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W
Smith, D. G., Jol H. M., Smith N. D., Kostaschuk R. A., & Pearce C. M. (2005).  The wave-dominated William River Delta, Lake Athabasca, Canada : its morphology, radar stratigraphy, and history. In L. Giosan and J. P. Bhattacharya, editors, River deltas - concepts, models and examples. SEPM Special Publication 83, 295-318.
T
Muwais, W. K., & Smith D. G. (1990).  Types of channel fills interpreted from dipmeter logs in the McMurray Formation, northeastern Alberta. 38(1), 53-63.
Smith, D. G. (1988).  Tidal bundles and mud couplets in the McMurray Formation, northeastern Alberta, Canada. 36, 216-219.
S
Smith, D. G. (1980).  Saskatchewan's sand dunes, a touch of Araby. 100(5), 24-29.
R
Smith, D. G., & Lynch G. M. (1974).  Red Cap sheep : their movements and migrations (1973 progress).
P
Rempel, L. L., & Smith D. G. (1998).  Postglacial fish dispersal from the Mississippi refuge to the Mackenzie River Basin. 55, 893-899.
Ellis, D. H., Lewis J. C., Gee G. F., & Smith D. G. (1992).  Population recovery of the whooping crane with emphasis on reintroduction efforts : past and future. 142-150.
N
Smith, D. G. (1975).  Natives and outsiders: Pluralism in the Mackenzie River Delta. Abstract
M
Smith, D. G. (1988).  Modern point bar deposits analogous to the Athabasca oil sands, Alberta, Canada. 417-432.
Smith, D. G. (1988).  Modern point bar deposits analogous to the Athabasca oil sands, Alberta, Canada. 417-432.
Smith, D. G. (1985).  Modern analogues of the McMurray Formation channel deposits, sedimentology of meso-tidal-influenced meandering river point bars with inclined beds of alternating mud and sand. Project No. 391, 78.
Smith, D. G. (1987).  Meandering river point bar lithofacies models: modern and ancient examples compared. Spec. Pub.39, 83-91.
L
Rhine, J. L., & Smith D. G. (1988).  The late Pleistocene Athabasca braided delta of northeastern Alberta, Canada: a paraglacial drainage system affected by aeolian sand supply. 158-169.
Rhine, J. L., & Smith D. G. (1988).  Late Pleistocene Athabasca braid delta of northeastern Alberta, Canada: a paraglacial drainage system affected by aeolian sand supply. 158-169.
Smith, D. G. (1987).  Landforms of Alberta.
Smith, D. G. (1991).  Lacustrine deltas. 35(3), 311-316.
G
Smith, D. G., & Fisher T. G. (1993).  Glacial Lake Agassiz : the north-western outlet and paleoflood. 21, 9-12.
Fisher, T. G., & Smith D. G. (1994).  Glacial Lake Agassiz : its northwest maximum extent and outlet in Saskatchewan (Emerson phase). 13, 845-858.
Smith, D. G., & editors Harris S. A. (1977).  Geomorphology of Banff Park and the Columbian Icefield.
Jol, H. M., & Smith D. G. (1992).  Geometry and structure of deltas in large lakes: a ground penetrating radar overview. Special Paper 16, 159-168.
E
Fisher, T. G., & Smith D. G. (1993).  Exploration for Pleistocene aggregate resources using process-depositional models in the Fort McMurray area. 20, 71-80.
Smith, D. G. (1979).  Effects of channel enlargement by river ice processes on bankfull discharge in Alberta, Canada. 15(2), 469-475.
C
Smith, D. G. (1989).  Catastrophic paleoflood from Glacial Lake Agassiz 9,900 years ago in the Fort McMurray region, northeast Alberta. p. 47.
Smith, D. G. (1977).  Canada's boreal desert : the Athabasca sand dunes, a geomorphological anomaly and inventory. 6(2), 406.
B
Smith, D. G., Wishart W. D., & Lynch G. M. (1977).  Bighorn ram movement at Cadomin, Alberta (1975-76 Progress). Unpublished report AFW-77-060, 23.

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