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Sole 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…
History, Tool marks & Load casts
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marks casts flute bed found groove object sole structures bottom mark sediment muddy tool cast long parallel generally along skip
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| a bed of algae or slumping of sediment.Drag marks are narrower | instance of | but shallow gouge left in a muddy bed caused by sliding of a soft-body object | 0.80 | text |
| deeper than slide marks | instance of | but shallow gouge left in a muddy bed caused by sliding of a soft-body object | 0.80 | text |
| but retain the same length | instance of | but shallow gouge left in a muddy bed caused by sliding of a soft-body object | 0.80 | text |
| Sole markings | related to history | Sole | 0.60 | section |
| Sole markings | related to history | Devonian | 0.60 | section |
| Sole markings | related to history | New York State | 0.60 | section |
| Sole markings | related to history | James Hall | 0.60 | section |
| Sole markings | related to history | Originally | 0.60 | section |
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