Libre de glaces en dérive multi-directionnel mudstone marques d'abrasion rock illustré dans l'image MWGBW Alamy2, Glen Scaladal Bay, île de Skye, Écosse, Royaume-Uni
2450 x 2450 px | 41,5 x 41,5 cm | 16,3 x 16,3 inches | 150dpi
Date de la prise de vue:
18 mai 2017
Lieu:
Elgol, Isle of Skye, UK
Informations supplémentaires:
For further information about Drift Ice Abrasion Marks refer to this paper. Drift-Ice Abrasion Marks along Rocky Shores - Journal of Glaciology, Volume 31, Issue 109 1985, pp. 237-241 Jean-Claude Dionne Abstract Drift-ice abrasion marks are common along present-day rocky shorelines in cold regions. They include polished surfaces, scratches, striations, small grooves, and minor friction cracks. Most are found on relatively soft rocks like shale, sandstone, limestone, dolomite, and basalt, and occasionally on harder rocks like granite and gneiss. They were made by rock fragments frozen at the base of ice cover or by ice floes pushed onshore by wind or dragged along the bottom by waves, tides, and currents. They are found both in the modern and Pleistocene marine, lacustrine, and fluvial environments. Along the Hudson Bay eastern shoreline, these abrasion marks are superimposed on glacially polished and striated surfaces. Along the St. Lawrence Estuary, they are more common on boulders in the tidal zone. Characteristics of drift-ice abrasion marks are described and their significance is pointed out.
