Canadarago Lake is a lake located in Otsego County, New York and is the source of Oaks Creek. The Village of Richfield Springs is located at the lake's northern end. It is the second largest lake in Otsego County, lying to the west of and parallel to the larger Otsego Lake. The lake's name is also spelled "Candajarago Lake" or "Caniadaraga Lake".

The lake has two islands. One island is known as Deowongo Island. The island's name is said to mean, "Place of Hearing", coming from the Oneida Iroquois nation’s language, and was given to the island because of the echo that was noticeable from that body of land. The island was protected in October 2012 and is currently open for public access. The other island is Loon Island which is a sunken island that disappeared in the early 19th century.

Canadarago Lake

Geography

Canadarago Lake is just over long with a surface area of . Its average depth is , with a maximum depth of . The northern end of the lake is in the Town of Richfield, and the southern end is in the Town of Otsego and bordered by the Town of Exeter on the west. The lake runs from the Village of Richfield Springs at the north end to the community of Schuyler Lake at the south end. The lake has historically also been known as Schuyler Lake, and the community mentioned earlier still bears this name.

Canadarago Lake

Islands

There is a small island near the eastern shore called Deowongo Island. There is a sunken island on Canadarago Lake called Loon Island. This island was less than an acre and stood toward the north end of the lake toward the northwest side, near the Baker’s Beach area.

Canadarago Lake

Adjacent mountains

One mountain near the lake is Nine Hill, which is located on the northwest side of the lake. King Hill is located on the east side of the lake. South of King Hill is Panther Mountain.

History

In 1778, there was an event known as the Andrustown Massacre during the American Revolutionary War near Canadarago Lake. There is a marker south of Hendersonville on the road to the lake known as the “Leatherstocking Trail”, which is a reminder of this massacre.

Until the early part of the 19th century, there was a second island on the lake called Loon Island. Smaller than the island that remains on Canadarago today, Loon Island was only half an acre in size. Its southern shore was marshy, but the northern end of the island (toward Richfield Springs) had trees and vegetation. In 1816..."the year without a summer", there was an early spring thaw and the streams that feed Canadarago were running high. Their water flow covered the lake ice. A north wind blew the ice pack into the southern portion of the lake. Not long after that, there was a hard freeze and the winds shifted from out of the south. The ice pack, larger than before, was sent back in the opposite direction. The saw effect took off the surface soil of the island and took down the trees and vegetation. It has been under water ever since.

In 1872, a small steamboat was launched on the lake as a pleasure craft.

The remaining island on Canadarago was called Deowongo Island (De-O-Won-Go) by the Oneida Indians who lived in the area. The name is said to mean, "Place of Hearing", and was given to the island because of the echo that was noticeable from that body of land. The island was purchased from the State of New York by Daniel Wormer in 1850. Then in 2012 the island was donated by the Schoenlein family to the Otsego Land Trust making it accessible by the public.

In 1902, the Southern New York Railroad, an electric railroad, was opened south of Herkimer and Mohawk to Jordanville, Richfield Springs, Canadarago Lake, Cooperstown and Oneonta. There were two stops along the lake including Canadarago Park and The Lake House. Canadarago Park was located on the east shore about a mile south of The Lake House.

June 2006 saw massive flooding of its banks after record rainfall. Legislation to create a Canadarago Lake District was approved by the New York State Legislature in 2007 but was subsequently vetoed by Governor Eliot Spitzer.

Geology

It is geologically related to the Finger Lakes, as they were both carved by glaciers, but is not counted among them. One difference is that Canadarago Lake is situated at a higher elevation () than the Finger Lakes (approximately ). Another difference is the Finger Lakes are part of the Lake Ontario watershed, and Otsego is part of the Susquehanna River watershed.

Canadarago Lake is a dimictic lake surviving a previous glacial period. The lake is also eutrophic.