I dug in a tub of iced beer and Quinn and I toasted the two cans as we sat back on Adirondack chairs to enjoy the late afternoon.
Lake Champlain, which lies beautifully in the valley between the Green and Adirondack mountains, belongs mostly to Vermont.
Murray (1840-1904), called "Adirondack Murray," from his Camp Life in the Adirondack Mountains (1868), was once pastor.
The most notable topographic feature is the roughly circular mountain area of north-eastern New York known as the Adirondack mountains (q.v.).
While igneous and metamorphic crystalline rocks form the bulk of the Adirondack area, it is surrounded by a ring of ancient Palaeozoic sediments in which these peripheral lowlands have been developed.
The Adirondack area proper, and much of the surrounding ring of more recent rocks, is either too rugged, or has a soil too thin and rocky for extensive agriculture.
South of the Adirondack region, and S.
Other notable falls are those of the Genesee at Portage and at Rochester, Trenton Falls, the Falls of Ticonderoga, and a multitude of falls and rapids in the Adirondack region and along the shores of the upper portions of the Finger Lakes.
In the Adirondack region the snowfall is heavy, the winter long and severe.
In the Adirondack region the trees were principally white pine, spruce, hemlock and balsam, but mixed with these were some birch, maple, beech and basswood, and smaller numbers of ash and elm; in the swamps of this region were also larch and cedar.
The original varieties of trees still abound, though in less numbers, on lands illadapted to agriculture, and in the Adirondack and Catskill Mountains, where the state has established forest preserves, and the Forest, Fish and Game Commissioner began reforesting in 1901, principally with pine, spruce and larch.
Of the fur and game animals which were inhabitants of the primeval forests few of the larger species remain except in the Adirondack region.
Of the Adirondack Mountains and in the rugged portions of the counties in the S.
The principal forest area is in the Adirondack region where the state has a forest preserve (in Clinton, Essex, Franklin, Fulton, Hamilton, Herkimer, Lewis, Oneida, St Lawrence, Saratoga, Warren and Washington counties) containing (1909) 1, 53 0, 559 acres, and there is as much or more in private preserves and in tracts owned by lumbermen.
(board measure); of this about five-eighths was from the Adirondack region, a little more than one-fourth was from the farming regions, and a little less than one-eighth was from the Catskill region.
As Wayne county, but the mines in Essex, Clinton and Franklin counties of the Adirondack region are by far the most productive.
Limestone 1 These include: the Adirondack Hatchery at Upper Saranac, Franklin county; the Caledonia Hatchery at Mumford, Monroe county; the Cold Spring Harbor Hatchery, at Cold Spring Harbor, Suffolk county; the Delaware Hatchery, at Margaretville, Delaware county; the Fulton Chain Hatcher y, at Old Forge, Herkimer county; the Linlithgo Hatchery, at Linlithgo, Columbia county; the Oneida Hatchery, at Constantia, Oswego county; and the Pleasant Valley Hatchery, at Taggart, Steuben county.
Graphite is widely distributed in the Adirondack region, but the mining of it is confined for the most part to Essex and Warren counties; in 1908 the output was 1,932,000 lb.
The so-called Adirondack Park, containing over 3,000,000 acres, includes most of the state preserve and large areas held in private ownership.
With the reservations that only in the case of certain red haematite bedded deposits can any estimate be made of relative accuracy, say within 10%; that the concentration deposits of brown ore can be estimated only with an accuracy represented by a factor varying between 0.7 and 3; and that the great Lake Superior and the less known Adirondack deposits can be estimated within 15 to 20%, the total supply of the country was estimated at 79,594,220,000 long tons73,21o,415,000 of which were credited to haematite ores and 5,054,675,000 to magnetite.
The Adirondack Mountains .T his rugged district of northern New York may be treated as an outlier in the United States of the Laurentian highlands of Canada, from which it is separated by the St Lawrence Valley.
A remarkable feature of the belt is the longitudinal chain of broad valleys - the Great Appalachian Valley - which, in the southerly sections divides the mountain system into two subequal portions, but in the northernmost lies west of all the ranges possessing typical Appalachian features, and separates them from the Adirondack group. The mountain system has no axis of dominating altitudes, but in every portion the summits rise to rather uniform heights, and, especially in the central section, the various ridges and intermontane valleys have the same trend as the system itself.
Turner; Reports of the New York Geological Survey from 1842 to 1854 (Albany); Reports of the Topographical Survey of the Adirondack Region of New York (Albany, 18731880); Reports of the New York Meteorological Bureau (1889 sqq.); and publications of the United States Weather Bureau.