Glacial erosion at the fjord onset zone and implications for the organization of ice flow on Baffin Island, Arctic Canada

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. 55-56 ◽  
Author(s):  
E. K. Dowdeswell ◽  
B. J. Todd ◽  
J. A. Dowdeswell

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

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

1984 ◽  
Vol 30 (105) ◽  
pp. 241-243 ◽  
Author(s):  
Johannes Krüger

AbstractClasts modified by glacial erosion are described from lodgement tills in front of the glacier Mýrdalsjökull, south Iceland. Many clasts show modification of their lower surfaces in the same way as their upper ones. However, the lower surfaces have a smoothed down-glacier face and a truncated up-glacier face, which is the opposite orientation to that of the upper surfaces. This so-called double stoss-lee form is interpreted as a response to basal transport over abrading materials, following deposition of the clast and succeeded by glacial erosion. It is suggested that clasts with a double stoss-lee form are a diagnostic criterion for subglacial deposition by lodgement. Furthermore, the distribution and orientation of clasts with a stoss-lee form was investigated on a ground-moraine surface. 17.3% of 2199 clasts with an a-axis diameter > 30 cm had a stoss-lee form. The proportion of clasts with their smoothed ends facing up-glacier within ± 22.5° of the ice-flow direction was 72.7%. Thus, the preferred stoss-side orientation is closely related to the ice movement and indicates the direction from which the ice came. Only 11.7% of boulders with a divergent stoss-side orientation are located in connection with annual moraines. It is suggested that such boulders have mainly been re-deposited beneath the ice and not at the ice front by minor advances of the glacier.


Sign in / Sign up

Export Citation Format

Share Document