﻿<?xml version="1.0" encoding="utf-8"?>
<rdf:Description rdf:about="https://catalogues.royalsociety.org:443/CalmView/record/catalog/PP/10/40" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/">
  <dc:title>Paper, 'Note on the geological bearing of Mr Davison’s paper' by Thomas George Bonney</dc:title>
  <dc:description>Bonney writes: 'The results obtained by Mr Davison ['On the distribution of strain in the Earth's crust resulting from secular cooling, with special reference to the growth of continents and the formation of mountain-chains', Proceedings of the Royal Society, volume 42] throw light upon one or two matters in regard to the petrology of the older rocks, which have always appeared to me difficult of explanation. I venture therefore to add a brief note to his paper, written from the point of view of a geologist.'

Annotations in pencil and ink.

Subject: Geology / Petrology

Received 7 April 1887. Read 5 May 1887.

A version of this paper was published in volume 42 of the Proceedings of the Royal Society as 'Note on the geological bearing of Mr. Davison’s paper'.</dc:description>
  <dc:date>1887</dc:date>
</rdf:Description>