The Knockmealdown Mountains: A Glacial Nunatak
DOI:
https://doi.org/10.55650/igj.1976.864Abstract
Farrington's 1947 hypothesis that the Knockmealdown Mountains were a glacial nunatak is tested and confirmed. The unglaciatcd area was considerably less than Farrington suggested and the maximum altitude reached by the ice around the mountains appears to have been around 365 m.Downloads
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2016-12-26
How to Cite
Lewis, C. A. (2016). The Knockmealdown Mountains: A Glacial Nunatak. Irish Geography, 9(1), 18–28. https://doi.org/10.55650/igj.1976.864
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