Leiaka TishaThe Cass Fault system of north-central Arkansas is composed of monoclines and normal faults that strike in an east-west direction. This complex structural system forms a transitional boundary between the Arkansas structural platform to the north and the Arkoma basin to the south. ...
Strata orientation indicated down-to-the-south faulting within the Cass system during the late Mississippian and early Pennsylvanian periods and other evidence useful for corroborating syndepositional faulting along the Cass.University of Arkansas.Welcome, Leiaka Tisha.University of Arkansas....