Eastern Cascades Slopes and Foothills (ecoregion)

This article is about the ecoregion designated by the EPA. For the mountains, see Cascade Range.

Eastern Cascades Slopes and Foothills ecoregion
The Pumice Plateau, looking west toward the Cascade Volcanoes
Eastern Cascades Slopes and Foothills (9)
Ecology
Borders	Cascades (4) Sierra Nevada (5) Columbia Plateau (10) Blue Mountains (11) North Cascades (77) Klamath Mountains (78) Northern Basin and Range (80)
Geography
Country	United States
States	Oregon, Washington and California
Coordinates	44°N 122°W / 44°N 122°W / 44; -122Coordinates: 44°N 122°W / 44°N 122°W / 44; -122

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.

Level IV ecoregions

Level IV ecoregions in the Eastern Cascades Slopes and Foothills in Washington and Oregon. Contiguous areas in California have not been mapped yet. (Full map).

Yakima Plateau and Slopes (9a)

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]

Grand Fir Mixed Forest (9b)

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]

Oak/Conifer Foothills (9c)

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]

Ponderosa Pine/Bitterbrush Woodland (9d)

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]

Pumice Plateau (9e)

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]

Cold Wet Pumice Plateau Basins (9f)

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]

Klamath/Goose Lake Warm Wet Basins (9g)

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]

Fremont Pine/Fir Forest (9h)

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]

Southern Cascades Slope (9i)

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]

Klamath Juniper Woodland (9j)

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]

Gallery

References

1 2 3 4 5 6 7 8 9 10 This article incorporates public domain material from the United States Geological Survey document: Thorson, T.D., Bryce, S.A., Lammers, D.A. et al. "Ecoregions of Oregon" (PDF). (color poster with map, descriptive text, summary tables, and photographs; with a Reverse side).
1 2 3 4 5 6 7 8 9 10 11 This article incorporates public domain material from the United States Geological Survey document: Pater, D., Bryce, S.A., Kagan, J. et al. "Ecoregions of Western Washington and Oregon" (PDF). (color poster with map, descriptive text, summary tables, and photographs; with a Reverse side).

Level III Ecoregions in Oregon

Marine West Coast Forest	1 Coast Range 3 Willamette Valley

Northwestern Forested Mountains	4 Cascades 9 Eastern Cascades Slopes and Foothills 11 Blue Mountains 78 Klamath Mountains

North American Deserts	10 Columbia Plateau 12 Snake River Plain 80 Northern Basin and Range

as defined by the United States Environmental Protection Agency

Level III Ecoregions in the United States

Marine West Coast Forest	1 Coast Range 2 Puget Lowland 3 Willamette Valley 111 Ahklun and Kilbuck Mountains 113 Alaska Peninsula Mountains 115 Cook Inlet 119 Pacific Coastal Mountains 120 Coastal Western Hemlock-Sitka Spruce Forests

Northwestern Forested Mountains	4 Cascades 5 Sierra Nevada 9 Eastern Cascades Slopes and Foothills 11 Blue Mountains 15 Northern Rockies 16 Idaho Batholith 17 Middle Rockies 19 Wasatch and Uinta Mountains 21 Southern Rockies 41 Canadian Rockies 77 North Cascades 78 Klamath Mountains 105 Interior Highlands 116 Alaska Range 117 Copper Plateau 118 Wrangell Mountains

Mediterranean California	6 Southern and Central California Chaparral and Oak Woodlands 7 Central California Valley 8 Southern California Mountains

North American Deserts	10 Columbia Plateau 12 Snake River Plain 13 Central Basin and Range 14 Mojave Basin and Range 18 Wyoming Basin 20 Colorado Plateaus 22 Arizona/New Mexico Plateau 24 Chihuahuan Deserts 80 Northern Basin and Range 81 Sonoran Basin and Range

Temperate Sierras	23 Arizona/New Mexico Mountains

Great Plains	25 Western High Plains 26 Southwestern Tablelands 27 Central Great Plains 28 Flint Hills 29 Central Oklahoma/Texas Plains 30 Edwards Plateau 31 Southern Texas Plains 34 Western Gulf Coastal Plain 40 Central Irregular Plains 42 Northwestern Glaciated Plains 43 Northwestern Great Plains 44 Nebraska Sand Hills 45 Piedmont 46 Northern Glaciated Plains 47 Western Corn Belt Plains 48 Lake Agassiz Plain

Eastern Temperate Forest	32 Texas Blackland Prairies 33 East Central Texas Plains 35 South Central Plains 36 Ouachita Mountains 37 Arkansas Valley 38 Boston Mountains 39 Ozark Highlands 51 North Central Hardwood Forests 52 Driftless Area 53 Southeastern Wisconsin Till Plains 54 Central Corn Belt Plains 55 Eastern Corn Belt Plains 56 Southern Michigan/Northern Indiana Drift Plains 57 Huron/Erie Lake Plains 59 Northeastern Coastal Zone 60 Northern Appalachian Plateau and Uplands 61 Erie Drift Plain 63 Middle Atlantic Coastal Plain 64 Northern Piedmont 65 Southeastern Plains 66 Blue Ridge 67 Ridge and Valley 68 Southwestern Appalachians 69 Central Appalachians 70 Western Allegheny Plateau 71 Interior Plateau 72 Interior River Valleys and Hills 73 Mississippi Alluvial Plain 74 Mississippi Valley Loess Plains 75 Southern Coastal Plain 82 Laurentian Plains and Hills 83 Eastern Great Lakes and Hudson Lowlands 84 Atlantic Coastal Pine Barrens

Northern Forests	49 Northern Minnesota Wetlands 50 Northern Lakes and Forests 58 Northeastern Highlands 62 North Central Appalachians

Tropical Wet Forests	76 Southern Florida Coastal Plain

Southern Semi-Arid Highlands	79 Madrean Archipelago

Taiga	101 Arctic Coastal Plain 102 Arctic Foothills 103 Brooks Range 104 Interior Forested Lowlands and Uplands 106 Interior Bottomlands 107 Yukon Flats 108 Ogilvie Mountains

Tundra	109 Subarctic Coastal Plains 110 Seward Peninsula 112 Bristol Bay-Nushagak Lowlands 114 Aleutian Islands

as defined by the United States Environmental Protection Agency

This article is issued from Wikipedia - version of the 11/29/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.