Northern Hemisphere climate history through and following the Last Glacial Maximum is recorded in detail in ice cores from Greenland. However, the period between Greenland Interstadials 1 and 2 (15–23 ka), i.e. the period of deglaciation following the last major glaciation, has been difficult to resolve in great detail. We here offer a new subdivision of this in the NGRIP, GRIP and GISP2 ice cores, by newly introducing spectral trend analysis to the study of climate‐related data series from ice cores. This analysis reveals patterns of change and discontinuity in the waveform properties of a data series, relating to the environmental (including climatic) history of accumulation of the rock or ice record. The application allows high‐resolution correlation between the ice cores, and a greatly improved subdivision of the study interval. Nine climatic phases are recognized, within which more identifiable events can also be correlated between the three locations.
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Ice‐marginal debris‐flow deposits (comparable to deposits elsewhere described as flow tills) are described from glacier‐proximal sediments in an Alpine foreland area. Debris‐flow deposits are characteristically interstratified with subaeric or subaquatie meltwater deposits, and occur in a wide variety of geomorpho‐logical settings. The granulomctric composition of debris‐flow deposits is more variable than that of subglacial tills. Within‐flow variability may occur as a result of the formation of graded bedding, lateral as well as vertical. Clast fabrics show both random and preferred orientations; unequivocal interpretation of these is not possible. Debris‐flow deposits are composed of material derived from various sources: sources from subglaeially‐derived debris as well as from previously deposited tills and walerlain sediments can be demonstrated.
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