and -cone sediments, 2) perched channels of wall-like form that are self-built as a result of man channelling water flow, and 3) fissure-ridge travertines that are cut by fissures roughly following ridge crests.
, river channels, alluvial cones and fans and slope failures with archaeological evidence of seismic events at the Acropolis along the eastern margin of the Argive Plain in order to obtain an improved understanding of the paleoseismicity of this region.