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BOARD00165
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Last modified
8/16/2009 2:46:08 PM
Creation date
10/4/2006 6:32:44 AM
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Board Meetings
Board Meeting Date
3/24/2003
Description
Flood Section - Special Contract Provisions for Montezuma County
Board Meetings - Doc Type
Memo
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<br />\~ .-' <br /> <br />'~ (;OL:~~-:'~~~~LEY <br /> <br />. <br /> <br />Although the old Corps of Engineer maps might be ~onsidered <br />acceptable in that they are only supposed to be accurate plus or <br />m:lnus2;S feet, that is only satisfactory for topographical <br />purposes such as calculation of volumes of cut or fill. However <br />for hydrological purposes such as predicting floods"such lack of <br />precision and inaccuracies are clearly unacceptable. Thus the <br />flood analyses used in issuing permits for mining along the river, <br />based on those old maps, are highly inaccurate. <br /> <br />In addition the earthworks linked to the gravel pits have,further <br />changed the topography, including lowered floodplains due to <br />stripping of topsoil, and the presence of dikes and stockpiles <br />which interfere with normal flood flows. These all create greater <br />risks of flooding. <br /> <br />1. LosS of floodplain due to dikes and temporary stockpiles <br /> <br />The large dikes and stockpiles constructed around the Line Camp <br />pits and at the Koenig site, reduce the flood-absorption capacity <br />of the floodplain at those sites. Any flood peak coming through <br />would be restricted to the main channel. This constriction would <br />cause a back-up in flood level upstream, and an increase in <br />velocities downstream. The increased velocities could cause the <br />river to jump its banks downstream, as well. <br /> <br />2. Trapping effect of gravel pits on flood peaks <br /> <br />If the floods inundate the pits, there would be a temporary <br />diversion of the main flow out of the channel and into the pits. <br />This would' provide only a temporary storage .off loodwaters,' about <br />the same as the normal floodplain. But it would run the risk of <br />diverting the main flow, as described below. <br /> <br /> <br />3. Diversion effects of dikes on floods <br /> <br />. <br /> <br />In the Line Camp and the Koenig areas, depending on the current <br />condition of the dikes and stockpiles, the trapping effect could <br />easily cause a buildup of waters behind the dikes, with the risk <br />ofa disastrous breakthrough. The dikes ,are not reinforced or <br />armored, thus they CQuld easily erode and break. This would <br />release a wall of water doWnstream. <br /> <br />Especiplly at the Line Camp pits, it is likely that the flood flow <br />would seek an outlet in the low area near the highway, with the <br />possibility that the flood could jump out of the river channel on <br />the eastern side near the mountain, and move, to the western side <br />against the, highway, following the low swale. This would put <br />several homes and Properties at risk downstream. <br /> <br />Dolores River <br /> <br />9/12/02 <br /> <br />page 2 <br /> <br />P.O. Bo)( 720 - Dolores, Colorado 81323 - V,S. of America <br />Telephone: (970) 882-7778 - Fax: (970) 882-7779 . e-mail: snail@fone.net <br />
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