期刊文献+

丹霞地貌与岩溶地貌旅游景观之比较研究 被引量:10

A Comparison between the Tourism Scenery of Danxia Landform and That of Karst Landform
下载PDF
导出
摘要 对丹霞地貌与岩溶地貌的旅游景观进行系统比较,揭示两者在发育条件及分布特点、自然及人文旅游景观方面的相似性与差异性。在发育条件上,两者的岩性、构造环境和主要外营力均存在显著差异;另一方面,两者的发育又都依赖于一定的水热条件和密集的节理裂隙。在空间分布上,两者发育最典型的地区均在我国南方亚热带、热带湿润区;其中,东南地区尤以丹霞景观见长,西南地区更以岩溶景观取胜。自然景观方面,丹霞景观与岩溶景观在类型、外形、组合上有较多相似之处;两相比较,岩溶风景胜在山奇洞奥,而丹霞风景则胜在赤壁丹崖。人文景观方面,丹霞地貌区与岩溶地貌区均遗存众多悬棺崖墓和摩岩题刻;此外,前者还以道教名山和佛教石窟众多而见长,后者则在古人类遗址和民族风情方面占据优势。 A systematic comparison is made between the tourism scenery of Danxia landform and that of Karst landform by introducing their similarity and diversity in development condition, spatial distribution, physical scenery, and human scenery. As to the development condition, there are obvious differences in lithology, structure environment, and main exterior forces, but, on the other hand, the development of both landform depend on sufficient water and heat, dense joints and fractures of the rocks. As to the spatial distribution, the most typically developed Danxia and Karst areas are in tropic and sub-tropic humid regions in south China, but Danxia scenery especially in southeast China, while Karst scenery especially in southwest China. As to physical scenery, Danxia and Karst have many similarities in type, shape, and compound, however, Karst scenery is superior in the miraculous hills and caves to Danxia scenery, while the latter is superior in the red walls and cliffs to the former. As to human scenery, there are many overhanging coffins and inscriptions on escarpments in Danxia and Karst landform areas, in addition, there are also many famous mountains of Taoism and grottoes of Buddhism in Danxia landform areas, and many paleoanthropological sites and charming landscapes of national culture in Karst landform areas.
出处 《热带地理》 2006年第1期12-17,共6页 Tropical Geography
基金 南京大学人才引进科研启动基金资助(005118)
关键词 丹霞地貌 岩溶地貌 人文旅游景观 自然旅游景观 比较研究 Danxia landform Karst landform Physical scenery Human scenery Comparison
  • 相关文献

参考文献9

二级参考文献31

  • 1钱方 凌小惠.元谋土林成因及类型的初步研究[J].中国科学,1989,(4):412-418.
  • 2张林源.论丹霞岩层的沉积环境与丹霞地貌的旅游开发[J].经济地理,1994,14:68-75.
  • 3彭华.中国丹霞地貌十年研究回顾[J].经济地理,2002,22:5-14.
  • 4Carson M A, Kirkby M J. Hillslope form and process[M]. London:Cambridge University Press, 1972.475- 478.
  • 5Hooke R L. Toward a uniform theory of clastic sediment yield in fluvial systems[J]. Geological Society of America Bulletin, 2000, 112:1778- 1786.
  • 6Davis W M. The geographical cycle[J]. Geography Journal: 1899,14:481 - 504.
  • 7Penck W. Morphological Analysis of Landforms[M]. New York:St.Martin's Press, 1953.429 - 431.
  • 8King L C. Canons of landscape evolution [J]. Geological Society of America Bulletin: 1953,64: 721 - 752 .
  • 9朱艳.甘肃丹霞地貌的特征与发育条件[J].经济地理,1998,18:88-95.
  • 10陈佳骆.丹霞地貌风景名胜区发展评述[J].经济地理,2002,22(6):87-92.

共引文献63

同被引文献125

引证文献10

二级引证文献69

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部