Lanterna Rally

Author: Edinburgh Mus. Of Sci. And Art

Publisher: Rarebooksclub.com

Published: 2013-09

Total Pages: 46

ISBN-13: 9781230191355

This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1870 edition. Excerpt: ...occasionally occur in the upper clays, even as far south as the coasts of Northumberland and Durham. No chalk now occurs in situ in Scotland, though, from the abundance of flints and other evidence in Banffshire and Aberdeenshire, there is reason to suppose that a portion of the chalk formation may exist under the Moray Firth and adjacent portions of the North Sea. The chalk fragments in the drift-clays of Mid-Lothian, probably either came from this area, or even from Denmark or the south of Scandinavia, where the chalk is still found. Hence, while the chief trend of the floating ice was eastward or south-eastward from the Highland mountains across the submerged plains of the midland counties, there were nevertheless occasional stray ice-floes, which found their way from the north of Scotland or from Scandinavia, and dropped their frozen sand and stones over the basin of the Firth of Forth. Nos. 360, 361 exhibit specimens of the minute forms of marine organisms which are found in the brick-clays. The skeleton of a seal was obtained from the Portobello clays a few years ago. From some of the higher parts of the clays, hazel-nuts, with other drifted land vegetation (359), and shells of Scrobicularia piperata--a mollusc still living in the estuary of the Forth--have been obtained. 318. Striated Stone. From boulder-clay. North Medwin Water, Lanarkshire. The following thirty-two specimens were obtained from the cuttings in boulderclay made for the new poorhouse at Craiglockhart, near Edinburgh. Nos. 319 to 327 inclusive have been derived from the rocks of the Highlands. Nos. 328 to 335 have, in all likelihood, come from the Lower Old Red Sandstone series of the Ochil Hills. Nos. 336 to 350 are from the Carboniferous area which stretches...