The river habitats are a subsection of the Lower Mackenzie Freshwater Ecoregion. The area around the river in Yukon is called the Liard River Valley, and the Alaska Highway follows the river for part of its route. This surrounding area is also referred to as the Liard Plain, and is a physiographic section of the larger Yukon–Tanana Uplands province, which in turn is part of the larger Intermontane Plateaus physiographic division.
The Indigenous name for the river is Nêtʼił Tué', which means Hanging Down River in the Kaska language. The name comes from a particularly narrow spot near the river's headwaters, where Kaska people used to set goat snares. The "hanging down" - "Nêtʼił" part of the name refers to the snares. The origin of the river's name in mainstream use today is obscure, but is derived from the French word for "Eastern Cottonwood" (a kind of poplar) which grow in abundance along sections of the river. Among the early fur traders, who traveled the river corridor the Liard above the Fort Nelson River was referred to as the "West Branch," while the Fort Nelson River was the "East Branch."
The first European to traverse most of the river was John McLeod of the Hudson's Bay Company (HBC). Leaving Fort Simpson on June 28, 1831, McLeod and eight others ascended the river, reaching and naming the Dease River in just over six weeks. Four days later, they reached the Frances River, and mistakenly ascended it, thinking it was the Liard's main branch. Nine years later, another HBC employee, Robert Campbell, journeyed to the source of the Liard in the St. Cyr Range, renaming the river McLeod had ascended for Frances Ramsay Simpson, the wife of the Sir George Simpson, the HBC's governor who had authorised both expeditions.
The entire Yukon and British Columbia's portion of the river corridor is said to be the traditional unceded territory of the Kaska Dena, who have lived in the area for thousands of years and claim it as their rightful home. This claim is contested by both the Acho Dene Koe First Nation and Fort Nelson First Nation who count among their memberships the former residents of communities along the Liard, east of the Grand Canyon of the Liard, like Nelson Forks, La Jolie Butte, and Francois, where the Acho Dene Koe signed Treaty 11. Their descendants still live and hunt in the area to this day. Despite Kaska Dene claims, much of the area has been recognized as Fort Nelson and Acho Dene Koe First Nation territory under Treaty 8 and 11 since 1910 and 1922 respectively.
Features
The Grand Canyon of the Liard is a 30 km (19 mi) stretch of the river beginning just east of Liard River Hotsprings. It contains numerous class IV and higher rapids. It is located between the Toad and Trout Rivers' confluences with the Liard.[3]59°27′00″N125°48′00″W / 59.45000°N 125.80000°W / 59.45000; -125.80000 The area was the site of extensive study in the late 1970s and early 1980s by BC Hydro for a potential hydroelectric dam. The location, initially known as Site E, later renamed to Devil’s Gorge, was intended as one of a number of potential sister projects to the Site C Dam on the Peace River. Though questions of feasibility and British Columbia’s future electricity needs would lead to the project, along with British Columbia’s other Site projects, being shelved in favour of Site C.
The historic Liard River Suspension Bridge, built in 1944, is located at kilometre 798 of the Alaska Highway.
Course
Yukon
The Liard River originates in south-eastern part of the Yukon, on the slopes of Mount Lewis, at 61°14′12″N131°37′39″W / 61.23667°N 131.62750°W / 61.23667; -131.62750, at an elevation of 1,500 m (4,900 ft). It flows south and east, between the ranges of Pelly Mountains, then south through the Yukon Plateau, where it receives the waters of Prospect Creek. It turns east after it receives the waters of the Caribou Creek from Caribou Lakes, then the Swede and Junkers Creek. It then follows the southern rim of the St. Cyr Range of the Pelly Mountains, where the Ings River flows into it. It follows the southern edge of the Simpson Range, receiving the waters of the Old Gold Creek, Rainbow Creek, Dome Creek, Quartz Creek and Scurvy Creek. The Liard River continues south-east, north of the Cassiar Mountains, from where it receives the Sayyea Creek and Cabin Creek while the Eckman Creek, Black River and Hasselberg Creek flow in from the north. It continues in a south-east direction, receiving the Sambo Creek, False Pass Creek, Meister River, Frances River, Rancheria River, Tom Creek, Watson Creek and Albert Creek before it flows through Upper Liard, west of Watson Lake, where it is crossed by the Alaska Highway. It receives the waters of Cormier Creek, then flows through the Liard Canyon and into British Columbia.
It flows south-east and east along the Alaska Highway, receiving the waters of Dease River, Kloye Creek, Trepanier Creek and Black Angus Creek. It continues east through the Dease Forest, where it receives the waters of the Hyland River south of Hyland River Provincial Park, then receives the Malcolm Creek, Tatisno Creek and Nustlo Creek. It flows along the Yukon border, where the Alaska Highway once again follows the Liard and receives the Cosh Creek, Contact Creek, Scoby Creek and Sandin Brook, then turns south around Mount Sandin, receiving water from Tsia Creek, Tsinitla Creek, Tatzille Creek and Leguil Creek. It turns eastwards along the northern margin of the Liard Plateau, where it receives the Kechika River near Skooks Landing, Niloil Creek from Niloil Lake and Coal River by Coal River. It continues east and south-east, south of Mount Reid, still followed by the Alaska Highway, receiving the waters of Geddes Creek, Grant Creek, Smith River, Lapie Creek, Teeter Creek, Mould Creek and Hoole Creek.
Liard River Suspension Bridge, built in 1944 on the Alaska Highway
It enters the Liard River Hot Springs Provincial Park, where the Trout River empties into the Liard. Alaska Highway runs south along the Trout River, while the Liard flows east through the Liard River Corridor Provincial Park and Protected Area, south of the Sentinel Range of the Muskwa Ranges, receiving the waters of Deer River and Canyon Creek in the Grand Canyon of the Liard. It continues south-east between the Barricade Range and Mount Rothenberg of the Sentinel Range, where the Moule Creek and Sulphur Creek flow in the Liard. It flows east, out of the Northern Rockies and through the foothills, where it receives waters from the Brimstone Creek, Crusty Creek, Grayling River, Graybank Creek and Toad River. It turns north-west, receiving the waters from Garbutt Creek, Lepine Creek, Chimney Creek, Ruthie Creek, Scatter River and Beaver River. It then turns south-east, receives the waters from Catkin Creek, Dunedin River and Fort Nelson River. From here it turns north, receiving the waters of Zus Creek, Sandy Creek and La Biche River and crosses into the Northwest Territories, immediately east of the Yukon border.
The Liard River continues north, receiving the waters of Big Island Creek, Kotaneelee River and Petitot River. It turns around Mount Coty of the Franklin Mountains near Fort Liard Airfield, where it meets the Liard Highway. It receives the waters of the Muskeg River, Rabbit Creek and Flett Creek as it flows east of the Liard Range and Mount Flett. The Liard meanders east of the Sawmill Mountain and receives waters from the Beaver Water Creek, Netla River and Bay Creek. After receiving the waters of South Nahanni River south of Nahanni Butte and east of the Nahanni National Park Reserve, the Liard turns east and north-east, receiving waters from Grainger River, Blackstone River, Dehdjida Creek, Matou River, Birch River and Poplar River. It then turns north, being followed by the Mackenzie Highway, and receives the Manners Creek before it empties into the Mackenzie River, immediately upstream of Fort Simpson, at Clay Point, at an elevation of 120 meters (390 ft). The Truesdell Island and Franklin-Clarke Island are formed at the river mouth.
Tributaries
From headwater to mouth, the tributaries of the Liard are:
