scholarly journals Surficial geology of the Queen Charlotte Basin: evidence of submerged proglacial lakes at 170 M on the continental shelf of western Canada

1993 ◽  
Author(s):  
H W Josenhans ◽  
J V Barrie ◽  
K W Conway ◽  
R T Patterson ◽  
R W Mathewes ◽  
...  
Keyword(s):  
Continental Shelf ◽  
Western Canada ◽  
Surficial Geology ◽  
Proglacial Lakes

scholarly journals Surficial Geology of the Continental Shelf off New Hampshire: Morphologic Features and Surficial Sediment

2021 ◽  
Author(s):  
Larry Ward ◽  
Zachary McAvoy ◽  
Maxlimer Coromoto Vallee-Anziani ◽  
Rachel Morrison
Keyword(s):  
Continental Shelf ◽  
New Hampshire ◽  
Surficial Sediment ◽  
Surficial Geology

scholarly journals Sponge bioherms on the continental shelf of western Canada

1989 ◽  
Author(s):  
K W Conway ◽  
J V Barrie ◽  
J L Luternauer
Keyword(s):  
Continental Shelf ◽  
Western Canada ◽  
Sponge Bioherms

Late Quaternary geology and geochronology of the central continental shelf of western Canada

1989 ◽  
Vol 89 (1-2) ◽  
pp. 57-68 ◽  
Author(s):  
John L. Luternauer ◽  
K.W. Conway ◽  
John J. Clague ◽  
Bertrand Blaise
Keyword(s):  
Continental Shelf ◽  
Late Quaternary ◽  
Quaternary Geology ◽  
Western Canada

Archaeocyathids and the Lower Cambrian Continental Shelf of the Canadian Cordillera

1975 ◽  
Vol 12 (12) ◽  
pp. 2014-2020 ◽  
Author(s):  
C. R. Stelck ◽  
A. S. Hedinger
Keyword(s):  
British Columbia ◽  
Continental Shelf ◽  
Lower Cambrian ◽  
Rocky Mountain ◽  
Canadian Cordillera ◽  
Western Canada ◽  
Early Cambrian ◽  
Structural Trend ◽  
East And West

The geographic occurrences of archaeocyathids are plotted for the Cordilleran region of western Canada. The archaeocyathids are found both east and west of, and within the Rocky Mountain Trench in British Columbia and are found east and west of the Tintina Trench in the southern Yukon. The overall pattern of the occurrences indicates that the shallow neritic portion of the continental shelf in Early Cambrian time traces a pattern widely diverse from that of the later, superimposed, Laramide structural trend. Portions of the continental shelf were already in existence west of the Rocky Mountain Trench by Early Cambrian time.

scholarly journals The Chaetognaths of Western Canadian Coastal Waters

1955 ◽  
Vol 12 (4) ◽  
pp. 593-617 ◽  
Author(s):  
Helen E. Lea
Keyword(s):  
Continental Shelf ◽  
Coastal Waters ◽  
Deep Sea ◽  
Open Ocean ◽  
Inland Waters ◽  
Western Canada ◽  
Outer Limit

Four species of chaetognaths were found in samples from 11 representative areas along the coastline of western Canada. Sagitta elegans was the most abundant and widely distributed species, occurring, at least in small numbers, in all the areas sampled. It was characteristic of the mixed coastal waters over the continental shelf and of the inland waters. Eukrohnia hamata, an oceanic form, occurred in most regions in small numbers as an immigrant, and was abundant toward the edge of the continental shelf. Sagitta lyra, strictly a deep sea species, was found only in the open waters along the outer coasts, and a few specimens of Sagitta decipiens, another oceanic form, were also taken in deep hauls from areas exposed to open ocean influence. The outer limit of Sagitta elegans corresponded with the inner limits of all three oceanic forms, though Eukrohnia hamata invaded the inland waters to some extent.

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