2008 Lincolnshire earthquake
|Date||27 February 2008|
|Depth||18.6 kilometres (12 mi)|
|Areas affected||United Kingdom|
|Max. intensity||6 EMS - Slightly Damaging|
|Casualties||1 injury reported; 0 fatalities|
The 2008 Lincolnshire earthquake struck Lincolnshire, in the United Kingdom, on Wednesday 27 February at 00:56:47.8s GMT. According to the British Geological Survey, the quake registered a reading of 5.2 on the Richter scale with the epicentre 2.5 miles (4 km) north of Market Rasen and 15 miles (24 km) south-west of Grimsby.
The duration of the earthquake was confirmed as roughly 10 seconds.
Spread of effect
The tremors were felt across a wide area of England and Wales, from Hampshire in the south to Newcastle upon Tyne in the north, and as far west as Bangor, Northern Ireland. It was also perceptible in the Netherlands, Belgium, and the far north of France. Structural damage was recorded in some areas, including one case where a chimney collapsed and injured a person in Wombwell, Barnsley, South Yorkshire.
The 2008 Lincolnshire earthquake was caused by the sudden rupture and motion along a strike-slip fault, 18.6 kilometres (12 mi) beneath Lincolnshire. Earthquake motion occurred over a time span of ~2 minutes but it was most intense and was felt at the surface for just 10 to 30 seconds; maximum vertical ground motion at the epicentre of the earthquake was only ~1 mm. Computer calculations carried out by the BGS imply sinistral motion on a N–S or dextral motion on a E–W oriented strike-slip fault. The nine aftershocks observed, ~5 kilometres (3 mi) SSW of the main earthquake event, point to an approximately N–S oriented fault. From the 5.2 ML magnitude of the main earthquake, a motion of a few centimetres along a ~2.5 kilometres (2 mi) long fault rupture is derived. The energy released was 3.98×1012 joules (equal to the detonation of ~950 tonnes of TNT).
Unlike typical earthquakes worldwide, the earthquakes of Northern Europe are intraplate earthquakes, meaning they are not close to tectonic plate boundaries. Most intraplate earthquakes in Northern Europe, including the UK, are thought to be driven by distant tectonic stresses – a combination of E–W North Atlantic Ridge and N–S African Plate regional stress fields, and local mantle conditions. Indeed, the motion on the strike-slip fault responsible for the 2008 Lincolnshire earthquake is compatible with a local NW–SE stress field; a product of the E–W and N–S regional stress fields.
Only a minority of earthquakes in the UK are related to post-glacial rebound e.g. the minor earthquakes (<3.5 ML) of western Scotland, where glaciers ~1 km thick existed during the peak of the last Ice Age.
The earthquake resulted in structural damage to many homes and businesses in the epicentral area. Buildings as large as apartment blocks were reported to have shaken for up to 30 seconds afterwards. Birds and pets became highly agitated. There were no deaths, but a 19-year-old man in Wombwell, Barnsley, South Yorkshire suffered a broken pelvis when a piece of chimney fell through the roof onto his attic bed. The earthquake was felt by people as far south as Bournemouth, where it was felt as a mild but noticeable vibration, and as far away as Bangor, Northern Ireland, where it woke people.
Police in the Midlands received more than 5,000 telephone calls in an hour from members of the public regarding the earthquake. The earthquake caused power cuts in some areas. A church in March, Cambridgeshire reported that, since the earthquake, water had been coming up from the ground into the cellar at a rate of 10 imperial gallons (45 l) per hour. The St Mary Magdalene church at Waltham on the Wolds in Leicestershire had its spire damaged and was to be rebuilt at a cost of £100,000. Also damaged were the spires of St Andrew's church in Haconby and St Vincent's church in Caythorpe, both in South Kesteven.
The tremor was the largest earthquake to affect the UK since the 1984 Llŷn Peninsula earthquake, which measured 5.4 on the Richter scale. The British Geological Survey gave the earthquake a reading of 5.2ML, while the United States Geological Survey reported it measured 4.8Mb. The French Atomic Energy Commission estimated the magnitude was 5.4ML.
A total of nine aftershocks were recorded. The largest, measuring 2.8 on the Richter scale, occurred around five weeks after the initial event, on 5 April at 13:57 GMT.
The BGS described the earthquake as an "extremely large earthquake in UK terms but not large in world terms". Approximately 200 earthquakes occur in the UK every year, approximately 175 of which are too weak to be noticed by humans.
- British Geological Survey
- Geology of the United Kingdom
- List of earthquakes in the United Kingdom
- London-Brabant Island
- "Market Rasen Earthquake 27 February 2008 00:56 UTC 5.2 ML". British Geological Survey. Archived from the original on 9 March 2008. Retrieved 8 December 2011.
- Yeoman, Fran (27 February 2008). "Earthquake hits Britain, 5.3 magnitude". London: The Times. Retrieved 27 February 2008.
- USGS 'Did you feel it?' intensity map
- "Earthquake hits much of England". BBC. 27 February 2008. Archived from the original on 3 March 2008. Retrieved 27 February 2008.
- Wells, Donald L.; Coppersmith, Kevin J. (1994). "New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement". Bulletin of the Seismological Society of America (Seismological Society of America) 84 (4): 974–1002.
- "Earthquake Power Calculator". [www.convertalot.com]. Retrieved 29 February 2008.
- Cloetingh, S.; Ziegler, P.A.; Beekman, F.; Andriessen, P.A.M.; Matenco, L.; Bada, G.; Garcia-Castellanos, D.; Hardebol, N.; Dezes, P.; Sokoutis, D. (2005). "Lithospheric memory, state of stress and rheology: neotectonic controls on Europe's intraplate continental topography". Quaternary Science Reviews 24 (3–4): 241–304. Bibcode:2005QSRv...24..241C. doi:10.1016/j.quascirev.2004.06.015.
- Bott, Martin H.P.; Bott, Jacqueline D.J. (2004). "The Cenozoic uplift and earthquake belt of mainland Britain as a response to an underlying hot, low-density upper mantle". Journal of the Geological Society 161 (1): 19–29. doi:10.1144/0016-764903-014.
- Firth, Callum R.; Stewart, Iain S. (2000). "Postglacial tectonics of the Scottish glacio-isostatic uplift centre". Quaternary Science Reviews 19 (14–15): 1469–1493. Bibcode:2000QSRv...19.1469F. doi:10.1016/S0277-3791(00)00074-3. Archived from the original on 2 March 2008.
- Kossof, Julian (27 February 2008). "Earthquake hits UK". The Daily Telegraph. Archived from the original on 3 March 2008. Retrieved 27 February 2008.
- "UK rocked by strongest earthquake in over 20 years". TV3 New Zealand. 27 February 2008. Archived from the original on 2 March 2008. Retrieved 27 February 2008.
- "Mystery of 'holy' water's source". BBC News Online. 26 March 2008. Archived from the original on 31 March 2008. Retrieved 26 March 2008.
- "Scaffolding due this week". Save Our Spire!. 10 March 2008. Retrieved 13 January 2009.
- "Steeple damage closes St Vincent’s Church in Caythorpe". Grantham Journal. 14 February 2012. Retrieved 5 October 2012.
- "Lincolnshire earthquake "one of biggest ever"". Lincolnshire Echo. Retrieved 27 February 2008.
- "Magnitude 4.8 - England, United Kingdom". United States Geological Survey. 27 February 2008. Archived from the original on 2 March 2008. Retrieved 27 February 2008.
- "Alerte Sismique" (in French). Commissariat à L'Energie Atomique (CEA). 27 February 2008. Archived from the original on 2 March 2008. Retrieved 27 February 2008.
- "Market Rasen aftershocks". British Geological Survey. 14 April 2008. Archived from the original on 6 April 2008. Retrieved 14 April 2008.
|Wikinews has related news: Minor earthquake shakes England|
- Report from the British Geological Survey
- Report from The Grimsby Telegraph
- Earthquake information by the European-Mediterranean Seismological Centre
- Earthquake information by the United States Geological Survey
- Report from BBC News
- Report from Sky News
- Location of epicentre on Google Maps
- Report and video from the Doncaster Free Press