The Numbers and Distribution of Greater Snow Geese on Bylot Island and near Jungersen Bay, Baffin Island, in 1988 And 1983

ARCTIC ◽  
1992 ◽  
Vol 45 (2) ◽  
Author(s):  
Austin Reed ◽  
Hugh Boyd ◽  
Pierre Chagnon ◽  
James Hawkings
1991 ◽  
Vol 65 (03) ◽  
pp. 361-382 ◽  
Author(s):  
H. J. Hofmann ◽  
G. D. Jackson

Coccoid and filamentous microfossils in the Borden Rift Basin on northwestern Baffin Island and western Bylot Island are reported from 14 localities at six general stratigraphic levels in the Society Cliffs Formation, and one in the Victor Bay Formation. At least seven of 12 fossiliferous Society Cliffs samples, and one of two Victor Bay samples, are from cherty dolostones formed in shallow restricted, peritidal evaporitic environments. The remaining six fossiliferous samples accumulated in somewhat deeper, less restricted waters. The assemblage is preserved in black chert nodules and layers and comprises 30 taxa, including the filamentous formsArchaeotrichion? sp.,Tenuofilum septatum, Eomycetopsis robusta, Siphonophycus inornatum, S. kestron, Rhicnonema antiquum, Brachypleganonsp.,Eomicrocoleussp.,Uluksanella baffinensisn. gen. and sp.,Talakania? sp., the coccoid taxaEosynechococcus medius, E. grandis, Archaeoellipsoides obesus, Sphaerophycus parvum, S. medium, Myxococcoides minor, M. grandis, Melasmatosphaeraspp.,Phanerosphaerops capitaneus, Palaeoanacystissp.,Tetraphycus hebeiensis, Eogloeocapsa bella, Gloeodiniopsis magna, G.sp. 1,G. mikros, Polybessurus bipartitus, Cymatiosphaera? sp., the fusiformEupoikilofusa? sp., and rare specimens of two unidentified and problematic taxa.


2017 ◽  
Vol 54 (1) ◽  
pp. 110-111
Author(s):  
C. Simon L. Ommanney

A similar investigation into calving glaciers and iceberg production on Baffin and Bylot islands was initiated by the Canadian Government in the 1970s. This is described and reference made to the Glacier Atlas of Canada, which, in identifying all individual glaciers in this region of the Canadian Arctic, obviates the need to develop an independent numbering system when individual glaciers need to be identified.


2015 ◽  
Vol 52 (11) ◽  
pp. 980-989 ◽  
Author(s):  
Wesley Van Wychen ◽  
Luke Copland ◽  
David O. Burgess ◽  
Laurence Gray ◽  
Nicole Schaffer

Speckle tracking of ALOS PALSAR fine beam data from 2007–2011 are used to determine the surface motion of major ice masses on Baffin Island and Bylot Island in the southern Canadian Arctic Archipelago. Glacier velocities are low overall, with peaks of ∼100 m a−1 and means of ∼20–60 m a−1 common along the main trunk of many outlet glaciers. Peak velocities on Penny and Bylot Island ice caps tend to occur near the mid-sections of their primary outlet glaciers, while the fastest velocities on all other glaciers usually occur near their termini due to relatively large accumulation areas draining through narrow outlets. Estimates of ice thickness at the fronts of tidewater-terminating glaciers are combined with the velocity measurements to determine a regional dynamic discharge rate of between ∼17 Mt a−1 and ∼108 Mt a−1, with a mid-point estimate of ∼55 Mt a−1, revising downward previous approximations. These velocities can be used as inputs for glacier flow models, and provide a baseline dataset against which future changes in ice dynamics can be detected.


2017 ◽  
Vol 54 (1) ◽  
pp. 112-112
Author(s):  
Wesley Van Wychen ◽  
Luke Copland ◽  
David O. Burgess ◽  
Laurence Gray ◽  
Nicole Schaffer

ARCTIC ◽  
1998 ◽  
Vol 51 (2) ◽  
Author(s):  
Denis Lepage ◽  
David N. Nettleship ◽  
Austin Reed

1987 ◽  
Vol 51 (1) ◽  
pp. 128 ◽  
Author(s):  
Austin Reed ◽  
Pierre Chagnon

Ibis ◽  
2016 ◽  
Vol 158 (4) ◽  
pp. 876-880 ◽  
Author(s):  
Anthony D. Fox ◽  
James O. Leafloor ◽  
Thorsten J. S. Balsby ◽  
Kathryn M. Dickson ◽  
Michael A. Johnson ◽  
...  

Bird-Banding ◽  
1974 ◽  
Vol 45 (3) ◽  
pp. 217
Author(s):  
J. Douglas Heyland ◽  
David B. Wingate ◽  
N. N. Powe
Keyword(s):  

1995 ◽  
Vol 83 (4) ◽  
pp. 653 ◽  
Author(s):  
Gilles Gauthier ◽  
R. John Hughes ◽  
Austin Reed ◽  
Julien Beaulieu ◽  
Line Rochefort
Keyword(s):  

Author(s):  
Moira Dunbar ◽  
M. J. Dunbar

In 1616 William Baffin, coasting up the icebound west coast of Greenland, reported: ‘The first of July we were come into an open sea, in the latitude of 75 degrees 40 minutes, which a new revived our hope of a passage…’ (Purchas 1625). From this point, at an unspecified longitude in the north part of Melville Bay, he cruised for 12 days in open water, up the Greenland coast to 77°30'N and down the west side of Baffin Bay to Bylot Island, seeing and naming on the way Smith, Jones, and Lancaster sounds. From Bylot Island south he found ‘a ledge of ice between the shoare and us’ as he continued past Pond Inlet and down the coast of Baffin Island. This is the first mention in written records, and the first known navigation, of an area that became well known two centuries later as the ‘North Water’.


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