Journey to Kamchatka | A glimpse of our 14 days adventure in Kamchatka

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• published: 02 Feb 2016
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Credit Music: "Newborn Dream" by soundroad - http://bit.ly/1Pp1JtA __ More Videos: Kamchatka - https://www.youtube.com/playlist?list=PLWMMZOvBcqdxLjBolZonISjPp201kcL4j __ The Kamchatka Peninsula (Russian: полуо́стров Камча́тка, Poluostrov Kamchatka) is a 1,250-kilometre-long (780 mi) peninsula in the Russian Far East, with an area of about 270,000 km2 (100,000 sq mi).[1] It lies between the Pacific Ocean to the east and the Sea of Okhotsk to the west.[2] Immediately offshore along the Pacific coast of the peninsula runs the 10,500-metre (34,400-ft) deep Kuril–Kamchatka Trench. The Kamchatka Peninsula, the Commander Islands, and Karaginsky Island constitute the Kamchatka Krai of the Russian Federation. The vast majority of the 322,079 inhabitants are ethnic Russians, but there are also about 13,000 Koryaks (2014).[3] More than half of the population lives in Petropavlovsk-Kamchatsky (179,526 people in 2010) and nearby Yelizovo (38,980). The Kamchatka peninsula contains the volcanoes of Kamchatka, a UNESCO World Heritage Site. Kamchatka receives up to 2,700 mm (110 in) of precipitation per year. The summers are moderately cool, and the winters tend to be rather stormy though rarely producing lightning. Politically, the peninsula forms part of Kamchatka Krai. The southern tip is called Cape Lopatka. The circular bay to the north of this on the Pacific side is Avacha Bay with the capital, Petropavlovsk-Kamchatsky. North up the Pacific side, the four peninsulas are called Shipunsky Point, Kronotsky Point, Kamchatsky Point and Ozernoy Point. North of Ozernoy is the large Karaginsky Bay, which features Karaginsky Island. Northeast of this (off the displayed map) lies Korfa Bay with the town of Tilichiki. On the opposite side is the Shelikhov Gulf. The Kamchatka or Central (Sredinny) Range forms the spine of the peninsula. Along the southeast coast runs the Vostochny or Eastern Range. Between these lies the central valley. The Kamchatka River rises northwest of Avacha and flows north down the central valley, turning east near Klyuchi to enter the Pacific south of Kamchatsky Point at Ust-Kamchatsk. In the nineteenth century a trail led west from near Klychi over the mountains to the Tegil river and town which was the main trading post on the west coast. North of Tegil is Koryak Okrug. South of the Tegil is the Icha River. Just south of the headwaters of the Kamchatka, the Bistraya River curves southwest to enter the Sea of Okhotsk at Bolsheretsk, which once served as a port connecting the peninsula to Okhotsk. South of the Bistraya flows the Golygina River. There is a road from Bolsheretsk to Petropavlovsk and another from this road up the central valley (with a bus service) to Ust-Kamchatsk. The northern end of the road is of poorer quality. Apart from the two roads, transport is by small plane, helicopter, four-wheel drive truck and army truck. The obvious circular area in the central valley is the Klyuchevskaya Sopka, an isolated volcanic group southeast of the curve of the Kamchatka River. West of Kronotsky Point is the Kronotsky Biosphere Reserve with the Valley of Geysers. At the southern tip is the Southern Kamchatka Wildlife Refuge with Kurile Lake. There are several other protected areas: Palana is located in the Koryak area on the northwest coast. Climate Although Kamchatka lies at similar latitudes to Great Britain, cold arctic winds from Siberia combined with the cold Oyashio sea current see the peninsula covered in snow from October to late May. Under the Köppen climate classification Kamchatka generally has a subarctic climate (Dfc) but higher and more northerly areas have a polar climate (ET). Kamchatka is much wetter and milder than eastern Siberia, and is essentially transitional from the hypercontinental climate of Siberia and northeast China to the rain-drenched subpolar oceanic climate of the Aleutian Islands. Opala volcano in the southern part of Kamchatka. There is considerable variation, however, between the rain-drenched and heavily glaciated east coast and the drier and more continental interior valley. In the heavily glaciated Kronotsky Peninsula, where maritime influences are most pronounced, annual precipitation can reach as high as 2,500 millimetres (98 in), whilst the southeast coast south of Petropavlovsk-Kamchatsky generally receives around 1,350 millimetres (53 in) of rainfall equivalent per year. Considerable local variations exist: southern parts of the Petropavlovsk-Kamchatsky metropolitan area can receive as much as 430 millimetres (17 in) more than the northern part of the city. Temperatures here are very mild, with summer maxima no higher than 15 °C (59 °F) and winter lows around −8 °C (18 °F), whilst diurnal temperature ranges seldom exceed 5˚C (9˚F) due to persistent fog on exposed parts of the coast. South of 57˚N there is no permafrost due to the relatively mild winters and heavy snow cover, whilst northward discontinuous permafrost prevails.