Ecological site group description
This ESG is typically found on the eastern side of the Southern Cascade mountains on backslopes from 4400 - 7200 feet, but most typically between 4400 - 6500 ft on slopes from 5-60%, but most typically 10-50%.
The average annual precipitation in this MLRA is typically 20 to 65 inches but can range from 13 to 123 inches (176 to 2,471 millimeters). This ESG averages 20-60 inches. It is lowest in the lower valleys and highest on the mountain peaks. The precipitation falls mainly from fall to spring, mostly as snow. Winter precipitation is from Pacific storms that are frontal in nature. The amount of precipitation decreases from west to east. Summers are typically warm and dry, but there are occasional thunderstorms. The average annual temperature is 27 to 61 degrees F (-3 to 16 degrees C). The frost-free period for this ESG is generally less than 100 days, and the freeze-free period averages 215 days and ranges from 85 to 350 days. The lowest annual temperatures and the shortest freeze-free periods occur in the mountains.
Soils for this ESG are shallow to moderately deep to lithic or paralithic contact and are typically colluvium and residuum derived from volcanic sources. Soil textures are most typically gravelly and very gravelly sandy loams, and sometimes stony loams.
Representative soils include:
Goulder, a Ultic Haploxerands
Rivalier, a Typic Vitrixerands
Eaglelake, a Vitrandic Haploxeralfs
Outland, a Vitrandic Haploxeralfs
Weste, a Andic Haploxeralfs
Easte, a Vitrandic Haploxerepts
Mounthat, a Pachic Melanoxerands
Swainow, a Ultic Haploxerands
This ESG is part of the Sierran mixed conifer habitat type and is an assemblage of conifer and hardwood species that forms a multilayered forest. Historically, burning and logging have caused wide variability in stand structure, resulting in both even-aged and uneven-aged stands. Virgin old-growth stands where fire has been excluded are often two-storied, with the overstory comprised of mixed conifer and the understory white fir and incense-cedar. Forested stands form closed, multilayered canopies with nearly 100 percent overlapping cover. When openings occur, shrubs are common in the understory. Closed canopy stand distribution is both extensive and patchy depending on scale, site, slope, soils, microclimate, and history.
At maturity, the dominant conifers range from 30 to 60 m (100 to 200 ft) tall with a highly variable basal areas of about 17 to 26 sq m (180 - 280 sq ft). Diameter breast height at maturity for pines and Douglas-fir is commonly greater than 1 m (40 in); white fir greater than 0.9 m (35 in) is common. Fuel loading in stands heavy with pine may reach 27,000 kg/ha (70 to 80 t/ac) in natural stands; whereas fuel loading in stands heavy with fir may reach 16,000 kg/ha (40 to 50 t/ac).
Five conifers and one hardwood typify the mixed conifer forest white fir, Douglas-fir, ponderosa pine, sugar pine, incense-cedar, and California black oak. White fir tends to be the most ubiquitous species (though most often a minor overstory component) because it tolerates shade and has the ability to survive long periods of suppression in brush fields Douglas-fir dominates the species mix in the north, but is absent south of the Merced River. Ponderosa pine dominates at lower elevations and on south slopes. Jeffrey pine commonly replaces ponderosa pine at high elevations, on cold sites, or on ultramafic soils. Red fir is a minor associate at the highest elevations. Sugar pine is found throughout the mixed conifer type. Black oak is a minor, but widespread, component in mixed conifer stands. Though black oak does best on open sites, it is maintained under adverse conditions such as shade, ridge tops, and south slopes where conifers may regenerate in its shade. This ESG is primarily dominated by white fir, ponderosa pine, Douglas-fir, incense cedar, snowbrush, squaw carpet, manzanita and bottlebrush squirreltail.
California Wildlife Habitat Relationships System
California Department of Fish and Game
California Interagency Wildlife Task Group
Barbara H. Allen (2005)
Major Land Resource Area
Southern Cascade Mountains
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