 Permian (Trias) period the footprints of the gigantic birds which trod its surface before it sank ; and to surmise that the intermediate body of the land-wave, along which the Dinornis may have travelled to New Zealand, has progressively subsided, and...  Journal of the Royal Geological Society of Ireland - 297 페이지저자: Royal Geological Society of Ireland - 1849전체보기 - 도서 정보
 | 1854 - 410 페이지
...of Travel » LjeU s ™ncil,l«i of Geology. Geological Conclusions on New Zealand* 293 stable and shifting crust of the earth, of which the opposite end, after having been submerged, has again risen with its accumulated deposits in North America, shewing in the Connecticut... | |
 | 1854 - 530 페이지
...Geology. \ Ibid. § Dr John Davy. || Ly ell's Principles of Geology. ^ Incidents of Travel. stable and shifting crust of the earth, of which the opposite end, after having heen submerged, has again risen with its accumulated deposits in North America, shewing in the Connecticut... | |
 | 1858 - 814 페이지
...almost be disposed to regard New Zealand as one end of the mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite end, after...again risen with its accumulated deposits in North Ameiica, showing us in the Connecticut Sandstones of the Permian period the foot-prints of the gigantic... | |
 | Society for the diffusion of useful knowledge - 1858 - 808 페이지
...almost be disposed to regard New Zealand as one end of the mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite end, after...again risen with its accumulated deposits in North Ameiica, showing us in the Connecticut Sandstones of the Permian period the foot-prints of the gigantic... | |
 | George Ripley, Charles Anderson Dana - 1859 - 814 페이지
...almost be disposed to regard New Zealand as one end of a mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite end, after...the Connecticut sandstones of the permian period the footprints of the gigantic birds which trod its surface before it sank; and to surmise that the intermediate... | |
 | John Holmes Agnew, Walter Hilliard Bidwell, Henry T. Steele - 1864 - 554 페이지
...of the mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite cud, after having been long submerged, has again risen with its accumulated deposits in North America, showinsj us in the Connecticut sandstones of the Permian period the footprints of the gigantic birds... | |
 | Charles Knight - 1866 - 586 페이지
...almost be disposed to regard New Zealand as one end of the mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite end, after having been long submerged, has again riaen with its accumulated deposits in North America, showing us in the Connecticut Sandstones of the... | |
 | 1883 - 586 페이지
...almost be disposed to regard New Zealand as one end of a mighty wave of the unstable and evershifting crust of the earth, of which the opposite end, after...showing us in the Connecticut sandstones of the Permian (Trias) period the footprints of the gigantic birds which trod its surface before it sank ; and to... | |
 | Atholl Anderson - 2003 - 262 페이지
...America by proposing that New Zealand lay at 'one end of a mighty wave of the unstable and ever-shifting crust of the earth, of which the opposite end, after having been submerged, has again risen with its accumulated deposits in North America . . . [while] the intermediate... | |
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