Sara Mitchell (Gran) Sara Mitchell (Gran) used 36 Cl to determine the movement history of an exceptionally well preserved, limestone fault scarp in the Galilee. Her first of its kind work showed that ...

Fault scarps may be modified by erosion. Streams flowing from hanging valleys on top of a scarp will cut down forming deeply-incised V-shaped valleys (wineglass structure) yielding and cutting the ...

This allowed them to study that stretch of the fault in unprecedented detail—and find a number of geological secrets hiding in plain sight. At one point in the Tintina segment, they discovered a fault ...

Fault scarps are in effect fossilised earthquakes. When the ground on one side moves relative to the other side, a step is left in the bedrock. Over time, erosion can reveal these long (up to tens of ...

An example of a bedrock fault scarp in the area above the settlements of Mercato and Fiamignano in the Central Apennine Mountains, Italy. This particular bedrock scarp is 1 of the 12 included in ...

Sara Mitchell (Gran) used 36 Cl to determine the movement history of an exceptionally well preserved, limestone fault scarp in the Galilee. Her first of its kind work showed that most likely three ...

At one point in the Tintina segment, they discovered a fault scarp—or a ridged crack in the surface—where the land broke and shifted by 1,000 m (3,280 ft.).

At one point in the Tintina segment, they discovered a fault scarp—or a ridged crack in the surface—where the land broke and shifted by 1,000 m (3,280 ft.).