there also stopped before they
led to a slope failure. A year later, in November
18
2002, multiple tension cracks formed in Botnabrún during a heavy rainstorm after a long wet
period. Most of the cracks that formed during the rainstorm occurred in the upper part of Botna-
brún, between Skuldarlækur and Nautaklauf. These movements
led to the release of two debris
slides, just west of Búðará
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf