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Solovetsky Islands
The Solovetsky Islands (russian: Солове́цкие острова́), or Solovki (), are an archipelago located in the Onega Bay of the White Sea, Russia. As an administrative division, the islands are incorporated as Solovetsky District of Arkhangelsk Oblast, Russia.Law #65-5-OZ Within the framework of municipal divisions, they are incorporated as Solovetskoye Rural Settlement within Primorsky Municipal District.Law #258-vneoch.-OZ The administrative center of both divisions is the settlement of Solovetsky, located on Bolshoy Solovetsky Island. Almost all of the population of the islands lives in Solovetsky. As of the 2010 Census, the district had a population of 861 inhabitants. The Solovetsky Monastery (founded in 1436), in 1923 became the site of the first Gulag establishment, the Solovki prison camp. Geography The archipelago has a total area of and consists of six islands: * Bolshoy Solovetsky Island, * Anzersky Island (Anzer), * Bolshaya Muksalma, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bolshoy Solovetsky Island
Bolshoy Solovetsky Island (russian: Большой Соловецкий остров), or simply Solovetsky Island (russian: Соловецкий остров) is the biggest island of the Solovetsky Islands archipelago in the White Sea, northern Russia. The island is home to Solovetsky Monastery, a medieval monastery and a fortress included in the World Heritage list. Location and geography The island is located on the southwestern side of the archipelago. To the east of Solovetsky Island there are Anzersky Island and Bolshaya Muksalma Island. From the Bolshaya Muksalma side, a bay, Dolgaya Bay (russian: Долгая Губа), several kilometers long, is connected by a narrow passage to the White Sea. Another bay in the north of the island is Sosnovaya Bay (russian: Сосновая Губа). Solovetsky and Anzersky islands are separated by the Anzerskaya Salma strait, and Solovetsky and Bolshaya Muksalma islands are separated by two straits: Severnye Zheleznye Vorota and Yuzhn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Solovki Prison Camp
The Solovki special camp (later the Solovki special prison), was set up in 1923 on the Solovetsky Islands in the White Sea as a remote and inaccessible place of detention, primarily intended for socialist opponents of Soviet Russia's new Bolshevik regime. The first book on the Gulag, namely, '' In the Claws of the GPU'' (1934) by Francišak Aljachnovič, described the Solovki prison camp. At first, the Anarchists, Mensheviks and Socialist Revolutionaries enjoyed a special status there and were not made to work. Gradually, prisoners from the old regime (priests, gentry, and White Army officers) joined them and the guards and the ordinary criminals worked together to keep the "politicals" in order. This was the nucleus from which the entire Gulag grew, thanks to its proximity to the first great construction project of the Five-Year Plans, the White Sea–Baltic Canal. In one way, Solovki and the White Sea Canal broke a basic rule of the Gulag: they were both far too close to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Labyrinths Of Bolshoi Zayatsky Island
The stone labyrinths of Bolshoi Zayatsky Island are a group of 13 or 14 labyrinths on Bolshoy Zayatsky Island, one of the Solovetsky Islands in Arkhangelsk Oblast, Russia. Lacking standard archaeological study, a research group from St. Petersberg theorize that the labyrinths are about 2500 years old, according to their orientation, their supposed ritual use, and changes in the direction of the zenith on the solstice throughout history. Most researchers doubt that they are that old; the vast majority of labyrinths in this area date at the earliest to the Middle Ages. Apart from the labyrinths, there are more than 850 heaps of boulders on Bolshoi Zayatsky Island, plus numerous other stone settings such as a stone symbol with radial spokes, possibly representing the sun. All the labyrinths are concentrated in an area of 0.4 km2 on the western part of the island. Another enormous complex of stone settings on Sopka Hill, in the eastern part of the island, does not include any lab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norway Spruce
''Picea abies'', the Norway spruce or European spruce, is a species of spruce native to Northern, Central and Eastern Europe. It has branchlets that typically hang downwards, and the largest cones of any spruce, 9–17 cm long. It is very closely related to the Siberian spruce (''Picea obovata''), which replaces it east of the Ural Mountains, and with which it hybridizes freely. The Norway spruce has a wide distribution for it being planted for its wood, and is the species used as the main Christmas tree in several countries around the world. It was the first gymnosperm to have its genome sequenced. The Latin specific epithet ''abies'' means “like ''Abies'', Fir tree” Description Norway spruce is a large, fast-growing evergreen coniferous tree growing tall and with a trunk diameter of 1 to 1.5 m. It can grow fast when young, up to 1 m per year for the first 25 years under good conditions, but becomes slower once over tall. The shoots are orange-brown and glabrous. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scots Pine
''Pinus sylvestris'', the Scots pine (UK), Scotch pine (US) or Baltic pine, is a species of tree in the pine family Pinaceae that is native to Eurasia. It can readily be identified by its combination of fairly short, blue-green leaves and orange-red bark. Description ''Pinus sylvestris'' is an evergreen coniferous tree growing up to in height and in trunk diameter when mature, exceptionally over tall and in trunk diameter on very productive sites. The tallest on record is a tree over 210 years old tree growing in Estonia which stands at . The lifespan is normally 150–300 years, with the oldest recorded specimens in Lapland, Northern Finland over 760 years. The bark is thick, flaky and orange-red when young to scaly and gray-brown in maturity, sometimes retaining the former on the upper portion.Trees for LifeSpecies profile: Scots pine/ref> The habit of the mature tree is distinctive due to its long, bare and straight trunk topped by a rounded or flat-topped mass of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Relief
Relief is a sculptural method in which the sculpted pieces are bonded to a solid background of the same material. The term ''relief'' is from the Latin verb ''relevo'', to raise. To create a sculpture in relief is to give the impression that the sculpted material has been raised above the background plane. When a relief is carved into a flat surface of stone (relief sculpture) or wood (relief carving), the field is actually lowered, leaving the unsculpted areas seeming higher. The approach requires a lot of chiselling away of the background, which takes a long time. On the other hand, a relief saves forming the rear of a subject, and is less fragile and more securely fixed than a sculpture in the round, especially one of a standing figure where the ankles are a potential weak point, particularly in stone. In other materials such as metal, clay, plaster stucco, ceramics or papier-mâché the form can be simply added to or raised up from the background. Monumental bronze reliefs a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Onega Peninsula
The Onega Peninsula is located in Arkhangelsk Oblast, Russia. It protrudes into the White Sea, with Onega Bay to the south-west, and Dvina Bay to the north-east. The length of the peninsula is about , and the width varies between and . Geography The coastal area of the peninsula is populated. The villages (counterclockwise) of Nyonoksa, Syuzma, Krasnaya Gora, Pertominsk, Unsky, Yarenga, Lopshenga, Letny Navolok, Letnyaya Zolotitsa, Pushlakhta, Lyamtsa, Purnema, and Nizhmozero are all located at or near the coast. The north-eastern coast of the peninsula is crossed by the Una Bay, a gulf in the Dvina Bay, which is about long. The villages of Una and Luda are located at the inner coast of the Una Bay. The interior of the peninsula (north-west of the line connecting Luda and Purnema) is a wilderness without any permanent population. There is some logging at Verkhneozersk, south-east of Luda. The interior of the peninsula is hilly, and there are many lakes, the biggest of which are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bolshoy Zayatsky Island
Bolshoy Zayatsky Island (Russian: Большой Заяцкий Остров (Great Hare Island)) is an island in the White Sea. It is one of six major islands comprising the Solovetsky archipelago. The island is famous for its history and nature. In prehistoric times, the island was used as a sanctuary by the indigenous coastal population. In the mid-16th century monks of the Solovetsky monastery organized a transit port on this island that later grew into the St. Andrew hermitage. Nowadays, the island is a protected territory with historical memorials of various periods. Since 1992 it has been listed as a UNESCO World Heritage Site as a part of the Solovetsky monastery complex. Geography Bolshoy Zayatsky island is located 2 km southwest from the central island of the archipelago. Its surface is . Just like other islands of this region, it was formed approximately 9000 years ago by a retreating glacier. The island has typical features of tundra landscape, however it is located ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bolshaya Muksalma
Bolshaya Muksalma () is one of the Solovetsky Islands. Bolshaya Muksalma is situated to the east of Bolshoy Solovetsky Island and is separated from it by two straits: Severnye Zheleznye Vorota and Yuzhnye Zheleznye Vorota (literally translated as Northern and Southern Iron Gates). The Yuzhnye Zheleznye Vorota Strait is crossed by a dam which was built by the monks of Solovetsky Monastery between 1865 and 1871 and now connects the two islands. The dam is several hundred meters long and wide. Southeast of Bolshaya Muksalma, there is Malaya Muksalma Island, as well as a number of tiny islets. The area of Bolshaya Muksalma is . In terms of the area, this is the third island of the archipelago behind Bolzhoy Solovetsky and Anzersky Islands. There is archaeological evidence that the island was populated in the second millennium BC. In historical time, Bolshaya Muksalma was made the location of the farm serving Solovetsky Monastery, as keeping female animals in close proximity to the mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_01.JPG "Click for more on -> Relief")
