...Glen S. Stockmal Abstract Recent mapping in the Blairmore East-Half map area indicates a pop-up structure transected by the Crowsnest River, near the leading edge of Eastern Cordilleran deformation. At scenic Lundbreck Falls, the sub-horizontal attitude of the Santonian Virgelle Formation (Milk...

...Lorne R. P. Rosenthal; Roger G. Walker Abstract The Chungo Member of the Wapiabi Formation (Campanian) shales out northward and (or) eastward from Lundbreck to the Bow Valley, southern Alberta. At Lundbreck, basinal mudstones are overlain by turbidite and hummocky cross-stratified sandstones...

... it is transitional and conformable. The major section of the Bearpaw that we studied is on the Crowsnest River in Lsd. 15 and 16, Sec. 26, Tp. 7, R. 2, W. 5 Mer., just north of Lundbreck (Fig. 6). Unfortunately, neither the lower nor the upper contact is exposed here, where the formation is calculated to be 915 ft...

... CITED Bullock , A. , 1980 , Sedimentation of the Wapiabi-Belly River transition (Upper Cretaceous) at Lundbreck Falls, Alberta : B.Sc. thesis, McMaster Univ . Hunter , D. F. , 1980 , Changing depositional environments in the Wapiabi-Belly River transition (Upper Cretaceous) near...

... The Alberta shale embraces the Colorado (Benton) and Montana series, but it is differentiable into these elements only on a faunal basis. Two formations or monothems 2 are recognized in the Alberta. The lower of these was termed Blackstone shale by Malloch in 1911. 3 The Blackstone is entirely...

... ( Fig. 1 ). Lithostratigraphic units included in the study area are the Upper Cretaceous Lundbreck Formation, the Willow Creek Formation spanning the K-T boundary, and the Paleocene Lower Porcupine Hills Formation ( Fig. 1 ). Unlike time-equivalent humid paleosols across the K-T boundary in the northern...

..., I report observations consistent with the occurrence of a PFS beneath the Great Plains of North America. This report presents evidence for the PFS but does not discuss the particular mechanism for the PFS formation, which requires much more analysis. The extent of the Great Plains PFS is still being...

...O. Ogunyomi; L. V. Hills ABSTRACT Paleoenvironmental interpretations based on sedimentological and micropaleontological analyses indicate that the Late Cretaceous (Campanian) Foremost Formation is transitional between the underlying marine Pakowki Formation and the overlying nonmarine Oldman...

.... The map shows the relative postions of the Turner Valley Structure, the Highwood Structure and the Oldman Structure. These three structures form the leading edge of the orogenic wedge between the towns of Black Diamond and Lundbreck. All three structures have a hinterland (west)-directed thrust fault...

...J. B. Webb; Leo George Hertlein ABSTRACT The importance of lithologic and fossil zones in the Alberta shale, more commonly known as the “Benton” formation or group, in the foothills of the Rocky Mountains in southwestern Alberta, is indicated. The territory covered extends for 350 miles along...

...Fig. 10. Field photograph showing a typical example of foreland-vergent minor structures exposed along the OIdman River, west of the upper detachment; view looking south (location indicated in Fig. 8 ). These meso-scale folds are developed within the Lundbreck Formation of the Belly River Group...

...Y. Greg Hu; A. Guy Plint Abstract The Santonian-early Campanian Puskwaskau Formation is a prismatic wedge <70 to >340 m thick that occupies the foredeep of the Western Canada foreland basin. It is dominated by muddy, offshore sediments deposited by storms in water probably no more than a few...

... of southern Alberta and Saskatchewan: Foremost, Oldman, and Dinosaur Park. In the foothills region of Alberta, the Belly River Group includes the Connelly Creek, Lundbreck, and Dinosaur Park/Drywood Creek Formations ( Jerzykiewicz and Norris, 1994 ; Hamblin and Abrahamson, 1996 ). Last, in addition...