple of nice, flat rocks in the sun on the lee side of a slope above what as late as August would be a small pond but is now dry ground.

Today’s beer was a repeat: Palisade Peach.

When we got back to Bear Lake, the line for the shuttle was pretty long. After the first bus loaded, it looked like there was more than a busful of people still in line in front of us. Somehow, we managed to get sardined onto the second bus. We didn’t even stop at the Glacier Gorge trailhead on the way down.

Traffic was bad all the way from the Park to my house. We were back to the car pretty much on my expected schedule, but by the time Chad dropped me off at home, it was half an hour later than expected. Traffic sucks.

In Summary

I enjoyed my day. I can finally cross Marigold off the list (or, more accurately, put it on the list). Marigold Lake had a nicer view than I expected, but I don’t think I’ll ever bother to return.

The time exploring the burned area was particularly rewarding. It won’t be like this for very long. The ash and black will soon be gone, and grass and wildflowers will soon be here. And I hope this will be the last fire in the Park for an extended period.

I’m sorry that I led Chad into a situation that he didn’t enjoy.

Colorful Lake Haiyaha

Posted on September 14, 2022 by dhill

Back on June 28, a large rockfall event occurred on the south slope of Hallett Peak, halfway up Chaos Canyon. My college geology teacher probably would have called it a “mass wasting event”. Mass wasting is simply the movement of rock or soil downslope due to gravity. In RMNP over the last decade, we’ve seen a number of these but most were due to flooding. The water loosened things up and gravity took over. This one, though, was not like those others.

Mountains erode over time. Generally, we think of erosion as being due to water or wind. Very little of it is due to wind. Erosion due to the normal, continuous flow of water isn’t that great, either, mostly just making jagged rocks round. Mass wasting, whether it be landslides due to flooding or rockslides like what happened in Chaos Canyon in late June, is by far the largest contributor to erosion.

Due to the rockslide, the NPS closed off access to most of Chaos Canyon above the lake. Obviously, things are quite unstable there and it’s entirely possible that more slides are in store. This closure doesn’t really affect me, as I’m not a rock climber. I’ve only been a significant distance up the canyon from the lake once when Ed and I hiked to the small, unnamed tarn near the head of the canyon.

It’s not the slide, though, that interests me. I’m interested in the glacial flour. Also called glacial silt or rock flour, glacial flour is the sediment from ground-up rock particles produced during glacial erosion. This stuff is very finely ground. The particle sizes typically range from 2 microns to 65 microns. Particles that small will hang suspended in water for a long time. (A human hair is around 70 microns thick, while wheat flour is in the 10-41 micron range.)

This glacial flour is what gives the turquoise color to lakes that are fed by glaciers.

Clear water absorbs longer wavelengths of visible light (yellow, orange, and red) and strongly reflects shorter blue and blue-green wavelengths. Therefore, unless there is another pigment present near the surface of the water, like algae, it will always appear blue or blue-green. The glacial flour that floats in the water provides reflects light back to our eyes and makes the water appear both opaque and bright. Interestingly, the composition of glacial flour absorbs most of the blue light and reflects some blue and green, as well as yellow, orange, and red (but, as mentioned above, these colors are absorbed by water). With the elimination of the colors absorbed by both the glacial flour and the water itself, what is left is mostly green and some blue light reflected back off the glacial flour to our eyes: turquoise. The more glacial flour present in the waters, the greener the water will appear.

There is no glacier in Chaos Canyon; there hasn’t been one for a long time. But it turns out that a significant amount of rock flour is released in these rockslides. There was a smaller rockslide here back in 2018. The lake changed color for a few months, but to a much lesser degree than right now.

I can’t predict how long the lake will have this color. It is my guess, though, that the water will be clear again next spring. Lakes fed by active glaciers are always being fled flour, but I doubt snowmelt will pick up more flour from this rockfall and so I expect the lake to be clear again in the spring.

Then: If I want to see the lake decked out in turquoise, I better go now.

Tuesday, September 13

Lake Haiyaha is only a couple of miles from the Bear Lake parking lot, so it’s one of the shortest hikes I take. And, being so close to the parking lot, the place is always crowded.

I followed the masses up the trail to Nymph Lake and Dream Lake. It was a conga line. The flip-flops and no-water crowd was well represented. Nearly everyone was talking. Some hikers on their way back to Bear Lake gave words of encouragement to those going up: “You’re almost there!” It amuses me that everyone seems to think everyone else is going to the same place they’re going to. In this case, “You’re almost there” meant Dream Lake, 1.1 miles from the parking lot.

At the turnoff for Haiyaha, the crowd thins a bit. I had three or four minutes where I could see nobody ahead of me or behind me.

Just before reaching the lake’s outlet, I head west to reach the northern shore of the lake. The trail dumps the crowd onto the boulder-strewn southern shore. To get to my spot on the quieter shore, I have to navigate a bit of talus and dodge downed trees, but it’s worth it. Even though nobody is over here, you don’t really get any solitude: sound travels surprisingly well over water. You can not only see the people on the other side of the lake, you can sometimes make out what they’re saying.

Sitting on my rock, enjoying a snack, I concentrated on my nearer surroundings. The water is translucent for only maybe six inches. Any water deeper than that appears opaque. I was wondering what effect the glacial flour has on fish, but I did see trout rise a few times. They can still see insects on the surface because of the shadow, and they’re now pretty much invisible to predators, so unless the flour interferes with their gills, the fish are probably doing fine.

I wanted to make my way to the top of the ridge between here and Dream Lake. I’ve been up there twice, once in winter and once in spring. There’s a really nice view of Haiyaha from there. I never made it. I was too far west when I started and never got more than halfway. I spent about twenty minutes in the attempt before capitulating and heading to the crowded side of the lake.

The Slide Area
Chaos
North Shore pano
Hazy Longs Peak
South Shore pano
Milky Stream
Not-So-Turquois Pond

There’s a social trail that leaves the main trail just before the main trail starts crossing a rock pile. A few feet up the social trail, the Park Service has posted a sign showing the area of the canyon that’s closed. I worked around the south shore for a bit until I found a nice, flat, unoccupied boulder to sit and have my picnic lunch on.

Today’s beer: Great Divide Brewing Company’s American Lager.

On the way back, rather than return the way I came, past Dream and Nymph, I headed down the “back way” on the trail that goes to Glacier Gorge junction.

An interesting thing about Lake Haiyaha is that it has a leak. In winter, the lake drains to a level several feet below the level of the outlet. I’m not exactly sure where this leak comes out onto the ground, but this trail follows the stream formed by the leak for a short way, to where it fills a pond. The stream itself looks milky, and the pond is less green and more a milky, pale blue.

I’m happy I got to see the lake in this condition. The small rockslide in 2018 didn’t have nearly the same effect as this year’s big slide. Seeing the lake this color may be a once-in-a-lifetime thing. And, although I complain about the crowds, I think it’s great that so many people can enjoy the Park. Besides, it helps me appreciate my hikes where I get hours of solitude.

[See some of my older Lake Haiyaha photos here.]

Dutch Town 3

Posted on September 4, 2022 by dhill

Wednesday, August 31

We had a leisurely morning. As our hike out would only take three hours (or a bit less, perhaps), we weren’t in any particular hurry.

I told Gordon that it wasn’t a marmot that ate my stuff. He told me he was visited by a squirrel that was trying to get into his things. He managed to shoo it away. I wondered if I shooed it towards him, or he towards me, or both. Pesky squirrel. I really do hope it got a bad case of the runs.

When I was packing up, I noticed that he’d gone after my backpack, too. He ate the zipper pulls on two of the pockets and devoured about half the mesh. Surely this is a sign of malice rather than a desire for salt. I really don’t sweat all over the zipper pulls.

Squirrel Damage Assessment

I’ve been saying for years that, for every situation, there’s either a Star Trek quote or a Monty Python quote that is apt. I’m tempted here to use “That rabbit’s dynamite!” from the Holy Grail and substitute “squirrel” for “rabbit”. Instead, I’ll go back to World War II and BDA: Bomb Damage Assessment. While my antagonist squirrel may be as vicious as Monty Python’s Rabbit of Caerbannog, it never tried to decapitate me, even though it was well within range. In the aftermath of our encounter, I am left to assess the damage.

Tasty Poles?
Delicious Day Pack?
Mmm, Mmm, Good Mesh!

The poles are the type that you twist to tighten to the proper length. I’ve never been happy with them and would have preferred to get the ones that use a cam. I guess this is an opportunity to upgrade. Meanwhile, I’ll see if I can find somebody to mend the packs.

The deeper question is: How do I prevent this from happening again (apart from never camping at Dutch Town)? My tent is too small to store all my belongings in it. I’d really rather not spray all my belongings with coyote piss or the like.

Miscellaneous Thoughts

There was at least one healthy doe that frequented the area around our camp. I spotted a doe five or six times. It may have been the same one every time, maybe there was more than one. She went by my tent that first night.

The air traffic was pretty annoying. Even in the wilderness, it’s everpresent. But here it was loud. They went right over us. I decided I should time them the night before. I noted the time of the next one: 7:09. Didn’t hear another plane for half an hour when a two-engine propellor plane went over. So at least they weren’t so bad at night. Then two came over at about 6 am that were really low, just to remind us they were still there.

Just as we left the Ditch, a pickup truck when by on the service road. Water Supply & Storage Company. Those guys have owned the Ditch since 1891. They operate a vast system of canals and reservoirs in the Poudre River valley.

Now that I know the route, I think it’s possible Lake of the Clouds is within my day hiking range. It would certainly be an easy hike with a single-night stay at Dutch Town. We were back to camp early enough we could have packed up and hiked out on Tuesday.

The mosquitoes were not nearly as bad as at Upper Ouzel Creek. I finally did apply some bug spray at one point, but I wouldn’t have been terribly upset had I forgotten to bring it.

We saw no other hikers until we got within a quarter mile of the Colorado River. I don’t doubt Foster’s word that that Lake of the Clouds is the most visited destination in the area. This indicates that, if you’re seeking solitude, the Never Summer Mountains are the place to go.

Dutch Town 2

Posted on September 3, 2022 by dhill

Tuesday, August 30

I awoke a bit after sunrise after a somewhat chilly night to clear blue skies. It looked to be another marvelous day in the Park.

The first thing I noticed was that my trek poles, which I had leaned up against a long, downed tree, had been knocked over. Maybe the deer (or whatever) that passed through last night knocked them over. On closer inspection, though, the grips of both poles had been munched on and the straps had been eaten completely. Did that passing deer eat my poles?

A few minutes later, we were greeted by a Park Service trail crew. They were here to make a few improvements to the campsite. The ranger in charge asked to see our permit while the crew stowed their shovels and axes not far from where Gordon and I put our bear canisters overnight.

Having established our right to be here, I started asking the ranger questions. How did you get here so early? “We drove along the Ditch from Poudre cabin, so we had a short hike.” What creature did this skull belong to? “I don’t know. Not an ungulate.” What do you suppose ate my trek poles? “Probably a marmot. They want the salt from your sweat.” Did this campsite use to be over there beyond the preservation area sign? “Yes. It was threatened by dead trees so we moved it here.”

Last evening I spent a fair amount of time trying to figure out what percentage of trees in the area have succumbed to pine beetles. After much study, it became clear to me that all the dead trees were the largest trees. I’d guess nine out of ten of the largest quartile or quintile of trees were dead but very few of the medium and small trees were. I couldn’t help but wonder if all beetle-kill was this way and I just never noticed it before, or if things were different in this area. So I asked the ranger.

While I was correct that these trees had been killed by beetles, they were from the spruce beetle, which is a cousin of the pine beetle. Spruce beetles go after the big trees first, those with trunk diameters greater than ten inches. The victims in this area have been dead for a while – none are brown, they’re all gray.

Before they worked on our campsite, they headed up to Lake of the Clouds. They said it would take them about an hour to get there from here, which is only a bit less than I’d guessed it might take us. They left and we finished our breakfasts and got ready for our hike.

I grabbed my day pack, which is the top part of my backpack. It has a compartment you unzip to reveal the shoulder straps for the day pack. I’d stored this in the atrium of my tent (the space between the tent and the rain cover). It sat all night about six inches from my head, where the rustling noises were last night. It turns out my marmot friend didn’t just dine on my trek poles but worked my day pack over pretty well. Each shoulder strap was half eaten through and much of the fabric at the top was thoroughly chewed up. I wasn’t hearing the breeze rustle my tent, I was hearing a rodent wrecking my stuff. I hope that marmot got a really bad case of diarrhea.

Luckily, it was still intact enough to get me through the day. I hoped. As long as I didn’t put too much weight in the pack.

Anyhow, lunch and water and GoPro in the mangled pack, using my now strapless and heavily gnawed trek poles, we headed up the trail to Lake of the Clouds.

The trail ends well before the lake, where it exits the forest and dumps the hiker on the shore of a sea of talus. To the south, to the north, and to the west, nothing but talus. I vaguely recall writing on this blog some time ago about a large amount of talus. Wherever that was, there is more talus here. (It isn’t only here – our campsite has a view of the north slope of Howard Mountain. It’s all talus. Except for some that looks like scree.)

The first thing I did, once we had the route to the lake in view, was to search for the work party. I found them, but not where I expected them to be. When I was here on my failed day-hike, I thought that if I hadn’t made my 45-minute wrong turn I’d have made it to the lake. I’m pretty sure I wouldn’t have made it because I surely wouldn’t have gone the correct way.

We worked our way across the talus between the end of the trail and the base of the slope we’d have to climb. That slope is talus. We worked our way up between a couple of growths of willow and over to a grassy ramp. Once on the ramp, the route of cairns was pretty easy to follow. There may be cairns in the talus we had to cross, but finding a cairn in a talus field is like finding a pile of rocks in a bigger pile of rocks.

The ramp is broken in the middle by another section of talus. Imagine that. Back on the ramp, following the cairns, we crossed the lake’s outlet stream and arrived atop the bench that holds the lake. It took us an hour and twenty minutes to get here from camp.

The slopes of Howard Mountain and Mount Cirrus rise steeply 1400′ above the lake. You guessed it: talus everywhere. The rocks these mountains are made of aren’t the giant granite slabs you see above Black Lake, for example. The rocks on Howard and Cirrus are fractured and full of cracks running in all directions. The freeze-thaw cycle undoubtedly keeps a significant amount of rock falling, endlessly adding to the piles of talus.

As is my wont, I chatted a bit with the members of the work crew. They were celebrating the end of the season (even though they’ll be working another month). The ranger in charge told me she has been doing this for eighteen years. She’s been just about everywhere in the Park but doesn’t visit very many summits. One of the guys will turn 30 in a couple of weeks. He decided that he’d take a dip in 30 lakes by then. Today he got his 23rd and he’s confident that he’ll get the remaining seven without too much difficulty. One day last week, he got six in one day: The Loch, Mills, Jewel, Black, Blue, and Green.

Gordon set off to circumnavigate the lake while I surveyed my surroundings. Looking out over the valley below, my metaphor likening the talus to a sea couldn’t be more apt. This sea of rock is arranged in what looks like storm-tossed waves. The troughs of the waves are lighter in color than the tops due to weathering.

I was surprised the lake was so green. Fluorescent green, nearly.

We stayed at the lake for a bit more than two hours. On the way down, we lost our chain of cairns a couple of times, forcing us to backtrack. And when we went looking for the terminus of the trail, we found we’d gone much too far to the north. Rather than backtracking across the talus, we worked our way back to the forest and followed a game trail back to the main trail.

Use the Grassy Ramp (photo from 2013)
Working our way up
A Cloud, Never Summer Peak, and Gordon
Lake of the Clouds
Lake of the Clouds
Lake of the Clouds
North Specimen, Specimen Mountian, South Specimen
A Sea of Talus
Campsite improvement: before
Campsite improvement: after
Today’s Beer

When we arrived at our campsite, the work crew had already left. They cut a long section out of the tree trunk I’d had my poles leaning on overnight. This expanded the area where one might want to pitch a tent. As I said earlier, I saw an axe and shovels. But they must have had a power saw and something to shred the tree trunk. To level the ground, they didn’t move any dirt around, they just spread a thick layer of shredded tree trunk. It looked like it might be comfy, but I wonder how well it’ll hold tent spikes and suspect it’ll retain a fair amount of water after a rain.

At ten minutes to four, I thought we were going to get a visitor. Pretty much wherever we sat at the campsite, we could see the main trail. I saw a lone hiker come up to the sign, look up at the campsite, then check his map. He had a full backpack – much more than he’d need for a day hike. My first thought was that maybe he had a permit for this site but showed up a day early. But after a short pause, he continued up the trail. If he was a day hiker, he was pretty late. As it takes more than an hour to reach the lake, he’d be looking at passing our site no sooner than 6 pm. We never did see him again, so my guess is he camped at Lake of the Clouds without a permit. I wonder how often that sort of thing happens.

When it came time to bed in for the night, I made sure to keep wearing my headlamp. If that pesky marmot made a return visit, I wanted to be able to scare him away without rummaging around for my light.

Sure enough, sometime around midnight, I heard a rustling noise. I turned the lamp on and found myself eyeball to beady little eyeball with… a squirrel! The little bastard was about four inches away from my face. The light didn’t scare him off – I had to hiss at him. We repeated this little ritual three or four more times before he finally gave up.

I take back all the bad things I was thinking about marmots.

Dutch Town 1

Posted on September 1, 2022 by dhill

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.

The Mighty Colorado River
At the Ditch
Mystery Skull
Today’s beer

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

Start	End	Distance (Miles)	Slope (Ft/Mile)	Elapsed Time	Miles per Hour
Trailhead	Red Mtn trail jct	0.5	12	:12	2.5
Red Mtn trail jct	Grand Ditch	2.8	425	1:33	1.8
Grand Ditch	Lake of the Clouds trail jct	1.9	-8	:40	2.9
Lake of the Clouds trail jct	Campsite	0.7	714	:30	1.4
Trailhead	Campsite	5.9	286	2:55	2.0

Distance and Slope are approximate

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