汶川地震堰塞湖旅游开发研究
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摘要
地震堰塞湖是指由于强烈地震诱发河道两侧山体发生块体运动,以滑坡、崩塌、泥石流等形式堆积的大量固体物质形成的土石堤坝横向堵塞河道,上游壅水而形成的湖泊。汶川地震后形成了132个堰塞湖,地震堰塞湖在对区域安全及环境造成了巨大危害的同时,也蕴藏了丰富的旅游资源。将地震堰塞湖开发成为旅游景区是国内外常见的堰塞湖利用方式之一。针对地震堰塞湖的安全性特点,浅析了旅游开发中存在的安全问题和旅游问题,并提出了相应的对策。
Dammed-lake induced by earthquake referred to the natural lake formed by backwater in the upper reaches of rivers,which caused by the accumulation of a large number of solid materials in the form of landslides,collapse,debris flows due to strong earthquake on both sides of the mountain,so as to form the earth dam to plug the horizontal river.123 dammed-lakes formed at Wenchuang earthquake caused great harm to the regional security and geological environment;it also contained a great deal of potential tourism resources.Earthquake Landslide Lake will be developed into tourist attractions is a common way to use Imprisoned Lake at home and abroad.The characteristics of Imprisoned Lake induced by earthquake were discussed in the paper,the security issues and tourism market issues in tourism development were also analyzed,and the corresponding countermeasures were put forward.
Dammed-lake induced by earthquake referred to the natural lake formed by backwater in the upper reaches of rivers,which caused by the accumulation of a large number of solid materials in the form of landslides,collapse,debris flows due to strong earthquake on both sides of the mountain,so as to form the earth dam to plug the horizontal river.123 dammed-lakes formed at Wenchuang earthquake caused great harm to the regional security and geological environment;it also contained a great deal of potential tourism resources.Earthquake Landslide Lake will be developed into tourist attractions is a common way to use Imprisoned Lake at home and abroad.The characteristics of Imprisoned Lake induced by earthquake were discussed in the paper,the security issues and tourism market issues in tourism development were also analyzed,and the corresponding countermeasures were put forward.
引文
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[9]吴成基,韩丽英,陶盈科,等.基于地质遗迹保护利用的国家地质公园协调性运作[J].山地学报,2004,22(1):17-21.
[10]毛学翠.地质公园建设与旅游资源开发探析[J].资源.产业,2003,5(4):11-12.
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[12]何德伟,马东涛,黄海,等.贡嘎山旅游景区泥石流灾害及减灾对策[J].水土保持通报,2008,28(1):140-144.
[2]聂高众,高建国,邓砚.地震诱发的堰塞湖初步研究[J].第四纪研究,2004,24(3):293-301.
[3]谢洪,王士革,孔纪名.“5.12”汶川地震次生灾害的分布与特点[J].山地学报,2008,26(4):396-401.
[4]崔鹏,韦方强,何思明,等.5.12汶川地震诱发的山地灾害及减灾措施[J].山地学报,2008,26(3):280-282.
[5]范晓.地震堰塞湖[J].中国国家地理,2008(9):16-23.
[6]范建容,田兵伟,程根伟,等.基于多源遥感数据的5.12汶川地震诱发堰塞体信息提取[J].山地学报,2008,26(3):257-262.
[7]严石.龙门山一座天然的地质博物馆[J].大自然探索2000(8):30-31.
[8]周玲强,林巧.湖泊旅游开发模式与21世纪发展趋势研究[J].经济地理,2003,23(1):139-143.
[9]吴成基,韩丽英,陶盈科,等.基于地质遗迹保护利用的国家地质公园协调性运作[J].山地学报,2004,22(1):17-21.
[10]毛学翠.地质公园建设与旅游资源开发探析[J].资源.产业,2003,5(4):11-12.
[11]刘丹萍,阎顺.新疆自然风景旅游地旅游环境保护浅析[J].干旱区地理,2001,24(4):365-370.
[12]何德伟,马东涛,黄海,等.贡嘎山旅游景区泥石流灾害及减灾对策[J].水土保持通报,2008,28(1):140-144.
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