Research indicates that nine large tsunamigenic
landslides struck Sullorsuaq Strait in prehistoric times during the
Holocene, seven of them from the southern coast of the Nuussuaq Peninsula and two others from the northern coast of Disko Island. Seven of the landslides apparently occurred between about 8020 BC and 6520 BC with unidentified tsunamigenic effects. The two most recent prehistoric landslides generated megatsunamis which struck
Alluttoq Island, the first sometime around 5650 BC with a run-up height of , and another that struck around 5350 BC with a run-up height of .
Erik the Red paid the first recorded visit to Disko Island at some time between 982 and 985. The island was used as a base for summer hunting and fishing by Norse colonists. The
coal mining town of
Qullissat was founded on the northeast coast of Disko Island in 1924. By 1952 it was a cultural hub and the third-largest settlement in Greenland, with a population of 995. On 15 December 1952, a major landslide on a slope of the mountain
Niiortuut () on the southern coast of the Nuussuaq Peninsula generated a
tsunami which traveled across Sullorsuaq Strait and struck Qullissat, where it had a run-up height of and inflicted damage on buildings. leaving the northern coast of Disko Island uninhabited. On 21 November 2000, a large landslide at
Paatuut on the southern coast of the Nuussuaq Peninsula generated a
megatsunami with a run-up height of near the landslide and at the former site of Qullissat, away, where it inundated the coast as far as inland. ==Geology==