The Canadian Rocky Mountain Parks World Heritage Site consists of seven contiguous parks including four national parks and three British Columbia provincial parks.
Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.
The Canadian Rockies or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.
Berg Lake is a lake on the Robson River just below the river's source located within Mount Robson Provincial Park, at the doorstep of the north face of Mount Robson, the highest peak in the Canadian Rockies. It is partly fed by the Berg Glacier.
Mount Robson Provincial Park is a provincial park in the Canadian Rockies with an area of 2,249 km2. The park is located entirely within British Columbia, bordering Jasper National Park in Alberta. The B.C. legislature created the park in 1913, the same year as the first ascent of Mount Robson by a party led by Conrad Kain. It is the second oldest park in the provincial system. The park is named for Mount Robson, which has the highest point in the Canadian Rockies and is located entirely within the park.
The Perito Moreno Glacier is a glacier located in Los Glaciares National Park in southwest Santa Cruz Province, Argentina, and originated in the Magallanes Region in Chile. It is one of the most important tourist attractions in the Argentine Patagonia.
The Matukituki River is a short braided river in the Southern Alps of New Zealand's South Island. Both its West Branch and East Branch originate from the Main Divide mountain ranges near Mount Aspiring / Tititea. Their largely glacier-fed waters each flow for approximately 20 kilometres (12 mi) before joining near Camerons Flat. After this confluence, the Matukituki River leaves the boundaries of Mount Aspiring National Park and continues for another 30 kilometres (19 mi) to exit into Lake Wānaka at the lake's southwestern edge.
The Taylor Glacier is a glacier in Antarctica about 35 nautical miles long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills. It flows to the south of the Asgard Range. The middle part of the glacier is bounded on the north by the Inland Forts and on the south by Beacon Valley.
Clearwater is a river of southern Alberta, Canada. Situated entirely in the Canadian Rockies and the Rocky Mountain foothills of Alberta, it is a glacier fed upper reach tributary of the North Saskatchewan River. The upper reach of the Clearwater has become popular for equestrian travellers due to the natural setting along the river.
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier.
A moulin is a roughly circular, vertical well-like shaft formed where a surface meltstream exploits a weakness in the ice. The term is derived from the French word for mill.
The Baltic Ice Lake is a name given by geologists to a freshwater lake that evolved in the Baltic Sea basin as glaciers retreated from that region at the end of the last ice age. The lake existed between 12,600 and 10,300 years Before Present (BP).
Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km (23 mi) northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide. Runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum.
The Abbot Pass hut was an alpine hut located at an altitude of 2,925 metres (9,596 ft) in Abbot Pass in the Rocky Mountains in Alberta, Canada. It was nestled between Mount Victoria and Mount Lefroy, straddling the Great Divide, which, in this region, defines the boundary between Banff National Park in Alberta and Yoho National Park in British Columbia. While close to the border, the hut lay entirely in Banff National Park, and was the second-highest permanently habitable structure in Canada. The hut was maintained by the Alpine Club of Canada.
Sperry Glacier is a glacier on the north slopes of Gunsight Mountain west of the Continental Divide in Glacier National Park in the U.S. state of Montana. Although many geologic features of Glacier National Park were formed during the much longer period of glaciation ending over 10,000 years ago, Sperry Glacier — like all the glaciers in the park today — is a product of the recent Little Ice Age, the period of cooler average temperatures starting in about the 13th century and concluding in the mid-19th century.
Babb is a small unincorporated farming and ranching community in Glacier County, Montana, United States, on the Blackfeet Indian Reservation. The community experiences a large influx of tourists in the summer months as it is the gateway to the Many Glacier area of Glacier National Park. For statistical purposes, the United States Census Bureau has defined Babb as a census-designated place (CDP). It had a population of 174 at the 2010 census.
The Robson Glacier is the primary source of the short Robson River, one of the uppermost tributaries of the Fraser River. Located on the British Columbia-Alberta Boundary and the Continental Divide to the east of Berg Lake in Mount Robson Provincial Park, it sits on the northeast flank of Mount Robson in Mount Robson Provincial Park, British Columbia in the Canadian Rockies. Its meltwater feeds unofficially named Robson Lake, whose outlet marks the start of the Robson River.
The Robson River is a short but swift, rapid and waterfall-infested river in Mount Robson Provincial Park of British Columbia. It is a tributary of the Upper Fraser River and it originates near Robson Pass, which divides the Robson River and the headwaters of the Smoky River drainage. There are three lakes along the river's course as well as four waterfalls.
Swiftcurrent Creek is a river in Mount Robson Provincial Park in British Columbia. It is a tributary of the Fraser River, entering the Fraser about 1.7 kilometres (1.1 mi) below the mouth of the Robson River.
Resplendent Mountain, or Mount Resplendent is a peak in the Canadian Rockies, located at the northern end of Mount Robson Provincial Park in British Columbia, Canada. It is a part of the Rainbow Range, and is a sister peak to the more famous Mount Robson, its nearest neighbour. Together they form a classic panorama seen by travellers on Via Rail trains and Highway 16. The mountain was named by Arthur P. Coleman, and Arthur O. Wheeler wrote, "On the east side it is clad from top to bottom in pure white snow, and presents with the sun shining upon it a spectacle of such wonderful brilliance that the aptness of the name became immediately apparent." The first ascent was achieved on the same historic 1911 trip in which Conrad Kain first scouted the climbing routes later to be used on the first ascent of Mount Robson.
