JOCKO RIVER SPRING STRUCTURE

JOCKO RIVER SPRING STRUCTURE

by: Charles O’Dale

  • Type: Simple
  • Location: N 46° 33’ 15″ W 79°17’ 13″
  • Age: <12,000 Yearsa
  • Diameter: >0.2 km

a The structure appears to be created in the glacial remains of the Late Wisconsin North American glacial episode, 25,000–12,000 years ago.

The red dot indicates the position of the Jocko River spring structure within the Jocko Rivers Provincial Park system. It is illustrated here in close proximity to the Brent meteorite crater (highlighted by the circle) in this Landsat image.
The Jocko River spring is a 0.2 km diameter circular structure surrounded by a prominent raised rim. In the early ’60s, my father and I went trout fishing in this area. While we were fishing in the “crater”, my father casually mentioned that this roundish lake kind of looks like a meteorite crater. Hmmm, that got me thinking…… (courtesy Google)
From my vantage point in GOZooM, I took this image of the Jocko River spring looking south west. The “X” illustrates the point on the shore where I will be standing with with my “rockhound” companion Joya (illustrated in an image below). My father and I paddled our canoe into this lake 52 years before this image. The trout were “yummy” !!
The Jocko River spring looking south east. Soundings taken from the lake centre to the entrance documents an underwater crater bowl shape.

Geological Features of Jocko Rivers Provincial Park

The bedrock of Jocko Rivers Provincial Park is within the Tomiko Terrane of the Central Gneiss Belt, in the northwest part of the Ontario Grenville Province. The Mesoproterozoic Tomiko Terrane consists mainly of metamorphosed quartzites and granitic plutons. Most of the park contains clastic siliceous metasediments in the form of arkosic quartz-feldspar gneisses, biotite and hornblende-rich quartz-feldspar gneisses and minor muscovite-quartzfeldspar gneisses. There is gneissic quartz monzonite of the Late Precambrian granitic suite also present within the park. The representation of clastic siliceous metasedimentary gneisses of the Tomiko Terrane is of regional significance (Frey and Duba 2002).

The structure appears to be created in the glacial remains of the Late Wisconsin North American glacial episode, 25,000–12,000 years ago.

The Quaternary geology of the park is Late Wisconsinan in age. The small areas of bedrock uplands along the shorelines have a discontinuous till cover of thin sandy-silty ground moraine (Frey and Duba 2002). (Jocko River, Ontario Parks 2006)

2016 Ground Expedition:

Ground exploration video documentation The interesting parts at- :0, :17, :40, :48, 1:04, 1:09.

The Joko River structure is illustrated at the lower right of this Google image. The “markings” superimposed on this Google image are the position reports from my SPOT Satellite Messenger during our exploration canoe trip.

An initial reconnaissance of the area established that immediately surrounding the structure is a very old dense forest with no trails to follow. In order to reach the clear lake within the structure we would have to haul our canoe kilometres through very dense bush and then down a very steep wall (and back again). Instead we decided to canoe to the crater starting from a crossing of the Jocko River over 6 kilometres to the north.  The starting point (extreme left of the Google image) is >1 metre higher in altitude than our “crater” destination (extreme right in the image) measured by GPS.

Yours truly with my “rock hound” companion “Joya”, taken on the south shore of the structure. Looking over my right shoulder is the position in the sky where I took the aerial image of this structure from GOZooM. The “X” in that aerial image indicates where I am now standing. My father and I paddled our canoe into this lake 52 years before this image. The trout were “yummy” !!
The ~50° slope of the “crater” rim.
I am balancing half way up the “crater” rim and holding a birch branch so it freely hangs vertical. Referencing the vertical branch with the one placed on the rim, the angle is ~50°.
This is a typical view of the crater rim from our canoe in the clear lake in the structure. I noticed that it was relatively high and steep all around the lake (with the exception of the lake output into the Jocko River).
The superimposed labels indicate the positions of the documented depth soundings. The lake bottom profile gleaned from these soundings are documented below.
JOCKO RIVER STRUCTURE PROFILE – represents the underwater profile of the clear lake within the structure.
The positions of the sounding points A – D are  illustrated on the Google image above.  The plot on the right documents the structure profile from lake bottom to the top edge of the rim.

We also measured a pH of 7.5 (normal) at the centre of the lake (point A in the above image)

Formation of the Structure (2 hypotheses)

After exploring this structure on foot and by canoe, I put forward these two hypotheses, one of which may be the explanation for the formation of this bowl shaped geological structure:

  • Erosion of the surrounding glacial regolith by the output of fresh-water springs on base of the crater south wall forming a circular gully; or
  • An impact from a cosmic-velocity bolide. Proof would entail either discovery of meteorite fragments around the structure from the original bolide and/or discovery of impact related geology. The Whitecourt Crater is an example of geological evidence for impact confirmation of a small crater of similar geology.

A metal detector search for meteorites around the south rim of the “crater” concluded with a negative result.

Area Geologic Description:

A water parting extending eastward from near the northern boundary of the area separates the Jocko River and Mattawa River drainage basins. Elevations along the water partings generally range from 1,000 to 1,400 feet with local elevations as low as 700 feet and as high as 1,600 feet. Lake Nipissing has an average elevation of 644 feet. Some waterways such as Trout Lake and the Mattawa River probably cover deep, pre-Pleistocene valleys in fault zones. Drainage within the area is controlled by three drainage systems: the Mattawa River system, the Jocko River system, and the Lake Nipissing – French River system. The Mattawa River and Jocko River systems are part of the Ottawa River drainage basin. (Lumbers 1971)

References

Brent Dalrymple, Radiometric Dating Does Work! Reports of the National Center for Science Education

Grieve R.A.F., Robertson P.B., IMPACT STRUCTURES IN CANADAthe Journal of the Royal Astronomical Society of Canada, February 1975

Jocko River

Frey, E. and D. Duba, 2002. P140 Jocko Rivers Provincial Park. (Draft Earth Science Checksheet)

Geological Report 94 Geology of the North Bay Area Districts of Nipissing and Parry Sound S. B. LUMBERS 1971

Northern Ontario Engineering Geology Terrain Study 101 NORTH BAY AREA (NTS31L/SW)Districts of Nipissing and Parry Sound by John F. Gartner

The Ghost of the Jocko River