Fault between grey limestone beds of Cretaceous Ayavacas formation in foreground and Tertiary Puno beds in background. At Ayavacas village.

Fault due to slumping in Whitemud and Frenchman formations. South side of Frenchman Valley near Whitemud Post Office.

Fault in Bearpaw (shale to right against sand to left); unconformably overlain by till. Lacustrine silts on till. Tributary to Snakebite Creek.

Fault scarp cutting throuh school, Anchorage.

Faults in deformed sand and gravel under till near Moose Jaw.

Femur of dinasaur at the base of Frenchman formation in sand facies with conglomerate. Swift Current Creek, Sask. "Corky" Jones excavating, Norman McIver watching.

Ferris of Number 1 coal seam at base of Ravenscrag (Paleocene) formation at type section. Notice shale break. Ravenscrag, Butte, Sask.

This fonds contains personal and research files on various topics, including a study of the Clwydian Range in North Wales, petrology, mineralogy, soil composition, oil and gas, sodium sulphate and soil mapping. In addition, there are a considerable number of area studies for Alberta, Saskatchewan, Manitoba, and specifically the Lloydminister area, as well as 75 research reports done for private companies. There are also articles on poetry and the theatre - two of Professor Edmunds's personal interests.

Fill terrace south of Oxbow, Sask.

First and last of the titanotheres. Right, Eotitanops of the Eocene epoch, left, Brontotherium of the Oligocene epoch. The latter stood about 8 feet high at the shoulders.

Flank of Cantaur field looking west along north boundary of T. 16, R. 16, W.3. Saline Lake in foreground.

"Flaring" of gully. Where gully at left has out through the drift into the underlying Bear Paw Shale noticeable "flaring" occurs and a wide bowl-shaped valley is formed, which is widened mainly by miniature pedimentation on the Bear Paw shales and which is used as a city dump area because it is a relatively hidden depression. Swift Current, old city dump. November 7, 1962.

Flat irons. Strata on end. Utah.

Flat-topped dolomite fill stone showing different sized striations in many directions. West of Halbrite, Sask. May, 1962.

Flaxville Pliocene (?) gravels at base overlain by about 2 feet basal till and up to 10 feet of stony ablation till. South edge of Loring Plateau where road descends into the Milk River Valley, outcrop along Loring-Malta road. April 1964.