Results 21 to 30 of about 203 (161)
Environmental Research Letters, 2021 Organic matter, upon dissolution into the aqueous state as dissolved organic matter (DOM), can undergo mineralization by microbes. There has been increasing effort to characterize DOM released from thawing permafrost because it may perpetuate a ...
Erin N MacDonald +4 more
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Composition and origin of the Middle Weichselian interstadial deposit in Veskoniemi, northern Finland [PDF]
Estonian Journal of Earth Sciences, 2010 The stratigraphy and sedimentology of a diamicton-stratified sand deposit have been studied in the Veskoniemi area, near Lake Inarijärvi in central Finnish Lapland. Test pit excavations were used for stratigraphical investigations.
Niko Putkinen +3 more
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Lithostratigraphy of Late Weichselian tills on the West Estonian Islands [PDF]
Bulletin of the Geological Society of Finland, 1998 Glacial stratigraphy of the West Estonian Islands comprises three different diamicton units which are correlated event-stratigraphically to the Pandivere and Palivere ice advances of the most recent (Late Weichselian) glaciation and included into the ...
E. Kadastik, V. Kalm
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Stream Recovery Post Channelization: A Case Study of Low-Gradient Streams in Central Illinois, USA
Hydrology, 2022 Stream channelization, which entails reducing the sinuosity of a stream, widening, and in some cases deepening the stream channel, is a widespread practice in agricultural regions.
Joseph P. Becker, Eric W. Peterson
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Danish Journal of Archaeology, 2015 In this short article, we take a brief but concise look at chronological, and to a limited extent environmental and typological, aspects of the Hensbacka culture group in Bohuslän.
Lou Schmitt, Krister Svedhage
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Glaciotectonically deformed glaciofluvial sediments with ruptured pebbles (the Koczery study site, E Poland) [PDF]
Bulletin of the Geological Society of Finland, 2018 Significant quantities of ruptured pebbles are found in glaciotectonically deformed glaciofluvial sediments of the Saalian glaciation (MIS 6) at the Koczery site (E Poland).
B. Woronko +3 more
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Bulletin of the Geological Society of Denmark, 1987 Deglaciation sequences comprising glaciolacustrine sediments overlain by till deposited in a subaqueous environment around the Danish coast of 0resund and in central Northeast Sjrelland are grouped into five facies (a, b, c, d and e ). Facies a and facies bare clays deposited from suspension fall out in ice dammed lakes.
Houmark-Nielsen, Michael, Lagerlund, E.
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Arctic, Antarctic, and Alpine Research, 2022 Arctic permafrost soils store substantial reserves of organic matter (OM) from which microbial transformation contributes significantly to greenhouse gas emissions of CH4 and CO2.
Ivaylo Kolchev +8 more
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Acta Universitatis Lodziensis. Folia Geographica Physica, 2021 The study presents the problem of complex genesis of eskers formed in N-channels on the example of an esker located near Tosie in east-central Poland.
Małgorzata Frydrych
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The origin of water‐borne diamictons and their relation to turbidites [PDF]
New Zealand Journal of Marine and Freshwater Research, 1967 Summary The term “diamicton” has recently been proposed as a non‐genetic name for any non‐calcareous terrigenous sediment containing a wide variety of grain sizes; the lithified equivalent is a “diamictite.” The present paper deals with the origin and classification of water‐borne diamictons. The latter have been divided by the writer
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