E. F. Hollyday J. V. Brahana 1988 In areas where dry stream reaches occur, subsurface drainage successfully competes with surface drainage, and sheet-like dissolution openings have developed parallel to bedding creating the ground-water reservoir. Union Hollow in south-central Tennessee is the setting for a case study that illustrates the application of the dry stream reach technique. In this technique, dry stream reach identification is based on two types of readily acquired information: remotely sensed black and white infrared aerial photography; and surface reconnaissance of stream channel characteristics. Test drilling in Union Hollow subsequent to identification of the dry reach proved that a localized ground-water reservoir was present. application/pdf 10.1111/j.1752-1688.1988.tb00907.x en American Water Resources Association Dry Stream Reaches in Carbonate Terranes: Surface Indicators of Ground-Water Reservoirs article