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- W2538127218 abstract "The effect on Ireland’s landscape of glacial erosion and deposition has been profound but many of the major landscape elements are demonstrably pre-Quaternary in origin. The island’s broad outline reflects the configuration of offshore post-Palaeozoic basins, while the disposition of hills and valleys commonly reflects the lithology and geological structure of the underlying bedrock. Most of Ireland’s largest rivers are structurally controlled and have their origins earlier in the Cenozoic, but several aspects of the Shannon suggest that parts at least of this system are far younger. The differential relief of Ireland’s landscape immediately prior to the onset of glaciation would have been greater than today, with often deeply karstified limestone lowlands interspersed with weathered silicate uplands. Glacial processes during the Pleistocene have largely scoured the weathered regolith from the uplands and buried much of the lowland karst, but a few remarkable sites afford glimpses of these pre-glacial landscapes and provide a measure of the extent, locally, of the glacial modification of this pre-existing landscape." @default.
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- W2538127218 date "2016-10-21" @default.
- W2538127218 modified "2023-09-23" @default.
- W2538127218 title "The Pre-Quaternary Landscape of Ireland" @default.
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- W2538127218 doi "https://doi.org/10.2991/978-94-6239-219-9_2" @default.
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