Conservationists from the ‘Friends of the Eramosa Karst’ and cavers from the ‘Toronto cave Group’ have joined together over these last three weekends (Nov – Dec 2012) to hopefully expose the tunnels that all suspect lie beneath the clogged entrance of Kinney Cave. Three weeks ago this karst feature was no more than a pile of glacially rounded boulders stacked at the edge of a walking path, now there is exposed entryway into the underground.
Vern, a local resident had first bought this spot to the attention of Brad, president of Friends of the Eramosa Karst. Vern could recall playing in this spot as a child, the hole was supposedly infested with Copper Heads and rattlers. Some time between then and now the cave had been filled in with enormous field-stone boulders. That is the norm in Ontario – farmers fill openings to the underground with rocks.
Anyway this dig has been an epic event, a collaboration between the Toronto Cave Group and the Hamilton based ‘Friends of the Eramosa Karst’. Both have come together in appreciation of what nature has given the area and to preserve for future generations what some obviously fail to see today. For the most part the conservationists are not cavers, but they can understand the idea of preserving something for its own sake. I could hear them talking about the highlights of the area, a stream flooded to the edges of its banks, trees swaying in the mist, dewdrops on bare branches, and various small creatures that they have proudly kept a habitat for – priceless.
This tunnel dig, as was pointed out, is returning the environment to what it was before farming and developers – and for me, I have this curiosity to know whats under there.
Today we dug downward and along a tunnel just beneath the surface. I struggled enormously with some of the huge flaked off pieces of rock, and moving them to the surface was exhausting. Jeff Collens spent his time deepening the entry shaft and in retrospect my time would have been better spent helping him. We all suspect a tunnel down at the bottom of the pit. There is said to be at least 30 feet of elevation between this sink point and its resurgence a few hundred meters away. Marcus explained how the water that sinks here and the water that sinks at another nearby stream cross paths, obviously at different levels – resurging in places that seem to make no sense.
See the video for the dig at the Eramosa Karst (Dec 2012) here
In comparing this entrance (Kinney Cave) to one that I had helped excavate at the initial clearing of the Eramosa Karst, they are very similar. Over a decade ago we began our investigation of the area at a place we called the Olmstead Caves. In a shaft much like this that we called ‘The Birth Canal’ I dug all day and the bottom finally dropped away with a distinct inward sucking of air and there beneath was a crawlway that led on to a chamber beyond. I made it as far as the chamber, but Nina Mueller and Marcus Buck (and maybe others of a slimmer build than myself) actually pushed the tunnel system way further, wiggling beneath rock flakes that are precariously wedged in muddy tubes way beneath the ground.
There is so much in this area, sinkholes everywhere that are rapidly being buried and secreted away by development interests. Jeff and I are still to explore the further reaches of our epic Wasteland Waterway discovery – it is in a similar geological setting and we often worry that in not making its whereabouts known to preservationists we might be jeopardizing its existence. Its a tricky situation and we are hope to resolve it eventually with the good advice of those who care about this kind of thing – the caving and preservation communities.
For more information on caving in Ontario, buy my book, “Caving in Ontario; Exploring buried Karst”. There is a link on the side of this page that connects to “Lulu” where the book can be purchased.
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Cave Shaft at Twin Trickles – exploring rocks and minerals from within (Bancroft), originally uploaded by Mic2006.
