Trail: Swan Lake Canoe Route
National Park: Kenai National Wildlife Refuge
Features: Lake(s)/pond(s)/reservoir(s)
Activities: Boating, non-motorized: Canoeing
Boating, non-motorized: Kayaking
Camping
Dogs - Mushing
Fishing
Snow - Skiing, cross-country
Snow - Showshoeing
Swimming
Wildlife observation - Birds

Miles: 60 miles
Desc: ‘A wilderness, in contrast with those areas where man and his own works dominate the landscape, is hereby recognized as an area where the earth and its community of life are untrammeled by man, where man himself is a visitor who does not remain.’ With these words, the Congress of the United States defined the general characteristics of a wilderness area. The Kenai Canoe Trails is one of only two wilderness canoe systems established in the United States (the other being Boundary Waters Canoe Area Wilderness in northeastern Minnesota). These trails are located within the northwestern section of the Kenai National Wildlife Refuge, an area of 1.3 million acres, established by the Alaska National Interest Lands Conservation Act of 1980 for its outstanding wildlife and recreational values.

The Kenai Canoe Trails are divided into two systems, the Swan Lake and Swanson River Canoe Routes. Both trails are National Recreation Trails. The Swan Lake System is perhaps the most visited of the two systems and contains 30 lakes linked with the main branch and the West Fork of the Moose River in an interconnecting system of waterways and portages. This forms a canoe route of about 60 miles, though many shorter excursions are possible and even likely. The Swanson River Canoe Route lies north of the Swan Lake System and connects 40 lakes with 46 miles of the Swanson River. In total, the Swanson River Canoe Route forms a trail system of just over 80 miles in length.

Besides the lakes directly connected by portages and waterways, this area contains thousands of other lakes which are seldom explored or even seen. The contour of this wilderness is not particularly rugged, but is generally a flat to gently undulating topography of ancient glacial deposits. Surrounding the lakes that are scattered throughout the area are rounded hills and ridges rising up to a maximum of 295 feet in elevation. But the lakes are the most noticeable feature. They drain either directly or indirectly into two systems, the Moose and Swanson Rivers. These are both shallow streams, following meandering paths through poorly-drained swamps and muskeg flats. Both the Moose and the Swanson River also offer interesting floating possibilities.