ancient karst的意思|示意
古喀斯特,古岩溶
ancient karst的用法详解
Ancient karst is a term used to describe the formation of underground structures in limestone and other soluble rocks. Karst is a type of landscape characterized by the presence of caves, sinkholes, and underground streams. These features are created by the chemical dissolution of the rock by water.
Ancient karst landscapes can be found in many parts of the world, most notably in the tropical regions of South and Central America, as well as in Southern Europe, Australia, and New Zealand. These landscapes are formed by rainwater, which slowly dissolves the underlying rock, creating caves and underground streams as it does so.
In ancient karst landscapes, the water flowing through underground channels often has a high mineral content, which means that it can result in the formation of stalactites, stalagmites, and other cave formations. These formations are often very beautiful and are a popular tourist attraction.
The term “ancient karst” is also used to describe the process of subsurface drainage from old-growth forests. When the soil of a forest is saturated with water, it can cause the water to flow downward, creating sinkholes and channels. This process is often referred to as “karstification”.
In addition to providing incredible natural sights, ancient karst is also an important aquifer. These underground features are often filled with groundwater, which is used by humans and animals as a source of drinking water. As such, ancient karst landscapes play an important role in water conservation.
ancient karst相关短语
1、 the ancient karst landform 古岩溶地貌
2、 ancient karst basin 古岩溶盆地
3、 ancient karst channel 古岩溶水道
4、 ancient karst physiognomy 古岩溶起伏
5、 ancient karst diagenetic facies 古岩溶成岩相
6、 ancient karst and weathering crust 古岩溶风化面
ancient karst相关例句
The study of ancient karst distribution laws should be carried out to restore the ancient landscape.
因此研究古岩溶分布规律,应先进行古地貌恢复。
The new movement and the modem climate promoted ancient karst further to grow forming the modern littoral karst.
新构造运动和现代天气促进古岩溶进一步发育形成现代滨海岩溶。
The mineralization is controlled by ancient karst structure and the NE-NNE oriented faults characterized by multi-stage activity.
矿化受古岩溶构造及具多期活动的NE - NNE向断裂控制。