[1] Much of the Pachaug Trail is flat or has gradual ascents and descents and is suitable for casual walking or hiking, running – or snowshoeing in the winter.

The Quinebaug Trail crosses streams and wetland areas that are subject to flooding in periods of significant rain and snow melt.

The trail diverge west of the Flat Rock "summit", with the Quinebaug Trail turning to the north to closely follow the western banks of Lockes Meadow Pond before veering north-west to its northern terminus on Spaulding road north of Dow Road in Plainfield Connecticut.

The Pachaug Trail passes through land located within the following Connecticut municipalities, from south to north: Griswold, Voluntown and Plainfield The Landscape in the area is generally low-lying and flat with some rolling hills.

Pachaug State Forest features large extents of undeveloped land, consisting of mature growths of hardwood and evergreens, along with swampy areas having extensive coverage by Mountain Laurel and other shrubs and smaller trees.

The foundations for stone cellars that can be found along the route indicate that much of the landscape was used for settlements and farms up until the late nineteenth and early twentieth century, after which much of the land was allowed to return to forests.

The land was remote and difficult to farm and many of the original settlements were subsequently abandoned, so stone walls and foundations can be found throughout the forest today.

[2] There are several unsubstantiated legends and ghost stories which surround the Hell Hollow area including a false claim of witchcraft involving a young girl named Maud Reynolds who died before her second birthday in 1890.

Trail descriptions are available from a number of commercial and non-commercial sources, and a complete guidebook is published by the Connecticut Forest and Park Association.

Encounter with small wildlife is always possible and hikers should be alert to signs of erratic behavior or other disease symptoms and take evasive action if warranted.

There are sections filled with stones and other evidence of erosion which has occurred when the trail has turned into a temporary stream.