Although the deposits are stratified and lenticular (Pl. The area is underlain by alluvial sediments of Pliocene to Recent age that are the most productive water-bearing rocks in the County. The Arkansas Valley is characterized by its extreme flatness and the poorly developed surface drainage of the land flanking the Arkansas River. Where ground-water conditions are not uniform within an area, it has been divided into subareas.įigure 20-Map of Sedgwick County, Kansas, showing generalized ground-water areas and subareas. There are four major ground-water areas: the Arkansas Valley, the Ninnescah Valley, the Wellington Upland, and the Ninnescah-Wellington Upland. Generalized ground-water areas and subareas within the County are shown on Figure 20 and are explained in the section of the report that follows. Ground Water, continued Ground-water Areas
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |