MOUNTAINOUS KARST OF THE CANADIAN ROCKIES AND COLUMBIA MOUNTAINS
The mountainous karst of the Canadian Rockies and Columbia Mountains, comprise the massive carbonate platforms of the Front Ranges of the former (which extends south into Montana, USA) and the marble stripe karsts in the metamorphic belts of the latter. However the majority of caves and associated drainage systems in this region are contained in the massive carbonates (limestones and dolomites) of the Front Ranges where karst drainage is in the order of 10’s of km2 within elevations ranges of 500-3000 m AMSL. The marble karst is less well explored but tends to comprise drainages of a few km2within elevations of 800-1800 m AMSL. The Canadian karst rocks of this region range in age from Holocene tufa (Banff Cave and Basin, Banff National Park) to pre-Cambrian marbles (Tupper - Raspberry cave system, Glacier National Park).
Mountainous karst has been studied in Western Canada for over 50 years with most research emanating from McMaster University. Since 1991 little directed research has been done in the Canadian Rockies and Columbia Mountains with the exception of a small area (Small River Caves Provincial Park) in the Canadian Rockies until 1997, which was introduced to the scientific community by the Alberta Speleological Society (ASS). In fact, volunteer groups such as the (ASS) and the British Columbia Caving Federation (BCCF) have continued exploration of western Canadian karst to the present day, providing baseline cave surveys, photographic records and exploration reports. The majority of this work has been published in the Canadian Caver Magazine, ASS and BCCF newsletters.