Buzuluksky Bor National Park
   HOME

TheInfoList



OR:

Buzuluksky Bor National Park (russian: Бузулукский бор) encompasses the Buzuluk Pine Forest, which is the largest grove of isolated high pine trees in the world. It is surrounded by
steppes In physical geography, a steppe () is an ecoregion characterized by grassland plains without trees apart from those near rivers and lakes. Steppe biomes may include: * the montane grasslands and shrublands biome * the temperate grasslands, ...
on the
East European Plain The East European Plain (also called the Russian Plain, "Extending from eastern Poland through the entire European Russia to the Ural Mountaina, the ''East European Plain'' encompasses all of the Baltic states and Belarus, nearly all of Ukraine, a ...
east of the
Volga River The Volga (; russian: Во́лга, a=Ru-Волга.ogg, p=ˈvoɫɡə) is the List of rivers of Europe#Rivers of Europe by length, longest river in Europe. Situated in Russia, it flows through Central Russia to Southern Russia and into the Cas ...
and west of the foothills running up to the southern
Urals The Ural Mountains ( ; rus, Ура́льские го́ры, r=Uralskiye gory, p=ʊˈralʲskʲɪjə ˈɡorɨ; ba, Урал тауҙары) or simply the Urals, are a mountain range that runs approximately from north to south through European ...
. This makes it an important habitat for scientific study, and is the site of the earliest forest management area in Russia. It is about 70 miles east from the city of
Samara, Russia Samara ( rus, Сама́ра, p=sɐˈmarə), known from 1935 to 1991 as Kuybyshev (; ), is the largest city and administrative centre of Samara Oblast. The city is located at the confluence of the Volga and the Samara rivers, with a population of ...
, and 15 km north of the town of
Buzuluk, Orenburg Oblast Buzuluk (russian: Бузулу́к) is a town in Orenburg Region, Russia, located on the Samara, Buzuluk, and Domashka Rivers, northwest of Orenburg and southeast of Samara. Population: History It was founded in 1736 as the fortress of ...
. About in size, Buzuluksky is a triangular patch of forest measuring roughly 53 km North-South, and 34 km West-East. It straddles the border of
Samara Oblast Samara Oblast ( rus, Сама́рская о́бласть, r=Samarskaya oblast, p=sɐˈmarskəjə ˈobləsʲtʲ) is a federal subjects of Russia, federal subject of Russia (an oblast). Its administrative center is the types of inhabited localitie ...
(Region) and
Orenburg Oblast Orenburg Oblast (russian: Оренбургская область, ''Orenburgskaya oblast'') is a federal subject of Russia (an oblast). Its administrative center is the city of Orenburg. From 1938 to 1957, it bore the name ''Chkalov Oblast'' () ...
(Region), with approximately half of its area in each. The park was officially constituted as a National Park in 2007, but has been a forestry management area since the early 1800s.


Topography

The park is bounded on the south by the
Samara River The Samara ( rus, Сама́ра, p=sɐˈmarə) is a river in Russia and a left-bank tributary of the Volga. It flows into the larger river at the city of Samara. Its largest tributary is the Bolshoy Kinel. It is long, and its drainage basin ...
, and on the other sides by non-forested steppes. The pine stand is surrounded by a thin band of broadleaf trees. The Borovka River flows southwest through the middle of the forest before emptying into the Samara at its southern end. The resultant river valley is about 100 meters in depth below the surrounding terrain. The sandy floodplain above the Borovka valley contains creeks and oxbow lakes. The Buzuluk pine stand occupies a large hollow filled with sandy sediments of marine genesis overlain by alluvial sands. The depth of the sands reaches 90 meters. At some points the river banks are made of red
sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) ...
s, conglomerates and
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
s of the
Permian The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleoz ...
and
Lower Triassic The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between Ma and Ma (million years ago). Rocks from this epoch are collectively known as the Lower Triassic Series, which is a un ...
.


Ecoregion and climate

The park is in the
Pontic–Caspian steppe The Pontic–Caspian steppe, formed by the Caspian steppe and the Pontic steppe, is the steppeland stretching from the northern shores of the Black Sea (the Pontus Euxinus of antiquity) to the northern area around the Caspian Sea. It extends ...
ecoregion, which is characterized by a
Temperate grasslands, savannas, and shrublands Temperate grasslands, savannas, and shrublands is a terrestrial biome defined by the World Wide Fund for Nature. The predominant vegetation in this biome consists of grass and/or shrubs. The climate is temperate and ranges from Semi-arid climate ...
biome A biome () is a biogeographical unit consisting of a biological community that has formed in response to the physical environment in which they are found and a shared regional climate. Biomes may span more than one continent. Biome is a broader ...
. The forest itself is thus out of character for the surrounding areas, with a forest canopy of conifers and deciduous trees. The climate is continental with hot summers and cold winters (
Koppen Koppen is a surname. Notable people with the surname include: * Dan Koppen (born 1979), American football offensive lineman * Erwin Koppen (1929–1990), German literary scholar * Luise Koppen (1855–1922), German author * Wladimir Köppen (1846 ...
BSk - Cold Semi-Arid Climates). This climate has large differences between the mean annual air temperature in winter (-13,8 °C in January) and summer (+20,4 °C in July). The average precipitation is 530 mm per year. The average length of snow cover is 169 days under the forest canopy, typically running from mid-November to mid-April. Surrounded by dry steppes, the forest creates a special mesoclimate in the area around it. Studies show that surrounding region experiences cooler temperatures, wetter soil, more variety of vegetation, and a greater covering by small groves of trees. These effects occur up to 20 km from the forest edge.


History

The forest was created by wind and water over the sand dunes of the ancient Caspian Sea, beginning several hundred thousand years ago. The area may have been the mouth of a larger river that flowed into the Caspian until the sea receded. Even today the forest overlays shifting sand dunes up to 30 m in depth. Until the early 1800s the area had extensive bogs and marshes which have been replaced by forest. A forestry management center was established in the early 1900s, and extensive experiments have been conducted in forestation of steppe environments since that time.


Tourism and use

There are hiking trails throughout the park, and areas from group meetings and camping in designated places. A museum displays historical and natural exhibits. The park's governmental charter emphasizes the protection of the habitat. Development is prohibited - no resource extraction, construction of building, trunk roads, disturbing of the geological or hydrological features. Hunting and fishing are prohibited, as are non-official motorized vehicles. Pets must remain on the common paths or designated areas.


Animals

The animal community of Buzuluksky reflects the combination of forest, steppe, and wetland habitats in close connection. The variety and quantity of plants support 55 mammal species -from the rodents such as squirrels and hamsters, to the smaller forest-dwelling animals (wolf, fox, badger, sandy, pine marten, ferret steppe, mink, ermine, weasel), up to large ungulates (moose, elk, wild boar, roe deer), and predators (including wolves that migrate through). One of the most valued animals is the badger, which each large numbers of larvae that are pests to the pine trees. Beaver re-appeared in the 1980s, and have built dams in the rivers and floodplain lakes. There are seven species of bats in the park, which feed on the forest insects and, like many birds, migrate away during the winter months. There are 155 different species of birds present, including birds of prey (owls, hawks and others) which feed on the rodents. Reflecting the various micro-haitats, there are waterfowl, forest birds, and bush nesters.


Recent events

The park comes under stress from the effects of recurrent drought, which dries the trees and creates favorable conditions for pine infestations. A wind-storm in 2010 felled almost 10% of the pine trees. In 2013, forest fires damaged more of the forest. There is oil under the Buzuluk park. Oil extraction was conducted in the forest from the 1950s to the 1970s, when a serious accident in 1971 led to the termination of drilling. There are currently about 160 capped oil wells in the park, some of which may be leaking. Proposals to explore in the area or to conserve the wells are currently being debated.


See also

National Parks of Russia There are currently 64 national parks in Russia. Together they cover approximately . Overview Until the 1960s only nature reserves and ''zakazniks'' existed in the Soviet Union, so international experience in creating a form of protected areas i ...


References


External links

* http://velobuguruslan.ucoz.ru/_bd/0/70766134.jpg Topographical Map of Buzuluksky NP, (VeloBuguruslan website) * https://www.youtube.com/watch?t=14&v=l1geLGDGmhg Video tour of Buzuluksky MP, YouTube {{authority control National parks of Russia Geography of Orenburg Oblast Geography of Samara Oblast