Areas of serpentine soil are currently yielding a profusion of native wildflowers along the Peninsula Watershed ridges.
Serpentine soil is derived from California’s state rock—the greenish metaphoric serpentine rock originating from the earth’s mantle. Serpentine rock outcrops are closely associated with California fault lines. The soil is high in magnesium and iron, but low in calcium, aluminum, and nutrient-rich clay, so that it is thin and inhospitable to many plant types. Its plant communities are typically composed of stubby, low-growing native grasses and small herbaceous plants.