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Banderishki Lakes
The Banderishki Lakes are a large group of lakes in the Pirin mountains in southwestern Bulgaria. They are situated in the Banderitsa valley and mark the beginning of the Banderitsa river. There are 17 lakes in all but only 5 have names. They are glacial lakes formed on granite basis with a total area of 126,7 decares. The temperature of the water in July is 10 to 12° С. *The Frog lake ( bg, Жабешко езеро) is the highest in the group, nestling on the southern slope of the Malka Todorka peak at an altitude of 2,322 m. Its surface is only 5,6 decares and is 2 m deep. The lake is elongated (138x63 m), the water is warm. *The Long lake (Bulgarian: Дългото езеро) is situated at 2,310 m and is called the Upper Banderishko lake. It is 450 m long and 150 m wide and has a surface area of 45,5 decares. The maximum depth is 10 m and the volume of water is 177,000 m³. *The Fish Banderishko lake (Bulgarian: Рибно Бъндеришко езеро) is located at ...
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Pirin
, photo=Pirin-mountains-Bansko.jpg , photo_caption=Pirin scenery in winter , country= Bulgaria, , parent= , geology= granite, gneiss, marble, limestone , area_km2=2585 , range_coordinates = , length_km=80 , length_orientation= north-south , width_km=40 , width_orientation= north-south , highest= Vihren , elevation_m=2915 , coordinates = , map_image=Bulgaria Pirin mountain geographic map bg.svg The Pirin Mountains ( bg, Пирин ) are a mountain range in southwestern Bulgaria, with Vihren at an altitude of 2,914 m being the highest peak. The range extends about 80 km from the north-west to the south-east and is about 40 km wide, spanning a territory of . To the north Pirin is separated from Bulgaria's highest mountain range, the Rila Mountain, by the Predel saddle, while to the south it reaches the Slavyanka Mountain. To the west is located the valley of the river Struma and to the east the valley of the river Mesta separates it from the Rh ...
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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 Macedonia to the west, Greece and Turkey to the south, and the Black Sea to the east. Bulgaria covers a territory of , and is the sixteenth-largest country in Europe. Sofia is the nation's capital and largest city; other major cities are Plovdiv, Varna and Burgas. One of the earliest societies in the lands of modern-day Bulgaria was the Neolithic Karanovo culture, which dates back to 6,500 BC. In the 6th to 3rd century BC the region was a battleground for ancient Thracians, Persians, Celts and Macedonians; stability came when the Roman Empire conquered the region in AD 45. After the Roman state splintered, tribal invasions in the region resumed. Around the 6th century, these territories were settled by the early Slavs. The Bulgars, led by Asp ...
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Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ...
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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 underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Malka Todorka
Malka or Malkah may refer to: Places * Malka (river), a river in Kabardino-Balkaria in Russia * Malka Balo, one of the districts in the Oromia Region of Ethiopia * Malka Hans, Punjab, a town in Pakistan * Malka Jara, a settlement in Kenya's Coast Province * Malka, Kamchatka Krai, a village on the Kamchatka Peninsula in Rusie * Malka Mari, a settlement in Kenya's Eastern Province * Malka, Pakistan, a town of Gujrat District in the Punjab province of Pakistan * Malka Polyana, a village in the municipality of Aytos in Burgas Province, Bulgaria * Malka Smolnitsa, a village in the municipality of Dobrichka in Dobrich Province, Bulgaria People Surname * Judah ben Nissim al-Malkah, a Moroccan-Jewish writer and philosopher of the 13th century * Marie Ortal Malka, Israeli musician * Moti Malka, an Israeli footballer * Motti Malka, mayor of the Israeli city of Kiryat * Napki Malka, a Hephthalite king of the 6th-7th century * Zadok Malka, a former Israeli footballer Given name * MAL ...
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Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ...
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Todorka
Todorka ( bg, Тодорка ) is a massive peak in the Pirin Mountains of south-western Bulgaria. It is the only peak of the Todorka side ridge and has a summit elevation of 2746 m (9009 ft.) above sea level. Todorka is the 11th highest peak in Pirin and is made of granite, and although not rocky, it is steep. It is a relatively short crest with three peaks - Golyama (Big), Sredna (Middle) and Malka (Little) Todorka. Golyama Todorka is located to the north and viewed from the town of Bansko looks like a dramatic pyramid. There are several ski tracks from its slopes, and has been developed extensively since 2000 and is now a major ski area, with a lift-served summit of 2600 m (8530 ft). Bansko hosted World Cup races for the women in 2009 and for the men in 2011.Bansko World Cup.com
- - accessed 2010-02-26 Following ...
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