Natural Resources
Conservation Service
Ecological site AX001X04X001
Mesic Udic Riparian Forest
Last updated: 5/07/2024
Accessed: 11/21/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 001X–Northern Pacific Coast Range, Foothills, and Valleys
This long and narrow resource area stretches along the Pacific Border Province of the Pacific Mountain System in Oregon and Washington. The area is bounded by the Olympic Mountains on the north and the Klamath Mountains on the south. Most of the area consists of hills and low mountains with gentle to steep slopes. The parent materials are composed primarily of young Tertiary sedimentary rocks with some minor volcanic rocks. Glacial till and outwash deposits are found in the northern half of the area within Washington. In the far southern portion of the area, near the Klamath Mountains, the sedimentary rocks are older and some have been metamorphosed. The average annual precipitation ranges from 60 to 200 inches, increasing with elevation.
The dominant soil orders in this MLRA are Andisols, Inceptisols, and Ultisols. Soil depth ranges from shallow to very deep. While most soils in the area are well drained and occur on foothills, mountain slopes and ridges, floodplain and depressional soils can range from well drained to very poorly drained. Soil textures are typically medial, loamy, or clayey. The dominant soils in the area have a mesic or frigid soil temperature regime and a udic soil moisture regime; however, soils with an aquic soil moisture regime or cryic soil temperature regime do occur.
LRU notes
The Southern Pacific Coast Range land resource unit (LRU 4) of MLRA 1 is located in central to southern Oregon State. The LRU extends from the Siletz River to the Rogue River and is bounded on the west by MLRA 4a Sitka Spruce Belt and MLRA 2 Willamette and Puget Sound Valleys to the east. Several major rivers carved valleys through the landscape depositing more recent alluvium. These include the Alsea, Coos, Coquille, Green, Yachats, Siletz, Siuslaw, Umpqua, and Rogue Rivers.
Ecological site concept
This ecological site is found on the western Coast Range in the Pacific Northwest from central to southern Oregon. It is found at low to middle elevations in narrow to wide riparian corridors on moderate to steeper gradient streams. These areas are subject to stream overflow. Riparian ecological sites typically differ in topography, vegetation, geomorphology, and microclimate from the surrounding uplands of the forest ecosystem (Dwire, 2003).
The most common overstory species are bigleaf maple (Acer macrophyllum), red alder (Alnus rubra), and cascara (Frangula purshiana). California laurel (Umbellularia californica), tanoak (Notholithocarpus desiflorus), and California live oak (Quercus chrysolepis) occur south of the Alsea River, at times quite prolifically (Pabst, 1999). Black cottonwood (Populus balsamifera spp. trichocarpa) is not present, or less than 5% cover. Douglas-fir (Pseudotsuga menziesii) is the most common conifer component, but typically limited to less than 25% cover (Hibbs, 2000). Regeneration is restricted by canopy cover and often limited to gaps where sunlight is most available and mineral soil is exposed from scouring (Pabst, 1999). Understory species diversity is greatest near the streams as a result of erosion and deposition creating openings for opportunistic species as well as the abundance of microsites which create unique environments (Spies, et. al, 2002). Common understory species include salmonberry (Rubus spectabilis), stink currant (Ribes bracteosum), thimbleberry (Rubus parviflorus), elderberry (Sambucus racemosa), vine maple (Acer circinatum), western swordfern (Polystichum munitum), and Oregon oxalis (Oxalis oregana).
The most common natural disturbance is flooding, with the volume and longevity of the flooding determining the effect on the dynamics of the forest. Although wildfire is uncommon in this ecological site (greater than 450-year return interval) when it does occur, it may be stand replacing (Balian, 2005). Fallen trees with exposed root systems and large woody debris is common.
Associated sites
AX001X04X002 |
Mesic Udic Flood Plain Forest Mesic Udic Flood Plain Forest is located in broad flood plain corridors of large river systems. Mesic Udic Riparian Forest is often found along the tributaries that lead to Mesic Udic Flood Plain Forest river systems. |
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Table 1. Dominant plant species
Tree |
(1) Acer macrophyllum |
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Shrub |
(1) Rubus spectabilis |
Herbaceous |
(1) Polystichum munitum |
Legacy ID
F001XD001OR
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