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Chemical analyses of water from 99 wells and 19 springs in the San Luis basin in Colorado and New Mexico were evaluated to determine selected waterquality characteristics as an aid in understanding the flow of ground water in the basin. The evaluation shows that the distribution of chemical water types in the basin is consistent with chemical changes to be expected along flow paths in rocks typical of those in the basin. The San Luis basin area is underlain by a surficial (less than 100 feet thick) unconfined aquifer and, in turn, by a confining bed and a deeper confined aquifer. Previous studies have indicated that the ground-water system is recharged around the edges of the basin and that ground water then moves toward discharge areas in the topographically closed part of the basin and along principal streams. Results of this ground-water-quality evaluation support these previously developed concepts of flow through the aquifer system in the San Luis basin.

Selected water-quality characteristics and flow of ground water in the San Luis basin, including the Conejos River subbasin, Colorado and New Mexico