Full text: Proceedings of Symposium on Remote Sensing and Photo Interpretation (Volume 2)

- 626 - 
remains barren. The light tone quality of this unvegetated sandy-silty 
material generally yields a conspicuous contrast with the surroundings. 
This is clearly detectable, particularly on large-scale air photographs 
together with the ridge distribution pattern and morphology. Conse 
quently, air photo interpretation may reveal coastal microrelief. 
BIBLIOGRAPHY 
Bird, B. 
1967. 
The Physiography of Arctic Canada with Special Reference 
to the Area South of Parry Channel. The John Hopkins 
Press, Baltimore Maryland. 336 pp. 
Davis, W.M. 
1902. Elementary Physical Geography, Ginn and Co. New York. 
401 pp. 
Johnson, D.W. 
1919. Shore Processes and Shoreline Development. John Wiley 
and Sons, New York. 584 pp. 
Kupsch, W.O. 
1962. Ice-thrust ridges in Western Canada. Jour. Geology, 
Voi. 45, p. 582-594. 
Mathews, W.H. and Mackay, J.R. 
1960. 
Deformation of soils by Glacier Ice and the Influence of 
Pore Pressures and Permafrost: Royal Soc. Canada Trans, 
v. 54, ser. 3, Sec. 4 p: 27-36. 
Rex, R.W. 
1955. 
Microrelief produced by sea ice grounding in the Chuckchi 
Sea near Barrow, Alaska. Arctic, Vol. 8, pp. 177-186. 
Rutten, M.G. 
1960. Ice-pushed Ridges, Permafrost and Drainage: Am. Jour. 
Sci. v. 258, p. 293-297. 
Shepard, F.P. 
1937. 
Revised Classification of Marine Shorelines, J. Geol. 
v. 45, pp. 602-624. 
1938. 
Classification of Marine Shorelines; a Reply. J. Geol. 
v. 46 pp. 996-1006. 
1963. 
Submarine Geology; 2nd ed. Harper and Row, New York pp. 557
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.