Lake Dringo (Indonesian: Telaga Dringo; also called Sedringo or Sendringo) is a volcanic crater lake located in Pekasiran, Batur, Banjarnegara, Central Java, Indonesia.[2] It was formed from the eruption of Dringo volcano in 1786.[2]
| Lake Dringo | |
|---|---|
 A view of Lake Dringo | |
  Lake Dringo  Lake Dringo | |
| Location | Central Java, Indonesia |
| Coordinates | 7°11′12″S 109°50′52″E / 7.18667°S 109.84778°E |
| Type | Volcanic/tectonic |
| Basin countries | Indonesia |
| Max. length | 330 m (1,080 ft) |
| Max. width | 330 m (1,080 ft) |
| Surface elevation | 2,028 m (6,654 ft) |
| Settlements | Pekasiran, Batur, Banjarnegara |
| References | [1] |
Geology
editDringo Volcano was formed during the post-caldera I period, which is about 1 - 2 million years ago, as a part of the Dieng Volcanic Complex in the Batur depression region. The Dringo Volcano was built up mostly of intermediate composition and pyroxene andesite.[1][3]
Lake Dringo is the site of Dringo volcano eruption, indicated by the pyroclastic flows breccia outcrops around the lake which are generally found in a weathered weathered, brown, and altered conditions. The breccia fragments consist of pyroxene andesite: plagioclase, pyroxene, opaque minerals, and glass as groundmass.[3]
References
edit- ^ a b "G. Dieng - Geologi". Pusat Vulkanologi dan Mitigasi Bencana Geologi. Retrieved 27 December 2022.
- ^ a b Anggara, A P; Kartijono, N E; Bodijantoro, P M H (1 October 2017). "Keanekaragaman Plankton di Kawasan Cagar Alam Tlogo Dringo, Dataran Tinggi Dieng, Jawa Tengah". Indonesian Journal of Mathematics and Natural Sciences. 40 (2): 74–79. doi:10.15294/ijmns.v40i2.12563 (inactive 1 November 2024). Retrieved 27 December 2022.
{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link) - ^ a b Yudiantoro, D. F.; Haty, I. P.; Pambudi, S.; E., Magdalena; Putri, A.; Takashima, I.; Abdurrachman, M. (6 December 2022). "Evolution Magmatism of Nagasari Volcano Dieng, Central Java, Indonesia". Journal of Geoscience, Engineering, Environment, and Technology. 7 (4): 140–150. doi:10.25299/jgeet.2022.7.4.10084. S2CID 255877485.