Chilkat-West Lynn Canal

The Chilkat-West Lynn Canal roadless area encompasses 199,772 acres of mountainous terrain in southeastern Alaska's Tongass National Forest, rising from tidewater to alpine summits including Nun Mountain (4,329 ft), Yang-Webster Peak (4,268 ft), and Mount Golub (4,194 ft). The landscape drains through multiple watersheds into the Gulf of Alaska, with the Beardslee River and named creeks—William Henry Creek, Goosh T'eik Héen, X'aak'ú T'eik Héen, and X̱'as'tuhéen—carrying snowmelt and rainfall from the high country to coastal waters. These waterways originate in alpine headwaters and flow through steep valleys, creating the hydrological backbone that connects mountain forest to marine ecosystem.

The area's vegetation reflects the transition from coastal temperate rainforest to alpine tundra. At lower elevations, Sitka spruce (Picea sitchensis) and western hemlock (Tsuga heterophylla) dominate the canopy, with an understory of devil's club (Oplopanax horridus), salmonberry (Rubus spectabilis), and deer fern (Struthiopteris spicant) thriving in the moist shade. As elevation increases, mountain hemlock (Tsuga mertensiana) becomes prevalent, giving way to sedge and grass meadows in the subalpine zone. Alpine vegetation communities occupy the highest ridges and peaks, where glacier bay paintbrush (Castilleja chrymactis) and mountain lady's-slipper (Cypripedium montanum), vulnerable (IUCN), bloom among low herbaceous plants. Wet meadow communities and herbaceous salt marsh vegetation occupy lower-elevation flats and coastal margins, where sea plantain (Plantago maritima) and western skunk cabbage (Lysichiton americanus) root in saturated soils.

The area supports wildlife across all elevation zones and habitat types. Brown bears move between salmon streams and alpine meadows, where hoary marmots inhabit rocky slopes above treeline. In the forest understory and canopy, the marbled murrelet, endangered (IUCN), nests in old-growth hemlock and spruce. Coastal waters host the federally endangered short-tailed albatross (Phoebastria albatrus), steller sea lions, vulnerable (IUCN), and humpback whales. Chum salmon (Oncorhynchus keta) and coho salmon (Oncorhynchus kisutch) return to named creeks to spawn, supporting both terrestrial predators and marine food webs. Bald eagles hunt from perches overlooking streams and bays. Western toads (Anaxyrus boreas) occupy wet meadows and forest pools, while harlequin ducks inhabit fast-moving mountain streams.

A person traveling through this landscape experiences sharp ecological transitions. Following a trail from tidewater through the Sitka spruce-hemlock forest, the understory darkens with devil's club and the forest floor softens underfoot with moss and accumulated needles. As elevation increases and the trail climbs away from creeks, the canopy opens, mountain hemlock becomes dominant, and the understory shifts to low shrubs and herbaceous plants. Breaking above treeline onto alpine meadows, the view expands across the Chilkat Range and surrounding peaks, with the sound of wind replacing the muffled quiet of the forest. In wet meadows and salt marshes near the coast, the ground squelches underfoot, and the vegetation drops to knee-height or lower, offering unobstructed views of the water and sky beyond.

The Chilkat-West Lynn Canal area has been home to the Chilkat Tlingit (Jilkáat Ḵwáan) and Chilkoot Tlingit (Lḵóot Ḵwáan) peoples for generations extending to time immemorial. The Chilkat Tlingit historically controlled approximately 2.6 million acres extending from interior mountain passes near Stonehouse Creek, British Columbia, to Berners Bay, including the west side of the Lynn Canal fjord, which they viewed as the "fenceposts" of their territory. The Lukaax̱.ádi Clan, a specific Tlingit clan documented as having historical ownership and use of the area, harvested salmon from the Chilkat and Chilkoot watershed runs using traditional weirs and traps. The Chilkat River estuary and its waters supported world-renowned eulachon runs, which the Tlingit harvested and processed into grease, a highly valued food and trade commodity. The rugged mountains of the West Lynn Canal supported hunting of mountain goats, whose wool was essential for weaving Chilkat blankets (Naaxein), the complex ceremonial regalia for which the Chilkat Tlingit became renowned. The Chilkat Tlingit maintained a lucrative trade monopoly controlling the mountain passes—including the Chilkoot and Chilkat Passes—that linked the Pacific coast to the interior Yukon Territory, exchanging coastal resources for furs and copper from interior Athabaskan groups such as the Tagish. The village of Klukwan, located just north of this area on the Chilkat River, remains one of the longest continuously inhabited Indigenous villages in North America.

In April 1811, the American maritime fur trading ship Otter, captained by Samuel Hill, engaged in violent conflict with the Chilkat Tlingit in the Chilkat Inlet. The battle resulted in the deaths of two crew members and an estimated 40 Tlingit, including 13 chiefs. In 1840, James Douglas of the Hudson's Bay Company established Fort Durham (also known as Fort Taku) at the mouth of the Taku River. During the late nineteenth century, Lynn Canal served as the primary maritime route for miners heading to the Klondike gold fields via Skagway and Dyea. A sawmill was established in 1889 by the Swedish Free Mission Church. The area was established as a gold and silver mining camp around 1895. The Chilkoot Trail and White Pass, established as Tlingit trade routes long before the Klondike Gold Rush, became focal points of overland access during the gold rush era. In 1903, Lynn Canal became a central point of contention in a boundary dispute between the United States and Canada.

The Alexander Archipelago Forest Reserve was established on August 20, 1902, by presidential proclamation from Theodore Roosevelt under the authority of the Creative Act of 1891. The Tongass National Forest was officially created on September 10, 1907, by another presidential proclamation from Theodore Roosevelt. On July 1, 1908, President Roosevelt consolidated the Alexander Archipelago Forest Reserve and the Tongass National Forest into a single administrative unit. A subsequent proclamation on February 16, 1909, significantly expanded the forest's boundaries to include most of Southeast Alaska. Additional boundary expansions followed in June 1909 and in 1925 under President Calvin Coolidge. Formal legislation declaring it a national forest was signed into law in 1909. In Tlingit and Haida Indians of Alaska v. United States, the court found that the creation of the Tongass National Forest constituted a taking of land from the Tlingit and Haida people, who held aboriginal title through time-immemorial occupancy.

Large-scale logging intensified in the 1950s following the establishment of long-term timber contracts, with the U.S. Forest Service managing the Tongass as a pulpwood farm through widespread clearcutting that continued through the 1990s. In 1952, the Aluminum Company of America (Alcoa) proposed the "Yukon-Taiya Project," a $400 million industrial development. The project was repeatedly proposed, studied, and shelved, most recently in 2016 due to budget crises and environmental opposition. For over 40 years, the area has been the center of debate regarding a road connection for Juneau, the only U.S. state capital inaccessible by road. Proposals have included a "West Side" route that would traverse this roadless area from William Henry Bay to Pyramid Harbor. As of 2025, the state has revitalized feasibility studies for a west-side "Chilkat Connector."

The Chilkat-West Lynn Canal area became a focal point of national conservation policy when the 2001 Roadless Area Conservation Rule protected 9.3 million acres of the Tongass from new road construction, including this 199,772-acre Inventoried Roadless Area. The forest has been subject to multiple exemptions and reinstatements of this rule via executive actions by subsequent administrations. Most recently, the Biden administration reinstated roadless protections in January 2023. In January 2025, the Trump administration issued an executive order titled "Unleashing Alaska's Extraordinary Resource Potential" seeking to rescind roadless protections. The USDA announced an intent to rescind the 2001 Roadless Rule entirely, which would include the Tongass National Forest.

Vital Resources Protected

Headwater Protection and Salmon Spawning Habitat

The Mount Golub headwaters and tributary network—including Beardslee River, William Henry Creek, Goosh T'eik Héen, X'aak'ú T'eik Héen, and X̱'as'tuhéen—form the cold-water foundation for Pacific salmon reproduction across the Chilkat watershed. These streams originate in alpine and subalpine terrain where snowmelt and groundwater maintain the low temperatures and stable flows that salmon eggs require to develop. The roadless condition preserves the intact riparian forest (Sitka spruce and western hemlock) that shades these channels, regulates water temperature, and supplies large woody debris that creates spawning substrate and juvenile rearing habitat. Road construction in this drainage would introduce sedimentation and canopy loss that would degrade these conditions across the entire downstream network.

Alpine and Subalpine Ecosystem Connectivity

The area's high-elevation terrain—Nun Mountain (4,329 ft), Mount Golub (4,194 ft), Yang-Webster Peak (4,268 ft), and the Chilkat Range—supports alpine vegetation and meadow communities that function as climate refugia for species sensitive to warming. The marbled murrelet (endangered, IUCN), dunlin (near threatened, IUCN), least sandpiper (near threatened, IUCN), and rufous hummingbird (near threatened, IUCN) depend on the unbroken elevational gradient from coastal forest through subalpine meadows to alpine tundra. This vertical connectivity allows species to track suitable habitat as climate shifts. Fragmentation by road corridors would sever this gradient, trapping populations in shrinking habitat bands and preventing upslope migration as lowland areas warm.

Intertidal and Nearshore Marine Habitat for Seabirds and Marine Mammals

The West Lynn Canal coastline—including Lance Point, Saint James Point, Point Howard, Danger Point, and Gux̱ X̱'aagák'u—provides critical feeding and resting habitat for the federally endangered short-tailed albatross, black-legged kittiwake (vulnerable, IUCN), and marbled murrelet (endangered, IUCN), which forage in nearshore waters. The area also supports the federally endangered sea otter (also endangered, IUCN) and the vulnerable Steller sea lion (vulnerable, IUCN), which haul out on rocky points and feed in kelp forests and nearshore channels. The roadless condition maintains the isolation and low human disturbance that these species require; the intact upland forest also prevents erosion and sedimentation that would degrade the nearshore benthic habitat these animals depend on.

Wet Meadow and Herbaceous Salt Marsh Communities for Migratory Shorebirds

Sedge/grass/forb meadows, wet meadows, and herbaceous salt marsh communities throughout the area provide critical stopover and breeding habitat for long-tailed duck (vulnerable, IUCN), black-bellied plover (vulnerable, IUCN), lesser yellowlegs (vulnerable, IUCN), and greater yellowlegs (near threatened, IUCN). These species use these open habitats for feeding and nesting during migration and breeding seasons. The roadless condition preserves the hydrological integrity of these wetlands—the water table, seasonal flooding patterns, and vegetation structure that make them suitable for shorebirds. Road construction would drain and fragment these communities, converting them to upland or disturbed habitat unsuitable for breeding and foraging.

Threats from Road Construction

Sedimentation and Stream Temperature Increase from Canopy Removal and Cut Slopes

Road construction in this mountainous terrain requires extensive cut slopes and removal of riparian forest to accommodate roadbed and drainage. Exposed mineral soil on steep slopes erodes rapidly, delivering fine sediment into the headwater streams that feed the Chilkat watershed. This sedimentation smothers salmon spawning gravel, reducing egg survival and preventing juvenile fish from accessing interstitial spaces where they hide from predators. Simultaneously, removal of the Sitka spruce and western hemlock canopy that currently shades the streams allows solar radiation to warm the water. Pacific salmon—particularly the species that spawn in these cold headwaters—have narrow thermal tolerances; even small temperature increases reduce metabolic efficiency and increase disease susceptibility. The combination of sedimentation and warming would degrade spawning and rearing habitat across the entire downstream network, affecting populations that support the seasonal concentration of bald eagles and other predators.

Habitat Fragmentation and Loss of Elevational Connectivity for Alpine and Subalpine Species

Road corridors create linear barriers that fragment the continuous forest and meadow habitat connecting lowland coastal forest to alpine tundra. This fragmentation isolates populations of marbled murrelet (endangered, IUCN), dunlin (near threatened, IUCN), least sandpiper (near threatened, IUCN), and rufous hummingbird (near threatened, IUCN) that currently move vertically through the landscape in response to seasonal changes and long-term climate shifts. The road itself becomes an edge—a zone of increased light, wind, and temperature fluctuation that favors invasive species and creates hostile conditions for interior forest and alpine specialists. As climate warming compresses suitable habitat upslope, these species will be unable to track their preferred conditions because the road will have severed the connectivity they require. Populations trapped below the road corridor will face local extinction as their habitat becomes unsuitable.

Culvert Barriers and Hydrological Disruption in Wetland and Meadow Communities

Road construction across wet meadows and herbaceous salt marshes requires fill material and culverts to manage water flow. Culverts—even when properly sized—create barriers to fish movement and alter the timing and magnitude of water flow through wetlands. More commonly, undersized culverts cause upstream ponding that converts meadow to open water, drowning the sedge and grass vegetation that long-tailed duck (vulnerable, IUCN), black-bellied plover (vulnerable, IUCN), lesser yellowlegs (vulnerable, IUCN), and greater yellowlegs (near threatened, IUCN) require for breeding and foraging. Downstream of the culvert, reduced flow dries out meadow habitat. Road fill also disrupts the shallow groundwater gradients that maintain wet meadows, causing them to transition to upland shrub or forest. These hydrological changes are difficult to reverse; once the water table is lowered and vegetation composition shifts, restoring the original wetland community requires decades or is impossible without active restoration.

Invasive Species Establishment and Edge-Effect Expansion Along Road Corridors

Road construction creates disturbed soil, gravel shoulders, and drainage ditches—all ideal habitat for invasive plants and vectors for invasive animals. The road corridor itself becomes a dispersal pathway for invasive species moving into previously undisturbed forest and meadow. Norway rats and black slugs, documented as spreading in nearby coastal areas, would gain access to the interior of the roadless area via the road and its associated disturbance. Invasive plants would establish in road shoulders and spread into adjacent forest, competing with native species and altering fire regimes and forest structure. For species like the marbled murrelet (endangered, IUCN) and sea otter (federally endangered), which depend on specific forest structure and kelp forest composition, invasive species establishment would degrade habitat quality across a much larger area than the road footprint itself. The edge effects—increased predation, parasitism, and competition from invasive species—extend hundreds of meters into the forest on either side of the road, effectively fragmenting habitat far beyond the physical road boundary.

The Chilkat-West Lynn Canal Roadless Area encompasses 199,772 acres of mountainous terrain in the Tongass National Forest, ranging from alpine peaks—including Nun Mountain at 4,329 feet and Yang-Webster Peak at 4,268 feet—down to coastal salt marshes and river deltas along Lynn Canal. The area's roadless condition preserves critical habitat for wild salmon and supports hunting and fishing that depend on intact, undisturbed watersheds. Access is primarily by water or floatplane; no roads penetrate the interior.

Hunting

The roadless area falls within Alaska Department of Fish and Game Management Units 1C and 1D and supports brown bear, moose, and mountain goat hunting. Mountain goat season in Unit 1C opens October 1; all goat hunters must complete an online identification quiz. Brown bear seasons typically run September 15 through December 31 (fall) and March 15 through May 31 (spring); nonresident bear hunters must be accompanied by a guide. Moose hunting in Unit 1D includes the TM059 Tier II Permit Hunt, restricted to Upper Lynn Canal residents. Porcupines are abundant in adjacent Chilkat State Park. The area provides critical wintering habitat for Sitka black-tailed deer and supports old-growth-dependent wildlife; this habitat value depends on the absence of roads. Access is primarily by marine routes through Lynn Canal and Chilkat Inlet, or via the Haines road system to the north. A proposed west-side road from William Henry Bay or Pyramid Harbor is under feasibility study but does not currently exist.

Fishing

The Chilkat River drainage and its tributaries support all five Pacific salmon species—Chinook, coho, sockeye, pink, and chum—along with steelhead, Dolly Varden char, and coastal cutthroat trout. The Beardslee River is a primary fish producer in the Tongass, noted for pink salmon escapement and sport fishing. Smaller tributaries near Lance Point and Saint James Point provide critical rearing habitat for coho salmon fry and coastal cutthroat trout. The area is managed for wild fish production; intact, undammed watersheds are essential to natural spawning and rearing. Fishing regulations are set by the Alaska Department of Fish and Game and change seasonally. Coho salmon saltwater limits are typically 6 per day and 12 in possession (16 inches or greater); freshwater limits in drainages near the road system are 2 per day and 2 in possession. King salmon retention is often restricted to protect wild stocks. Access for anglers is by boat via Lynn Canal to William Henry Bay, Pyramid Harbor, and Saint James Bay, or by floatplane. The northern boundary is accessible via the Haines Highway and Klehini River Bridge. The roadless condition preserves the "Salmon Forest" character—undammed, wild-producing waterways that generate 25 percent of commercially caught salmon on the U.S. West Coast.

Paddling

Sea kayaking and canoeing occur in the lower reaches of the Beardslee River, William Henry Creek, and the Chilkat River where it meets Lynn Canal, as well as in the lower 2.5 to 3 miles of the Endicott River. Paddling is primarily marine-based, with tidal influence affecting navigation in coastal estuaries; shallow passages may only be navigable at high tide. The primary season runs May through mid-September. Paddlers typically launch early (4:00 AM to 6:00 AM) to avoid strong afternoon winds common in the fjord. Put-in and take-out locations include William Henry Bay, small coves on the western Chilkat Peninsula, and the Endicott River mouth, where an unpaved airstrip provides floatplane access. Haines serves as a northern staging point. Commercial outfitters operate multi-day guided sea kayaking tours along the coastline and river mouths. The roadless condition preserves the quiet, undisturbed character of these coastal and river ecosystems; roads would fragment habitat and alter the natural tidal and freshwater dynamics that make paddling here distinctive.