PPT-Bedforms
Author : briana-ranney | Published Date : 2016-07-05
in Unidirectional Flow Sedimentary layer thicknesses span several orders of magnitude from mm to more than a meter That continuum is arbitrarily subdivided
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Bedforms: Transcript
in Unidirectional Flow Sedimentary layer thicknesses span several orders of magnitude from mm to more than a meter That continuum is arbitrarily subdivided anything lt1 cm is called a lamina gt1 cm is a . OR. Strategy:. Relate sedimentary characteristics of ancient deposits (grain size, . sedimentary . structures, geometry) to features observed in modern rivers. Bedforms. during traction deposition from unidirectional flow. Sedimentary layer . thicknesses span . several orders of magnitude, from . mm . to more than a . meter. That continuum is arbitrarily subdivided: anything <1 cm is called a lamina, >1 cm is a .
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