 ... beds. They are named the Kintla formation from their occurrence in mountains on the 49th parallel, northeast of Upper Kintla lake. They also form conspicuous peaks west of Little Kootna creek. The Kintla formation closely resembles the Grinnell, and...  Bulletin of the Geological Society of America - Seite 322von Geological Society of America - 1902Vollansicht - Über dieses Buch
 | Geological Society of America - 1902 - 756 Seiten
...calcareous beds. They are named the Kintla formation from their occurrence in mountains on the 49th parallel, northeast of Upper Kintla lake. They also...thickness is not known, and the series remains incomplete. CA RBOXIFBRO US— rAKtNIKAK LIMESTONE It having been determined by the work of McConnell and Dawson... | |
 | Geological Society of America - 1902 - 746 Seiten
...calcareous beds. They are named the Kintla formation from their occurrence in mountains on the 49th parallel, northeast of Upper Kintla lake. They also...thickness is not known, and the series remains incomplete. CA RBONIFEROUS— YA KINIKA K LIMESTONE It having been determined by the work of McConnell and Dawson... | |
 | Thomas Chrowder Chamberlin - 1906 - 1060 Seiten
...also occasional beds of white quartzite and some calcareous; thickness 800 feet; no upper limit seen.3 The Kintla formation closely resembles the Grinnell,...total thickness is not known, and the series remains incomplete.4 Discussion. — The very similar general nature of these formations at a distance of 150... | |
 | Thomas Chrowder Chamberlin - 1906 - 850 Seiten
...also occasional beds of white quartzite and some calcareous; thickness 800 feet; no upper limit seen.3 The Kintla formation closely resembles the Grinnell,...total thickness is not known, and the series remains incomplete.4 Discussion. — The very similar general nature of these formations at a distance of 150... | |
 | Joseph Barrell - 1919 - 620 Seiten
...also occasional beds of white quartzite and some calcareous; thickness 800 feet; no upper limit seen.3 The Kintla formation closely resembles the Grinnell,...total thickness is not known, and the series remains incomplete.4 Discussion. — The very, similar general nature of these formations at a distance of... | |
 | Joseph Barrell - 1907 - 242 Seiten
...to correspond to the Marsh shale. Willis notes c in the Kintla argillite the casts of salt crystals "apparently significant of aridity, as the red character is of subaerial oxidation." ABSENCE OF PALEOZOIC AND MESOZOIC FORMATIONS. Within the limits of the district the sedimentary formations... | |
 | Geological Survey (U.S.) - 1907 - 234 Seiten
...to correspond to the Marsh shale. Willis notes c in the Kintla argillite the casts of salt crystals "apparently significant of aridity, as the red character is of subaerial oxidation." ABSENGE OF PALEOZOIC AND MESOZOIC FORMATIONS. Within the limits of the district the sedimentary formations... | |
 | 1912 - 682 Seiten
...Kintla formation closely resembles the Grinnell, and represents a recurrence of conditions favourable to deposition of extremely muddy, ferruginous sediment....is not known, and the series remains incomplete.'* To Willis' account the following details may be added for this section. The basal member is sixty feet... | |
 | Reginald Aldworth Daly - 1912 - 718 Seiten
...Kintla formation closely resembles the Grinnell. and represents a recurrence of conditions favourable to deposition of extremely muddy, ferruginous sediment....is not known, and the series remains incomplete.'* To Willis' account the following details may be added for this section. The !i;ia! member is sixty... | |
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