Wednesday, October 7, 2026

Foliage Season Bits and Pieces

 
 
Took a hike into the Greeley Ponds on 9/22, with foliage just getting started. This view looks up to the K2 Cliff and the west knob of Mt. Kancamagus from Upper Greeley Pond.





East Osceola from Upper Greeley Pond.






The cliff-faced NE spur of East Osceola.




The Kancamagus west knob from Lower Greeley Pond.



 
 
Lower Greeley Pond.




 
 
Looking into Mad River Notch from the south end of Lower Greeley Pond.




An old beaver dam at the south end of Lower Greeley Pond.




 
View from the SE corner of Lower Greeley Pond.





The Painted Cliff is seen to the left.





A ring of red maples around a ledge slab on a slide that fell off East Osceola in 1897, partly filling in Lower Greeley Pond. 



 
A profile of the K1 Cliff.




Red leaves and green water at Upper Greeley Pond. 

 

 

 

A few days later I hiked to Allen's Ledge on Hedgehog Mountain partly via bushwhack, enjoying this view of Mount Passaconaway from the top of an old gravel slide along Downes Brook. 





Looking up at Potash Mountain.
 





Junction with the short, steep side trail to Allen's Ledge.





Approaching the lower and more open perch at Allen' Ledge. Allen’s Ledge is named after Jack Allen, a hunter, trapper, guide and crusty character who frequented the Albany Intervale in the late 1800s and early 1900s. According to Charles Edward Beals, Jr., writing in  Passaconaway in the White Mountains, his classic 1916 history of the area, when someone asked Allen what the rocks up on the side of Hedgehog were, he replied, “Them are called Allen’s Ledge!” 



A wide view across the Albany Intervale to the Moat Range on the horizon.



 

Looking towards Mount Chocorua and Mount Paugus.




Looking north to the Nancy Range, Mount Tremont, Bartlett Haystack and part of Bear Mountain.




Foliage along the Franconia Notch bike path, north of the Gallen memorial.






At the Gallen Memorial Bridge.



Checking out the newly open mile-long relocation on Falling Waters Trail, moving the trail onto the slope north of Dry Brook, away from  the waterfalls and the slippery section where so many hikers have been injured over the years.  I had walked this a couple of times in 2025 but wanted to see it in its final form.




The first part of the relocation follows an old logging road at an easy grade. The grades are easy to moderate throughout the relocated section.





There are some beautifully crafted rock steps, though not nearly as many as on Old Bridle Path.




 
A spur route (0.4 mile long) can be used to reach Cloudland Falls, the highest and prettiest waterfall on Dry Brook.






A short sidecut section of new trail leads down and across the slope to link up with the old route. 




 
The spur route ends at the base of Cloudland Falls. The old trail is closed and heavily brushed in above and below the spur.





Cloudland Falls, framed by foliage. Back on the main trail, I continued up to the upper end of the relocation, which joins the old trail just below the last crossing of Dry Brook. On a drizzly day, the only other hiker I met on this usually busy trail was fellow Lincoln resident Tony Drapeau.





Late on a cloudy afternoon I returned for a third visit to a short new trail built by the Dartmouth Outing Club in the Baker River valley, near Moosilauke Ravine Lodge. The Hatch Brook Trail is now open, making possible an easy two-mile valley loop in combination with Asquam Ridge Trail and Gorge Brook Trail. 





The new trail passe through beautiful hardwood forest after it diverges from Asquam-Ridge Trail.



 
The first section follows an old logging road from the 1940s.




 
Long view into the forest.




Hobblebush color.




 

View from front of Ravine Lodge. 

 

 

 

 

On another cloudy afternoon, Beaver Pond in Kinsman Notch from the parking area at the north end.




 
View from meadow at south end of Beaver Pond, reached by side path off Beaver Brook Trail.




 
A rugged knob rises above the pond.




 

Closer look. 

 

 


 Rustic bridge over washout on Beaver Brook Trail.

 

 

 

First cascade on Beaver Brook Trail. 

 

 
 
Mount Liberty from Flume Visitor Center parking lot. 




Mount Flume from Flume Visitor Center parking lot.





Mount Flume from gazebo on Roaring River Nature Trail.




Artist's Bluff parking lot on a foliage weekday.




 

Eagle Cliff from Profile Lake. 

 

 

 

 

 

Friday, October 2, 2026

Return to a Slide in The Bowl

A trip into The Bowl - the spacious, wooded glacial cirque enclosed by Mount Whiteface, Mount Passaconaway and the Wonalancet Range - is always a special treat for this bushwhacker. There are big trees to admire in the old growth hardwood forest on its floor, and on its walls are several old slides to explore. On this trip I wanted to return to a slide I've been to several times in the past in different seasons. 

New signage at the Ferncroft parking lot.
 



Partly sunny skies were predicted, but mid-level clouds hung tough all day and I saw one peek of sun for about 30 seconds. In the classic Ferncroft view, Mount Whiteface was socked in and a cloud was kissing the top of Mount Wonalancet.



 
 
Across a field on Dicey's Mill Trail before entering the woods. Thanks to the landowners who allow hikers to access these trails.



 
 
Into the WMNF and the Sandwich Range Wilderness.




 
The Wonalancet Out Door Club (WODC) does an exceptional job maintaining its trails, as evidenced by the many solid rock waterbars on Dicey's Mill Trail.





Pleasant walking beyond the Tom Wiggin Trail junction as Dicey's Mill Trail enters the 1,500 acre Bowl Research Natural Area, which is drained by two branches of the Wonalancet River. Research indicates that the larger western valley, which is The Bowl proper, has never been logged. Note that camping and fires are not allowed in The Bowl RNA.

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Leaving the trail and crossing the east branch of Wonalancet River. This stream is sometimes called Passaconaway Brook.



 
 
Into The Bowl!





Some mildly thick whacking en route to a stand of large sugar maples.




 
There is an ample growth of hobblebush in places. 
 
 

 

 

 

 A fallen giant.

 




 
Wandering through a stand of large sugar maples. One of the outstanding features of The Bowl is the extensive stand of old-growth hardwood on its broad floor, a rarity in the White Mountains. (Most of the old-growth spruce and fir on the walls of the cirque were destroyed by hurricanes and other natural catastrophes.) The vegetation and ecology of the valley have been intensively studied over the years, and serve as a valuable reference to compare with the primarily second-growth forests of the region.





One of the largest trees in the stand. A new botanical survey of The Bowl is being conducted this year by ecologist Michael Whittemore of Rewild Ecological (www.rewildecological.com) in partnership with the WMNF and WODC. Citizen naturalists have been involved in this project, reporting their findings on iNaturalist. Michael has also authored a new book, Ecology of New Hampshire's 48 4,000-Foot Mountains: A Natural History Trail Guide to the White Mountains, which is due out November 1st. This book has a wealth of information on the natural history and ecology of the Whites, with specific information on each of the 48 4000-footers. Highly recommended! It will of course be available at the Mountain Wanderer.
 



 
A glance upward reveals the majesty of the hardwood forest on the floor of The Bowl. It's believed that some of these maples are up to 250 years old. The Bowl was saved from lumbering about 1915 through the efforts of Katherine Sleeper and other members of the Wonalancet Out Door Club. The land was then added to the White Mountain National Forest, and in 1931 much of the western valley was designated as a 510-acre Natural Area. In the 2006 Forest Plan, what is now called The Bowl Research Natural Area was expanded to over 1,500 acres.



 
 
Mossy islets adorn the mountain stream known as Wonalancet River.



 
 
Beauty in The Bowl.




 
Meandering up the western side of the valley.



 
 
This could be a contender for most humongous maple in The Bowl.
 


 
 
You could get a sore neck looking up.




 
 
One of a number of stony/rocky brookbeds that come down off the steep east side of Mount Whiteface. The challenge is to figure which ones lead up to a slide.





There are some big yellow birches in here, as well.




There must be a good view from up there.



 
From previous trips, I knew that this particular brookbed would lead me to the slide I wanted to visit.

 



Coming in from the side is the track of a more northern slide that I visited a few years ago.
 


 
 
Approaching the bottom of my target slide, where there is a field of rubble with low vegetation.




 
A long series of ledge slabs ends at this pool. The brookbed was mostly dry below, but had some flow here.





Side view.






A long series of sliding cascades. Too wet and slick to climb directly; I took to the woods on the side. 

 

 

 

To continue up, I had to carefully cross this slippery slab at the base of another slide track coming in from the side. 

 

 

 

 

Looking up that slide track. These slides on the flank of Whiteface are old, and only certain sections remain as open ledge slabs.

 

 

 



Approaching the massive footwall that is the most impressive feature of this slide.






Getting closer.




Fully revealed! This is transformed into a massive ice cliff in winter.




 An overhang adorns the north side of the footwall.

 





Wide angle of the footwall.





I climbed a very steep wooded slope and scooted over for a look at a narrow slide that runs parallel to the north.



 
 
Continuing up through steep woods.





Encountering a ledge wall. On a November trip a few years ago I found a way up through here, but on this day I backed off from a spot that was just a little too sketchy.
 


 
 
I cut across to the edge of the main slide above the footwall and had glimpses of its ledge steps and cascades above.






Interesting pattern on this ledge.
 
 

 

 

I fashioned a careful route to the top edge of the footwall for a peek at Hibbard Mountain across the valley. 




 
Zoomed. 
 
 
 
 
 
 
 
 
Down-look.
 




Parting shot from the base of the footwall. Is that blue sky up there?

 

 

 

Random boulder, probably deposited by the slide. 




Big rocks in the slide track.
 


 
 
One of a number of "seeps" on the floor of The Bowl. These wet areas may be home to unusual plants and bushwhackers should avoid walking through them. Mindful walking - such as avoiding obviously fragile areas - can minimize impact when traveling off trail.





Homeward bound on Dicey's Mill Trail. 







At dusk, Whiteface has broken free from its gray shroud.