The Adirondack Park Agency (APA) will hold its regularly scheduled monthly meeting this Thursday, April 15, 2010 at APA Headquarters in Ray Brook, NY. The April meeting is one day only and will be webcast live.
Among the topics on this month’s agenda are proposed amendments to the Independence River Wild Forest Unit Management Plan, fire towers in the St. Regis Canoe Area and the Hurricane Primitive Area, the proposed Crown Point Bridge, a proposed parking lot and trail relocation for the Stillwater Mountain area, the large-scale Tall Timbers development in at North Creek, a Twitchell Lake waterfront development project, a Raquette River Boat Club rezoning, the 2009 State Land Classification and Reclassification package (tentatively scheduled), and a commemoration of Earth Day. » Continue Reading.
The state Department of Environmental Conservation’s proposal to remove fire towers from St. Regis and Hurricane Mountains raises some difficult philosophical questions, starting with: what is wilderness?
In calling for the towers’ removal, DEC relies on the definition in the Adirondack Park State Land Master Plan, which is taken from the federal Wilderness Act: “an area where the earth and its community of life are untrammeled by man—where man himself is a visitor who does not remain.” » Continue Reading.
The New York State Department of Environmental Conservation has rescheduled two public meetings that had been canceled due to poor weather. A meeting on the draft amendment to the St. Regis Canoe Area Unit Management Plan (UMP) will now be held at 6:30 p.m. Wednesday, March 10, in the Freer Science Building Auditorium at Paul Smiths College, at the intersection of Routes 86 and 30 in Paul Smiths.
A meeting on draft UMPs for Jay Mountain Wilderness and Hurricane Mountain Primitive Area will be held at 6:30 p.m. Thursday, March 11, in Keene Central School, 33 Market Street in Keene Valley. A presentation on Adirondack Park Fire Tower Study will be made at both meetings, followed by a presentation on the draft UMPs or draft amendment, after which public comments will be taken. Comments for the draft UMPs or the draft amendment will be taken at either meeting.
Copies of the documents are available on compact discs (CD) at DEC offices in Albany, Herkimer, Warrensburg, and Ray Brook. To request a copy, e-mail email@example.com or call 518-897-1291. CDs containing all four documents are also available for public review at the town offices of Santa Clara, Brighton and Harrietstown in Franklin County, and the town offices of Elizabethtown, Jay, Keene and Lewis in Essex County.
The following libraries also have CDs containing the documents for public review:
Saranac Lake Free Library, (518) 891-4190. Joan Weil Library, Paul Smiths College, (518)327-6313. Elizabethtown Library, (518) 873-2670. Keene Public Library, (518) 576-2200. Keene Valley Public Library, (518) 576-4335.
Additional information about the study, the draft UMPs and the draft amendment and the full documents may be viewed or downloaded at the DEC web site as follows:
Fire Tower Study – www.dec.ny.gov/lands/62283.html
Scandinavian folklore has described eskers as being formed by large sea serpents crawling inland to die. Celtic lore describes eskers as being formed by monks carrying baskets of sand inland from the sea as a form of penitence. What are eskers? They’re glacial features that kind of look like an up side-down riverbed. As a glacier retreats, it leaves behind outwash deposits of sand, gravel, and stone that may form long, interrupted, undulating ridges. Sometimes, just like a river, they branch off and there may be two or three in a roughly parallel arrangement. Colloquially, they have been called horsebacks, hogbacks, serpent ridges, and sand dunes.
Luckily, these interesting features are commonly encountered while paddling (and carrying) in the Adirondacks. Most Adirondack eskers run in a NE to SW arc, starting near the N. Br. of the Saranac and extending to Stillwater Reservoir, with the highest concentration within the combined St. Regis/Saranac basin. Others are found in the drainages of West Canada Creek and the Schroon, Moose, Hudson, and Cedar Rivers. The Rainbow Lake esker bisects that lake; A. F. Buddington, an early geologist, says this is one of the finer examples of an esker and considers it to extend (in a discontinuous manner) for 85 miles.
There is a long discontinuous esker from Mountain Pond through Keese Mill, passing between Upper St. Regis Lake and the Spectacle Ponds, and continuing to Ochre, Fish, and Lydia Ponds in the St. Regis Canoe Area. Other very interesting eskers are found on the lower Osgood, at Massawepie Lake (you drive on the esker to get to this lake), near Hitchins Pond on the Bog River/Lows Lake trip, and along the Saranac River near its namesake village. An esker in the Five Ponds Wilderness can be paddled to (though is usually hiked to). It bisects theses ponds and, at 150 feet high, is among the tallest.
Examples of twin or double eskers are those at Rainbow and Massawepie Lakes and there are triple ridges near Jenkins Mountain and Cranberry Lake. Eskers make for great hikes. They generally support tall stands of white pines. You can often see related glacial features such as kames, kettle holes, and kettle ponds. If you’re lucky, you might also find some sea serpent scales. If you can’t find these, put on your penitent face and bring along a basket of ocean sand on your next paddling trip.
Map of the Rainbow Lake esker (to come) by A. F. Buddington, 1939-1941. Esker ridges are indicated by yellow shading. Source: Geology of the Saranac Quadrangle, New York, a 1953 New York State Museum bulletin (# 346)
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