...Fig. 16. Sedimentary features of sandstone units from the Beatton High: A) low-angle bedding (1) capped by a large ripple (2), and B) erosional basal contact (arrow) of a sandstone unit. Bar scale in 1 cm divisions. ...

... with the Permian Beatton High to the northeast. Although the influence of these two highs on Triassic sedimentation, if any, remains unclear, the Baldonnel is thinned and the Pardonet missing over a smaller structural high on trend with the western end of the Beatton High. The boundary between the underlying Upper...

... in this mapped area (derived and modified from figure 19 in Dixon, 2004 ). Stratigraphic relationship 2 is limited to the vicinity of the Beatton High, a local tectonic feature about 100 km long and 40 km wide, in the Beatton River area (map-sheet 94H) of northeast British Columbia (see Davies, 1997...

... Uplift, Beatton High and Grassy High (Davies and Majid, 1993), and other elements. The record of the offshore volcanic island arc-subduction complex of western Canada in Triassic time is preserved now in allochthonous terranes in western British Columbia and the Yukon Territory. The migrating terranes...

... by the development of stratigraphically significant interfluve surfaces. This was based upon sets of closely-spaced thin sections taken from interfluve sequence-bounding paleosols exposed at Beatton River canyon, British Columbia, Canada. Micromorphology, field morphologies, and major physicochemical characteristics...

...DAVID JON FURBISH Abstract The migration of a river bend depends in part on the high flow velocities that characteristically impinge on its outside bank. Recent models have treated this in terms of a spatial convolution, whereby local bend migration is mathematically a weighted aggregate of up...

... of the" "filament of high velocity, starts to develop at the bend entrance and increases downstream as" "far as the curvature of the bend is sustained. Local rates of bend migration measured normal" "to the channel centerline are then proportional to the local flow asymmetry. The average" "migration rate for a bend...

...Fig. 16. Correlations in the Beatton River area, northeast British Columbia, showing onlap of sandstones onto the Beatton High. Gamma-ray logs. ...

.... The detrital material composing the Halfway Formation probably came from a northeasterly source and was carried southward by longshore drift. The ‘upper’ sandstone developments of the Beatton, Milligan, Willow, Wildmint and Bulrush trend were formed as longshore bars during a pause in the northeastward...

..., no direct observations were made of the interior of the point-bar platform. Later investigations of the interiors of point bars, using cores and ground penetrating radar, suggested that the upper sands corresponded to high-amplitude nearly horizontal reflectors, that the lower sands and gravels corresponded...

... of the Halfway River – Beatton River drainage divide. This study was conducted in the Charlie Lake map area (National Topographic System (NTS) 94A), which is located within the Alberta Plateau subprovince of the northern Interior Plains ( Fig. 1 ). The area is a flat to gently rolling plateau deeply incised...

... northward to encompass the Peace River Plains and Foothills, where Plint has measured more than 30 outcrop sections. Our aim is to integrate parasequences in outcrop with those documented in regional subsurface correlation lines, which currently extend 350 km from Beatton River (Twp. 86) to Berland River...