... in the Athabasca River valley at site C and Pelican Cliffs. Sandstone at site C is exclusively quartz arenite. ...

...-Cretaceous Unconformity. The study area is outlined by the red rectangle. C) Isopach map of the McMurray Fm in the study area with maximum thicknesses observed along the axes of the Pelican, Sparrow, and Grouse paleovalleys and minimum thicknesses over the carbonate highlands. Pelican, Sparrow, and Grouse...

..., garnet schist, and chlorite). A steep cliff composed largely of greenschist was encountered by the deep submergence vehicle (DSV) Alvin during Dive 641 (Woods Hole Oceanographic Institution) in 1976 (Heerzen et al., 1985) on the north wall of Mona Block (red line in Fig. 1B) between depths of 3640 m...

... River north of Nelson Forks locality. Because their position in the Shaftesbury formation is considered to be between the Gastroplites and Neogastroplites horizons, and because of the different composition of the Pelican sandstone compared with that of the Sikanni sandstone member, the Pelican formation...

... part of the section which he named the Lyons conglomerate. He also recognized the artesian water possibilities of the region; consequent on this discovery the deep well at Pelican Hill ( Fig. 2 , well location 52) was drilled and yielded an artesian flow. F. G. Clapp, who visited this and other...

... unconformably atop the Devonian limestones. Any traveler in northern Alberta sees many interesting things, but none so likely to interest him or to stimulate his imagination as the great cliffs and slopes of bituminous sand along the banks of the Athabaska River. The exposures, some of them over 200 feet...

..., 153 72.3 43.9 14.3 15.2 10 MI Missi Conglomerate Fm.: clasts MIb Beaverdam Mbr.: conglomerate clasts < 1855±2 28, 30* 69.4 29.6 4.8 5.5 11 MIr Little Cliff Mbr.: conglomerate clasts < 1845±2 30, 45* 72.4 70.8 17.2 18.1 11 MO N Molson dikesA: pegmatitic...

... and is the main stratigraphic unit that formed the bed of the Palaeolake Etosha. It now forms the present floor of Etosha Pan but this is several metres below the original top of the member. In scarp exposures, the top is at 1084.2 m at Pelican Island and 1086 m on the eastern side of Poacher’s Point...

... karst on the top of Codrington reef-front deposits at present sea level. The same deposit is traceable southwards, making small sea cliffs at Welch Point and at Pelican Bay; where it disappears landward beneath Holocene dune sands to reappear on their west side. Here the caliche overlies Codrington back...

..., and solutional remnants of undercut limestone sometimes are left behind by the retreating scarp in much the same way that sea stacks are left behind a retreating coastal cliff. The steep-sided remnants constitute examples of tower karst, and their 60° to 90° slopes, among other things, serve to distinguish them...

... ( 1991 ) and is part of a regional examination of Paddy stratigraphy ( Buckley and Plint, 2013 ; Vannelli, 2016 ; Vannelli et al., 2017 ; Plint et al., 2018 ). A 5 km long cliff exposure on the west bank of the Peace River allows detailed examination of the Cadotte and the unconformably overlying...

... of matrix slab showing typical texture of fish scale bone bed at locality F7a (see Fig. 3 ). Arrow indicates shark tooth. Fig. 7. View to the north showing the concentration of fossiliferous siltstone blocks in creek bed at locality B4 (Ammonite Cliff), interpreted as having eroded out from...

... andesite tuff SLB-93-101 Tuff Igneous 1882 3 3 11 Stern and Lucas 1994 Vick Lake shoshonite tuff SLB-92-17 Tuff Igneous 1885 3 3 12 Stern et al. 1993 Two Portage Lake rhyolite tuff 52-79-1217 Crystal tuff Igneous 1886 2 2 13 Gordon et al. 1990 Cliff Lake pluton SLB-94-123...

... et al. 1995 ; Marshall et al. 1997 ). One of the best-dated shear zones in the THO is the Pelican Thrust, a major ductile shear zone that appears to have been active for most of the 1840–1800 Ma time period ( Ashton et al. 1999 ; Sun et al. 1996 ). The timing of movement on the NFSZ appears to have...

... as the Pelican rocks, Friendship Quarry, Dunmore Hill, Southern Cunapo Road, and other places in southern and central Trinidad. These Midway glauconitic shell beds, representing rather shallow-water conditions, are probably indications of zones of limited uplift, whereas in the major part...

... Report 97-4, pp.  55 – 64 . Ashton K.E. Lewry J.F. Heaman L.M. Hartlaub R.P. Stauffer M.R. Tran H.T. 2005 . The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon – Glennie Complex, Trans-Hudson Orogen . Canadian Journal...

... and G. menardii to the laboratory is feasible, cultivating multigenerational cultures represents the next scientific hurdle that is necessary to conduct experiments with sufficient sample sizes to control for multiple variables. We would like to thank the crew of RV Pelican (Louisiana...

... and an important rate of karstification highlighted by small surfaces and large-scale dissolution features: lapiez, microkarsts, karsts ( Figs. 7A – 7C ). Samples are taken near the Stadium Quarry, located hundred meters just above the sanctuary, at the foot of the cliff ( Fig. 3 ). Fig. 7 Parnassus...