A PRELIMINARY CLASSIFICATION OF KARSTIC SPRINGS OF LEBANON
Only 331 of those karstic springs had reliable discharge measurements. Due to the lack of continuous measurements of springs, Meizer’s classification of springs based on discharge rate was used to classify them. From this, the minimum average discharge was used because it was more frequently reported and it is more reliable than the reported maximum discharge. None of the springs identified belonged to Class I and only five springs had a minimum discharge rate to be in Class II. Those five springs are: Ain ez Zarqa (South Bekaa) spring located at the axis of a syncline and is a drainage-overflow spring with a lower stratigraphic barrier. Chekka Submarines springs are artesian springs with upper stratigraphic control and fracturing allowing outflow. Ain el Zarka (North Bekaa) and Jeita springs are mainly overflow springs with a frontal barrier of steep dipping beds. Nabaa el Aarbine is dominantly an overflow spring located in a pull-apart basin with a frontal barrier made up of a major faulting zone. There are also 57 in Class III and 78 in Class IV. The rest are in Class V and VI.
This preliminary classification of Lebanese springs is the first step in understanding them, defining their static and dynamic reserves, and identifying those in need for further analyses and future protection measures.