greatest w'idth being about one mile, encircling twenty islands, and affording a delightful land- scape.
The Statistics and Gazetteer of New-Hampshire, Seventh Edition, Compiled by Alonzo J. Fogg. Concord, N.H.: D.L.
Mi?ierals. Bog iron ore, zinc and copper ore are found in vari- ous localities.
Employments. The inhabitants are largely engaged in farming. The lumber business is extensive- ly carried on. 1,400 bushels wheat, 3,000 bushels corn, and
9,000 bushels of oats and barley are annually produced.
Resources. Productions of the soil, $61,254; mechanical labor, $ 15,000; money at interest, $ 19, 976; deposits in savings banks, $ 20; stock in trade, $ 8,800; from tourists, $ 3,000.
Churches and Schools. Christian, Union, and Methodist. There are six schools in town. Average length of schools for the year, twenty-three weeks.
Hotel. Monroe House.
First Organization. . Monroe was disannexed from the western part of Lyman, and formed into a separate town, July 13, 1854.
Boundaries. North by Little- ton, east by Lyman, south by Bath, and west by Barnet, Vermont. Area of improved land, 8,246 acres.
Distances. By railroad, ninety- seven miles north from Concord, and fifteen north from Haverhill.
Railroad. At Mclndoes Falls, on the Passumpsic Railroad, in Vermont, is the station for Mun- l'oe.
MOULTONBOROIJGH.
Carroll County. The surface of Moultonborough is mountain- ous, but the soil is deep and fer- tile, and yields good crops of |
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wheat, corn, potatoes, &c. The town ranks as the sixth town in the county, in the value of its ag- ricultural products.
Rivers, Ponds, &e. Red Hill River, the principal stream, origi- nates in Sandwich, and passes through this town into the Winni- piseogee. Long Pond is a beauti- ful sheet of water, and connects with the lake by a channel sixty rods in length. Squam and Win- nipiseogee Lakes lie partly in this town.
Mountains. Red Hill, lying wholly in this town, is about 2,000 feet above the level of the sea, and commands notice from the east, south, and west, and extends about three miles from east to west, between Red Hill River on the north, Great Squam on the west, Great Squam and Long Pond on the south, terminating south-east by a neck of fine land, extending into the Winnipiseogee. A number of oval bluffs rise on its summit, from each of which the prospect, on either hand, is extensive and delightful. The north bluff is supposed to consist of a body of iron ore. Bog ore is found in a brook descending from this bluff. This mountain is cov- ered with soil, and is wooded nearly to its summit. It owes its name to the circumstance of the leaves, JJva Ursa, with which it is covered, changing to a brilliant red in the autumn. Ossipee Mountain extends its base into this town, and is a commanding elevation.
Springs. On the south part of Ossipee Mountain, in Moultonbo- rough, is a mineral chalybeate spring, the water strongly impreg- nated with iron and sulphur, and |