Till
Till or glacial till is unsorted glacial sediment.Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines.
Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Provided by Wikipedia
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102by Ballarotta, Maxime, Drijfhout, Sybren, Kuhlbrodt, Till, Döös, KristoferGet access
Published in Ocean Modelling (2013)
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103by Hochet, Antoine, Tailleux, Rémi, Ferreira, David, Kuhlbrodt, TillGet access
Published in Ocean Science (2019)
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114by Till, Jessica L., Moskowitz, Bruce, Poulton, Simon W.Get access
Published in Frontiers in Earth Science (2021)
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116by Kuhlbrodt, Till, Swaminathan, Ranjini, Ceppi, Paulo, Wilder, ThomasGet access
Published in Bulletin of the American Meteorological Society (2024)
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117by Ballarotta, Maxime, Drijfhout, Sybren, Kuhlbrodt, Till, Döös, KristoferGet access
Published in Ocean Modelling (2013)
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120by Daniel Draebing, Till Mayer, Benjamin Jacobs, Samuel T. McCollGet access
Published in Communications Earth & Environment (2022)
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