Natural Resources
Conservation Service
Ecological site F006XB802OR
Mesic Xeric North Slopes 15-25 PZ
Last updated: 9/11/2023
Accessed: 11/14/2024
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): 006X–Cascade Mountains, Eastern Slope
Stretching from northern Washington to southern Oregon, MLRA6 encompasses the mountain slopes, foothills, elevated plateaus and valleys on the eastern slopes of the Cascade mountains. This MLRA is a transitional area between the Cascade Mountains to the west and the lower lying Columbia Basalt Plateau to the east.
Situated in the rain shadow of the Cascade Crest, this MLRA receives less precipitation than portions of the cascades further west and greater precipitation than the basalt plateaus to the east. Geologically, the majority of the MLRA is dominated by Miocene volcanic rocks, while the northern portion is dominated by Pre-Cretaceous metamorphic rocks and the southern portion is blanketed with a thick mantle of ash and pumice from Mount Mazama. The soils in the MLRA dominantly have a mesic, frigid, or cryic soil temperature regime, a xeric soil moisture regime, and mixed or glassy mineralogy. They generally are moderately deep to very deep, well drained, and loamy or ashy. Biologically, the MLRA is dominated by coniferous forest, large expanses of which are dominated by ponderosa pine, Douglas-fir or lodgepole pine. Areas experiencing cooler and moister conditions include grand fir, white fir, and western larch while the highest elevations include pacific silver fir, subalpine fir and whitebark pine.
Economically, timber harvest and recreation are important land uses in these forests. Historically, many of these forests would have experienced relatively frequent, low and mixed severity fire favoring the development of mature forests dominated by ponderosa pine or Douglas-fir. In the southern pumice plateau forests, less frequent, higher severity fire was common and promoted the growth of large expanses of lodgepole pine forests.
LRU notes
This unit is characterized by ash mantled lava flows and glacial outwash plains on lower mountain slopes and foothills of the East Cascades in Oregon. Vegetation is largely dominated by forests of ponderosa pine with transitional dry mixed conifer forests where Douglas-fir and grand fir are sub dominant occurring in areas with greater effective precipitation.
Historically, these forests have been influenced by a fire regime whereby frequent to moderately frequent, low and mixed severity fires would have favored the development of open stands of mature ponderosa pine. The climate of this unit is cool and dry with a predominately xeric soil moisture regime and frigid soil temperature regime.
Geologically, underlying lithologies are dominated by Quaternary and late Tertiary basalt and basaltic andesite as well as mixed grain sediments deposited during Pleistocene glacial retreat. Unlike the nearby pumice plateau, this unit lacks the coarse pumice fragments that dominate the soil profile and cooler temperatures that favor lodgepole pine. This unit is south of the climate influences of the Columbia gorge and therefore does not support woodlands of Oregon white oak.
Classification relationships
Plant Associations of the Commercial Forest of the Warm Springs Indian Reservation (Marsh 1987):
Ponderosa pine – Douglas-fir / Snowberry
Ponderosa pine – Douglas-fir / Snowberry (Mutton)
Landfire Biophysical Setting (Landfire 2007):
0710531: Rocky Mountain Ponderosa Pine Woodland and Savanna (Landfire 2007)
Ecological site concept
This site represents a dry forest community at the transition zone between the foothills of the eastern slopes of the Oregon cascades and the Columbia plateau. The distribution of this site is largely within the vicinity of Mutton Mountain yet it may occur elsewhere. The historical reference plant community is that of a ponderosa pine (Pinus ponderosa), Douglas-fir (Pseudotsuga menziesii) forest with Oregon white oak (Quercus garryana) found sporadically in openings, an herbaceous layer characterized by heartleaf arnica (Arnica cordifolia) and shrub layer dominated by common snowberry (Symphoricarpos albus).
This site is often found adjacent to drier ponderosa pine – bitterbrush (Purshia tridentata) communities and sites with shallow, clayey soils that include western juniper (Juniperus occidentalis) as a common woody associate. In comparison to adjacent East Cascade foothill plant communities which are not highly influenced by aspect, this site typically occupies north slopes which increase effective moisture and therefore encourage occupancy by Douglas-fir.
This site exists toward the southern-most extent of the white oak woodlands of the Northern Oregon cascades. In comparison to areas with greater maritime climate influence to the north, it supports a lower composition of white oak due to fewer frost free days within this precipitation range allowing Douglas-fir and ponderosa pine to attain greater dominance.
This is a provisional ecological site that groups characteristics at a broad scale with little to no field verification and is subject to extensive review and revision before final approval. All data herein was developed using existing information and literature and should be considered provisional and contingent upon field validation prior to use in conservation planning.
Associated sites
F006XB800OR |
Frigid Xeric Foothills 20-30 PZ Upslope positions, frigid soil temperature regime |
---|---|
R006XB208OR |
Shallow Slopes 14-20 PZ Adjacent south aspects with shallow soils, non-forested plant community |
F006XY710OR |
Mesic Xeric Foothills 14-20 PZ Occupying non-north aspects and warmer slope positions where the sites co-occur |
Similar sites
F006XY709OR |
Mesic Xeric Foothills 20-25 PZ More gentle slopes, higher precipitation, occupying all aspects, QUGA absent |
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F006XY710OR |
Mesic Xeric Foothills 14-20 PZ More gentle slopes, occupying all aspects, warmer landscape positions and somewhat lower elevations |
F006XB800OR |
Frigid Xeric Foothills 20-30 PZ Somewhat higher elevations, frigid soil temperature regime, out of the modified maritime zone, QUGA absent |
Table 1. Dominant plant species
Tree |
(1) Pseudotsuga menziesii |
---|---|
Shrub |
(1) Symphoricarpos albus |
Herbaceous |
Not specified |
Click on box and path labels to scroll to the respective text.
Ecosystem states
T1B | - | Extensive timber harvest |
---|---|---|
R2A | - | Forest restoration, stand replacing fire |
State 1 submodel, plant communities
Communities 1 and 5 (additional pathways)
1.1A | - | Fire cycle(s) missed |
---|---|---|
1.1B | - | Historical disturbance regime sustained for extended duration |
1.2B | - | High severity, stand replacing fire occurs |
1.2A | - | Mixed severity fire occurs |
1.3B | - | High severity, stand replacing fire occurs |
1.3A | - | Historical fire regime sustained for extended duration |
1.4A | - | High severity, stand replacing fire occurs |
1.4B | - | Fire cycle(s) missed |
1.5A | - | High severity, stand replacing fire occurs |