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" in the midland counties, the Fuller's earth rock of Mr. Smith does by no means furnish a constant or wellmarked line of distinction between the middle (great or Bath) oolite and the inferior oolite ; and I am decidedly of opinion, that in the northern... "
Illustrations of the Geology of Yorkshire, Or, A Description of the Strata ... - Página 154
por John Phillips - 1829 - 192 páginas
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Geological Notes

Henry Thomas De La Beche - 1830 - 132 páginas
...oolite. Mr. Phillips observes (Illustrations, &c. p. 158), "In the midland counties, the fuller's earth rock of Mr. Smith does by no means furnish a constant...throughout Rutland and Lincolnshire, there is but one thick oolite rock beneath the cornbrash, resting upon brown sandstone which immediately covers the upper...
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Report of the ... Meeting of the British Association for the ..., Volumen17

British Association for the Advancement of Science - 1848 - 784 páginas
...opinion previously published by Professor J. Phillips, that "in the midland counties, the Fuller's earth rock of Mr. Smith does by no means furnish a constant...sandstone, which immediately covers the upper lias shale." (Geol. York, vol. ip 130.) The upper lias which forms the base of the series here described, occurs...
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Report of the Annual Meeting

British Association for the Advancement of Science - 1848 - 680 páginas
...J. Phillips, that " iu the midland counties, tie Fuller's earth rock of Mr. Smith does by no meaos furnish a constant or wellmarked line of distinction...and throughout Rutland and Lincolnshire, there is bat one thick oolitic rock beneath the cornbrash, resting upon brown sandstone, which immediately covers...
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Report of the ... and ... Meetings of the British ..., Volumen17,Parte1847

British Association for the Advancement of Science. Meeting - 1848 - 754 páginas
...opinion previously published by Professor J. Phillips, that " in the midland counties, the Fuller's earth rock of Mr. Smith does by no means furnish a constant...sandstone, which immediately covers the upper lias shale." (Geol. York, vol. ip 130.) The upper lias which forms the base of the series here described, occurs...
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