EGU Blogs

Photo of the Week

Geology Photo of the Week #30

The photo for this week was taken in Quebec near the town of Thetford. These are a really beautiful example of pillow basalts. Pillow basalts form during underwater volcanic eruptions and have the unusual quality of appearing bulbous and rounded. The ones pictured below have had their tops shorn off and are therefore visible in plane view. e.g. You’re looking down at them from above after they have had the tops cut off. As I mentioned above these particular pillows are located in Thetford Mines, which is a mining town (obviously). The principle commodity of Thetford Mines is the extremely dangerous and controversial mineral asbestos.

Here is a fantastic video showing pillow basalts forming today.

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Cheers,

Matt

 

Geology Photo of the Week #29

The photo this week is of another self collected beauty. I collected this piece below at the Marmoraton Iron Mine in Marmora, Ontario a few years ago. When I found it none of the garnet crystals you see were visible. They were all covered by a thick layer of calcite. I could just make out the edge of a broken crystal at the side. However, I have been collecting at Marmora a lot and I knew that this had the possibility to turn out beautifully since at this quarry calcite often hides terrific and undamaged crystals below. You can still make out a little bit of it here and there (it is yellowish white). The key is to just get rid of it. Luckily, for me and many other collectors of Marmora minerals calcite dissolves easily in hydrochloric acid. So cleaning a find like this becomes a simple matter of placing it in a basin of HCl and waiting for the magic (chemistry)  to happen. After a few days, and a few changes of the acid the result is what you see pictured below: a beautiful cluster of 1-1.5cm grossular garnet crystals, with some magnetite veins, minor epidote and left over calcite.

(Photo: Matt Herod)

 Unfortunately, the garnet crystals of Marmora are not gem quality or anywhere near it, but they do form very attractive crystals of which I have a large, large number after years of collecting there. Marmora is also a great place to collect epidote, pyrite, calcite, pyrolusite, magentite, ilmenite, marcasite and actinolite. All of which are common and relatively easy to find with a bit of work. e.g. sledgehammering.

The quarry is larger than the town of Marmora!

Cheers,

Matt

p.s. Watch this space for EGU2013 updates starting tomorrow!! I’m really looking forward to the Fukushima press conference.

Geology Photo of the Week #28

Happy April Fools/Easter everyone! I know that I am a day late, but yesterday was a holiday in Canada. Spring is also in the air, not today actually since it is -7 currently, but we have no more snow, and we had a few nice days over the Easter weekend. It is therefore appropriate for the photo of the week to be something eggy.

A piece of Pleistocene emu egg shell. Found near an ancient aboriginal campground in South Australia. (Photo: Matt Herod)

This photo is of a fragment of Pleistocene age emu egg shell that was found in Port Augusta, South Australia.

Bonus Photo: The duck-billed platypus, a monotreme and one only two types of egg laying mammal in the world.

Platypus (Photo: Matt Herod)

Cheers,

Matt

Photo of the Week #27 – Someone’s had a few too many

The photo of the week came to me this morning on my walk to school. Yes, it is now warm enough in Ottawa to comfortably walk to school! All the melting ice and the slight smell of spring and undergrad panic in the air got me thinking about permafrost degradation and nights out during my undergrad. An odd combination of thoughts, I grant you. Well, what do these two very separate things have in common? Observe the photos below, particularly the trees in the hillside to find out.

(Photo: Matt Herod)

(Photo: Matt Herod)

The trees all look a little askew. This is because they are the epitome of a “drunken forest”. Many of you may not have encountered this amazing term, which I assure you is the real one, for trees that sit on degrading permafrost  or ice wedges that become drunkenly tilted as the ice melts. The ground underneath the tilted trees also looks somewhat heaved which is characteristic of melting permafrost terrain. I took these photos just outside of Dawson city next to ongoing placer mining operations.  So there you have it. The strange explanation for what links the melting of spring ice to memories of my own spring experiences in undergrad (never now…).

Cheers,

Matt