Angus Cobblestone Farmhouse and Barn Complex

Jephtha Earl Cobblestone Farmhouse is a historic home located at Benton in Yates County, New York. The farmhouse was built about 1850–1860 and is an example of Italianate style, cobblestone domestic architecture. The main block is a two-story, L-shaped mass with a cross-gable roof and pedimented front gable, connecting a number of wings. It is built of tiny, reddish, oval-shaped cobbles. The farmhouse is among the nine surviving cobblestone buildings in Yates County.It was listed on the National Register of Historic Places in 1992.

The Finger Lakes AVA is an American Viticultural Area located in Upstate New York, south of Lake Ontario. It was established in 1982 and encompasses the eleven Finger Lakes, but the area around Canandaigua, Keuka, Seneca, and Cayuga Lakes contain the vast majority of vineyard plantings in the AVA. Cayuga and Seneca Lakes each have their own American Viticultural Areas completely contained within the Finger Lakes AVA (Cayuga Lake AVA and Seneca Lake AVA). The Finger Lakes AVA includes 11,000 acres (4,452 ha) of vineyards and is the largest wine-producing region in New York State.

Bellona is a hamlet in Yates County, New York, United States. The community is 6.9 miles (11.1 km) north-northeast of Penn Yan. Bellona has a post office with ZIP code 14415, which opened on May 14, 1816.

Whitaker House is a historic home located at Benton in Yates County, New York. It is a Late Gothic Revival style structure built about 1850.It was listed on the National Register of Historic Places in 1994.

Dresden is a village in Yates County, New York, United States. The population was 308 at the 2010 census. The village was named after Dresden in Germany. The Village of Dresden is located in the Town of Torrey and is twelve miles south of Geneva. Dresden is located in the Finger Lakes Region of New York.

Robert Ingersoll Birthplace, also known as Robert Green Ingersoll Birthplace Museum, is a historic home located at Dresden in Yates County, New York. It is a Federal-style structure that consists of a two-story, three-bay, gable-roofed central block with a two-part, 1+1⁄2-story saltbox ell on the west side. The central block and the front portion of the ell were built separately and joined sometime before they were moved to their present location prior to 1833. The rear portion of the ell was added on-site at the current location at an unknown date. The house was the birthplace of noted agnostic and politician Robert G. Ingersoll (1833–1899). It was listed on the National Register of Historic Places in 1988, and added to New York State's Register of Historic Places in 1987.

Christopher Willis House is a historic home located at Dresden in Yates County, New York. It is a Greek Revival/Italianate style structure built about 1830.It was listed on the National Register of Historic Places in 1994.

Keuka Lake Outlet is a river located in Yates County, New York. It drains Keuka Lake and flows into Seneca Lake by Dresden, New York. The Crooked Lake Canal was developed along the route of the river. The canal was later replaced by a railroad which is now a hiking and cycling trail, the Keuka Outlet Trail.

The Crooked Lake Canal was a canal in western New York, United States. Built from 1830-1833, the canal linked two Finger Lakes: Keuka and Seneca lakes. The name refers to the unusual shape of Keuka Lake, which was formerly called "Crooked Lake". The Keuka Outlet Trail now follows much of the route of the former canal.

Torrey is a town in Yates County, New York, United States. The population was 1,282 at the 2010 census. The name is taken from that of early county political leader Henry Torrey. The Town of Torrey is in the east central part of the county and is south of Geneva. The town of Torrey is unrelated to the 10,000+ acre Torrey Farms, located in Elba and Potter, which is one of the largest farms in New York.

Crooked Lake Outlet Historic District is a national historic district located near Penn Yan in Yates County, New York. The district is located along a seven-mile recreational trail (the Keuka Lake Outlet Trail) that parallels the Keuka Lake Outlet. The district includes several mill sites along the gorge. It also includes nine areas that contain surface and subsurface archaeological remains.It was listed on the National Register of Historic Places in 1996.

A tunnel valley is a U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. They can be as long as 100 km (62 mi), 4 km (2.5 mi) wide, and 400 m (1,300 ft) deep. Tunnel valleys were formed by subglacial erosion by water and served as subglacial drainage pathways carrying large volumes of meltwater. Their cross-sections often exhibit steep-sided flanks similar to fjord walls. They presently appear as dry valleys, lakes, seabed depressions, and as areas filled with sediment. If they are filled with sediment, their lower layers are filled primarily with glacial, glaciofluvial or glaciolacustrine sediment, supplemented by upper layers of temperate infill. They can be found in areas formerly covered by glacial ice sheets including Africa, Asia, North America, Europe, Australia and offshore in the North Sea, the Atlantic and in waters near Antarctica. Tunnel valleys appear in the technical literature under several terms, including tunnel channels, subglacial valleys, iceways, snake coils and linear incisions.