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  • Topographical thresholds for ephemeral gully initiation in intensively cultivated areas of the Mediterranean
  • and topographical, lithological, land-use and climatic factors.
  • of a landscape to gully erosion. Two important components of gully erosion studies are the prediction of where gullies begin and where they end. To address some of these issues, topographical thresholds for gully initiation and sedimentation in 6 different
  • characteristics, such as topographical parameters, material properties and climate. The ultimate goal is to identify the most important controlling factors of past and present bank gully erosion. 55 active bank gullies formed in different lithologies by various