User:J. Johnson/Sandbox4
Infobox testing
[edit]Trying to recreate the extraneous "UTC time" above the template as seen at the doc.
| UTC time | ?? |
|---|---|
| USGS-ANSS | ComCat |
| Local date | 7 September 2017 |
| Local time | 23:49:21 CDT |
| Magnitude | 8.2 Mw[1] |
| Depth | 50.1 km (31.1 mi) |
| Epicenter | 15°04′05″N 93°42′54″W / 15.068°N 93.715°W |
| Type | normal fault |
| Areas affected | Mexico, Guatemala[2] |
| Max. intensity | IX (Violent) |
| Tsunami | Yes |
| Casualties | 98 dead, 300+ injured |
Problem
[edit]
  London Canterbury  | |
| Date * | 21 May 1382 |
|---|---|
| Magnitude | 6.0 Ms[4] |
| Depth | 25–30 km |
| Epicenter | 51°20′N 2°00′E / 51.34°N 2.00°E[5] |
| Areas affected | Kent, England |
| Max. intensity | VII-VIII - Very strong to severe |
| * Deprecated | See documentation. |
The 1382 Dover Straits earthquake occurred at 15:00 on 21 May. It had an estimated magnitude of 6.0 Ms and a maximum felt intensity of VII-VIII on the Mercalli intensity scale.[6] Based on contemporary reports of damage, the epicentre is thought to have been in the Straits of Dover. The earthquake caused widespread damage in southeastern England and in the Low Countries. The earthquake interrupted a synod convened in part to examine the religious writings of John Wycliffe, which became known as the Earthquake Synod.
Earthquake
[edit]The magnitude for this event has been estimated using the distribution of felt intensities. Musson in 2008 gave a magnitude of 5.8 ML,[7] while Camelbeek et al. 2007 gave 6.0 Ms .[4]
The epicentral location has also been estimated from the distribution of felt intensities A location in the middle of the Dover Straits, somewhat to the northeast of the similar 1580 Dover Straits earthquake is preferred.[7][4]
There were significant aftershocks on the 23 May and on the 24 May, the latter being the strongest recorded. The 24 May aftershock was also described as a "Waterquake" affecting anchored ships.[7]
Damage
[edit]In England, the most severe damage was recorded in Canterbury, particularly to St Augustine's Abbey and Christ Church, Canterbury, where the bell-tower was destroyed. The manor house and church at Hollingbourne, Kent were also badly damaged. This has been used to estimate intensity in the range VII-VIII.[6] In London there was damage to St Paul's Cathedral and Westminster Abbey with an estimated intensity of VI–VII.[7]
In the Low Countries damage was reported from Ypres, Bruges, Liege and Ghent.[6]
There is no record of casualties associated with this event.
Earthquake synod
[edit]William Courtenay, the Archbishop of Canterbury convened a synod that met in Blackfriars, in London on the day of the earthquake. The synod was intended to consider the challenges to the church by the group of thinkers that became known as the Lollards, particularly the writings of John Wycliffe. During the deliberations the monastery was shaken by the earthquake, but Courtenay turned it to his advantage saying
"This earthquake portends the purging of the kingdom from heresies, For as there are shut up in the bowels of the earth many noxious spirits, which are expelled in an earthquake, and so the earth is cleansed, but not without great violence: so there are many heresies shut up in the hearts of reprobate men, but by the condemnation of them the kingdom is to be cleansed, but not without irksomeness and great commotion"
. The court found ten of Wycliffe's propositions to be heretical and another six erroneous, allowing Lollards to be prosecuted and executed.[8]
References
[edit]- ^ ANSS: Chiapas 2017 .
- ^ Cumes, William (7 September 2017). "Temblor de 7.7 grados sacude Guatemala". Prensa Libre (in Spanish).
- ^ @SSNMexico (21 September 2017). "Hasta las 5:30 am del 21-sep: 34 réplicas (M4.0 la mayor) del sismo del 19-sep M7.1 y 3831 réplicas (M6.1 la mayor) del sismo del 7-sep M8.2" (Tweet) – via Twitter.
- ^ a b c Camelbeek T.; Vanneste K.; Alexandre P.; Verbeeck K.; Petermans T.; Rosset P.; Everaerts M.; Warnant R.; van Camp M. (2007). "Relevance of active faulting and seismicity studies to assessments of long-term earthquake activity and maximum magnitude in intraplate northwest Europe, between the Lower Rhine Embayment and the North Sea" (PDF). The Geological Society of America Special Paper. 425. doi:10.1130/2007.2425(14).
- ^ British Geological Survey. "1382 Dover Straits". Historic British Earthquakes. Retrieved 17 March 2018.
- ^ a b c Varley, P.M. (1996), "Seismic risk assessment and analysis", in Harris, Colin S. (ed.), Engineering geology of the Channel Tunnel, Thomas Telford, pp. 195–8, ISBN 978-0-7277-2045-0
- ^ a b c d Musson R.M.W. (2008). "The seismicity of the British Isles to 1600" (PDF). British Geological Survey Open Report , OR/08/049. British Geological Survey. pp. 45–48. Retrieved 14 March 2018.
- ^ Wylie J.A. (2013) [1874]. The History of Protestantism.
Category:Earthquakes in the United Kingdom Category:14th-century earthquakes
UCERF3
[edit]From UCERF3 Table 7
| Region | M ≥ 6.0 | 6.7 | 7.0 | 7.5 | 7.7 | 8.0 |
|---|---|---|---|---|---|---|
| All CA | 100% 100% 100% | 97% 100% 100% | 77% 93% 100% | 17% 48% 85% | 03% 27% 71% | 00% 07% 32% |
| N. CA | 100% 100% 100% | 84% 95% 100% | 55% 76% 96% | 08% 28% 60% | 01% 15% 45% | 00% 05% 25% |
| S. CA | 100% 100% 100% | 77% 93% 100% | 44% 75% 97% | 09% 36% 79% | 02% 22% 68% | 00% 07% 32% |
| SF | 89% 98% 100% | 52% 72% 94% | 27% 51% 84% | 05% 20% 43% | 00% 10% 32% | 00% 04% 21% |
| LA | 84% 96% 100% | 28% 60% 92% | 17% 46% 87% | 05% 31% 77% | 01% 20% 68% | 00% 07% 32% |
xxx
[edit]scale table
[edit]| Scale | ~Mag. | Distance |
|---|---|---|
| ML | 2-7.5 | 0–600 km |
| Mw | >3.5 | all |
| Me | >3.5 | all |
| Ms_20 | 5-8.5 | 20-160 ° |
| mb | 4-7 | 15-100° |
| mbLg | 3.5-7 | 150–1100 km |
| Md | <4 | 0–400 km |
From http://earthquake.usgs.gov/earthquakes/eventpage/terms.php
From M/sandbox: