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The Great Colchester Earthquake; The effects of the earthquake on the area of Eastern Essex south of the River Blackwater Archived 20 November 2008 at the Wayback Machine; Meldola, Raphael; White, William (1885). Report on the East Anglian Earthquake of April 22nd, 1884. Essex Field Club Special Memoirs. Vol. 1. London: Macmiillan & Co.
The 1880 Southern Luzon earthquakes, were one of the most destructive tremors on record in the history of the country.The shocks continued, with greater or less interruption, from July 14–25, 1880; highlighted by three violent quakes measuring M w 7.0, M w 7.6, and M w 7.2 respectively.
The Philippine Sea plate or the Philippine plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea, to the east of the Philippines. Most segments of the Philippines, including northern Luzon , are part of the Philippine Mobile Belt , which is geologically and tectonically separate from the Philippine Sea plate.
Pages in category "1884 earthquakes" The following 2 pages are in this category, out of 2 total. This list may not reflect recent changes. 0–9.
1976 Moro Gulf earthquake [10] [14] 1983 August 17 20:17 Luzon 6.5 VIII 16 dead, 47 injured 1983 Luzon earthquake [10] [14] 1985 April 24 Luzon: Benguet, Baguio 6.1 VII 6 dead, 11 injured [10] 1988 June 19 04:19 Mindoro: San Jose, Calapan 6.2 VII 2 dead, 2 injured 1988 Mindoro earthquake [10] [16] 1990 February 8 15:15 Bohol 6.8 VII 6 dead ...
Major physiographic elements of the Philippine Mobile Belt Puerto Princesa Subterranean River National Park marker describing the geologic history of the Philippines. In the geology of the Philippines, the Philippine Mobile Belt is a complex portion of the tectonic boundary between the Eurasian plate and the Philippine Sea plate, comprising most of the country of the Philippines.
The Rizal Shrine in Calamba is an example of bahay na bato.. Báhay na bató (Filipino for "stone house"), also known in Visayan languages as baláy na bató or balay nga bato, and in Spanish language as Casa de Filipina is a type of building originating during the Spanish colonial period of the Philippines.
The northern and southern extensions of the Philippine Fault Zone experience infrequent earthquakes and often described as locked segments which are capable of larger magnitude earthquakes. The largest (M7.0) and most destructive earthquakes are generated along the Guinayangan fault every 30–100 years with slip rates of 20–33 mm/year as ...