Here we have not facts of deposition to calculate from in this district, but those of denudation. What length of time must have elapsed between the close of the Upper Silurian and the commencement of the Carboniferous, to allow of the removal of probably... Mountain and Moor - Стр. 14авторы: John Ellor Taylor - 1879 - Страниц: 256Полный просмотр - Подробнее о книге
| Christopher Benson - 1819 - Страниц: 362
...founded. The same source, to which we have applied with success for the solution of the last question as to the length of time which must have elapsed between the death of Herod and the arrival of the Magi, will help us also, if not satisfy us, with regard to the... | |
| Henry Woodward - 1879 - Страниц: 636
...facts of deposition to calculate from in this district, but those of denudation. What length of time must have elapsed between the close of the Upper Silurian and the commencement of the Carboniferous, to allow of the removal of probably more than 20,000 feet of rock, so that the Mell Fell conglomerate... | |
| Henry Woodward - 1879 - Страниц: 634
...facts of deposition to calculate from in this district, but those of denudation. What length of time must have elapsed between the close of the Upper Silurian and the commencement of the Carboniferous, to allow of the removal of probably more than 20,000 feet of rock, so that the Mell Fell conglomerate... | |
| Henry Woodward - 1879 - Страниц: 790
...facts of deposition to calculate from in this district, but those of denudation. What length of time must have elapsed between the close of the Upper Silurian and the commencement of the Carboniferous, to allow of the removal of probably more than 20,000 feet of rock, so that the Mell Fell conglomerate... | |
| 1879 - Страниц: 546
...author, and a discussion of the changes in the physical geography of Western Europe which took place between the close of the Upper Silurian and the commencement of the Carboniferous period. It is illustrated by maps and sections. 10. Outlines of Field Geology, by ARCHIBALD GEIKIE. 216pp.... | |
| Geological Society of London - 1881 - Страниц: 444
...his memoir traces the series of changes in the physical geography of Western Europe which took place between the close of the Upper Silurian and the commencement of the Carboniferous period. Viewed in a large sense the Old Eed Sandstone of Great Britain groups itself etratigraphically into... | |
| Leeds Geological Association - 1885 - Страниц: 878
...and the immensity of time required for denudation. As has been pertinently asked, what length of time must have elapsed between the close of the upper silurian and the commencement of the carboniferous to allow of the removal of probably more than 20,000 feet of rock, so that the basement conglomerate... | |
| 1889 - Страниц: 72
...and the immensity of time required for denudation. As has been pertinently asked, what length of time must have elapsed between the close of the upper silurian and the commencement of the carboniferous to allow of the removal of probably more than 20,000 feet of rock, so that the basement conglomerate... | |
| 1879 - Страниц: 1080
...author, and a discussion of the changes in the physical geography of Western Europe which took place between the close of the Upper Silurian and the commencement of the Carboniferous period. It is illustrated by maps and sections. 10. Outlines of IField Geology, by ARCHIBALD GEIKIE. 2 1 6... | |
| |