Quartz

The Quartz Roadless Area encompasses 143,003 acres within the Tongass National Forest in southeastern Alaska, positioned across the varied terrain of the Ketchikan-Misty Ranger District in Ketchikan Gateway County. The Rousseau Range defines the area's dominant landforms, contributing to a landscape shaped by the convergence of coastal and montane influences. Hydrology is central to this area's character: the Wilson Arm headwaters originate here, feeding the Wilson River system, while the Keta River, Bartholomew Creek, Blossom River, Red Creek, and Fish Ladder drain water from interior slopes toward the coast. These drainages create a network of cold, oxygen-rich channels through valley bottoms and forested hillsides, sustaining the hydrological integrity of Wilson Arm.

The forested communities of the Quartz area follow the moisture and elevation gradients characteristic of the outer coast of Southeast Alaska. In valley bottoms and on lower slopes with high soil moisture, Sitka Spruce–Western Hemlock Forest predominates. Western hemlock (Tsuga heterophylla) and Sitka spruce (Picea sitchensis) form the canopy, with red alder (Alnus rubra) and black cottonwood (Populus trichocarpa) occupying riparian edges along creek banks. The understory beneath this canopy is dense: devil's-club (Oplopanax horridus) fills shaded gaps, while salmonberry (Rubus spectabilis) colonizes disturbed and wet margins. Deer fern (Struthiopteris spicant), false lily-of-the-valley (Maianthemum dilatatum), and yellow skunk cabbage (Lysichiton americanus) characterize the wet ground layer. On higher slopes where fog and cold air pool, Mountain Hemlock–Alaska-cedar communities emerge, with mountain hemlock (Tsuga mertensiana) and Alaska-cedar (Callitropsis nootkatensis) sharing the canopy above a ground layer of oval-leaf huckleberry (Vaccinium ovalifolium), bog rosemary (Andromeda polifolia), and common Labrador-tea (Rhododendron groenlandicum). Peatlands and bog openings interrupt the forest matrix, supporting common cotton-grass (Eriophorum angustifolium), swamp gentian (Gentiana douglasiana), roundleaf sundew (Drosera rotundifolia), and the carnivorous greater bladderwort (Utricularia macrorhiza) in standing water.

American black bear (Ursus americanus) moves through this landscape using the full range of forest and wetland habitats, foraging on salmonberry, thimbleberry (Rubus parviflorus), and red elderberry (Sambucus racemosa) during summer. Along the rivers and creeks, Indian rice (Fritillaria camschatcensis) marks the riparian edge. The horned grebe (Podiceps auritus), classified as vulnerable by the IUCN, uses the area's water bodies during portions of its annual cycle. In the forest interior, Steller's jay (Cyanocitta stelleri) moves between canopy layers, while the pigeon guillemot (Cepphus columba) occupies coastal fringe habitats at the interface with Wilson Arm. The western toad (Anaxyrus boreas) uses wet ground habitats near ponds and stream margins, and is sensitive to hydrological disturbance. Methuselah's beard lichen (Usnea longissima), a slow-growing old-growth indicator, drapes the branches of mature conifers throughout the wetter forest zones. Portions of this area fall within the potential range of several federally listed species; see the Conservation section for details.

A person moving through the Quartz area on foot follows the logic of water. Along the Keta River corridor, the ground is spongy underfoot, the canopy of hemlock and spruce dense enough to diffuse light to a uniform gray-green. Devil's-club commands the understory between streamside alders. Climbing away from the river toward the Rousseau Range, the forest shifts: the spruce gives way to mountain hemlock, the understory opens, and bog laurel (Kalmia microphylla) and yellow mountain-heath (Phyllodoce glanduliflora) appear between patches of exposed mineral soil. The sound of moving water recedes and is replaced by wind in the upper canopy. These transitions — from saturated floodplain to open subalpine — define the ecological range of the Quartz area.

The Quartz Roadless Area lies within the Tongass National Forest on the Ketchikan-Misty Ranger District in southeastern Alaska, within the watershed of Wilson Arm and the Keta River system. The human story of this land begins more than 10,000 years ago, when the first evidence of maritime people appears along the newly emerged coastlines of Southeast Alaska [1]. Microblades and cores found at campsites connect these early inhabitants to Siberian migrations that followed the retreat of glacial ice [1]. Over succeeding millennia, the Tlingit, Haida, and Tsimshian peoples established themselves as the sovereign nations of this region, stewarding lands and waters, developing complex trade networks, and building permanent villages anchored by salmon fishing and the resources of the forest [2][3].

European contact arrived in 1741, when Captain Chirikov's expedition encountered the peoples of Southeast Alaska [1]. Russian traders followed, bartering iron and metal goods for sea otter pelts until, by 1830, the sea otter population had collapsed under commercial pressure [1]. Russia's sale of Alaska to the United States in 1867 opened the territory to accelerating outside development [1]. Miners moved through the region extracting gold, copper, and other minerals, while canneries spread across traditional fishing areas and sawmills began cutting timber to supply fish traps, pilings, and construction lumber for the growing fishing industry [5][4].

In 1902, President Theodore Roosevelt established the Alexander Archipelago Forest Reserve, a direct precursor to the Tongass National Forest [3]. On September 10, 1907, he formally established the Tongass National Forest by proclamation, bringing nearly all commercial timberland in Southeast Alaska — including the lands that now encompass the Quartz area — under federal management [3]. By 1909, timber harvest in the region averaged approximately 15 million board feet annually, much of it supporting local fishing and mining operations [4].

The Tlingit and Haida peoples did not accept this federal appropriation without challenge. In 1929, the Alaska Native Brotherhood passed a resolution to sue the United States government for creating the Tongass National Forest and Glacier Bay National Park without the consent of Southeast Alaska's Indigenous peoples [2]. After decades of legal proceedings, the U.S. Court of Claims ruled in 1959 that the Tlingit and Haida Indians had asserted original use and occupancy from time immemorial over all lands and waters they had claimed in Southeast Alaska [2]. In 1968, the court awarded the Central Council of Tlingit and Haida Indian Tribes of Alaska $7.5 million for lands withdrawn to create the Tongass [2].

Federal forest administration brought new programs alongside commercial development. During the 1930s, the Civilian Conservation Corps built campgrounds, roads, and trails across the Tongass and worked to restore Native totem poles [3]. World War II brought intensified logging: in 1942, the Alaska Spruce Log Program established logging operations across the Tongass to supply high-grade spruce for British military aircraft [3][5]. After the war, a 1947 act of Congress — the Tongass Timber Act — authorized long-term timber sale contracts, and by 1951 the first 50-year contract was signed with the Ketchikan Pulp Company, which secured cutting rights for approximately 8.25 billion board feet of timber across Revillagigedo Island and Prince of Wales Island [4][5]. This industrial-scale logging era shaped the economic life of the Ketchikan region for over four decades. Today, the Quartz area remains part of the Tongass National Forest, designated as a roadless area under the care of the Ketchikan-Misty Ranger District.

Vital Resources Protected

Cold Headwater Stream Integrity The Quartz Roadless Area contains the Wilson Arm headwaters along with the Wilson River, Keta River, Bartholomew Creek, Blossom River, Red Creek, and Fish Ladder — a network of cold drainages originating in the Rousseau Range. The roadless condition preserves the natural hydrology of these headwater systems: uncompacted soils and undisturbed riparian vegetation maintain water temperature, channel morphology, and sediment delivery at naturally low levels. Cold, silt-free water is a functional requirement for aquatic food webs throughout the watershed, and protecting it at the source is significantly more effective than attempting restoration downstream.

Unfragmented Interior Forest Habitat Across 143,003 acres, the Sitka Spruce–Western Hemlock and Mountain Hemlock–Alaska-cedar forest communities of the Quartz area remain structurally intact and unfragmented. Interior forest conditions — characterized by closed canopy, deep litter accumulation, coarse woody debris, and the absence of road-edge disturbance — support old-growth structural complexity, including the slow-growing Methuselah's beard lichen (Usnea longissima), which requires decades of canopy continuity to establish. Species dependent on intact interior conditions, including the horned grebe (Podiceps auritus, IUCN Vulnerable) and the white bog orchid (Platanthera dilatata, IUCN Vulnerable), are sensitive to the edge effects that forest fragmentation introduces.

Wetland and Bog Hydrological Function Bog and peatland communities within the Quartz area — supporting roundleaf sundew (Drosera rotundifolia), swamp gentian (Gentiana douglasiana), common cotton-grass (Eriophorum angustifolium), and the IUCN Endangered Quinine Conk fungus (Laricifomes officinalis) — depend on stable hydrological regimes maintained by undisturbed watershed function. These wetland systems retain carbon, buffer downstream flow, and provide hydrological connectivity between the forested uplands and valley bottom drainages. Their function depends on undisrupted water tables and the absence of surface drainage alteration.

Potential Effects of Road Construction

Sedimentation and Stream Temperature Alteration Road construction in forested watersheds like those of the Quartz area generates cut slopes and compacted road surfaces that accelerate erosion and deliver elevated sediment loads directly to streams. Fine sediment clogs the interstitial spaces of gravel beds, impairs water clarity, and raises stream temperatures by opening the canopy above riparian corridors. These changes degrade aquatic habitat quality in the Wilson River, Keta River, and Bartholomew Creek drainages in ways that are slow to reverse without active restoration, which is rarely fully effective in high-precipitation coastal Alaska systems.

Forest Fragmentation and Edge Effects Road construction bisects interior forest, converting closed-canopy habitat to edge habitat along the road corridor. Edge effects — increased solar exposure, wind penetration, altered humidity, and elevated predation pressure — extend well into the adjacent forest, reducing the effective area of functional interior habitat. In the Sitka Spruce–Western Hemlock and Mountain Hemlock–Alaska-cedar communities present here, fragmentation disrupts the structural continuity on which old-growth-dependent organisms rely. Because old-growth structural complexity in Southeast Alaska forests takes centuries to redevelop after disturbance, these losses are not reversible on human timescales.

Wetland Drainage Disruption and Invasive Species Introduction Road fill and drainage infrastructure alter the surface and subsurface hydrology of bog and peatland systems, lowering water tables and disrupting the saturated conditions that define these communities. Once drained, peatland plant communities shift toward upland-adapted species, and the hydrological function of the wetland — carbon storage, flow buffering — is diminished or lost. Roads also serve as dispersal corridors for invasive species, which readily establish in the disturbed margins of road cuts and spread into adjacent intact habitats; in the closed-canopy forests of Southeast Alaska, invasive species have few established pathways until roads create them.

Federally Listed Species The short-tailed albatross (Phoebastria albatrus), listed as Endangered under the Endangered Species Act, occurs within the potential range of this area. Conservation of intact habitat and undisturbed coastal and marine corridors adjacent to the Quartz area remains a relevant consideration for the long-term recovery of this species.

Hiking

The Bakewell Lake Trail (Trail #55702) is the one formally documented trail within the Quartz Roadless Area. The trail covers 0.8 miles on native material surface and is designated for hiker use. It provides foot access through the forested terrain of the area toward Bakewell Lake, moving through the Sitka Spruce–Western Hemlock forest communities that characterize the lower slopes of the Quartz area. No maintained trailheads or campgrounds are documented within the area, so preparation for dispersed backcountry travel is required — including route-finding, appropriate gear for Southeast Alaska's high-precipitation coastal environment, and leave-no-trace practices on native-surface trail.

Wildlife Observation

The Quartz area's confirmed wildlife includes species that reward patient observers across a range of habitats. American black bear (Ursus americanus) moves through the area's forest and wetland zones throughout the warmer months, foraging on salmonberry (Rubus spectabilis), thimbleberry (Rubus parviflorus), and red elderberry (Sambucus racemosa) in riparian and forest-edge habitats. Black bears are active near stream corridors during salmon runs in the Keta River and Wilson River drainages.

Steller's jay (Cyanocitta stelleri) is the most consistently audible bird in the interior forest, calling loudly through the hemlock and spruce canopy. White-crowned sparrow (Zonotrichia leucophrys) is found in shrubby openings and forest edges, particularly near the bog and wetland communities where nootka lupine (Lupinus nootkatensis) and fireweed (Chamaenerion angustifolium) create open-structured habitat. The pigeon guillemot (Cepphus columba) uses the coastal fringe near Wilson Arm, where forested uplands meet the intertidal zone — this species is typically observed from the water or from the shoreline rather than from the forest interior.

The horned grebe (Podiceps auritus, IUCN Vulnerable) uses the area's water bodies, and the western toad (Anaxyrus boreas) occupies wet ground habitats near ponds and stream margins throughout the area. Both species are best observed with minimal disturbance during their active seasons.

Fishing and Water Access

The Keta River, Wilson River, Bartholomew Creek, Blossom River, and Red Creek drain the Quartz area, with the Fish Ladder feature indicating active salmon passage infrastructure in at least one drainage. These river systems provide opportunities for fishing in a remote, road-free setting. Access to interior stream reaches requires travel on foot, consistent with the backcountry character of the area. Anglers fishing the Keta River system should consult current Alaska Department of Fish and Game regulations for species, seasons, and any area-specific restrictions.

Botanical and Natural History Observation

The Quartz area supports a documented flora of more than 100 species spanning forest, bog, wetland, and subalpine communities — a range that rewards visitors interested in plant identification and natural history. In the bog and peatland openings, sundews (Drosera rotundifolia and Drosera anglica) grow alongside swamp gentian and common cotton-grass. The riparian zones along Bartholomew Creek and Blossom River support western columbine (Aquilegia formosa), arrowleaf groundsel (Senecio triangularis), and deer-cabbage (Nephrophyllidium crista-galli) — a plant characteristic of wet, open subalpine and bog habitats in Southeast Alaska. Devil's-club (Oplopanax horridus) dominates the shaded understory in the mature forest stands, and its autumn red berries mark the forest floor.

Roadless Character and What It Provides

The recreation value of the Quartz area is directly tied to the absence of roads. The Bakewell Lake Trail delivers hikers into forest that is not fragmented by road corridors or road-edge disturbance. The stream systems — Keta River, Wilson River, the Bartholomew Creek and Blossom River drainages — run cold and largely undisturbed in a watershed where headwaters originate within the protected area boundary. Fishing and wildlife observation here happen in the quiet of an unroaded landscape: no motorized traffic, no road dust, no cut slopes interrupting the forest. Road construction in areas like this typically reduces these conditions irreversibly — fragmenting the forest, warming and silting streams, and introducing the noise and disturbance that displace wildlife from corridors they currently use. The backcountry character of the Quartz area is not incidental to its recreation value; it is the foundation of it.