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316 BERBERIAN AND TCHALENKOSalmas Fault and Derik Spring in the southwestern extension of the Derik Fault.new spring, the Zelele Bolaghi (literally, the earthquake spring), appeared on theSalmas Plain and is still responding to-day to local earthquake tremors.4. 2. Salmas FaultThe Salmas Fault is the longer of the two faults, and the one-that produced th~larger displacement. It is formed by two separate en 6chelon segmen.ts ~’efe’l’red to her~Fig. 37. Hablaran village. The village was destroyed and large rockfalls were started by the earthquake.