The Eastern Cascades Slopes and Foothills ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency (EPA) in the U.S. states of Oregon, Washington, and California. In the rain shadow of the Cascade Range, the eastern side of the mountains experiences greater temperature extremes and receives less precipitation than the west side. Open forests of ponderosa pine and some lodgepole pine distinguish this region from the Cascades ecoregion, where hemlock and fir forests are more common, and from the lower, drier ecoregions to the east, where shrubs and grasslands are predominant. The vegetation is adapted to the prevailing dry, continental climate and frequent wildfire. Volcanic cones and buttes are common in much of the region.[1][2]
The Eastern Cascades Slopes and Foothills ecoregion has been subdivided into ten Level IV ecoregions, as described below. Level IV mapping is not yet complete in California, and the information below includes only the sections in Washington and Oregon.
The high, unglaciated Yakima Plateau and Slopes ecoregion is characterized by plateaus, buttes, and canyons, with medium to high gradient permanent and intermittent streams and rivers on a surface of basalt. Natural springs occur, especially in the south. Elevation varies from 2500 to 5000 feet (762 to 1524 m). The dry continental climate supports open woodlands dominated by ponderosa pine and bitterbrush, with some Douglas-fir and Oregon white oak. Fire is an integral part of the ecosystem. The region covers 1,793 square miles (4,644 km2) in Washington, mainly on land belonging to the Yakama Nation.[2]
The Grand Fir Mixed Forest ecoregion is characterized by high, glaciated plateaus, mountains, and canyons containing high gradient streams and rivers. Scattered lakes occur in glacial rock basins. Elevation varies from 2200 to 6500 feet (671 to 1829 m). The frigid soils and snowy, continental climate support a mix of grand fir and Douglas-fir, with some ponderosa pine and western larch. Plants in the understory include vine maple, hazel, snowberry, and oceanspray. The region covers 812 square miles (2,103 km2) in Washington and 162 square miles (420 km2) in Oregon, on the eastern slopes of Mount Rainier, Mount Adams, and Mount Hood, and on Black Butte. It contains land belonging to the Yakama Nation and public land within the Wenatchee, Gifford Pinchot, Deschutes, and Mount Hood National Forests (including the Badger Creek Wilderness).[1][2]
The Oak/Conifer Foothills ecoregion is lower and drier than the Grand Fir Mixed Forest and more diverse than other parts of the Eastern Cascades. It consists of foothills, low mountains, plateaus, and valleys from 500 to 3500 feet (152 to 1067 m). Marine weather enters the region via the Columbia River Gorge, moderating the otherwise continental climate. As a result, soil, climate, and vegetation share characteristics of both eastern and western Oregon. The region is characterized by Oregon white oak woodlands and ponderosa pine forests in the east and Douglas-fir and western hemlock forests in the west. Some grasslands also occur. Understory plants include Idaho fescue, bluebunch wheatgrass, antelope bitterbrush, Oregon grape, hazel, and snowberry. Common land uses include forestry, recreation, grazing, rural residential development, orchards, and, in the valleys, grain and hay farming. The land is mostly privately owned. The region covers 563 square miles (1,458 km2) in Washington and 461 square miles (1,194 km2) in Oregon along the Columbia River corridor, including the lower reaches of the White Salmon and Klickitat River drainages.[1][2]
The Ponderosa Pine/Bitterbrush Woodland ecoregion has a terrain dominated by high, undulating volcanic plateaus and canyons, with permanent, medium gradient streams. Elevation varies from 2400 to 5200 feet (732 to 1585 m). Stream flow is consistent year-round, due to the volcanic hydrogeology. The well-drained, frigid soils are derived from Mazama Ash, which was produced by the catastrophic eruption of Mount Mazama about 6,845 years ago, and support nearly homogenous stands of ponderosa pine. Historically, frequent fires burned undergrowth, creating open groves of pines. Lodgepole pine is largely absent here. Understory vegetation varies with elevation; at lower elevations, antelope bitterbrush is important winter browse for deer. At higher elevations, greenleaf manzanita and snowberry are found. Riparian areas support mountain alder, stream dogwood, willows, and sedges. The region covers 1,077 square miles (2,789 km2) in Oregon, east of Mount Jefferson, Three-Fingered Jack, and the Three Sisters, in the Deschutes National Forest and on the Warm Springs Indian Reservation.[1][2]
The Pumice Plateau ecoregion is a high volcanic plateau, characteristically covered by thick deposits of Mount Mazama ash and pumice. Elevation varies from 4200 to 8300 feet (1280 to 2530 m). Residual soils are very deep, highly permeable, and subject to drought, with intermittent, low to medium gradient streams and spring-fed creeks and marshes. Freezing temperatures are possible any time of year. Ponderosa pine forests are common on slopes, with white fir at higher elevations. Colder depressions and flats, where pumice deposits are thickest, are dominated by lodgepole pine, with an understory of antelope bitterbrush and Idaho fescue. Riparian areas support mountain alder, stream dogwood, willows, and quaking aspen. The Pumice Plateau is the largest of the Eastern Cascades subregions, covering 4,236 square miles (10,971 km2) in Oregon between Bend and Klamath Falls. It contains extensive areas within the Deschutes and Fremont-Winema National Forests (including the Gearhart Mountain Wilderness) and the lower elevations of the Newberry National Volcanic Monument.[1][2]
The Cold Wet Pumice Plateau Basins ecoregion includes Sycan Marsh, Klamath Marsh, and La Pine Basin, which are surrounded by the Pumice Plateau but have distinct vegetation and topography. At an elevation of 4100 to 5200 feet (1250 to 1585 m), they function as cold air catch-basins during the winter, which results in lower minimum temperatures. Soils in the basins have water tables at or near the surface for significant periods of the year, in contrast to the soils of the Pumice Plateau. The La Pine Basin is underlain by thick lacustrine deposits that exhibit high groundwater levels during the spring snowmelt. It supports lodgepole pine stands, as well as wet, forested wetlands of lodgepole pine, willow, and aspen. Scattered ponderosa pine shrub forest is found on the driest soils. The Sycan and Klamath marshes support wetland meadow vegetation, including tules and tufted hairgrass. Marshes, lakes, reservoirs, wetland forests, and medium and low gradient rivers provide important habitat for migratory waterfowl. The region covers 651 square miles (1,686 km2) in Oregon, a mixture of private and public lands, including the Deschutes and Fremont-Winema National Forests and the Klamath Marsh National Wildlife Refuge.[1][2]
The Klamath/Goose Lake Warm Wet Basins ecoregion (named for Upper Klamath and Goose lakes) is drier than elsewhere in the eastern Cascades, yet it contains floodplains, terraces, and a pluvial lake basin. Elevation varies from 4000 to 5400 feet (1219 to 1646 m). A variety of wildrye, bluegrass, and wheatgrass species once covered the basins, but most of the wet meadows and wetlands have been drained for rural residential development, pasture, and cropland, including alfalfa, potatoes, and small grains. Potential vegetation includes bluebunch wheatgrass, Idaho fescue, antelope bitterbrush, big sagebrush, and low sagebrush on the steppes, with tules, cattails, and sedges in the wetlands. Several marshland wildlife refuges within the Klamath Basin National Wildlife Refuges Complex are key to preserving regional biodiversity, particularly at-risk bird and fish species. The region covers 1,039 square miles (2,691 km2) in Klamath and Lake counties, Oregon. Contiguous areas in California have not been mapped yet.[1][2]
The Fremont Pine/Fir Forest ecoregion contains steeply to moderately sloping mountains and high plateaus that rarely exceed timberline. Elevation varies from 5000 to 8000 feet (1524 to 2439 m). Residual soils are common in the region, in contrast to the Pumice Plateau, where soils have been deeply buried by pumice and ash. Reservoirs, a few glacial rock-basin lakes, many springs, and high gradient intermittent and ephemeral streams occur. The continental climate and diverse terrain support a range of vegetation types. Ponderosa pine and western juniper woodlands are common at lower elevations. White fir, sugar pine, whitebark pine, lodgepole pine, and California incense-cedar are found on north slopes and at higher elevations. Understory plants include snowberry, heartleaf arnica, Wheeler bluegrass, antelope bitterbrush, and longstolon sedge. The region covers 1,672 square miles (4,330 km2) in Oregon, mainly on public land within the Fremont-Winema National Forest. Contiguous areas in California have not been mapped yet.[1][2]
The Southern Cascades Slope ecoregion is a transitional zone between the Cascades ecoregion and the drier Eastern Cascade Slopes and Foothills, characterized by moderately sloping mountains with medium to high gradient streams. Elevation varies from 3600 to 6300 feet (1097 to 1920 m). It is higher than other subregions in the Eastern Cascades and typically receives greater precipitation. Forests of ponderosa pine blanket the mountainous landscape; white fir, Shasta red fir, Douglas-fir, and incense cedar grow at higher elevations. Understory plants include Idaho fescue, antelope bitterbrush, Ross' sedge, western fescue, snowberry, and golden chinkapin. The region covers 515 square miles (1,334 km2) in Oregon, south of Aspen Butte in the Klamath River watershed, including Bear Valley National Wildlife Refuge. Contiguous areas in California have not been mapped yet.[1][2]
The Klamath Juniper Woodland ecoregion is composed of undulating hills, benches, and escarpments covered with a mosaic of rangeland and woodland, at an elevation of 4400 to 6200 feet (1341 to 1890 m). Mean annual precipitation ranges from 12 to 20 inches (30 to 51 cm) per year. Western juniper grows on shallow, rocky soils with an understory of low sagebrush, Wyoming big sagebrush, bitterbrush, and bunchgrasses. Several species found in the shrub-steppe grasslands are uncommon in eastern Oregon, such as woolly wyethia, Klamath plum, and birchleaf mountain-mahogany. The diverse shrublands provide important wildlife habitat. Reservoirs dot the landscape and are important to lowland irrigation. The region covers 784 square miles (2,031 km2) in Oregon, south of Klamath Falls in the Lost River watershed, a mixture of public and private land. Contiguous areas in California have not been mapped yet.[1][2]
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