Disko Island (Greenlandic: Qeqertarsuaq, Danish: Diskoøen) is a large island in Baffin Bay, off the west coast of Greenland. It has an area of 8,578 km2 (3,312 sq mi),[1] making it the second largest of Greenland after the main island and one of the 100 largest islands in the world.
The island has a length of about 160 km (100 mi), rising to an average height of 975 m (3,199 ft), peaking at 1,919 m (6,296 ft). The port of Qeqertarsuaq (named after the island, and also known as Godhavn) lies on its southern coast. Blæsedalen valley is north of Qeqertarsuaq.
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 41 to 66 metres (135 to 217 ft), and another that struck around 5350 BC with a run-up height of 45 to 70 metres (148 to 230 ft).[3]
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.[4]
The coal mining town of Qullissat was founded on the northeast coast of Disko Island in 1924.[5] By 1952 it was a cultural hub and the third-largest settlement in Greenland, with a population of 995.[6] On 15 December 1952, a major landslide on a slope of the mountain Niiortuut (70°20′56″N53°10′41″W / 70.349°N 053.178°W / 70.349; -053.178 (Niiortuut)) on the southern coast of the Nuussuaq Peninsula generated a tsunami which traveled 30 kilometres (19 mi) across Sullorsuaq Strait and struck Qullissat, where it had a run-up height of 2.2 to 2.7 metres (7 ft 3 in to 8 ft 10 in) and inflicted damage on buildings.[6] By 1966, Qullissat was the sixth-largest town in Greenland with a population of 1,400,[5] but it was abandoned in 1972,[7] 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 50 metres (164 ft) near the landslide and 28 metres (92 ft) at the former site of Qullissat, 20 kilometres (11 nmi; 12 mi) away, where it inundated the coast as far as 100 metres (328 ft) inland.[8]
Geology
[edit]Native iron from Disko Island (size: 4.9 x 2.9 x 1.5 cm [1.9 in. x1.1 in. x 0.6 in.])Polished slab from this same deposit, now at the Carnegie Museum of Natural History
Mineral deposits, fossil finds and geological formations add to interest in the area. One of the interesting geological features is the native iron found at the island. A 22-ton (44,000 lbs; 20 tonnes) lump mixture of iron and iron carbide (cohenite) has been found. There are only a few places on earth where native iron is found which is not of meteoric origin.[9][10]
There are numerous hot springs on the island. The microscopic animal Limnognathia, the only known member of its phylum, was discovered in the Isunngua spring.
^Seaver, Kirsten A. “Greenland and Vinland.” The Frozen Echo: Greenland and the Exploration of North America, Ca. A.D. 1000-1500, Stanford University Press, 1998, pp. 28–29.
^Dahl-Jensen, Trine; Larsen, Lotte; Pedersen, Stig; Pedersen, Jerrik; Jepsen, Hans; Pedersen, Gunver; Nielsen, Tove; Pedersen, Asger; Von Platen-Hallermund, Frants; Weng, Willy (2004). "Landslide and Tsunami 21 November 2000 in Paatuut, West Greenland". repec.org. Ideas. Retrieved 14 October 2023.
^Bird; John M.; Goodrich; Cyrena Anne; Weathers; Maura S. (1981). "Petrogenesis of Uivfaq iron, Disko Island, Greenland". Journal of Geophysical Research. 86 (B12): 11787–11805. Bibcode:1981JGR....8611787B. doi:10.1029/JB086iB12p11787.
^Todaro MA; Balsamo M & Kristensen RM (2005). "A new genus of marine chaetonotids (Gastrotricha) with a description of two new species from Greenland and Denmark". Journal of the Marine Biological Association of the United Kingdom. 83 (6): 1391–1400. doi:10.1017/S0025315405012579. S2CID53120866.
