10/06/2024
I ❤️ the Gammon Ferrigunious! I even have a cool shirt that says so.
Today I fell in love with it all over again. It began as a simple journey into the backcountry to examine some outcrops which I had previously identified... but deep in the bush, my GPS signal was bouncing around and I took the wrong fork in the creek... and just as the poem says, taking the path less traveled makes all the difference! Actually there wasn't a path at all. Just thick bush, creeks and then, outcrops!
The first one belonged to the Boyne Member of the Carlile Formation. I'm old friends with the Boyne, but it's too far down section of the Gammon, however just near the top of the outcrop, something looked suspiciously 'gammonous' so rather than turn around and retrace my steps to try and find the correct fork of the creek, I followed my geological nose further into the deep bush, following the logic that since I'm hiking upstream, future outcrops that I might encounter should, in theory, be approaching the formational contact with the Pierre Shale. And my faith in geology proved well placed! As I rounded a sharp bend in this new creek country, suddenly there it was... The Gammon Ferruginous Member of the Pierre Shale, sitting conformably atop the Boyne Member of the Carlile Formation. Textbook style stratigraphy. And there was lateral bentonite seams WITHIN the Gammon! I've only ever encountered thin bentonite (~1-3 cm) in the Upper Unit of the Gammon Ferrigunious and at one other site that I found just last year, where it was on par with that which I discovered today.
As I pressed yet further into the bush, my knack for sniffing out this unique sedimentary layer continued to manifest, as a short distance upstream I found an even larger exposure, with multiple lateral bentonite layers, WITHIN the Gammon.
The literature suggests that the Gammon Ferrigunious has three distinct units: upper, middle, and lower. These were identified from oil wells in the 1970s and 'suggested' from electric logs of the subsurface conducted in 1980, but never identified in outcrop in the Pembina Mountain area until 2010, when I identified it during a Xiphactinus excavation along with some friends at the Manitoba Geological Survey. (Sorry for the lack of references here, I'm just going by memory but you can message me for references if you're interested.)
I've spent countless man-hours in all three units, so I'm extremely familiar with them; in fact I'm the industry field expert on the Gammon Ferrigunious of Manitoba. So that is why I'm pretty excited that these outcrops simply do not match up with any of the three units that I'm familiar with... I've developed an eye for it, the feel for it, the field skills for it, to say with certainty that this outcrop is stratigraphically absolutely the Gammon Ferrigunious Member of the Pierre Shale; but it is also different in it's physical properties than any of the three recognized units that I am familiar with. It's hard for carbonaceous shale! The lateral bentonite layers are new. The Gammon is conformably overlain by the "I" Beds of the Pembina Member. Everything is correct, it's just my field experience talking that this Gammon is somehow physically different from the recognized three units. Yet there it is!
In 14 years of hunting this shale out of the Manitoba Escarpment, just when I thought I had it nailed, ol' Mother Earth is showing me that we're actually just getting started on unraveling the mysteries of this elusive chapter from Prehistoric Manitoba!
As I hiked back to the truck, I kept hearing Yoda's voice in my head saying, "Much to learn, you still have." And learn it, I will. And that is exactly why I do what I do. I'm genuinely curious about this, I want to solve the riddle of whether the Pembina Mountain region of the Manitoba Escarpment actually has four, or more, units of the Gammon? And what are the unique characteristics of these new exposures? The bentonite is also interesting, again this is just field experience talking, not geochemical analysis: this bentonite in the Gammon more closely resembles the bentonite of the underlying Boyne Member of the Carlile Formation, rather than the calcium bentonite of the overlying Pembina Member of the Pierre Shale. As the Gammon and it's bentonite are in fact the basal Member of the Pierre, I would have expected it's bentonite to be more Pembina-esque, as the shale is. But it looks and feels closer to Boyne bentonite. Interesting geological crossover. If we can source the new Gammon bentonite to it's volcanic origin, we may be able to answer some questions of deposition and stratigraphic correlation to other bentonite horizons of the Gammon closer to the type locality in the United States, which in turn would provide us with a view of which part of the larger Gammon sequence across the Great Plains that our little snapshot of geology has captured for us to study along the Manitoba Escarpment.
There was something special about the orange color of ferrigunious shale on a beautiful October day during peak leaf season in Manitoba's Pembina Valley that added to the ambiance of my geological journey.
It was a good day. ⛏️