Abstract
Awara Terrace consists of diluvial sand and conglomerate, which bear unconfined ground-water. The basal bed is Miocene sandstone and early Pliocene pyroclastic substances.
Several deep wells were developed for the sake of irrigation, and the resources of city water have been here looked for. A planning of such deep wells may stand in the way of irrigation owing to ground-water. An agricultural discharge of ground-water brings a recharge with time lag, while the others take water out of strata solely. This paper deals with a difference of theirs to that effect, striking a hydrologic balance by means of an intake rate, a fall of the static level, and all the withdrawal.
