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The Lowe sequence describes a set of sedimentary structures in turbidite sandstone beds that are deposited by high-density turbidity currents. It is intended to complement, not replace, the better known Bouma sequence , which applies primarily to turbidites deposited by low-density (i.e., low-sand concentration), turbidity currents.
The bib apron's humble beginnings began when people used scraps of fabric to make a bib-like covering that slipped over the neck and tied at the back. [1] The bib apron's intuitive design and full coverage have made it a popular apron for tradesmen and people in low-economic classes since the 1880s—and maybe even earlier.