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Archive for the ‘FOTEK’ Category

Embryo Cave, originally uploaded by Mic2006.

JC and I spent the weekend at one of our favorite northerly destinations exploring both Embryo and Twin Trickles caves. Both these caves are seldom visited and if it were not for the initial visit by Marcus and Brad they likely would be entirely forgotten by now.

Both Embryo Cave and Twin Trickles are marble caves at the edge of the Canadian Shield (near Toronto Canada), but they are very different in character.

Much as you might imagine, Embryo Cave is a cave that is smooth inside, easily traversed, the long borehole crawl being in soft silt, while Twin trickles is a cave in which you shred your knees, cave suit and anything else on or around you. The rock in Twin Trickles is sharp and jagged, the cave dips quickly downward through jagged portals and though the marble is beautifully banded there is more a feeling of intimidation in this cavity, it varies between tight and spacious, dry and soaking wet, jagged and more jagged, with lots and lots of black flies – see video on Embryo Cave here.

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Karst geography near Toronto – a likely spot for caves

To be successful as a cave hunter, that is a person who searches the countryside for caves, you must combine a variety of skills. In particular, by experience, the mind now tips me off to areas that are likely cave locations. A sound knowledge of sedimentary geology is helpful, understanding a little about physical geography will certainly add to your success, and most importantly, cave geography really tips the scales. In Ontario it helps to understand something about how glaciers influenced the landscape and of course the human interaction on top of that – in particular the tendencies of farmers over the last 150 years and their preference for plugging openings in their fields with coils of wire and other household debris.

Jeff and I went out searching this past weekend and we found a likely cave location on this area of land above a valley. Thus far researchers have visited and dye traced the most obvious spring out to a resurgence in the side of the nearby valley. We followed along and tried to intercept a possible tunnel entrance. It seems to be that in some cases tunnels get bigger deeper in. In this case we found a large soil pipe that had the sound of rushing water flowing beneath its clayish plug.

See the video here to learn more about how we search for caves in Ontario.

The above picture is a spot near where we found our promising soil pipes – it is a blind valley where a small stream disappears under ground.

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Descending a pit is a somewhat awe inspiring experience, especially if that pit has never been descended before. This particular area of Ontario is absolutely pocked with holes and solution shafts through the rock and this past weekend we found another cluster somewhere near the cave that we call the Death Bell.

See video on the descent of the pit – here

When I got to the bottom of the pit I discovered that I was standing on a boulder choke and beneath that choke you could see a shaft that dropped down at least another 30 or 40 feet. Any dig of the boulder choke would have to be done very carefully as there is the hazard of engulfment where the floor could collapse away and you would find yourself tumbling down amongst hundreds of tons of rock. Bottom line – diggers would have to be roped off.

The size of this shaft is out of all proportion to the water that presently drains into it so I would imagine that it is a relic from the glacial past – in fact the clusters of shafts in the area are generally aligned along some prominent joint and there is little that would explain why they had formed there. Without surface wear marks that would suggest a river that had drained into the shaft the only other thought that I am having is that the shafts formed beneath a glacier with an enormous pressure head that injected water deep along the bedding planes – kind of similar to the formative process of Museum or Leopard Frog Cave.

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We descended by cable ladder into the cave that we call the Death Bell. That morning we had no idea what we would find. My greatest fear was rattle snakes. I have come across the Massasagua rattle snake in caves before, but being in Ontario, we are fortunate that the Massasagua is the only poisonous snake.

We cleared loose rock from the lip of the shaft and Greg joked that it was like an episode from the X – Files where Skully and Mulder found the black slime alien in a cave much like this one.

See video on the Death Bell here.

As we followed into the cavern – down the swinging ladder it soon became apparent that this shaft was like no other that we had visited. You step off the ladder onto a boulder that is perched atop a 10 foot high mound of bones. Some of the bones were those of animals likely thrown in, along with some garbage from a nearby farm, but by the size of the mound you would imagine that it would have taken thousands of years to grow and depending upon the initial depth of the shaft, the pile might go down well beneath ten feet.

A tunnel led off at the deepest point, following downward along a joint. I crunched through a sediment of tiny black nuggets similar in appearance to charred rice. A puff of wind blew from the terminal pinch-point. Possibly the tunnel goes onward, but it has been blocked by the crunchy fill-in. I believe it must be the casings of a thousand years of maggots that have feasted on the ever-growing heap of corpses from fallen animals.

I am optimistic that this is a solution cave as opposed to a sea cave. Sea caves in Ontario; Rover Cave or Grieg’s Caves for example are generally wide mouthed and narrowing like a funnel. This cave seems to have no surface connection but the porthole in it’s roof, and that hardly provides a suitable portal for erosion.

Whatever the case, an animal that falls in to the Death Bell is doomed to a slow and lingering death – there’s no way out. And for a human, much the same without a ladder.

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Cave shaft – Canada, originally uploaded by Mic2006.

In the same area where we discovered the Tooth Tube, a cave that we have been clearing of a glacial plug of clay, we have also found numerous deep shafts, aligned along joints they tend to be deep and narrow with fluted sides and moss around their upper lips. To a caver, a cave shaft is generally indicative of something that might be occuring lower down. Often, but not always, the shaft represents the dominant passage of water as it drops beneath the surface, and as Marcus Buck had pointed out in the excavation of the ‘Birth Canal’ at Olmstead in the Eramosa Karst, “Usually if you follow where the water goes, it takes you on to tunnels”.

This particular field of shafts and pits is in an area that is not too far north of Toronto, Ontario , Canada. For a Torontonian I believe it is one of the coolest things to do near Toronto.

The shafts that we found occur in a plateau that sits well above a large body of water and though the local water table is sometimes known to be perched, it would appear that by looking down into some of these holes, it must still be way below the surface. Many of the more slender shafts appear to be relatively debris-free. Wider shafts tend to be clogged with soil and leaves and logs. They can approach a diameter of about 10 feet in width and we speculate that like in the St. Edmunds System, water may have entered the underground at a time when the area was beneath a kilometer thick sheet of ice. As the pressure head built up, the water beneath the glacier was forced down tiny crevices, down to the bedding plane, and then out at the base of the plateau. Most of these shafts are at the bottom of a conical depression of between 10 and 25 feet in depth. In an old manuscript Martin Davis mentions a stream that he had dye traced that seems to take most of the surface water from this area and drains it out at a single point in the cliffs around the edges of the plateau.

Strings of shafts line up along the general orientation of local joints and we intend to plumb the depths of one such shaft this weekend. Our best case scenario is to find an open cave tunnel that requires minimal digging to clear it. I dropped a bolder down one deep shaft where I could not see the bottom and after an impressive pause I heard the muted ‘thunk’ of tin that had been pounded by my falling missile.

In one relatively shallow shaft we have found a crevice that seems to drop down into a water worn passage beneath, that will be our first priority. It was hard to get a good look at the passage as the crevice above still requires some cleaning, but I had the distinct impression it was human sized and floored with cobbles like we found in the Wasteland Waterway – still to be pushed to its endpoint.

For a final look at where we got with our excavation on the Tooth Tube – Click for cave video of the Tooth Tube here.

Check out the shaft at C-H sink, it is also in an area where sinks dimple local fields. Check out a short video of the C – H sink here

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Death brings life underground, originally uploaded by Mic2006.

It would seem that one night in the middle of one of those incredible storms that blow off the lake, one hapless creature stumbled over this narrow crevice in the grass and slid down to become wedged between the back and the front of it’s skull; it was as good as dead the instant that it disappeared beneath the surface. There was no returning from the crack and as it’s head became wedged the creature would have hung for days before it died of suffocation, hypothermia or thirst.

Now moss is starting to grow on the skull and the remainder of it’s bones are likely scattered beneath it. Next time I visit the area I am bringing a hook to try and retrieve the skull. This is by no means a rare sight in caves and cavities beneath the rock of Ontario,, especially in systems with precipitous entrances, like shelburne, G-Lake and a new cave that we’ve just found this past weekend.

to see the video on this macabre find click here … ‘video – Death brings Life Underground’

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This was our third weekend of digging in the cave we call The Toothtube. We suspected that there was a tunnel entrance in a blind valley and in digging in a likely spot this tunnel was broken open. Glacial clay filled the sealed passages to within about a foot of the roof, but with bucket and garden claw we persevered.

Admittedly its nice to open up a passage but our real goal is to intercept the main branch tunnels that we know must lie beneath. It only stands to reason that there must be some huge underground rivers in this area, all the features point in that direction – in particular some impressive shafts that are partly filled with soil, the lack of surface resurgences, the thickness of the local bedding planes and other nearby tunnel systems that stretch beyond the ability of humans to explore them. This lower level if dug out might provide an eventual connection to this main trunk drain.

See the video on today’s efforts and the downward sloping conduit that we found – video for Ontario cave passage here.

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FOTEK Dinner and Dance, originally uploaded by Mic2006.

Tucked away in the back of Michaelangelo’s plush event room is the dinner table of several Ontario cavers. The event was FOTEK’s annual dinner and dance fundraiser 2012. There were at least 400 people present. After dinner conversation was punctuated by various speechs from politicians and the raffling of a print of Josh Tiessen’s, ‘Guardian of the Karst’ painting. Josh is a member of FOTEK – Friends of the Eramosa Karst’. Our table won 5 of the 20 door prizes. It felt like the odds were in our favor, so it was especially hard to accept our loss of that wonderful painting to a non-caving guest.

Dinner was either beef or chicken, roasted potatoes pasta to start and steamed vegetables – money well spent for both the cause and the company. Moving around the table left to right, myself, Jeff Collens (my regular caving partner), Steve Worthington and Marcus Buck (co-authors of the report – Earth Sciences Inventory and evaluation of the Eramosa Karst Area of Natural Scientific Interest), Marcus’s wife Norma, two ladies who I had not met, and Nina. People who were present but not in the picture were Greg Warchol – schmoozing with some local dignitaries and my wife Maggie who took the picture.

It was Greg Warchol who had first investigated the Eramosa karst area and exposed the significance and possible loss of valuable Niagara escarpment features to the caving community – in particular Marcus Buck, and it was Marcus (who had been the key-note speaker at last year’s event) in co-operation with Steve Worthington who had undertaken all the scientific study to legitimize the Eramosa Karst’s value as an area of natural scientific interest – thus preserved from the impending developments. Derek Ford, a world renown cave scientist from McMaster University had supported the project in saying that the Eramosa Karst was one of the gems of the Niagara Escarpment.

Of greatest interest to cavers are the features of Nexus and Potruff Cave. Unbeknown to everyone in the the room (with the exception of our table) is the incredible occurrence of another similar caving feature within about a 15 minute drive of the Michaelangelo’s Conference room. Jeff and I had discovered the cave last spring and since then we have made several forays into the tunnels. we call the feature Wasteland Waterway and in response to our request to Marcus to accompany us in the near future on a mapping expedition Norma said, “he’ll have to bring his walker.” (there’s a story to be told on that). Anyway, the point is, there’s a lot more in Ontario than people might imagine – especially around the Hamilton area, my book Caving in Ontario; Exploring Buried Karst speaks of the province’s undiscovered and yet exciting caving potential.

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