1707, Chichester, and Coast from Havant to Shoreham.

Beckett., 1931 - Periodicals. A part of Ruthin Castle was ruined and the bell in the market town of Denbigh sounded two strokes. Reprinted with additions in 1887. The British Geological Survey later referred to an earthquake of magnitude 5 in this (Chichester-Isle of Wight) area, 1882 - Tsunami at Hurst Spit? North Sea]. 88.] Indeed, many Puritans blamed the emerging theatre scene of the time in London, which was seen as the work of the Devil, as a cause of the quake. 1089, Aug. 11, 3rd hour of the night. There has to be a correction for distance of the seismometer from the focus of the earthquake, and certain types of waves are used for measurement.

Flux and reflux lasted 3 hours.
Seismicity and Earthquake Hazard in the UK. (Destruction of St. Michael's on the Mount, the church on Glastonbury Tor). 1833, 13th November, 6 am. Musson (of the British Geological Survey).

31, p. 1761, 6th February, Sturminster.

The earthquakes have been attributed to minor re-activation on a deep north-south strike-slip fault, which is the eastern termination of the Isle of Wight type of structures, and may be linked southward to the Massif Central of France. The epicentre was undoubtedly between Dover and Calais, and the earthquake was felt over most of England, certainly as far as York and possibly as far as Edinburgh in Scotland (the dating of the Edinburgh report is uncertain).

1426. (Wikipedia List and Earthquake Track) Depth 10km. 1756, Extensive shocks in the Alps; also felt at London, Dover, Deal, Margate, Canterbury (Mallet).
At London and environs the earthquake lasted about one minute. Magnitude (modern system) 8.5 - 9. In Dover, part of the chalk cliff collapsed, taking with it part of Dover Castle. The disturbed area is 30 miles long, 20 miles wide and contains about 470 square miles. A notable area for mostly minor earthquakes is the region of Chichester (and adjacent Portsmouth) and the emphasis is on this region because the associated webpages are on the Wessex Coast. They are listed here as "Davison intensity 5" and should not be confused with a modern magnitude system. Unconfirmed as a Chichester earthquake but quite possible. KENT EARTHQUAKE, 22nd MAY 2015, [data from newspapers, TV, BBC website etc. BGS. See Mallet, 1858] It was remarked that the summits of the building were violently shaken whilst their foundations were not. Of considerable value in itself, it is interesting as the first report of a committee instituted for the study of British earthquakes." The report which he drew up was communicated to the Royal Society, but only a very brief summary was published [Royal Society Proceedings, vol. Chichester. These earthquakes were studied by an unofficial committee in Chichester, of which Mr. J.P. Gruggen was secretary. This is followed by a description of British seismicity from region to region, with remarks on some key earthquakes of interest. 1834. Some are listed by Davison are according to his own scheme, and do not relate to a modern system. Cat. Estimate 5.9. Rygate [Reigate}, Croydon and Darkin [Dorking]in Surrey.
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1707, Chichester, and Coast from Havant to Shoreham.

Beckett., 1931 - Periodicals. A part of Ruthin Castle was ruined and the bell in the market town of Denbigh sounded two strokes. Reprinted with additions in 1887. The British Geological Survey later referred to an earthquake of magnitude 5 in this (Chichester-Isle of Wight) area, 1882 - Tsunami at Hurst Spit? North Sea]. 88.] Indeed, many Puritans blamed the emerging theatre scene of the time in London, which was seen as the work of the Devil, as a cause of the quake. 1089, Aug. 11, 3rd hour of the night. There has to be a correction for distance of the seismometer from the focus of the earthquake, and certain types of waves are used for measurement.

Flux and reflux lasted 3 hours.
Seismicity and Earthquake Hazard in the UK. (Destruction of St. Michael's on the Mount, the church on Glastonbury Tor). 1833, 13th November, 6 am. Musson (of the British Geological Survey).

31, p. 1761, 6th February, Sturminster.

The earthquakes have been attributed to minor re-activation on a deep north-south strike-slip fault, which is the eastern termination of the Isle of Wight type of structures, and may be linked southward to the Massif Central of France. The epicentre was undoubtedly between Dover and Calais, and the earthquake was felt over most of England, certainly as far as York and possibly as far as Edinburgh in Scotland (the dating of the Edinburgh report is uncertain).

1426. (Wikipedia List and Earthquake Track) Depth 10km. 1756, Extensive shocks in the Alps; also felt at London, Dover, Deal, Margate, Canterbury (Mallet).
At London and environs the earthquake lasted about one minute. Magnitude (modern system) 8.5 - 9. In Dover, part of the chalk cliff collapsed, taking with it part of Dover Castle. The disturbed area is 30 miles long, 20 miles wide and contains about 470 square miles. A notable area for mostly minor earthquakes is the region of Chichester (and adjacent Portsmouth) and the emphasis is on this region because the associated webpages are on the Wessex Coast. They are listed here as "Davison intensity 5" and should not be confused with a modern magnitude system. Unconfirmed as a Chichester earthquake but quite possible. KENT EARTHQUAKE, 22nd MAY 2015, [data from newspapers, TV, BBC website etc. BGS. See Mallet, 1858] It was remarked that the summits of the building were violently shaken whilst their foundations were not. Of considerable value in itself, it is interesting as the first report of a committee instituted for the study of British earthquakes." The report which he drew up was communicated to the Royal Society, but only a very brief summary was published [Royal Society Proceedings, vol. Chichester. These earthquakes were studied by an unofficial committee in Chichester, of which Mr. J.P. Gruggen was secretary. This is followed by a description of British seismicity from region to region, with remarks on some key earthquakes of interest. 1834. Some are listed by Davison are according to his own scheme, and do not relate to a modern system. Cat. Estimate 5.9. Rygate [Reigate}, Croydon and Darkin [Dorking]in Surrey.
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dover earthquake uk


(some notes from On the Wight webpage, 2011). "On the Facts of Earthquake Phenomena." The list is not comprehensive. ;

1707, Chichester, and Coast from Havant to Shoreham.

Beckett., 1931 - Periodicals. A part of Ruthin Castle was ruined and the bell in the market town of Denbigh sounded two strokes. Reprinted with additions in 1887. The British Geological Survey later referred to an earthquake of magnitude 5 in this (Chichester-Isle of Wight) area, 1882 - Tsunami at Hurst Spit? North Sea]. 88.] Indeed, many Puritans blamed the emerging theatre scene of the time in London, which was seen as the work of the Devil, as a cause of the quake. 1089, Aug. 11, 3rd hour of the night. There has to be a correction for distance of the seismometer from the focus of the earthquake, and certain types of waves are used for measurement.

Flux and reflux lasted 3 hours.
Seismicity and Earthquake Hazard in the UK. (Destruction of St. Michael's on the Mount, the church on Glastonbury Tor). 1833, 13th November, 6 am. Musson (of the British Geological Survey).

31, p. 1761, 6th February, Sturminster.

The earthquakes have been attributed to minor re-activation on a deep north-south strike-slip fault, which is the eastern termination of the Isle of Wight type of structures, and may be linked southward to the Massif Central of France. The epicentre was undoubtedly between Dover and Calais, and the earthquake was felt over most of England, certainly as far as York and possibly as far as Edinburgh in Scotland (the dating of the Edinburgh report is uncertain).

1426. (Wikipedia List and Earthquake Track) Depth 10km. 1756, Extensive shocks in the Alps; also felt at London, Dover, Deal, Margate, Canterbury (Mallet).
At London and environs the earthquake lasted about one minute. Magnitude (modern system) 8.5 - 9. In Dover, part of the chalk cliff collapsed, taking with it part of Dover Castle. The disturbed area is 30 miles long, 20 miles wide and contains about 470 square miles. A notable area for mostly minor earthquakes is the region of Chichester (and adjacent Portsmouth) and the emphasis is on this region because the associated webpages are on the Wessex Coast. They are listed here as "Davison intensity 5" and should not be confused with a modern magnitude system. Unconfirmed as a Chichester earthquake but quite possible. KENT EARTHQUAKE, 22nd MAY 2015, [data from newspapers, TV, BBC website etc. BGS. See Mallet, 1858] It was remarked that the summits of the building were violently shaken whilst their foundations were not. Of considerable value in itself, it is interesting as the first report of a committee instituted for the study of British earthquakes." The report which he drew up was communicated to the Royal Society, but only a very brief summary was published [Royal Society Proceedings, vol. Chichester. These earthquakes were studied by an unofficial committee in Chichester, of which Mr. J.P. Gruggen was secretary. This is followed by a description of British seismicity from region to region, with remarks on some key earthquakes of interest. 1834. Some are listed by Davison are according to his own scheme, and do not relate to a modern system. Cat. Estimate 5.9. Rygate [Reigate}, Croydon and Darkin [Dorking]in Surrey.

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