Lhoknga
District in Great Aceh Regency, Aceh Province, Indonesia
Lhoknga (Acehnese: Lhôk Nga; Jawoe: تلوق ڠا, pronounced [lʱoʔ ŋa], alternative names Lho'nga, Lho-nga, Lhok Nga) is a town within the district of the same name, in Aceh Besar Regency, Aceh Special Region, Indonesia, located on the western side of the island of Sumatra, 13 km southwest of Banda Aceh. It was completely flattened and destroyed by the 2004 Indian Ocean earthquake and tsunami, where its population dwindled from 7,500 to 400.
Nº Q3535102 ★
Común · Lugares
Lhoknga
District in Great Aceh Regency, Aceh Province, Indonesia
Lhoknga (Acehnese: Lhôk Nga; Jawoe: تلوق ڠا, pronounced [lʱoʔ ŋa], alternative names Lho'nga, Lho-nga, Lhok Nga) is a town within the district of the same name, in Aceh Besar Regency, Aceh Special Region, Indonesia, located on the western side of the island of Sumatra, 13 km southwest of Banda Aceh. It was completely flattened and destroyed by the 2004 Indian Ocean earthquake and tsunami, where its population dwindled from 7,500 to 400.
En el mapa
Último precio
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Precio mínimo
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Mediana 7 d
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Ventas 30 d
0
Rango 30 d
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En circulación
0
Cotización
mediana
mín – máx
ventas
Sin ventas en el periodo
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Historial de ventas
- Última venta
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- Media 30 d
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- Mínimo 30 d
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- Máximo 30 d
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- Ventas 7 d
- 0
- Ventas 30 d
- 0
Aún no hay ventas.
Ventas anónimas: sin comprador ni vendedor. Las cifras solo cuentan ventas entre jugadores.
En Wikipedia
Texto en inglés Aún no hay artículo en tu idioma: extracto en inglés.
Lhoknga (Acehnese: Lhôk Nga; Jawoe: تلوق ڠا, pronounced [lʱoʔ ŋa], alternative names Lho'nga, Lho-nga, Lhok Nga) is a town within the district of the same name, in Aceh Besar Regency, Aceh Special Region, Indonesia, located on the western side of the island of Sumatra, 13 km southwest of Banda Aceh. It was completely flattened and destroyed by the 2004 Indian Ocean earthquake and tsunami, where its population dwindled from 7,500 to 400. Tsunami runups following eyewitness accounts of waves were recorded being 35 m in height (waves landing at the height of 35 m), Such high and fast waves arising from the epicentre by megathrusts were later found to be due to splay faults, secondary faults arising due to cracking of the sea floor to jut upwards in seconds, causing waves' speed and height to increase.
Texto: Wikipedia en inglés, CC BY-SA 4.0. · Imagen: Unknown authorUnknown author (CC BY-SA 3.0) ·
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