Karakul, Qarokul (Kyrgyz for "black lake", replacing the older Tajik name Siob; Russian: Каракуль; Tajik: Қарокӯл) is a 25km (16mi) diameter lake[2] within a rather large 52km (32mi) impact crater.[3] It is located in the Tajik National Park in the Pamir Mountains in Tajikistan.
Karakul lies within a circular depression interpreted as an impact crater with a rim diameter of 52km (32mi).[3] Some estimates give its age as relatively recent. Preliminarily, it was thought to be c. 25Ma[2] or less than 23Ma.[4] However, it may even be from the recent Pliocene (5.3 to 2.6 Ma).[5] The Earth Impact Database (EID) also lists it as younger than 5Ma.[3] It is larger than the Eltanin impact (2.5 Ma), which has already been suggested as a contributor to the cooling and ice cap formation in the Northern Hemisphere during the late Pliocene.[6]
The Karakul impact structure was first identified around 1987 through studies of imagery taken from space.[5][7]
Lake description
The lake/crater lies at an elevation of 3,960m (12,990ft) above mean sea level. A peninsula projecting from the south shore and an island off the north shore divide the lake into two basins: a smaller, relatively shallow eastern one, between 13 to 19m (43 to 62ft) deep, and a larger western one, 221 to 230m (725 to 755ft) deep. It is endorheic (lacking a drainage outlet) and the water is brackish. There is a small village with the same name on the eastern shore of the lake.[8]
The lake level was 35 m higher after the last ice age.[9][10]
Environment
Although the lake lies within a national park, much of the surroundings are used as pasture. The lake, with its islands, marshes, wet meadows, peat bogs, and pebbly and sandy plains, has been identified by BirdLife International as an Important Bird Area (IBA) because it supports significant numbers of the populations of various bird species, either as residents, or as breeding or passage migrants.
These species include bar-headed geese, ruddy shelducks, common mergansers, saker falcons, Himalayan vultures, lesser sand plovers, brown-headed gulls, Tibetan sandgrouse, yellow-billed choughs, Himalayan rubythroats, white-winged redstarts, white-winged snowfinches, rufous-streaked accentors, brown accentors, black-headed mountain finches and Caucasian great rosefinches. The lake's islands are the main places where waterbirds rest and nest.
Higher than Lake Titicaca, Karakul hosted the Roof of the World Regatta from 2014 to 2017.[11] This replaced the Alpine Bank Dillon Open, held on the Dillon Reservoir in Colorado, United States as the highest sailing regatta in the world.[12]
References
"Karakul Lake". Ramsar Sites Information Service. Archived from the original on 17 May 2018. Retrieved 25 April 2018.
"Kara-Kul". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2021-02-14.
Bouley, S.; Baratoux, D.; Baratoux, L.; Colas, F.; Dauvergne, J.; Losiak, A.; Vaubaillon, J.; Bourdeille, C.; Jullien, A.; Ibadinov, K. Karakul: a young complex impact crater in the Pamir, Tajikistan. American Geophysical Union, Fall Meeting 2011. American Geophysical Union. Bibcode:2011AGUFM.P31A1701B. Archived from the original on 2020-07-10. Retrieved 2020-07-08.
Gurov, E. P., The Kara-Kul Lake depression in the Pamirs - A Probable Astrobleme (abstract). Eighth Soviet-American Microsymposium, pp. 37-39. 1988
"Karakul lake and mountains". Important Bird Areas factsheet. BirdLife International. 2013. Archived from the original on 2018-07-19. Retrieved 2013-04-04.
Komatsu, Tetsuya; Tsukamoto, Sumiko (2015). "Late Glacial Lake-Level Changes in the Lake Karakul Basin (a Closed Glacierized-Basin), eastern Pamirs, Tajikistan". Quaternary Research. 83 (1): 137–149. doi:10.1016/j.yqres.2014.09.001.
Aichner, Bernhard; Makhmudov, Zafar; Rajabov, Ilhomjon; Zhang, Qiong; Pausata, Francesco S. R.; Werner, Martin; Heinecke, Liv; Kuessner, Marie L.; Feakins, Sarah J.; Sachse, Dirk; Mischke, Steffen (2019). "Hydroclimate in the Pamirs Was Driven by Changes in Precipitation‐Evaporation Seasonality Since the Last Glacial Period". Geophysical Research Letters. 46 (23): 13972–13983. doi:10.1029/2019GL085202.
Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.
2019-2024 WikiSort.org - проект по пересортировке и дополнению контента Википедии