摘要
在湖北恩施市沐抚地区发育着独特岩柱群地貌,具有很高的观赏和科研价值。从整个地下水文地质单元特征来看,有其独特的发育形成条件。岩层产状平缓,垂直节理发育,第四纪冰期的缺失都为岩柱群地貌的形成提供了有利的条件。现通过实地考察对岩柱群地貌的形成提出了初步的见解。认为这种特殊的地貌类型是多种自然作用下的产物,而特殊的水循环条件是岩柱体地貌形成的主要因素。岩柱群地貌有别于其它的峰林地貌,是一种新的地貌类型。
In Mufu area of Enshi City, Hubei Province, a unique landscape of rock-columns with high ornamental and scientific value was developed. From groundwater hydrological geological unit,it had a unique formation conditions of the development. Rock occurrence flat, vertical joint s of the development, the missing Quaternary glacial were good for the formation of this landform. In this paper, we presented a preliminary view of the formation of landforms by fieldwork. This particular landscape type was the action of a variety of natural products, and the main factors were the special body of water cycle. The rock-columns were different from others and of a new type of landscape.
出处
《南水北调与水利科技》
CAS
CSCD
2010年第2期107-109,共3页
South-to-North Water Transfers and Water Science & Technology
基金
中法岩溶科考队湖北恩施洞穴科学考察项目资助
