On the second day of the Bancroft Trip, we started out (once again) in the greenschist facies of the metamorphic pressure-temperature diagram:

Figure from http://serc.carleton.edu/research_education/equilibria/classicalthermobarometry.html

Our first stop was at a great outcrop of massive amygdyloidal metabasalt. This stuff was chock full of amygdules (former vesicles filled by minerals), and all of them were full of lovely green epidote and chlorite (which are diagnostic of the fairly low-grade metamorphic facies).

Amygdyloidal metabasalt in a roadcut on Blairton Road (48)?

Amygdules in the metabasalt

More amygdules

Some offset veins of (mostly) epidote on the east side of the roadcut

We didn't just see epidote and chlorite - there were also some pretty crystals of what appeared to be pyrite encrusting the fractured surfaces of the outcrop.

Our next stop was back on ON-7, about 16 km east of Marmora. Here we could see something very different: inclined surfaces on very shiny rocks with a pronounced slaty cleavage. But that wasn’t the only neat thing about this outcrop; there was also something interesting on top of those rocks.

The right hand of god commands your attention!

Pretty spiffy contact, right?

Here, you can actually see a contact surface where bits of the underlying phyllite have been incorporated into the overlying conglomerate with the quartz clasts. There may be some time missing here, but probably not as much as the previous day’s outcrop. We’re still in the greenschist facies here.

Beautiful plumose structures in the phyllite.

But we didn’t stay there for long! The next stop (about 5 km east of ON-62 on ON-7) was actually suggested by a Canadian university group that we met at the phyllite stop. They called it the “pink marble” roadcut, and as you can see, it certainly was quite pink.

Lots of drill holes here, but it was still a striking rock face. The whole thing is about 5 meters high.

Admiring the pinkness

Up close, it looks like marble. Most of the outcrop is composed of calcite, in bands of grey and pink; there are even some little folds in there.

Folds!

More folds

Farther to the east, there’s a big section that must have been hydrothermally altered at some point; it’s really cruddy, rusty rock. There was lots of staining here, and pyrite encrusting everything.

Very 'stewed' rocks

But if you look carefully at the more pristine parts of the roadcut, there are some tell-tale minerals that let us know this is more than just marble – it’s probably a skarn. Why? Because it has garnets!

Grossular garnet (the black specks)

Same garnets, a little closer (yes, I know I'm cheating and there's no scale in this one)

Garnets are a common mineral in skarn, and these are probably either grossular garnet (Ca₃Al₂(SiO₄)₃) or andradite (Ca₃Fe₂(SiO₄)₃) – exactly what you’d expect to find in a calcium- and silica-rich setting. And because there are garnets here, we’ve moved out of the greenschist faces and into the amphibolite faces.

Next up: more outcrops in the amphibolite facies!