Saturday, January 17, 2026

Greeley Ponds & East Osceola Slide

It took me a long time to get going on this bitterly cold, windy day, but I finally headed in to the Greeley Ponds around 12:30 pm. The Greeley Ponds hiking trailhead has not been plowed for several years, but on this day the lot was well-packed by vehicle traffic and easy to access. The trail was a solid microspike highway, packed down by Osceola peakbaggers.



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The Greeley Ponds Trail was not as solidly packed after the Mount Osceola Trail junction, so I switched to snowshoes here.


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Cold winter beauty at solidly frozen Upper Greeley Pond. The wind was biting, especially at the south end of the pond.



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Striking views up to the rugged ridge of East Osceola.


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Zoom on the two upper forks of a long slide that fell off East Osceola in the 1950s. 


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The Mount Osceola Trail climbs alongside this huge slab at ~3300 ft. It is part of an old slide that came crashing down in 1892. On the lower slope it merges with the 1950s slide track. I intended to climb partway up the merged slide track after visiting the ponds.



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The cliffs on the NE ridge of East Osceola. There are ice climbing routes up there, including one dubbed "Drool of the Beast."


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Wide angle shot of East Osceola from the SE corner of Upper Greeley Pond.


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Looking north down the pond.


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The west knob of Mt. Kancamagus from the SW corner of the pond.


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Zoom on the K2 Cliff, so named by Waterville Valley hikers in the early 1900s. There was actually a short-lived trail that led up to the top.


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I followed the gently descending trail through open hardwoods on the floor of Mad River Notch, down to Lower Greeley Pond.


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The west knob of Mt. Kancamagus and the K2 Cliff from the NW corner of Lower Greeley Pond.



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Looking south down Lower Greeley Pond to the SW ridge of Mt. Kancamagus and a side profile of the K1 Cliff. The wind was brutal here, so it was a short visit.


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The combined lower track of the 1950s and 1892 slides comes right down to the trail just south of Upper Greeley Pond. The long, curving 1950s slide is fairly popular with backcountry skiers. Luckily for me, there was a rock-solid, snowshoe-wide ski track providing me a route up the gently-rising lower track, leading up to the foot of the long, steep part of the slide.


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Approaching the steep section.


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Access to the first steep pitch looked difficult, so I opted to bushwhack around it.
 


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I climbed up through a steep little gully.


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Up through the woods.


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Tracks.


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Much of the slide is down in a steep-sided gully.


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Farther up, I worked my way down to a wide section of the slide.


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I snowshoed a zigzag route up this snowy, moderately-graded swath. Looking back, I could see the sunlit SW ridge of Mt. Kancamagus.


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Close-up of an ice bulge, of which there are many on this slide. The passage through these ice bulges was a little too steep for my liking. Though avalanche danger below 3000 ft. was rated as low by the Mt. Washington Avalanche Center on this day, I wanted to avoid the steepest grades (~30 degrees or more).


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So I retraced my tracks down to the base of this swath and headed back into the woods to bypass the ice bulges.


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Catching a nice view of Mt. Tripyramid from the woods above the edge of the slide.


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I struggled up through some dense woods and popped back out onto the slide above the ice bulges, where the grade is less steep.


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Zoom on the slabby slide below the K2 Cliff.


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Looking up the slide to the crest of East Osceola far above.
 

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An inviting snowy corridor ahead.


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Looking back. It was tempting to climb farther up the slide, but the hour was late.


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Heading back down.
 

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The profile on the K1 Cliff overlooks Tripyramid.


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Making my way down a steep pitch along the edge, where the snow cover was thinner. 


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Wonderful spot.


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Tracks along the edge.


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Side view.


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Back down through the woods.


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Along the lower track.


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Heading back across Upper Greeley Pond.



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Dusk view of East Osceola.


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Parting shot.


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Thursday, January 15, 2026

1869 Slide, Carter Dome

Made the long drive over to the north end of Pinkham Notch for a hike up Nineteen Mile Brook Trail and a bushwhack to a large open slab on the track of a slide that fell off Carter Dome in 1869. I had visited this slab a couple of years ago on a rainy summer day with no views, so a return visit was in order.



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Nineteen Mile Brook was fairly well locked in.



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Cover was thin on the lower half of the trail, with plenty of ice. 


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Was glad to have Hillsounds for this slightly exposed icy spot on the brookbank.



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The large footbridge built as part of a relocation a few years ago.



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The last half-mile or so before the junction with Carter Dome Trail has many little ups and downs, and there were a few icy pitches.


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A major traffic split at this junction - left for the Carters, ahead for Carter Notch Hut and Wildcat.


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A new footbridge over the tributary just beyond the junction.



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And another new footbridge for the tributary 0.2 mile farther along.


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There was more snow farther up the valley. Time to put the snowshoes on.


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I always enjoy this flat stretch through open woods.


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This small brook at 3.1 miles comes down from the track of the 1869 Carter Dome slide.



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Heading off-trail for the largest remaining open slab on the slide track.


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Grouse tracks.


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Breaking trail. Depending on tree cover, the depth varied from under a foot to two feet plus.



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It was deep and heavy in this sunny spot.


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Nice open woods.




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Looking back.



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Circling up, around and down to avoid some steep terrain.



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Emerging at the top of the big slab, at 3240 ft., with an excellent view of the Northern Presidentials.



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Closer view.
 
 
 
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Down-look. This slide provided an exciting descent route from the summit of Carter Dome (then trailless) for a trio of AMC explorers - William Nowell, guide Charles Lowe and Dr. F.I.R. Stafford - in 1876. In his account of the trip in Appalachia (March 1877), Nowell reported his measurements of the slide, which had a maximum slope of 42 degrees in both its upper and lower sections. He estimated that 20 acres of rock, soil and forest growth had been stripped away. The lower part was mostly “perfectly bare” ledge, from 30 to 60 meters wide. After a “rough and difficult descent” that took two hours, they climbed over a terminal moraine and continued down the picturesque brook below, catching a “baker’s dozen” of trout, and took the Aqueduct Path to the Glen House. Accompanying Nowell's Appalachia account were several profile sketches of Carter Dome, with the slide prominently shown as a curving double line. In 1877, Nowell, Lowe and others opened the Nineteen Mile Brook Trail up the valley to Carter Notch. One of the landmarks noted along the new trail was "the foot of the Great Slide."



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One of the sketches accompanying the Appalachia article. The outline of the curving slide is seen top center. The slide fell on October 4, 1869, in the same storm that triggered the first South Slide on Mt. Tripyramid.


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Looking out from the top center of the slab, where there was a comfortable shelf..


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Side view.



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How the slab looked on a wet summer day. This is a big expanse of rock, 150 feet long and up to 70 feet wide.



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A steep spur ridge of Carter Dome on the north side of the slide.


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There's a wild crag up there.


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Above the slab the old slide is almost completely revegetated, save for one smaller ledge a bit higher up the track.


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Tracks. 



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Jefferson Ravine and Jefferson's Knee, the improbable route of the Six Husbands Trail.





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Mt. Adams, John Quincy Adams, and the ice-draped headwall of Madison Gulf.


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The northern ridge of Wildcat Mountain across the valley.




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A much more recent slide that has fallen on that ridge. Note the huge boulder in the center.


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Heading back down.


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Rejoining Nineteen Mile Brook Trail.



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Homeward bound.



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