 Thus there cannot be the shadow of a doubt as to the length of time which must have elapsed between the close of the Upper Silurian and the commencement of the Carboniferous Period, and of the greatness of the work accomplished in that time.  Geological Magazine - Page 58edited by - 1879Full view - About this book
 | Christopher Benson - Bible - 1819 - 362 pages
...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... | |
 | John Ellor Taylor - Botany - 1879 - 294 pages
...all transpired in the interval between the close of the Upper Silurian and the deposition of the Red Conglomerate of Mell Fell, ushering in the great Carboniferous...assign the formation of the various granitic centres. I have already treated of the probable pressure under which they were respectively formed, and called... | |
 | Henry Woodward - Electronic journals - 1879 - 790 pages
...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 - Electronic journals - 1879 - 634 pages
...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... | |
 | Geology - 1879 - 546 pages
...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 - Electronic journals - 1881 - 444 pages
...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 - Geology - 1885 - 878 pages
...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... | |
 | Geology - 1889 - 72 pages
...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 - 1080 pages
...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... | |
| |
