THE GREAT ICE AGE, AND ITS RELATION TO THE ANTIQUITY OF MAN1877 |
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accumulations ancient angular aphelion appear arctic åsar basin beds blocks boulder-clay boulders brick-clay Britain Bute Caithness climate Clyde coast cold Cumbrae Cumbrae College Dalmuir depth districts drift Duntroon earth erratics evidence flow fossils fresh-water Garvel Park Genus Geol Geological geologists glace glacial deposits glacial epoch glaciers Glen gravel gravel and sand Greenland Greenock ground heat height hemisphere hills hippopotamus hollows ice-sheet icebergs inter-glacial period intercalated islands kames Kilchattan Kilchattan Tile-work Kyles of Bute lakes land latitudes Linn Loch Lochgilp low-grounds lower Lowlands mammalia marine mass mer de glace morainic débris mountain valleys neolithic northern occur Paisley paleolithic peat peat-mosses Peeblesshire post-glacial pre-glacial present raised beaches reached regions ridges river river-gravels rock-basins sand and gravel Scotland Scottish sea-lochs shells silt slopes Southern Uplands stones stony clay streams submergence summer surface temperature terraces thickness trace West Tarbert winter woolly rhinoceros
Beliebte Passagen
Seite 149 - It is better, on this account, in graduating the bottle, to make two scratches as represented in the drawing, one at the top and the other at the bottom of the curve : this prevents any future mistake.
Seite 121 - He finds, however, that though the effect of this change on the mean temperature of the year may be small, the effect on the extreme temperature of the seasons will be much more considerable; " so as to produce alternately, in the same latitude of either hemisphere, a perpetual spring, or the extreme vicissitudes of a burning summer and a rigorous winter.