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Banyusumurup

Cemeteries established in the 17th centuryCemetery stubsImogiriJava geography stubs
Entrance to Banyusumurup graveyard in the 1990s
Entrance to Banyusumurup graveyard in the 1990s

Banyusumurup is a sub-village (dusun) in Girirejo village, southeast of Imogiri in Bantul Regency, Special Region of Yogyakarta, Indonesia. The sub-village was acknowledged as a 'kris making' location at some stages in the 20th century.Banyusumurup is known for Banyusumurup Graveyard, part of the Imogiri Royal Graveyard complex, traditionally associated with being the 'outcast' graveyard of those who fell out of favour with rulers – in most cases in the 17th and 18th centuries.

Excerpt from the Wikipedia article Banyusumurup (License: CC BY-SA 3.0, Authors, Images).

Geographical coordinates (GPS)

Latitude Longitude
N -7.9293965 ° E 110.385826 °
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Address


55782 Imogiri
Special Region of Yogyakarta, Indonesia
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Entrance to Banyusumurup graveyard in the 1990s
Entrance to Banyusumurup graveyard in the 1990s
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Nearby Places

2006 Yogyakarta earthquake
2006 Yogyakarta earthquake

The 2006 Yogyakarta earthquake (also known as the Bantul earthquake) occurred at 05:54 local time on 27 May with a moment magnitude of 6.4 and a maximum MSK intensity of VIII (Damaging). Several factors led to a disproportionate amount of damage and number of casualties for the size of the shock, with more than 5,700 dead, tens of thousands injured, and financial losses of Rp 29.1 trillion ($3.1 billion). With limited effects to public infrastructure and lifelines, housing and private businesses bore the majority of damage (the 9th-century Prambanan Hindu temple compound was also affected), and the United States' National Geophysical Data Center classified the total damage from the event as extreme. Although Indonesia experiences very large thrust earthquakes offshore at the Sunda Trench, this was a large strike-slip event that occurred on the southern coast of Java near the city of Yogyakarta. Mount Merapi lies nearby, and during its many previous historical eruptions, large volume lahars and volcanic debris flowed down its slopes where settlements were later built. This unconsolidated material from the stratovolcano amplified the intensity of the shaking and created the conditions for soil liquefaction to occur. Inadequate construction techniques and poor quality materials contributed to major failures with unreinforced masonry buildings (then the most prevalent type of home construction), though other styles fared better.