Remote Sensing Interpretation about Landform of Glacial Erosion at Quaternary Period in Eastern Side of the Southern Segment of Taihang Mountain

Guo Qingshi

doi:10.11834/jrs.1991005

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Remote Sensing Interpretation about Landform of Glacial Erosion at Quaternary Period in Eastern Side of the Southern Segment of Taihang Mountain
Issue 1, Pages: 30-35(1991)
Published：1991
DOI： 10.11834/jrs.1991005
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[1]郭庆十.河北省太行山南段东坡第四纪冰川遗迹的遥感解译[J].环境遥感,1991(01):30-35+2. DOI： 10.11834/jrs.1991005.

Guo Qingshi. Remote Sensing Interpretation about Landform of Glacial Erosion at Quaternary Period in Eastern Side of the Southern Segment of Taihang Mountain[J]. Journal of Remote Sensing, 1991, (1): 30-35. DOI： 10.11834/jrs.1991005.

摘要

利用大比例尺黑白航空像片首次在太行山南段东坡发现了大面积保存较完好的冰川遗迹如角峰、刃脊、冰斗、悬谷、冰蚀盆地及冰蚀槽谷等

经系统组合、配套后认为

第四纪时期

该区曾发育过三一四期冰川活动

第I、II冰期冰川属于山谷一山麓冰川类型

而第IⅡ、IV（?）期冰川则为冰斗冰川。本文详述了各类冰蚀地貌的期次

分布、类型及发育特征

为该区第四纪古冰川活动的研究提供了新的证据。

Abstract

The large are of glacial erosion landform is discovered by the interpretation on large scale white-black airphotos in the eastern side of the southern segment of the Taihang mountain. 3 to 4 glacial epochs of landform of glacier erosion are distinguished. The glaciers of first and second epoch are valley-piedmont glacier. Other landforms are cirque

hanging valley

firn-basin and trough

etc. The glacial stage

its distribution tyge and characteristic of glacier are described in this paper. This work provids new evidences for futher researching the glacier movement in quaternary period in this area.

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遥感影像中地形辐射校正研究综述