龙里高山草原形成机理与旅游资源初评

龙里高山草原是一个待开发的风景旅游区，它由海拔1578-1674m的山巅坪台及深切到海拔1100m左右的岩溶峡谷组合而成，包括无边无际的平坦草原、险而奇的岩溶森林峡谷，及残丘、岩溶洼地、峰林等多种类型的地貌，草原坪台上覆盖着草甸，岩溶峡谷内长满竹林及阔叶混合林，是开展多种旅游项目不可多得的绿色旅游资源，该景区的形成与特殊的地质地貌演化历史有关，即新构造运动使得区内地壳不断抬升，分布在平缓的箱状背斜轴部的石炭系石灰岩上的石英砂岩，由于其抗风化能力强，而残留在一级剥夷面上成为山巅坪台，即方山地貌，该旅游区具有“奇、新、特”及距贵阳近的得天独厚的旅游优势。

THE FORMING PROCESS OF THE LONGLI ALPINE MEADOW AND EVALUATION OF ITS TOURISM RESOURECE

The Longli alpine meadow is a scenic place not yet developed.It is composed of the plateau of altitude 1578～1674 meters and the karst gorge of altitude about 1100 meters, including a boundless plain meadow,dangerous and marvelous karst forest gorge, residual hills, karst swallows and peak forests.The meadow platform is covered with meadows, and bamboos and bushes grow in karst gorge, which are very good tourism resources.The formation of the scenic place is related to the special geological and geomorphologic history. The place is situated on a gentle box anticline axis,Carboniferous limestone strata are covered with quartzose sandstone.The tour district is “marvelous”,“original”,“peculiar” and adjacent to Guiyang.So the place can be developed as a new tour spot.