46-Karst hill
2015-03-25 20:14 | Author：gzzjd | Reading：amount |
|
Hills formed by karstification are karst hills with weak karstification degree. Typical type of karst hill is combined with hill and solution depression. It is of round top and mild slope, and the width of hill bottom is larger than its height with a relative height between 100m and 150m. It is mainly distributed at the region unfavorable for rapid karstification, such as carbonatite area with limestone, siliceous limestone and dolomite limestone stratum under condition of subtropical climate. Karst hills in the geopark mainly distribute in the slope zone at both banks of Qijiehe River and Liuchonghe River, which mainly develop in carbonatite stratum of Triassic system (with dolomite limestone as the main lithologic character).  |
Park Profile
31-Daluoquan Tian
41-Qijiehe River
HOT
Copyright statement
1、《46-Karst hill》this article is supported by net friend, all copyrights author, if want to reproduce, please indicate the source.
2、Reproduced of reference or informative public free information for the purpose of reference to goodwill, should not be allowed to twist 、modify the content meaning ,at the same time, you must retain this net indicate the source of manuscript and own the copyright and other legal responsibility.
3、Caused by improper for reproduced or quoted this net content of civil disputs and administrative processing or other losses,we do not undertake any responsibility。
