Photo © Ian Coristine/1000IslandsPhotoArt.com
 You are here:  Back Issues      Archive      Nature Search   

Thousand Islands Rocks


For many of us the beauty and uniqueness of the Thousand Islands is without question. And yet we may know little of their origin. How were they formed? How long have they been here? The beauty that we see is a product of over a billion years of geologic activity. Eons of mountain building, erosion, and glacial activity have resulted in the islands as we see them today.

Thousand Islands, Photo by Chris Murray
The Thousand Islands, part of the Frontenac Arch  
Chris Murray © 2010

The Thousand Islands are a relatively recent geological feature carved from very ancient rock. The Islands as we know them were created at the end of the last Ice Age, approximately 10,000 years ago. However, the rock of which they are comprised is some of the oldest rock on earth, dating back to 1.1 billion years old. The pinkish hued Precambrian gneiss (pronounced “nice”) we see throughout the region is an extension of the vast Canadian Shield, a massive body of solid rock that forms the nucleus of the North American continent. The Thousand Islands portion of the Shield is known as the Frontenac Arch and connects the main body of the Canadian Shield to the west with the Adirondack Mountains to the east. It is interesting to note that the Adirondacks were also born of the same geologic forces that shaped the Thousand Islands.

The Islands are actually the roots of an ancient mountain system that has been uplifted and eroded through the millennia. The dominant rock type that we associate with the islands is a combination of Precambrian granite gneiss and quartzite, both metamorphic rocks. Potsdam Sandstone is also prevalent throughout the area, particularly along the flanks of the Frontenac Arch.

Frontenac Arch
Map of the Frontenac Arch, connecting the Canadian Shield with the Adirondack Mountains

 

The Potsdam Sandstone was deposited in a shallow sea and is much younger than the granite gneiss, roughly half its age at 500 million years old. While imperceptible to us, the uplift of the arch is responsible for the erosional stripping of the younger sedimentary rock such as the Potsdam and the exposure of the Precambrian gneiss. There is an interesting road cut a few miles east of Alexandria Bay along Route 12. It is an example of an unconformity, which is a gap in time between two rock types caused by erosion or non-deposition of sediment. Here the 500 million year old Potsdam Sandstone lies unconformably on top of the 1.1 billion year old granite gneiss, a gap in time of 600 million years11!

Potsdam Sandstone, photo by Chris Murray © 2010
Unconformity (indicated by red line) between the Potsdam Sandstone and underlying Precambrian gneiss.
Chris Murray © 2010

While the rock is ancient the Islands themselves are a product of the end of the last Ice Age. The glacial ice sheet covered this region with ice miles thick, advancing and retreating on numerous occasions. The St. Lawrence River occupies an ancient geologic depression known as the St. Lawrence Lowlands. Prior to the ice leaving the valley the Great Lakes drained eastward through the Mohawk River Valley in New York. As the glaciers retreated northward into Canada the St. Lawrence Valley was initially filled with seawater. This can be evidenced in the marine fossils that have been discovered in the Thousand Island Region. However, as the land rebounded once the weight of the ice was removed the marine incursion diminished and the Great Lakes then began to drain via the St. Lawrence River. A thousand hilltops, the roots of ancient mountains, became the Thousand Islands in this flooded landscape.

Precabrian, photo by Chris Murray © 2010
Polished glacial furrow in Precambrian gneiss outside Keewaydin State Park.
Chris Murray © 2010

The islands are elongated parallel to the river, with blunt upstream ends and gentle downstream trailing slopes. Evidence of the glaciers can be seen throughout the region in the form of glacial furrows, glacial erratics, and potholes. A glacial pothole is a semi cylindrical hole gouged out of the bedrock by the scouring action of rocks and pebbles in the floodwaters of retreating glaciers. The best known (and largest) example of a pothole in the Islands is Half Moon Bay on Bostwick Island. Several smaller examples of potholes can be seen along the Eel Bay Trail portion of the Minna Anthony Nature Center on Wellesley Island. An example of a glacial furrow can be found in the road cut on Route 12 just outside of Keewaydin State Park. Here the bedrock of Precambrian gneiss has been scoured and polished by boulders at the bottom of the glaciers. Glacial erratics are boulders from elsewhere that were carried by the ice and then dumped as the glaciers melted. These can be found throughout the region.

 

Glacieal Erratic, Chris Murray © 2010
Glacial erratic
Chris Murray © 2010

By Chris Murray

Chris Murray has been practicing landscape photography for fifteen years.  During that time he has also worked as a geologist, earning his B.S. in geology from SUNY Plattsburgh and his Ph.D. from the University of South Carolina.  He continues to work part time as a geological consultant, devoting the rest of his time to his photography.

Chris’ interest in photographing landscapes is derived mainly from his love of the natural world, the same love that led him to choose geology as a profession. [In June 2010, TI Life featured Chris in: Chris Murray's Photoraphy]. 

For Chris, the appeal of photography lies in the blending of the technical and the artistic.  As a scientist, he is naturally drawn to the technical aspects of photography: decisions regarding filters, shutter speed, aperture, and so on. The skills he has learned as a scientist, the attention to detail and careful observation, have also helped him immensely as an artist.

Chris Murray resides in Syracuse, NY.  You can find him online at Chris Murray Photography 

1

Bradford B. Van Diver, Roadside Geology of New York, (Mountain Press Publishing Company), 295.

Posted in: Nature
Print this story
Please feel free to leave comments about this article using the form below. Comments are moderated and we do not accept comments that contain links. As per our privacy policy, your email address will not be shared and is inaccessible even to us. For general comments, please email the editor.

Comments

Alan Medcalf
Comment by: Alan Medcalf ( )
Left at: 11:18 AM Saturday, January 15, 2011
Great article. I've long been fascinated by Canada's geologic roots and history. Since moving here from SW Ontario a couple of years ago, I've been learning more about the 1000 Islands region.

In this article, the third sentence reads, "However, the rock of which they are comprised is some of the oldest rock on earth, dating back to 1.1 million years old." I believe this is a typo ... the Grenville foundation here is 1.1 billion years old!
...alan
Susie Smith
Comment by: Susie Smith
Left at: 11:23 AM Saturday, January 15, 2011
Whoops... my mistake. Thanks Alan. And I apologize to Chris Murray too. (I just fixed this).

Susan Smith, Editor
Rob Russell
Comment by: Rob Russell ( )
Left at: 9:18 AM Wednesday, January 19, 2011
Thanks for a great article. I have been curious about the geology of the region for many years and never knew where to start.

Count on a Plattsburgh alum to open doors to more knowledge.

Suny Plattsburgh Class of '86
Alan Medcalf
Comment by: Alan Medcalf ( )
Left at: 11:07 AM Wednesday, January 19, 2011
@Rob - I too had some difficulty in finding info on the geology of this region but have come across a few things you might be interested in.

The first is a soft-cover geology text called "Ontario Rocks" by Nick Eyles, available from Amazon.com. For a broader view, also see "Canada Rocks" co-authored by Nick Eyles and Andrew Miall. While both of these focus on the eponymous regions, they do provide a broader view.

Next, for the past few years, a volunteer group has done a "geo-tour" of the 1000 Islands, and I have the guide booklets from those tours. If you contact me by e-mail at alan(at)medcalf(dot)ca and you've got email capacity to receive large pdf files (9 Mb total), I'll send them to you.
...alan
Chris Murray
Comment by: Chris Murray ( )
Left at: 7:14 AM Thursday, January 20, 2011
Thank you Rob and Alan. Another good source (and interesting read if you are a NYS resident) is Roadside Geology of New York. It was written by a SUNY Potsdam geology professor. He does an excellent job of explaining things in layman terms.
Catharine Van Sickle
Comment by: Catharine Van Sickle ( )
Left at: 6:33 AM Saturday, January 29, 2011
We are most fortunate to have this information available .A lot to digest all of great interest Thank you for it.
Alan Medcalf
Comment by: Alan Medcalf ( )
Left at: 9:27 AM Thursday, April 28, 2011
If anyone's still watching this commentary, here's yet another easily-digestible source of geologic information: http://www.rideau-info.com/canal/history/geology.html
Cheers,
...alan
Anonymous User
Comment by: Anonymous User
Left at: 12:03 PM Wednesday, September 25, 2013
http://misterwilkinson.wordpress.com/2013/09/25/the-st-lawrence-lowlands/
Anonymous User
Comment by: Anonymous User
Left at: 12:03 PM Wednesday, September 25, 2013
http://misterwilkinson.wordpress.com/2013/09/25/the-st-lawrence-lowlands/
Anonymous User
Comment by: Anonymous User
Left at: 12:04 PM Wednesday, September 25, 2013
http://misterwilkinson.wordpress.com/2013/09/25/the-st-lawrence-lowlands/
Frances
Comment by: Frances
Left at: 1:40 AM Monday, May 29, 2017
Very interesting information, thank you for the lovely photos.

Post Comment

Name (required)

Email (required)