| 四川四姑娘山风景名胜区地貌特征 |
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| 引用本文： | 曹俊. 四川四姑娘山风景名胜区地貌特征[J]. 四川地质学报, 2004, 24(4): 237-240 |
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| 作者姓名： | 曹俊 |
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| 作者单位： | 四川省地勘局区域地质调查队,四川,双流,610213 |
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| 摘 要： | 四姑娘山为国家重点风景名胜区和国家级自然保护区，其主峰海拔6250m，是四川省第二高峰。区内山势陡峭，地貌差异明显。海拔3800m以下，发育流水侵蚀、堆积地貌；海拔3800m以上广泛发育第四纪冰蚀地貌和古冰川堆积地貌。现代冰川海拔大约在5500m左右，受局部地形、供雪量影响，最低处可达4600m左右。
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| 关 键 词： | 古冰川地貌 流水地貌 现代冰川 四姑娘山 相对高差 |
| 文章编号： | 1006-0995(2004)04-0237-04 |
| 修稿时间： | 2004-03-15 |
Geomorphic Features in the Siguniangshan Scenic Spots,Sichuan |
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| CAO Jun. Geomorphic Features in the Siguniangshan Scenic Spots,Sichuan[J]. Acta Geologica Sichuan, 2004, 24(4): 237-240 |
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| Authors: | CAO Jun |
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| Abstract: | Mt Siguniang is key national scenic spots and national nature reserves with the highest peak at an elevation of 6 250 m, the second highest peak in Sichuan This region is characterized by precipitous landform with fluvial erosion and accumulation landform below 3 800 mabove sea level and Quaternary glaciated landform and drift landform above 3 800 m above sea level and development of present glaciers at an elevation of about from 5 500 m to 4 600 m |
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| Keywords: | former glacial landform fluvial landform present glacier Mt Siguniang |
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