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PROJ00109
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Last modified
5/9/2011 10:59:42 AM
Creation date
10/5/2006 11:36:12 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153347
Contractor Name
Starkville, Town of
Contract Type
Loan
Water District
19
County
Las Animas
Bill Number
SB 78-69
Loan Projects - Doc Type
Feasibility Study
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Item 6. Provide a new six (6) inch distribution line from the <br />middle storage tank to the Town limits and loop the town with <br />a 6 inch line. In addition, add fire hydrants to gain a reasonable <br />fire protection system. <br /> <br />Item 7. Provide additional storage of raw water or treated water. <br />Raw water storage can be developed by using a low head dam on <br />C1ear Creek. Initial calculations show that a 40 ft. thin arch <br />dam cou1d develop about 2.5 million cubic feet of storage or 100 <br />days of town usage; a 20 ft. dam would develop about 50 days usage. <br />It is believed because of the excellent sandrock formations that <br />a thin arch dam would be equivalent in costs to a potable ground <br />storage tank of equal capacity. At the present time when fully <br />utilized, the Town has about 25 days storage. <br /> <br />Geologic Formations <br /> <br />The watershed lies within three basic geologic formations <br />which are: Basic lava flows and flow breccias (Tep); Poison <br />Canyon Formations (Tpc) , and Raton Formation (Tka). These form- <br />ations are important because combined they create the spring flow <br />conditions around Fishers Peak. In addition, the Raton Formations <br />should provide excellent foundation materials for building storage <br />facilities, either dams or tanks. <br /> <br />Figure 5 illustrates the Geologic Formations discussed above. <br />Figure 4 indicates the same geologic area and the landslide con- <br />ditions around Fishers Peak. The landslide areas are shown in <br />black on Figure 4. The black area matches closely the Poison <br />rock formations. Comparisons of these geologic formations with <br />the general topographic map, Figure 3, provide an insight to the <br />spring flows. The springs are surfacing at the toe of the land- <br />slide areas which also conforms to the plane difference of the <br />Poison and Raton Formations shown on Figure 5. <br /> <br />~ <br /> <br />~ <br /> <br />23 <br /> <br />~ <br />
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