The Willsboro School

Willsboro Congregational Church is a historic Congregational church on NY 22 in Willsboro, Essex County, New York. It was built in 1834 and is a simple rectangular limestone building with a gable roof. It features an engaged bell tower at the east gable end. It was listed on the National Register of Historic Places in 1984.

Willsboro is a hamlet and census-designated place (CDP) in the town of Willsboro in Essex County, New York, United States. The population of the CDP was 753 at the 2010 census, out of a total town population of 2,025.

Willsboro is a town in Essex County, New York, United States, and lies 30 miles (48 km) south of the city of Plattsburgh. As of the 2020 census, the town's population was 1,905. The town is named after early landowner William Gilliland.

Sheldon–Owens Farm is a national historic district located at Willsboro in Essex County, New York. The district contains seven contributing buildings, one contributing site, and seven contributing structures. They are set on a property assembled between 1784 and 1945. The oldest structure is a barn dated to the late 18th century. A number of the outbuildings date to the 1830s and include barns, a granary, brick smokehouse, and sugar house. The farmhouse dates to 1853 and was constructed on the foundation of the 18th-century house. Dated to the early 20th century are a storage shed, machine shed, well house, and additions and renovations to older buildings. The property has been adapted for use as a bird sanctuary. It was listed on the National Register of Historic Places in 1993.

The Abraham Aiken House is a historic house and estate located at Willsboro in Essex County, New York.

The Boquet River (pronounced BO-kwet) is a small river in upstate New York, United States. It was sometimes called the Bouquet River before a 1982 Board on Geographic Names decision. It is the steepest river in New York state, with a vertical drop of over 2,700 feet (823 m) over 40 miles (64 kilometers) from its source on Dix Mountain in the Adirondack Mountains to its mouth at Lake Champlain. The South Fork of the Boquet originates on South Dix Mountain in North Hudson. It runs northeast through Keene and enters Elizabethtown where it joined from the west by the North Fork of the Boquet near the intersection of US route 9 and NY route 73. Northeast of downtown Elizabethtown, it becomes the border of the Town of Lewis. It then flows east under the Adirondack Northway (Interstate 87) in Lewis, turns south to pass through the southwest corner of Essex into Westport before looping north back into Essex and then Willsboro where it empties into Lake Champlain at Noblewood Park. It traverses several waterfalls, including at Split Rock, a large flume falls in the center of Wadhams, and in downtown Willsboro. The river flows through the Boquet River Nature Preserve in downtown Willsboro. Tributaries of the Boquet include the North Branch, The Branch or Little Boquet, Spruce Mill Brook, and The Black River/Lincoln Pond. The watershed drains 280-square miles within the Adirondack Park in Essex county.

The Octagonal Schoolhouse built in 1827 is an historic stone octagon-shaped school building located in the hamlet of Boquet in the western part of the town of Essex, New York. On January 17, 1973, it was added to the National Register of Historic Places.

Foothills Baptist Church is an historic Carpenter Gothic church located at 2172 New York Route 22 in the Boquet section of Essex, New York, in the United States. Built in 1855 as St. John's Episcopal Church, it became the Union Church at Boquet Chapel in 1880, the Church of the Nazarene in 1949 and Foothills Baptist Church in 2005. It has also been known as Boquet Chapel. The church was listed on the National Register of Historic Places as the Church of the Nazarene in 1973. It was listed for its architecture: the church follows a published design by architect Richard Upjohn, and was described as being "remarkably untouched and yet well-maintained example of the simplest of Richard Upjohn's standard ecclesiastical designs."

Essex Village Historic District is a national historic district located at Essex in Essex County, New York. The district contains 150 contributing buildings. It encompasses the historic core of the hamlet of Essex and primarily contains early-19th-century buildings. The predominant building materials are clapboarded wood frame, brick, and stone and none of the buildings exceed 2+1⁄2 stories in height. The oldest documented structure is Dower House, built prior to 1793. Other notable buildings include Wright's Inn (1798), Essex Free Library (1818), and "Hickory Hill" (1822), "Rosslyn" (ca. 1830), the "Old Brick Schoolhouse" (1830), and "Greystone" (1853). It was listed on the National Register of Historic Places in 1975.

Essex is a town in Essex County, New York, United States overlooking Lake Champlain. The population was 621 at the 2020 census. The town is named after locations in England. The town is on the eastern edge of the county. It is 17 miles (27 km) south-southwest of Burlington, Vermont, which is on the opposite shore of Lake Champlain, 32 miles (51 km) south of Plattsburgh, 94 miles (151 km) south of Montreal, Quebec, and 135 miles (217 km) north of Albany. Essex is inside the Adirondack Park.

The Crater Club is a seasonal residential enclave on the shore of Lake Champlain approximately one mile south of Essex, New York within the Adirondack Park region. The club was originally developed as a summer retreat by the naturalist and outdoor writer John Bird Burnham in the early 1900s. Currently the Crater Club consists of over 40 homes, a clubhouse, playing fields, four clay tennis courts, and a waterfront featuring a permanent pier and a screened building known as Burnham's Landing. This latter building is also the headquarters of the Split Rock Yacht Club, which maintains a small but active racing fleet of Cape Cod Knockabout sailboats and holds weekly sailboat races during the summer season open to these and other small one-design classes. Like the Scouting Movement, the Crater Club is an example of the American movement that embraced basic, "frontier" values in contrast to the rampant urbanization and industrialization of the late 19th and early 20th centuries. Early members purchased lots from Burnham then built simple cottages that deliberately eschewed the luxuries and decorative excesses of Adirondack "Great Camps" such as those designed by William L. Coulter of Saranac Lake. Crater Club members swam, sailed small boats, and hiked for pleasure, believing in the salubrious effects of exposure to Nature on work-wearied urbanites and their children. Although many of the early residents were in business, others were academics and other professionals. A number of books have been produced by Crater Club residents during their sojourns there, and the club and its facilities still provide a warm community for families seeking a quiet and unassuming place to vacation and recharge in the summer months.

The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley. Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont. The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County. Most of this area is part of the Adirondack Park, offering tremendous views of the Adirondack High Peaks region and many recreational opportunities in the park and along the relatively undeveloped coast line of Lake Champlain. The city of Plattsburgh is to the north, and the historic town of Ticonderoga is in the southern part of the region. The northern part of Lake George is located at, and near Ticonderoga, and therefore is a part of the Champlain Valley.