
 | Geology
of San Marcos Foothills
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Vegetation How
Geology Influences the Vegetation in the Foothills
Vegetation in the foreground
changes abruptly from grassland over Rincon Shale to brush over Vaqueros Sandstone |  |
Streambed
Alluvium High porosity in the alluvial gravels
and sands allows good drainage for water that runs year-round. Thick brush, poison
oak, willows, and oaks thrive in the alluvium of the streambeds. | Fanglomerate
Oak savannah is the typical
cover for the broad, high sweeps of the Fanglomerate. This area contains sandy
ground filled with boulders, and grassland dotted with occasional oaks. | Rincon
Shale Grasslands in the lower elevations are underlain
by a dark, thick clay soil that has weathered from the Rincon Shale. Grasses can
tolerate this area where the clay soil is characterized by low porosity, swelling
when wet, and shrinkage cracks when dry. | Vaqueros
Sandstone Scrubby brush, yucca and some oak grow
in the steeper slopes underlain by the Vaqueros Sandstone. Between rocky outcrops,
the soil is tan and sandy with good drainage. | Sespe
Redbeds Heavy brush and chaparral
grow in the silty soils of the Sespe redbeds. Where there is more sand present,
some grasses grow as well. Local avocado farmers take advantage of the Sespe soils
for their orchards. These can be seen in abundance along Casitas Pass Road below
Carpinteria, and to a lesser extent in some of the Sespe hills north of the Foothill
property. |
Geology
of the San Marcos Foothills by Susan Bartz
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