II.—On the Wenlock and Ludlow Strata of the Lake District

J. E. Marr

doi:10.1017/S0016756800196189

Extract

The beds above the Borrowdale volcanic group, and below the Coniston Flags, have been treated, in detail in other communications, but, notwithstanding all that has been written of the higher Silurian rocks of the Lake District, something remains to be said about them.

References

^{page 535 note 1} For use of this term, and those of the subdivisions of the Coldwell Beds, see Marr, , Q.J.G.S. vol. xxxiv. p. 880.Google Scholar

^{page 536 note 1} GEOL. MAG. Decade III. Vol. IV. p. 37.

^{page 536 note 2} Geology of the Country around Ingleborougb, p. 13.

^{page 540 note 1} Cf. Tullberg, Skånes graptoliter. Part I. p. 14.

^{page 540 note 2} Cf. Aft. ur. geol. Fören. i. Stockholm Fördhandl. 1880, No. 59, Bd. V. No. 3.

^{page 541 note 1} Survey Memoir, Geology of the Country about Kendal, Sedbergh, etc., p. 16.

^{page 541 note 2} GEOL. MAG. Decade 1. Vol. X. p. 519.

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II.—On the Wenlock and Ludlow Strata of the Lake District

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