Fault scarps, if well-preserved, include precise evidence of past earthquakes. Using
cosmogenic 36 Cl dating, the timing and slip of paleoearthquakes are recoverable beyond …

Topography is a reflection of the tectonic and geodynamic processes that act to uplift the
Earth's surface and the erosional processes that work to return it to base level. Numerous …

Active normal faults on the Mediterranean island of Crete form prominent limestone scarps
together with basin and range topography. These faults mainly strike E‐ESE and N‐NNE in …

Geomorphological survey along the coasts of Crete revealed widespread evidence of
uplifted and submerged tidal notches, different phases of beachrock formation, and many …

Subduction forearcs are subject to seismic hazard from upper plate faults that are often
invisible to instrumental monitoring networks. Identifying active faults in forearcs therefore …

We present the Quaternary slip history of the Kenchreai Fault, Gulf of Corinth, based on
geomorphological, palaeoseismological, geo-archaeological data and literally determined …

The 72-km-long Teton normal fault bounds the eastern base of the Teton Range in
northwestern Wyoming, USA. Although geomorphic surfaces along the fault record latest …

Western Anatolia is one of the most seismically active regions worldwide. To date, the
paleoseismic history of many major faults, in terms of recurrence intervals of destructive …

Sets of marine terraces, sediments, and paleoshorelines are commonly found in forearc
regions worldwide. A common assumption holds that crustal uplift prevents these features …

Constraining the past seismic activity and the slip-rates of faults over several millennials is
crucial for seismic hazard assessment. Chlorine 36 (36 Cl) in situ produced cosmogenic …