2000 Iceland earthquakes

Coordinates: 63°58′N 20°22′W / 63.97°N 20.37°W / 63.97; -20.37
Source: Wikipedia, the free encyclopedia.

2000 Iceland earthquakes
Location of earthquakes
Location of earthquakes
UTC timeDoublet earthquake:    
 A: 2000-06-17 15:40:41
 B: 2000-06-21 00:51:46
ISC event 
 A: 1736604
 B: 1736730
USGS-ANSS 
 A: ComCat
 B: ComCat
Local date17 June 2000 (2000-06-17)
21 June 2000 (2000-06-21)
Magnitude 
 A: 6.5 Mwc[1]
 B: 6.5 Mwc[2]
Depth6.3 kilometres (3.9 mi) (17 June)
5.1 kilometres (3.2 mi) (21 June)
Epicenter63°58′N 20°22′W / 63.97°N 20.37°W / 63.97; -20.37
63°59′N 20°43′W / 63.98°N 20.71°W / 63.98; -20.71
Max. intensity17 June:
MMI VIII (Severe)
21 June:
MMI IX (Violent)
Casualties3 injured

The 2000 Iceland earthquakes struck southern Iceland on 17 and 21 June. There were no fatalities but three people suffered minor injuries and there was considerable damage to infrastructure.[3] The two earthquakes were the first major seismic activity in Iceland for 88 years.[4] The recorded magnitude of both of the main quakes was 6.5 Mwc.[1][2]

Tectonic setting

Iceland lies on the spreading axis of the

strike-slip faults, although there is also evidence of WSW–ENE trending faults.[5]

According to historical records, there have been 33 damaging earthquakes in the SISZ from the 11th century up to June 2000, with the latest being in 1896 and 1912.[5]

Earthquakes

The first of the earthquakes occurred at 15:40 UTC on 17 June at a depth of 6.3 km. The magnitude estimated by the Icelandic Meteorological Office was 6.4 Mw , assuming a single fault, although such a model did not fit all the available data. The extent of aftershocks defined a 16 km long north-south fault rupture, continuing down to 10 km. The causative fault was the Árnes Fault and a large number of surface fissures were mapped along this structure in the days following the event.[5]

The second earthquake occurred at 00:51 UTC on 21 June at a depth of 5.1 km. The extent of aftershocks defined an 18 km fault rupture down to 8 km depth. The causative fault was the Hestfjall Fault. Surface fissures were developed over a distance of about 25 km.[5]

See also

References

  1. ^ a b "M 6.5 Iceland 2000-06-17". earthquake.usgs.gov. United States Geological Survey. Retrieved 27 April 2019.
  2. ^ a b "M 6.5 Iceland 2000-06-21". earthquake.usgs.gov. United States Geological Survey. Retrieved 27 April 2019.
  3. ^ South Iceland Earthquakes 2000: Damage and Strong-Motion Recordings
  4. ^ Ragnar Stefánsson; Gunnar B. Guðmundsson. "The two large earthquakes in the South Iceland seismic zone on June 17 and 21, 2000". Archived from the original on 25 July 2001. Retrieved 25 July 2001.
  5. ^ .

External links