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Section M261G
Modoc Plateau

This section corresponds to most of the Modoc Plateau, which is related structurally to the Basin and Range Province and lithologically to the Columbia Plateau.  It is in MLRAs 21.

Geomorphology.  Northwesterly trending fault-block mountains and ridges with intervening basin-like grabens commonly interspersed with lake bed deposits, shield volcanoes, cinder cones or lava flows.  Modoc Plateau geomorphic province (part of the Basin and Range province flooded with volcanics related to those of the Cascade Ranges province).

Lithology.  Cenozoic volcanic and nonmarine sedimentary rocks and alluvial deposits.

Soil Taxa.  Alfisols, Andisols, Aridisols, Entisols, Histisols, Inceptisols, Mollisols and Vertisols in combination with mesic, frigid or cryic soil temperature regimes and xeric, aquic or aridic soil moisture regimes.

Vegetation.  Predominant potential natural communities include the Big sagebrush series, Western juniper series, Idaho fescue series, Bluebunch wheatgrass series, Ponderosa pine series, White fir series, Low sagebrush series, Jeffrey pine series, Lodgepole pine series, Aspen series and sedge meadow communities.

The following series are found throughout the section and are not restricted to or extensive in any subsection.  Series dominated by exotic plants are not listed under subsections unless they are extensive and stable.

Fauna.  Mammals include mule deer, pronghorn, black bear, mountain lion, coyote, bobcat, yellow-bellied marmot, wolverine, jack rabbit and porcupine.  Birds include eagles, hawks, owls, woodpeckers, falcons, osprey, quail and sage grouse.  The section contains wetlands that are important resting, feeding and nesting areas for migrating waterfowl.  Species of concern include the California and spotted owl (western part).  Species no longer occurring in the section include mountain sheep and sharp-tailed grouse.

Elevation.  3000 to 9900 feet.

Precipitation.  8 to 30 inches.

Temperature.  35° to 52°F.

Growing Season.  25 to 150 days.

Surface Water Characteristics.  Few slow flowing rivers and few slow to moderately rapid flowing streams, although most streams do not flow throughout the summer.  Rivers and streams flow in alluvial and bedrock controlled channels to the Sacramento and Klamath Rivers, or to basins within the Modoc Plateau or the Northwestern Basin and Range section.  Numerous small to very large lakes and reservoirs occur throughout the section.

Disturbance Regimes.

Land Use. Composition and successional sequence of some communities has changed because of plant and animal species introduced between the mid 1800’s and early 1900’s related to grazing, forestry and agriculture.

Cultural Ecology.  Humans have been utilizing the plateau for about 10,000 years, and have been an integral part of its ecology for 3,000 to 5,000 years.  Extensive prehistoric procurement and processing of obsidian resources have left vast areas of the plateau pockmarked and littered with lithic debitage.  Euroamerican influx into the area in the mid-1800’s, along the Oregon and California Trails, ushered in agricultural pursuits.  Contemporary attitudes and beliefs tend to be dominated by commodity oriented long-time resident values and a rural lifestyle.  The economy is dominated by government employment, but ranching and lumbering continue to be important.

Subsections.  The Modoc Plateau Section is divided into 16 subsections.


To obtain information about a particular subsection, click the subsection.


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