Geology√

Looking south toward glacier in the background

WOK 17-89
Item
1963

Axel Heiberg. Looking south (upstream) from station 63 K 111 towards glacier in the background.

Looking toward terminus of glacier and recently abandoned moraine

WOK 17-97
Item
1963

Axel Heiberg Gr. Looking toward terminus of glacier near station 63 K 120. Notice recently abandoned moraine and ice-marginal channels in front of glacier.

Looking west from station 63 K 178

WOK 17-113
Item
1963

Part of W.O. Kupsch fonds

Axel Heiberg Gr. Looking west from station 63 K 178. Helicopter and Victor Mauguy in foreground.

Lower and middle Devonian tectonic maps

WOK 14-40
Item
[1961-62]

Part of W.O. Kupsch fonds

Lower and middle Devonian tectonic maps (Raasch et al., 1961, v. 1, p. 446).

Lower part of land slide and earth flow - Fort Qu'Appelle

WOK 3-147
Item
1956

Part of W.O. Kupsch fonds

Lower part of land slide and earth flow in tributary valley near Fort Qu'Appelle.

Lower Pennsylvanian tectonic map

WOK 14-43
Item
[1961-62]

Part of W.O. Kupsch fonds

Lower Pennsylvanian (Raasch et al., 1961, v. 1, p. 448).

Lower stratified drift Swift Current Creek section

WOK 11-143
Item
September 1960

Part of W.O. Kupsch fonds

Lower stratified drift Swift Current Creek section along north side of tributary to Swift Current Creek in Sec. 10, T. 19, R. 13, W. 3 meridian. At this place the Lower stratified drift may possible represent a weathered till (cf. Wickenden 1931 C, Sec. C) as it is not stratified, non-sorted, contains some erratics, is highly calcareous but is not a marl (organic, mainly algal, deposit) as Christiansen (1959) reported. Spade is placed on gradational zone from Wymark Till to Lower Stratified drift. Peter David holds hand on sharp contact between Lower stratified drift and AIkins Till. Tuesday September 13, 1960.

Lowest member of Whitemud formation. Near Gould's Quarry

WOK 1-115
Item
1954

Part of W.O. Kupsch fonds

Lowest member of Whitemud formation consisting of kaolinized sand. Near Gould's Quarry, Eastend, Sask.

Lunch time at the entrance to Brown's Gulch

WOK 14-71
Item
1961

Part of W.O. Kupsch fonds

Lunch time at the entrance to Brown's Gulch, Little Rocky Mountains. October, 1961.

Magnetic field of the earth

WOK 13-14
Item
1960

Part of W.O. Kupsch fonds

Magnetic field of the earth. Top chart shows the total field, which has a regular component, as might be produced by a bar magnet in the earth's core and an irregular component. The bottom chart shows the irregular component alone. This is obtained by subtracting a uniform north-south field from the total observed field. In the top chart the arrows indicate the direction in which a compass needle would point if there were no axial field. Runcorn, 1955, Sci. Am., v. 193, no. 3, p. 153.

Main physiographic and geological regions of Canada