The soil is very good, and the surface variegated and elevated. Branches of the Charles, the Con- cord, and the Blackstone rise in this town, and, although their streams here are not large, they afford the town a good water power. The min- eral springs in this town have become celebrated. They contain carbonic acid, and carbonate of lime and iron. These are 3 in number, each dif- fering in its properties from the other. They are situated near White Hall Pond, which abounds in fine fish of various kinds. 30 miles W. S. W. from Boston, and 14 E. by S. from Woi'cester.
Hopkinton, N. H., Merrimac co. Contoocook River and its branches, Warner and Blackwater, pass through the town. On these streams are valuable intervale and meadow land. The prin- cipal village is 7 miles from the State House in Concord. In the W. part of the town is a thriv- ing village, on Contoocook River, known as Hill's Bridge or Contoocookville, where is a valuable water power. Eirst settlers, emigrants from Hopkinton, Ms., in 1740. 28 miles N. from Am- herst, and 7 W. from Concord.
Hopkinton, N. Y., St. Lawrence co. Watered by the Racket and St. Regis Rivers. The sur- face and soil are extremely varied, the S. part being the most level, and having the best soil. 25 m. E. from Canton, and 234 N.W. from Albany.
Hopkinton, R. I., Washington co. Wood River, a valuable mill stream, passes through this town. The soil of the town is generally well adapted for grazing and the cultivation of grain. It pro- duces large quantities of fruit and excellent cider. Shad and alewives are taken in Paucatuck River. There are several ponds w'ithin the town. Con- siderable wood and timber are sent to market from this place.
Hopkinton City, at the S. part of the town, on the Tommaquag branch of Charles River, is very pleasant and flourishing.
Horicon, N. Y., Warren co. On the E. side of the Hudson. Watered on the N. by Schroon Lake, which lies mostly in this town. It con- tains also Brant, and several other small lakes. The surface is hilly and mountainous, a large part being waste. 28 miles N. from Caldwell, and 90 N. from Albany.
Hornby, N. Y., Steuben co. Drained by Mead's Creek and some smaller streams. Surface hilly; soil well adapted to grazing. 18 miles S. E. from Bath, and 196 W. by S. from Albany.
Hornellsville, N. Y., Steuben co. Watered by Canisteo River and some of its branches. The surface is somewhat hilly and broken. 20 miles W. from Bath, and 236 W. by S. from Albany.
Horry District, S. C., c. h. at Conwaysboro'. Little Pedee forms its W. boundary, and the Waccamaw, a branch of the Great Pedee, drains the S. and E. portions. Surface level; soil sandy and wet.
Horsham, Pa., Montgomery co. Drained by Pennypack and a branch of Neshaminy Creek. Surface level; soil calcareous loam. 118 miles E. from Harrisburg.
Hot Springs County, As., c. h. at Hot Springs. Bounded N. by Perry co., E. by Saline, S. by Dallas and Clark, and W. by Montgomery. Sur- face rough and hilly. Watered by the Wachita River and branches.
Houghton County, Mn., includes the mining district on Keewaiwona Point, projecting into Lake Superior. The principal settlement is at Eagle River.
Houlton, Me., c. h. Aroostook co. About 90 miles W. of N. from Calais, with which it is con- nected by a good road, and 120 N. N. E. from Bangor. It is on the boundary of New Bruns- wick, and is a U. S. military station. The' dis- tance to Fredericton, N. B., is 75 miles W. N. W. The land is fertile, and the town thriving.
Houma, La., c. h. Terre Bonne parish. On the W. side of Bayou Terre Bonne. 132 miles S. W. from New Orleans.
Houndsjield, N. Y., Jefferson co. Bounded on the N. by Black River, and W- by Lake Ontario. Surface mostly level; soil clay and sandy loam. 6 miles W. from Watertown, and 160 N. W from Albany.
Houston County, Ga., c. h. at Perry. Bounded N. by Bibb co., E. by the Ockmulgee River, sep- arating it from Twiggs co., and by Pulaski co., S. by Dooley, and W. by Macon and Crawford counties. Drained by branches of the Ockmul- gee River.
Houston, Mi., c. h. Chickasaw co. On the head branches of Octibbeha Creek. 145 miles N. E. from Jackson.
Houston, Mo., c. h. Texas co.
Houston County, Ts., c. h. at Crockett. E. cen-, tral, between Trinity and Neches Rivers.
Houston, Ts., c. h. Harris co. This flourishing place is situated on the Buffalo Bayou, which opens into the N. W. arm of Galveston Bay, and about 80 miles from the city of Galveston, with which it is connected by regular steam communi- cation. Being in the centre of an extensive cot- ton-growing region, it has a large and increasing business as a depot for this important article of commerce.
Howard County, la., c. h. at Kohomo.
Howard County, Mo., c. h. at Fayette. Bounded N. by Chariton and Randolph counties, E. by Boone co., S. and W. by the Missouri River, separating it from Cooper and Saline counties. Drained by Great Manitou and Bonne Femme Rivers, and Salt Creek.
Howard, N. Y., Steuben co. Drained by sev- eral small branches of Canisteo and Conhocton Rivers. Surface undulating; soil clay loam, well adapted to the growth of grass and grain. 10 miles W. from Bath village, and 228 W. by S. from Albany.
Howard, Pa., Centre co. Watered by Bald Eagle Creek and its branches, and by Marsh and Beach Creeks. The main ridge of the Alleghany Mountains passes through this town. Soil cal- careous loam in the valleys. 97 miles N. W. from Harrisburg.
Howell, Mn., c. h. Livingston co. 51 miles W. by N. from Detroit.
Howell, N. J., Monmouth co. Drained by Shark, Mettecunk, and Manasquan Rivers. Sur- face level; soil chiefly sandy loam and clay.
Howland, Me., Penobscot co. This is a large township of good land, in which the Piscataquis and Seboois Rivers form a junction. At the mouth of the former, about 50 rods from the Pe- nobscot, are several saw mills. The banks of the river are low and very beautiful. Howland was incorporated in 1826. It lies 117 miles N. E. from Augusta, and 34 N. from Bangor.
Hubbardston, Ms., Worcester co. Formerly a part of Rutland, named after Thomas Hub- bard, of Boston, a principal proprietor. Hub- bardston is pleasantly situated on the height of ground between Connecticut River and the | |