大维迪夫岭采石场的浮雕(以vynnychky采石场为基础)

Pavlo Horishnyy, Andriy Baitsar
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引用次数: 0

摘要

Davydiv山脊构成了一个独特的地貌自然区域,位于Podillia高地的边缘地带,构成了Podillia北部边缘的一部分。Davydiv山脊也被认为是利沃夫高原的东部部分。该地区包括19个采石场,其中大多数已不再运营。这些采石场主要开采沙子,少部分开采石灰石和壤土。从地形上看,Davydiv ridge的采石场主要是倾斜的(9),而分水岭和倾斜分水岭采石场较少。最长的采石场,Davydiv-2,延伸约750米,而最短的,被称为Honchari,跨度160米。采石场的深度从5米到30米不等,最常见的范围是15米到25米。以Vynnychky采石场为代表,详细考察了Davydiv岭采石场的地形特征。这个特殊的采石场长570米,宽420米,最大深度30米。从平面上看,它呈现出一个复杂的多边形形状,从北向南延伸。采石场的北面、西面和南面都有岩壁,与东面的自然地形无缝过渡。Vynnychky采石场的地貌组成包括剥蚀性、剥蚀-堆积性和堆积性地貌元素和形态。剥蚀地形的关键组成部分包括上覆岩层、作业矿壁、护坡、人为丘和矿底板。作业矿墙的高度从5米到30米不等,而覆盖层台阶的高度达到7米到10米。护堤分布在采石场的北部和南部地区,并与覆盖层长凳有遗传联系。矿井底板分为两个相对明显的部分:北部和南部。自然地形的残余形式,被称为人为丘,位于矿山的底板内。剥蚀堆积地形包括采石场北部的剥蚀堆积斜坡和地表。堆积堆积又分为内部堆积和外部堆积。这些垃圾场按年龄分类:1)长达5年;2) 5-10年;3)超过10年。内部堆积场占据了矿山底板的大部分,表现为平坦、丘陵和丘陵洼地形式。外部垃圾场位于采石场采掘区之外,具有不同年龄的丘陵和相对平坦的地层,以及堤防。关键词:采石场;蓬救援;累计救助;Davydiv山脊。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RELIEF OF QUARRIES OF DAVYDIV RIDGE (BASED ON VYNNYCHKY QUARRY)
Davydiv ridge constitutes a distinct geomorphological natural region situated within the marginal zone of the Podillia Upland, which forms part of the northern ledge of Podillia. The Davydiv ridge is also considered the eastern segment of the Lviv Plateau. This region comprises 19 quarries, the majority of which are no longer operational. Predominantly, these quarries extract sand, with a smaller proportion dedicated to limestone and loam excavation. In terms of topography, the quarries of Davydiv ridge are primarily sloping (9), while watershed and sloping watershed quarries are less common. The longest quarry, Davydiv-2, extends approximately 750 meters, while the shortest, known as Honchari, spans 160 meters. Quarry depths vary between 5 and 30 meters, with the most common range being 15 to 25 meters. A detailed examination of the relief features within the quarries of Davydiv ridge is illustrated using the Vynnychky sand quarry as a representative example. This particular quarry spans 570 meters in length and 420 meters in width, with a maximum depth of 30 meters. It exhibits a complex polygonal shape in a plan view, extending from north to south. The quarry is flanked by ledges to the north, west, and south, seamlessly transitioning into the natural terrain to the east. The geomorphological composition of the Vynnychky quarry encompasses denudational, denudational-accumulative, and accumulative relief elements and forms. Key components of the denudational relief include the overburden benches, operational mine walls, berms, anthropogenic buttes, and the mine floor. Operational mine walls range in height from 5 to 30 meters, while overburden benches reach heights of 7 to 10 meters. Berms are distributed locally across the northern and southern regions of the quarry and are genetically linked to the overburden benches. The mine floor is divided into two relatively distinct sections: northern and southern. Residual forms of natural relief, referred to as anthropogenic buttes, are located within the mine's floor. Denudational-accumulative relief encompasses denudational-accumulative slopes and surfaces in the northern portion of the quarry. Accumulative relief is further categorized into interior and exterior dumps. These dumps are classified by age: 1) up to 5 years; 2) 5-10 years; and 3) over 10 years. Interior dumps dominate the majority of the mine floor, exhibiting flat, hilly, and hilly-depression forms. Exterior dumps are situated beyond the quarry extraction area, featuring hilly and relatively flat formations of varying ages, as well as embankments. Key words: quarry; denudational relief; accumulative relief; Davydiv ridge.
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