Castleguard Cave is a limestone cave located at the north end of Banff National Park in the Rocky Mountains of Canada. With 20,357m of surveyed passages (as of 2007), it is Canada's longest cave, and its fifth deepest at 384m. Castleguard Cave ascends gently from its entrance and terminates beneath the Columbia Icefield.
General information :
Castleguard Cave is modest in size compared to other great caves of the World, but nevertheless is well known amongst cavers and speleologists internationally. It is the subject of a film and a coffee-table book, and is mentioned in most cave reference books in print.
This attention is due in part to its magnificent, remote mountain setting. Its location within a protected area in a national park prohibits motorized ground access, and the risk of flooding in its entrance has limited most explorations to mid or late winter, so cavers must access it via a 20 km (12 mi) ski with towed sleds, or by helicopter. This feeling of remoteness is compounded by the cave's linear layout and its single entrance. The classic trip, from the entrance to the Ice Plug by the shortest route, traverses 9 km (6 mi) of cave passage. Cavers often are underground for four or five days, staying at two underground camps.
Cave setting and form :
Castleguard Cave lies within the Cathedral Formation limestone, except the headward complex which is in the overlying Stephen Formation shaley limestones. Their gently-dipping bedding (about 5 degrees) is reflected in the near-horizontal aspect of the cave. Although the entrance and headwater sections are more complex, the central portion of the cave consists of a single main passage alternating between long sections of vadose (rift or canyon) passages linked by shorter phreatic (tubular) sections. Much of the cave is dry, excepting the entrance series which floods unpredictably in summer.
Castleguard Cave has had a long genesis. The accessible, explored portion of the cave, sometimes referred to as Castleguard 1, is a long-abandoned drain. Studies of pollen found within cave sediments suggest that these cave passages were fully developed and dewatered at least 1M years before present. It is postulated that an underlying cave, Castleguard 2, carries the present-day glacial drainage, resurging at Big Springs. A third cave system, Castleguard 3, collects surface melt from Castleguard Meadows at right-angles to the main cave, joining it somewhere prior to the Big Springs resurgence. Castleguard 3 has been proven by dye tracing and has not been entered to any significant degree by cavers.
Discovery and exploration :
Undoubtedly the cave was known to natives throughout prehistory, but the first recorded visit was by Cecil Smith, an outfitter rounding up stray horses during a guided trip to Castleguard Meadows in 1921. Smith's client happened to be the head of the U.S. Geological Survey, and three years later the cave entrance was revisited and photographed as part of an article on the Columbia Icefield for National Geographic magazine.
Sporadic local visitations likely continued for many years, but the first formal investigations were in the summer of 1967 by members of the Karst Research Group (from McMaster University in Hamilton, Ontario) led by Dr. Derek Ford, following up on a tip from a local outdoorsman. KRG teams penetrated past the cave's first obstacle, an 8m drop, and explored the main trunk passage.
After Peter Thompson and Mike Boon were trapped in the cave by sudden flooding near the entrance, explorations were limited to mid or late winter, with attendant difficulties. The Ice Plug, the 'end' of the cave, was discovered by Mike Boon during a controversial solo trip in the winter of 1970. Soon thereafter cavers helped produce The Longest Cave, a National Film Board production, during which some side passages were explored.