 | |
| UTC time | 2008-05-29 15:46:00 |
|---|---|
| ISC event | 13230288 |
| USGS-ANSS | ComCat |
| Local date | 29 May 2008 |
| Local time | 15:46 |
| Magnitude | 6.3 Mwc[1] |
| Depth | 10 km (6.2 mi)[1] |
| Epicenter | 63°58′N 20°59′W / 63.96°N 20.99°W[1] |
| Type | Right-lateral strike-slip[2] |
| Areas affected | Iceland |
| Max. intensity | MMI VIII (Severe) [3] |
| Casualties | 30 injuries |
The 2008 Iceland earthquake was a doublet earthquake that struck on 29 May at 15:46 UTC in southwestern Iceland.[2] The recorded magnitudes of the two main quakes were 5.9 Mw and 5.8 Mw , respectively, giving a composite magnitude of 6.1 Mw .[4] There were no human fatalities, but injuries were reported and a number of sheep were killed.[citation needed] The epicenter of the earthquake was between the towns of Hveragerði and Selfoss, about 45 kilometers (28 mi) east-southeast of the capital, Reykjavík. It was the strongest earthquake to hit Iceland since the summer of 2000.[5]
YouTube Encyclopedic
-
1/3Views:1 1191 2749 700 932
-
Leirgerdur Hot Pools (emerged in 2008 after 6.3 earthquake), Hveragerdi, Iceland
-
Hrifla, Reykjamori and Skjalfti, the new Icelandic hot springs from 2008 Earthquake.
-
Volcano Eruptions Size Comparison (2021)
Transcription
Characteristics
Iceland straddles the mid-Atlantic ridge where the Eurasian and North-American tectonic plates move away from each other. Volcanic activity is common along such divergent boundaries but strong earthquakes are rare. In Iceland the ridge is somewhat off-set, creating two transform faults where plates move horizontally along each other.[6] One is in the north of the country and one in the south; the strongest Icelandic earthquakes happen along those transform faults.[7] The 29 May quake is classified by geologists as a typical Suðurlandsskjálfti (literally: Southern Region quake), a strong earthquake that happens on Iceland's southern fault.
Damage
Unlike the quakes in the summer of 2000, the 29 May quake happened in the most densely populated part of the South Iceland district. The population of the affected area is about 12,000 and it includes the towns of Selfoss and Hveragerði as well as Eyrarbakki, Stokkseyri and Þorlákshöfn. Many farms were also affected.
See also
References
- ^ a b c ISC-EHB Event 13230288 [IRIS].
- ^ a b Decriem et al. 2010, p. 1144.
- ^ ANSS: Iceland 2008, ShakeMap .
- ^ Decriem et al. 2010, p. 1128.
- ^ BBC News 2008.
- ^ Einarsson, P. (1991). "Earthquakes and present-day tectonism in Iceland". Tectonophysics. 189 (1–4): 261–279. Bibcode:1991Tectp.189..261E. doi:10.1016/0040-1951(91)90501-I.
- ^ Ward, P. L. (1971). "New Interpretation of the Geology of Iceland". Geological Society of America Bulletin. 82 (11): 2991–3012. doi:10.1130/0016-7606(1971)82[2991:NIOTGO]2.0.CO;2.
Sources
- ANSS, "M6.3 – Iceland", Comprehensive Catalog, U.S. Geological Survey
- "Strong earthquake rocks Iceland". BBC News. 29 May 2008. Retrieved 29 May 2008.
- Decriem, J.; Árnadóttir, T.; Hooper, A.; Geirsson, H.; Sigmundsson, F.; Keiding, M.; Ófeigsson, B. G.; Hreinsdóttir, S.; Einarsson, P.; LaFemina, P.; Bennett, R. A. (2010), "The 2008 May 29 earthquake doublet in SW Iceland", Geophysical Journal International, 181 (2): 1128–1146, Bibcode:2010GeoJI.181.1128D, doi:10.1111/j.1365-246x.2010.04565.x.
- International Seismological Centre, ISC-EHB Bulletin, Thatcham, United Kingdom
Further reading
- Vogfjord, K. S., et al. "Fault interaction in the South Iceland Seismic Zone: The May 2008, M6. 3 earthquake". EGU General Assembly Conference Abstracts. Vol. 11. 2009.
- Brandsdottir, Bryndis, et al. "The May 29th 2008 earthquake aftershock sequence within the South Iceland Seismic Zone: Fault locations and source parameters of aftershocks." Jökull 60 (2010): 1–22.
External links
- The International Seismological Centre has a bibliography and/or authoritative data for this event.
63°59′31″N 21°00′50″W / 63.992°N 21.014°W
 | This Iceland-related article is a stub. You can help Wikipedia by expanding it. |
This page was last edited on 1 April 2024, at 09:58