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<br />28 Jq..USTRATIONs--Long List--Continued <br /> <br />. <br /> <br />Figure 10. Junction Creek Sanc1stone over lain by tJl€ <br /> <br /> <br />Morrison Formation near McElmo Creek <br /> <br /> <br />11. Nap shOl-Jing generalized depth to the <br /> <br /> <br />Dakota Sandstone in the western area <br /> <br /> <br />sou th of the Ute Mountains <br /> <br />5;3 <br /> <br />?& <br /> <br />12. <br /> <br />Prominent lithologic zone in tl,e Mancos <br /> <br /> <br />Shale equiv~lent to the Greenhorn Lime- <br /> <br /> <br />stone of other areas . <br /> <br /> <br />13. Juana Lopez Ner.tber of the Mancos Shale, Kmj, <br /> <br />of CQrlilc age elt. '''l'he Mound." 1\ few feet <br /> <br /> <br />above the Juana Lopez is a 9-foot glauconitic <br /> <br /> <br />sandstone, g, of Niobrara age. Mancos <br /> <br />1 1 9'-~/ <br />S ,a e, I~. <br /> <br />14. Intertongulng and gradational relation <br /> <br /> <br />between the lower Point Lookout Sandstone <br /> <br />and the Mancos Shale on Chlmney Rock. /?/ <br /> <br /> <br />15. Layout of infiltration gallery, G-l, <br /> <br />northwest of Towaoc I 3+ <br /> <br /> <br />16. Areas available to grazing by the development <br /> <br /> <br />of permanent ground-water or temporary <br /> <br />surface-\"ater supplies . I g J7 <br /> <br /> <br />17. Curves showing depth to water in well B-17 <br /> <br /> <br />~lile discharging 40 to 60 gpm for <br /> <br />periods ranging from 0.1 to 100 days /4<& <br /> <br /> <br />18. T11eoretical declines in water level caused <br /> <br /> <br />by a vie 11 d ischarg ing 20 and 40 gpm from <br /> <br /> <br />the Junction Creek, Entrada, Navajo, and <br /> <br /> <br />Wingate Sandstones for 100 days at <br /> <br /> <br />distances ranging from 10 to 10,000 feet <br /> <br />from the discharging '_"ell /-.if' <br /> <br /> <br />19. T11e four general ground-water regions in <br /> <br /> <br />the project area. /5,1 <br /> <br />7J <br /> <br />. <br /> <br />. <br />