Windsor Meadows State Park

The Captain John Bissell Memorial Bridge carries I-291 over the Connecticut River, connecting the towns of Windsor, Connecticut and South Windsor, Connecticut. There is a pedestrian crossing on the bridge on the westbound, upstream side.

The Oliver W. Mills House is a historic house at 148 Deerfield Road in Windsor, Connecticut. Built in 1824, it is a well-preserved local example of a Federal period brick house. It was listed on the National Register of Historic Places in 1985.

The Captain Benjamin Allyn II House, also known locally as the Thomas Allyn House, is a historic house at 119 Deerfield Road in Windsor, Connecticut. Built in the mid-18th century or possibly earlier, it is a well-preserved example of a Colonial era brick house. It was listed on the National Register of Historic Places in 1979.

The Timothy Dwight Mills House is a historic house at 184 Deerfield Road in Windsor, Connecticut. Built about 1833, it is a well-preserved local example of transitional Federal/Greek Revival architecture executed in brick. It was listed on the National Register of Historic Places in 1988.

The Elijah Mills House is a United States historic house at 45 Deerfield Road in Windsor, Connecticut. Built in 1822, it is a well-preserved local example of a Federal period brick house. It was listed on the National Register of Historic Places in 1985.

Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam at present-day Rocky Hill, Connecticut, to St. Johnsbury, Vermont (about 320 kilometres (200 mi)). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook. Lake Hitchcock is an important part of the geology of Connecticut. It experienced annual layering of sediments, or varves: silt and sand in the summertime (due to glacial meltwater) and clay in the wintertime (as the lake froze). Analysis of varves along Canoe Brook in Vermont was conducted by John Ridge and Frederick Larsen, including radiocarbon dating of organic materials. Their research indicates that the lake formed sometime prior to around 15,600 years ago. Later, abrupt changes in sediment composition around 12,400 years ago appear to mark the initial breaching of the lake's dam. These varved lake deposits were later used by European settlers for brick-making. The lake was named after Edward Hitchcock (1793–1864), a geology professor from Amherst College who had studied it.

The Giles Barber House is a historic house at 411-413 Windsor Avenue in Windsor, Connecticut. Built about 1825, it is a well-preserved local example of a transitional Federal-Greek Revival brick house. It was listed on the National Register of Historic Places in 1988.

The Capt. James Loomis House is a historic house at 881 Windsor Avenue in Windsor, Connecticut. Built about 1825, it is a good local example of transitional Federal-Greek Revival architecture executed in brick. The house was listed on the National Register of Historic Places on September 15, 1988.

The George G. Loomis House is a historic house at 1003 Windsor Avenue in Windsor, Connecticut. Built about 1856, it is a good local example of transitional Greek Revival-Italianate architecture executed in brick. It was listed on the National Register of Historic Places in 1988.

The Gordon Loomis House is a historic house at 1021 Windsor Avenue in Windsor, Connecticut. Built in 1835, it is a good local example of transitional Federal-Greek Revival architecture executed in brick. It was listed on the National Register of Historic Places in 1988.

The Windsor Farms Historic District encompasses a large historically agricultural area and the historic town center of South Windsor, Connecticut. Its built environment extends mainly along Main Street, between Interstate 291 in the south and Strong Road in the north, with a diversity of architecture spanning three centuries. The district includes agricultural fields on both sides, many of which remain in tobacco cultivation. The district was listed on the National Register of Historic Places in 1986.

The Ira Loomis Jr. House is a historic house at 1053 Windsor Avenue in Windsor, Connecticut. Built in 1833, it is a good local example of transitional Federal-Greek Revival architecture executed in brick. It was listed on the National Register of Historic Places in 1988.