Fig. 3
From: Seismic history of western Anatolia during the last 16 kyr determined by cosmogenic 36Cl dating
a Rahmiye fault scarp surface showing two patterns of weathering; solid lines in the upper section show horizontal and vertical fractures and dissolutions, whereas dashed lines represent vertical dissolution traces in the lower part of the fault surface; b the sampled profile of the Rahmiye fault scarp; and c Cartoon of Rahmiye fault showing important parameters of the fault scarp for modeling, including scarp height, scarp dip, colluvium dip, top surface dip and density of the bedrock and colluvium. White dashed line shows the sampled surface