...Keith Dewing; J.C. Harrison; Brian R. Pratt; Ulrich Mayr Abstract The Kennedy Channel and Ella Bay formations are the two oldest stratigraphic units exposed in the Franklinian margin sedimentary sequence in the Canadian Arctic Islands. An Early Cambrian age had previously been accepted...

... W. = Kap Weber Trilobites collected by Cowie and Adams in 1955 from Ella Ø and the Albert Heim Bjerge area were borrowed from the National Museum of Wales, Cardiff. Cowie and Adams (1957) published lists of fossils recovered from the Bastion and Ella Island Formations, including brachiopods...

... of this part of the formation to the Portfjeld succession along the northern coast of Greenland, and further to the Ella Bay Formation of Ellesmere Island, is equivocal. Detailed locality and stratigraphic information was provided by Long (1989 a ) and Dewing et al. (2004) . In addition...

... Devonian time. This t ime interval is represented by a succession extending f rom the Ella Bay Format ion (Pe) to the uppermost par t of the undivided Allen Bay - Read Bay fomations (O-Dar) . The fo rmat ions in this interval are general ly much th icker than the same or equivalent units on the Central...

... in East Greenland. Study sites include Geanies in Easter Ross, Scotland; Hoxa Head on South Ronaldsay, Orkney; Hegglie Ber on Sanday, Orkney; Ella Ø (island), and Heintzbjerg in East Greenland ( Fig. 1 ). All sites contain continuous lacustrine sequences except for the Heintzbjerg samples, which...

...J. William Kerr ABSTRACT History of the Franklin miogeosyncline and adjacent Central Stable Region between Proterozoic and Late Devonian is well displayed on Ellesmere Island. Three long persistent sedimentary regimes displayed in these rocks are broadly similar to rocks in eastern and western...

... of a tsunami at Dickson Fjord on various social media channels (see Data and Resources ), where the remote event was identified due to water waves hitting a military unit located on Ella Island. In this study, we show satellite imagery in which we identify a missing cliff patch on the southern shore...

... of shales and microbial, muddy and grainy limestone, with minor dolostone at the base and top, terminates at the cryptic Fimbulfjeld disconformity. The formation has yielded trilobites collected on Ella Ø, Albert Heim Bjerge, and Kap Weber by C. Poulsen (1920s and 1930s), J. W. Cowie and P. J. Adams (1950s...

... by their English names then in use, such as Mountain (Mt.), Island, Peninsula, etc., which on modern Danish maps have been replaced by Fjeld or Bjerg, Ø. Halve, etc. Geographical names of very many important topographical features were given in the 19th century by English, German (Austrian), and Swedish...

...-water strata of the Ella Bay Formation of Ellesmere Island and correlative with the Portfjeld and Paradisfjeld formations of northern Greenland ( Fig. 3 ). Dewing et al. (2004 , 2008) further suggested that the Grant Land Formation is the deep-water equivalent of Lower Cambrian shallow-water strata...

... stages of rifting along the Franklinian margin prior to the emplacement of the Yelverton Formation between 574 and 532 Ma. On Ellesmere Island, the tectonic interpretation of the Ediacaran–early Cambrian Kennedy Channel and Ella Bay formations, and overlying Ellesmere Group ( Kerr 1967 ; Long 1989...

... Oilweek , v. 17, no. 14, p. 23-24. Copyright © 1966, The Canadian Society of Petroleum Geologists 1966 602 ABSTRACT S LATE PROTEROZOIC AND EARLY PALEOZOIC GEOSYNCLINE S AND CRATONS IN CANADA ' R. J . W. DOUGLA S Geological Survey of Canada, Ottawa, Ontari o ABSTRACT Some aspects of the nature...

... ) ~ e e Cornwa l l i s land o Q Axe l He iberg i s land Eg l in ton / z I s land Bathurs t Dyarn ar,o ~- I s land ~. . , . - - J - VISCOUNT 11o ° MELV ILLE SOUND loo ° / I Devon i s land C5 9°° Island ~ V L BAFF IN BAY Outline of the Sverdrup Basin ( . . . ) , distribution of Norian-Pliensbachian...

... in the Albanian chain and in a narrow, elongated, SW-verging imbricate belt located at the front of the External Dinarides, which extended from the NE edge of the Istria peninsula southwards, across the coastal islands and in the Adriatic offshore ( S cisciani et alii , 2009 ). The Apennines is a E- to NE...

... than 500 meters. The shallowest 13 4*E 135°E JAPAN I SEA ?°N D OKI ISLAND 36°N .TOTTORI SCALE ° I 2~o ~ alOkm. FIG. 1Position of Oki Bank. Japan. At the southwestern end of this chain, about 70 kilometers northeast of Oki Island, is a large submarine moun- spot at the southeast end is 288 meters deep...

... in Proceedings of the Second and Third Italian Meetings on Environmental Micropaleontology, edited by R. Coccioni and A. Marsili: Urbino, Italy, Grzybowski Foundation Special Publication 11, 2006, 101 pages. B ergamin , L., D i B ella , L., F rezza , V., D evoti , S., N isi , M. F., S ilenzi , S., and C...

...G. W. Chiplonkar; R. M. Badve SHORTER COMMUNICATIONS NEWER OBSERVATIONS ON THE STRATIGRAPHY OF THE BAGH BEDS O. W. CHIPLONKAR AND R. M. BADVE M. A. C. S. Research Institute, Poona Our recent work covering all the known outcrops of the Bagh beds has revealed that Deola·Chirakhan Marl of Bose (1884...

... Ø and Hyolithus Creek Formations of central East Greenland and the Hawke Bay Formation of New-foundland ( Swett 1981 ). Salterella has been reported from the Fucoid Beds, Serpulite/ Salterella Grit and lower Grudaidh Formation of northwest Scotland ( Yochelson 1983a ), the Wulff River, Ella...

... olenellid trilobites in the upper Bastion Formation, the age of this unit is likely within Cambrian Stage 4; a similar age is also likely for the overlying carbonate-dominated Ella Island Formation (Stouge et al. 2001 ; Skovsted, 2006 ; Stein, 2008 ). In addition to trilobites, the upper Bastion...