 | Sir Charles Lyell - 1841 - 486 Seiten
...Jura, a chain which lies to the north of this valley. The average height of the Jura is about one third that of the Alps, and is now entirely destitute of...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | sir Charles Lyell (bart.) - 1863 - 578 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | Sir Charles Lyell - 1863 - 634 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | Sir Charles Lyell - 1863 - 546 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | Sir Charles Lyell - 1863 - 558 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | Sir Charles Lyell - 1863 - 556 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...astonished and perplexed the geologist for more than half 11 century. No conclusion can bo more incontestable than that these angular blocks of granite, gneiss,... | |
 | Sir Charles Lyell - 1863 - 564 Seiten
...of glaciers; yet it presents almost everywhere moraines, and polished and grooved surfaces of rocks. The erratics, moreover, which cover it present a phenomenon...astonished and perplexed the geologist for more than half u century. No conclusion can bo more incontestable than that these angular blocks of granite, gneiss,... | |
 | Sir Charles Lyell - 1865 - 830 Seiten
...of the Jura is about one-third that of the Alps, and it is now entirely destitute of glaciers ; yc-t it presents almost everywhere similar moraines, and...more than half a century. No conclusion can be more incontestable than that these angular blocks of granite, gneiss, and other crystalline formations,... | |
 | Sir Charles Lyell - 1866 - 866 Seiten
...of the Alps, and it is now entirely destitute of glaciers; yet it presents almost everywhere simular moraines, and the same polished and grooved surfaces...cavities. The erratics, moreover, which cover it, presents a phenomenon which has astonished and perplexed the geologist for more than a half a century.... | |
 | Sir Charles Lyell - 1871 - 656 Seiten
...the north of this valley. The average height of the Jura is about one-third that of the Alps, and it is now entirely destitute of glaciers ; yet it presents...moraines, and the same polished and grooved surfaces. The erratics, moreover, which cover it, present a phenomenon which has astonished and perplexed the... | |
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that of the Alps, and is now entirely destitute of glaciers, yet it presents almost everywhere similar moraines, and the same polished and grooved surfaces, and waterworn cavities. The erratics, moreover, which cover it, present a phenomenon which has... 
