Daftar danau terdalam di dunia: Perbedaan antara revisi
Tidak ada ringkasan suntingan Tag: Suntingan perangkat seluler Suntingan peramban seluler |
Tidak ada ringkasan suntingan Tag: Suntingan perangkat seluler Suntingan peramban seluler |
||
Baris 54: | Baris 54: | ||
|- |
|- |
||
| bgcolor="FFCBCB"| 3. |
| bgcolor="FFCBCB"| 3. |
||
| ([[ |
| ([[Danau Kaspia|Kaspia]]<ref name=Caspian>The [[Caspian Sea]] is generally regarded by geographers, biologists and [[limnologist]]s as a huge inland [[salt lake]]. However, the Caspian's large size means that for some purposes it is better modeled as a sea. Geologically, the Caspian, [[Black Sea|Black]], and [[Mediterranean Sea|Mediterranean]] seas are small oceans, remnants of the ancient [[Tethys Ocean|Tethys]]. Politically, the distinction between a sea and a lake may affect how the Caspian is treated by international law.</ref>) |
||
| {{flag|Kazakhstan}}<br>{{flag|Turkmenistan}}<br>{{flag|Azerbaijan}}<br>{{flag|Rusia}}<br>{{flag|Iran}} |
| {{flag|Kazakhstan}}<br>{{flag|Turkmenistan}}<br>{{flag|Azerbaijan}}<br>{{flag|Rusia}}<br>{{flag|Iran}} |
||
| [[Cekungan endoreik]] Kaspia |
| [[Cekungan endoreik]] Kaspia |
Revisi per 29 April 2024 20.20
Berikut adalah daftar danau-danau terdalam di dunia:
Secara geologis Laut Kaspia seperti Laut Hitam dan Laut Mediterania, merupakan sisa dari Samudra Tethys purba.
Informasi warna setiap Benua | ||||||
---|---|---|---|---|---|---|
Afrika | Asia | Eropa | Amerika Utara | Oseania | Amerika Selatan | Antarktika |
Danau diberi peringkat berdasarkan kedalaman rata-rata
Kedalaman rata-rata dapat menjadi indikator yang lebih berguna daripada kedalaman maksimum untuk banyak tujuan ekologis. Sayangnya, angka kedalaman rata-rata yang akurat hanya tersedia untuk danau yang dipelajari dengan baik, karena harus dihitung dengan membagi volume danau dengan luas permukaannya.[10] Angka volume memerlukan survei batimetri.[10] Oleh karena itu, angka kedalaman rata-rata tidak tersedia untuk banyak danau di lokasi terpencil.[10] Rata-rata kedalaman danau di Bumi berkisar 41,8 meter (137,14 kaki)[10]
Daftar ini berisi semua danau yang rata-rata kedalamannya diketahui melebihi 100 meter (328 kaki).
Informasi warna Benua | ||||||
---|---|---|---|---|---|---|
Afrika | Asia | Eropa | Amerika Utara | Oseania | Amerika Selatan | Antarktika |
Lihat pula
Pranala luar
- ^ a b Lake Baikal is also the largest freshwater lake by volume.
- ^ a b The Caspian Sea is generally regarded by geographers, biologists and limnologists as a huge inland salt lake. However, the Caspian's large size means that for some purposes it is better modeled as a sea. Geologically, the Caspian, Black, and Mediterranean seas are small oceans, remnants of the ancient Tethys. Politically, the distinction between a sea and a lake may affect how the Caspian is treated by international law.
- ^ a b Lake Vostok in Antarctica is a subglacial lake with a depth ranging from 400 to more than 900 meters.
- ^ *Identifican el lago más profundo de América: está en la Patagonia argentina
- ^ *CECS, Depth sounding of Lake O'Higgins/San Martín[pranala nonaktif permanen]
- ^ a b Crater Lake in Oregon has a maximum depth of 594m, based on its USGS benchmark surface elevation of 1883m. The US National Park Service publishes different values (1881m for surface elevation, and 592m for the maximum depth). The technical basis of the values determined by the USGS is documented in Bacon, C. R.; Gardner, J. V.; Mayer, L. A.; Buktenica, M. W.; Dartnell, P.; Ramsey, D. W.; Robinson, J. E. (2002). "Morphology, volcanism, and mass wasting in Crater Lake, Oregon". GSA Bulletin. 114 (6): 675–692. Bibcode:2002GSAB..114..675B. doi:10.1130/0016-7606(2002)114<0675:MVAMWI>2.0.CO;2. ISSN 0016-7606. OCLC 4642976847. Diakses tanggal 2013-07-08. (perlu berlangganan)
- ^ a b c d Murdie, Ruth E.; Pugh, David T.; Styles, Peter; Muñoz, Miguel (1999), "Heatflow, Temperature and Bathymetry of Lago General Carrera and Lago Cochrane, Southern Chile" (PDF), Extended Extracts of the Fourth International Symposium on Andean Geodynamics, Gottingen, Germany 04-06/10/1999, Paris: Institut de Recherche pour le Développement, hlm. 539–542
- ^ a b c d e f g h i j k l m n o p q r s t u v Walter K. Dodds; Matt R. Whiles (23 September 2010). Freshwater Ecology: Concepts and Environmental Applications of Limnology. Academic Press. hlm. 141–142. ISBN 978-0-12-374724-2. Diakses tanggal 22 February 2012.
- ^ Degens, E.T.; Wong, H.K.; Kempe, S.; Kurtman, F. (June 1984), "A geological study of Lake Van, eastern Turkey", International Journal of Earth Sciences, Springer, 73 (2): 701–734, Bibcode:1984GeoRu..73..701D, doi:10.1007/BF01824978
- ^ a b c d Cael, B. B.; Heathcote, A. J.; Seekell, D. A. (2017). "The volume and mean depth of Earth's lakes". Geophysical Research Letters (dalam bahasa Inggris). 44 (1): 209–218. doi:10.1002/2016GL071378. hdl:1912/8822 . ISSN 1944-8007. Diarsipkan dari versi asli tanggal 2021-08-24. Diakses tanggal 2021-09-11.
- ^ Dow, Christine; McCormack, Felicity; Cook, Sue (July 17, 2016). "What Lies Beneath Antarctica's Ice? Lakes, Life and the Grandest of Canyons". The Conversation. Diakses tanggal June 25, 2018.
- ^ Buzzi (1997), Documento dell'Istitutoitaliano di idrobiologia
- ^ Maciolek, J. A. (April 30, 1982), Lakes and Lake-like Waters of the Hawaiian Archipelago (PDF), Occasional Papers of Berenice P. Bishop Museum, 25 (1)[pranala nonaktif permanen]
- ^ Coombs, C. R.; Hawke, B. R.; Wilson, L. (1990), "Terrestrial analogs to lunar sinuous rilles - Kauhako Crater and channel, Kalaupapa, Molokai, and other Hawaiian lava conduit systems", Lunar and Planetary Science Conference Proceedings, 20: 195, Bibcode:1990LPSC...20..195C