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<br /> <br />112 <br /> <br />: WATERLA W REVIEW <br /> <br />Volume 5' <br /> <br />, <br />IV. COMPA~T ADMINISTRATION ISSUES <br /> <br />A. COMPETITIOr:. WITH THE NATURAL ENVIRONMENT <br /> <br />Since the inception of the La Plata River Compact in 1922, many <br />of the issues and concerns that served as the impetus to create a <br />defined interstate water flIlocation system have continued to plague <br />the river system. Fore~ost among these problems is the limited <br />amount of water availabltj to serve irrigation demands. This problem <br />is especially acute after th:e spring runoff. As indicated by Article II of <br />the Compact, Coloradoj must deliver one-half of the measured <br />streamflow at Hesperus t9 the state line." Further compounding the <br />difficulty of providing water to the state line is competition among the <br />natural elements. The headwaters of the La Plata River reach 13,000 <br />feet in elevation, the river quickly descends 4,900 feet during its six <br />mile journey to Hesperu~, accompanied by a climatic transformation <br />from alpine to arid-dese~t conditions," The river channel itself is <br />composed of a consorth,lm of cobbles, gravel, and fine sands that <br />promote excessive seepage into the shallow alluvium." Consumptive <br />use from riparian vegetation also affects the delivery of water through <br />the river corridor. Withi/1 the fifty-two miles the La Plata River flows <br />from Hesperus to FarmiNgton, New Mexico, there are an estimated <br />3,580 acres of riparian/wetland plant communities within the one-mile <br />wide river corridor." The plant species in this area vary in type and <br />density, but the pre<ilominant phreatophyte species include <br />cottonwood trees and willpws, which consume an average of 5.5 feet of <br />water each year." Thefe natural, physical elements can have a <br />dramatic effect on the jdelivery of one-half of the streamflow at <br />Hesperus to the state lin~. For example, during dry periods in the <br />middle to late summer ",hen the streamflows at Hesperus are in the <br />80-100 cubic feet per second range, the transit losses through the <br />thirty-one mile river corridor to the state line routinely approach 45-50 <br />percent." As the flows continue their decline to a "benchmark" of <br />twenty-five cubic feet pe:r second at Hesperus, the La Plata River <br />streambed often b~come~ completely dry for intermittent stretches <br />above the state line. I <br /> <br />54. Id. <br />55, See USGS, supra note 11,!at 400. <br />56. 1 U.S. DEP'T OF INTERIO*, ANIMAS-LA PLATA PROJECT: FINAL SUPPLEMENT TO THE <br />FINAL ENVIRONMENTAL STATEME"[f III.56 (1996). <br />57. Id. i <br />58. See MORTON, W. BlTI1NG~R & GLEN, E. STRINGHAM, A STUDY OF PHREATOPHYrE <br />GROWTH IN THE LOWER ARKANSAS RIvERVALLEYOF COLORADO 17 (1963). <br />59. Report of the La Plata ~ver Compact Administration, prepared by the Division <br />VII Irrigation Engineer 11 (1954). <br />60. See id. <br />