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graded bedding

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graded bedding

Sedimentary feature in which the sedimentary layer shows a gradual change in particle size, usually coarse at the bottom to fine at the top. It is useful for determining which way was up at the time the bed was deposited.



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The matrix material is heterogeneous and fluvial sedimentary in origin, finely clastic with moderate clay content, and with local expressions of graded bedding in limestone cavities.
between beds 6 and 7, is marked by a distinct, strongly pyritized discontinuity surface overlain by bed 7 of skeletal grainstone with graded bedding.
 
 
 
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