The late Mr Blackadder, C.E., appears to have presented two papers on local superficial geology to the Wernerian Society, one of which appears in their memoirs, while the unpublished one contains sections of the superficial deposits on which Edinburgh is built. Many of the sections have since appeared in print; but some of the MSS. ones are interesting, as they shed light on recent investigations on this department of local geology. At Fettes Row clayey sand belts were seamed with vertical belts of coal grains; while nearer Bellevue the brown clayey strata, speckled with traversing lines of minute coal grains, in some places became segregated into a firm rock. Here, too, in an exposure of 8 feet, were found vertical crooked openings in the stratified sand of the nature of veins, and filled with foreign matter. They occurred from a depth of a few inches to that of 10 feet, the deeper ones of 10 feet extending many yards horizontally and in a crooked course. Sometimes four or five of those veins were seen a foot or two apart. The direction of the beds was horizontal or slightly inclined. A section at Ann Street is interesting, when connected with similar superficial beds changed into hard stone near the old City Poor House, described to this Society. The following was the section:—1. Gravel. 2. Gravel to the thickness of 3 feet cemented into a calcareous mass, which gradually thinned away into the general mass of loose gravel. In the interstices betwixt
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