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The river is flanked by a dense expansion of large trees and brush in the course of the majority of its course, and during Element of the yr floor-h2o discharge by evapotranspiration almost certainly exceeds discharge to the stream. Wellington Upland (Spot C)
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The lithology in the sediments underling the valley is quite heterogeneous, and generalizations pertaining to favorable web-sites for ground-h2o developments can't be produced from the info offered. Locally the complete portion could possibly be composed of silt, and a brief distance absent sand and fantastic gravel could predominate.
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The area has been divided into two subareas on the basis of your incidence of ground h2o. The 2 subareas are shown on Figure 20 as being the Loess-sand Subarea (D1) along with the Loess-shale Subarea (D2). Subarea D1 is largely confined to the uplands but does include things like the modest abandoned valley during the southwest corner on the County in which floor-drinking water circumstances are identical. In Subarea D1 more info the floor materials is loess that ranges in thickness from the featheredge to about 40 toes. The loess is underlain by deposits of sand and gravel made up of some silt.