Coppermine

History

The river was named for the copper ores which are located along the river, by Samuel Hearne in 1771. Hearne found only one lump of copper and commercial mining was not considered viable.

Bloody Falls, part of the Kugluk/Bloody Falls Territorial Park, is located 18.5 kilometres (11.5 mi) from Kugluktuk, and was home to the Kogluktogmiut a sub-group of the Copper Inuit. It is the site of the Bloody Falls Massacre, when Matonabbee, Samuel Hearne's guide, and his fellow Chipewyan warriors ambushed and massacred the local Inuit.

Ecology

Willow was observed growing at the top of the basalt deposit at Bloody Falls. Locals described the willow being a recent arrival and appeared in previous decades according to a study in 1970. The area is at the northern edge of the tree line. White spruce was found in the area but its height was stunted. The landscape is on the border of stunted forest and shrubs shifting to Arctic tundra. A survey conducted in 2014 found 300 plant species in the lower Coppermine River valley, which was considered to be relatively high compared to other regional and local areas in Nunavut and more diverse than plant species found in Tuktut Nogait National Park.

Geology

The river is on the northwestern part of the Canadian Shield. It was part of the broad region covered by the Laurentide ice sheet, which melted away 10,000 years ago. Above and below Bloody Falls, the river's width is broad due to fluvioglacial erosion. At the falls, the river is described to be a narrow and fast-moving rapid with the elevation dropping by 10 metres (33 ft) from the start to the end of the falls. The Coppermine River at Bloody Falls is surrounded by steep rocky slopes and sandy gullies. There is a basalt deposit which reaches 20 m above the river and displays a gradual slope into a flat, rocky beach downstream. The Coppermine Mountains are located on the west side of the river.