Definitions
from The Century Dictionary.
- noun See
false bedding , under false.
Etymologies
Sorry, no etymologies found.
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Examples
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Uploaded into this terrestrial machine would be all the data accumulated by the USGS on cross-bedding.
Cross-Bedding, Bedforms, and Paleocurrents, or: A Proposal for a New Civic Plaza in Chicago 2008
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Or did you mean this DVD containing all the cross-bedding animations found at the USGS website (with extra content)?
Cross-Bedding, Bedforms, and Paleocurrents, or: A Proposal for a New Civic Plaza in Chicago 2008
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Below are some screen captures taken from animations of cross-bedding formation that you can download from the U.S.
Cross-Bedding, Bedforms, and Paleocurrents, or: A Proposal for a New Civic Plaza in Chicago 2008
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Can't say I've fully grasped the science behind cross-bedding yet, but I was quickly and fully hypnotized by these computer animations of sedimentary migration and deposition.
Ripple Topography 2006
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Can't say I've fully grasped the science behind cross-bedding yet, but I was quickly and fully hypnotized by these computer animations of sedimentary migration and deposition.
Archive 2006-01-01 2006
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Uploaded into this terrestrial machine would be all the data accumulated by the USGS on cross-bedding.
Archive 2008-07-01 2008
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Below are some screen captures taken from animations of cross-bedding formation that you can download from the U.S.
Archive 2008-07-01 2008
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So I can infer certain characteristics of the sedimentary environment from the local bedforms. ie a current of this velocity and this depth and sand grains of this diameter will result in this type of cross-bedding.
More North American Upper Treeline: Wilson-Luckman 2002, 2003 « Climate Audit 2007
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It is easy to identify this type of deposition by means of its characteristic 25-to-31-degree cross-bedding and its typically well-rounded, frosted quartz sand particles.
The Source John Clayton Nils Jansma 2001
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It is easy to identify this type of deposition by means of its characteristic 25-to-31-degree cross-bedding and its typically well-rounded, frosted quartz sand particles.
The Source John Clayton Nils Jansma 2001
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