Avala
Avala is a mountain in Serbia, overlooking Belgrade. It is situated in the south-eastern corner of the city and provides a great panoramic view of Belgrade, Vojvodina and Šumadija, as the surrounding area on all sides is mostly lowlands. It stands at above sea level, which means that it enters the locally defined mountain category just by.
Location
Avala is located south-east of downtown Belgrade. The entire area of the mountain belongs to the Belgrade City area, the majority of it being in the municipality of Voždovac, with the eastern slopes being in the municipality of Grocka, and the southernmost extension in the municipality of Sopot. It is possible that in the future the entire area of Avala would create a separate municipality of Belgrade, named Avalski Venac.Geography
Avala is a low type of the Pannonian island mountain, though it is actually the northernmost mountain in Šumadija. Until 600,000 years ago, when the surrounding low areas were flooded by the inner Pannonian Sea, Avala was an island, just as the neighboring mountains, thus earning its geographical classification. However, Avala remains an "island mountain" as the area around it, Pinosava plateau of the northern Low Šumadija, is low and mostly flat. In the north it extends into the woods of Stepin Lug.The mountain is built of serpentinite, limestone and magmatic rocks, which are injected in the shape of cone. Other peaks include Ladne vode, Zvečara, Sakinac. The Avala had deposits of ores, most notably lead and mercury's ore of cinnabarite and mining activities which can be traced to the pre-Antiquity times. Other metals mined on the mountain include silver, gold and zinc. At the Šuplja Stena localities, seven quartz-carbonate veins with minerals and cinnabarite ore were discovered, with 13 additional between Šuplja Stena and Topčiderka river.
Avala is also a location where the mineral avalite, named after the mountain, was found. A greenish mineral, chromian, magnesian or potassic aluminosilicate, it was discovered by Serbian chemist Sima Lozanić who established its formula. Optically examined by the Israeli mineralogist Tamir Grodek who classified it as a member of the mica mineral group.
On the southern slopes, in the area of Ripanj, the closed Tešićev Majdan is located. The stone pit was privately owned, but was confiscated by the state after World War II and stopped operating before 1960. In the process of restitution after 2000, the quarry was returned to the surviving owners, but they live abroad so the quarry is still not operational. It is the only known location of kersantite in Serbia, a rare type of greenish granite. For decades, kersantite was used for Belgrade buildings. Features built with this stone include the fountain between the Novi Dvor and Stari Dvor, the bordure of the Hotel Bristol, Small Staircase in Kalemegdan Park, pedestal of the Play of Black Horses statues in front of the House of the National Assembly of Serbia and buildings of Belgrade Cooperative, Elementary School King Petar I, Cathedral Church of St. Michael the Archangel and Main Post Office Building. As the buildings began to deteriorate over time, city authorities showed interest in the quarry, not only for the repairs but also for future construction. For now, when some deteriorated kersantite feature has to be replaced, the artificial stone is used. Geologists suggested to the city to obtain the ownership over the land on which the pit is located and to reopen it. The Belgrade City government announced in 2012 that it will unilaterally explore the pit until it gets reopened and inspected it in 2013. Large amounts of already cut kersantite were found. Locals have been illegally extracting the stone and crushing it to use as road cover. After the political change in Belgrade in late 2013, the motion was dropped.
On the mountain itself, there are several springs, of which Sakinac is best known. Despite being the only mountain in the area, Avala is not a source of many rivers. The Topčiderka river, originating in the woods of Lipovička šuma on the south-west, flows on the western slopes of Avala, while the river Bolečica flows on the eastern slopes. Other minor flows include the Vranovac, a tributary to the Bolečica. A small artificial lake near the village of Pinosava was created on the western slope of the mountain. The settlements in the area are notorious for problems with shortages of drinking water during summer.
Wildlife
Protection
The mountain has been protected since 1859 as a natural monument, or, by the modern standards, "sight of the exquisite values". That year, Serbian ruling prince Miloš Obrenović issued an order for the Avala to get fenced and protected that way. He also banned construction of houses on the mountain itself.In the early 20th century, plans were made for further forestation of the mountain. In his last visit to Serbia in 1903, Austro-Hungarian naturalist Felix Philipp Kanitz noted that the mountain would become "another exceptional excursion area", after the Topčider park. Remains of the medieval Žrnov were removed in 1934 to make way for the Monument to the Unknown Hero. The destruction of Žrnov, which was demolished with dynamite, caused massive discontent among the citizens of Belgrade. In the period of the Kingdom of Yugoslavia, the mountain was declared a national park, in 1936. In 1946, by the ukaz of the Presidium of the National Assembly of Serbia, Avala was reduced to the status of the "public property of general benefit" and placed under direct management of the Government of Serbia.
Despite being officially protected for almost 150 years, it was only in 2007 that preservation plans for the mountain were made. That way, Avala entered a circle of protected green areas of Belgrade, which also included the mountain of Kosmaj, the island of Veliko Ratno Ostrvo and the woods of Stepin Lug, with the forests of Košutnjak and Topčider to be added next. Protected areas of Avala spread over
Some areas within the mountain are additionally protected., including the "Complex of mountain beech, oak, maple and elm", which is in the first level of protection. It is located in the valley of the Vranovica stream, close to the "Čarapićev Brest" visitors' complex.
In early September 2020, unknown persons began clearing the field in the protected downhill of Avala. The field was a recorded habitat of Caspian whipsnake. Illegal construction of the complex of houses, without any permits, began in January 2021. Inspections closed it, but the construction continued before it was halted. Demolition of the complex began in August 2022.
Plant life
Avala is known for its diverse plant life, despite not being a tall mountain. There are over 600 plant species living on the mountain. Some of them are protected by the law as natural rarities, like certain types of laburnum, box tree, black broom, common holly and martagon lily. The area is also abundant in medicinal herbs, like the early-purple orchid and belladonna. Almost 70% of Avala is forested, or. Thus, the meadow plant communities are rare. Other protected plant species include common yew and oregano. High woods mostly consist of durmast oak, Turkey oak, hornbeam, beech, linden, black pine, black locust and other trees.Animal life
Almost 100 species of birds live on Avala, including strictly protected Eurasian sparrowhawk, European honey buzzard and European green woodpecker. Total of 21 bird species is protected. Other species include common buzzard, stock dove, common kestrel, and Eurasian scops owl.A section of the mountain is organized as a game hunting ground.
Name
In the Middle Ages, the town of Žrnov or "Avalski Grad" was located on top of Avala. In 1442. it was conquered by the Ottoman Empire, which built a new town in Žrnov's place as a counter-fortress to the Belgrade city fort, and renamed it "havale", which originally comes from Arabic and means "obstacle" or "shelter".Human history
Mining
Archeologist Miloje Vasić believed that the vast mines of cinnabarite on Avala were crucial for the development of the Vinča culture, on the banks of the Danube circa 5700 BC. Settlers of Vinča apparently melted cinnabarite and used it in metallurgy. Mining was active on the mountain at 3000 BC. However, it is still contested when people began mining on Avala, from the Neolithic, to the earnest mining by the Celtic Scordisci, prior to Roman conquest. There are three major mines, Šuplja Stena, Crveni Breg and Ciganlija, the first being the most explored.Vasić also claimed that Vinča hosted a Ionian trade colony from the Aegean around 6000 BC, and that Ionian seamen discovered primitive mine in Šuplja Stena. The Ionians continued to mine cinnabarite and with their final departure from Vinča, the mine stoppe working until being partially revived by the Celts. Pots with mercury were discovered in Šuplja Stena, but not the smelting artefacts or slag. A vast number of potteries discovered in Vinča was internally glazed with cinnabarite, with some quartz and phyllosilicates. Examination showed that it matches materials from Avala. Vinča developed c.5700 BC, Vladimir Milojević claim the production for certain from 2000 BC to 750 BC without being able to say when the mining began. Remains from both the Neolithic and the last Ice Age are also discovered in the cave.
It is still debated whether Šuplja Stena is a natural cave or was completely dug for the mining purposes. Remains of the Neanderthal culture were discovered in it. In his 1943 Prehistoric mine Šuplja Stena on Avala hill near Belgrade , Vladimir Milojčić said that the "cave is old as Avala", formed by the volcanic activity and elevation of the terrain. The cave was first used by the wild animals and later by the prehistoric peoples, with animal and human remains, and prehistoric mining artefacts have been discovered. However, geographer Dragan Petrović in his work on the caves of Šumadija, lists caves on the present Belgrade's territory, but makes no mention of Šuplja Stena.
In Medieval Serbia mining on Avala began in c.1420, after the Law on mines was issued by the Despot Stefan Lazarević in 1412. In this period, the cinnabarite was used for fresco paintings and was exported to Greece. Mining activities ceased by the 1960s, when the last two mines, Šuplja Stena and Crveni Breg, were closed. Šuplja Stena was a mercury mine while in Crveni Breg, lead, zinc, silver and gold were extracted. Crveni Breg was closed in 1953 and has traces of the usage from the Roman period. It has seven levels, out of which four are flooded, and the stalactites are being formed inside. By 2009 the upper level was prepared for visitors, having been cleaned and lighted for some, but the project of turning it into a tourist attraction failed.
The survey of the Crveni Breg began in 1870, and the mine was opened in 1886. Lead, zinc and silver were mined. It was intermittently operational till 1901 when it was purchased by the Belgian company from the previous Serbian owners. Operational again from 1902, it was sold to the French owners in 1906. It worked until 1941, and in this period 18,800 tons of ore was extracted. It was reopened in 1948 and closed in 1953. 55,000 tons of ore was extracted in this period, containing lead, zinc, silver, gold and copper. Along the road to Mladenovac there is the Ciganlija mine, with numerous smaller horizontal pits covered with overgrowth. Next to the mine is Zavljak stream, where remains of the slag dated to Antiquity were discovered. The slag contains lead, zinc, copper and silver.
The ore in Šuplja Stena was rediscovered in 1882, and in 1883 survey began with digging of the "Jerina" horizontal pit. By 1886, horizontal pit "Prečica" with smelters, was also finished. During this period, numerous pits and shafts were dug, with being dug only in 1891. From 1884 to 1889 it was majority owned by Đorđe Vajfert, when he sold it to an English firm, but continued to manage works. The ore was exported to Vienna, London and China. Though officially closed in 1893, the mine was extracting ore only from 1887 to 1891. From 1889 to 1890 some 30 tons of mercury was sold. The survey of Šuplja Stena was continued in 1910 and, with interruptions, lasted until 1959, while the preparatory works for the reopening began in 1967. Smelters was built, the production continued in 1968 and until spring 1972 when it was finally closed, the mine produced 80 tons of mercury. Mine in Šuplja Stena is considered one of the best explored one, in geological, chemical, mineralogical and mining sense.