Towns in Clinton County, NY
FROM: Gazetteer and Business Directory
OF Franklin and Clinton Counties, N. Y. For 1862-3.
Compiled and Published By Hamilton Child, Ogdendburg, NY 1862

GAZETTER OF TOWNS.


ALTONA

ALTONA was taken from Chazy, December 2d, 1857. It is an in terior town lying north of the center of the County. The west half is underlaid by Potsdam Sandstone, and hundreds of acres are covered with the naked rock. Great Obazy or Champlain River is the principal stream. Its surface is a rolling upland, with a slight northeasterly inclination. The / soil is light. and sandy, and a large siare is unfit for cultivation. The town is thinly populated and the settlers are principally engaged in lumbering. There is no village in town. Chazy (Altona P. O.) in the north part is a water and wood station on the O. R. R. Ellenburgh Dept is on the west line. The first settler was Simeon Wood, who located in 1800. It has an area of 61,553 acres.


AU SABLE

AU SABLE, pronounced Aw Saw-ble, a French name signifying river of sand, was taken from Peru, March 29, 1839. It is the southeast corner town in the County, Its surface is nearly level in the east, rolling in the center and hilly in the west. The Au Sable forms nearly the whole Qf the South botindary, the Little Sable flows northeasterly through. the west part. Its soil is generally a light sandy loam, fertile in the east and center, but poor for. agricultural purposes in the west. Upon the Au Sable, where it breaks through tbe Potsdam Sandstone, is a beautiful cascade, known as Birmingham Falls. This cascade is located about two miles below Keeseville, and the romantic and picturesque scenery will well repay the tourist for the trip to see them. Iron ore of an excellent quality is to be found. The. principal ore bed now worked is that of Messrs. Arnold & Co., which yields from 1,000 to 1,500 tons anüually. Keeseville, named from Oliver and Richard Keese, Sons of John Keese, one of the original proprietprs-upon the Au Sable, five miles from the Lake, contains seven churches, the Keeseville Academy, two extensive rolling mills, three nail factories, a machine shop, an ax and edge tool factory, a cupola furnace, an axietree factory, a horseshoe factory, a planing mill, two grist mills, and a nail keg factory.

Clintonville, upon the Au Sable, in the west part of the town, was incorporated April 11, 1 1825. The Iron Works located here manufacture over 7,000 tons of iron annually.

New Sweden, further up the Au sable, in the southwest corner of the town, contains two forges. Birmingham Falls, at the head of the rapids, upon Au Sable river is a hamlet. The Union is a hamlet on the line of Peru, and contains two Quaker meeting houses. The first settlers were John Keese and others, about 1795. Edward Everett had located upon the site of the Union in 1786. The town has an area of 22,476 acres.


BEEKMANTOWN

BEEKMANTOWN, names from Wm. Beckman, to whom with oth ers, the town was granted on March 27, 1769-was taken from Plattsburgh, February 25, 1820. Dannemora was taken off in 1854. It lies upon Lake Champlain, near the, center of the east border of the County. It is drained by many small creeks and brooks. The surface is level in the east, and moderately hilly in the west. . Point an Roche and Ram's Head are capes upon the lake. St. Armand's Bay extends into the southeast corner. The soil is a clay loam in the east and center, and a light sand in the wesy. Beekmantown (P O.) and East Beekmantown (P. O.) are hamlets on and near the line of the Plattsburg and Montreal R. R. The first settlers were Maj. Benjamin Mooers and seven associates. who located at Point an Roche, August 10th, 1783. On the 6th of Sept., 1814, the British passed through the town, when a slight skirmish took place, resulting in the death of Lieut. Colonel Wellington and Ensign Chapman, of the enemy, and several American militia. The town has an area of 35,802 acres.


BLACK BROOK

BLACK BROOK, named from its principal stream, was taken from Peru, March 29, 1839. It is the southwest corner of the County. Its surface is rocky and mountainous, the highest peaks being 1,500 to 2,500 feet above the lake. Among the mountains are several nearly level table lands, 200 to 300 feet above the general level. The forest trees are thinly scattered, and nearly the whole town is too rough and poor for cultivation. The Au Sable river forms a portien of the south boundary. The Saranac flows north-esterly across the northwest corner. Great and Little Black Brook; tributaries of the Au Sable, drain the central parts of the town. Among the mountains are several small lakes and ponds. The soil is cold, wet, and poorly calculated for agricultural pursuits. Extensive beds of iron ore are scattered through the town. The Palmer mine, two miles north of Au Sable Forks, yields from 16,000 to 20,000 tons annually. The Myers and Trombois mines are also largely worked. The people are principally engaged in the manufacture of iron, charcoal and lumber.

Sable Forks, on the Au Sable River. in the south-east part of the town, is mostly in Essex County. Messrs. J. & J. Rogers have extensive works here and at Black Brook1 and they manufacture over 2,500 tons of blooms, neaily 1,000 tons of merchant iron, 50,000 kegs of nails, using 1,600,000 bushels of charcoal per annum. Black Brook village, near the south border, contains extensive iron works and several sawmills. Clayburgh, on the Saranac, in the north part, lies partly in the town of Saranac. It contains Iron works and mills. Union Falls (P. O.) and Garlick Falls (P. O.,) both on the Saranac, are hamlets and lumber stations. The first settler was Zephaniah Palmer, who settled at Au Sable Forks about 1825. Several plank roads have been built in town to facilitate the iron and lumber business. The town has an area of 82,004 acres.


CHAZY

CHAZY- prononnced Sha-zee- was taken from Champlain, March 20, 1804. Altona was taken off in 1857. It lies upon Lake Champlain north of the center of the county. Its surface is rolling, having a gentle inclination towards the lake. The principal stream is the Little Chazy, flowing north-easterly through near the center of the town. Corbeau Creek drains the north-west part. The soil is clayey and productive in the east, and sandy and poor in the west.

Chazy village, upon Little, Chazy River, contains two churches, a saw and grist mill, large quantities of excellent lime are burned and fitted for market at this place.- West Chazy, in the south part of the town, on the Little Chazy River, is a Station on the Plattsburgh & Montreal R. R.

Sciota is a station on the P. & M. R. R., in the north-west corner. Chary Landing is a hamlet on the lake shore. Ingraham is a Post Office in the south-east corner of the town. The first settler was John La Trombois, who came into town in 1763. After the Revolution, the first settlers were refugees from Canada and Nova Scotia. The town has an area of 32,628 acres.


CLINTON

CLINTON was formed from Ellenburgh, May 14, 1845. It is the north west corner town of the county. Its surftce is elevated, but generally level. The highest portion along the south border is about 1,050 feet above Lake Champlain. It is nearly all underlaid by Potsdam Sandstone, which is here remarkably white. It is drained by small brooks. - More than three fourths of the town is yet a wilderness, the principal settlements being in the northeast part. The soil is a light sandy loam, capable of bearing but a thin growth of forest trees. A large part of the land is owned by capitalists and speculators. Cherubusco is a Post Office and the "Summit" station upon the O. R. R. The Frontiers (Frontier p. o.), on the north border, and Wrightsville on the west border are hamlets. The first settlers located upon the Old Military Road and near the Frontiers previous to 1820. The town has an area of 42,054 acres.


DANNEMORA

DANNEMORA named by Gen. Skinner from a celebrated iron loca lity in Sweden, was taken from Beekrnantown, Dec. 14, 1854. It is the central town upon the west border of the county. Its surfaee is mostly a wild, mountainous upland, covered with a sandy soil and light growth of forest trees; Chazy Lake, near the centre, 3½ miles long by 1¼ wide, discharges its waters into C hazy River, Upper Chateaugay Lake on the west border, 5 miles long and 1½ miles wide, discharges its waters west into Chateaugay River. The settlements are confined to the southeast corner. Dannemora is a small village grown up around the Clinton Prison. This prison was located here in 1845, for the purpose of employing convicts in the mining and manufacture of iron, so that their labor would not come so directly in competition with the other mechanical trades. The first permanent settler was Thomas Hooker, who came to reside in 1838. The town has an area of 32,889 acres.


ELLENBURGH

ELLENBURGH, named in compliment to Ellen, daughter of John R. Murray, of New York, the principal proprietor of Township, No. 5 of the Military Tract, was formed from Mooers, April 17, 1830. Clinton was taken off in 1845, it lies upon the west border of the county, north of the center. It is an upland, mountainous in the south and rolling in the north, with an inclination towards the north-east. It is watered principally by the west branch of the Chazy River. Crystal Brook flows through the extreme north part. The soil is generally sandy, in many places covered with a rich vegetable mould. The settlements are chiefly confined to the east and west valley, near the north line of
the town. Lumbering is extensively carried on. Ellenburgh Corners and Ellenburgh Centre are thriving little villages. Ellenburgh Depot, on the O. R. R. is a hamlet on the line of Altona. The first permanent settler was Abner Pomeroy, from Vt., about 1800. It has an area of 59,275 acres.


MOOERS

MOOERS, named from Maj. Gen. Benj. Mooers, an early settler and prominent citizen of the county, was formed from Champlain, March 20, 1804. Ellenburgh was taken off in 1830. Its surface is tenerally level with a gentle northeasterly inclination. The principal. streams are Great Chazy and English Rivers. The surface is entirely underlajd by Potsdam Sandstone. and is covered with a light sandy soil. Along the north border are several small swamps. Upon the Canada line in the northwest corner, is a remarkable chasm in the rocks; called The Gulf; it is 16 rods wide and 300 feet deep. At its bottom is a pond of water saideto be 150 feet deep. The walls are of sandstone and perpendicular. No existing agencies could have pro4uced the chasm. The lumbering business is carried on in town to a large extent.

Centerville, (Mooers Forks, p. o.) upon the Chazy River, is a station of the O. R. R.

Mooers upon the Chazy, in the east part, contains several stores and mechanic shops. It is half a mile, south of the junction of the O. and P. &~ M. R. R's. Angelville upon- Corbean Creek is a hamlet in the southeast corner of the town. The first settler was Joshua C. Bosworth, who located in town in 1796. The town has an. area of 50,320 acres.


PERU

PERU, named from its mountainous Character- was taken from Plattsburgh and Willsborough, (Essex Co.) Dec. 28, 1792. A part was annexed to Willsborough in 1799, and Au Sable and Black Brook were taken off in 1839. It lies upon Lake Champlain, south of the center of the county. The surface ih the center and east part is rolling and slightly inclines towards the lake, and in the west it is broken and mountainous. The Au Sable flows across the southeast corner, and along its course are extensive swamps. Little Sable and Salmon Rivers drain the remainder of the town. Military Pond lies on the west line, and is drained by Black Brook. A strip of laud two miles wide, extending along the lake, has a sell composed of clay and clayey loam. Most of this is a plain 4 miles wide, of a sandy soil, interspersed with swamps. In the west, the soil is a light sandy loam. Peru village on the Little Sable, near the center of the town, Laphams Mills, two miles below Peru, and Peasleville, on Salmon River, in the northwest part, are thriving villages. Port Jackson (Valcour, p. o.) on the lake, opposite Valcour Island, is a hamlet containing a church. Peru Landing is a hamlet, north of the mouth of the Little Sable, The first settler was Wm. Hay, a Scotchman who located upon Steward's Patent in 1772. The town has an area of 46,763 acres.


SARANIC

SARANIC- was taken from Plattsburgh, March 29, 1824. It lies upon the west border of the county, south of the centre. Its surface is a broken and mountainous upland. The highest summits along the west border are 4,000 feet above tide. It is watered principally by the Saranac River and its tributaries. There are several falls upon the Saranac, affording an immense amount of water-power. The east- part sloping towards the river is covered with a light sandy soil, and the river intervale with a sandy loam and alluvium. The soil among the mountains is bandy; but the whole western region is too rough for cultivation. Saranac Hollow, Radford and Russia, all on the Saranac River, are small villages. The first settlement was begun in 1802; by Russell Case and Ezekiel Pearce. The town has an area of 69,555 acres.


SCHUYLER FALLS

SCHUYLER FALLS, named from the proprietor of the present village site, was taken from Plattsburgh April 4, 1848. It is an interior town, lying a little southeast of the center of the county. Its surface is rolling in the east and hilly in the west, with an easterly inclination. The Saranac forms its north boundary, and Salmon River flows along its south border. The soil is a light sandy loam. Schuyler Falls, on Salmon River, Mossisonville, on the Saranac, (lying partly in Piattsburgh), and Norrisville, upon Salmon River, three miles west of Schuyler Falls, are thriving manufacturing villages. The first settler was Ezra Turner, who located upon Salmon River in 1797. The town has an area of 22,050 acres.

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