This research define and study geomorphological properties of the Karstic spring
nameled “Al Gamka” , characterized one of seasonal springs that flux up as “fontain” .
For this issue, we achieved a detailed geological and geomorphological Study in
the
region of spring, in addition to the field measures to draw and define the main karstic paths
and its tributaries, which recharge this spring by groundwater coming from north-east side.
To show the changes happened to the spring path, and to control water level variations
inside this karstic paths and tributaries and the relation with groundwater influx periods
through this “fountain”.
This study showed reasons that led to groundwater influx through this spring with
high discharge, and the relation between this spring discharge with the amount of
precipitation on the recharge area. Finally, I presented detailed explanation about karstic
extension, Which recharge this spring, in addition to the geomorphological development of
the spring region through previous times.
