RELIEF AND GEOLOGICAL STRUCTURE OF CARPATHIAN BIOSPHERE RESERVE

Y. Kravchuk, V. Brusak
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Abstract

The relief and geological structure of Carpathian Biosphere Reserve represent the features of the geological and geomorphological structure of the four geomorphological regions of the Ukrainian Carpathians. The block mid-mountains of the Polonynsko-Chornohirsky Carpathians (Chornohora, Svydovets, and Uholsko-Shyrokoluzhansky massifs) and the folded mid-mountains of Marmarosy crystal massif (Marmarosy and Kuziy-Trybushansky massifs) are well protected within the reserve. The analysis of the morphostructure and morphosculpture of the reserve is carried out taking into account the longitudinal (NW–SE) and transverse divisions of the Ukrainian The analysis of the morphostructure and morphosculpture of the reserve is carried out taking into account the longitudinal (NW–SE) and transverse divisions of the Ukrainian Carpathians. The longitudinal division is associated with morphostructures of higher orders, such as second and third. The transverse division is associated with the fourth and fifth orders of morphostructures. In the analysis of morphosculpture of the reserve, the types characterized for all regions of Flysch and Crystal Carpathians are allocated. All mountain massifs and ridges could be characterized by an asymmetrical structure, such as steep northeastern slopes and acclivous southwestern slopes. The relic morphosculpture is represented by: 1) fragments of denudation surfaces of different ages such as Polonynska, Pidpolonynska, and riparian; 2) ancient glacial and extra glacial landforms; 3) areas of ancient longitudinal valleys. River valleys with a complex of different age terraces represent inherited morphosculpture. Modern morphodynamic processes are represented by height (tier) differentiation. The processes of sheet erosion, deflation, and rill erosion play an important role in the relief modeling for the tiers of strongly dissected mid-mountain relief. The lower tier of the terraced and non-terraced bottoms of the valleys are associated with the processes of leaching and erosion as well as a significant accumulation of erosion products and mudflows. Stabilized and active displacements are the most recorded among the gravitational processes and block motions. Key words: Carpathian Biosphere Reserve; Ukrainian Carpathians; relief; morphostructure; morphosculpture.
喀尔巴阡山脉生物圈保护区地形与地质构造
喀尔巴阡生物圈保护区的地形和地质构造代表了乌克兰喀尔巴阡山脉四个地貌区的地质和地貌结构特征。Polonynsko-Chornohirsky喀尔巴阡山脉的块状中山(Chornohora、Svydovets和Uholsko-Shyrokoluzhansky地块)和Marmarosy晶体地块的褶皱中山(Marmarosy和Kuziy-Trybushansky地块)在保护区内得到了很好的保护。考虑到乌克兰喀尔巴阡山脉的纵向(西北-东南)和横向划分,对保护区的形态结构和形态雕刻进行了分析。纵向分裂与更高阶的形态结构有关,如第二和第三阶。横向分裂与第四和第五阶的形态结构有关。在自然保护区的形态分析中,划分了弗理石和水晶喀尔巴阡山脉所有地区的特征类型。所有的山体和山脊都具有不对称的结构特征,如东北坡陡,西南坡陡。遗迹形态雕刻主要表现为:1)不同年代Polonynska、Pidpolonynska、河岸等剥蚀面碎片;2)古冰期和特冰期地貌;3)古纵向河谷区。具有不同时代梯田的河谷代表着继承的形态雕刻。现代形态动力学过程表现为高度(层)分化。薄片侵蚀、剥蚀和细沟侵蚀过程在强切分中段地形的地形模拟中起着重要作用。河谷梯田和非梯田底部的下层与淋滤和侵蚀过程以及侵蚀产物和泥石流的大量积累有关。在重力过程和块体运动中,稳定位移和活动位移记录最多。关键词:喀尔巴阡山脉生物圈保护区;乌克兰喀尔巴阡山;救援;形态结构;刻蚀地貌。
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