IV.—On the Drifts of the West and South Borders of the Lake District, and on the Three Great Granitic Dispersions

Boulder-scars.—From Maryport to Parkgate, the E. coast of the Irish Sea at intervals exhibits accumulations or concentrations of large boulders, which are locally called scars. They may be seen in all stages of formation, from the denudational area, where they are in course of being left by the wash...

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Publicado en:	Geological Magazine
Autor Principal:	D. Mackintosh
Formato:	Artigo
Idioma:	inglés
Publicado:	Cambridge University Press 1871
Subjects:	Geological formations and processes Geology and Paleoclimatology Research Geological Studies and Exploration glacial till glacial drift glacial denudation glacial deposition Lake District
Acceso en liña:	https://zenodo.org/record/2059415 https://doi.org/10.1017/s0016756800161497
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