The Pirin Mountain (Bulgarian: Пирин) is a mountain range in southwestern Bulgaria, with Vihren at an altitude of 2,914 m being the highest peak. One hypothesis is the mountain was named after Perun, the highest god of the Slavic pantheon and the god of thunder and lightning. Another version is that the etymology of the range derives from the Thracian word Perinthos, meaning "Rocky Mountain".
The range extends about 80 km from the north-west to the south-east and is about 40 km wide, spanning a territory of 2,585 km2 (998 sq mi). 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 Rhodope Mountains. Pirin is dotted with more than a hundred glacial lakes and is also the home of Europe's southernmost glaciers, Snezhnika and Banski Suhodol.
The northern part of the range, which is also the highest one, is protected by the Pirin National Park, declared a UNESCO World Heritage Site in 1983. Pirin is noted for its rich flora and fauna, as well as for the presence of a number of relict species. Much of the area is forested, with some of the best preserved conifer woods in Bulgaria, holding important populations of the Balkan endemic species Macedonian pine, Bosnian pine and Bulgarian fir. Animals include many species of high conservation value, such as brown bear, gray wolf, wildcat, European pine marten, wild boar, red deer, roe deer, chamois, etc.
The combination of favourable natural conditions and varied historical heritage contribute makes Pirin an important tourist destination. The town of Bansko, situated on the north-eastern slopes of the mountain, has grown to be the primary ski and winter sports centre in the Balkans. A number of settlements at the foothills of Pirin have mineral spring and are spa resorts — Banya, Dobrinishte, Gotse Delchev, Sandanski, etc. Melnik at the south-western foothills of the mountain is Bulgaria's smallest town and is an architectural reserve. Within a few kilometres from the town are the Melnik Earth Pyramids and the Rozhen Monastery.
Pirin scenery in winter
|Elevation||2,915 m (9,564 ft)|
|Length||80 km (50 mi) north-south|
|Width||40 km (25 mi) north-south|
|Area||2,585 km2 (998 sq mi)|
|Type of rock||granite, gneiss, marble, limestone|
Pirin is situated in south-western Bulgaria and is part of the Rila–Rhodope Massif. To the north the Predel Saddle and mountain pass at 1140 m altitude separates it from the Rila mountain range. To the east Pirin borders the Razlog Valley, the valley of the river Mesta and the Momina Klisura Gorge that separate it from the Rhodope Mountains. To the south the Paril Saddle (1170 m) divides it from the Slavyanka mountain range. To the west Pirin reaches the valley of the river Struma, including the Kresna Gorge and the Sandanski-Petrich Valley, that serve as a divide from the mountains Vlahina, Maleshevo and Ograzhden further to the west.
The main orographic ridge extends from the north-west to the south-east. Pirin spans an area of 2,585 km2 with an average height of 1,033 m. The maximum length between the Paril and Predel saddles is 80 km; the maximum width is 40 km. Reaching an altitude of 2,914 m Pirin is the second highest mountain range in Bulgaria after Rila (2,925 m) and the eighth highest in Europe after the Caucasus, the Alps, Sierra Nevada, the Pyrenees, Mount Etna, the aforementioned Rila, and Mount Olympus.
Geologically and morphologically Pirin is divided into three parts: north, central and south, which differ sharply in size and altitude. North Pirin is the largest of the subdivisions and the mountain's downright part. It takes up 74% of the whole range's territory, being about 42 km long and ranging from Predel to the north to the Todorova Polyana Saddle (1,883 m) to the south. It is the most often visited part of the mountain, the only one to have an Alpine appearance, featuring many glacial lakes, resthouses and shelters. North Pirin is itself divided into two zones by the Kabata Saddle and the valleys of the Banderitsa and Vlahinska rivers. The northern zone consists of the steep marble Vihren ridge with the three highest summits in the range: Vihren (2914 m), Kutelo (2908 m) and Banski Suhodol (2884 m). The marble ridge is narrow and very steep, reaching a width of only 0.5 m at the ridge Koncheto (2810 m). The southern zone is more massive and consists primarily of granite ridges, including Pirin's fourth highest summit Polezhan, at 2851 m. The southern zone also has marble ridges, such as the Sinanitsa ridge with its homonymous summit (2516 m). In total the northern section of Pirin includes two summits with an altitude over 2900 m, seven over 2800 m, 13 over 2700 m and 60 over 2500 m.
Central Pirin extends between the Todorova Polyana Saddle and the Popovi Livadi Saddle. It constitutes the smallest and the shortest of the three subdivisions, covering only 7% of Pirin's total area. It is composed of crystalline schists and granite, as well as of marbled limestone in the south. Because of the karstic relief there are no lakes; the rivers springing up from Central Pirin are short and with low water volume. It is largely covered by deciduous forests. The highest peak is Orelyak (2,099 m), while the other summits are under 2,000 m.
South Pirin stretches from the Popovi Livadi Saddle to the Paril Saddle and is the lowest and least rugged part. The highest peak is Ushite at 1,978 m, although Svesthnik (1,975 m) had long been considered the highest summit. It constitutes 19% of the mountain's territory. Despite being characterised with relatively flat ridges, its lateral slopes are steep. South Pirin is composed of granite with marbled limestone in the periphery. It lacks glacial forms and is covered with forests. Like Central Pirin the springs are short and with low water discharge.
Geologically Pirin is a horst forming a massive anticline situated between the complex graben valleys of the Struma and the Mesta, formed by metamorphic rocks — gneiss, biotite and crystalline schists, amphibolite, quartzite and marble. Granite rocks cover 62% of the mointain's area. The tectonics of the Pirin is primarily the result of Precambrian, Hercynian, alpine and tectonic movements and events. Its hoisting alternated with long dormant periods. As a result of the activisation of the ancient Struma and Mesta faults during the Neogene and the Quaternary Pirin rose as a massive horst.
The modern relief of Pirin was shaped in the Pleistocene when the mountain was subjected to alpine glaciation related to the global cooling. This glaciation occurred in parallel with that of the Alps. The process formed pointed pyramidal peaks, long U-shaped valley, cirques, moraine fields and vertical cliffs that characterise Pirin's contemporary appearance. These forms are most prominent at the north-eastern ridges of the mountain. Some lateral moraines may reach heights of more than 1100 m. The lower line of the glaciers was at 2200–2300 m. Karst landforms also shape Pirin's relief with ponors, swallow holes, caves, etc.
The main Pirin ridge is clearly distinguished; it begins in Rila and passes through the Predel saddle as far as the Paril saddle. It links the separate smaller ridges of the mountain into one system with the highest peaks situated on it. Although it curves a lot, its main direction is from the northwest to southeast and it is also a watershed between the Struma and the Mesta rivers. There are many spurs but four of them are so large that they create the appearance of the mountain: Sinanishko, Todorino, Polezhansko and Kamenishko.
There are two peaks above 2,900 m, Vihren and Kutelo; seven above 2,800 m; 13 above 2,700 m; 32 above 2,600 m and 60 above 2,500 m. The highest granite peak is the Banderishki Chukar (2,732 m). Some of the highest peaks are:
The most recognisable rock formation in the mountain range are the Melnik Earth Pyramids situated in the southwestern reaches of Pirin in the vicinity of the homonymous town. They are located at an altitude between 350 and 850 m and are composed of sandstone and conglomerates dated from the Neogene and the Quaternary Periods. The Pyramids were formed as a result of erosion as the Melnishka River and its tributaries had carved their way into the hills forging pyramid-like forms of significant aesthetic value that reach height of 100 m. This process began 4–5 million years ago and is still ongoing. The combination of pale Pliocene sandstones and red Quaternary conglomerates determines the yellowish and reddish colour gamut and the diverse shapes. The Melnik Earth Pyramids constitute a specific and unique micro habitat of high conservation value and were designated a natural landmark in 1960.
Similar rock formations are found further north along the slopes of Pirin facing the Struma Valley near the town of Kresna.
Pirin is situated within the continental Mediterranean climate zone and due to its altitude the higher sectors have Alpine climate. The climate is influenced by Mediterranean cyclones mainly in late autumn and in winter, bringing frequent and high rainfall, and by the Azores anticyclone in summer, making the summer months hot and dry. The relief has a crucial influence on the climate. Pirin has three altitude climate zones — low between 600 and 1000 m, middle between 1000 and 1800 m and high above 1800 m. The low altitude zone is heavily influenced by the Mediterranean climate, the influence being more pronounced on the western slopes facing the Struma valley than on the eastern slopes along the Mesta valley. The high altitude zone is characterised by low temperature, low temperature amplitude, many cloudy days, lasting and thick snow cover, strong winds and intensive sun radiation.
Winters are cold and prolonged while summers are cool and short. The temperature decreases with the altitude, which is more visible in summer. The mean annual temperature is around 9–10 °C in the low, 5–7 °C in the middle and 2–3 °C in the high altitude zone. The coldest month is January with average temperature varying between −5 and −2 °C. The hottest month is July with temperature averaging 20 °C at 1600 m and 15 °C at 2000 m. Temperature inversions, i.e. increase in temperature with height, are observed in 75% of the winter days.
The annual precipitation in Pirin is 600–700 mm in the lower zones and 1000–1200 mm in the higher. The rainfall occurs mostly in winter and spring, while summer is driest season. The air humidity is 60–75% in August and 80–85 % in December. In winter the precipitation is mainly snow, varying from 70–90% at the lower altitudes to 100% at higher. The average number of days with snow cover varies from 20–30 to 120–160. The highest thickness of the snow cover reaches 40–60 cm at 1000–1800 m in February and 160–180 cm above 1800 m in March (190 cm on Vihren). In some winters the snow thickness can reach 250–350 cm. Avalanches are frequent.
The prevailing wind direction is from the west and the north-west but southern and south-western winds are also frequent. The wind speed can reach 34–40 m/s at the high ridges, being highest in February and March and lowest in August and September. The percentage of windless days increases in summer and autumn to 30–40% at lower altitude and 10–15% at higher. In the highest zone the percentage does not exceed 5–7% annually.
Pirin forms the water divide between the basins of the rivers Struma and Mesta. The watershed follows the main ridge of the mountain in direction north-west to south-east. As the main ridge is situated closer to the Mesta valley, the tributaries to the Struma tend to be longer. The rivers are short, steep and with high water volume; the river bottom is rocky or covered with large sediments. The water discharge is highest in May and June and lowest in September. The streamflow is largely derived from snow melting and glacial lakes in spring and summer and almost exclusively from groundwater in winter. The rivers and streams form numerous leaps and waterfalls but they are generally not as high as those in Rila or the Balkan Mountains. The highest one is Popinolashki waterfall, measuring some 12 m. Pirin is the source of 10 tributaries to the Struma, including Pirinska Bistritsa, Sandanska Bistritsa, Melnishka reka and Vlahina reka, as well as another 10 to the Mesta, such as Iztok, Disilitsa and Retizhe. Reaching a length of 53 km, Pirinska Bistritsa is the longest river in the massif. Pirin has abundant mineral springs, being among Bulgaria's richest areas. Based on the chemical composition they are divided into two thermal groups — in the Mesta and the Struma basins. The springs in the Mesta basin to the east are more alkaline, with lower mineralisation (below 400 mg/l) and conductance; those on the western slopes reach higher temperatures, up to 86 °C.
A total of 176 glacial lakes are situated in the mountain range, all of them in the North Pirin. Of them, 119 are permanent, and the rest dry out in summer. About 65% of them are located in the north-eastern area and discharge into the Mesta basin; the other 35% are to the south-west, their water flowing into the tributaries of the Struma. Approximately 90% of the lakes are nestled between 2100 m and 2450 m. At an altitude of 2710 m the Upper Polezhan Lake is the highest in Pirin, as well as in Bulgaria and the Balkan Peninsula. The total area of all lakes is 18 km2; the largest one being Popovo Lake with 123,600 m2, which makes it the fourth largest glacial lake in the country. With a depth of 29.5 m, it is also Pirin's deepest lake and Bulgaria's second. The water is transparent as deep as 15 m. Many of the lakes are covered with ice during most of the year. The ice thickness reaches 3 m in the highest lakes. The lakes and the lake groups are:
Pirin is also home to two small glaciers, remnants from the last Ice Age. Snezhnika is located in the deep Golemiya Kazan cirque at the steep northern foot of Vihren and is the southernmost glacier in Europe. Banski Suhodol Glacier is larger and situated a bit to the north below Koncheto Ridge.
The vegetation of Pirin is vertically divided into five distinct elevation zones: Mediterranean, deciduous, coniferous, that combined form the tree line reaching approximately altitude of 2,000 m, shrubs forming the subalpine line up to 2,500 m and alpine meadows, also known as the alpine line above 2,500 m. The Mediterranean zone is dominated, among other, by pubescent oak (Quercus pubescens) and Oriental Hornbeam (Carpinus orientalis), the deciduous zone by European oak (Quercus robur) and European beech (Fagus sylvatica), and the coniferous — by Macedonian pine (Pinus peuce), Bosnian pine (Pinus heldreichii) and Scots pine (Pinus sylvestris). The subalpine line is mainly covered with dwarf mountain pine (Pinus mugo) and common juniper (Juniperus communis). The alpine line is covered with grass, moss, lichen and abundant in bilberries and rare flowers such as the edelweiss (Leontopodium alpinum). Pirin is home to Bulgaria's oldest tree, the 1300–year Baikushev's pine — a Bosnian pine that is a contemporary of the foundation of the Bulgarian state in 681 AD.
The total number of vascular plants is 1315 species, or approximately 1/3 of Bulgaria's flora, many of them being rare and under protection. There are 18 species endemic to Pirin, including Pirin poppy (Papaver degenii), Pirin meadow-grass (Poa pirinica), Urumov oksitropis (Oxytropis urumovii) among others, as well as another 17 taxa restricted only to Bulgaria, which makes a total of 35 Bulgarian endemic species. The non-vascular plants are represented by 165 algae, 329 moss and 367 lichen species.
The vertebrate fauna of Pirin consists of 229 species. The mammal species are 45 and include brown bear, gray wolf, wildcat, European pine marten, wild boar, red deer, roe deer and chamois. The total number of bird species is 159, including three relicts — boreal owl, white-backed woodpecker and Eurasian three-toed woodpecker, and a number of birds of prey, such as lesser spotted eagle, booted eagle, golden eagle, short-toed snake eagle, saker falcon, peregrine falcon, etc. There are 11 reptile, 8 amphibian and 6 fish species. The number of invertebrate species discovered so far is 2091 but they remain poorly studied and are expected to rise to 4500.
The rich wildlife in the mountain is protected by the Pirin National Park founded in 1962 and designated a UNESCO World Heritage Site in 1983. The park spans an area of 403,32 km2 and includes two nature reserves, Bayuvi Dupki–Dzhindzhiritsa and Yulen. There are two more reserves in Pirin beyond the limits of the national park, Tisata and Orelyak.
Due to the fertile foothills and the favourable terrain for defence Pirin has been continuously inhabited since prehistoric times. Archaeological remains left by the Thracians have been discovered at the western foothills along the Struma Valley and in the Razlog Valley. As the region was annexed by the Roman Empire by the 1st century BC the number of settlements saw further expansion. During the Early Middle Ages the area around Pirin was settled by Slavic tribes along with most of the Balkans and was absorbed by the Bulgarian Empire in the 9th century. Throughout the Middle Ages Pirin remained contested between the Bulgarian and the Byzantine Empires until it was conquered by the Ottoman Turks in the late 14th century. The population of the region played an active role during the Bulgarian National Revival and the struggle for national liberation. The important 18th century Bulgarian enlightener Paisius of Hilendar and author of Istoriya Slavyanobolgarskaya was born in Bansko at the northern foothills of Pirin. Bulgaria achieved liberation in 1878 but as a result of the Congress of Berlin Pirin remained in the Ottoman Empire. In response, the local population in Pirin rebelled in the Kresna–Razlog uprising (1878–1879) and later took part in the Ilinden–Preobrazhenie Uprising (1903) but both were quelled by the Ottomans. The region was finally liberated by the Bulgarian Army in October 1912 during the course of the First Balkan War (1912–1913).
Pirin is a sparsely populated mountain range with all the settlements located at the foothills and none in the mountain itself. Administratively it falls entirely in Blagoevgrad Province. From north to south there are four towns at the western foothills facing the Struma Valley, namely Simitli (pop. 6,647 as of 2016), Kresna (3,267), Sandanski (26,023) and Melnik (170), as well as three more to the north and the east — Bansko (7,369), Dobrinishte (2,377) and Gotse Delchev (19,087). There are a number of villages, including among others Brezhani, Vlahi, Ploski, Lilyanovo, Dzhigurovo, Gorna Sushitsa, Kashina, Pirin, Belyovo, Novo Delchevo, Kremen, Breznitsa, Dobrotino, Kornitsa, Lazhnitsa, etc.
Pirin is served by two main roads — the first class I-1 road, part of European route E79, along the Struma valley to the west that links the capital Sofia and the provincial centre Blagoevgrad with Greece at Kulata, and the second class II-19 road which branches off I-1 at Simitly, goes east crossing the Predel Saddle and then turns south along the Mesta Valley to Gotse Delchev and the border with Greece at Ilinden. The Struma motorway is planned to run in parallel with the I-1 road, with one section between Novo Delchevo and the border already finished and another one linking Novo Delchevo and Kresna under construction as of 2017. Due to the rugged relief Pirin is crossed by only one road, the third class III-198 road that links I-1 and II-19 through the Paril Saddle between Central and South Pirin. The mountain range is served by the Bulgarian State Railways via railway line No. 5 along the Struma Valley in the west and the Septemvri–Dobrinishte narrow-gauge line with terminus at the latter town in the northern foothills.
The economy is based on agriculture, industry, services and tourism. There are small deposits of sub-bituminous coal as well as significant quantities of high-quality marble that is processed in Sandanski and part of the production is exported. A number of small hydro power plants have been constructed, mainly along Sandanska Bistritsa River. The rivers are also used for irrigation. Forests cover 1,996 km2 (771 sq mi), or 5.5% of Bulgaria's total, and are of commercial importance because of the high-quality timber. As logging is restricted in the protected areas the wood-processing industry in Pirin forms 3.5% of the nation's total production in that sector. The lower parts of the mountain offer favourable conditions for agriculture, the most important cash crops being grapes, peanuts, tobacco and anise. The region around Melnik is renown for its centuries-old traditions in producing distinct red wines. Manufacturing industry is centres in Sandanski, Gotse Delchev, Bansko and Simitli; the main sectors are food processing, machine building and furniture production.
The favourable natural conditions for winter sports, spa and recreation combined with the architectural heritage make Pirin a popular tourist destination. Bansko is by far the most developed winter resort in the mountain range, being also Bulgaria's most popular one for foreigners — over 79,000 foreign tourists have stayed in Bansko for the 2016/17 winter season spending an average of four nights. Bansko has 75 km ski runs equipped with artificial snow machines as well as 22 km lifting facilities and provides conditions for alpine skiing, cross-country skiing, biathlon, snowboard, etc. The top elevation is 2560 m while the lowest is 990 m. Bansko regularly hosts European alpine ski and biathlon cups. Another much smaller resort is Dobriniste with 5 km of ski tracks.
The abundant mineral springs are a prerequisite for health and spa tourism. The most developed spa resorts are Dobrinishte and Sandanski. The former has 17 springs with a total discharge of 782 l/min and temperature of 28°С to 41.2°С and has a mineral beach among the other facilities. Sandanski is home to 11 springs with a total discharge of 1200 l/min and temperature of 33°С to 83°С that have been utilised since Antiquity. Other mineral baths are located in Bansko, Banya, Vlahi, Dolna Gradeshnitsa, Levunovo, Marikostinovo, Musomishta, Oshtava, Simitli and Hotovo.
There are 20 marked hiking trails within the borders of Pirin National Park. The steep rock faces in Northern Pirin provide favourable conditions for alpine climbing. The most popular places for practising climbing are the north wall of Vihren, as well as the peaks Kamenitsa, Banski Suhodol, Sinanitsa and Dzhengal among others. Pirin Golf Club near Bansko has 18- and 5-hole golf courses.
Cultural tourism is also well developed. Melnik has been designated an architectural reserve and one of the 100 Tourist Sites of Bulgaria. Among the main sights are the ruins of the medieval fortress and the Church of St Nicholas, as well as a number of national revival style houses, such as the Kordopulov House. A few kilometres to the east of the town is Rozhen Monastery, the biggest one in Pirin. The monastery was established in the early 13th century during the Second Bulgarian Empire and has the shape of an irregular hexagon. There are frescoes dated from the 16th century. Rozhen Monastery was a regional centre for learning and calligraphy. In close proximity to the monastery is the Church of Saints Cyril and Methodius, built on the initiative of the Prominent Bulgarian revolutionary Yane Sandanski, which nowadays houses his tomb. The town of Sandanski boasts the ruins of a 5-6th century episcopal basilica that has been recently renovated. Bansko also has an old quarter with 18-19th century houses and the Church of Holy Trinity whose 30-meters high belfry is the symbol of the town.
The 1980–81 Bulgarian Cup was the 41st season of the Bulgarian Cup (in this period the tournament was named Cup of the Soviet Army). Botev Plovdiv won the competition, beating Pirin Blagoevgrad 1–0 in the final at the Vasil Levski National Stadium.1990–91 Bulgarian Cup
The 1990–91 Bulgarian Cup was the 51st season of the Bulgarian Cup. Levski Sofia won the competition, beating Botev Plovdiv 2–1 in the final at the Ivaylo Stadium in Veliko Tarnovo.1993–94 Bulgarian Cup
The 1993–94 Bulgarian Cup was the 54th season of the Bulgarian Cup. Levski Sofia won the competition, beating Pirin Blagoevgrad 1–0 in the final at the Vasil Levski National Stadium in Sofia.2008–09 Bulgarian Cup
The Bulgarian Cup 2008–09 was the 27th official Bulgarian annual football tournament. The competition started on October 15, 2008 with the Preliminary Round and ended on May 26, 2009. The defending champions were Litex Lovech, who successfully defended their title against Pirin Blagoevgrad.2012–13 Bulgarian Cup
The 2012–13 Bulgarian Cup was the 31st official season of the Bulgarian annual football knockout tournament. The competition began on 13 October 2012 with the matches of the Preliminary Round and ended with the final on 15 May 2013. Ludogorets Razgrad were the defending champions, but were eliminated by CSKA Sofia in the second round. Beroe Stara Zagora won the title, their second overall, after defeating Levski Sofia in the final by penalties.
The winners of the competition, Beroe Stara Zagora, qualified for the second qualifying round of the 2013–14 UEFA Europa League.Blagoevgrad Province
Blagoevgrad Province (Bulgarian: област Благоевград, oblast Blagoevgrad or Благоевградска област, Blagoevgradska oblast), also known as Pirin Macedonia or Bulgarian Macedonia (Bulgarian: 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.FC Pirin Gotse Delchev
Football Club Pirin (Bulgarian: Футболен клуб Пирин) is a Bulgarian football club, based in Gotse Delchev. The club currently plays in the fourth division of Bulgarian football. The team's biggest success came in 2012, when they managed to promote to the A PFG for the very first time. Their spell in the top-flight lasted two years. Pirin play home games at the Gradski stadium, with a capacity of 5,000. They play in green and white stripped kits. The club logo represents the Pirin mountain range in Southwestern Bulgaria and the predominant green color on the kits is in reference to the many forested areas around Gotse Delchev.FC Pirin Razlog
Football Club Pirin Razlog (Bulgarian: Пирин Разлог) is a Bulgarian football club based in Razlog, that competes in the South-West Third League.Maleševo-Pirin dialect
The term Maleševo-Pirin dialect (also spelt Maleshevo) is used in South Slavic linguistics to refer to a group of related varieties that are spoken on both sides of the border of Bulgaria and the Republic of North Macedonia. Some linguists treat them as dialects of the Bulgarian language, while Victor Friedman views them as part of the Macedonian language. According to some authors, they are linguistically transitional between the two national languages, Bulgarian and Macedonian and form part of the larger dialect continuum between them. The dialect group is named after the mountain ranges of Pirin in Bulgaria and Maleševo in Macedonia. When referring specifically to the dialects on the Bulgarian side, the term Petrich-Blagoevgrad dialect, after the two major towns in the area, is also used.Some Macedonian linguists tend to treat the whole group as part of the Macedonian language, classifying it as part of a southeastern group of Macedonian dialects; others, like Krume Kepeski do not classify it as part of Macedonian, whereas from the perspective of Bulgarian linguistics, the varieties in Bulgaria are classified as parts of the eastern subgroup of the southwestern group of Bulgarian.
This dialect is spoken in the towns of Delčevo, Pehčevo, Berovo and the surrounding villages in the east of the Republic of Macedonia,
and in the regions of Blagoevgrad, Petrich and Sandanski in Bulgaria.The Blagoevgrad-Petric dialect is also closely related to the neighbouring Kyustendil and Samokov dialects, and especially to the Dupnitsa dialect,
whereas the Maleshevo dialect is closely related especially with the Strumica dialect.OFC Pirin Blagoevgrad
Pirin (Bulgarian: Пирин) is a Bulgarian municipal association football club based in Blagoevgrad, which currently competes in the Second League, the second division of Bulgarian football.
The club was founded in 2008, after a merger between two clubs from Blagoevgrad, Pirin 1922 and PFC Pirin Blagoevgrad. By an official court decision later that year, the club was announced as a historical successor of the club records of the former FC Pirin, founded in 1922. In 2011, following a bankruptcy of the entity, which represented the football club, Pirin's football department was merged once again with Perun Kresna, to eventually become OFC Pirin.
Pirin Blagoevgrad's name is adopted from Pirin, a mountain range in southwestern Bulgaria. The club's home ground is the Hristo Botev Stadium in Blagoevgrad with a capacity of 7,000 spectators. Pirin's nickname is Orletata (the Baby Eagles) and their kit colours are dark green and white.
To date, the club has four domestic cup finals and most notably, enjoys high praise for its development of football players, as several noted Bulgarian footballers were produced by Pirin's youth academy. Among them are the 1994 FIFA World Cup bronze medallists Petar Mihtarski and Ivaylo Andonov, as well as former Manchester United striker Dimitar Berbatov, who won two Premier League titles and was the 2010-11 Premier League top goalscorer.PFC Bansko
Bansko (Bulgarian: Банско) is a Bulgarian professional association football club from the town of Bansko, currently playing in the South-West Third League, the third division of Bulgarian football. Its home matches take place at the Saint Petar Stadium.
The club was founded in 1951. Until the 2008–09 season, the team participated in either the amateurs Bulgarian divisions. After the union by the two clubs from Blagoevgrad – "Pirin" and "Pirin 1931", FC Bansko took licence of Pirin for participation in the West B Group.PFC Pirin Blagoevgrad
PFC Pirin Blagoevgrad was a Bulgarian professional football club based in Blagoevgrad.Perin
Perin (Persian: پرين, also Romanized as Perīn; also known as Ferīn, Parad, and Pīrīn) is a village in Poshtkuh-e Rostam Rural District, Sorna District, Rostam County, Fars Province, Iran. At the 2006 census, its population was 616, in 119 families.Pirin Glacier
Pirin Glacier (Bulgarian: ледник Пирин, ‘Lednik Pirin’ \'led-nik 'pi-rin\) is the 5.7 km long and 6 km wide glacier situated next east of Chavdar Peninsula on Davis Coast on the Antarctic Peninsula. Situated west of Wright Ice Piedmont, north of Gregory Glacier and east of Samodiva Glacier. Draining north-northwestwards from Boulton Peak to enter Curtiss Bay east of Seaplane Point.
The glacier is named after Pirin Mountain in southwestern Bulgaria.Pirin Macedonia
Pirin Macedonia or Bulgarian Macedonia (Bulgarian: Пиринска Македония; Българска Македония) (Pirinska Makedoniya or Bulgarska Makedoniya) is the smallest part of the geographical region Macedonia located on the Balkan Peninsula, today in southwestern Bulgaria. This region coincides with the borders of the Blagoevgrad Oblast, adding the surrounding area of the Barakovo village from the Kyustendil Province. After World War I, Strumica and the surrounding area were broken away from the region and were ceded to Yugoslavia.
It covers an area of about 6,798 km2 which is 10.18% of the geographical region Macedonia. One of the regional centers is Blagoevgrad. The region is bordering with Kyustendil Province and Sofia Province to the north, Pazardzhik Province and Smolyan Province to the east, Greece to the south and North Macedonia to the west. The population is estimated around 325.000 people.Pirin National Park
Pirin National Park (Bulgarian: Национален парк "Пирин"), originally named Vihren National Park, encompasses the larger part of the Pirin Mountains in southwestern Bulgaria, spanning an area of 403.56 km2 (155.82 sq mi). It is one of the three national parks in the country, the others being Rila National Park and Central Balkan National Park. The park was established in 1962 and its territory was expanded several times since then. Pirin National Park was declared a UNESCO World Heritage Site in 1983. The altitude varies from 950 m to 2,914 m at Vihren, Bulgaria's second highest summit and the Balkans' third.
The park is situated in Blagoevgrad Province, the nation's south-westernmost region, on the territory of seven municipalities: Bansko, Gotse Delchev, Kresna, Razlog, Sandanski, Simitli and Strumyani. There are no populated places within its territory. Two nature reserves are located within the boundaries of Pirin National Park, Bayuvi Dupki–Dzhindzhiritsa and Yulen. Bayuvi Dupki–Dzhindzhiritsa is among the oldest in Bulgaria, established in 1934 and is included in the World Network of Biosphere Reserves under the UNESCO Man and Biosphere Programme. The whole territory is part of the network of nature protection areas of the European Union, Natura 2000.
Pirin is renowned for its 118 glacial lakes, the largest and the deepest of them being Popovo Lake. Many of them are situated in cirques. There are also a few small glaciers, such Snezhnika, located in the deep Golemiya Kazan cirque at the steep northern foot of Vihren, and Banski Suhodol. They are the southernmost glaciers in Europe.
Pirin National Park falls within the Rodope montane mixed forests terrestrial ecoregion of the Palearctic temperate broadleaf and mixed forest. Forests cover 57.3% of the parks area and almost 95% of them are coniferous forests. The average age of the forests is 85 years. Bulgaria's oldest tree, Baikushev's pine, is located in the park. With an approximate age of about 1,300 years it is a contemporary of the foundation of the Bulgarian state in 681 AD. The fauna of the Pirin National Park is diverse and includes 45 species of mammals, 159 species of birds, 11 species of reptiles, 8 species of amphibia and 6 species of fish.Stanislav Kostov
Stanislav Kostov (Bulgarian: Станислав Костов; born 2 October 1991) is a Bulgarian footballer who plays as a centre-forward for Levski Sofia.United Macedonian Organization Ilinden–Pirin
United Macedonian Organisation: Ilinden–Pirin (Обединена македонска организация: Илинден–Пирин) is a Macedonian organisation in Bulgaria, whose self-declared aims are protection of the human rights, language and nationality of the Macedonian minority in the country. In Bulgaria itself the organization is regarded as a foreign government-funded separatist organization.
In 1999, the organisation was registered as a political party and took part in the municipal elections the same year. The party polled approximately 3,000 votes in the party's core region, Blagoevgrad Province (Pirin Macedonia), in line with the number of self-declared ethnic Macedonians in the region according to the latest Bulgarian census (3,100 in 2001). The party received, however, almost no votes in the rest of the country.
On February 29, 2000, by decision of the Bulgarian Constitutional Court, UMO Ilinden–Pirin was expelled from the Bulgarian political system, as a separatist party. On November 25, the European Court of Human Rights in Strasbourg, condemned Bulgaria because of violations of the OMO Ilinden–Pirin's freedom of organising meetings. The court stated that Bulgaria had violated Act 11 from the European Convention of Human Rights.On 26 June 2006, the party held a new founding meeting and provoked some controversy in the Bulgarian media. The meeting was held in the southwestern town of Gotse Delchev despite an IMRO-BNM protest demonstration. IMRO-BNM deputy Boris Yachev accused the Macedonian government of sponsoring the party with €75,000 and called for the recall of the Macedonian ambassador Abdurahman Aliti. The party's leader, Stojko Stojkov, called the party Bulgarian and not ethnically based.On July 30 Sofia's City Court confirmed the decision to deny registration; the arguments advanced by the court were, among others, that the necessary quorum of 530 signatures had not been reached and that there were many irregularities among those presented.UMO Ilinden–Pirin has been accepted as a full member of the European Free Alliance in April 2007.Vihren
Vihren (Bulgarian: Вихрен) is the highest peak of Bulgaria's Pirin Mountains. Reaching 2,914 metres (9,560 ft), it is Bulgaria's second and the Balkans' third highest, after Musala and Mount Olympus. Although due to the karst topography Vihren is deprived of lakes and streams, a number of Pirin's lakes are located around the peak, as is Europe's southernmost glacial mass, the Snezhnika glacielet. Until 1942 Vihren was known as Eltepe (peak of storms); it was also called Buren (stormy) and Malnienosets (lightning-bringer). The UNESCO World Heritage Site Pirin National Park was originally known as the Vihren National Park. Vihren is included in the 100 Tourist Sites of Bulgaria under No. 2.