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Lithology and Stratigraphy. This subsection contains predominantly Pliocene and Quaternary marine and nonmarine sediments and recent alluvium in inland valleys and on the Santa Rosa Plain; and upper Pliocene marine sediments on the hills between the Santa Rosa Plain and the Pacific Ocean. Franciscan rocks of the Central and Coastal Belts are minor components in this subsection.
Geomorphology. This subsection contains moderately steep hills on upper Pliocene sediments that have been faulted and eroded to expose rocks of the Franciscan Complex, Quaternary nonmarine terraces, and floodplains. The elevation range is from sea-level up to about 900 feet. Fluvial erosion is the main geomorphic process on the coastal plain and nonmarine terraces. Fluvial erosion and deposition are active on the alluvial plains.
Soils. The soils on the rolling hills are mostly Ultic Haplustalfs. On upper Pliocene sediments of the Santa Rosa Plain they are Haploxerults, Pelloxererts, and Palexeralfs. On Quaternary terraces they are Durixeralfs, Albaqualfs, and Haploxeralfs. And on recent alluvium they are Fluvaquentic Haploxerolls and Pelloxererts. The soil temperature regimes are mesic and thermic inland, mesic on the rolling hills between the Santa Rosa plain and the Pacific Ocean, and isomesic along the coast. Soil moisture regimes are xeric (nearly ustic) and aquic on the Santa Rosa Plain and vicinity, and ustic, and possibly some udic, on the rolling hills west of the Santa Rosa plain and along the coast.
Vegetation. The predominant natural plant communities are Needlegrass grasslands and Valley oak series in the inland valleys. Northern claypan vernal pools occur on the Santa Rosa Plain, and Pacific reedgrass series and Needlegrass grasslands occur on the rolling hills westward to the coast. Coast live oak series is common on some leeward slopes in the rolling hills.
Surface Water. Water runs off to streams and alluvial plains
moderately rapidly, but it accumulates in slight depressions on alluvial
plains. The ephemerally flooded depressions are called vernal pools.
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