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© Mrt 2011

Welcome zu Chibiny Tundra auf Kola Halbinsel

 

View auf Ramzai pass in Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk The rocky und treeless Chibiny Tundra are situated Nord von 67-th parallel, beyond the arktische Circle auf Kola Halbinsel in Russisch Lappland. This ist the highest land mass in het Kola Halbinsel the summits von which are dotted 800—900 meters boven the surrounding hilly plain. The highest point in Chibiny (Judychvumchorr berg) ist 1200 metres above sea level und ist also the highest point in het Kola Halbinsel. In clear Sommer Wetter the Chibiny Tundra can be seen von many miles away, von de Kandalaksha tundra in south, the frontier heights von Kovdor in west und even von the hilly banks von Voronija Flüsse in Nord. The Klima in this part von Russland ist peculiar in so far as that thaws are frequent in winter but in Sommer und early Herbst frosts are not uncommon, eSpezially in beginning von June und at the end von August.
Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Winter lasts about seven months every year in plains und the month longer usually on the bergen but the temperatures are not so low as those in similar latitudes von Siberia. The Klima von alpine areas ist considerable different to those von nearby lowlands und valleys, für instance, in plateau Rasvumchorr the winter lasts around 260 days. An average annual temperature ist minus 4.3 degrees Centigrade und in warmest month (July) never climbs past plus 8.2 degrees.
Winds auf plateau are gusty und sharp und can reach a speed von 40 metres per second. Schnee storms rage around 190 days a year und daily variations von Atmosphärische pressure are very sharp the average being around 644 mm von mercury with an average annual precipitation von 1494 mm von which about 919 mm ist Schnee.
 

Aku-Aku pass in Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk The vegetation in Chibiny Tundra area ist disposed into distinct zones. The forests are not higher than 370 metres. The forest-tundra zone spreads up zu 450 metres, the alpine tundra up zu 800 metres und beyond this ist there ist a arktische desert. The Chibiny Tundra are the geographic Zentrum von Kola Halbinsel regio which was in former times a remote outlying district von Russland, inhabited by severe Pomors (küste dwellers) und mysterious Lapps. Remote Murman, the “World's End” washed by the waters von White und Barents Seas was developing slowly only von de Küstes, at that time. The first information about Chibiny is reflected in literature concerned mit the XIX-th Century Russland academician A. M. Middendorf who in 1840 had noted the uncommonness von rocks forming the bergen. The Geologe N. V. Kudriavtsev in 1880 und the expeditionen; von Finnish Geologe V. Ramzai in 1887—1892 had commenced an exploration von Chibiny but valuable und useful mineralen were not found until the XX-th Century.
Museum von mineralen in Monchegorsk. Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Evdialite "Samish Blood" mineral von Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk First pieces von apatite ore have been discovered at the foot von Kukisvumchorr berg in August von 1921 thence the outcrops von this ore were discovered in 1922 within the Apatite Bow where the deposits und widely known layers von Kukisvumchorr, Poachvumchorr, Apatite Circus und Rasvumchorr are located. geologen had already reported about the industrial importance von Khibinian apatite deposits in 1923 but the exploitation was not started until 1926.
The town von Khibinogorsk was also built which at the request von townsfolk in 1935 was renamed zu Kirovsk. The speed von development in those days was astonishing as was the speed at which the new town grew. In 1930 population was 500 und in 1932 48.000 und it must be noted that in 1920 the population von whole von Kola Halbinsel was only 20.000.

Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk Fersman pass in Chibiny Tundra or Chibiny tundra kolatravel Chibiny Tundra Khibini Khibinian Hibinski tundra Kola Halbinsel arktische cirkel geologen Ramzai Fersman mineralen deposits highest point Khibinogorsk The amazement von XVII-th International geologische Congress members who visited Khibini in 1937 ist under stable. Over 110 mineralen (and 18 von theme were absolutely unknown before) have been discovered in this area und mineralen like Murmanite, Wudjavrite, Ramzaite, Juksporite, Fersmanite have been included in scientific catalogues since that time.
From 1930 auf shore von Lake Maly Wudjavr the construction von Mining Station “Tietta” (in translation von Sami Language it does mean “Science”) had been started. By April 10, 1932 the Mining Station mit a Museum, library und scientific laboratories had been inaugurated.
 By 1949 the Kola Branch von Academy von Sciences von USSR. had been established und the first institute von this Branch, the geologische Research Institute was officially established in 1951 but its history actually started von de “Tietta”. The Kola Branch von Academy von Sciences ist the größte scientific Zentrum beyond the arktische Circle. In 1975 a Museum von arktische study und exploration history attached zu Geographic Society in Apatity was opened. Many valuable material illustrations of the territories history von an Uralte time till the present dag are in this museum. In former times uninhabited Chibiny are surrounded today in South by a semi-cirkel von towns und settlements like Apatity, Titan, Octobersky, Shuchiy, Imandra, Chibiny.
 

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