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1692 Jamaica earthquake

Coordinates: 18°00′N 76°30′W / 18.00°N 76.5°W / 18.00; -76.5
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1692 Jamaica earthquake
1692 Jamaica earthquake is located in Jamaica
1692 Jamaica earthquake
Local date7 June 1692 (1692-06-07)
Local time11:43
Magnitude7.5 Mw[1]
Depth10 km
Epicenter18°00′N 76°30′W / 18.00°N 76.5°W / 18.00; -76.5
Areas affectedJamaica
TsunamiYes
CasualtiesAround 5,000

The 1692 Jamaica earthquake struck Port Royal, Jamaica, on 7 June. A stopped pocket watch found in the harbor during a 1959 excavation[2][3][4] indicated that it occurred around 11:43 AM local time.[5]

Known as the "storehouse and treasury of the West Indies" and as the "wickedest city in the world",[2] Port Royal was, at the time, a key city in colonial Jamaica and one of the busiest and wealthiest ports in the Americas, as well as a common home port for many of the privateers and pirates operating on the Caribbean Sea.

The 1692 earthquake caused most of the city to sink below sea level. About 2,000 people died as a result of the earthquake and the following tsunami, and another 3,000 people died in the following days due to injuries and disease.[5]

Tectonic setting

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The Gonâve microplate, showing the main fault zones that bound it

The island of Jamaica lies on the boundary between the Caribbean Plate and the Gonâve Microplate. The Gonâve microplate is a 1,100 km (680 mi) long strip of mainly oceanic crust formed by the Cayman spreading ridge within a strike-slip pull-apart basin on the northern transform margin of the Caribbean Plate with the North American Plate.[6] Jamaica was formed by uplift associated with a restraining bend along this strike-slip structure.[7] The focal mechanisms of earthquakes around Jamaica are primarily sinistral strike-slip along WSW-ENE trending faults and minor reverse or thrust motion on NW-SE trending faults.[6] The 1692 event is thought to have occurred on one of these strike-slip faults.

Damage

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Old map of Port Royal
Map of Port Royal showing shorelines before and after the earthquake

Two-thirds of the town, about 13 ha (33 acres), sank into the sea immediately after the main shock.[5] According to Robert Renny in his An History of Jamaica (1807): "All the wharves sunk at once, and in the space of two minutes, nine-tenths of the city were covered with water, which was raised to such a height, that it entered the uppermost rooms of the few houses which were left standing. The tops of the highest houses were visible in the water and surrounded by the masts of vessels, which had been sunk along with them."[8]

Before the earthquake the town consisted of 6,500 inhabitants living in about 2,000 buildings, many constructed of brick and with more than one storey, and all built on loose sand. During the shaking, the sand liquefied and the buildings, along with their occupants, appeared to flow into the sea.[9] More than twenty ships moored in the harbour were capsized. One ship, the frigate HMS Swann, was carried over the rooftops by the tsunami.[10] During the main shock, the sand was said to have formed waves. Fissures repeatedly opened and closed, crushing many people. After the shaking stopped the sand again solidified, trapping many victims. Palisadoes cemetery, where the grave of the former pirate Sir Henry Morgan was located, was one of the parts of the city to fall into the sea; his body has never been found.[11]

At Liguanea (present-day Kingston), all the houses were destroyed and water was ejected from 12-metre (40-foot) deep wells. Almost all the houses at St. Jago (Spanish Town) were destroyed.[12]

Many landslides occurred across the island.[5] The largest, the Judgement Cliff landslide, displaced the land surface by up to 800 metres (2,625 ft) and killed 19 people.[6] Several rivers were temporarily dammed and a few days after the earthquakes the harbour became flooded with large numbers of trees stripped of their bark brought down after one of these dams was breached.[13]

A pocket watch, made in the Netherlands by the French maker Blondel in about 1686, was recovered during underwater archaeological investigations led by Edwin Link in 1959.[2] The watch was stopped with its hands pointing to 11:43 AM; this matches well with contemporary accounts of the timing of the earthquake.[5]

Aftermath

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Even before the destruction was complete, some of the survivors began looting, breaking into homes and warehouses. The dead were also robbed and stripped, and, in some cases, had fingers cut off to remove the rings that they wore.[9]

In the immediate aftermath of the earthquake, it was common to ascribe the destruction to divine retribution on the people of Port Royal for their sinful ways. Members of the Jamaica Council declared: "We are become by this an instance of God Almighty's severe judgement." This view of the disaster was not confined to Jamaica; in Boston, the Reverend Cotton Mather said in a letter to his uncle: "Behold, an accident speaking to all our English America".[9]

After the earthquake, the town was partially rebuilt. But the colonial government was relocated to Spanish Town, which had been the capital under Spanish rule. Port Royal was devastated by a fire in 1703 and a hurricane in 1722. Most of the sea trade moved to Kingston. By the late 18th century, Port Royal was largely abandoned.[14]

Characteristics

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Earthquake

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There were three separate shocks, each with increasing intensity, culminating in the main shock.[5] The estimated size of the event was 7.5 on the moment magnitude scale.[1]

Despite reports of the town flowing into the sea, the main result of the earthquake was subsidence caused by liquefaction. This would also explain an eyewitness account of houses being swallowed and people being buried up to their necks in the sand.[15] The probable triggering of the Judgement Cliff landslide during the earthquake occurred along the line of the Plantain Garden fault. Movement on this structure has been suggested as the cause of the earthquake.[6]

Landslides

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The Judgement Cliff landslide is a complex rock-slide slump with a volume of about 131–181 × 106 m3. The slip surface is found within zones of clay and shale with gypsum at the base of a limestone unit. This landslide occurred after the earthquake but it remains possible that heavy rain over the few days after the event, or possibly during a hurricane in October later that year was the final trigger for the slip.[16]

Tsunami

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The sea was observed to retreat by about 300 yd (270 m) at Liguanea (probably near Kingston) while at Yallahs it withdrew 1 mi (1.6 km). It returned as a 6 ft (1.8 m) high wave that swept over the land.[5] One possible cause of the tsunami is thought to be the slump and grain flow into the harbour from beneath the town itself, although the waves in the harbour may be better described as seiches and larger waves reported elsewhere, such as at Saint Ann's Bay, are explained as the result of an entirely separate submarine landslide, also triggered by the earthquake.[12]

Future seismic hazard

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Estimates of current deformation of Jamaica suggest that sufficient strain has accumulated to generate a M=7.0–7.3 earthquake, similar in size to the 1692 event. This may mean that a repeat of this event is imminent, although this estimate relies on many assumptions, such as that none of the motion on the Plantain Garden fault is accommodated by aseismic creep.[6]

See also

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References

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  1. ^ a b McCann, W.R. (2004). "Estimating the threat of tsunamigenic earthquakes and earthquake induced-landslide tsunami in the Caribbean" (PDF). In Mercado-Irizarry A, & Liu P. (ed.). Caribbean tsunami hazard: Proceedings of the NSF Caribbean Tsunami Workshop. World Scientific Publishing Co. pp. 43–65.
  2. ^ a b c Hamilton, D.L. (1991). "4: Simon Benning, Pewterer of Port Royal". In Little, B.J. (ed.). Text-Aided Archaeology. CRC Press. p. 40. ISBN 978-0-8493-8853-8.
  3. ^ Sunken Pirate City at Port Royal
  4. ^ a b c d e f g USGS (21 October 2009). "Historic Earthquakes: Jamaica 1692 June 07 UTC". Archived from the original on 17 December 2009. Retrieved 6 December 2009.
  5. ^ a b c d e DeMets, C.; Wiggins-Grandison W. (2007). "Deformation of Jamaica and motion of the Gonâve microplate from GPS and seismic data". Geophysical Journal International. 168 (1): 362–378. Bibcode:2007GeoJI.168..362D. doi:10.1111/j.1365-246X.2006.03236.x.
  6. ^ Mann, P.; Demets C. & Wiggins-Grandison M. (2007). "Toward a better understanding of the Late Neogene strike-slip restraining bend in Jamaica: geodetic, geological, and seismic constraints" (PDF). In Cunningham W.D. & Mann P. (ed.). Restraining bends, transpressional deformation and basement controls on development. Geological Society, London, Special Publications. Vol. 290. Geological Society, London. pp. 239–253.
  7. ^ Renny, Robert (1807). An history of Jamaica: with observations on the climate, scenery, trade, productions, negroes, slave trade, diseases of Europeans, customs, manners, and dispositions of the inhabitants: to which is added, an illustration of the advantages which are likely to result from the abolition of the Slave Trade. J. Cawthorn. p. 333.
  8. ^ a b c Gragg, L. (2000). "The Port Royal Earthquake". History Today. Retrieved 21 December 2009.
  9. ^ O'Loughlin, K. F.; Lander J. F. (2003). Caribbean Tsunamis: a 500-year history from 1498–1998. Advances in natural and technological hazards research. Vol. 20. Springer. p. 263. ISBN 978-1-4020-1717-9.
  10. ^ Allen, Hubert Raymond (1976). Buccaneer : admiral Sir Henry Morgan. London: Barker. ISBN 0-213-16569-4. OCLC 2202685.
  11. ^ a b "The Port Royal, Jamaica Earthquake and Tsunami of June 7, 1692" (PDF). TsuInfo Alert v. 3, No.4. 2001. Archived from the original (PDF) on 21 December 2009.
  12. ^ Lyell, Charles (1837). "XXV" (PDF). Principles of Geology. Vol. 1. p. 447. Archived from the original (PDF) on 21 May 2009.
  13. ^ Tortello, Rebecca. "1692:Earthquake of Port Royal". Archived from the original on 9 March 2010. Retrieved 22 December 2009.
  14. ^ "Eye Witness Account of Port Royal 1692 Earthquake".
  15. ^ Maharaj, R.J. (1994). "The morphology, geometry and kinematics of Judgement Cliff rock avalanche, Blue Mountains, Jamaica, West Indies". Quarterly Journal of Engineering Geology. 27 (3): 243–256. doi:10.1144/GSL.QJEGH.1994.027.P3.05. S2CID 129588923.

Further reading

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