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Malak Polezhan
Malak Polezhan ( bg, Малък Полежан , meaning ''Little Polezhan'') is a peak in the northern section of the Pirin mountain range, south-western Bulgaria. Its height is 2,822 m which places it among the top ten summits of Pirin. The peak is built up of granite. Malak Polezhan is situated on the Polezhan side-ward ridge of the range between the peaks of Polezhan (2,851 m) to the north-east and Dzhengal (2,730 m) to the south. It is linked with Polezhan via a short and shallow saddle. To the east adjacent to the saddle is situated the Upper Polezhan Lake (2,706 m), the highest glacial lake in Pirin and the second one in Bulgaria, although some authors consider its altitude being 2,710 m which would make it the highest in Bulgaria. South of Malak Polezhan in direction of Dzhengal there are several lowers elevations with distinct shape known and the ''Obidim Ears''. The eastern slopes of Malak Polezhan are very steep, at places vertical, grassy, an ...
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Blagoevgrad Province
Blagoevgrad Province ( bg, област Благоевград, ''oblast Blagoevgrad'' or Благоевградска област, ''Blagoevgradska oblast''), also known as Pirin Macedonia or Bulgarian Macedonia ( bg, Пиринска Македония; Българска Македония), (''Pirinska Makedoniya or Bulgarska Makedoniya'') is a province (''oblast'') of southwestern Bulgaria. It borders four other Bulgarian provinces to the north and east, the Greek region of Macedonia to the south, and North Macedonia to the west. The province has 14 municipalities with 12 towns. Its principal city is Blagoevgrad, while other significant towns include Bansko, Gotse Delchev, Melnik, Petrich, Razlog, Sandanski, and Simitli. Geography and climate Geography The province has a territory of and a population of 323,552 (). It is the third largest in Bulgaria after Burgas and Sofia Provinces and comprises 5.8% of the country's territory. Blagoevgrad Province includes the mou ...
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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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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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Polezhan
Polezhan ( bg, Полежан , known pre-1942 as Mangar Tepe ( ) is a 2,851 m cone shaped high peak in the Pirin mountain range, south-western Bulgaria. It is the highest granite summit in Pirin and the fourth highest in the mountain range after the marble peaks Vihren (2,914 m), Kutelo (2,908 m) and Banski Suhodol (2,884 m). It is situated on the Polezhan side ridge which also includes the summits of Malak Polezhan (2,822 m), Gazey (2,761 m), Bezbog (2,645 m), Kaymakchal (2,763 m) and Disilitsa (2,700 m), as well as the imposing edge of Strazhite. The closest mountain refuge is Bezbog named after homonymous peak which lies near Polezhan. Depending on weather conditions the mountain refuge is about 2-3h from Polezhan. Two of the highest lakes in Pirin are situated in the vicinity of Polezhan, namely the Upper Polezhan Lake at 2,706 m, the second highest lake in Bulgaria, as well as the Upper Gazey Lake at 2,642 m. ...
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Dzhengal
Dzhengal () is a peak on the Bulgarian Pirin mountain range. It is situated in one of the external ridges of the mountain, the Polejan Ridge, between the Dzhengal Gate and Momin Dvor Peak and towers to the west of the Popovo Lake. It is 2,730 m high, which places it in the top 10 peaks in the range. Dzhengal is a granite peak that can be climbed from three points. The easiest track starts from the Samodivski Lakes and ascends towards Momin Dvor. The other ways are more difficult and require fine preparation and experience. Name According to the most popular version, the name derives from the Turkish word ''dzhangal'' which means sheep without lamb. When the herds were sheared, those sheep were marked with pendants. If the peak is viewed from the Bezbog refuge it looks like there is a pendant attached to it. Another legend says that the peak is named after the son of God Perun, Dzhengal. When the evil god Bes (Bez) decided to kidnap Perun's daughter while she was playing around ...
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Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ...
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Flagstone
Flagstone (flag) is a generic flat stone, sometimes cut in regular rectangular or square shape and usually used for paving slabs or walkways, patios, flooring, fences and roofing. It may be used for memorials, headstones, facades and other construction. The name derives from Middle English ''flagge'' meaning turf, perhaps from Old Norse ''flaga'' meaning slab or chip. Flagstone is a sedimentary rock that is split into layers along bedding planes. Flagstone is usually a form of a sandstone composed of feldspar and quartz and is arenaceous in grain size (0.16 mm – 2 mm in diameter). The material that binds flagstone is usually composed of silica, calcite, or iron oxide. The rock color usually comes from these cementing materials. Typical flagstone colors are red, blue, and buff, though exotic colors exist. Flagstone is quarried in places with bedded sedimentary rocks with fissile bedding planes. Around the thirteenth century, the ceilings, walls and floors in Eur ...
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Gazey
Gazey () is a peak in the Pirin mountain, Bulgaria situated on a small sideward ridge of the Polejansli Ridge. It is 2,761 m high, which makes it ninth in the mountain. Viewed from Polejan it looks small, rising slightly above the Upper Polejan lake but its western slopes are dizzy as they descent towards the valley of Damyanitsa. The peak looks majestic from the valley, it can be clearly seen even from the Razlog Valley. Below the larger peak tower a lower one which also looks imposing. The ridge of the same name forms a cirque in which the two Gazey lakes, some of the highest in the Balkans are located as well as the Gazey river. Gazey Nunatak in Antarctica is named after the peak. References

{{Reflist Mountains of Pirin Landforms of Blagoevgrad Province Two-thousanders of Bulgaria ...
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Sofia
Sofia ( ; bg, София, Sofiya, ) is the capital and largest city of Bulgaria. It is situated in the Sofia Valley at the foot of the Vitosha mountain in the western parts of the country. The city is built west of the Iskar river, and has many mineral springs, such as the Sofia Central Mineral Baths. It has a humid continental climate. Being in the centre of the Balkans, it is midway between the Black Sea and the Adriatic Sea, and closest to the Aegean Sea. Known as Serdica in Antiquity and Sredets in the Middle Ages, Sofia has been an area of human habitation since at least 7000 BC. The recorded history of the city begins with the attestation of the conquest of Serdica by the Roman Republic in 29 BC from the Celtic tribe Serdi. During the decline of the Roman Empire, the city was raided by Huns, Visigoths, Avars and Slavs. In 809, Serdica was incorporated into the Bulgarian Empire by Khan Krum and became known as Sredets. In 1018, the Byzantines ended Bulgarian rule ...
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Mountains Of Pirin
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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