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The Catalan earthquake of February 2, 1428, known in Catalan as the terratrèmol de la candelera because it took place during Candlemas, struck the region of Catalonia, especially Roussillon, with an epicentre near Camprodon. The earthquake was one of a series of related seismic events that shook Catalonia in a single year. Beginning on February 23, 1427, tremors were felt in March, April, May 15 at Olot, June, and December. They caused relatively minor visible damage to property, notably to the ; but they probably caused severe weakening of building infrastructure. This would account for the massive and widespread destruction that accompanied the subsequent 1428 quake.

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  • Terratrèmol de Catalunya de 1428 (ca)
  • Erdbeben von Olot (15. Jahrhundert) (de)
  • 1428 Catalonia earthquake (en)
  • Terremoto de Cataluña de 1428 (es)
  • Séisme du 2 février 1428 en Catalogne (fr)
  • Sismo da Catalunha de 1428 (pt)
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  • Das Pyrenäengebiet gilt als seismisch aktive Zone. Im Laufe der Geschichte wurden immer wieder Beben um den Pyrenäenkamm herum berichtet. Der spanische Historiker Jeronimo Zurita erwähnt ein großes Beben vom 2. Februar 1373 in der Grafschaft Ribagorça mit starken Verwüstungen und vielen Toten. Zu Ende des ersten Drittels des 15. Jahrhunderts – genauer von 1427 bis 1429 – kulminierte das seismische Geschehen in einer Serie von Erdbeben in der Gegend von Olot. (de)
  • Le séisme de 1428 en Catalogne est un séisme d'intensité VIII-IX sur l'échelle MSK et de magnitude 6,5 ayant eu lieu le 2 février 1428. Il est aussi connu sous le nom de séisme de la Chandeleur. C'est le séisme le plus fort de mémoire d'homme dans les Pyrénées (fr)
  • El terratrèmol del 2 de febrer de 1428, conegut popularment com el terratrèmol de la Candelera, tingué l'epicentre situat prop de Camprodon. El moviment va assolir una intensitat de 9 i una magnitud de 6.5., i va ocasionar danys a tot el Principat de Catalunya i també als Comtats (Catalunya Nord).És el darrer d'una sèrie que començà al , seguit el 15 de maig de 1427 a Olot i aquest del 1428 què es considerà el més intens que ha patit Catalunya des del primer documentat el 1373. Causà més de mil morts entre: Camprodon (200), Puigcerdà (100-300, per l'enfonsament de l'església), Barcelona (20-30, a Santa Maria del Mar), i la pràctica totalitat dels habitants de Queralbs. (ca)
  • The Catalan earthquake of February 2, 1428, known in Catalan as the terratrèmol de la candelera because it took place during Candlemas, struck the region of Catalonia, especially Roussillon, with an epicentre near Camprodon. The earthquake was one of a series of related seismic events that shook Catalonia in a single year. Beginning on February 23, 1427, tremors were felt in March, April, May 15 at Olot, June, and December. They caused relatively minor visible damage to property, notably to the ; but they probably caused severe weakening of building infrastructure. This would account for the massive and widespread destruction that accompanied the subsequent 1428 quake. (en)
  • El terremoto de Cataluña del 2 de febrero de 1428, conocido en catalán como terratrèmol de la candelera debido a que tuvo lugar durante la Candelaria, azotó la región de Cataluña, sobre todo el Rosellón y el norte en general, con el epicentro cerca de Camprodón, en los Pirineos. El sismo fue una serie de eventos sísmicos asociados que sacudió a Cataluña en un solo año. A partir del 23 de febrero de 1427, los temblores se sintieron en marzo, abril, 15 de mayo en Olot, en junio y en diciembre. (es)
  • O Sismo da Catalunha de 1428, conhecido em Catalão como o terratrèmol de la candelera pois aconteceu durante Candlemas, atingiu a região da Catalunha, especialmente Rossilhão, com um epicentro perto de Camprodon. O terremoto foi um de uma série de eventos sísmicos relacionados que atingiram a Catalunha em um ano. Começando em 23 de Fevereiro de 1427, tremores foram sentidos em Março, Abril, 15 de Maio em Olot, Junho e Dezembro. Estes causaram dano visível relativamente pequeno à propriedades, notavelmente no monastério de Amer; Mas provavelmente causaram severos enfraquecimentos na infraestrutura de construções. Isto contaria no contexto da massiva e generalizada destruição que acompanhou o sismo subsequente de 1428. (pt)
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