Connecticut
Cancellation alerts

Devil's Hopyard

We watch every site at Devil's Hopyard 24/7, then email you the moment a cancellation opens up.

40% of weekends booked at top sites·Peak Jul–Sep·21 sites
Set up an alert for Devil's Hopyard

Pick your dates, pick the sites you want, we do the watching.

Park favorites

The 10 most popular campsites at Devil's Hopyard

Ranked by how often each site reserves on weekends in peak season (Jul–Sep). Set up an alert and we'll email you on cancellations.

Site 22

Best here
Ranked #1 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 14

Top pick
Ranked #2 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 01

Top pick
Ranked #3 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 16

Standout
Ranked #4 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 09

Standout
Ranked #5 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 10

Decent
Ranked #6 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 02

Decent
Ranked #7 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 11

Decent
Ranked #8 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 05

Wait for better
Ranked #9 of 21
STANDARD NON ELECTRIC · Sleeps 6

Site 06

Wait for better
Ranked #10 of 21
STANDARD NON ELECTRIC · Sleeps 6

These sites rebook within minutes of being cancelled. Set an alert at Devil's Hopyard and we’ll email you the moment one opens up.

Set up an alert →

About this park

Devil's Hopyard's principle feature, Chapman Falls, drops more than sixty feet over a series of steps in a Scotland Schist stone formation. The water from the splash pool at the base of the falls, continuing as the Eight Mile River, flows through the park's hemlock-canopied picnic area, providing a tranquil setting for a family outing. Many myths surround the name of the park, including one about a man named Dibble, who grew hops for beer-brewing. Through usage, Dibble's Hopyard supposedly became Devil's Hopyard. Another tale says that the Devil passed by the falls and accidentally wet his tail. Furious, he burned holes in the stones with his hooves as he bounded away. Now, we know that the potholes near the falls, which are some of the finest examples of pothole stone formations in this section of the country, were formed by stones moved downstream by the current, trapped in an eddy where the stone was spun around, wearing a depression in the rock. When the rock wore itself down, another would catch in the same hole and enlarge it. Perfectly cylindrical, the potholes range from inches to several feet in diameter and depth.