爱尔兰大西部湖区受威胁的喀斯特地貌

Geology Today Pub Date : 2022-10-13 DOI:10.1111/gto.12407
Michael J. Simms, Matthew A. Parkes
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引用次数: 0

摘要

石灰石是出了名的易漏的岩石。在许多石灰岩覆盖的地区,地表河流很少,而且互不相连。它们消失在水池里,有时会在几公里外的泉水里重新出现。这不是一个典型的湖泊存在的环境。爱尔兰大约40%的土地被石灰岩覆盖,然而爱尔兰的低地却散布着无数大大小小的湖泊。在许多地方,下面的石灰岩被一层冰碛物有效地封住了;另一些则是在浅水层以下的凹陷处形成的。在许多湖岸周围,裸露的石灰岩基岩和巨石支撑着一系列奇特的蚀刻特征,这些特征实际上仅限于这个湖岸环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The threatened karst of the Great Western Lakes, Ireland

Limestone is a notoriously leaky rock. In many areas that are underlain by limestone, surface rivers are few and disjointed. They disappear into sinks only to reappear, sometimes many kilometres away, at springs. It is not an environment in which lakes are typically found. Some 40 percent of Ireland is underlain by limestone, yet the Irish lowlands are scattered with countless lakes, large and small. In many the limestone beneath is effectively sealed by a cover of glacial till; others have formed where hollows descend below a shallow water table. Around the shores of many, exposed limestone bedrock and boulders support a range of peculiar etched features that are virtually confined to this lakeshore environment.

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