Matches in DBpedia 2016-04 for { ?s ?p "The Great Kantō earthquake (関東大震災, Kantō daishinsai) struck the Kantō Plain on the Japanese main island of Honshū at 11:58:44 a.m. JST (2:58:44 UTC) on Saturday, September 1, 1923. Varied accounts indicate the duration of the earthquake was between four and ten minutes.The earthquake had a magnitude of 7.9 on the moment magnitude scale (Mw), with its focus deep beneath Izu Ōshima Island in Sagami Bay. The cause was a rupture of part of the convergent boundary where the Philippine Sea Plate is subducting beneath the Okhotsk Plate along the line of the Sagami Trough."@en }
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- 1923_Great_Kantō_earthquake abstract "The Great Kantō earthquake (関東大震災, Kantō daishinsai) struck the Kantō Plain on the Japanese main island of Honshū at 11:58:44 a.m. JST (2:58:44 UTC) on Saturday, September 1, 1923. Varied accounts indicate the duration of the earthquake was between four and ten minutes.The earthquake had a magnitude of 7.9 on the moment magnitude scale (Mw), with its focus deep beneath Izu Ōshima Island in Sagami Bay. The cause was a rupture of part of the convergent boundary where the Philippine Sea Plate is subducting beneath the Okhotsk Plate along the line of the Sagami Trough.".
- Q274498 abstract "The Great Kantō earthquake (関東大震災, Kantō daishinsai) struck the Kantō Plain on the Japanese main island of Honshū at 11:58:44 a.m. JST (2:58:44 UTC) on Saturday, September 1, 1923. Varied accounts indicate the duration of the earthquake was between four and ten minutes.The earthquake had a magnitude of 7.9 on the moment magnitude scale (Mw), with its focus deep beneath Izu Ōshima Island in Sagami Bay. The cause was a rupture of part of the convergent boundary where the Philippine Sea Plate is subducting beneath the Okhotsk Plate along the line of the Sagami Trough.".