Karakul (Tajikistan)

Karakul or Qarokul (Kyrgyz for "black lake", replacing the older Tajik name Siob; Template:Langx; Template:Langx; Template:Langx, Template:Lang; Template:Langx) is an endorheic lake, Template:Cvt in diameter, located within a Template:Cvt impact crater.<ref name=nasa>Template:Cite web</ref><ref name=karakul>Template:Cite Earth Impact DB</ref> It is located in the Tajik National Park in the Pamir Mountains in Tajikistan.

Impact crater

Karakul lies within a circular depression, which has been interpreted as an impact crater with a rim diameter of Template:Cvt.<ref name=karakul/> Some estimates say the impact is relatively recent. A preliminary estimate dated it to between 25 Ma<ref name=nasa/> and 23 Ma.<ref>Template:Cite conference</ref> However, it may be from the recent Pliocene epoch (5.3 to 2.6 Ma).<ref name=gurov>Template:Cite journal</ref> The Earth Impact Database (EID) also lists it as younger than 5 Ma.<ref name=karakul/> 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.<ref name="pomti">Template:Cite web</ref>

The Karakul impact structure was first identified around 1987 through studies of imagery taken from space.<ref name =gurov/><ref>Gurov, E. P., The Kara-Kul Lake depression in the Pamirs - A Probable Astrobleme (abstract). Eighth Soviet-American Microsymposium, pp. 37-39. 1988</ref>

Lake description

File:Karakul lake Tajikistan.jpg

As seen from the Pamir Highway

The lake/crater lies at an elevation of Template:Cvt 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 Template:Cvt deep, and a larger western one, Template:Cvt deep.<ref>{{#if: |

   |{{#ifeq: Kara-Kul |
                |{{#ifeq: |
                             |
                             |
                           }}
                |
               }}
  }}{{#ifeq:  |
   |{{#ifeq: y |
                                    |This article
                                    |One or more of the preceding sentences
                                   }} incorporates text from a publication now in the public domain: 
  }}{{#invoke:template wrapper|{{#if:|list|wrap}}|_template=cite EB1911
   |_exclude=footnote, inline, noicon, no-icon, noprescript, no-prescript, _debug

   | noicon=1
  }}{{#ifeq:  ||}}</ref> 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.<ref name="bli">Template:Cite web</ref>

The lake level was 35 m higher after the last ice age.<ref>Template:Cite journal</ref><ref>Template:Cite journal</ref>

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.

The only fish in the lake are Triplophysa lacusnigri.<ref>Template:Citation</ref>

Events

Higher than Lake Titicaca, Karakul hosted the Roof of the World Regatta from 2014 to 2017.<ref>Template:Cite web</ref> This replaced the Alpine Bank Dillon Open, held on the Dillon Reservoir in Colorado, United States as the highest sailing regatta in the world.<ref>Template:Cite web</ref>