Pisgah State Park includes 0ver 13,500 acres (5695 in Chesterfield) of rough forested terrain encompassing a complete watershed north of the Ashuelot River. Within the Cheshire County towns of Winchester, Chesterfield and Hinsdale, the park protects seven ponds, four highland ridges and numerous wetlands. The area's 21 square miles make it the largest property in the New Hampshire state park System.

A national memorial for all American war dead, Cathedral of the Pine's Altar of the Nation is comprised of stones donated as tributes from all United States Presidents since and including Harry Truman.
The Cathedral is available for Weddings, Memorial Services, Religious Services, Baptisms, Bar and Bat Mitzvahs, Services for Fraternal Groups, Veterans Groups, and Baccalaureate Services.
The Cathedral Hill Top House will be open during the winter months (November through April) by reservation for meetings, weddings and services.

The Wyman Tavern, one of Keene's most historic houses, was built more than two centuries ago. The Tavern is maintained as a period house museum representing the period from 1770 to 1820. It has been placed on the National Register of Historic Places.
It was from this tavern that 29 minutemen started their march to Lexington and Concord in April of 1775 under the command of Captain Wyman, a veteran of the Indian Wars.

If you pass along a quiet New England road in fall and come upon what appears to be someone's misplaced home, you're tempted to recall the romantic version of the origin of covered bridges.
They, of course, were built for discretely kissing your favorite girl while on a long buggy ride home from church...

The Stately Federal style house, located on Main Street in Keene, was the home of Horatio Colony, descendent of one of Keene's historic families. This old-time New England home is filled with original family furnishings and fabulous collections which offer a gracious view of a vanishing lifestyle of culture, refinement and travel. Preview the history, virtual tour, and all the offerings on our web site. But to truly experience the house and nature preserve, come and visit both sites in the historic New England city of Keene, New Hampshire.

is a naturally occurring geologic phenomenon located along Rt. 9 in Chesterfield, NH.

Geologists have three theories about the possible formation of Chesterfield Gorge. All the theories state that the rock bed of the gorge has been worn down by running water. Over thousands of years the stream has worn its path deeper and deeper into the bedrock. Ice has worked to break up the rock even more. As water in the cracks of the rock freezes, the ice expands to make large and small chunks break away from the cliffs. These two "weathering" forces continue to shape the gorge today.

But how did the stream get here in the first place? Here are the three theories:

One holds that the stream began in a fault. Faults are cracks in the Earth's crust in which rock on one side moves in relation to the other side. On either side of the crack the rock layers no longer line up.