EGU Blogs

Photo of the Week

Geology Photo of the Week #9 – Oct 21-27

Check out this wicked awesome rock!!

This awesome formation is aptly known as “Split Apple Rock”. It is probably one of the more unique rock formations that I have seen. It is located in Abel Tasman National Park in New Zealand’s South Island. As the with the Pancake Rocks post a few weeks ago I was in the area for a conference and was touring around afterwards. Split Apple Rock is composed of granite.

The theory on its formation is an interesting one. From what I have been able to discover online, which is very limited,  the consensus is that this formation had a glacial origin and that it formed due to freeze-thaw fracturing, although I am not sure that this fully explains it. I realize that this area was glaciated, however, I would think erosion by sea spray on an already existing fracture could make something like this too. If you know more about this rock please comment or simply state your opinion!! Meanwhile, enjoy the pictures.

Cheers,

Matt

Geology Photo of the Week #8 – Oct 14-20 – Guessing Game!

This weeks photo is a giant bone! I leave it to you to surmise which creature it belongs to….I hope you accept the challenge. Please post your guesses in the comment section below. If no one gets it within the first few hours I’ll start posting hints about the creature. You can click on the photo to enlarge it. Have fun!

Hint 1: This bone was discovered in the Yukon Territory and is housed at the Yukon Archaeological and Palaeontological Survey, which is where I took the photo. Their facility houses all of the bones found in the Yukon as well as all of the archaeological artefacts.

Well, the mystery has been solved.  Congrats to everyone who provided the answer on Twitter as well.

The answer that you have all been waiting for is Wooly Mammoth (Mammuthus primigenius). Yep, this is a bone from a mammoth and it is all of a metre long!! Absolutely massive!

Here are some other pictures of mammoth remains that I snagged from the collection and the local museum.

A complete and gorgeous mammoth skeleton at the Beringia Centre in Whitehorse.

A tusk at the survey.

A newly discovered tusk that just arrived at the survey and had yet to be catalogued.

 Cheers,

Matt

Geology Photo of the Week #7 – Oct 7-13

Sorry this post is a bit late…the Thanksgiving holiday was Monday, class this morning and then hockey! Anyway,  for the 7th edition of Photo of the Week we travel to the Pancake Rocks, in Punakaiki on the west coast of New Zealand’s South Island. I was there in 2011 for a conference in Wellington and went travelling around afterwards.  One of my stops was here. The Pancake Rocks are made of 30 million year old limestone that is very finely laminated. The daily pounding of the surf has led to the amazing convoluted structures in the picture. As to the formation of the Pancake Rocks themselves I cannot find a definitive answer…some sources claim that they are interbedded lime mud and coarser material. Others state that they contain stylolites. Unfortunately, I don’t remember from my own visit which is the case…although I feel like I would remember if it were stylolites so I am inclined to believe the bedding view. Plus the beds seem too regularly spaced for stylolites.  Does anyone else have a definitive answer?

Thanks for reading and let me know which hypothesis you support for the formation of the bedding.

Cheers,

Matt

Geology Photo of the Week #6 – Sept 30 – Oct 5

This is my first official post, besides the welcome post, at GeoSphere – EGU edition. It seems fitting to begin with a post that is part of a continuing series from my old home and is bridging the way to my new one.  The photo of the week, while still only six weeks old, is and will stay a regular fixture on my blog. The photo for this week is of some fantastic glacial striations in glacially polished marble located in Cantley, Quebec, which is about a 40 minute drive from Ottawa and is one of the most popular field trip sites for students from uOttawa.

Glacial striations are an interesting feature. They are pretty much ubiquitous across Canada, but rarely are they so defined as they are in Cantley. Striations form from the abrading action of rocks and sediment particles embedded in the base of a glacier. As the glacier slides across the bedrock it scrapes these sediments along the rock below making these striations. In order to form a striation the glacier must be sliding, which only occurs when there is a little water at the bed-glacier interface to lubricate things. Furthermore, if you look at striations under high magnification you can see that the sliding is discontinuous. In fact, it is a series of perfectly aligned slips of only a millimetre or two that are connected to form a perfectly straight groove up to several metres long. Another great feature about striations is that they can tell us the orientation of glacial movement. Indeed, the parallel lines in the rock below point the way to glacier was flowing. However, it is very difficult to tell the glacial flow direction from a striation since the glacier could have been flowing in either direction to make a straight line. In Ottawa we know from numerous other glacial features that the Laurentide Ice Sheet was flowing roughly from north to south. During the Pleistocene epoch, about 10,000 years ago, glaciers were covering pretty much all of Canada as well as most of Europe. The ice sheet at Cantley was ~2km thick.

Glacial striations at Cantley Quarry, Cantley, Quebec. Click for a larger image. (Photo: Matt Herod)

Thanks for reading!

Matt