Danu Baikal
Danu Baikal | |
---|---|
Genah | Sibéria, Rusia |
Koordinat | 53°30′N 108°0′E / 53.500°N 108.000°E |
Tipe danu | Danu kuna, Danu celahan banua |
Primary inflows | Selenga, Barguzin, Upper Angara |
Loloan utama | Angara |
Wewengkon tangkapan toya | 560000 km2 |
Basin saking negara | Mongolia miwah Rusia |
Lantang maks. | 636 km |
Linggah maks. | 79 km |
Jimbar pamukaan | 31722 km2[1] |
Rerata dalem | 744.4 m (2,442 ft)[1] |
Dalem maks. | 1642 m[1] |
Luang toya | 23615.39 km3[1] |
Galah meneng | 330 warsa[2] |
Lantang pasih1 | 2100 km |
Élevasi pamukaan | 455.5 m |
Beku | Januari–Méi |
Nusa | 27 (Nusa Olkhon) |
Paumahan | Severobaykalsk, Slyudyanka, Baykalsk, Ust-Barguzin |
Kritéria | Natural: vii, viii, ix, x |
Pustaka | 754 |
Prasasti | 1996 (sési ka-20) |
Jimbar | 8,800,000 ha |
1 Lantang pasisi punika nénten ukuran sané kapastika becik. |
Danu Baikal (aksara Bali:danubaikal·; Baikal Lake /baɪˈkɑːl,
Danu Baikal silih tunggil danu toya tawar pinih ageng mawit volume ipun ring guminé, madaging 22 nganti 23% toya pamukaan gumi.[5][6] antuk 23615.39 km3 toya,[1] madaging luwih langkung toya saking sinamian gabungan Danu Ageng ring Amérika Kalér.[7] Antuk jero maksimal ipun 1642 m,[1] Baikal punika danu pinih jero ring guminé.[8] Punika pinih ngenah[9] miwah danu pinih kuna ring guminé,[10] ring 25–30 yuta warsa.[11][12] Rumasuk danu pinih ageng kepitu ring guminé mawit jimbar pamukaan.
- ↑ 1,0 1,1 1,2 1,3 1,4 1,5 "A new bathymetric map of Lake Baikal. Morphometric Data. INTAS Project 99-1669. Ghent University, Ghent, Belgium; Consolidated Research Group on Marine Geosciences (CRG-MG), University of Barcelona, Spain; Limnological Institute of the Siberian Division of the Russian Academy of Sciences, Irkutsk, Russian Federation; State Science Research Navigation-Hydrographic Institute of the Ministry of Defense, St. Petersburg, Russian Federation". Ghent University, Ghent, Belgium. Kaarsipin saking versi asli tanggal 25 December 2018. Kaaksés 9 July 2009.
- ↑ M.A. Grachev. "On the present state of the ecological system of lake Baikal". Limnological Institute, Siberian Division of the Russian Academy of Sciences. Kaarsipin saking versi asli tanggal 20 Agustus 2011. Kaaksés 9 Juli 2009.
- ↑ "Baikal". Collins English Dictionary.
- ↑ Dervla Murphy (2007) Silverland: A Winter Journey Beyond the Urals, London, John Murray, p. 173
- ↑ Schwarzenbach, Rene P.; Philip M. Gschwend; Dieter M. Imboden (2003). Environmental Organic Chemistry (édisi ka-2). Wiley Interscience. p. 1052. ISBN 9780471350538.
- ↑ Tyus, Harold M. (2012). Ecology and Conservation of Fishes. CRC Press. p. 116. ISBN 978-1-4398-9759-1.CS1 maint: uses authors parameter (link)
- ↑ Bright, Michael, ed. (2010). 1001 natural wonders : you must see before you die. preface by Koichiro Mastsuura (édisi ka-2009). London: Cassell Illustrated. p. 620. ISBN 9781844036745.
- ↑ "Deepest Lake in the World". geology.com. Kaaksés 18 August 2007.
- ↑ Jung, J., Hojnowski, C., Jenkins, H., Ortiz, A., Brinkley, C., Cadish, L., Evans, A., Kissinger, P., Ordal, L., Osipova, S., Smith, A., Vredeveld, B., Hodge, T., Kohler, S., Rodenhouse, N. and Moore, M. (2004). "Diel vertical migration of zooplankton in Lake Baikal and its relationship to body size" (PDF). Ring Smirnov, A.I.; Izmest'eva, L.R. (eds.). Ecosystems and Natural Resources of Mountain Regions. Proceedings of the first international symposium on Lake Baikal: The current state of the surface and underground hydrosphere in mountainous areas. "Nauka", Novosibirsk, Russia. pp. 131–140. Kaarsipin saking versi asli (PDF) tanggal 15 June 2011. Kaaksés 9 August 2009.CS1 maint: uses authors parameter (link)
- ↑ "Lake Baikal – A Touchstone for Global Change and Rift Studies". United States Geological Survey. Kaarsipin saking versi asli tanggal 29 June 2012. Kaaksés 3 January 2016.
- ↑ "Lake Baikal – UNESCO World Heritage Centre". Kaaksés 5 October 2012.
- ↑ "Lake Baikal: Protection of a unique ecosystem". ScienceDaily. 26 July 2017. Kaaksés 16 January 2018.