.... The upper interval, of probable Upper Leonardian to Guadalupian age, is represented in the upper half of the Tahkandit Format ion and contains Spiriferella rajah var B and 2. keilhavii. BASAL BELLY RIVER SANDSTONE (UPPER CRETACEOUS). PEMBINA FIELD, ALBERTA, CANADA DAULAT S I~G~ KHAMESRA 1963, University...

...) strata are designated the Lacombe Member. These strata occur as isolated outcrops upstream from Joffre Bridge along the Red Deer and Blindman river valleys, and comprise the majority of bedrock west to the disturbed belt. Adjacent to the Alberta Foothills near Hinton, strata of the Obed-Marsh coal zone...

...Figure 2 — 1 – 15, Ectypodus elaphus n. sp., Blindman River localities, middle Tiffanian (Ti3), Paskapoo Formation, Alberta. 1 – 3, UALVP 45996, right P4 in 1, labial, 2, lingual, and 3, occlusal view; 4 – 6, UALVP 46225, right M1 in 4, labial, 5, lingual, and 6, occlusal view...

... diversion of a tributary. The Drumheller oil field is reflected by a marked diversion and arcuate pattern of Michichi Creek. The Homeglen-Rimbey oil field is in the Blindman River system in which the tributaries flow southeasterly. At the oil field all streams are diverted toward the west, resuming...

... to the floras of Gao Mine and the nearby Munce’s Hill site (Tiffanian Ti4). The remainder of the taxa are common in late Paleocene floras of North Dakota, Montana, and Wyoming, all USA. The floras of the nearby Joffre Bridge Roadcut and Blindman River sites (both Tiffanian Ti3) are more diverse, but both...