Crag-and-tail features: convergent ice flow through Eclipse Sound, Baffin Island, Arctic Canada

2016 ◽  
Vol 46 (1) ◽  
pp. 55-56 ◽  
Author(s):  
E. K. Dowdeswell ◽  
B. J. Todd ◽  
J. A. Dowdeswell
Geomorphology ◽  
2008 ◽  
Vol 97 (1-2) ◽  
pp. 126-134 ◽  
Author(s):  
Jason P. Briner ◽  
Gifford H. Miller ◽  
Robert Finkel ◽  
Dale P. Hess

2016 ◽  
Vol 46 (1) ◽  
pp. 193-194 ◽  
Author(s):  
E. K. Dowdeswell ◽  
B. J. Todd ◽  
J. A. Dowdeswell
Keyword(s):  

2019 ◽  
Vol 176 (6) ◽  
pp. 1093-1106 ◽  
Author(s):  
Scott Jess ◽  
Randell Stephenson ◽  
Søren B. Nielsen ◽  
Roderick Brown

1985 ◽  
Vol 31 (108) ◽  
pp. 99-107 ◽  
Author(s):  
N. F. Mcintyre

AbstractA comparison of data from aircraft altimetry, Landsat imagery, and radia echo-sounding has shown characteristic surface topographies associated with sheet and stream flow. The transition between the two is abrupt and occurs at a step in the subglacial topography. This marks the onset of basal sliding and high velocities caused by subglacial water; it results in crevassed amphitheatre-like basins round the head of outlet glaciers. It is also the zone of maximum driving stress beyond which values decline rapidly as velocities increase. This abrupt transition appears to be topographically controlled since basal temperatures are at the pressure-melting point well inland of the change in regime. The Marie Byrd Land ice streams exhibit qualitative differences from other ice-sheet outlets, however; the change to lower driving stresses is much more gradual and occurs several hundred kilometres inland. Such ice streams have particularly low surface slopes and appear in form and flow regime to resemble confined ice shelves rather than grounded ice. The repeated association of the transition to rapid sliding with a distinct subglacial feature implies a stabilizing effect on discharge through outlet glaciers. Acceleration of the ice is pinned to a subglacial step and propagation of high velocities inland of this feature seems improbable. Rapid ice flow through subglacial trenches may also ensure a relatively permanent trough through accentuation of the feature by erosion. This is concentrated towards the heads of outlet glaciers up-stream of the region where significant basal decoupling occurs. This may be a mechanism for the overdeepening of fjords at their inland ends and the development of very steep fjord headwalls.


1989 ◽  
Vol 63 (1) ◽  
pp. 25-33 ◽  
Author(s):  
Rong Jia-Yu ◽  
Brian Jones ◽  
F. W. Nentwich

Proconchidium brodeurensis n. sp. occurs 212 m above the base of member B of the Baillarge Formation on Brodeur Peninsula, Baffin Island, 8 m below the Ordovician–Silurian boundary. Study of Proconchidium shows that it can be easily distinguished from Eoconchidium but possesses many characters that are similar to those in Tcherskidium. Analysis of internal structures suggests that the three genera can be distinguished from each other and belong to Virgianidae. Tcherskidiidae is a synonym of Virgianidae and should be abandoned.This represents the first recorded occurrence of Proconchidium in North America. Although this genus and its related genera Tcherskidium Sapelnikov, 1972, and Eoconchidium Rozman, 1967, are common in Ashgill strata of Eurasia, they have not been recorded or illustrated from North America. This led to the suggestion that distinct brachiopod biogeographic provinces may have existed during the Ashgill. The occurrence of these genera probably indicates that they may have lived in mostly tropical and subtropical zones.


2009 ◽  
Vol 25 (2) ◽  
pp. 146-161 ◽  
Author(s):  
Elizabeth K. Thomas ◽  
Jason Szymanski ◽  
Jason P. Briner

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