苏伊山脉(苏台德山脉,波兰西南部)的地貌-地貌模式和人为影响

IF 1.1 Q3 GEOGRAPHY
P. Migoń, Agnieszka Latocha-Wites, Kacper Jancewicz
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引用次数: 1

摘要

苏台德山脉中部的索伊山脉是一个地貌学研究不足的地区,尽管它们在波西米亚地块内的大量地形中具有潜在的代表性,这些地形由变质基岩构成。除了对过去的工作进行概述外,本文还利用数字地形模型的可视化结果总结了该地块的主要地形特征,并概述了人为对地形的广泛影响。苏伊山脉的特征地貌包括断裂形成的岩性控制的悬崖、悬崖附近的山脊和山谷地形、分水平原、片麻质断层、农业梯田以及与以前采矿和军事用途有关的各种地貌。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomorphology of the Sowie Mountains (Sudetes, SW Poland) – Landform patterns and anthropogenic impact
The Sowie Mountains in the central part of the Sudetes range are an under-researched area in terms of geomorphology, despite their potential representativeness for a large number of terrains within the Bohemian Massif, built of metamorphic bedrock. Apart from providing an overview of past work, the paper summarizes the main topographic features of the massif using visualizations of the digital terrain model, and outlines the wide range of anthropogenic impacts on relief. Characteristic landforms of the Sowie Mountains include faultgenerated lithology-controlled escarpments, ridge-and-valley topography near the escarpments, water-divide flats, gneissic tors, agrarian terraces and various landforms related to former mining and military use.
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来源期刊
Geographia Polonica
Geographia Polonica GEOGRAPHY-
CiteScore
2.40
自引率
0.00%
发文量
9
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