1. Sole markingsSole marks are sedimentary structures found on the bases of certain strata, that indicate small-scale (usually on the order of centimetres) grooves or irregularities. This usually occurs at the interface of two differing lithologies and/or grain sizes. They are commonly preserved as casts of these indents on the bottom of the overlying bed (like flute casts). This is similar to casts and molds in fossil preservation.
Read “Sole markings” on English Wikipedia
Read “底痕” on Japanese Wikipedia
Read “Sole markings” on DBpedia
Read “Sole markings” on English Wikipedia
Read “底痕” on Japanese Wikipedia
Read “Sole markings” on DBpedia
Discussions
Log in to talk about this word.