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(Liu TS, Loess and the environment) Much effort was put into the setting up of regional and local loess stratigraphies and their correlation (Kukla 1970, 1975, 1977).But even the chronostratigraphical position of the last interglacial soil correlating to marine isotope substage 5e has been a matter of debate, owing to the lack of robust and reliable numerical dating, as summarized for example in Zöller et al.
The word loess, with connotations of origin by wind-deposited accumulation, came into English from German Löss ( Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non-stratified and often calcareous.Loess grains are angular with little polishing or rounding and composed of crystals of quartz, feldspar, mica and other minerals. Loess deposits may become very thick; more than a hundred meters in areas of China and tens of meters in parts of the Midwestern United States.It generally occurs as a blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick.The form of these loess dunes has been explained by a combination of wind and tundra conditions.
Loess comes from the German Löss or Löß, and ultimately from Alemannic lösch meaning loose as named by peasants and masons along the Rhine Valley.
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