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CRISS-CROSS PATTERN [1 record]

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Record 1 1991-04-23

English

Subject field(s)
  • Geology
  • Geomorphology and Geomorphogeny
CONT

Till may also be squeezed into fracture systems or crevasses in the marginal zone of a receding ice sheet and form a criss-cross, irregular pattern of straight ridges that is more or less oblique to the direction of ice flow; some ridges, however, are transverse and some parallel to this direction. Such crevasse fillings have also been termed linear disintegration ridges

French

Domaine(s)
  • Géologie
  • Géomorphologie et géomorphogénie

Spanish

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