Hiking Giant Mt. & Rocky Peak Ridge

GiantMt. (4,627 ft.) & and Rocky Peak Ridge (4,420 ft.)

June26, 2011

12miles

WesChapman

GiantMountain

I had been out with clients eating very large steakstwo nights in a row, and I was feeling fat, lethargic and tired. I had chewedway too much Trident gum, and was nearing toxic levels of aspartame. This is adangerous combination, and can lead to a continuing pattern of sloth (thefourth of the 7 deadly sins), which is particularly dangerous since I have adouble century bike ride in under two weeks time. I caught an early flight homefrom Ohio, got a good night sleep and headed out to Keene Valley in NY, and aday of hiking with my dogs.

Finding the trailhead can be a bit of an issue inthe Adirondacks, as the forever wild regulations do not seem to impede themaintenance of private clubs with overbearing and obnoxious rules. The primeoffender this week was the Au Sable club. Check out the regulations; theyreally don’t like dogs – not my kind of people. The club itself is magnificentand a holdover from an earlier era with a more relaxed definition of “ForeverWild”. I guess that if it was wild enough for great grandfather, then it’s wildenough for me.

Abroad definition of forever wild

TheAu Sable Club – where the Wild Things are

We hiked up the Roaring Brook Trail, which startedout with a waterfall and ended with a series of rock slides. Along the way wepassed through some truly magnificent hemlock stands, with the trail green withshed hemlock needles – not a good sign. I suspect the malfeasance of the woolyadelgid, relative of the aphid which was introduced from Asia in the 1920’s andhas been slowly spreading up the East Coast since the 1960’s. It is notreported this far north, but the needles on the trail tell another story.

About a mile from the summit, the trail steepenedand the quality deteriorated considerably. These mountains are young,remarkably consistent in rock type, and prone to developing exfoliation domes.These are very long slides, and make it very difficult to lay out and maintaintrails.

Significanttrail erosion on a rock slab on the way up Giant

The view from the top of Giant was obscured byclouds, and a passing rain shower drove us off the summit and over to RockyPeak Ridge. The trail off the top was wet rock, steep slabs and mud. This madefor pretty slow going for us and the handful of fellow travelers that we bumpedinto.

The descent off the summit was a slow affair, and wearrived back at the auto tired, cleansed of our sloth, and ready for a boat rideback to Vermont.

Rockslides on Giant from the top of Rocky Peak Ridge

Mrs.Katie on the top of Rocky Peak Ridge – not bad for 12 years old

Climbing Mt. Marcy & Table Top Mt.

Mt. Marcy
5,344 feet
Table Top Mountain
4,413 feet
18.0 miles
June 6, 2011
Wes Chapman
Mt. Marcy from Marcy Dam
Mt. Marcy or Tahawus (Cloud Splitter)
Mt. Marcy sits squarely at the intersection of two great hiking lists – the 46, 4,000 footers of the Adirondacks and the high points of all 50 states. It also dominates the very impressive skyline of the High Peaks of Adirondack Park in upstate New York, and last weekend was the target of affection for The Girls (my hiking companion poodles Kate and Baby) and me. We headed out across Vermont, then taking the ferry across Lake Champlain and into Adirondack Park.
Marcy is named after Governor William Learned Marcy, who directed its surveying and summiting in 1837. The name Tahawus, or Cloud Splitter, was adopted in a fit of native culture frenzy by early settlers, who could not accept the fact the indigenous people had no name for the mountain at all.   
The view of The High Peaks from Lake Champlain – Our own Rift Valley
The Adirondacks – The Youngest Mountains in America
The Adirondacks began growing above a geological “hot spot” about 10 million years ago, thrusting ancient rock (principally Anorthosite) through the surrounding limestone cap. They are a real oddity in the Eastern US, and produced a radial drainage pattern and fault blocks surrounding the uplift zone. These fault blocks produced some interesting geological anomalies including “horst and graben” type faulting in the Champlain and Lake George Valleys. Faults of this type are normally associated with rift zones like the Great Rift in Africa and the horst and graben province of the Great Salt Lake Valley in Utah.
No matter the geological origin, the view across the Lake is simply breath taking, and the ferry ride to Essex, NY a real treat.
Glaciation made a major impact on the geomorphology of the Adirondacks. The Pleistocene era, beginning about 1.6 million years ago, brought with it four main continental periods of glaciation, the last ending about 12,000 years ago. The combined forces of a 2 mile deep pile of ice grinding from above, and a gently rising magma plume from below, built some of the most striking topography in the US. The Adirondacks still have a radial drainage pattern reflecting the uplift, and surface features entirely of recent glacial origins. Additionally, some really unusual windblown, lake bottom deposits around Lake Placid, form some splendid farming soil, and a handy place to put America’s finest ski jumps.
The Olympic Ski Jumps on a wind-blown glacial lake bed
Adirondack Park – a Constitutional Mandate
Mt. Marcy is the crown jewel of Adirondack Park, a 6,000,000 acre chunk of land (larger than the entire State of Vermont) created in 1885 as a forest preserve, and then as a park in 1892. It is protected by its mandate as forever wild, although it has over 130,000 permanent residents, and over 40 sawmills for the processing of “forever wild” timber. The initial impetus for the Park came from the concerns of businessmen and a local surveyor, Verplanck Colvin, who claimed that failure to stop forest operations, would result in the silting up and destruction of the Erie Canal and the Hudson River. While the concerns regarding silting were transitory, the purchase of the cut-over land was permanent, and relieved the businessmen of their future property tax burdens on worthless property.  
Adding to the legal oversight, the Park was added to the NY State Constitution in 1892, augmenting the already large amounts of confusing and internally contradictory regulation in its Constitution. Today, the NY Constitution has over 56,000 words, exceeding by more than 10x the US Constitution (4,400 words). The net result is a complex regulatory structure in the Park which delights bureaucrats, and alienates backpackers. Specifically, the design, routing and cutting of trails is very slow to respond to use patterns. The result is a large number of poorly designed and implemented trails, and the development of unmaintained “herd paths” which result in very high rates of erosion. There is a preposterous number of “do not” signs and regulations, and very little constructive and productive planning and oversight. 
Bureaucratic Oversight to Maintain a Wilderness
Regulations for those suffering from Agent Orange Flatulence
Adirondak Loj and up the Van Hoevenberg Trail
One Melvin Dewey, a champion of simplified spelling, was responsible for the naming of the facilities of the Adirondack Mountain Club in the Park, and their idiosyncratic spelling. Upstate New York has seen a huge number of utopian reformers, including John Brown and Mr. Dewey. Neither Dewey nor Brown made any long term impact, but Dewey lives on, to the horror of English teachers everywhere.
The trail is extraordinary in its elegant, if overbuilt, bridges and stairways up to the Marcy Dam. The trail gains elevation very gradually up from there to the last .6 mile, where it goes above tree line and gets fairly steep. The view from the top is extraordinary, and the youth of the mountains and their very hard Anorthosite rock is reflected in huge rockslides visible in all directions.
On the trip down, we did a swing up Table Top Mountain to check out the “herd path” access to the top of some of the less frequented mountains in the area. The trail had been cleared with saws, but was not otherwise maintained. The path went straight up the hill, and the erosion was pretty severe.
These are extraordinary mountains, and feel very different than their much older cousins to the East in Maine, New Hampshire and Vermont. This is an area which is clearly worth a visit, and we’ll be back for some more.
A plank bridge across a beaver flowage
The Marcy Dam is built of logs- Old School
The View from the top of Marcy