Level IV ecoregions
Level IV ecoregions in the Cascades in Oregon and Washington. A separate section on California's Mt. Shasta has not been mapped yet. (Full map
Western Cascades Lowlands and Valleys (4a)
The Western Cascades Lowlands and Valleys ecoregion comprises a network of steep ridges and narrow valleys on the lower slopes of the Cascade Mountains. Elevation varies from 600 to 4,000 feet (180 to 1,220 m). Its mild, wet climate promotes lush forests dominated by western hemlock and Douglas-fir, with western redcedar, bigleaf maple, red alder, vine maple, salal, rhododendron, Oregon grape, huckleberry, thimbleberry, swordfern, oxalis, hazel, and blackberry. Soils are warmer here than in higher elevation ecoregions, and it is one of the most important timber producing areas in the Pacific Northwest. The steep valleys trending to the west contain high and medium gradient rivers and streams that support cold water salmonids, including the threatened Chinook salmon, steelhead, and bull trout. Notable river drainages in Oregon include the North Umpqua, North and Middle Forks of the Willamette, McKenzie, North Santiam, South Santiam, Clackamas, Salmon and Bull Run River watersheds; and in Washington, the Lewis, Cowlitz, Nisqually, Puyallup, White, and Green River watersheds. Reservoirs store winter snowmelt for irrigation and municipal water supply in the Willamette Valley. The Westerns Cascades Lowlands and Valleys is the largest of the Cascades subregions, covering 3,905 square miles (10,110 km2) in Oregon and 2,397 square miles (6,208 km2) in Washington.
Western Cascades Montane Highlands (4b)
The Western Cascades Montane Highlands ecoregion is characterized by steeply sloping, dissected mountains with high to medium gradient streams and glacial rock-basin lakes. Elevation varies from 3,000 and 6,500 feet (910 and 2,000 m). The western Cascades are older and more eroded than the lava plateau and prominent snow-covered cones of the High Cascades to the east. They are underlain by dark basalt in contrast to the gray andesite of the High Cascades. The region has lower temperatures and receives more winter snow than the lowlands and valleys to the west. Soils have a frigid or cryic temperature regimes. Abundant precipitation supports forests dominated by Douglas-fir and western hemlock, with mountain hemlock, noble fir, subalpine fir, grand fir, Pacific silver fir, red alder, and Pacific yew, and an understory of vine maple, rhododendron, Oregon grape, huckleberry, and thimbleberry. Today, the region is heavily managed for logging and recreation, and it is an important water source for lower elevation urban, suburban, and agricultural areas. It is the second largest of the Cascades subregions, covering 2,729 square miles (7,070 km2) in Oregon and 1,828 square miles (4,734 km2) in Washington.
Cascade Crest Montane Forest (4c)
The Cascade Crest Montane Forest ecoregion consists of an undulating plateau punctuated by volcanic buttes and cones that reach a maximum elevation of about 6,500 feet (2,000 m). Volcanism in the Pliocene epoch overtopped the existing Miocene volcanics of the Western Cascades Montane Highlands. Later, Pleistocene glaciation left numerous rock-basin lakes throughout the plateau. Sinuous, medium gradient streams cross the subdued, glaciated terrain. The region is extensively forested with mountain hemlock, Pacific silver fir, and subalpine fir, with some grand fir, noble fir, Douglas-fir, Engelmann spruce, and lodgepole pine, and an understory of vine maple, huckleberry, rhododendron, beargrass, twinflower, and wintergreen. Mountain meadows support sedges, dwarf willows, and tufted hairgrass. The region covers 1,909 square miles (4,940 km2) in Oregon and 310 square miles (803 km2) in Washington, running along the spine of the Cascades; an isolated pocket of this ecoregion can be found on Newberry Volcano southeast of Bend.
Cascades Subalpine/Alpine (4d)
The Cascades Subalpine/Alpine ecoregion is an area of high, glaciated, volcanic peaks rising above subalpine meadows, with cascading streams, glacial cirques, and tarns. Pleistocene glaciation reshaped the mountains above 6,500 feet (2,000 m), leaving moraines, glacial lakes, and U-shaped glacial canyons. Glaciers and permanent snowfields still occur on the highest peaks, decreasing from north to south. The vegetation is adapted to high elevations, cold winter temperatures, a short growing season, and a deep winter snow pack. Herbaceous and shrubby subalpine meadow vegetation and scattered patches of mountain hemlock, subalpine fir, and whitebark pine occur near the timberline. Wet meadows support Brewer's sedge, Holm's sedge, black alpine sedge, tufted hairgrass, and alpine aster. Elsewhere, there is bare rock. The region covers 388 square miles (1,000 km2) in Washington and 331 square miles (860 km2) in Oregon and contains many of the prominent volcanic peaks of the high Cascades, including Mount Rainier, Mount Adams, Mount Hood, Mount Jefferson, Three Sisters, Mount Bachelor, Diamond Peak, Mount Scott, and Mount McLoughlin.
High Southern Cascades Montane Forest (4e)
The High Southern Cascades Montane Forest ecoregion is an undulating, glaciated, volcanic plateau punctuated by isolated
buttes and cones. Many tarns occur. With an elevation that varies from 4,000 to 8,200 feet (1,200 to 2,500 m), it is an intermediate zone between the Southern Cascades and the Subalpine/Alpine zone. Cryic soils support mixed coniferous forests dominated by mountain hemlock, lodgepole pine, and Pacific silver fir; they are colder than the mesic and frigid soils of the Southern Cascades. Grand fir, white fir, and Shasta red fir also occur and become more common toward the south and east. Whitebark pine is found at high elevations. Understory plants include woodrush, Prince’s pine, lupine, and sidebells shinleaf. At the highest elevations, open meadows support Shasta buckwheat, Newberry knotweed, and Brewer's sedge. The region tends to be drier than the Cascade Crest Montane Forest, with a longer summer drought and more intermittent streams. The region covers 915 square miles (2,370 km2) in Southern Oregon and includes the lower elevations of Crater Lake National Park.
Southern Cascades (4f)
The Southern Cascades ecoregion is lower in elevation and less rugged than the surrounding regions and is characterized by gently sloping mountains and broad valleys. Elevation varies from 1,400 to 5,300 feet (430 to 1,620 m). The climate is drier than other parts of the Cascades, and the vegetation reflects the long summer drought. River and stream discharge are also significantly lower than in systems to the north. Western hemlock and western red cedar, which are indicator species in the Western Cascades ecoregions, decline southward in the Southern Cascades, and are replaced by Sierra Nevada species such as California incense-cedar, white fir, Shasta red fir, and sugar pine, with an understory of snowberry, twinflower, Oregon grape, serviceberry, golden chinkapin, and oceanspray. At lower elevations, Douglas-fir and ponderosa pine are prevalent. The region covers 1,414 square miles (3,660 km2) in Southern Oregon, in the South Umpqua and Rogue River watersheds, separated from the Western Cascades by the Calapooya Divide.