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The 573-acre (2.32 km 2) pond is within 3,000 acres (12 km 2) of public land. There is a public cement boat ramp on Sanctuary Road. The Kettle Pond Visitor Center, operated by U.S. Fish and Wildlife Service and the Rhode Island National Wildlife Refuge, hosts school field trips and educational programs about the pond's flora, fauna and habitats.
Kettle Pond State Park is a state park near Marshfield, Vermont in the United States. [1] It is one of seven state parks located in Groton State Forest. The park is on Vermont Route 232 two miles west of Groton. The park is located on Kettle Pond (109 acres), an undeveloped pond. [2]
900 acres, Kettle Pond Visitor Center features exhibits, education programs Norman Bird Sanctuary: Middletown: Newport: 325 acres with 7 miles of trails, natural history museum Save the Bay Exploration Center & Aquarium: Newport: Newport: website, 2 facilities, aquarium, environmental education and conservation programs Tri-Pond Park Nature Center
Walden Pond is a historic pond in Concord, Massachusetts, in the United States. A good example of a kettle hole , it was formed by retreating glaciers 10,000–12,000 years ago. [ 4 ] The pond is protected as part of Walden Pond State Reservation , a 335-acre (136 ha) state park and recreation site managed by the Massachusetts Department of ...
Maple, oak and beech trees, the remains of a 250-year-old mill, stone slab bridges and the last dam on the Pawcatuck River are seen in Westerly.
Visitors can obtain maps and trail guides for the parks and forest. The Center is within walking distance of Big Deer State Park, Stillwater State Park and Boulder Beach State Park. The other parks in Groton State Forest are Kettle Pond State Park, New Discovery State Park, Ricker Pond State Park and Seyon Lodge State Park.
Park. Estimated Visitors. Busiest Month. Straight Lake State Park. 7,406. July (1,191) Menominee River Recreation Area. 11,627. July (2,016) Tower Hill State Park
A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased ...