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Musala Lakes ( bg, Мусаленски езера) are a group of seven glacial lakes situated in the Rila mountain range of southwestern
Bulgaria Bulgaria (; bg, България, Bǎlgariya), officially the Republic of Bulgaria,, ) is a country in Southeast Europe. It is situated on the eastern flank of the Balkans, and is bordered by Romania to the north, Serbia and North Macedo ...
at an altitude between 2,322 m and 2,709 m.


Location

Administratively, the belong to
Samokov Samokov ( bg, Самоков ) is a town in Sofia Province in the southwest of Bulgaria. It is situated in a basin between the mountains Rila and Vitosha, 55 kilometres from the capital Sofia. Due to the suitable winter sports conditions, Sam ...
Municipality of
Sofia Province Sofia Province ( bg, Софийска област, translit=Sofiyska oblast) is a province (''oblast'') of Bulgaria. The province does not include Sofia in its territories, but Sofia remains its administrative center. The province borders on t ...
. The seven Musala lakes are situated in the homonymous cirque and belong to the basin of the river Musalenska Bistritsa, a tributary of the Iskar. To the east is situated the summit of Deno (2,790 m), to the southeast is Irechek (2,852 m), to the south are
Musala Musala ( bg, Мусала ); from Arabic through Ottoman Turkish: from ''Musalla'', "near God" or "place for prayer" is the highest peak in the Rila Mountains, as well as in Bulgaria and the entire Balkan Peninsula, standing at . With a topogr ...
(2,925 m) and
Malka Musala Malka Musala ( bg, Малка Мусала, meaning ''Lesser Musala'') is a summit in the eastern part of the Rila Mountain in southwestern Bulgaria. With an altitude of 2,902 m, it is the second highest peak in Rila after Musala (2,925  ...
(2,902 m), to the west is the valley of Beli Iskar river. The lakes are formed in three interconnected cascading cirques, giving rise to the glacial valley of the Musalenska Bistritsa, which starts at Rila's highest summit Musala and reaches the winter resort of
Borovets Borovets ( bg, Боровец ), known as Chamkoria ( ) until the middle of the 20th century, is a popular Bulgarian mountain resort situated in Sofia Province, on the northern slopes of Rila, at an altitude of 1350 m. Borovets is located app ...
further downstream in norther direction, in the northern foothills of Rila. The first cirque, measuring 740 × 490 m, hosts the first lake. The second, third and fourth lakes are located on three levels in the second cascade cirque Aleko. The next three lakes are located in another cascading cirque measuring 1500 × 500 m, known as the Karakashev cirque. The connection of the last two circuses takes place between the fourth and seventh lakes.


Geology

Geologically, the Musale Lakes fall entirely within the Musala body of the Rila-Western Rhodope batholith, built up of medium- to coarse-grained
granite Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies under ...
dating from the
Bartonian The Bartonian is, in the ICS's geologic time scale, a stage or age in the middle Eocene Epoch or Series. The Bartonian Age spans the time between . It is preceded by the Lutetian and is followed by the Priabonian Age. Stratigraphic defini ...
age 40 to 35 million years old. The granite are leucocratic, light gray to gray-white, with a massive uniform-grained texture. The structure is poikilitic and hypidiomorpho-grained. The main rock-forming minerals are
plagioclase Plagioclase is a series of tectosilicate (framework silicate) minerals within the feldspar group. Rather than referring to a particular mineral with a specific chemical composition, plagioclase is a continuous solid solution series, more pro ...
,
orthoclase Orthoclase, or orthoclase feldspar ( endmember formula K Al Si3 O8), is an important tectosilicate mineral which forms igneous rock. The name is from the Ancient Greek for "straight fracture," because its two cleavage planes are at right angles ...
,
quartz Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical ...
and biotite. Amphibole is rare; the accessory minerals are
allanite Allanite (also called orthite) is a sorosilicate group of minerals within the broader epidote group that contain a significant amount of rare-earth elements. The mineral occurs mainly in metamorphosed clay-rich sediments and felsic igneous rock ...
,
zircon Zircon () is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium. Its chemical name is zirconium(IV) silicate, and its corresponding chemical formula is Zr SiO4. An empirical formula showing some of t ...
, xenotime,
monazite Monazite is a primarily reddish-brown phosphate mineral that contains rare-earth elements. Due to variability in composition, monazite is considered a group of minerals. The most common species of the group is monazite-(Ce), that is, the ceriu ...
, apatite and ore minerals.


Lakes


First lake

The first lake is the highest in the group and is also called the ''Icy Lake''. Situated in a small cirque at 365 m to the northeast of Mount Musala, the lake lies at an altitude of 2,709 m, which makes it the highest one in the Rila and on the Balkan peninsula. It has an area of 1.8 ha and a depth of 16.4 m, which makes it the third largest and deepest of the group. Its shape is oval, slightly elongated; the slopes are steep and covered with scree. The highest water temperature during the summer reaches 7.8 °C on the surface, and decreases to 5.1 °C in depth.


Second lake

The second lake, also called the ''Upper'' or ''Nameless Lake'', as it is located in the Aleko cirque at the foothills of summit Bezimenen (2,792 m), is located 133 m below the first lake, at 800 m north of Musala, at an altitude of 2,576 m. It has an area of 1.24 ha and a depth of 5.8 m. It is watered via underground passage from the Ice Lake.


Third lake

The third lake, known as ''Alekovo Lake'', is located in the middle level of Aleko cirque 32 m below the second one, at the foothills of Aleko peak, at 1,160 m north-northwest of Musala at an altitude of 2,544 m above. The lake has an area of 2.39 ha and a depth of 14 m. Water inflow and outflow are underground.


Fourth lake

The fourth lake, called ''Ferdinandovo Lake'', is located 58 m below the third one and 1,650 m north of Musala at an altitude of 2,486 m above. It is of variable area and depth and occupies the lowest level of the Aleko cirque. There is no visible inflow and outflow of water, and at the end of summer the lake significantly reduces its volume. Its surface area is 0.9 ha.


Fifth lake

The fifth lake is located 93 m below the fourth, at 1,500 m north-northeast of Musala, at an altitude of 2,393 m. It is known as ''Karakashevo Lake''. It has an area of 2.62 ha, which makes t is the largest of the group, and a depth of 6.6 m. .


Sixth lake

The sixth lake is located at 1,770 m north of Musala at an altitude of 2,391 m. It has an area of 0.26 ha and is the smallest of the group. Its depth does not exceed 0.5 m.


Seventh lake

The seventh, also known as the ''Lower Lake'', is located at 1,890 m north of Musala at an altitude of 2,389 m. It has an area of 1.34 ha and a depth of 1.6 m. The Musala refuge is situated on its northern shore.


Citations


References

* {{cite book , ref={{harvid, Geographic Dictionary of Bulgaria, 1980 , title = Географски речник на България , trans-title = Geographic Dictionary of Bulgaria , last1 = Мичев (Michev) , first1 = Николай (Nikolay) , last2 = Михайлов (Mihaylov) , first2 = Цветко (Tsvetko) , last3 = Вапцаров (Vaptsarov) , first3 = Иван (Ivan) , last4 = Кираджиев (Kiradzhiev) , first4 = Светлин (Svetlin) , chapter = , year = 1980 , language = Bulgarian , publisher = Наука и култура (Nauka i kultura) , location = София (Sofia) , isbn = * Kamenov, B., I. Peycheva, L. Klain, K. Arsova, Y. Kostitsin, E. Salnikova. 1999. Rila-West Rhodopes batholith: Petrological and geochemical constraints for its composite character. – Geochem., Mineral., Petrol., 36, 3 – 27. * Kuhlemann, J., E. Gachev, A. Gikov, S. Nedkov, I. Krumrei, P. Kubik. 2013b. Glaciation in the Rila Mountains (Bulgaria) during the last glacial maximum. – Quaternary International, 293, 51 – 62. Tourist attractions in Sofia Province Landforms of Sofia Province Samokov Municipality Lakes of the Rila Lake groups of Bulgaria