| Sir Charles Lyell - 1833 - 578 Seiten
...Grampians, the opposite walls sometimes preserve an exact parallelism for a considerable distance. It is not uncommon for one set of granite veins to...as in the environs of Heidelberg, where the granite of the right bank of the Rhine is seen to consist of three varieties differing in colour, grain, and... | |
| Sir Charles Lyell - 1833 - 570 Seiten
...Grampians, the opposite walls sometimes preserve an exact parallelism for a considerable distance. It is not uncommon for one set of granite veins to...as in the environs of Heidelberg, where the granite of the right bank of the llhine is seen to consist of three varieties differing in colour, grain, and... | |
| Sir Charles Lyell - 1834 - 422 Seiten
...Grampians, the opposite walls sometimes preserve an exact parallelism for a considerable distance. It is not uncommon for one set of granite veins to...as in the environs of Heidelberg, where the granite of the right bank of the Rhine is seen to consist of three varieties, differing in colour, grain, and... | |
| sir Charles Lyell (bart.) - 1835 - 480 Seiten
...Grampians, the opposite walls sometimes preserve an exact parallelism for a considerable distance. It is not uncommon for one set of granite veins to...differing in colour, grain, and various peculiarities of mineral composition. One of these, which is evidently the second in age, is seen to cut through an... | |
| Sir Charles Lyell - 1837 - 584 Seiten
...Grampians, the opposite walls sometimes preserve an exact parallelism for a considerable distance. It is not uncommon for one set of granite veins to...differing in colour, grain, and various peculiarities of mineral composition. One of these, •which is evidently the second in age, is seen to cut through... | |
| Sir Charles Lyell - 1838 - 582 Seiten
...point of Scotland, ^_ and the southernmost extremity of Africa, as the annexed drawings will show. It is not uncommon for one set of granite veins to intersect another; and sometimes there are tliree sets, as in the environs Granite veins traversing clay slate, of Heidelberg, where the Table... | |
| Sir Charles Lyell - 1838 - 606 Seiten
...the southernmost extremity of Africa, as the annexed drawings will show. It is not uncommon for ope set of granite veins to intersect another; and sometimes there are three sets, as in the environs Granite veins traversing clay slate, of Heidelberff, where the Table Mountain, Cape of Good Hope* granite... | |
| Sir Charles Lyell - 1839 - 330 Seiten
...veins traversing clay It is not Uncommon for One Set of S Q<, t o e dxop'e4 M °'"" aia ' Cat "' ° f granite veins to intersect another; and sometimes there are three sets, as in * MacCulloch, Gcol. Trans., vol. iii. p. 259. Granite Veins. the environs of Heidelberg, where the... | |
| Anthony Nesbit - 1841 - 208 Seiten
...Materials; the lower Formation penetrating the upper variety, every where, in Veins.—Near Herdelberg, the Granite on the Banks of the River Necker, is seen...differing in Colour, Grain, and various Peculiarities of mineral Composition. One of these, which is evidently the second in Age, is seen to cut through an... | |
| 1841 - 346 Seiten
...that the granite has been in state of fusion, the heat of which has softened and ent the upper rocks. It is not uncommon for one set of granite veins to intersect another; and sometimes here are three sets, as in the vicinity of Heidelberg, where the granite on the banks of the Neekcr,... | |
| |