Cortland-Onondaga Federation of Kettle Lake Associations, Inc.

Feral Swine in Cortland and Onondaga Counties - articleFeral_Swine_for_newsletter.pdf
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Andrew Brainard's Presentation to C-OFOKLA, August, 2012
Read our Comments to the NYS Department of Environmental Conservation
regarding the proposed regulations for 
Liquefied Natural Gas Facilities
- Public comment period ending Dec. 4, 2013

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 Diet for a Small Lake
Available for Purchase by downloading this Order Form

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Click on the link to Read 
My Poor Little Lake

by Scott Kishbaugh and Karen Stainbrook

A great article from the New York State Conservationist, April 2014, 
about Chauttauqua Lake and harmful algal blooms.


The 31st NYSFOLA Annual Conference
"Celebrating Lake Stewardship"

May 2-4, 2014
at White Eagle Conference Center in Hamilton, NY

It's not too late to sign-up!
For more information, and to register on-line, go to:


Read what the Tully Newsletter had to say about
our C-OFOKLA Event, Water Travels, with David O. Brown.


What is a Kettle Lake?
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 

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