 ... older date, there occur in this part of France a multitude of volcanic cones like those in Auvergne, produced, in all probability, each by a single eruption. These cones are much more dilapidated than the majority of those near Clermont, of which...  The Geology and Extinct Volcanos of Central France - Seite 178von George Poulett Scrope - 1858 - 258 SeitenVollansicht - Über dieses Buch
 | William Gifford, Sir John Taylor Coleridge, John Gibson Lockhart, Whitwell Elwin, William Macpherson, William Smith, Sir John Murray (IV), Rowland Edmund Prothero (Baron Ernle) - 1827 - 624 Seiten
...than the majority of those near Clermont, of which chain they appear to constitute the prolongation. ' They are so thickly sown along the axis of the granitic range that separates the Loire and Allierfrom Paiilhaguet to Pradelle, as generally to touch each other by their bases, and form an almost... | |
 | William Gifford, Sir John Taylor Coleridge, John Gibson Lockhart, Whitwell Elwin, William Macpherson, William Smith, Sir John Murray (IV), Rowland Edmund Prothero (Baron Ernle) - 1827 - 634 Seiten
...Clermont, of which chain they appear to' constitute the prolongatibn. ' They are so thickly sown along tbe axis of the granitic range that separates the Loire and Allier from Paidhaguet to Pradelle, as generally to touch each other by th<?ir bases, and form an almost continuous... | |
 | Andrew Ure - 1829 - 704 Seiten
...thickly sown along the axis of the granitic range, that separates the Loire and Allier from Palhaguet to Pradelle, as generally to touch each other by their bases, and thus to form an almost continuous chain. Germany, particularly on the banks of the Rhine, in Hessia,... | |
 | 1827 - 630 Seiten
...than the majority of those near Clermont, of which chain they appear to constitute the prolongation. ' They are so thickly sown along the axis of the granitic range that separates the Loire and Allierfrom Paulhaguet to Pradelle, as generally to touch each other by their bases, and form an almost... | |
 | George Poulett Scrope - 1858 - 362 Seiten
...broken forth are still marked by numerous volcanic cones of scoriae, whose projection, as in Auvergno, accompanied the development of the volcanic phenomena....few being also found on the further side of each. Between-Pradelle and Aubenas they occur more rarely, and none to the south of the latter town. There... | |
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