Balch Pond

Lake Ivanhoe (also known as Round Pond) is located in Carroll County, New Hampshire, in the United States. The lake has no traditional inlets or outlets. Historically, a small stream drained Lake Ivanhoe to Great East Lake, but construction filled in that stream many years ago and now drainage flows via groundwater to Great East Lake. Lake Ivanhoe is classified as "Potentially Impaired" according to the New Hampshire Department of Environmental Services water quality parameters. Lake Ivanhoe receives this designation due to its in-lake phosphorus concentration which exceeds the water quality standards for oligotrophic lakes. The Lake Ivanhoe watershed is 455 acres (184 ha) and is 64% forested. The watershed is currently 17%, developed with 59% of the watershed being buildable area. The Lake Ivanhoe shoreline is primarily composed of low density residential houses and camps (66%). The majority of these structures (88%) are within 50 feet of the water's edge. Lake Ivanhoe water quality monitoring has been collected since 1981. During this period, 16 years of secchi disk transparency data, 17 years of total phosphorus (TP) data, 16 years of chlorophyll-a (Chl-a) data, and 14 years of dissolved oxygen (DO) data have been collected. From this data, the median TP concentration is 8.0 parts per billion (ppb) and the mean transparency is 4.7 metres (15 ft).

East Wakefield is an unincorporated community in the town of Wakefield in Carroll County, New Hampshire. It is located in the eastern part of Wakefield along New Hampshire Route 153, 3 miles (5 km) northeast of Wakefield village and directly south of Pine River Pond. Balch Pond and Ivanhoe Pond are also nearby. The area is a popular summer home location. East Wakefield has a different ZIP code (03830) from the rest of the town of Wakefield.

Great East Lake is an 1,825-acre (7.4 km2) water body located in Carroll County, New Hampshire, and York County, Maine, in the United States. The lake is shared by the towns of Wakefield, New Hampshire, and Acton, Maine, with 45% of its surface area in Acton and 55% in Wakefield. The lake is the farthest upstream of the five headwater lakes of the Salmon Falls River, a tributary of the Piscataqua River. Water from Great East Lake flows out its dam and through the 800-foot (240 m) Newichawannock Canal into Horn Pond, then into the Salmon Falls River below Horn Pond. The widest part of the lake is in New Hampshire. The lake narrows to the east in Maine, creating the First, Second and Third basins. Great East Lake is the largest of the Salmon Falls headwater lakes. Great East Lake supports abundant wildlife, and 21 fish species including lake trout (togue), rainbow trout, smallmouth bass, largemouth bass, American eel, hornpout, white perch, black crappie and chain pickerel.Water quality monitoring data has been collected since 1974, including 29 years of secchi disk transparencies, 23 years of total phosphorus (TP) data, 20 years of chlorophyll-a (Chl-a) data and 7 years of dissolved oxygen (DO) profiles. Sampling results from Station 1 (1974-2008) show a median TP concentration of 6.4 parts per billion (ppb), a mean secchi disk transparency of 9.2 m (30.2 ft), and a mean Chl-a concentration of 1.2 ppb. The data indicates that Great East Lake is a high quality water by both the Maine Department of Environmental Protection and New Hampshire Department of Environmental Services standards.The Great East Lake watershed is located in Acton, Maine, and Wakefield, New Hampshire, and covers approximately 9,939 acres (40.2 km2). Great East Lake is part of the Piscataqua River major drainage basin and the Salmon Falls River subdrainage basin. Great East Lake flows into Horn Pond which in turn starts the Salmon Falls River at its outflow. The Salmon Falls River then flows into the Piscataqua River and into the Great Bay estuary and the Gulf of Maine. The Great East Lake watershed is currently 66% forested, 9% developed, and 52% buildable area. The shoreline of Great East Lake is composed of primarily medium density residential houses and camps (77%). The majority of these structures (64%) are within 50 feet (15 m) of the shoreline.The Great East Lake Improvement Association (GELIA) was founded in 1932 and has been dedicated to the welfare of Great East Lake, its wildlife, and environment. The nonprofit organization sees education as its primary function to help protect the lake. Great East Lake has several other programs and organizations dedicated to protecting its pristine water quality. A boat inspection program is run by the NH Lake Host Program where over 1,000 boats are inspected annually for invasive aquatic plants. There is also a weed watchers program (similar to the Invasive Plants Patrollers Program in Maine).

Pine River Pond is a 570-acre (2.3 km2) lake located in Carroll County in eastern New Hampshire, United States, in the town of Wakefield. Its outlet is the Pine River, which flows northwest to Ossipee Lake. The lake is classified as a warmwater fishery, with observed species including smallmouth and largemouth bass, chain pickerel, horned pout, and black crappie.

The Newichawannock Canal is a man-made canal which drains Great East Lake into Horn Pond at the border between Wakefield, New Hampshire, and Acton, Maine, in the northeastern United States. It is at the head of the Salmon Falls River, which the Abenaki called Newichawannock, meaning "river with many falls". Begun in 1850 by the Great Falls Company to increase the water available for its mills in Somersworth, New Hampshire, the 0.75-mile (1.21 km) canal is unusual as it was built for strictly industrial purposes in an area remote from the actual industrial site. The canal forms the boundary between the states of New Hampshire and Maine, and is spanned by a stone bridge built at the same time. The canal and bridge, along with related artifacts, were listed on the National Register of Historic Places in 2014.

Horn Pond is a 227-acre (92 ha) water body located on the border of Acton, Maine, and Wakefield, New Hampshire, in the United States. The lake is both spring-fed and fed by the outflows of Great East Lake to the north and Wilson Lake to the east. Horn Pond's outlet is the Salmon Falls River which forms a natural border between Maine and New Hampshire and empties into the Piscataqua River east of Dover, New Hampshire, and ultimately the Gulf of Maine. Horn Pond is classified as "Potentially Non-supporting" under the New Hampshire Department of Environmental Services' revised water quality standards for oligotrophic lakes. The Horn Pond watershed covers 1,139 acres (461 ha) that is primarily forested (70%). Only 6% of the watershed is developed, with 34% buildable area. The shoreline of Horn Pond is composed primarily of low density houses and camps (51%) and undeveloped shoreline (44%). 70% of the structures along the shoreline are within 50 feet (15 m) of the water's edge.Horn Pond water quality monitoring has been collected since 1982. During this period, 11 years of secchi disk transparency data, 7 years of total phosphorus (TP) data, 2 years of chlorophyll-a (Chl-a) data, and 5 years of dissolved oxygen (DO) data has been collected. From this data, the median TP concentration is 8.0 parts per billion (ppb) and the mean transparency is 6.6 m (21.7 ft).The Horn Pond Association has been recently redeveloped and aims to protect and improve the water quality of Horn Pond.The lake is classified as a warm- and coldwater fishery and contains brook trout, rainbow trout, brown trout, largemouth and smallmouth bass, Eastern chain pickerel, brown bullhead, white perch and bluegill.

The District No. 2 Schoolhouse, also known as the Little Red Schoolhouse, is a historic one-room schoolhouse at 2851 Wakefield Road in Wakefield, New Hampshire. Built in 1858–59, it was at the time one of the finest district schoolhouses in rural New Hampshire. It was used as a school until 1941, and now houses the museum of the local historical society. The building was listed on the National Register of Historic Places in 1980.

Wilson Lake is a 308 acres (0.5 sq mi; 1.2 km2) waterbody located in York County, Maine in the United States. The lake is spring-fed and drains to Horn Pond which flows into the Salmon Falls River and eventually empties into the tidal waters of the Piscataqua River in Portsmouth, NH, Great Bay and the Gulf of Maine. Wilson Lake is classified as "good" under the Maine Department of Environmental Protection water quality parameters. The Wilson Lake watershed covers 2,479 acres (3.9 sq mi). The watershed is currently 79% forested, 8% developed, and has 49% buildable area. The Wilson Lake shoreline is primarily composed of low density residential houses and camps (63%). The majority of structures (70%) are within 50 feet of the shoreline. Wilson Lake water quality has been measured since 1977. During this period 29 years of secchi disk transparency data, 9 years of phosphorus data, 5 years of chlorophyll-a (Chl-a) data, and 17 years of dissolved oxygen (DO) data has been taken. From this data, the median total phosphorus (TP) concentration in 2008 was 6.5 parts per billion (ppb) and mean secchi disk transparency was 5.9 m (19.4 ft). The Wilson Lake Association was established to maintain a program that will reverse any trend of degrading water quality. The associations also encourages all of the lake's stakeholders to be involved and support cooperative efforts to reduce or eliminate the impact of contaminants on lake water quality.

The Wakefield House is a historic house on New Hampshire Route 153 in the Wakefield Corner area of Wakefield, New Hampshire. The 2+1⁄2-story wood-frame house is believed to have been built c. 1785, but its exterior styling is mainly Federal in character, dating to the 1820s or later. It was used as an inn on the busy stagecoach route through town in the 19th century. It was listed on the National Register of Historic Places in 1983.

The Wakefield Village Historic District encompasses the historic village center of Wakefield, New Hampshire. It is centered at the junction of New Hampshire Route 153 and Mountain Laurel Road, which was historically the major north–south route in Carroll County. The district consists mainly of residential properties dating from the 18th to early 20th centuries, and also includes the 1836 town hall (supplanted in 1895 by the current town hall in Sanbornville), public library¸ Grange Hall, and a one-room schoolhouse that now houses the local historical society. The district was listed on the National Register of Historic Places in 1984.The junction around which the village grew was created in 1778, when the road branching northeast was laid out in the direction of Parsonsfield, Maine. Most of the houses in the district date roughly from this time to the 1820s, and are either vernacular or Federal in style. The notable exceptions are "Westlook", a Colonial Revival house built in 1929, and the Jackson Horne House, built in 1875 and remodeled in 1865. The oldest house in the district is believed to be "The Anchorage", a vernacular Cape style house that appears to date to the 1770s.The Old Town Hall was built in 1836, and hosted the town's meetings until 1895, when the new town hall was built. It has since been leased to the Congregational Church, which uses it for social service functions. The Lovell Grange Hall was built in 1918 for a chapter organized in 1892. It is a rectangular wood frame clapboarded structure mounted on concrete piers. The old portion of Wakefield Library building began as a lawyer's office in the 1860s, and was acquired by the town in 1895 as a gift from Seth Low. The newer portion, also donated by Low, was built in 1902–03. The Colonial Revival Congregational Church was built in 1958, replacing an 1831 church that burned in 1956; it is not historically significant.

The Wakefield Public Library serves the town of Wakefield, New Hampshire. It is located at 2699 Wakefield Road in the Wakefield Village, in an architecturally distinguished Colonial Revival building donated to the town by educator and politician Seth Low. The building was listed on the National Register of Historic Places in 1984.

Wakefield is a town in Carroll County, New Hampshire, United States. The population was 5,201 at the 2020 census. The town includes the villages of Wakefield Corner (the original town center), East Wakefield, North Wakefield, Sanbornville, Union, Woodman and Province Lake. Wakefield Corner, popular with tourists, is a picturesque hilltop village of antique buildings. The state of Maine is on the eastern border of Wakefield.