Abstract
ABSTRACT Three unusual sedimentary structures are described. An exact displaced image of mud cracks on the same bedding plane surface as the mud cracks themselves may have been produced during deformation. Parallel, low, uneven ridges were probably formed by sand-laden wind passing over damp exposed sediment on which the sand became trapped. It is suggested that numerous, low mounds on a bedding plane surface were produced by large, closely-spaced rain drops falling on dry unconsolidated sand.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.