PALAEO VOLCANIC RELIEF FORMS AS A PART OF THE GEOHERITAGE IN THE REPUBLIC OF MACEDONIA, THEIR VALUATION AND PROTECTION

A. Todorova, Dragan Kolchakovski, Ss. Cyril, Methodius
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Abstract

In its geological evolution, the territory of the Republic of Macedonia was characterized by a great volcanic activity, but given the fact that active volcanic processes are not present today, the palaeo-volcanic relief forms are being emphasized. They occur in the form of volcanic cones, volcanic necks or plugs, remnants of volcanic craters, plateaus and other forms that are most prominent in the areas of extinct volcanic activity. The significance of the objects of the geoheritage is based on their defined values. Upon the termination of the volcanic activity to date, the volcanic forms are significantly morphologically modified mostly as a result of the large erosive processes and anthropogenic influences. Therefore, the prominent palaeo-volcanic relief forms that are part of the geoheritage need adequate protection. They deserve special attention, due to the fact that some of them are natural rarities that exceed not only the borders of the Balkan Peninsula but also in Europe.
古火山地貌作为马其顿共和国地质遗产的一部分,其价值和保护
马其顿共和国领土在其地质演变过程中具有强烈的火山活动的特点,但鉴于今天不存在活跃的火山作用,因此强调古火山地形形式。它们以火山锥、火山颈或火山塞、火山口残余物、高原和其他形式出现,这些形式在死火山活动地区最为突出。地质遗产对象的意义是基于其确定的价值。在火山活动结束后,火山形态发生了显著的形态变化,主要是由于大规模的侵蚀过程和人为影响。因此,作为地质遗产一部分的突出的古火山地貌需要得到充分的保护。它们值得特别关注,因为其中一些是自然稀有的,不仅超越了巴尔干半岛的边界,而且在欧洲也有。
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