Zastinoche and budaniv sandstone deposits as potential geotourism objects of the Ternopil region

Ivan Knysh, Nadiya Kremin
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Abstract

The article provides information on existing quarries for sandstone mining as promising geotourism locations within the Ternopil region (Western Ukraine). The study area is famous for its ancient mining of natural stone from Terebovlya sandstones. The object of research is located within the Eastern European platform on the territory of Zastinoche and Budanіv deposits. Since princely times, stone has been mined here for the construction of fortresses and defensive structures. Sediments of the Neogene and Devonian ages take part in the geological structure of the Zastinoche deposit. The mineral is represented by Devonian sandstone with an average thickness of 12 m, broken by horizontal and vertical cracks into boulders. Macroscopically, sandstone is represented by red-brown, brownish-red, greyish-red, reddish-grey, brownish-grey, pink-grey, greenish-grey and light grey variations. The Budaniv deposit is composed of Quaternary, Neogene, Cretaceous and Devonian rocks. The minerals here are the sandstones of the Ivanovo formation (Devonian), the sandstone stratum consists of two horizons. The average thickness of sandstones of the first horizon (red, thick-tiled) is 14.4 m, in the thickness of sandstones there are layers of argillites and siltstones. Sandstones of the second horizon are more thinly tiled, characterized by a thickness of 2.6 to 4.3 m. With depth, sandstones have a pink and pink-red colour. Both gray and pink variations of sandstones are fine-grained, quartz, feldspar-quartz, mica.. Cement is iron-clay; the clay part of it is sericite-silicon. Mining of sandstones at both deposits is carried out manually with the help of crowbars and wedges to the full depth. All processes for the extraction and manufacture of side and rubble stone are performed manually. Terebovlya sandstone is environmentally friendly, so it is used for the construction of facades as a natural heat insulator. Sandstone is frost-resistant and acid-resistant. It is widely used in modern architectural design and restoration of historical monuments in Europe; it is made of almost everything for facades. Among the architectural structures built of Terebovlya sandstone – a nine-arch railway bridge-viaduct near the village. Plebanivka, Terebovlya and Budaniv castles, Pidhoryany monastery of St. Basil the Great, a large number of churches and cathedrals. Geological and geotourism survey of Zastinoche and Budanіv sandstone quarries in the Ternopil region gives grounds to consider these locations as potential geotouristic objects.
扎斯蒂诺什和布达尼夫砂岩矿床是捷尔诺比尔地区潜在的地质旅游对象
文章提供了现有的采石场砂岩开采作为有前途的地理旅游地点在捷尔诺皮尔地区(乌克兰西部)的信息。该研究地区以其古老的Terebovlya砂岩天然石材开采而闻名。研究对象位于东欧平台Zastinoche和budanv矿床的领土上。从王侯时代起,这里就开始开采石头来建造堡垒和防御结构。新近系和泥盆系沉积物参与了Zastinoche矿床的地质构造。该矿物以泥盆纪砂岩为代表,平均厚度12 m,由水平和垂直裂缝破碎成砾石。宏观上,砂岩有红棕色、棕红色、灰红色、红灰色、棕灰色、粉灰色、绿灰色和浅灰色等变化。布达尼夫矿床由第四纪、新近系、白垩系和泥盆系岩石组成。这里的矿物是伊万诺沃组(泥盆纪)的砂岩,砂岩层由两个层位组成。第一层位(红色,厚纹)砂岩平均厚度为14.4 m,厚度上有泥质层和粉砂岩层。第二层的砂岩铺层较薄,厚度为2.6 ~ 4.3 m。随着深度的增加,砂岩呈现粉红色和粉红色。灰色和粉红色的砂岩都是细粒的,石英、长石石英、云母……水泥是铁粘土;粘土部分是绢云母硅。这两个矿床的砂岩开采都是在撬棍和楔子的帮助下进行的。所有提取和制造边石和碎石的过程都是手工完成的。Terebovlya砂岩是环保的,因此它被用作外墙的天然隔热材料。砂岩具有抗冻和耐酸的特性。在欧洲广泛应用于现代建筑设计和历史古迹修复;它是由几乎所有的立面。在Terebovlya砂岩建造的建筑结构中,村庄附近有一座九拱铁路桥-高架桥。Plebanivka, Terebovlya和Budaniv城堡,Pidhoryany圣巴西尔大帝修道院,大量的教堂和大教堂。对Ternopil地区的Zastinoche和budanv砂岩采石场的地质和地质旅游调查提供了将这些地点考虑为潜在的地质旅游对象的理由。
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