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Formation of Baiyun Karst Cave Landscapes in the Kongshan Mountain of Lincheng County, Hebei Province

机译:河北省临城县孔山白云岩溶洞穴景观形成

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摘要

Baiyun Cave in the Kongshan Mountain is a cave which developed mostly in thick-layer oolitic limestone of the Middle Cambrain Zhangxia Formation in the Quaternary period.The spatial distribution of the karst cave was cotrolled by the NNW,NE and near-EW faults.The karst cave system consists of three layers,includes mainly hall type and corridor type,within which there are diversified sedimentary landscapes and corrosion landscapes,especially"Reticular helictite","Jade-hairpin pointing at bottle","Yin and yang jade columns"and many other special landscapes can hardly be found in other karst caves.Influenced by the strong tectonic activities since the Quaternary period,the cave collapsed several times,and landscapes within the cave have been seriously damaged.Study on the landscape formation of karst caves and influence of cave environment changes on its landscape development will contribute to the reasonable development and protection of tourist resources in the cave.
机译:孔山白云洞是第四纪坎布林张峡组中厚层鲕状灰岩中发育的溶洞,岩溶洞的空间分布受NNW,NE和近EW断层的支配。喀斯特溶洞系统由三层组成,主要包括大厅型和走廊型,其中有多种沉积景观和腐蚀景观,特别是“网状红云母”,“玉bottle指瓶”,“阴阳玉柱”和在第四纪以来强烈的构造活动的影响下,该洞穴几次坍塌,并且其内部景观受到严重破坏。研究喀斯特洞穴的景观形成及其影响研究洞穴环境变化对其景观发展的影响将有助于洞穴的合理开发和旅游资源的保护。

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