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Structure from Motion Multisource Application for Landslide Characterization and Monitoring: The Champlas du Col Case Study, Sestriere, North-Western Italy. [PDF]
Sensors (Basel), 2019 Cignetti M +3 more
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Evidence for a palaeo-subglacial lake on the Antarctic continental shelf. [PDF]
Nat Commun, 2017 Kuhn G +9 more
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Using GIS to Evaluate an Enigmatic Diamicton in the Spring Mountains, Southern Nevada
Professional Geographer, 2003Abstract The Spring Mountains are located in southern Nevada and lie along the western margin of the Las Vegas Valley. A diamicton located approximately 2,590 m (8,500 ft) above sea level in the Spring Mountains contains numerous striated limestone clasts ranging in size from 0.5 cm to 1.0 m.
John G. Van Hoesen, Richard L. Orndorff
exaly +2 more sources
Pebble Fabric in an Ice-Rafted Diamicton
The Journal of Geology, 1985Pebble fabric studies on ice-rafted diamictons have been limited to general observations, with authors noting preferences toward vertical, random, or horizontal orientations. To clarify such observations, pebble fabric data were collected from a fossiliferous diamicton of late Pleistocene age located on Whidbey Island, Washington. The ice-rafted origin
Eugene W. Domack, Daniel E. Lawson
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Microstructures in diamictons—evidence of subglacial bed conditions
Geomorphology, 1992Abstract Examination of microstructures within diamictons from southern Ontario, Canada, and southern Bavaria, and Baden-Wurttemburg, Germany reveal evidence illustrative of certain subglacial bed conditions. The microstructures from Ontario were obtained from a complex glacial melange unit that forms the internal structure of an isolated drumlin ...
J. Menzies, A.J. Maltman
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Sedimentology and depositional environments of the Lund Diamicton, southern Sweden
Boreas, 1990The Lund Diamicton (earlier named Lund Till) in SW Skåne, S. Sweden, is a glacioaquatic sediment consisting of clay and massive and laminated diamictons. It is characterized by clasts derived from the Baltic depression and its depositional history can be summarized as follows: After deglaciation, large fields of stagnant ice remained in the area and a ...
KÄRSTIN MALMBERG PERSSON +1 more
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Origin of diamictons on the Barents Sea shelf
Lithology and Mineral Resources, 2009Occurrence conditions and lithological-paleontological characteristics of two diamicton units developed in the southeastern segment of the Barents Sea shelf are considered. It is shown that they are lithologically analogous to the present-day (undoubtedly aqueous) diamicton mud.
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Problems associated with seismic facies analysis of diamicton-dominated, shelf glacigenic sequences
Geo-Marine Letters, 1990Diamicton-dominated shelf glacigenic sequences are characterized on high-resolution seismic records by a structureless to chaotic acoustic texture, often with abundant hyperbolic (point-source) reflections. Existing depositional models, based primarily on seismic data, have been constructed on the basis that this acoustic signature is indicative of ...
F. S. Stewart, M. S. Stoker
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