3 March 2015
Posted by Callan Bentley
At the Spiral Tunnels overlook on the Trans-Canada Highway, you can look at trains.
Or, you can check out some lovely trace fossils in boulders which divide the viewing area from the highway:
These are in the Gog Formation, a Cambrian-aged quartz arenite, mostly fused to quartzite nowadays…
I know which subject I would choose to spend my time looking at…
Callan Bentley is Associate Professor of Geology at Piedmont Virginia Community College in Charlottesville, Virginia. He is a Fellow of the Geological Society of America. For his work on this blog, the National Association of Geoscience Teachers recognized him with the James Shea Award. He has also won the Outstanding Faculty Award from the State Council on Higher Education in Virginia, and the Biggs Award for Excellence in Geoscience Teaching from the Geoscience Education Division of the Geological Society of America. In previous years, Callan served as a contributing editor at EARTH magazine, President of the Geological Society of Washington and President the Geo2YC division of NAGT.
Other geobloggers are writing about