Kolsky Uyezd
Kolsky Uyezd (russian: Ко́льский уе́зд) was an administrative division (an uyezd) of the Tsardom of Russia and later of the Russian Empire. History 16th–17th centuries Russian expansion to the Kola Peninsula can be traced to the early 16th century when the Russian monk Trifon founded an Orthodox monastery at Pechenga.''A Short History of Finland'', pp. 36–37 Later in 1556, Ivan the Terrible, by his own will, gave the monastery a large part of land on the peninsula. This land covered territories which Norway—then a part of the kingdom of Denmark–Norway—traditionally considered as their own. Consequently, Frederick II, the King of Denmark–Norway, sent two expeditions in the 1580s and in 1586 to give up the peninsula. His claims were, however, contested by Sweden, then the major power in the Baltic region. At first, Sweden extracted the Kola Peninsula from both Russia and Denmark–Norway in a series of wars and resulting treaties. However, i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Map Of Alexandrovsky Uyezd (1913)
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, while others are dynamic or interactive. Although most commonly used to depict geography, maps may represent any space, real or fictional, without regard to context or scale, such as in brain mapping, DNA mapping, or computer network topology mapping. The space being mapped may be two dimensional, such as the surface of the earth, three dimensional, such as the interior of the earth, or even more abstract spaces of any dimension, such as arise in modeling phenomena having many independent variables. Although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'the world'. Thus, "map" became a shortened term referring to ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lovozero (rural Locality)
Lovozero (russian: Лово́зеро; sjd, Луяввьр; sms, Luujäuʹrr; se, Lujávri; fi, Luujärvi) is a rural locality (a '' selo'') and the administrative center of Lovozersky District in Murmansk Oblast, Russia, located on both banks of the Virma River, which is not far from Lake Lovozero, and southeast of Murmansk, the administrative center of the oblast. Population: It is the second largest locality in the district after Revda. History In 1574, the settlement of Loyyavrsiyt (literally, "settlement of strong people by the lake") was founded at the site of modern Lovozero. Lovozero itself is first mentioned in chronicles in 1608. Economy The main business in Lovozero is the agricultural and reindeer husbandry cooperative ''Tundra''. Fishing, hunting, and picking cloudberries are also important. Transportation The closest railway station is in Revda, located to the west. Military A military helicopter base is located to the southeast. Culture Sev ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pogost
''Pogost'' (russian: погост, from Old East Slavic: погостъ) is a historical term with several meanings in the Russian language. It has also been borrowed into Latgalian (''pogosts''), Finnish (''pogosta'') and Latvian (''pagasts''), with specific meanings. The original usage applies to the coaching inn for princes and ecclesiastics with the word being similar to modern Russian ''gost (гость), "guest". It is assumed that originally ''pogosts'' were rural communities on the periphery of the ancient Rus` state, as well as trading centers (Old Russian: ''gost'ba'', гостьба). In the end of the 10th century ''pogosts'' transformed into administrative and territorial districts. ''Pogosts'' varied in size, ranging from tens to hundreds of villages in 11th—14th centuries. As Christianity spread in Russia, churches were built in ''pogosts''. In 1775 the last ''pogosts'' that served as administrative districts were destroyed. Since then they became known as ci ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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65th Parallel North
The 65th parallel north is a circle of latitude that is 65 degrees north of the Earth's equatorial plane. It crosses the Atlantic Ocean, Europe, Asia and North America. At this latitude the sun is visible for 22 hours, 4 minutes during the summer solstice and 3 hours, 35 minutes during the winter solstice. Around the world Starting at the Prime Meridian and heading eastwards, the parallel 65° north passes through: : See also *64th parallel north *66th parallel north The 66th parallel north is a circle of latitude that is 66 degrees north of the Earth's equatorial plane, about 61 km south of the Arctic Circle. It crosses the Atlantic Ocean, Europe, Asia and North America. This latitude also roughly c ... {{geographical coordinates, state=collapsed n65 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kandalaksha
Kandalaksha (russian: Кандала́кша; fi, Kantalahti, also ''Kandalax'' or ''Candalax'' in the old maps; krl, Kannanlakši; sms, Käddluhtt) is a town in Kandalakshsky District of Murmansk Oblast, Russia, located at the head of Kandalaksha Gulf on the White Sea, north of the Arctic Circle. Population: 40,564 ( 2002 Census); History The settlement was founded the 11th century but may have existed as a temporary stop for fisherman from the 9th century. In the 13th century, it became a part of the Novgorod Republic along with the southern part of the Kola Peninsula, and in 1478 was annexed by the Grand Duchy of Moscow. In 1915, the construction of a seaport started, and in 1918 a railroad connecting Moscow to Murmansk running through Kandalaksha was opened. On August 29, 1927, Kandalaksha was made the administrative center of the newly established Kandalakshsky District,''Administrative-Territorial Division of Murmansk Oblast'', p. 35 and on June 1, 1932, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Leshya Lapps
''Lesya'', according to the Jain theory of karma, is the coloring of the soul on account of its association with the karmic matter. The colour of ''leśyā'' varies from person to person depending on the psychic states and mental activities behind an action. The coloring of the soul is explained through the analogy of crystal, that acquires the color of the matter associated with it. In the same way, the soul reflects the qualities of colour, taste, smell and touch of associated karmic matter, although it is usually the colour that is referred to when discussing the ''leśyās.'' Paul Dundas notes the key text expressing this Jain doctrine, explaining how the literary form of the text is helpful in dating and reconstructing the history of transmission. A full statement of the theory of ''lesya'' occurs in chapter 34 of the Uttaradhyayana, one of the fundamental ''sutras'' of the scriptural canon. Inspection of the metrical structure there, which consists of a cluster of old ''sl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Turiy Peninsula
Turiy Peninsula (russian: Турий полуостров) is peninsula located in Murmansk Oblast, Russia. It is the biggest peninsula on the south of Kola Peninsula. It protrudes into the White Sea The White Sea (russian: Белое море, ''Béloye móre''; Karelian and fi, Vienanmeri, lit. Dvina Sea; yrk, Сэрако ямʼ, ''Serako yam'') is a southern inlet of the Barents Sea located on the northwest coast of Russia. It is s ..., with Sosnovaya Bay to the west, and Karzh Bay to the east. Sources Map of Turiy peninsula Peninsulas of Murmansk Oblast {{MurmanskOblast-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |