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Lhoknga
EntityQ3535102· pop 13· linked from 16 articles

Also known as Kecamatan Lhoknga, Lhok Nga, Lhoknga District

thumb | right | Picture of Lam Puuk Beach near the town of Lhoknga one year after the tsunami disaster. Lhoknga (pronunciation [lhoʔ-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

Key facts

Settlement.official_name
Lhoknga
Settlement.native_name
Lhôk Nga
Settlement.pushpin_map
Indonesia Sumatra
Settlement.pushpin_map_caption
Location in Sumatra
Settlement.pushpin_mapsize
300
Settlement.subdivision_type
Country
Settlement.subdivision_type1
Province
Settlement.subdivision_name1
Aceh
Settlement.population_as_of
2006
Settlement.population_total
400
Settlement.timezone
WIB
Settlement.utc_offset
+7

via Wikipedia infobox

Wikidata facts

Instance of
kecamatan
Country
Indonesia
Located in
Great Aceh
Elevation
7
Time zone
UTC+07:00
Image
COLLECTIE TROPENMUSEUM Tjemara's langs de kust bij Lhonga Atjeh TMnr 10012959.jpg
Show 3 more facts
Commons category
Lhoknga
Statistics Indonesia area code
1108020
name
Lhoknga
Sources (5)

via Wikidata · CC0

~1 min read

Encyclopedic overview

1 sections
Contents
  • Notes and references

thumb | right | Picture of Lam Puuk Beach near the town of Lhoknga one year after the tsunami disaster. Lhoknga (pronunciation [lhoʔ-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.

== Notes and references ==

Excerpted from Wikipedia’s “Lhoknga” article, available under the CC BY-SA 4.0 licence.

On the map

3 mapped locations