Canadian Arctic Islands -- scenery and geology

This document is a sampling of scenery, wildlife, flora, and geology I have photographed mainly on Ellesmere, Axel Heiberg, and Amund Ringnes islands in the Canadian Arctic during geological fieldwork in 1987, 1990, and 1993. The Candian Arctic is a stunningly beautiful place, but unfortunately it is one of the least accessible parts of Canada. By sharing these images and comments, I hope to communicate what the area is like, so people can appreciate it even if they do not have the opportunity to go there, or if they have not considered going there before.

Location

outline of the Queen Elizabeth Islands, northern Canada Axel Heiberg and Ellesmere islands

Images

view looking west down Kanguk Peninsula, western Axel Heiberg Island, July 1990. Strand Fiord, with a few icebergs and some seasonal ice, is visible on the left. "Split Mountain" is visible in the distance at centre right.

Purple saxifrage (Saxifraga oppositifolia) from west of Resolute Bay, Cornwallis Island, July, 1993.

looking northeast, up Otto Fiord, northwest Ellesmere Island. A glacier at the end of the fiord has calved icebergs, many of which are stranded in the shallow fiord. July, 1987.

looking south from Dragon Mountain, across Expedition Fiord, towards "Split Mountain". Western Axel Heiberg Island. Both seasonal sea ice and icebergs are visible in the fiord. July, 1993.

Capitate lousewort (Pedicularis capitata) from near Kanguk River, western Axel Heiberg Island, July, 1990.

looking towards the west at flood basalt lava flows on Dragon Cliffs, north side of Expedition Fiord, western Axel Heiberg Island. These lava flows are part of the Albian (late Early Cretaceous) age Strand Fiord Formation. At Dragon Cliffs, there are more than 10 flow units totalling over 200 metres of stratigraphic thickness. The cliffs approach 300 metres tall at this location, and drop precipitously into the fiord, which is covered in seasonal ice. The rounded peak on the left is Surveyor Mountain, and beyond that is Iceberg Bay and the Triangle Peninsula. On the horizon are the icefields north of South Fiord, which get as high as 1200 metres (3945 feet). July, 1993.

closer view of the flood basalt lava flows on Dragon Cliffs, north side of Expedition Fiord, western Axel Heiberg Island. This view is close enough that columnar jointing is visible in individual flows (the vertical striations). It is formed due to contraction and propigation of stress-related cracks during the cooling of the flows. The columns in this unit are usually 1 to 3 metres in diameter, giving some idea of the impressive scale. July, 1993.

Alpine arnica (Arnica alpina). North of Bastion Ridge, near the head of Expedition Fiord, south of the Expedition River. July, 1993.

A days catch for a paleontologist. These specimens are Cretaceous (Middle Albian) in age, and occur within calcium-carbonate concretions in the shales of the Christopher Formation. Ammonites, probably Neogastroplites or related genera, are the most common fossils; but also present are occasional inoceramid clams, and complete fossil fish (top specimen). As you can see, the shape of the concretions often conforms to the fossil contained within. From near Dragon Mountain, western Axel Heiberg Island. July, 1993.

Nodding bladder campion (Melandrium apetalum ssp. arcticum). Near Dragon Mountain, north of Expedition Fiord, western Axel Heiberg Island. July, 1993.


Acknowledgements

Fieldwork in this area would not be possible without the logistical and financial support of the following organizations:

The Polar Continental Shelf Project

The Arctic Institute of North America

The Department of Indian and Northern Affairs

and others.


Unless otherwise noted, images are copyright (c) 1996 Andrew MacRae, email: macrae@geo.ucalgary.ca, and are freely distributable for non-commercial use provided the original source and copyright is indicated. For other uses, please contact the author.