"Unstratified" Quotes from Famous Books
 ... stratified deposits; but he cannot witness the reconversion of the sedimentary into the crystalline by subterranean heat. He is in the habit of regarding all the sedimentary rocks as more recent than the unstratified, for the same reason that we may suppose him to fall into the opposite error if he saw the origin of ...
— The Harvard Classics Volume 38 - Scientific Papers (Physiology, Medicine, Surgery, Geology) • Various
... cared for in time of need (citizens as well as servants, holding a ballot as well as a broom, I tell her), and bringing back to us the lowly, underfoot virtues of contentment and humility, which we do so need to carpet the barren and hungry thoroughfare of our unstratified existence. ...
— The Autocrat of the Breakfast-Table • Oliver Wendell Holmes, Sr. (The Physician and Poet not the Jurist)
... stratified and tolerably horizontal, these rains would have cut them out into tablelands divided by deep gullies, such as may be seen in Abyssinia, and in certain parts of the western United States. But these rocks are altogether amorphous and unstratified, and have been poured or spouted out as lumps, dykes, and sheets of lava, of every degree of hardness; so that the rain, in degrading them, has worn them, not into tables and ranges, but into innumerable cones. And the process of degradation ...
— At Last • Charles Kingsley
... then, considered with respect to their first raising and first sculpture, may be conveniently divided into two great groups; namely, those made up of beds or layers, commonly called stratified; and those made of more or less united substance, called unstratified. The former are nearly always composed of coherent rocks, the latter of crystallines; and the former almost always occupy the outside, the latter the centre of mountain chains. It signifies, therefore, very little whether we distinguish the groups by calling one stratified ...
— Modern Painters, Volume IV (of V) • John Ruskin
... been shown, in various cases, to pass one into the other; as at Valorsine, near Mont Blanc, where the two, in contact, are observed to "both undergo a modification of mineral character. The granite still remaining unstratified, becomes charged with green particles; and the talcose gneiss assumes a granitiform structure without losing its stratification." In the Aberdeen-granite, lumps of unmelted gneiss are abundant; and we can ourselves bear witness that the ...
— Essays: Scientific, Political, & Speculative, Vol. I • Herbert Spencer |
