The magnitude 8.0 North Anatolia earthquake causes 8,000 deaths in northern Anatolia, Ottoman Empire, and is the most powerful earthquake recorded in Turkey

Quando

17 de ago. de 1668

Tipo

Terremoto

Coordenadas

38.40° N, 27.10° E

Description

The magnitude 8.0 North Anatolia earthquake causes 8,000 deaths in northern Anatolia, Ottoman Empire, and is the most powerful earthquake recorded in Turkey.

Posicionado em: coordinates of the event it links, 1668 North Anatolia earthquake.

Most powerful earthquake in Turkish history

Northern Anatolia was struck by a large earthquake on 17 August 1668 in the late morning. It had an estimated magnitude in the range 7.8–8.0 Ms and the maximum felt intensity was IX on the Modified Mercalli intensity scale. The epicenter of the earthquake was on the southern shore of Ladik Lake. It caused widespread damage from as far west as Bolu and as far east as Erzincan, resulting in about 8,000 deaths.

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• Wikipedia year pages (English), by Wikipedia contributorsWikipedia contributorsCreative Commons Attribution-ShareAlike 4.0Página da fonte
• Wikipedia year pages (Turkish), by Wikipedia contributorsWikipedia contributors · registra como “Samsun'da Ladik Gölü merkezli 8.0 büyüklüğündeki 1668 Kuzey Anadolu depreminde”Creative Commons Attribution-ShareAlike 4.0Página da fonte
• Wikipedia year pages (German), by Wikipedia contributorsWikipedia contributors · registra como “Ein Erdbeben in Nordanatolien, im Norden der Türkei, mit einer Stärke zwischen 7,8 und 8,0 verursacht entlang des 600 km langen Abschnitts der Nordanatolischen…”Creative Commons Attribution-ShareAlike 4.0Página da fonte
• Wikipedia year pages (French), by Wikipedia contributorsWikipedia contributors · registra como “un violent séisme de magnitude 8,0 frappe l'Anatolie du Nord provoquant environ de”Creative Commons Attribution-ShareAlike 4.0Página da fonte
• Wikipedia year pages (Spanish), by Wikipedia contributorsWikipedia contributors · registra como “en Anatolia (Turquía) un terremoto de 8,0 deja 8000 muertos”Creative Commons Attribution-ShareAlike 4.0Página da fonte