ADIRONDACKS
, a See also:group of mountains in See also:north-eastern New See also:York, U.S.A., in See also:Clinton, See also:Essex, See also:Franklin and See also:- HAMILTON
- HAMILTON (GRAND or ASHUANIPI)
- HAMILTON, ALEXANDER (1757-1804)
- HAMILTON, ANTHONY, or ANTOINE (1646-1720)
- HAMILTON, ELIZABETH (1758–1816)
- HAMILTON, EMMA, LADY (c. 1765-1815)
- HAMILTON, JAMES (1769-1831)
- HAMILTON, JAMES HAMILTON, 1ST DUKE OF (1606-1649)
- HAMILTON, JOHN (c. 1511–1571)
- HAMILTON, MARQUESSES AND DUKES OF
- HAMILTON, PATRICK (1504-1528)
- HAMILTON, ROBERT (1743-1829)
- HAMILTON, SIR WILLIAM
- HAMILTON, SIR WILLIAM (1730-1803)
- HAMILTON, SIR WILLIAM ROWAN (1805-1865)
- HAMILTON, THOMAS (1789-1842)
- HAMILTON, WILLIAM (1704-1754)
- HAMILTON, WILLIAM GERARD (1729-1796)
Hamilton counties, often included by geographers in the Appalachian See also:system, but pertaining geologically to the Laurentian See also:highlands of See also:Canada
.
They are bordered on the E. by See also:Lake See also:Champlain, which separates them from the See also:Green Mountains
.
Unlike the Appalachians, the Adirondacks do not See also:form a connected range, but consist of many summits, isolated or in See also:groups, arranged with little See also:appearance of system
.
There are about one See also:hundred peaks, ranging from 'zoo to 5000 ft. in height; the highest See also:peak, Mt
.
See also:Marcy (called by the See also:Indians Tahawus or "See also:cloud-splitter"), is near the eastern See also:part of the group and attains an See also:elevation of 5344 ft
.
Other noted peaks are M`Intyre (5210 ft.), Haystack (4918), See also:Dix (4916) and Whiteface (4871)
.
These mountains, consisting of various sorts of See also:gneiss, intrusive See also:granite and See also:gabbro, have been formed partly by faulting but mainly by erosion, the lines of which have been determined by the presence of faults or the presence of relatively soft rocks
.
See also:Lower Palaeozoic strata See also:lap up on to the crystalline rocks on all sides of the See also:mountain group
.
The region is See also:rich in magnetic See also:iron ores, which though See also:mined for many years are not yet fully See also:developed
.
Other See also:mineral products are See also:graphite, See also:garnet used as an abrasive, pyrite and See also:zinc ore
.
The mountains form the See also:water-parting between the See also:Hudson and the St See also:- LAWRENCE
- LAWRENCE (LAURENTIUS, LORENZO), ST
- LAWRENCE, AMOS (1786—1852)
- LAWRENCE, AMOS ADAMS (1814–1886)
- LAWRENCE, GEORGE ALFRED (1827–1876)
- LAWRENCE, JOHN LAIRD MAIR LAWRENCE, 1ST BARON (1811-1879)
- LAWRENCE, SIR HENRY MONTGOMERY (1806–1857)
- LAWRENCE, SIR THOMAS (1769–1830)
- LAWRENCE, STRINGER (1697–1775)
Lawrence See also:rivers
.
On the See also:south and south-See also:west the See also:waters flow either directly into the Hudson, which rises in the centre of the group, or else reach it through the See also:Mohawk
.
On the north and See also:east the waters reach the St Lawrence by way of Lakes See also:George and Champlain, and on the west they flow directly into that stream or reach it through Lake See also:Ontario
.
The most important streams within the See also:area are the Hudson,' See also:Black, Oswegatchie, Grass, Raquette, Saranac and Ausable rivers
.
The region was once covered, with the exception of the higher summits, by the Laurentian See also:glacier, whose erosion, while perhaps having little effect on the larger features of the See also:country, has greatly modified it in detail, producing lakes and ponds, whose number is said to exceed 1300, and causing many falls and rapids in the streams
.
Among the larger lakes are the Upper and Lower
Saranac, Big and Little See also:Tupper, Schroon, Placid, See also:Long, Raquette and See also:Blue Mountain
.
The region known as the Adirondack See also:Wilderness, or the See also:Great North See also:Woods, embraces between 3000 and 6000 sq. m. of mountain, lake, See also:plateau and See also:forest, which for scenic grandeur is almost unequalled in any other part of the See also:United States
.
The mountain peaks are usually rounded and easily scaled, and as roads have been constructed over their slopes and in every direction through the forests, all points of See also:interest may be easily reached by See also:stage
.
See also:Railways penetrate the See also:heart of the region, and small steamboats ply upon the larger lakes
.
The See also:surface of most of the lakes lies at an elevation of over 1500 ft. above the See also:sea; their shores are usually rocky and irregular, and the See also:wild scenery within their vicinity has made them very attractive to the tourist
.
The mountains are easily reached from Plattsburgh, See also:Port See also:Kent, See also:Herkimer, See also:Malone and See also:Saratoga Springs
.
Every See also:year thousands spend the summer months in the wilderness, where cabins, See also:hunting lodges, villas and hotels are numerous
.
The resorts most frequented are in the vicinity of the Saranac and St Regis lakes and Lake Placid
.
In the Adirondacks are some of the best hunting and fishing grounds in the eastern United States
.
Owing to the restricted See also:period allowed for hunting, See also:deer and small See also:game are abundant, and the See also:brooks, rivers, ponds and lakes are well stocked with See also:trout and black See also:bass
.
At the See also:head of Lake Placid stands Whiteface Mountain, from whose See also:summit one of the finest views of the Adirondacks may be obtained
.
Two See also:miles south-east of this lake, at North See also:Elba, is the old See also:farm of the abolitionist See also:John See also:- BROWN
- BROWN, CHARLES BROCKDEN (1771-181o)
- BROWN, FORD MADOX (1821-1893)
- BROWN, FRANCIS (1849- )
- BROWN, GEORGE (1818-188o)
- BROWN, HENRY KIRKE (1814-1886)
- BROWN, JACOB (1775–1828)
- BROWN, JOHN (1715–1766)
- BROWN, JOHN (1722-1787)
- BROWN, JOHN (1735–1788)
- BROWN, JOHN (1784–1858)
- BROWN, JOHN (1800-1859)
- BROWN, JOHN (1810—1882)
- BROWN, JOHN GEORGE (1831— )
- BROWN, ROBERT (1773-1858)
- BROWN, SAMUEL MORISON (1817—1856)
- BROWN, SIR GEORGE (1790-1865)
- BROWN, SIR JOHN (1816-1896)
- BROWN, SIR WILLIAM, BART
- BROWN, THOMAS (1663-1704)
- BROWN, THOMAS (1778-1820)
- BROWN, THOMAS EDWARD (1830-1897)
- BROWN, WILLIAM LAURENCE (1755–1830)
Brown, which contains his See also:grave and is much frequented by visitors
.
Lake Placid is the See also:principal source of the Ausable See also:river, which for a part of its course flows through a rocky chasm from too to 175 ft. deep and rarely over 30 ft. wide
.
At the head of the Ausable Chasm are the See also:Rainbow Falls, where the stream makes a See also:vertical leap of 70 ft
.
Another impressive feature of the Adirondacks is See also:Indian Pass, a See also:gorge about eleven miles long, between Mt
.
M`Intyre and Wallface Mountain
.
The latter is a majestic cliff rising vertically from the pass to a height of 1300 ft
.
See also:Keene Valley, in the centre of Essex See also:county, is another picturesque region, presenting a pleasing See also:combination of peaceful valley and rugged hills
.
Though the See also:climate during the See also:winter months is very severe—the temperature sometimes falling as See also:low as -42° F.—it is beneficial to persons suffering from pulmonary troubles, and a number of sanitariums have been established
.
The region is heavily forested with spruce, See also:pine and broad-leaved trees
.
Lumbering is an important See also:industry, but it has been much restricted by the creation of a See also:state forest preserve, containing in 1907, 1,401,482 acres, and by the See also:purchase of large tracts for game preserves and recreation grounds by private clubs
.
The so-called Adirondack See also:Park, containing over 3,000,000 acres, includes most of the state preserve and large areas held in private ownership
.
For a description of the Adirondacks, see S
.
R
.
See also:Stoddard, The Adirondacks Illustrated (24th ed., Glen Falls, 1894); and E
.
R
.
See also:Wallace, Descriptive See also:Guide to the Adirondacks (See also:Syracuse, 1894)
.
For See also:geology and mineral resources consult the Reports of the New York State Geologist and the Bulletins of the New York State Museum
.
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