loess is found in mountain
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Typical loess is a yellow calcareous silt, which is unconsolidated, unbedded and structureless when freshly cut, but on drying develops a coarse prismatic structure with deep vertical joints or fissures.
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During the Quaternary, loess and loess-like sediments were formed in periglacial environments on mid-continental shield areas in Europe and Siberia, on the margins of high mountain ranges like in Tajikistan and on semi-arid margins .
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