Appendix E: Regional Geophysical Data
APPENDIX E: REGIONAL GEOPHYSICAL DATA GEOPHYSICAL REGIONS We used the USGS uaternary deposits data, together with current topo- graphic data from the National Elevation Dataset ⅓-arc second Digital Elevation Model, and rainfall isohyets from the Sonoma County Water Agency, to divide the Laguna into geophysical regions. A study of surficial geology, precipitation, and topography revealed eighteen distinct geophysical regions. Defining these has proven to be especially useful in explaining why we see patterns of vegetation and the consequent patterns of human development throughout the watershed. Plate shows the eighteen geophysical regions of the Laguna. Their boundaries are well defined through the natural expression of rainfall pat- terns, surficial geology, elevation, soil, and vegetation. The immediate imprint of the rainfall pattern on the land is to create a natural landscape of softwood and hardwood forests, grasslands and chap- arral. Together with other natural ingredients, such as geological deposits, topographical features and soil characteristics, distinct vegetation zones become recognizable. BENNETT VALLEY This region is situated in the eastern half of the watershed and is wholly encompassed by the Matanzas region. Matanzas Creek itself forms the region’s western backbone. The region is called out for its distinct topog- raphy, which is gently tipped towards the west. The region enveloping Bennett Valley from the south, east and west, is characterized by steeper hills with drainage towards this bowl-shaped valley. From southeast to northwest, the region’s major axis is about three miles long. The valley is 472 Enhancing and Caring for the Laguna almost one and a half miles wide at its southern end and tapers down to about three-fourths of a mile in width at its northern end.
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