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Project Level Watershed Analysis McBride Springs Campground ...

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Riparian Reserves are applied along both sides of rivers,<br />

stream, lakes and wetlands. Riparian Reserves appear as<br />

natural corridors throughout the Matrix. 3<br />

Management activities are evident but subordinate to the<br />

viewer within this area.<br />

Supplemental Management Direction includes:<br />

“Manage for a high level of water quality of important domestic<br />

water sources at …<strong>McBride</strong> <strong>Springs</strong>…” 4<br />

Water samples are taken at all developed recreation sites on the forest and<br />

sent to a water quality laboratory for analysis and approval for culinary use<br />

prior to opening the campground for the public. 5<br />

The upper two-thirds of the watershed is public land while the lower third includes the city<br />

of Mount Shasta and private land ownership. General characteristics for the project and<br />

watershed area are shown in the following table:<br />

Characteristics <strong>Project</strong> Area <strong>Watershed</strong> <strong>Analysis</strong> Area<br />

Area (square miles) 10 acres 7,803 acres<br />

Elevation Range (feet)<br />

The elevation of the project area<br />

ranges between 4800 to 5000 feet.<br />

Elevations range from 7623 feet on<br />

Mount Shasta to approximately 4800.<br />

Relief (Slope Gradients)<br />

Slopes in the project area are<br />

Upper slopes in the watershed are<br />

generally 5% becoming greater than very steep, greater than 100%; mid-<br />

10% upslope and downslope from the<br />

project area.<br />

slopes, 100%; alluvial fan, greater<br />

than 10%.<br />

Aspect South – facing South - facing<br />

Geology<br />

Basalt and andesite boulders lie Andesitic strato-volcano with basalt<br />

above the campground, forming a<br />

colluvial fan with finer material<br />

downslope of the campground.<br />

ridges.<br />

Geomorphology<br />

At base of basalt lava flow adjacent Slopes are formed by lava flow<br />

to large drainage with evidence of features forming ridges on a more<br />

frequent avalanche and debris flow uniform flank as well as frequent<br />

activity.<br />

rock falls.<br />

Hydrology<br />

Snowmelt during the warmer summer<br />

months activates several small<br />

Intermittent streams and springs<br />

occur within the analysis area<br />

intermittent springs and streams in includes a portion of a narrow,<br />

the project area. During very wet avalanche dominated drainage,<br />

periods, closure of some campsites is<br />

required.<br />

Cascade Gulch, lying east of the<br />

project area. Infiltration rates into<br />

the coarse boulder dominated<br />

substrate is high. Intermittent flow<br />

from infrequent rapid snowmelt<br />

events bypasses the project area.<br />

Vegetation<br />

White fir, ponderosa pine, incense Mixed conifer forest with dense<br />

(Forested Areas)<br />

cedar with occasional Douglas fir.<br />

Ponderosa pine and incense cedar<br />

understory and brushfields of<br />

Arctostaphylos and Ceanothus<br />

contains dwarf mistletoe. Annosus occur in the watershed.<br />

3 LRMP Ch. 4-84 to 85.<br />

4 LRMP Ch. 4-86.<br />

5 Results for the <strong>McBride</strong> <strong>Campground</strong> water tests are available on file at the Mount Shasta Ranger District.<br />

<strong>Project</strong> <strong>Level</strong> <strong>Watershed</strong> <strong>Analysis</strong> <strong>McBride</strong> <strong>Springs</strong> <strong>Campground</strong> Diseased Trees Removal <strong>Project</strong>

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