Speleotem
Tampilan
![](http://upload.wikimedia.org/wikipedia/commons/thumb/a/a1/Labeled_speleothems.jpg/220px-Labeled_speleothems.jpg)
Speleotem (pengucapan: /ˈspiːliːəθɛm/; bahasa Yunani Kuno: "deposit gua"), umumnya dikenal sebagai formasi gua, adalah endapan mineral sekunder yang terbentuk dalam sebuah gua. Speleotem biasanya terbentuk dalam gua soliter batu kapur atau dolomit.
Referensi
[sunting | sunting sumber]- V.A.Maltsev, C.A.Self. Cupp-Coutunn cave system, Turkmenistan, USSR // Proceedings of Bristol University speleological society, 1992, vol.19, pp. 117–150.
- Self, Charles A.; Hill, Carol A. (2003). "How speleothems grow: An introduction to the ontogeny of cave minerals" (PDF). Journal of Cave and Karst Studies. 65 (2): 130–151. ISSN 1090-6924. Diakses tanggal 2010-06-30.
- Viktor A. Slyotov. Concerning the ontogeny of crystallictite and helictite aggregates of calcite and aragonite from the karst caves of Southern Fergana. Cave Geology, vol. 2, Number 4, March 1999, pp. 197–207, Petersburg, PA
Pranala luar
[sunting | sunting sumber]![](http://upload.wikimedia.org/wikipedia/commons/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png)
Wikimedia Commons memiliki media mengenai Speleothems.
- The Virtual Cave: an online guide to speleothems
- Mineral aggregates from carst caves, formed in capillary film solutions
- Gallery of speleothems Diarsipkan 2013-01-23 di Wayback Machine. from NPS Cave and Karst Program