Monday, May 5, 2014

2014-05-03 Balsam and Eagle Mountains, a 17th/18th century robber baron, and wildflowers

On Saturday, May 3, 2014, I took a hike to visit another couple of the Catskill 3500-foot summits, Balsam and Eagle Mountains. I visited Mount Haynes (3425 feet) twice as well, traversing it once southbound and once northbound, because it was in the way.

The road to the trailhead is fairly remote, winding up a narrow valley in the middle of the Catskills. A somewhat surprising sight on the road is a garage and prefab building with a sign out front reading, "Hardenbergh Town Hall."

Hardenbergh (population 215 at the last census) is a very odd township right in the middle of the hills. While it is in Ulster County, it is completely cut off from the rest of the county by a line of mountains that includes several of the Catskill 3500 peaks, and hiking trails provide the only routes that connect it. It's also cut off from itself: the northern part of the town is accessible by highway only from Delaware County, while the southern part is accessible only from Sullivan County. The Dry Brook Ridge separates the two. (Incidentally, the Dry Brook is anything but dry: apparently the name is a corruption of a Dutch phrase meaning "third brook" (off the East Branch of the Delaware). The first two are the Beaver Kill and Mill Brook. Of course, there are many smaller streams feeding the East Branch among these three large ones.

Hardenbergh is the last vestige of a mighty kingdom that belonged to one Johannes Hardenbergh (1670-1745) and seven of his cronies. Hardenbergh claimed title to some two million acres (3100 square miles, 8100 square kilometres) - a parcel spanning the area from Stamford, Great Gorge and Palenville in the north to Wurtsboro and Narrowsburg in the south. This enclosed the whole of the modern Catskill Park (indeed, was over six times its area), and spanned the whole of the Catskills from the West Branch of the Delaware to the Great Wall of Manitou. The metes and bounds of the land deeds in that part of the world to this day often bear reference to one or another of the 'Great Lots' into which the Hardenbergh patent was subdivided.

Suffice it to say that old Hardenbergh was something of a swindler. He was allegedly a major in the British army, having enlisted in the Ulster County Regiment in 1690, and knighted by Queen Anne for valiant service under the Duke of Marlborough in the Battle of Blenheim. (Blenheim, New York, near the northernmost extent of his great land patent, is another vestige of his memory.) All this was a great lie: contemporary records from both Ulster County and the Dutch Reformed church in Kingston (New York, not Jamaica!) show him to have been a prosperous businessman, who was in Ulster County - and nowhere near Blenheim - in 1704. None of this kept him from adopting the title, 'Sir,' and thereafter signing papers with only his surname: "HARDENBERGH."

His land grab seems to have been another swindle of the same nature. He negotiated title to the entire tract for £60 in 1707 from "Nanisinos, a sachem of the Esopus Indians." Not only was the legality of the deed questionable, so also were the metes and bounds. In particular, the land between the two branches of the Delaware was part of the Oneida Nation, and no Esopus would have the right to sell it. Nevertheless, the grant was confirmed by the governor, and survived a courtroom challenge in 1769 (in which another former British officer, John Bradstreet, claimed title to 50,000 acres or so of it).

The patent was divided and subdivided, and title to parcels of it passed among heirs of the original patentees and others so many times, with terms of sale that were complex even by the Byzantine standards of 18th-century British land title, that the ownership of the land remained clouded for generations. At times, the courtroom battles even spilled over into actual bloodshed. Even as recently as 1845, a tenant's association entered into a gun battle with a 167-man sheriff's posse over non-payment of rent, ending with one deputy lying dead and 90 men indicted for his murder. Somehow, in the present day, these battles are but a dim memory. The parcels have been divided and subdivided again, the great landlords (who never gained much profit from their lands) have sold their holdings, and the land wars are a dim memory, left engraved in the names on the land.

There's much more in a 1910 issue of Olde Ulster that's available on the Internet Archive, and at the Web site of the Hardenbergh family.

Map of the hike

OK, enough with the digression on how the nearly-depopulated Town of Hardenbergh came to be, and onto the hike itself. The trailhead is at the end of the maintained section of Rider Hollow Road, which is an old turnpike that served tanners and quarrymen back to the 18th Century and the days of Hardenbergh. The modern road ends abruptly at the boundary of State land (the Big Indian Wilderness; the story of Winnisook, the Big Indian, will wait for another hike).

Rider Hollow trailhead

I signed in there and started in on the old road, now part of the Oliverea-Mapledale trail. Near the trailhead, the trail maintainers have replaced a bridge that washed out in Hurricane Irene with a handsome and sturdy new one, wide enough for two hikers easily to pass abreast.

New bridge

Not far from this bridge, there is a trail relocation that hikers should be aware of. Right near where the Rider Hollow and Mine Hollow brooks converge, between the trailhead and the shelter, the hurricanes damaged a section of the road beyond repair. The trail has been relocated up the hill on the north side of the brooks. Coming in from the road, the Oliverea-Mapledale trail leaves the road (which has been blocked by a pile of brush, but this early in the spring it's hard to tell a brushpile from blowdown) and proceeds up the hill to the left. Be alert for the red double blaze marking the turnoff.

Rider Hollow Road.

The junction between the Oliverea-Mapledale and Mine Hollow trails is up on this relocated section. The old signpost has been moved up there, and is quite prominent. (I have no picture, because, like a fool, I had left my smartphone in my truck. I reached into my pocket at this point to pull it out and mark a GPS waypoint for the trail junction and realized I'd left it behind. By the time I'd hiked the 0.3 miles back, retrieved the phone, and hiked back in again, I was too flustered to remember to take a picture of the junction. Sorry.)

Coming back down from the Mine Hollow trail, again, there's a brushpile on the old road. There's no double blaze, but the yellow-blazed trail fairly clearly departs up and to the right. The next blaze is visible in the picture. Stay alert here!

Trail leaves Mine Hollow road

Finally, coming out from the lean-to, just after the steel bridge, there's a wooden billet with a blaze warning of a right turn.

Warning blaze

The trail goes straight up the hill as the road bends left (with another small brushpile on it). This is probably the easiest place to go astray in the relocation.

Trail relocation

Of course, I came upon these at different times during the day, but I thought I'd get that whole business out of the way and get on with the meandering story of the trip.

Perhaps the thing I noticed most, as I was panting up the climb of the Mine Hollow and Pine Hill-West Branch trails toward the summit of Balsam Mountain, was that the forest floor was a riot of colour. Just as the desert blooms briefly after the rains, so the forest floor blooms after the snowmelt - and for much the same reason. The wildflowers have at most a few weeks to gather the Sun's rays and try to reproduce before they will be in deep shade under the forest canopy. They all bloom during this brief period. All are hardy perennials - the winters here are intense, and this brief growing season is far too short to support annuals. By Memorial Day, they'll already have gone to seed. But for this brief period, they work magic. In addition to the Viola lanceolata that I saw last week, I notice Spring Beauties (Claytonia virginica),

Spring Beauties

yellow violets (What a contradiction the vulgar name appears to be! Viola pubescens is considerably more pedestrian.):

Yellow violet

Trillium erectum:

Trillium

and trout-lilies (Erythronium americanum):

Trout lilies

None of the trilliums is yet in bloom. It's a pity; I haven't seen them in years, because I always seem to miss their short season. (This year may prove no exception: I'm busy for the next few weekends.) In this part of the world, some of the old folk still call this flower Wake Robin when it appears in its red color morph. (It has several, ranging from deep purple to clear white.) Apparently, the red blossoms reminded the locals of Robin Red-breast, who is arriving from his southern range just as they are in bloom. John Burroughs was so enamoured of this flower that he chose the title, "Wake Robin" for one of his collections of nature essays.

The trail also makes its way through a few stands of ancient hemlocks, which have somehow come to what must be an age of 300-400 years while escaping the attention of the tanners. This felicitous situation has likely come about simply because the slope is so steep and the valley so remote that it wasn't profitable to fell them and haul out the bark. Nevertheless, I'm pleased that they are left for 21st-century humans to enjoy, and even more pleased that I could spot no sign of the Wooly Adelgid (Adelges tsugae) anywhere in these groves.

Hemlocks!

It seems ironic that this majestic tree, by far the largest of the Eastern woodlands, has the smallest cone of all. It's often little bigger than a dime. A great many of them crunched underfoot as I moved up the trail.

Hemlock cones

With all this beauty to inspire me, I made quick time up the north side of Balsam Mountain. Well, quick time for me, anyway: I'm not the fastest of hikers. Ordinarily, I'd budget two and a half hours for the 2.8-mile, 1600-foot ascent, but today I made it in under two. I knew I was in the home stretch when my nose caught a trace of the sweet perfume of balsam. Sure enough, in a moment or two, I sighted my first fir tree of the journey. A few steps further on, the 3500-foot marker greeted me:

Balsam Mountain 3500 foot marker

Just beyond, there's a short rock scramble. There's always one just around the marker. (There are actually geological reasons for this, but I'll save that for another post.)

3500 foot scramble

And the scramble is the gateway to another world. In just that short space, the Eastern mixed woodland comes to an end and the mysterious glades of the boreal forest beckon.

Balsam Mountain summit ridge

The duff and flowers carpeting the forest floor are gone, replaced with mossy rock (which later in the season will have a morass of pricker bushes and nettles; early Spring is a good time to travel these mountains!). The balsam fragrance is heady. A gradual incline leads to the mountain's northern (false) summit, only a few feet lower than the true one.

False summit of Balsam Mountain

The walk between the two summits is a pleasant easy ridge walk, at the midpoint of which the trees open out into a breathtaking view:

Balsam Mountain view

I'm able to identify no fewer than nineteen of the Catskill high peaks: Slide (I have to lean out a bit to spot it to the right), Panther, Kaaterskill High Peak, Indian Head, Twin, Sugarloaf, Plateau, Hunter, Leavitt, West Kill, North Dome, Sherrill, Halcott, Bearpen, Vly, Blackhead, Black Dome, Thomas Cole and Windham High Peak are all visible. (It's easier to identify them now that my boots have trodden over half the ones I can see!) Even far-off Mount GreylockFrissell in Massachusetts is visible through a gap in the skyline.

The camera obstinately refused to see well enough through the rain, but with my eyes I could spot the network of old logging roads on one of the nearer ridges: branching roads following contour lines, all joining with a central incline that probably had a cableway when the logging companies were operating. I'd never seen such a pattern that clearly before. It's most likely visible only in the brief period when the snow is off the ground but the leaves are not yet on the trees.

At the overlook, I was overtaken by a group of five hikers, one of whom was making the final ascent for his Catskill 3500 Club membership. I congratulated him, and we all sat down to lunch - not by any agreement, it's simply a lovely lunch spot and I was getting ready to eat just as they arrived. Similarly, we all packed up again and left at the same time and headed south together - not hiking together, just moving in the same direction at about the same speed. This togetherness meant that I was able to ask to have my picture taken at the cairn near the true summit, and of course return the favor for the others. Here, the photographer was standing on the summit rock looking a couple of feet down at me.

Balsam Mountain summit

We made our way down to the col - with the other group moving faster. (Of course: everyone's faster than me!) I overtook them, and met another solo hiker who was just returning from Eagle, my next destination, at the trail junction in the col. We took our leave, with a final round of congratulations for the new 35er and encouragement for me and the other soloist (who was completing what for him were ascents 32 and 33), and I headed on south up the ridge to Mount Haynes. I climbed to this 3425-foot summit twice this day, for no better reason than that it was in the way. But once I'd done the work of getting up on the ridge, I wanted to bag Eagle - even with Haynes in the way, two-thirds of the work is already done. Of course, a few rock scrambles remain, but nothing too difficult nor too exposed.

Rock scramble

At one of them, I clearly saw blazes leading right up the the face of the rock, but no path left or right, and no blaze visible above. I paused a moment in confusion, but then noticed, right in front of my nose:

Crampon marks

Who needs trail markers when you have crampon scratches pointing the way?

The trail has taken a bit of a beating in the winter. Most of the blowdown has already been brushed out: quite promptly, since the ice has only been gone up here for a week or so. A couple of big things are awaiting a trail crew with axes and saws. In once spot, the crown of a dead tree has broken off about 30 feet above the ground, and fortunately fallen away from the trail. I saw immediately what killed the tree. The spiral lightning scar makes an interesting sculpture.

Lightning scar

In another spot, the wind has uprooted a big beech tree and laid its crown directly in the middle of the trail. While it appears that some other hikers had pushed through it, I took the lazy man's approach and whacked over to the left far enough that I could step over the trunk.

Blowdown

The trail drops down off Mount Haynes, and then makes its ascent onto Eagle Mountain. Once again, I'm enjoying the balsam forest, although Eagle's mostly seems composed of very straggly grey birch, which, alone among the deciduous trees, sometimes survives the harsh conditions in the boreal zone. When the trail stops ascending, a well-beaten herd path (marked with a bit of flagging tape when I was up there) heads off to the west about 75 yards to a pair of cairns marking the true summit. It's viewless, and apart from checking a box on my tally sheet is nothing to write home about. Nevertheless, I set up the tripod for a selfie ("Hello, world!\n")

Eagle summit

and laid my watch atop one of the cairns so that the altimeter was visible:

Eagle Mountain summit

After that, there was no reason to stick around, so I turned back the way I came, climb Haynes (I've now been up there four times, and its viewless summit has very little to recommend it; it's a nice enough walk in the woods, but hardly worth the work of climbing up there!), and got back to the col between Haynes and Balsam. There I turned west and started the remaining descent (it was still 1.8 miles, with 1200 feet elevation loss) back to my car.

Just off the col, there's a rock face with a substantial seep leading to a bog full of skanky water. I don't recommend that as a water source even treated, because not too much farther down the trail, there's a spring right on the trail. Water is bubbling out of cracks in a largish area of rock at quite a brisk pace. I understand that it generally has some flow even in high summer. It's the headwaters for the brook in Rider Hollow, and it continues to pour noisily down beside the trail for the rest of the hike.

Spring near the Balsam-Haynes col

It would be more accurate in spots to say that the stream pours noisily in the trail. As I've observed many times, the difference between a trail and a stream is that the trail ordinarily has more bootprints and the stream generally has more trout, but this is far from guaranteed.

Sometimes, the trail just is a stream

And I don't necessarily just mean a muddy spot, or a trickle of water.

First stream crossing

This early in the spring, water was high everywhere. Even apart from the occasional cascade in the trail, there are four substantial stream crossings, all of which had their stepping stones completely awash. For the first three, I was able with little trouble to find alternative rock hops, even with my poor balance.

Stream crossing

After that, the trail picked up the old turnpike and mellowed out for a while. It went by another few old-growth hemlocks:

Hemlocks

These may have been saved because they were in someone's front yard. I noticed old stone walls and foundations quite nearby.

Old stone walls

Old stone piles

Down near the Rider Hollow shelter, there's a final stream crossing, and that one offered no obvious rock hop. There was nothing for it but to wade across. Given that it was just half a mile of fairly level trail to my car, I decided not to trouble changing into water shoes, and just plooshed through. Even clunky leather boots with a Gore-Tex membrane and high gaiters do nothing to keep your socks dry when the water is over your boot tops.

Rider Hollow shelter

Then the Rider Hollow shelter was in sight, I checked it out. It's a trail shelter. I'd much rather tent. I inspected the privy (I rather felt the need to conduct an inspection tour). I checked out what I thought was a log book. It wasn't. It was a catalog from an axe manufacturer, with several pages torn out. I think it was in the shelter as fire starter. I tucked it back farther under the overhang in hopes of keeping it dry for the next hiker, sanitized my hands again, had a quick snack, and continued on out.

Just past the shelter, the trail recrosses the stream on a steel kingpost bridge. The bridge looks impressive from far off.

Steel kingpost bridge by the Rider Hollow shelter

But once you're on it, you realize that it's a bridge in miniature. The decking is just three 2×6's, and I had to duck my head under the top tie while my shoulders brushed against the king posts on either side. Still, it was nice not to have to deal with the water underneath, since here the channel between the banks is narrow and it was running at least knee deep.

Steel kingpost bridge by the Rider Hollow shelter

From there, it was up and around the trail relocation and a quick level walk back to the car.

All in all, a fun hike. 10 miles (counting the little jaunt to retrieve the smartphone) and 5200 feet of elevation change in about 7.5 hours. I'm slow, but that's still about guidebook time. Most guidebook authors go by "30 minutes per mile or 1000 feet of elevation change." Normally, at my pace, I'd have budgeted at least an hour longer, and that's without counting all the time I spent on compulsive photography.
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Sunday, April 27, 2014

Saturday walk, 2014-04-26, Huntersfield Mountain, Prattsville, NY

I took a walk on Saturday to Huntersfield Mountain, in Prattsville, NY, with a side trip to Ashland Pinnacle? Where in the world are these places? Google Maps offers directions to the trailhead. Once you're there, you can follow along with me on my own map, with my GPS track overlaid. As always, you can click through to embiggen.

Map of the hike

The trailhead is an old gravel pit at the pass where Huntersfield Road turns into Jim Cleveland Road. Note that within the state forest boundary, neither road receives maintenance from the highway department. They are impassable to vehicles in winter, and 4WD is recommended during bad weather at other times of the year. The trail climbs rapidly upward from the right-hand side of the pit. When I was there, I found the place quite a pigsty. Apparently, some irresponsible shooters had been firing at improvised targets. I found spray cans, Chinese food containers, ammunition boxes, beer cans and similar rubbish, all shot up. And I must have picked up two hundred spent 12-gauge shells.

 Trailhead

Right above the pit are some old foundations, probably workings for the pit.

 Old foundations above the gravel pit

The trail continues up the mountain on a broad woods road. The trees surrounding are in bad shape. Many of them were split and blasted in the hurricanes of the last few years, and there is a lot of standing dead timber and deadfall.

 Woods road

The dead trees are home to many polypore fungi. With the highly inflammable pith of these, and all the dead wood about, I wouldn't want for fuel for a fire if I needed one. Even in a pounding rainstorm, I'd be able to get one going readily.

 Tinder fungus

The woods echo with the hammering of pileated woodpeckers. The dead wood makes ideal homes for the birds, and the termites are a major food source for them. Many trees have large excavations and corresponding large piles of sawdust at the base.

 Woodpeckers have been here

Near the summit, the trail joins with the loop trail serving the Huntersfield lean-to. The yellow markers for the loop appear.

 Trail marker

At this elevation, the frost is still in the ground, and the water cannot percolate. The trail surface is punctuated with mudholes. I was glad I wore clunky leather boots and high gaiters!

 Soggy trail

As the trail levels off on the flat summit, the lean-to appears. Uh-oh, it appears that someone's left the register box open.

 Huntersfield Mountain Lean-To

The register has been gnawed a bit by rodents, but it's still legible. I note the name of one of my sometimes hiking partners, who's been up there two weeks earlier. At that point, he was still on snowshoes. It's amazing the difference that two weeks can make. I appear to have the forest to myself on this day of threatening weather. I sign in. Since I'm feeling good, I decide to explore the former route of the New York Long Path over to Ashland Pinnacle, and indicate my intention in the book. The Long Path no longer follows this route, because a disgruntled landowner has canceled a trail easement farther down, and now has several miles of roadwalk just to avoid his parcel. Hikers, please make doubly sure to follow Leave No Trace principles in the places where a trail crosses private land!

 Trail register

The trees have been cut away from the front of the lean-to, offering a view of the Catskill high peaks. I enjoy this lovely spot while I sit down to eat my lunch.

 View from Huntersfield lean-to

After lunch, I encounter the trail junction just east of the shelter, and set off on the old Long Path route. The trail is now blazed with red DEC markers as a spur trail, but the aqua blazes of the Long Path are still quite apparent.


Aqua blazes

I keep darting my eyes to the ground in hopes of spotting the Mourning Cloak and Grey Comma butterflies, which a friend has reported are already out. Alas, I don't see any butterflies all day. A flash of orange in the treadway turns out to be someone's dropped safety whistle. I pick it up, both in the interest of keeping the place clean and because the whistle, cleaned up, will probably be of use to someone.

 Safety whistle

This section of trail is well blazed, but is so little traveled that it often feels like a bushwhack, particularly since I'm the only hiker up here. There is a considerable amount of blowdown - I brush out as best I can, but I have to leave a few heavy trees for the maintainers. And there's lots of light growth right in the treadway. In the summer, this section must be a hell of prickers and nettles. It's also quite muddy. In fact, I spot some Viola lanceolata growing right underfoot in the treadway. Since this species is an obligate wetland dweller, this particular spot of trail must be muddy year round! (There's probably a seep or spring just above.)

 Viola lanceolata

A mile or so down the trail, I spot a DEC marker disc, hung backward with the print facing the tree, and "VIEW" scratched on its back side. To the side, I spot an abandoned woods road that it seems to be indicating. Despite the fact that the road is all grown to prickers and beech saplings, it's not at all hard for an experienced eye to see the ruts leading off to the south. Never one to pass over a nice view, I head off down the road in search of the promised view. After maybe two hundred yards, I turn around. The road is clearly dropping in elevation into the valley of a creek, and it suddenly occurs to me that I'm straying off a trail easement on private land. Oops. I head back to the trail, having seen no view any better than what the trail offers. (A troll of Google and Bing satellite imagery suggests that there's none to be had.)

Farther along, there is a nice view, at least this early in the spring when the leaves are still off the trees. Looking out through the trees, I can see the Blackhead range, Ski Windham, and the Devil's Path.

 From the former Long Path.

The last vestiges of the snow still cling to the ski runs.


Ski runs

The trail crosses a patchwork of state, private, and New York City watershed land. I'm glad I've brought my New York City watershed access permit.

 he old Long Path goes just north of the Ashland Pinnacle summit, so I hope for a view from there as well. But the summit itself is on private land. There's a private trail that goes over there, but I respect the posters. The private trail is considerably better maintained than the public one. I suspect the landowner is an ATV rider or snowmobiler.

Private trail

Just then, a sudden cloudburst makes me adjust clothing. The temperature takes a rapid dip. (The ideal combination for the rest of the hike turns out to be rainsuit and underwear, with no midlayer.) I turn around and head back for Huntersfield, noticing some views of the Schoharie valley to the northwest that I hadn't seen on the trip out, largely because they were behind me. Between the rain and mist, and the trees in the foreground, they're not very photogenic, and I didn't get any usable shots to show you. But I was able to spot the Schoharie Reservoir gleaming in the distance, and the upper pond of the Mine Kill pumped storage facility.

At the top of Huntersfield, I turned right this time, and continued down the former Long Path down a slope of shale and scree, made squishy and slippery by the rain, which by now was starting to turn to sleet. The occasional fallen rock slab or overhanging ledge gave me a reminder that even though I was at the far northern end, this is still a Catskill trail.

At the bottom, the old Long Path route reaches one of the private land closures, and the trail, now carrying only the red DEC disks, continues its descent until it reaches another broad woods road, this one serving the plantations of the state reforestation area. (The whole mountain, once upon a time, was clearcut.) The road is broad and flat, but often underwater - this is mud season, after all. The rain falling on top, the reflected trees and clouds, and the vegetation and red sandstone make an interesting composition.

Wet woods road

Along the road are many stone walls and foundations, evidence of former habitation.


Old walls Old walls

The plantations that the road traverses have an unnatural (although not entirely unpleasant) feel to them. They consist of stands of trees, all the same species and age, growing in orderly rows. I notice at least pitch pines, white pines, red spruces, and hemlocks. A healthy understory is starting to grow up, and sooner or later Nature will restore some semblance of biodiversity, but recovery will take a very long time. In the defence of the foresters, at the time the trees were planted, the goal was rather to recover the economic value of the land by planting useful timber, and the homogeneous stands would make a subsequent harvest easier - another clearcut, years down the road. It was surely better than the previous generation's practice of merely leaving the land bare, with slash strewn everywhere, which led to horrific wildfires.

Old woods road

The woods road takes me down to the Huntersfield Brook, where I pick up the road I drove in on and walk up it the rest of the way to my car. It's a steep slog, as roadwalks go, about 400 feet of elevation gained over a half mile or so.

Getting back to the car, I grabbed my trash bag and brave the wind and sleet to pick up the trash, because I promised myself I'd leave the trailhead less of a mess than I found it. I called Mary Ann and apologized for the late departure - I'm going to be home about an hour and a half later than expected - and headed off down the hill. By the time I was down into Prattsville, the weather was rain showers and temperatures in the high 40's Fahrenheit - a major change from the mid-30's and sleet up above. Mountains make their own weather.

All in all, not a bad day. About an eight-and-a-half mile hike with 1900 feet of elevation gained and lost (about 1000 feet of elevation change between the summit of Huntersfield and the crossing of Huntersfield Brook). At my usual pace, I'd apply my personal Naismith Rule guidelines of 30 minutes to the mile, 40 minutes per 1000 feet of elevation, and arrive at roughly 4:15 for the distance and 2:40 for the climb and descent, for a total of 6:55. As it was, I did the loop in 6:05 with a twenty-minute break for lunch. I'm a slow hiker, but that's not too bad for having sat on my arse all winter, having shifted a fair amount of fallen brush out of the trail as I went, and getting slowed down a bit on wet shale.
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Sunday, March 30, 2014

Saturday walk, Holt preserve, Clarksville, NY 2014-03-29

I took a walk yesterday on Copeland Hill in Clarksville, NY.

I was mostly trying to relieve a bad case of cabin fever, but also brought along my smartphone, so that I could grab GPS tracks and put up the trail network on Open Street Map. This will eventually let me update my topographic map set for southeastern New York - but I only make a new set once every few months, because that's quite laborious.

This was probably the first weekend since winter began in earnest that the road into the upper trailhead was drivable. It is unmaintained in winter. With the spring thaw part way along, it's still a morass of ice and mud, passable only to a 4WD.



There was one dry parking space in the lot. Of course I grabbed it.


The trail register showed one other visitor on Saturday, plus one earlier in the week. The other visitor had apparently already come and gone. I saw no sign of him or his car. I had the place to myself all day.


The entrance offers the choice of an overlook or a pond.


I chose to visit the pond first, getting the panorama at the top of the post. A pretty place, isn't it? I walked around the pond, then followed the other red-blazed spur trail down to the blue trail from the entrance - so as to have the GPS log. The outlet of the pond was unfrozen, and babbling away merrily.


As I was turning around, I fumbled my notebook into the slush. Fortunately, it was back in its Ziploc, so no harm done. I picked it up again, and finished my walk around the pond. On the north side of the pond, the conservancy volunteers have placed a park bench for bird-watchers. It looks out across the pond, screened by the natural cover of a couple of spruces.


I stopped off there for a water break, and decided to enter the location of the bench as a GPS waypoint. I reached into my pocket for the smartphone. "Oh, my God, where's the phone?" Checked all the rest of my many pockets, to no avail. "It probably fell when I dropped the notebook." Walked back down there and had a look around. Nothing. Walked clear around the pond and the length of both the little spur trails, back to the entrance, with eyes on the ground. Nope. "Maybe I left it in the register box? I was there when I started the track recording." No such luck.

Facepalm!
Glumly, I headed back to my Explorer. If I was going to have to deal with bureaucrats over handset insurance, the walking was over for the day. I opened the tailgate, sat down, pulled off my Microspikes, opened my pack to put them away again, and... there's the phone. The phone doesn't go in my pack. I never put it in there. What the heck did I put it in there for?

Oh, well. I put the spikes back on, and headed back in, determined to try to enjoy the day now that that particular piece of idiocy was taken care of.

[Post hoc: I went and added the graphic after writing and saving this entire report. Something happened on my computer (it's got one of those buttonless touch-pads that always seem to act squirrely when I'm around), and the entire post got selected, and deleted, and 'undo' brought back only a single space character. So just as the 'facepalm' got put it, it brought about another one.]

Anyway, back to the walk. The preserve is an artificially reforested area, which has now grown to a mature but highly abnormal woodland. The trails traverse plantations, each of which has trees of a single species and a single age. While a healthy understory is starting to develop, the lack of diversity in canopy species is striking. I walked through stands of several species of pine (white pine, yellow pine, Scotch pine),

of spruce (at least red spruce and Norway spruce appeared),

of hemlock, and of tamarack.

The trail suffered somewhat from the 'monorail effect.' The tramp of snowshoes compacts the snow, and fresh snow blows into the trail. After several rounds of this, the trail is solid ice while the ground around it is soft snow. When the thaw comes, the snow melts faster than the ice, leaving a rail of ice where the trail is, and sometimes bare ground on either side.

(That ice is thicker than it looks: there's quite an accumulation of duff on top of it.) In spots, I could even see the prints of individual snowshoes, now sticking up in relief out of the ice.


I walked around the loops on the north side of the preserve. At the north end, they offer limited views to the north off the Helderberg escarpment. I would imagine that in summer, with the leaves on the trees, the views would be a disappointment, but in winter they're pretty.


After doing those loops, I returned to the entrance by the yellow trail. It is on a south-facing slope, and the snow is mostly gone from it. I was easily able to spot the stone walls and foundations of a long-abandoned farmstead.


The well of the farm is securely capped, so that it does not present a pitfall for the unwary visitor. Those who venture off trail in this part of the world need to be careful; there were several periods of boom and bust in local industries, and hence there is much abandoned settlement. Old wells, open mineshafts, and cellars of ruined buildings occasionally lie in wait.


Once I got back to the entrance, I walked down the road (impassable to motor vehicles, but a nice walk) to the lower entrance, and in on the white access trail, which I had missed when going by. There was a bridge out of place on the white trail, apparently by design, since it was secured to two trees with steel cables. It was fetched up on a gravel bar, with the main part of a stream flowing on one side and a small rivulet welling up from a seep on the other.


The stream, even bridgeless, was no major obstacle. It was easy to find a place so narrow that one long stride would clear it.


In fact, the road itself posed a much greater risk of wet feet. It was about six inches deep in ice, with water trickling over it, sometimes across the entire width.

Nevertheless, Microspikes were entirely up to the challenge, even on the 10-15% grade, and getting up was no more difficult than getting down.

I got back to the Ford just as it started to rain. I stopped to snag a few pictures of the more recently ruined farm right where the pavement ends.




The road out from the trailhead offered the best view of the day, a sweeping vista across the Hudson Valley with the mountains of Massachusetts and Vermont dimly visible through the rain and haze.


I drove home, took my wife out to a nice birthday dinner, and deferred writing about the trip until today.

All in all, a fun outing.

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