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2015 Speaker Series Unveiled

We are pleased to announce our 2015 Speakers Series with three diverse and important topics for residents of the Kettle Lake region and beyond.  All events are free and open to the public, but registration is encouraged to ensure your seat.

March 16th Monday, 7PM – Tully Elementary School

Deer in Urban, Suburban or Rural Environments: The Need for Intensive Commitment

Guest Speaker: Justin Gansowski is a Wildlife Disease Biologist  USDA, APHIS, Wildlife Services.
Get your free tickets now!

April 27 th  Monday-  7:00 PM – Tully High School

Transforming NYS to a Fossil Fuel Free Future: Why and How


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Welcome to Our New Site

Welcome to the new home on the web for C-OFOKLA. We hope to continue to provide you with important information on the Kettle Lakes region of Central New York with this updated site as well as continue to expand our educational and community offerings.

Take a few minutes to explore the site and, over the coming weeks, we’ll post some more detailed information about our new

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What is a Kettle Lake?

C-OFOKLA (Click to Enlarge)

C-OFOKLA (Click to Enlarge)

Onondaga and Cortland Counties, are unique and beautiful regions in central New York. One of the defining characteristics is the presence of several kettle-hole or kettle lakes. 

According to the United States Geological Survey (USGS), the area was formed by the advancing and retreating of glacial ice during the last glacial period in North America.  To the west of us, the same glacial process formed the Finger Lakes. The process here, however, caused smaller holes to be formed when huge chunks of ice broke off the glacier. These holes, or “kettles” were then buried by till [1] as the glacier receded. When these ice chunks melted, the depression remained.

Each kettle lake has its own unique properties. Some have natural or created outlets, while others are landlocked. All of these lakes are, however, connected to the surficial aquifer. A surficial aquifer is generally defined by the USGS, as an “unconfined, shallow aquifer system, recharged by rainfall and leakage from surface water bodies.”

The glaciers also formed the Valley Heads Moraine, an area of sand and gravel deposited when the retreating ice paused. The moraine runs east to west and separates the Tully Valley to the north from the Tioughnioga Valley to the south. This moraine also forms the surface water divide for the St. Lawrence River drainage (north) and the Susquehanna River drainage (south).[2]

[1] sediment of various particle sizes deposited by the direct action of ice

[2] Information from USGS