广西岩溶地貌发育基本上均处于热带、亚热带环境中，为一较为典型的热带岩溶地貌。
The development of Guangxi karst geomorphology, with long geological history, was basically under tropical or subtropical environment, so it belongs to tropical karst geomorphology.
我国西南岩溶区位于亚热带，水热条件良好，水资源储存量相当丰富。
Karst region in southwest of China is located in the sub tropic with good combination of water and temperature.
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