편마암과 한국의 지형발달
Gneiss and landform processes in South Korea
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초록
This study is to describe geomorphlogical landscapes of Southern Korea relating with it’s environment based on gneiss field survey and literature synthesis. This work is to review the gneiss landforms studies by Korean geographers. It is verified that geomorphlogical characteristics of gneiss present landscapes characterized by 1) in case of mountains, are difficultly and regularly weathered, so as to develop earthy forms; 2) in case of stream valley that is massif highland, high relief with colluvium. Korean peninsula have endured erodible geomorphlogical processes since Miocene when warping it up. Therefore many intermontane basins are located on the crossing tecto-lineament line areas which are surrounded by mountains composed of much less Precambrian gneiss complex. In fact, intermontane basin is mainly linear fault-line valley. All these facts owing to generalized superficial weathering and soil forming attitudes, vegetation on gneiss mountains and hills is dense. These features are related to predominance of mass-movement(mainly creep) over irregular topsoil and play an important role in maintaining slope regularity and ecological stability. Landscapes are sum of landform relating with rock weathering mode and soil, climate, water, vegetation, human activity.
Abstract
This study is to describe geomorphlogical landscapes of Southern Korea relating with it’s environment based on gneiss field survey and literature synthesis. This work is to review the gneiss landforms studies by Korean geographers. It is verified that geomorphlogical characteristics of gneiss present landscapes characterized by 1) in case of mountains, are difficultly and regularly weathered, so as to develop earthy forms; 2) in case of stream valley that is massif highland, high relief with colluvium. Korean peninsula have endured erodible geomorphlogical processes since Miocene when warping it up. Therefore many intermontane basins are located on the crossing tecto-lineament line areas which are surrounded by mountains composed of much less Precambrian gneiss complex. In fact, intermontane basin is mainly linear fault-line valley. All these facts owing to generalized superficial weathering and soil forming attitudes, vegetation on gneiss mountains and hills is dense. These features are related to predominance of mass-movement(mainly creep) over irregular topsoil and play an important role in maintaining slope regularity and ecological stability. Landscapes are sum of landform relating with rock weathering mode and soil, climate, water, vegetation, human activity.
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