Knowledge (XXG)

Kelimutu

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status of the fluid of each lake, and also considering the abundance of different major elements, such as iron and manganese. Oxidation-reduction status depends on the balance of volcanic gas input and rainfall rate, and is thought to be mediated by the groundwater system in the volcano itself. The colors in the lakes change independently from each other, as each has its own unique connectivity to the underlying volcano's activity. Between January and November 2016, the colors of the craters changed six times. Although it is widely believed that the changes are unpredictable, it is more accurate to say that the lack of any regular monitoring of the volcanic system precludes scientists from having the data necessary to drive widely available predictive models.
128: 121: 404: 416: 814: 379: 197: 392: 428: 346: 29: 378: 325:. There are regular flights to Ende from Bali. The drive from Ende to Moni, the town at the base of Kelimutu where accommodation is available, takes about 3 hours, while from Moni to Kelimutu vehicle park, a 13 kilometres (8.1 mi) drive, needs 45 minutes. Usually tourists sleep one night to catch sunrise at Kelimutu. 283:
Kelimutu is also of interest to geologists, because the three lakes have different colors, yet are at the crest of the same volcano. According to Kelimutu National Park officials, the colour changes as a result of chemical reactions resulting from the minerals contained in the lake perhaps triggered
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of varying colors. Tiwu Ata Bupu (Lake of Old People) is usually blue and is the westernmost of the three lakes. The other two lakes, Tiwu Ko'o Fai Nuwa Muri (Lake of Young Men and Maidens) and Tiwu Ata Polo (Bewitched or Enchanted Lake) are separated by a shared crater wall and are typically green
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The science of the Kelimutu lakes is relatively well-known, and the changes in color and temperature are concluded to be related to volcanic activity and the resulting fluid flux at vents at the bottom of the lakes. The Lake colors periodically change due to adjustments in the oxidation-reduction
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In the early days of developing the local national park in the Kelimutu area, there were some disputes with local communities over the use of the resources. More recently, forest rangers have worked to develop better relations with nearby village communities and overall management has improved.
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Kelimutu is sacred to the local Lio people, who believe the souls of the dead migrate here. Young people's souls go to the warmth of Tiwu Koo Fai Nuwa Muri (Lake of Young Men and Maidens), old people's to the cold of Tiwu Ata Bupu (Lake of Old People), and those of the wicked to Tiwu Ata Polo
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Aerial view from the krater lakes, at the lower left is the Tiwu Ata Mbupu (Lake of Old People), at the upper centre Tiwu Ko'o Fai Nuwa Muri (Lake of Young Men and Maiden) and Tiwu Ata Polo (Bewitched, or Enchanted Lake) at the upper
334:(Bewitched or Enchanted Lake). Pork, betel nuts, rice and other valuable offerings are left on ceremonial rocks beside the lakes, amid the dancing of the Lio's annual 'Feed the Spirit of the Forefathers' ceremony, on August 14. 858: 593:
Pasternack, G. B. 1993. Acid-brine crater lake systematics: a case study. Undergraduate High Honors thesis. Wesleyan University, 160 pp, 4 appendices. DOI: 10.13140/RG.2.1.3414.1040.
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Herrick, Julie. (2013). Nevado del Tolima (Colombia): Non-eruptive activity during 2005-2012: hazard assessment and glacial retreat. Bulletin of Global Volcanism Network. 38. 27.
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The area is said to have begun to attract attention after being noticed by a regional Dutch military commander, B. van Suchtelen in 1915 and became more well known after
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in historical time. The summit of the compound 1,639 m (5,377 ft) high Kelimutu volcano is elongated 2 km (1.2 mi) in a WNW-ESE direction; the older
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of Kelido and Kelibara are located respectively 3 km (1.9 mi) to the north and 2 km (1.2 mi) to the south. The scenic lakes are a popular
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by volcano gas activity. However, it is more accurate to refer to the color changes as being driven by oxidation-reduction chemical dynamics.
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Soil properties of the eastern toposequence of Mount Kelimutu, Flores Island, East Nusa Tenggara and their potential for agricultural use'
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Some details of the characteristics of volcanic soils in the area can be found at Hikmatullah, H. Subagyo, and B.H. Prasetyo, '
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Exotic NTT: 200 tempat paling menantang dan eksotis di provinsi Nusa Tenggara Timur: wisata alam, bahari, budaya, dan tradisi
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lake in West Java, south of Bandung, is another crater lake in Indonesia with some similarities to the lakes at Kelimutu.
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Pasternack, Gregory B.; Varekamp, Johan C. (1997-05-01). "Volcanic lake systematics I. Physical constraints".
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in Indonesia which are mountains in Indonesia which are more than 1,000 metres (3,281 ft) high.
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or red respectively. The lake colors vary on a periodic basis. Subaqueous
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province. It has three volcanic crater lakes that differ in color.
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is a special issue of the journal dedicated to Volcanic lakes.
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Murphy, Sam; Wright, Robert; Rouwet, Dmitri (January 2018).
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Volume 28, No. 3, pp. 137-306 of the Geochemical Journal
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The Tiwu Ko'o Fai Nuwa Muri has been a source of minor
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Index


Elevation
Listing
List of volcanoes in Indonesia
Spesial Ribu
Coordinates
8°46′S 121°49′E / 8.77°S 121.82°E / -8.77; 121.82
Kelimutu is located in Flores
Ende Regency
Flores Island
Indonesia
Mountain type
Complex volcano
Last eruption

5,000-rupiah banknote
[kəliˈmutu]
volcano
Flores island
Indonesia
Ende, Indonesia
Ende regency
East Nusa Tenggara
crater lakes
fumaroles
upwelling
phreatic eruptions
cones
tourist destination
Kawah Putih

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