Studying glacial drift in NW. England, he finds evidence of intense glacial activity, but the molluscan fauna does not appear to indicate a low sea temperature. Requests information on Tierra del Fuego molluscs for comparison.
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Studying glacial drift in NW. England, he finds evidence of intense glacial activity, but the molluscan fauna does not appear to indicate a low sea temperature. Requests information on Tierra del Fuego molluscs for comparison.
Sends his paper ["Tidal action as a geological cause", Proc. Liverpool Geol. Soc. 2 (1874): 50–72].
Has not yet studied CD’s list of South American molluscs.
TMR believes rate of limestone formation is same now as in past.
He expects his address [of 10 Oct 1876] on geological time [Proc. Liverpool Geol. Soc. 3 (1878): 211–35], which contradicts William Thomson’s view of the earth’s age, to appear soon.
Sends his paper ["Oceans and continents", Geol. Mag. 7 (1880): 385–91].
Thinks John Murray of Edinburgh goes out of his way to deny an elevation/subsidence view of coral reefs ["On the structure and origin of coral reefs and islands", Proc. R. Soc. Edinburgh 10 (1878–80): 505–18].
Argues against volcanic origin of coral islands and for the submergence of continents. Cites Judd’s argument on the volcanoes of the moon.
Praise for Earthworms.