3 edition of Notes on the occurrence of Eozoon Canadense at Côte St. Pierre found in the catalog.
Notes on the occurrence of Eozoon Canadense at Côte St. Pierre
John William Dawson
|Other titles||Quarterly journal of the Geological Society., On the occurrence of Eozoon Canadense at Côte St. Pierre.|
|Statement||by J.W. Dawson.|
|Series||CIHM/ICMH Microfiche series -- no. 06862|
|The Physical Object|
|Pagination||1 microfiche (10 fr.)|
|Number of Pages||10|
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Côte St. Pierre, in the Seigniory of Petite Nation, on the river Ottawa, is the locality whence some of the most instructive specimens of Eozoon were obtained by the late Mr.
Lowe, whose collections are referred to in papers presented to this Society by Sir W. Logan and the writer. Believing that a reexamination of this place would afford a good opportunity for collecting additional Cited by: 2.
Additional Physical Format: Print version: Dawson, John William, Sir, Notes on the occurrence of Eozoon Canadense at Côte St. Pierre. Get this from a library.
Notes on the occurrence of Eozoon Canadense at Côte St. Pierre. [John William Dawson, Sir]. Notes on the occurrence of Eozoon Canadense at Côte St. Pierre [electronic resource] / By Sir J.
(John William) Dawson. Abstract. Caption title."[From the Quarterly Journal of the Geological Society for February ]"es bibliographical onic of access: Internet.4 Topics. Fig. - Stansfield (): occurence d'Eozoon canadense à Côte-St-Pierre, QC, au N de Ripon.
Quelques éléments de la légende: E: Eozoon ; A: Asbestos (amiante): Limestone: marbre ; Lac Allard: lac Charlebois d'aujourd'hui ; le chemin correspond à la route moderne. «Entre la roche à diopside [Diopside rock de la carte] et le marbre normal [Grenville limestone], se place une Author: Henri Lessard.
In members of the Geological Survey of Canada found further specimens of Eozoon at Grenville, Quebec and nearby at Côte St. Pierre. Logan tried to get Elkanah Billings involved, but he declined, and the microscopic slides of the specimens were passed to Author: Christopher Brett.
Notes On The Occurrence Of Eozoon Canadense At Caote St. Pierre: T+ 23 MB: Administering Policy For Talented And Gifted Education: T+ 20 MB: The Institution Of War: T+ 25 MB: Measuring The Water Status Of Plants And Soils: T+ 23 MB: Frank OHara. Full text of "Specimens of Eozoon canadense and their geological and other relations [microform]" See other formats.
Notes on the Occurrence of Eozoon canadense at Côte St. Pierre. Dawson. Quarterly Journal of the Geological Society, 32, Notes on the Physical Geology of East Anglia during the Glacial Period. Quarterly Journal of the Geological Society, 32,1 Februaryhttps.
Notes on the Occurrence of Eozoon canadense at Cote St. Pierre. January J. Dawson; Côte St. Pierre, in the Seigniory of Petite Nation, on the river Ottawa, is the locality whence some of. Dawson JW () Notes on the occurrence of Eozoön canadense at Côte St. Pierre. Quarterly Journal of the Geological Society London 66–75 CrossRef Google Scholar Dawson W () Note on Cryptozoon and other ancient by: "In decalcifying by means of a dilute acid some of the specimens from Côte St.
Pierre, placed in his hands inDr. Carpenter found that the action of the acid was arrested at certain portions of the skeleton, presenting a yellowish-brown surface; and he showed me, two or three weeks ago, that in a specimen recently given him, from the.
Eozoon canadense: pseudofossile découvert en dans un marbre précambrien (province de Grenville, 1 milliard d'années et plus). Localisation Côte-St-Pierre, au nord de Saint-André-Avellin, routecollines au NW du lac Charlebois (Québec).
CORRECTION (8 févr. - J'avais cru qu'on trouvait l'Eozoon sur le territoire de Ripon. Full text of "The bibliography of the Foraminifera recent and fossil, including Eozoon and Receptaculites. [i.e. ]-Jan. 1, " See other formats. Notes on the occurrence of Eozoon Canadense at Côte St.
Pierre, (short work) external scan The earthquake of November 4,(short work) external scan Lower Carboniferous fishes of New Brunswick, (short work) external scan.
Eozoon Canadense, shown in the middle to upper half of the specimen, consists of the thin 1 mm thick alternating bands of green serpentine (with grains of spinel) and bands of grey dolomite.
The banding appears as raised ridges on one weathered edge of the specimen that is in the display cabinet. You can write a book review and share your experiences.
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