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107-785: The Stob Earth Pyramids are located at the western foothills of the Rila mountain range in the Balkan Peninsula at an altitude between 600 and 750 m. They occupy the Klisura ridge facing the valley of the Rilska River , a left tributary of the Struma . They are situated at less than one kilometre east of the village of Stob in Kocherinovo Municipality , Kyustendil Province . They lie some 83 km south of

214-492: A five-domed church, a defensive tower and monastic apartments encircling an inner yard. The exterior of the complex resembles a fortress with its high stone walls and little windows. The oldest surviving structure is the 23 m high Hrelyo's Tower, constructed in 1334–1335. The Church of Theodore Tyro and Theodore Stratelates in Dobarsko at an elevation of about 1,000 m is a small three-naved stone basilica half dug into

321-638: A number of archaicisms preserved until the early 20th century (the articulation of yat as / æ / in Boboshticë , Drenovë , around Thessaloniki, Razlog , the Rhodopes and Thrace and of yery as / ɨ / around Castoria and the Rhodopes, the presence of decomposed nasalisms around Castoria and Thessaloniki, etc.), the dialect is posited to have been part of a macrodialect extending from the Adriatic to

428-649: A result of earlier alternations between short and long vowels in roots in Proto-Indo-European , Proto-Balto-Slavic and Proto-Slavic times, and of the fronting of vowels after palatalized consonants, the following vowel alternations are attested in OCS: /ь/ : /i/;  /ъ/ : /y/ : /u/; /e/ : /ě/ : /i/; /o/ : /a/; /o/ : /e/; /ě/ : /a/; /ъ/ : /ь/; /y/ : /i/; /ě/ : /i/; /y/ : /ę/. Vowel:∅ alternations sometimes occurred as

535-858: A result of sporadic loss of weak yer , which later occurred in almost all Slavic dialects. The phonetic value of the corresponding vocalized strong jer is dialect-specific. As an ancient Indo-European language, OCS has a highly inflective morphology. Inflected forms are divided in two groups, nominals and verbs. Nominals are further divided into nouns, adjectives and pronouns. Numerals inflect either as nouns or pronouns, with 1–4 showing gender agreement as well. Nominals can be declined in three grammatical genders (masculine, feminine, neuter), three numbers (singular, plural, dual ) and seven cases : nominative , vocative , accusative , instrumental , dative , genitive , and locative . There are five basic inflectional classes for nouns: o/jo -stems, a/ja -stems, i -stems, u -stems, and consonant stems. Forms throughout

642-573: A variant of the angular Glagolitic alphabet was preserved in Croatia . See Early Cyrillic alphabet for a detailed description of the script and information about the sounds it originally expressed. For Old Church Slavonic, the following segments are reconstructible. A few sounds are given in Slavic transliterated form rather than in IPA, as the exact realisation is uncertain and often differs depending on

749-544: Is 2,560 m while the lowest is 1,300 m. Over 36,000 foreign tourists have stayed in Borovets for the 2016/17 winter season spending an average of five nights. Other much smaller ski resorts include Panichishte with several ski runs, Semkovo with seven ski runs totaling 4 km, Bodrost with 5 km ski runs and Govedartsi with a single 1.7 km ski run. The Balmeken High Mountain Sports Complex

856-746: Is 2.6 °C on the northern slopes and 3.1 °C on the southern. With an average annual temperature of −3.0 °C, Musala is the coldest place in Bulgaria. The lowest absolute temperature in Rila was also measured there: −31.2 °C; the lowest mean monthly temperature was recorded there in February: −11.6 °C. The absolute maximum temperature at Musala is 18.7 °C. Temperature amplitude decreases with elevation from 20 °C at 800 m to 15 °C at 2,800 m. Temperature inversions , i.e. increase in temperature with height, are frequent on

963-464: Is also influenced by the terrain, the exposure of the slopes and the orientation of the valleys. The average temperature decreases and the average precipitation increases with elevation. The coldest month is March and the hottest one August. Negative temperatures remain on average for about nine months in the Alpine zone, often continuing until the end of June. A steady rise in temperature is observed in

1070-488: Is also likely to have preserved an extremely archaic type of accentuation (probably close to the Chakavian dialect of modern Serbo-Croatian ), but unfortunately, no accent marks appear in the written manuscripts. The South Slavic and Eastern South Slavic nature of the language is evident from the following variations: Old Church Slavonic also shares the following phonetic features only with Bulgarian : Over time,

1177-594: Is called Lakatitska Rila. It is linked with the Verila mountain range to the north through the Klisura Saddle, and with Central Rila to the east through the Kobilino Branishte saddle. The average elevation is 1,556 m; the highest summit is Mount Golyiam Kupen at an elevation of 2731 m. There are 29 peaks over 2,100 m. This subdivision is known for its rugged peaks and picturesque lakes in

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1284-415: Is closely linked to the snowline during the last glacial period and most of them lie at elevations between 2,100 m and 2,500 m. Most lakes (28) are situated at elevations between 2,300 m and 2,350 m; there are 23 between 2,350 m and 2,400 m, 19 between 2,250 m and 2,300 m and 19 between 2,400 m and 2,450 m. Their length varies between 800 m and 20 m,

1391-463: Is covered by dwarf mountain pine ( Pinus mugo ) and common juniper ( Juniperus communis ) formations mixed with green alder ( Alnus viridis ) at wetter localities and Rhododendron myrtifolium in East Rila. The alpine line is covered with grass, moss, lichen, rare flowers, dwarf willows such as Salix herbacea , Salix retusa and Salix reticulata , etc. Due to the difficult terrain,

1498-690: Is determined by the elevation. At the lowest portions there are xerothermal oak forests dominated by Hungarian oak ( Quercus frainetto ), pubescent oak ( Quercus pubescens ) and Austrian oak ( Quercus cerris ) with some Mediterranean cenosis of cade juniper ( Juniperus oxycedrus ) and scorpion senna ( Hippocrepis emerus ). Higher in the mountain up to 1,300 m the deciduous forests are primarily of sessile oak ( Quercus petraea ) with smaller participation of European hop-hornbeam ( Ostrya carpinifolia ), common hornbean ( Carpinus betulus ), Heldreich's maple ( Acer heldreichii ), Balkan maple ( Acer hyrcanum ) and European ash ( Fraxinus excelsior );

1605-554: Is divided into four distinct parts. East Rila, known also as Musala Rila, is the largest and highest subdivision, situated between the valleys of the rivers Beli Iskar and Belishka. It is formed of two main ridges. The Musala Ridge spans in north–south direction between the valleys of Beli Iskar and Maritsa; the Ibar Ridge runs in west–east direction from the summit of Marishki Chal to the Avramovo Saddle. It covers 37% of

1712-469: Is expected to rise to over 7000; of them 34 are endemic to Rila, 123 — to Bulgaria and another 123 — to the Balkans. The biodiversity, ecosystems and the pristine landscapes are protected by Rila National Park declared in 1992, which is Bulgaria's largest spanning a territory of 810.46 km , and Rila Monastery Nature Park covering another 252.535 km . There are four nature reserves in

1819-401: Is given in the table below. Autocephaly recognized by some autocephalous Churches de jure : Autocephaly and canonicity recognized by Constantinople and 3 other autocephalous Churches: Spiritual independence recognized by Georgian Orthodox Church: Semi-Autonomous: Written evidence of Old Church Slavonic survives in a relatively small body of manuscripts , most of them written in

1926-536: Is in autumn and winter. The largest waterfalls are Skakavitsa (70 m) and Goritsa (39 m). There are abundant mineral springs that include the hottest one in South-eastern Europe at Sapareva Banya forming a geyser with a temperature of 101.4 °C. The cirques at the high elevation zone contain 189 glacial lakes; there are also about 30 smaller ones that evaporate in summer, including tectonic lakes like Panichishte. Their location

2033-478: Is located at an elevation of 2,050 m in East Rila and is used for training, medical and biological research by athletes but also provides opportunities for family recreation. The mountain range was a favourite place of retreat for the Bulgarian monarchs Ferdinand I (r. 1887–1918) and his son Boris III (r. 1918–1943). The palace of Tsarska Bistritsa was constructed between 1898 and 1914 above Borovets in

2140-406: Is occasionally used by Western scholars in a regional context. According to Slavist Henrik Birnbaum , the term was introduced mostly by Macedonian scholars and it is anachronistic because there was no separate Macedonian language, distinguished from early Bulgarian, in the ninth century. The obsolete term Old Slovenian was used by early 19th-century scholars who conjectured that the language

2247-530: Is reddish with alternating layers of cobble conglomerate and lightly soldered sandstone, as well as larger rock pieces originating from the slopes of Rila. The principal factor for the formation of the Stob Earth Pyramids is erosion due to rainfall. The rain drops penetrate the lightly soldered sediment and continuously wash it away. The location of the rock pieces in the stratum determines the place, size and shape of each pyramid because they prevent

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2354-478: Is renowned mainly for the glacial lakes Ribni , Dzhendemski, Manastirski, as well as the largest glacial lake in the Balkan Peninsula ;— Smradlivo Lake . Northwest Rila, known also as Malyovitsa Rila, occupies about 24% of Rila and is situated between the valleys of Rilska to the south, Levi Iskar to the east, Samokov to the north-east and Dupnitsa to the west. Its much lower northern section

2461-641: Is served by the Bulgarian State Railways via railway line No. 1 in the north-east with stations at Kostenets and Belovo, railway line No. 5 along the Struma Valley in the west and the Septemvri–Dobrinishte narrow-gauge line in the south-east. The most important sectors of the local economy are tourism, services, industry and agriculture. The abundant water resources are utilised by some of Bulgaria's largest hydro power plants,

2568-520: Is situated there. Rila is a fault-block mountain and represents a crescent-shaped horst with two fault systems — concentric and radial. It is part of the oldest land in the Balkans, the Macedonian–Thracian Massif. The mountain range is formed mainly by metamorphic and intrusive rocks . The core of Rila is built up predominantly by granite. It is covered by a thick layer of crystalline schists and granite– gneiss ; this layer

2675-563: Is sometimes called Old Slavic , which may be confused with the distinct Proto-Slavic language . Bulgarian, Croatian, Macedonian, Serbian, Slovene and Slovak linguists have claimed Old Church Slavonic; thus OCS has also been variously called Old Bulgarian , Old Croatian , Old Macedonian or Old Serbian, or even Old Slovak , Old Slovenian . The commonly accepted terms in modern English-language Slavic studies are Old Church Slavonic and Old Church Slavic . The term Old Bulgarian ( Bulgarian : старобългарски , German : Altbulgarisch )

2782-471: Is the Rila Monastery , Bulgaria's largest and most important monastery, founded in the 10th century by Saint John of Rila . Due to its outstanding cultural and spiritual value it was declared a UNESCO World Heritage Site in 1983. Rila is also a popular destination for hiking, winter sports and spa tourism, hosting the nation's oldest ski resort Borovets , as well as numerous hiking trails. Some of

2889-574: Is the designation used by most Bulgarian-language writers. It was used in numerous 19th-century sources, e.g. by August Schleicher , Martin Hattala , Leopold Geitler and August Leskien , who noted similarities between the first literary Slavic works and the modern Bulgarian language. For similar reasons, Russian linguist Aleksandr Vostokov used the term Slav-Bulgarian . The term is still used by some writers but nowadays normally avoided in favor of Old Church Slavonic . The term Old Macedonian

2996-605: Is the first Slavic literary language and the oldest extant written Slavonic language attested in literary sources. It belongs to the South Slavic subgroup of the Balto-Slavic branch of the Indo-European language family and remains the liturgical language of many Christian Orthodox churches. Until the reforms of Patriarch Nikon of Moscow between 1652 and 1666, Church Slavonic was the mandatory language of

3103-688: Is the highest mountain range of Bulgaria, the Balkan Peninsula , and Southeast Europe . It is situated in southwestern Bulgaria and forms part of the Rila– Rhodope Massif. The highest summit is Musala at an elevation of 2,925 m which makes Rila the sixth highest mountain range in Europe after the Caucasus , the Alps , Sierra Nevada , the Pyrenees and Mount Etna , and the highest one between

3210-565: Is the oldest winter resort in Bulgaria and the largest one in Rila. It has 27 marked ski runs with a total length of 58 km equipped with 12 lifts facilities and provides conditions for alpine skiing , cross-country skiing , night skiing , biathlon , snowboard , etc.; it has hosted competitions in the FIS Alpine Ski World Cup and the Biathlon World Championships 1993 . The top elevation

3317-571: Is the smallest part spanning 9% of the Rila's total area but has the most Alpine character and the highest average elevation — 2,077 m. It stretches between the valleys of the rivers Beli Iskar, Cherni Iskar, Levi Iskar, Iliyna and Rilska . The later divides the two main ridges in Central Rila, Skakavitsa and Rilets. The highest summit is Cherna Polyana (2,716 m); other important peaks are Skalata, Small and Big Skakavets, Rilets; there are 28 peaks over 2,100 m. This subdivision

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3424-552: Is topped by sandstones and conglomerates which were formed by elevated Tertiary sediments. Traces of these sediments are found in the Northwest Rila at an elevation of up to 1,900 m. The highest zones are made mainly of granite, and below are crystalline schists, whose compound minerals are sequentially deposited. They are represented by gneiss, mica schists, and amphibolite . In many places granite passes into granite–gneiss. There are marbles and amphibolites formed in

3531-513: The Balkan Peninsula , and the sixth highest in Europe after the Caucasus , the Alps , Sierra Nevada , the Pyrenees and Mount Etna . Musala is the fourth most isolated peak in continental Europe after Mont Blanc , Mount Elbrus and Galdhøpiggen raising at a distance of 810 km from the nearest point of the same elevation. With a prominence of 2,473 m, Musala ranks seventh among Europe's ultra-prominent peaks . The mountain range

3638-594: The Black Sea , and covering southern Albania, northern Greece and the southernmost parts of Bulgaria. Because of the very short time between Rastislav 's request and the actual mission, it has been widely suggested that both the Glagolitic alphabet and the translations had been "in the works" for some time, probably for a planned mission to the Bulgaria . The language and the Glagolitic alphabet, as taught at

3745-585: The Common Slavic period, such as intrasyllabic synharmony and the law of open syllables . For consonant and vowel clusters and sequences of a consonant and a vowel, the following constraints can be ascertained: As a result of the first and the second Slavic palatalizations, velars alternate with dentals and palatals. In addition, as a result of a process usually termed iotation (or iodization ), velars and dentals alternate with palatals in various inflected forms and in word formation. In some forms

3852-655: The Cyrillic script developed early on at the Preslav Literary School, where it superseded Glagolitic as official in Bulgaria in 893. The texts written during this era exhibit certain linguistic features of the vernaculars of the First Bulgarian Empire . Old Church Slavonic spread to other South-Eastern, Central, and Eastern European Slavic territories, most notably Croatia , Serbia , Bohemia , Lesser Poland , and principalities of

3959-593: The First Bulgarian Empire during the late 10th and the early 11th centuries. The language has an Eastern South Slavic basis in the Bulgarian-Macedonian dialectal area, with an admixture of Western Slavic (Moravian) features inherited during the mission of Saints Cyril and Methodius to Great Moravia (863–885). The only well-preserved manuscript of the Moravian recension, the Kiev Missal , or

4066-563: The Kievan Rus' – while retaining characteristically Eastern South Slavic linguistic features. Later texts written in each of those territories began to take on characteristics of the local Slavic vernaculars, and by the mid-11th century Old Church Slavonic had diversified into a number of regional varieties (known as recensions ). These local varieties are collectively known as the Church Slavonic language . Apart from use in

4173-637: The Paleozoic over 250 million years ago and subsequently elevated during the Tertiary period. The coarse–grained granites are the dominant rocks forming almost two–thirds of the area of the Rila's higher parts. Rila was subjected to glaciation during the Pliocene and the Pleistocene . Its modern Alpine relief was formed during the last Würm glaciation some 10–12 000 years ago, when the snowline of

4280-533: The Province of Thessalonica (in present-day Greece ). Old Church Slavonic played an important role in the history of the Slavic languages and served as a basis and model for later Church Slavonic traditions, and some Eastern Orthodox and Eastern Catholic churches use this later Church Slavonic as a liturgical language to this day. As the oldest attested Slavic language, OCS provides important evidence for

4387-656: The Russian Orthodox Church . Historians credit the 9th-century Byzantine missionaries Saints Cyril and Methodius with standardizing the language and undertaking the task of translating the Gospels and necessary liturgical books into it as part of the Christianization of the Slavs . It is thought to have been based primarily on the dialect of the 9th-century Byzantine Slavs living in

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4494-532: The Struma motorway and the parallel first class I-1 road that form part of European route E79 along the Struma valley. The third class III-107 branches from I-1 at the municipal centre Kocherinovo and heads for 7 km to north-east to Stob. The Stob Earth Pyramids were declared a natural landmark in 1964 with a total extension of the protected area of 7.4 hectares, or 0.74 km. Rila Rila ( Bulgarian : Рила , pronounced [ˈriɫɐ] )

4601-680: The 120 are nesting within Rila National Park. These include three relicts — boreal owl , Eurasian pygmy owl and Eurasian three-toed woodpecker , and species that require special conservation measures like short-toed snake eagle , golden eagle , peregrine falcon , black stork , Eurasian woodcock , western capercaillie , hazel grouse , rock partridge , grey-headed woodpecker , black woodpecker , white-throated dipper , wallcreeper and Alpine chough among others. There are 18 reptile, 10 amphibian and 12 fish species. The invertebrate fauna discovered so far includes 4186 species and

4708-604: The 17–19 centuries due to production of iron and has a number of monuments, including churches, a convent, a 17th-century Ottoman drinking fountain and a museum of history. Near Belchin is located the recently restored Tsari Mali Grad Fortress. Rila Point on Livingston Island in the South Shetland Islands , Antarctica is named after Rila Mountain. Old Bulgarian language Old Church Slavonic or Old Slavonic ( / s l ə ˈ v ɒ n ɪ k , s l æ ˈ v ɒ n -/ slə- VON -ik, slav- ON - )

4815-664: The 9th and 11th century in Great Moravia and the First Bulgarian Empire. The language was standardized for the first time by the mission of the two apostles to Great Moravia from 863. The manuscripts of the Moravian recension are therefore the earliest dated of the OCS recensions. The recension takes its name from the Slavic state of Great Moravia which existed in Central Europe during the 9th century on

4922-649: The Alpine zone that include the Seven Rila Lakes and the Urdini Lakes . Central Rila includes the mountain's highest waterfall, Skakavitsa (70 m). Southwest Rila stretches between the valleys of the Rilska, Iliyna and Belishka rivers to the north, the Predel Saddle that separates it from Pirin to the south, and Simitli and Blagoevgrad valleys to the west. It covers about 30% of the area of

5029-679: The Alps and the Caucasus. It spans a territory of 2,629 km with an average elevation of 1487 m. The mountain is believed to have been named after the river of the same name , which comes from the Old Bulgarian verb "рыти" meaning "to grub". Rila has abundant water resources. Some of the Balkans' longest and deepest rivers originate from Rila, including the Maritsa , Iskar and Mesta rivers. Bulgaria's main water divide separating

5136-570: The Balkan area. Established in the First Bulgarian Empire by the medieval Bulgarian hermit and saint John of Rila during the reign of emperor Peter I of Bulgaria (r. 927–969), the monastery developed into one of the main cradles of Bulgarian culture, literature and spirituality. In the 18th century it became one of the main hubs of the Bulgarian National Revival . The complex covers an area of 8,800 m and consists of

5243-537: The Balkans separating the drainage basins of the Black Sea and the Aegean Sea passes through Rila's northern ridge, including the summit of Musala. Some of the Balkans' longest rivers originate from Rila, including the Maritsa , Iskar and Mesta , as well as several important tributaries of the Struma  — Rilska , Dzherman and Blagoevgradska Bistritsa . Of them, the Iskar and its tributaries belong to

5350-481: The Balkans. Rila accounts for 6% of Bulgaria's timber resources. Manufacturing industry is centred in Blagoevgrad, Dupnitsa, Samokov, Razlog and Belovo; the main sectors are food processing, machine building, pharmaceutical and paper mills. Rila is a popular tourist destination for winter sports, spa tourism, recreation and cultural tourism. Borovets , situated on the northern slopes at 9 km from Samokov,

5457-640: The Balkans; 31 are Tertiary or pre-glacial relicts and 104 are glacial relicts. Notable Bulgarian endemic species include Rila primrose ( Primula deorum ) and rhapontic rhubarb ( Rheum rhaponticum ); taxa restricted to the Balkans include Bulgarian avens ( Geum bulgaricum ), yellow columbine ( Aquilegia aurea ), Bulgarian gentian ( Gentianella bulgarica ), Balkanian butterwort ( Pinguicula balcanica ), Crocus veluchensis , Dianthus microlepis , etc. The non-vascular flora includes 974 algae , 313 moss and 251 lichen species. The fungi are represented by 665 species, including 64 mushrooms listed in

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5564-525: The Barakovo one is built up by conglomerate and sandstone. During the Pliocene the area was at the bottom of a shallow lake and accumulated sediments that form a 200 and 250 m thick stratum consisting of little fragments with a lot of clay. The colour is dull white to yellowing. It forms the foundations of the pyramids but the erosion reveals only small patches this layer. The Pleistocene stratum above

5671-606: The Black Sea and the Aegean Sea drainage systems follows the main ridge of Rila. The mountain range is dotted with almost 200 glacial lakes such as the renowned Seven Rila Lakes , and is rich in hot springs in the fault areas at the foothills, including the hottest spring in South-eastern Europe in Sapareva Banya . The mountain range has varied flora and fauna with a number of endemic and relict species and some of

5778-428: The Black Sea drainage basins, and all the rest — to the Aegean. About 78% of the water flows into the Aegean drainage system. The runoff comes from snowmelt in the Alpine zones and rainfall. Water discharge reaches its maximum in late spring and early summer with spring accounting for more than half of the total annual discharge. The maximum at the highest elevations is in summer due to the late snowmelt. The minimum

5885-430: The Byzantine missionary contingent in 886. Exiled students of the two apostles then brought the Glagolitic alphabet to the Bulgarian Empire , being at least some of them Bulgarians themselves. Boris I of Bulgaria ( r.  852–889 ) received and officially accepted them; he established the Preslav Literary School and the Ohrid Literary School . Both schools originally used the Glagolitic alphabet, though

5992-529: The East it had a status analogous to that of Latin in Western Europe , but had the advantage of being substantially less divergent from the vernacular tongues of average parishioners. Some Orthodox churches, such as the Bulgarian Orthodox Church , Russian Orthodox Church , Serbian Orthodox Church , Ukrainian Orthodox Church and Macedonian Orthodox Church – Ohrid Archbishopric , as well as several Eastern Catholic Churches, still use Church Slavonic in their services and chants. Initially Old Church Slavonic

6099-429: The Great Moravian Academy ( Slovak : Veľkomoravské učilište ), were used for government and religious documents and books in Great Moravia between 863 and 885. The texts written during this phase contain characteristics of the West Slavic vernaculars in Great Moravia. In 885 Pope Stephen V prohibited the use of Old Church Slavonic in Great Moravia in favour of Latin . King Svatopluk I of Great Moravia expelled

6206-516: The Kiev Folia, is characterised by the replacement of some South Slavic phonetic and lexical features with Western Slavic ones. Manuscripts written in the Second Bulgarian Empire (1185–1396) have, on the other hand, few Western Slavic features. Though South Slavic in phonology and morphology, Old Church Slavonic was influenced by Byzantine Greek in syntax and style, and is characterized by complex subordinate sentence structures and participial constructions. A large body of complex, polymorphemic words

6313-412: The Red Book of Bulgaria. The mammal species within Rila National Park and its surroundings are 62 and include taxa of high conservation value, such as brown bear , gray wolf , wildcat , least weasel , European pine marten , marbled polecat , wild boar , red deer , roe deer , chamois , European ground squirrel , as well as the glacial relict European snow vole . The bird species are 156; of

6420-450: The Slavic countries, Old Church Slavonic served as a liturgical language in the Romanian Orthodox Church , and also as a literary and official language of the princedoms of Wallachia and Moldavia (see Old Church Slavonic in Romania ), before gradually being replaced by Romanian during the 16th to 17th centuries. Church Slavonic maintained a prestigious status, particularly in Russia , for many centuries – among Slavs in

6527-468: The abrasion of the layers below. They are covered by a 1 cm thick coat of hardened sun burned clay which protects the fragile sandstone and delays the erosion. The Stob Earth Pyramids vary in shape from sharp through conical to mushroomlike. About half of the formations are crowned by rocks, whose area is sometimes two to three times larger than the cross-section of the pyramid below. Their height averages some 6 to 10 m but can reach up to 12 m;

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6634-498: The alternations of /c/ with /č/ and of /dz/ with /ž/ occur, in which the corresponding velar is missing. The dental alternants of velars occur regularly before /ě/ and /i/ in the declension and in the imperative, and somewhat less regularly in various forms after /i/, /ę/, /ь/ and /r /. The palatal alternants of velars occur before front vowels in all other environments, where dental alternants do not occur, as well as in various places in inflection and word formation described below. As

6741-412: The area that a text originated from. For English equivalents and narrow transcriptions of sounds, see Old Church Slavonic Pronunciation on Wiktionary . For English equivalents and narrow transcriptions of sounds, see Old Church Slavonic Pronunciation on Wiktionary . Several notable constraints on the distribution of the phonemes can be identified, mostly resulting from the tendencies occurring within

6848-403: The best preserved forests in the country. The biodiversity and the pristine landscapes are protected by Rila National Park which covers much of the mountain; the rest lies within Rila Monastery Nature Park . In addition, there are five nature reserves : Parangalitsa , Central Rila Reserve , Rila Monastery Forest , Ibar and Skakavitsa . The most recognisable landmark of the mountain range

6955-409: The biggest and most complex hydroelectric complex in Bulgaria, with a combined installed capacity of 1,599 MW. At an elevation of 1,900 m is located the second biggest reservoir in Rila, Beli Iskar , constructed between 1939 and 1945, that provides 25% of Sofia's potable water and powers a small 16 MW hydro power station. At an elevation of 2,394 m, Kalin is the highest reservoir in

7062-447: The development of Slavonic liturgy. As part of preparations for the mission, in 862/863, the missionaries developed the Glagolitic alphabet and translated the most important prayers and liturgical books , including the Aprakos Evangeliar , the Psalter , and the Acts of the Apostles , allegedly basing the language on the Slavic dialect spoken in the hinterland of their hometown, Thessaloniki , in present-day Greece . Based on

7169-400: The fault lines along the northern foothills of Rila favour health and spa tourism. The most significant spa resorts from west to east are Sapareva Banya with a total discharge of 33 L/sec and temperature of 33–101.4 °C, Belchinski Bani with a total discharge of 24 L/sec and temperature of 40–41.5 °C, Dolna Banya with a total discharge of 22 L/sec and temperature of 56.3 °C and

7276-536: The features of Proto-Slavic , the reconstructed common ancestor of all Slavic languages. The name of the language in Old Church Slavonic texts was simply Slavic ( словѣ́ньскъ ѩꙁꙑ́къ , slověnĭskŭ językŭ ), derived from the word for Slavs ( словѣ́нє , slověne ), the self-designation of the compilers of the texts. This name is preserved in the modern native names of the Slovak and Slovene languages. The terms Slavic and Slavonic are interchangeable and either may be used correctly in English. The language

7383-560: The foothills, inhabited by c. 250,000 people. Administratively it falls in four of Bulgaria's 28 provinces: Blagoevgrad , Kyustendil , Sofia and Pazardzhik . From west to east there are five towns at the northern foothills — Sapareva Banya (pop. 3,815 as of 2016), Samokov (25,880), Dolna Banya (4,510), Kostenets (6,228) and Belovo (3,533); there are four towns at the western foothills (from north to south) — Dupnitsa (35,255), Rila (2,359), Kocherinovo (1,723) and Blagoevgrad (66,886); as well as three more at

7490-399: The forests of Rila are not much influenced by anthropogenic activities and their average age is above 100 years. Some Norway spruces and European silver firs reach height of 60 m. The number of vascular plants includes about 1400 species registered only within the territory of Rila National Park, of them 34 are endemic to Bulgaria, including three restricted to Rila, and 89 — to

7597-406: The former — Parangalitsa , Central Rila Reserve , Ibar and Skakavitsa , and another one, Rila Monastery Forest , in the latter. Parangalitsa was declared a UNESCO Biosphere Reserve in 1977, while the Central Rila Reserve is the largest one in the Balkans with an area of 123.937 km . Rila is a sparsely populated mountain range with most of the settlements located in the valleys at

7704-496: The ground, constructed in 1614 and painted in 1672. The church is noted for its abundance of original frescoes and icons. The Church of Saint Nicholas in Sapareva Banya is small medieval edifice, constructed anytime from the 11th to the 14th century. It was built using red bricks and white mortar and is of a simple cross-in-square design, with a single nave and apse. The town of Samokov achieved economic prosperity during

7811-760: The highest lakes. The largest glacial lake in Rila and in the Balkans is Smradlivo with an area of 212 decares; the longest is the Upper Ribno Lake reaching 801 m; the deepest is Okoto, one of the Seven Rila Lakes with a depth of 37.5 m; the highest is Ledeno at an elevation of 2,709 m; the lowest is Suho at 2,045 m. The most important lake groups are the Seven Rila Lakes (seven lakes), Musala Lakes (seven), Marichini Lakes (seven), Urdini Lakes (six), Malyovishki Lakes (three), Elenski Lakes (three), Chanakgyolski Lakes (two), Vapski Lakes (two), etc. The vegetation

7918-663: The highest peaks are: Rila is situated in the southern zone of the humid continental climate region and has typical Alpine climate with elevational zones. The climate is influenced by the Icelandic and the West Mediterranean cyclones , the former mainly in late spring and early summer, and the latter — in winter, bringing frequent and high rainfall, as well as by the Azores and Siberian anticyclones in summer and winter, bringing droughts. The local microclimate

8025-661: The highest sections of the mountain with an elevation between 2,800 and 2,400 m. It represents practically leveled terrain with gently folded surface, formed in the place of ancient forest massifs. The next Late Miocene level, the young Miocene, is situated on the main side ridges with an elevation between 2,600 and 2,300 m. The third level formed during the Early Pliocene has an elevation of 1,800 and 1,600 m. The Late Pliocene level occupies areas with an elevation of up to 1,300 m. There are two summits above 2,900 m, Musala and Malka Musala . Some of

8132-572: The inflectional paradigm usually exhibit morphophonemic alternations. Fronting of vowels after palatals and j yielded dual inflectional class o  : jo and a  : ja , whereas palatalizations affected stem as a synchronic process (N sg. vlьkъ , V sg. vlьče ; L sg. vlьcě ). Productive classes are o/jo- , a/ja- , and i -stems. Sample paradigms are given in the table below: Adjectives are inflected as o/jo -stems (masculine and neuter) and a/ja -stems (feminine), in three genders. They could have short (indefinite) or long (definite) variants,

8239-405: The influx of warm Mediterranean air masses. Winds may reach speed of 40–45 m/s (over 100 km/h) at the summits, with mostly south-western and western orientation. The north-west and north-east winds are more moderate. The average monthly wind speed on the highest mountain summits reaches 11–12 m/s. In the lower parts, the average monthly speed varies from 1.2 to 2.5 m/s and in

8346-450: The language adopted more and more features from local Slavic vernaculars, producing different variants referred to as Recensions or Redactions . Modern convention differentiates between the earliest, classical form of the language, referred to as Old Church Slavonic, and later, vernacular-coloured forms, collectively designated as Church Slavonic . More specifically, Old Church Slavonic is exemplified by extant manuscripts written between

8453-404: The latter being formed by suffixing to the indefinite form the anaphoric third-person pronoun jь . Synthetic verbal conjugation is expressed in present, aorist and imperfect tenses while perfect, pluperfect, future and conditional tenses/moods are made by combining auxiliary verbs with participles or synthetic tense forms. Sample conjugation for the verb vesti "to lead" (underlyingly ved-ti )

8560-587: The main ones. The bottom of cirques are often occupied by glacial lakes . As a result of the weathering , scree formations of varied nature have been accumulated. In the south-western foothills of Rila the Stob Earth Pyramids were formed under the influence of erosion. The staged elevation of the mountain during the geological eras and the large range of vertical folds have led to the formation of four denudation levels of distinct age, height and range. The oldest Early Miocene level encompasses

8667-413: The massif. In the west along the Struma Valley runs Struma motorway paralleled by the first class I-1 road , both part of European route E79 , that connect the national capital Sofia and Greece via the provincial centre Blagoevgrad . The second class II-62 road branches off I-1 at Dupnitsa and runs east to Samokov where it joins the second class II-82 road which continues in eastern direction until

8774-466: The middle and end of July. Even during the summer months, temperature over 10 °C do not hold up for long periods. About five to ten days in June, July and August have an average temperature above 15 °C. This determines the short vegetation period in the high elevation areas which varies from three to six months; it lasts about three months at elevation over 2,000 m. The average annual temperature

8881-523: The middle height zone it ranges from 2.5 to 3.2 m/s. Winds are usually strongest in winter and lightest in autumn. The annual duration of sunshine in the Alpine zone is 1930 hours with maximum in August and minimum in December–January; it raises to more than 2150 hours at 1,000 m. Rila is an important hydrological unit in Bulgaria with very high hydropower potential, representing about 1/4 of

8988-518: The most important hydro power stations in Bulgaria are situated in the eastern part of the mountain range, including the Belmeken–Sestrimo–Chaira Hydropower Cascade (1,599 MW), the largest and most complex hydroelectric complex in Bulgaria. Rila is a mountain range in south-western Bulgaria, part of the Rila– Rhodope Massif. It is situated between five valleys – Dupnitsa Valley to the north-west, Samokov Valley to

9095-557: The most important of them being fueled by the Belmeken Dam in East Rila ;— Chaira Pumped Storage Hydro Power Plant (864 MW), Belmeken Pumped Storage Hydro Power Plant (375 MW), Sestrimo Hydro Power Plant (240 MW) and Momina Klisura Hydroelectric Power Station (120 MW). Chaira is the largest pumped storage HPP in South-eastern Europe. They form the Belmeken–Sestrimo–Chaira Hydropower Cascade ,

9202-406: The mountain range. With an average elevation of 1,307 m, it has the lowest elevation in Rila. The highest summit is Angelov Peak (2,643 m). The Blagoevgradska Bistritsa River divides it in two distinct ridges to the north and to the south. Apart from its northernmost part, Southwest Rila does not have the Alpine character of the other three subdivisions. The biosphere reserve Parangalitsa

9309-463: The mountain was 2,100–2,200 m. The glaciers reached elevations as low as 1,200 m. Above this boundary, the glaciers radically altered the existing relief, forming deep cirques, pyramidal peaks , steep cliffs, long U-shaped valleys , moraine fields and other glacial forms. On the slopes of some valleys such as those of the rivers Beli Iskar, Maritsa and Rilska there are hanging glacier valleys  — tributary valleys located higher than

9416-487: The mountain's territory and contains the highest summit in the range — Musala (2,925 m), as well as 12 of the 18 summits over 2,700 m — Irechek (2,852 m), Deno (2,790 m), Mancho (2,771 m) and others; there are 46 peaks over 2,100 m. East Rila contains a number of glacial lake groups, including Musala Lakes and Marichini Lakes , as well as the nation's largest ski resort Borovets . Central Rila, known also as Skakavitsa Rila,

9523-562: The national capital Sofia and 18 km north of the city of Blagoevgrad . Geologically, the Stob Earth Pyramids are part of the Blagoevgrad Graben that consists of lakebed, alluvial and sloping deposits dated from the Pliocene and Pleistocene epochs. They are built up by Precambrian metamorphic rocks. There are two geological formations : the Dzherman Formation consists of aleurolite, clay and sandstone;

9630-480: The north, Kostenets–Dolna Banya Valley to the north-east, Razlog Valley to the south and Blagoevgrad Valley to the south-west. Five saddles link Rila to the surrounding mountain ranges – Klisura Saddle (1,025 m) with Verila to the north-west, Borovets Saddle (1,305 m) with Sredna Gora to the north, Yundola (1,375 m) and Avramovo Saddles (1,295 m) with the Rhodope Mountains to

9737-638: The northern slopes and after 20–30 December on the southern. Its average monthly thickness reaches 20 to 30 cm in February at low elevations. In the Alpine zone above 2,000 m the snow cover is thickest in March, reaching 70 to 80 cm. In the highest ridges the maximum thickness reaches 200 to 240 cm. The snow cover remains for an average of 70–80 days at elevations of 1,200–1,300 m and 180 to 200 days at elevations above 2,000 m. Avalanches are frequent, often caused by temperature changes by

9844-516: The northern slopes and occur especially often in the Samokov Valley, Borovets and Musala, where it is observed in 250 days annually. The annual precipitation varies with elevation and slope orientation. The annual precipitation is 653 mm at Samokov (1,029 m), 932 mm at Borovets (1,350 m) and 1200 mm at Musala (2,925 m); about 80% of it being snow at the later. The rainfall occurs mostly in summer and spring on

9951-493: The northern slopes, with maximum in June and minimum in February; the rainfall increases in winter and decreases in summer on the southern slopes and yet the monthly maximum and minimum are the same; there are 130–160 days with rainfall/snowfall. Air humidity in the highlands of Rila ranges between 80 and 85%. The coldest winter months are also the driest. Humidity differs on the northern and southern slopes of Rila. The snow cover above 1,000 m begins to form on 10–15 December on

10058-414: The south-east and Predel Saddle (1,140 m) with Pirin to the south. Within these limits Rila spans an area of 2,629 km and has an average elevation of 1,487 m. The high elevation zone over 1,600 m forms about 50% of the total territory. There are over 140 main peaks above 2,000 m. With an elevation of 2,925 m at Musala, Rila is the highest mountain range in Bulgaria and

10165-441: The south-eastern foothills (from west to east) — Razlog (12,036), Belitsa (2,964) and Yakoruda (5,288). There are a number of villages, including among others Govedartsi , Belchin , Madzhare , Kostenets , Pastra , Stob , Barakovo , Dobarsko , etc. Some of the settlements on the Rila include a small Aromanian minority. The mountain range is served by several roads running along its foothills. No roads traverse

10272-549: The summit of Musala. Rila Monastery is the most important architectural monument in the mountain range. It is situated at an elevation of 1,147 m and was declared a UNESCO's world heritage site in 1983. The Monastery is considered to be a cultural and spiritual centre of Bulgaria. With its architecture and frescos Rila Monastery represents a masterpiece of the creative genius of the Bulgarian people and has exerted considerable influence on architecture and aesthetics within

10379-835: The thickness at the base is up to 40 m. Most of them are facing in southern direction but there are also a few grouped together on the northern slopes of the ridge overlooking Stob. Groups of individual Pyramids have been named the Towers, the Brothers, the Hammers, the Wedding Couple, the Pinnacles, the Samodiva Chimneys, etc. They are tourist destination, although not as popular as the much larger Melnik Earth Pyramids . The rock formations are easily accessible via

10486-465: The total potential of the country. The water reserves that form within the mountain range are the most important source of clean potable water for the surrounding settlements, the national capital Sofia and part of the population of Northern Greece and European Turkey. The regime of the rivers of Rila is directly related to the elevation and about half of the water reserves in the mountain are at an elevation above 2,050 m. The main drainage divide in

10593-524: The town of Kostenets, where it joins the first class I-8 road , part of European route E80 . The second class II-19 road which branches off I-1 at Simitli , goes east crossing the Predel Saddle into the Razlog Valley and at the homonymous town links with the second class II-84 road which runs in north-eastern direction along the Avramovo Saddle and links with the I-8 road/E80 near Pazardzhik . Rila

10700-602: The traditional Bulgarian National Revival style with several edifices and a park. Its 170 kW hydroelectric generator installed in 1912 is still working unaltered. Two other hunting lodges were constructed for the monarchs — Sitnyakovo and Saragyol . There are 17 mountains refuges with a total of 1938 beds. There are 198 km primary and 363 km secondary hiking trails in Rila National Park, including E4 European long distance path that traverses it from west to south and E8 European long distance path that traverses it from north-west to south. Rila National Park

10807-476: The village of Kostenets with a total discharge of 12 L/sec and temperature of 46–73 °C. Rila has well developed cultural tourism and contains five of the 100 Tourist Sites of Bulgaria  — the Church of Theodore Tyro and Theodore Stratelates in the village of Dobarsko , the Rila Monastery and the Stob Earth Pyramids , the Seven Rila Lakes, the museum of history and the convent in the town of Samokov, and

10914-425: The width — between 375 m and 10 m, the area — between 1 m and 212 decares, the depth — between 0.5 m and 37.5 m. Most of them are between 2 m and 10 m deep and four reach depth of over 20 m. The water is transparent as deep as 15 m. Most of the lakes are covered with ice during most of the year — from October to June. The ice thickness reaches 3 m in

11021-549: The zone between 1,300 m and 1,600 m is dominated by European beech ( Fagus sylvatica ), at places mixed with European silver fir ( Abies alba ). The endemic Rila oak ( Quercus protoroburoides ) inhabits only the Rilska River valley. The forests of coniferous zone between 1,600 m and 2,100 m consist of primarily of Norway spruce ( Picea abies ), Macedonian pine ( Pinus peuce ) и Scots pine ( Pinus sylvestris ). The sub-Alpine zone up to 2,500 m

11128-406: Was based on the dialect of Pannonia . It is generally held that the language was standardized by two Byzantine missionaries, Cyril and his brother Methodius , for a mission to Great Moravia (the territory of today's eastern Czech Republic and western Slovakia; for details, see Glagolitic alphabet ). The mission took place in response to a request by Great Moravia 's ruler, Duke Rastislav for

11235-613: Was coined, first by Saint Cyril himself and then by his students at the academies in Great Moravia and the First Bulgarian Empire , to denote complex abstract and religious terms, e.g., ꙁълодѣꙗньѥ ( zъlodějanьje ) from ꙁъло ('evil') + дѣти ('do') + ньѥ (noun suffix), i.e., 'evil deed'. A significant part of them wеrе calqued directly from Greek. Old Church Slavonic is valuable to historical linguists since it preserves archaic features believed to have once been common to all Slavic languages such as: Old Church Slavonic

11342-583: Was visited by about 100,000 tourists annually for the period 2000–2014 reaching a peak of 268,000 in 2012, while with a little more than 1 million visitors Rila Monastery Nature Park is the second most visited one in the country, after Vitosha . In 2000 on the south-western slopes was established the Dancing Bears Park Belitsa that shelters all dancing bears from Bulgaria following the ban of that practice, as well as individuals from Albania and Serbia. The abundant mineral springs along

11449-580: Was written with the Glagolitic alphabet , but later Glagolitic was replaced by Cyrillic , which was developed in the First Bulgarian Empire by a decree of Boris I of Bulgaria in the 9th century. Of the Old Church Slavonic canon , about two-thirds is written in Glagolitic. The local Serbian Cyrillic alphabet, known as Srbinčica , was preserved in Serbia and parts of Croatia , while

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