柴埠溪岩溶峡谷景观
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摘要
柴埠溪岩溶峡谷位于鄂西南岩溶山区,岩溶形态丰富多样,岩溶景观主要为峰林、象形山、洞穴、天生桥等。峡谷以中上寒武统娄山关组的白云岩地层为物质基础,在地壳抬升,河流侵蚀下切作用下形成,形态优美。峡谷区具有很高的美学价值和旅游价值,开发利用景观资源,需要加强生态环境保护工作,积极进行科普宣传。
Chaibuxi karst gorge is located in the southwest of Hubei karst mountain area,karst morphological diversity.The karst landscapes are generally classified into peak forest,pictographic mountains,caves,natural arch,et al.All are developed in Upper-Middle Cambrian dolomite strata of the Loushanguan group as the foundation,formed under the cut under the action of crustal uplift,river erosion,beautiful shape.The aesthetic value and tourist value in Canyon area are high.Development and utilization of landscape resources need to be strengthened ecological and environmental protection work,positive for science popularization.
Chaibuxi karst gorge is located in the southwest of Hubei karst mountain area,karst morphological diversity.The karst landscapes are generally classified into peak forest,pictographic mountains,caves,natural arch,et al.All are developed in Upper-Middle Cambrian dolomite strata of the Loushanguan group as the foundation,formed under the cut under the action of crustal uplift,river erosion,beautiful shape.The aesthetic value and tourist value in Canyon area are high.Development and utilization of landscape resources need to be strengthened ecological and environmental protection work,positive for science popularization.
引文
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[6]赵璧,邹亚锐,辛杰,等.湖北省地貌景观主要类型和科学意义简述[J].资源环境与工程,2018,32(4):657-662,698.ZHAO Bi,ZOU Yarui,XIN Jie,et al.The main types and scientific significance of geomorphologic landscape in Hubei[J].Resources Environment&Engineering,2018,32(4):657-662,698.
[7]徐松华.鄂西南溶洞旅游资源空间分布特征[J].中国岩溶,2018,37(3):440-449.XU Songhua.Spatial distribution of karst cave resources in south-western Hubei region[J].Carsologica Sinca,2018,37(3):440-449.
[2]李江风,汪华斌,吕贻峰.清江流域旅游资源分布规律及成因[J].地球科学,1999(4):374-377.LI Jiangfeng,WANG Huabin,LYU Yifeng.Distribution pattern and origin of tourism resources in Qingjiang river,Hubei province,China[J].Earth,1999(4):374-377.
[3]方起东,祝炜平.峡谷的自然地理特征与旅游开发研究[J].地域研究与开发,2002(2):68-71.FANG Qidong,ZHU Weiping.On the features of Canyon's physical geography and its tourism value[J].Areal Research and Development,2002(2):68-71.
[4]韦跃龙,罗书文,陈伟海,等.贵州绥阳地质公园白云岩喀斯特景观特征及其形成演化分析[J].地球学报,2018,39(3):365-383.WEI Yuelong,LUO Shuwen,CHEN Weihai,et al.Characteristics and formation and evolution analysis of the dolomite Karst landscape of Suiyang geopark,Guizhou province[J].Acta Geoscientica Sinica,2018,39(3):365-383.
[5]周俊华.湖北省五峰地质公园地质遗迹及保护[J].华南地质与矿产,2010(3):73-76.ZHOU Junhua.Geoheritage characteristics and protection in Wufeng geopark,Hubei province[J].Geology and Mineral of South China,2010(3):73-76.
[6]赵璧,邹亚锐,辛杰,等.湖北省地貌景观主要类型和科学意义简述[J].资源环境与工程,2018,32(4):657-662,698.ZHAO Bi,ZOU Yarui,XIN Jie,et al.The main types and scientific significance of geomorphologic landscape in Hubei[J].Resources Environment&Engineering,2018,32(4):657-662,698.
[7]徐松华.鄂西南溶洞旅游资源空间分布特征[J].中国岩溶,2018,37(3):440-449.XU Songhua.Spatial distribution of karst cave resources in south-western Hubei region[J].Carsologica Sinca,2018,37(3):440-449.