Published online by Cambridge University Press: 01 May 2009
At the last meeting of the British Association certain facetted pebbles derived from the Olive group of the Salt Range, and presumably of glacial origin, were exhibited and commented on. Some doubt appears to have been expressed as to their being due to glacial action. The following notes on these pebbles and the bed they were derived from may prove of interest.
page 32 note 1 1 See Geol. Mag. 1886, Decade III. Vol. III. pp. 492, 494, 574.Google Scholar
page 34 note 1 Geol. Mag. Dec. II. Vol. IV. p. 293 (1877).Google Scholar