The Upper Tertiary basaltic flows are located in the western Bekaa valley, and occur within Neogene limestone strata. The rocks occur in a number of flows reaching two meters in thickness. The flows contain both highly vesicular to massive basaltic rocks.
Description:
Thesis (M.S.)--American University of Beirut. Department of Geology, 2001;"Advisor: Dr. Abdel-Fattah M. Abdel-Rahman, Associate Professor, Geology--Member of Committee: Dr. Amir Mokhtary-Fard,Assistant Professor, Geology--Member of Committee: Dr. Ulrich K
