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Vyzhnytsia National Nature Park
Vyzhnytsia National Nature Park is a protected area in south-western Ukraine which administration is located in the town Berehomet. The park has 87 employees with 6 of them working in the scientific section and 29 in the security service. The park was created for the conservation, restoration and sustainable use of natural landscapes of Bukovyna Carpathian with its unique historical and cultural complexes.
==Nature conditions==
It is one of the smallest National Parks in the Ukrainian Carpathians. Vyzhnytsia park represents a lowland part of the Carpathians with a fairly mild climate. Thermophilic species – beech and fir dominate in the woods. The park is situated on the edge of the Outer Carpathians and the Precarpathian region. In the area of lowland Pokuttya-Bukovyna Carpathian terrain the mountain ranges are low, have smoothed peak crests, and only Smydovatyi ridge in the southern part of the park can be attributed to middle elevations of 1000 m or more above sea level. Overall the relief of the national park characterizes with soft contours, due to low resistance against denudation of flysch sediments, that compose it. Sharp terrain forms and slopes over 45 - 50° occur only in the western part of Cheremosh river in places of sandstones and erosional downcutting of riverbeds. Sometimes there are landslides and small sized screes. The landscape diversity of the park is determined by the affiliation to the basins of Cheremosh river and Siret river. Eastern part, where the Siret flows has more smoothed contours of mountain ridges, broad valleys of tributaries, fewer geological delaminations. The western part, where Cheremosh River flows is much more intensively dissected. It is the reason why steep slopes with outcrops of geological rocks, scenic cliffs, numerous waterfalls, gorges-gate are common here.
The climate in the National Park is temperate continental, with ample and abundant moisture, not hot summers, mild winters and warm autumns. There are significant microclimatic differences between the two parts of the park, Siretska and Cheremoshska (generally, Cheremoska part is noticeably warmer) and within these areas - between the slopes of the southern and northern exposures. Usually in winter on the northern slopes is held a steady thick snow cover, while on its southern part there is no snow.
The soil cover varies greatly because of its geomorphological and climatic differences within its territory
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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