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Appendix 2 <br />"ALLUVIAL VALLEY FLOOR" <br />Legislative Directions and Interpretations <br />Definition of Alluvial Valley Floor Consistent with HR 9725: <br />"'alluvial valley floors' means the unconsolidated s <br />deposits holding streams where water availability i <br />for subirrigation or flood irrigation agricultural <br />Source - 701(27) HR 25(94th) <br />FURTHER DESCRIPTION <br />"Alluvial valley floors refers to those unconsolidated deposits formed by streams <br />(including their meanders) where the ground water level is so near the surface that <br />it directly supports extensive vegetation or where flood stream flows can be diverted <br />for flood irrigation." <br />Source - p. 65, Conference Report HR 9725 (95th). <br />".,.alluvial valley floors are the upper, near - horizontal surface of the unconsoli- <br />dated stream -laid deposits which border perennial, intermittent, or ephemeral <br />streams. The alluvium that makes up the stream -laid deposits is composed of clay, <br />silt, sand, gravel, or similar detrital material that has been, or is being, trans- <br />ported and deposited by streams. Alluvial valleys within this definition are tra- <br />versed by perennial or intermittent streams or by ephemeral stream channels: are <br />irrigated in most years by diversion of natural flow or ephemeral flood flow on the <br />modern flood plain and adjacent low terraces, or by subirrigation of the flood plain <br />by underflow: and are used for the production of hay and other crops that are an in- <br />tegral part of an agricultural operation." <br />Source - ibid. <br />"Excluded...are the colluvial and other superficial deposits that normally occur <br />along the valley margins, are higher than the modern flood plain and low terraces, <br />are not irrigated by diversion of natural flow or by ephemeral flood flow, and are <br />not subirrigated by underflow." <br />Source - ibid. <br />"Alluvial valley floors do not include upland areas which are generally overlain by <br />a thin veneer of colluvial deposits composed chiefly of debris from sheet erosion, <br />deposits by unconcentrated runoff or slope wash, together with talus, other mass <br />movement accumulation and wind blown deposits." <br />Source - p. 83, Conference Report HR 25(94th) <br />".,.alluvial valley floors must be (an) integral part of a drainage network that tra- <br />verses the area...These are part of a through flowing stream (hydrologic) system and <br />are not small areas of Isolated internal drainage." <br />Source - p. 65, Conference Report HR 9725(95th) <br />"Some characteristics of alluvial valley floors which are essential for agricultural <br />areas include: (l) sufficient runoff to allow for flood water irrigation each year; <br />(2) development of flood plain and low terraces where water can be spread easily <br />without significant mechanical alteration of the surface; and (3) shallow ground <br />water where subirrigation is used and (which) therefore requires a minimum of valley <br />floor dissection so that ground water is not drained." <br />Source - pp. 82 -83, Conference Report HR 25(94th) <br />