The Burdur Basin, which is located in the Lakes Region SW Anatolia, was formed by vertical faulting movements. erosion surfaces were developed on marl deposit accordance with lowering of base level each movement east Basin. These are at an elevation 980, 995, 1040, 1115, 1200, 1300-1340 m Neogene and knickpoints along valleys indicate six times depressed fault lines scarp extending Basin dissec...

Abstract Lobate scarps (thrust faults) in the lunar south polar region (90°–60°S) provide important insights into tectonic history, seismicity, and seismic hazard potential of landing sites. In this study, we discovered 75 new lobate >500 segments, exhibiting latitudinal variation geometry movement directions. Formation ages 141 prominent scarp segments show fault growth rates directions, de...

In this study, we analyse deep-seated gravitational slope deformations (DSGSDs) in central Sardinia. The area is characterised by plateaus with a prominent limestone scarp overlying metamorphites. A comprehensive mapping of structural, karst, fluvial, and morphologies Pardu Ulassai valleys presented herein. uplift linked to the Plio-Pleistocene tectonic activity leads high-slope topography, whi...

Fully softened shear strength mobilized in first-time slope failures, introduced by Skempton 1970, corresponds to a random edge-face arrangement and interaction of clay particles an entirely destructured fabric stiff clays shales. A series triaxial compression tests was conducted on reconstituted normally consolidated specimens 15 shale compositions. Based the laboratory results empirical corre...

In Pakistan, many subsurface (SS) drainage projects were launched by the Salinity Control and Reclamation Project (SCARP) to deal with twin problems (waterlogging salinity). some cases, sump pumps installed for disposal of SS effluent into surface channels. Presently, have become dysfunctional due social financial constraints. This study evaluates alternate design Paharang system that could per...