The King's Crown and the Crown Jewels
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CNC/IUGG: 2019 Quadrennial Report
CNC/IUGG: 2019 Quadrennial Report Geodesy and Geophysics in Canada 2015-2019 Quadrennial Report of the Canadian National Committee for the International Union of Geodesy and Geophysics Prepared on the Occasion of the 27th General Assembly of the IUGG Montreal, Canada July 2019 INTRODUCTION This report summarizes the research carried out in Canada in the fields of geodesy and geophysics during the quadrennial 2015-2019. It was prepared under the direction of the Canadian National Committee for the International Union of Geodesy and Geophysics (CNC/IUGG). The CNC/IUGG is administered by the Canadian Geophysical Union, in consultation with the Canadian Meteorological and Oceanographic Society and other Canadian scientific organizations, including the Canadian Association of Physicists, the Geological Association of Canada, and the Canadian Institute of Geomatics. The IUGG adhering organization for Canada is the National Research Council of Canada. Among other duties, the CNC/IUGG is responsible for: • collecting and reconciling the many views of the constituent Canadian scientific community on relevant issues • identifying, representing, and promoting the capabilities and distinctive competence of the community on the international stage • enhancing the depth and breadth of the participation of the community in the activities and events of the IUGG and related organizations • establishing the mechanisms for communicating to the community the views of the IUGG and information about the activities of the IUGG. The aim of this report is to communicate to both the Canadian and international scientific communities the research areas and research progress that has been achieved in geodesy and geophysics over the last four years. The main body of this report is divided into eight sections: one for each of the eight major scientific disciplines as represented by the eight sister societies of the IUGG. -
Pingualuit Crater Lake): Diatom Inferred Paleoenvironmental Record for Three Previous Interglacial Periods
THE “CRYSTAL EYE OF NUNAVIK” (PINGUALUIT CRATER LAKE): DIATOM INFERRED PALEOENVIRONMENTAL RECORD FOR THREE PREVIOUS INTERGLACIAL PERIODS 1,2Jessica L. Black, 1Sonja Hausmann, 2Reinhard Pienitz, 3Veli-Pekka Salonen, 4Guillame St-Onge, 5Michel Bouchard, 6Laura Cunningham, 7Pierre Francus, and 8Michel Lamothe 1Department of Geosciences, University of Arkansas, 113 Ozark Hall, Fayetteville, AR 72701, [email protected], 2Université Laval, Québec, G1V 0A6, Canada, 3Department of Geology, Univ of Helsinki, P.O. BOX 64, Helsinki, FIN-00014, Finland, 4ISMER/GEOTOP, University of Quebec at Rimouski, Rimouski, QC G5L 3A1, Canada, 5Centre des Technologies de l'Environment de Tunis (CITET), Université de Montréal, Montréal, QC H3T 1J4, Canada, 6Abisko Scientific Research Station, Umea University, Abisko, SE-981 07, Sweden, 7Centre Eau, Terre et Environnement, Institut national de la recherche scientifique, 490 rue de la couronne, Québec, QC G1K 9A9, Canada 8Département des sciences de la Terre et de l’Atmosphère, Université du Québec à Montréal, CP 8888 Centre-ville, Montréal, QC H3C 3P8, Canada The sediments of the 1.4. Ma old Pingualuit Crater Lake known as the “Crystal Eye of Nunavik” offer the unique opportunity to study terrestrial climate dynamics not only during the postglacial period, but over several hundreds of thousands of years as its deep sediment infill yields an uninterrupted arctic paleoclimate record. The Pingualuit meteoritic crater (Nunavik, Canada; 61o17' N, 73o41' W) is located in the northernmost part of the Ungava Peninsula in northern Quebec - close to the area where the Laurentide Ice Sheet reached maximum thickness during the last (Wisconsinan) glaciation. In May, 2007 ~10 m of sediments was recovered from the crater lake at a water depth of 270 m using a UWITEC piston percussion corer system. -
Deglacial and Postglacial Evolution of the Pingualuit Crater Lake Basin, Northern Québec (Canada)
Geomorphology 248 (2015) 327–343 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Deglacial and postglacial evolution of the Pingualuit Crater Lake basin, northern Québec (Canada) Pierre-Arnaud Desiage a,b,⁎, Patrick Lajeunesse b,c, Guillaume St-Onge a,b, Alexandre Normandeau b, Grégoire Ledoux c,HervéGuyarda,b,d, Reinhard Pienitz c a Institut des sciences de la mer de Rimouski (ISMER), Canada Research Chair in Marine Geology, Université du Québec à Rimouski, Rimouski, Canada b GEOTOP Research Center, Canada c Centre d'études Nordiques (CEN) & Département de Géographie, Université Laval, Québec, Canada d Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR CNRS 7154, Paris, France article info abstract Article history: The Pingualuit Crater, located in the Ungava Peninsula (northern Québec, Canada) is a 1.4-Ma-old impact crater Received 15 January 2015 hosting a ~245-m-deep lake. The lake has a great potential to preserve unique paleoclimatic and paleoecological Received in revised form 9 July 2015 sedimentary records of the last glacial/interglacial cycles in the terrestrial Canadian Arctic. In order to investigate Accepted 10 July 2015 the stratigraphy in the lake and the late Quaternary glacial history of the Pingualuit Crater, this study compiles Available online 29 July 2015 data from three expeditions carried out in May 2007 (~9-m-long sediment core), in August 2010 (~50 km of seismic lines), and in September 2012 (high-resolution terrestrial LiDAR topography of the inner slopes). Despite Keywords: fi lake levels the weak penetration (~10 m) of the 3.5-kHz subbottom pro ling caused by the presence of boulders in the Mass movements sedimentary column, seismic data coupled with the stratigraphy established from the sediment core enabled Laurentide Ice Sheet the identification of two glaciolacustrine units deposited during the final stages of the Laurentide Ice Sheet Sedimentological processes (LIS) retreat in the crater. -
Results of Recent Sediment Drilling Activities in Deep Crater Lakes
of the subtropical region of South Ameri- beyond the instrumental record, as well del Puerto, L, García-Rodríguez, F., Inda H., Bracco, R., Castiñeira, C., J.B. and Adams, J.B., 2006: Paleolimnological evidence of Holocene ca (i.e., the transition between the tropics as to design new strategies for the sus- paleoclimatic changes in Lake Blanca, southern Uruguay, Journal and the extra tropics) in deciphering the tainable development of ecosystems and of Paleolimnology, 36: 151-163. forcing factors of past changes in atmo- natural resources. García-Rodríguez, F., 2006: Inferring paleosalinity changes using the chrysophyte cyst to diatom ratio in coastal shallow temperate/ spheric circulation. Both Argentinean and subtropical lagoons influenced by sea level changes, Journal of Uruguayan Holocene paleolimnologi- Acknowledgements Paleolimnology, 36,165-173. PEDECIBA, SNI-ANII and CSIC-Program Piovano, E., Ariztegui, D., Bernasconi, S.M. and McKenzie, J.A., 2004: cal records indicate similar paleoclimatic Stable isotopic record of hydrological changes in subtropical trends, i.e. dominant dry conditions were “Contratación de investigadores provenientes Laguna Mar Chiquita (Argentina) over the last 230 years, The del exterior” (Uruguay) are thanked for finan- observed during cold phases, whereas Holocene, 14(4): 525-535. cial support. Part of this study was supported Piovano, E.L., Ariztegui, D., Córdoba, F., Cioccale, M. and Sylvestre, F., wet conditions prevailed during warm by Argentina through funding of CONICET (PIP 2009: Hydrological variability in South America below the Tropic climatic phases. To our knowledge, this is 5947; PIP 112-200801-00808), FONCYT (PICT Nº of Capricorn (Pampas and Patagonia, Argentina) during the last 13.0 In: Vimeux, F. -
Uncorrected Proof
Quaternary Science Reviews xxx (2018) xxx-xxx Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com Late-Quaternary glacial to postglacial sedimentation in three adjacent fjord-lakes of the Québec North Shore (eastern Canadian Shield) Antoine G. Poiréa, ∗, Patrick Lajeunessea, Alexandre Normandeaua, b, Pierre Francusc, Guillaume St-Onged, Obinna P. Nzekwec a Département de géographie & Centre d’études nordiques, Université Laval, Québec, Qc G1V 0A6, Canada b Geological Survey of Canada (Atlantic), Bedford Institute of Oceanography, P.O. Box 1006, Dartmouth, Nova Scotia B2Y 4A2, Canada c Centre Eau Terre Environnement, Institut National de la Recherche Scientifique, Québec, Qc G1K 9A9, Canada, Canada Research Chair in Environmental Sedimentology & GEOTOP d Institut des sciences de la mer de Rimouski, Université du Québec à Rimouski, Rimouski, Qc, Canada, Canada Research Chair in MarinePROOFGeology & GEOTOP ARTICLE INFO ABSTRACT Article history: High-resolution swath bathymetry imagery allowed mapping in great detail the sublacustrine geomorphology Received 23 June 2017 of lakes Pentecôte, Walker and Pasteur, three deep adjacent fjord-lakes of the Québec North Shore (eastern Received in revised form 31 January 2018 Canada). These sedimentary basins have been glacio-isostatically uplifted to form deep steep-sided elongated Accepted 11 February 2018 lakes. Their key geographical position and limnogeological characteristics typical of fjords suggest excep- Available online xxx tional potential -
Carlyle Smith Beals Fonds (R15735) Finding Aid No MSS2580 MIKAN
Date: 15/06/2017 Carlyle Smith Beals fonds (R15735) Page 1 Finding aid no MSS2580 Y:\App\Impromptu\Mikan\Reports\Description_reports\finding_aids_&_subcontainers_simplelist.imr MIKAN Container File/Item Cr. file/item Hierarchy Title, etc Date of/de Extent/Media/Dim/Access cde # Contenant Dos./pièce Dos./item cr. Hiérarchie Titre, etc création Support ou Média / Dim. / Accès 4938572 Series Personnal papers [textual record, graphic material] 1922-1978 4941473 1 1 File Personal papers 1947-1972 Textual records / 90 S&C : Biographical information, genealogical information on the Beals family. Contains also a passeport and a manual with french expressions and vocabulary. 4941474 1 2 File Personal correspondence 1965-1978 Textual records / 90 S&C : Correspondence not related to the professional activities of C.S. Beals. Contains also several postal cards. 4941475 1 3 File Scholarship records, Degrees, Honors and letters of 1922-1977 Textual records / 90 recommendation S&C : Contains a scholarship record of Yale University for 1922, letters from the University of London that certify the reception of two Ph.D. by C.S. Beals in 1926 and 1934. Contains the certification of the registrar's Office of the University of Toronto for the M.A. of 1923. Contains also letters of recommendation from the different schools attented by C.S. Beals. Contains also a letter from the Royal Society of Canada informing C..S. Beals.that he'll be recommended as fellow of the RSC, a letter from The Profesionnal Institute of the Public Service of Canada for the reception of the Institute's Gold Medal (1977), correspondence and documentation concerning the reception of a Honorary Degree from Queen's University in Kingston in 1960 and a certificate of the Royal Society of Canada certifying 45 years of membership. -
Project Caribou an Educator’S Guide to Wild Caribou of North America
An Educator’s Guide to Wild Caribou of North America Copyright 2018 This book may be reproduced for educational purposes only. The illustrations may be duplicated solely for instructional use of this material. Reproduction for any other purpose is strictly prohibited without written permission from the publisher. For more information please contact: Environmental Education and Youth Programs Government of Yukon, Department of Environment Conservation Officer Services Box 2703, Whitehorse, Yukon Y1A 2C6 (867) 667-3675 or 1-800-661-0408 fax (867) 393-6206 [email protected] ISBN: 978-1-55362-794-4 Photo and illustration credits Government of Yukon, Department of Environment Government of Northwest Territories 1, 4, 6, 7, 8, 11, 12, 13, 16, 17, 19, 23, 25, 26, 27, 29, 31, 55, 65, 78, 87, 89 90, 94, 98, 99, 100, 102, 122 Government of Nunavut Doug Urquhart (illustrations) 132 3, 20, 26, 27, 29, 31, 34, 36, 42, 53, 63, 68, 75, 84, 98, 121 Joyce Majiski Government of Canada, Canadian Wildlife Service Cover, i 2, 9, 15, 18, 22, 24 Tanya Handley (illustrations) vii, 37, 40, 43, 102, 103 Jennifer Staniforth (illustrations) 4, 5, 10, 63 Beverly and Qamanirjuaq Caribou Management Board (illustrations) 47, 48, 49, 50 Northern Contaminants Committee 37, 40, 42, 43 Government of Quebec 112, 115 Project Caribou An Educator’s Guide to Wild Caribou of North America Project manager: Remy Rodden, Government of Yukon, Department of Environment Consultants: Darielle Talarico, Arctic Vision, Whitehorse, Yukon Principal writer: Kirsten Madsen, Whitehorse, Yukon Original illustrations: Jennifer Staniforth, Doug Urquhart, Tanya Handley Cover: Joyce Majiski Editing and production: Walker LeBrun Creative Services, Whitehorse, Yukon Government of Yukon, Department of Environment (2018 edition) Beverly and Qamanirjuaq Caribou Management Board i Project Caribou Acknowledgments Project Caribou is the result of the Sharon Russell Nova Scotia efforts of many individuals. -
Astroblemes, Scientific America~?-, Vol
Waste Isolation Pilot Plant Compliance Certification Application Reference 176 Dietz, R.S., August 1961. Astroblemes, Scientific America~?-, Vol. 205, #2, p 50-58. Submitted in accordance with 40 CFR § 194.13, Submission of Reference Materials. .. ~H ..\TTER COXE rour inrhes hi~h is one or many in igneous rork XEST OF COXES in dolomite. a tn~ or lime~tone. is rrom Wrlls or the \·rederort Ring in South ..\rrira. a strurture that i& prob Creek Ba~in ~trurture in Tenllt"'-"ft'. Thi& ~roup i~ II iMhet hi~h. ably the remains or tl1e large>l meteorite crater known on earth. Shork pre~~ur~ generated by meteorite imparl rreate ourh ron~. (;J..\.XT SH.-\TTER COXF., over rour reea long. i& !ihown in 1•lare amons jumbled rorks in a Rat. geolor:iralJy underormrd terrain at the Kentland Jime~tone quarry in Indiana. These c·ones round indirate that the quarry i~ an anrienl meteorite-im:-t ,ite. UMI Article Clearinghouse has reproduced this material with SO perLmLi'~-s~on of the copyright owner. Further reproduction IS Thi~ newly. ('Oined w·ord refers to anctent scars left in the earth·~ cru~t by huge tneteoriteH. The evidence for such itnpacts is largely the h igh-pre~~ure tnineral coesite and ~~shatter cones~' in the rocks b,· Hobert S. Dietz t is ;m awesome experience to stand authorih· was such that it took more than fall every 10,000 years, some 50,000 on the rim of B;minger Crater in :30 years' to re\·erse his judgment. But the giant meteorites must have struck the I Arizona and reflect on the cosmic scienc.-es progress not so much by the dis earth during the past 500 million ~·ears. -
Provincial Plaques Across Ontario
An inventory of provincial plaques across Ontario Last updated: May 25, 2021 An inventory of provincial plaques across Ontario Title Plaque text Location County/District/ Latitude Longitude Municipality "Canada First" Movement, Canada First was the name and slogan of a patriotic movement that At the entrance to the Greater Toronto Area, City of 43.6493473 -79.3802768 The originated in Ottawa in 1868. By 1874, the group was based in Toronto and National Club, 303 Bay Toronto (District), City of had founded the National Club as its headquarters. Street, Toronto Toronto "Cariboo" Cameron 1820- Born in this township, John Angus "Cariboo" Cameron married Margaret On the grounds of his former Eastern Ontario, United 45.05601541 -74.56770762 1888 Sophia Groves in 1860. Accompanied by his wife and daughter, he went to home, Fairfield, which now Counties of Stormont, British Columbia in 1862 to prospect in the Cariboo gold fields. That year at houses Legionaries of Christ, Dundas and Glengarry, Williams Creek he struck a rich gold deposit. While there his wife died of County Road 2 and County Township of South Glengarry typhoid fever and, in order to fulfil her dying wish to be buried at home, he Road 27, west of transported her body in an alcohol-filled coffin some 8,600 miles by sea via Summerstown the Isthmus of Panama to Cornwall. She is buried in the nearby Salem Church cemetery. Cameron built this house, "Fairfield", in 1865, and in 1886 returned to the B.C. gold fields. He is buried near Barkerville, B.C. "Colored Corps" 1812-1815, Anxious to preserve their freedom and prove their loyalty to Britain, people of On Queenston Heights, near Niagara Falls and Region, 43.160132 -79.053059 The African descent living in Niagara offered to raise their own militia unit in 1812. -
Arctic Workshop 2013 Program Summary
Arctic Workshop 2013 Program Summary SUNDAY 10 MARCH 9:00 – 4:00 Pre-workshop field trip Hotel Lobby 7:00 – 9:30 Evening reception, Check-In, Level 11 Registration (load presentations onto computer) MONDAY 11 MARCH 8:00 – 8:30 Check-in & Registration Level 2 Reading Room (load presentations onto computer) 8:45 Welcome & Introduction Level 2 Reading Room 9:00 Paleoceanography I Level 2 Reading Room 10:10 Morning Break Level 1 Auditorium 10:40 Paleoceanography II Level 2 Reading Room 12:00 LUNCH - 1:00 pm Glacial History Level 2 Reading Room 3:50 Afternoon Break Level 1 Auditorium 4:00 POSTERS I (odd-numbered posters) Level 1 Auditorium 6:00 End of session Level 1 Auditorium 6:30 Non-student Dinner Julie B-G’s house 7:00 Student-only Pizza Party University Club TUESDAY 12 MARCH 9:00 Paleolimnology Level 2 Reading Room 10:30 Morning Break Level 1 Auditorium 10:50 Modelling Level 2 Reading Room 12:10 LUNCH - 1:20 pm Special Talk (Kevin Knobloch, UCS) Level 2 Reading Room 1:50 Glaciology Level 2 Reading Room 3:45 Afternoon Break Level 1 Auditorium 4:00 Chasing Ice – documentary film ISB Auditorium 5:15 Afternoon Break Level 1 Auditorium 5:30 POSTERS II (even numbered posters) Level 1 Auditorium 7:00 End of session Level 1 Auditorium 7:00 Workshop Banquet Level 1 Auditorium Keynote: John H. England Level 1 Auditorium WEDNESDAY 13 MARCH 8:45 Paleoclimatology I Level 2 Reading Room 10:35 Morning Break Level 1 Auditorium 10:50 Paleoclimatology II Level 2 Reading Room 12:40 End of Meeting. -
An Unusual Occurrence of Coesite at the Lonar Crater, India
Meteoritics & Planetary Science 52, Nr 1, 147–163 (2017) doi: 10.1111/maps.12745 An unusual occurrence of coesite at the Lonar crater, India 1* 1 2 1 3 Steven J. JARET , Brian L. PHILLIPS , David T. KING JR , Tim D. GLOTCH , Zia RAHMAN , and Shawn P. WRIGHT4 1Department of Geosciences, Stony Brook University, Stony Brook, New York 11794–2100, USA 2Department of Geosciences, Auburn University, Auburn, Alabama 36849, USA 3Jacobs—NASA Johnson Space Center, Houston, Texas 77058, USA 4Planetary Science Institute, Tucson, Arizona 85719, USA *Corresponding author. E-mail: [email protected] (Received 18 March 2016; revision accepted 06 September 2016) Abstract–Coesite has been identified within ejected blocks of shocked basalt at Lonar crater, India. This is the first report of coesite from the Lonar crater. Coesite occurs within SiO2 glass as distinct ~30 lm spherical aggregates of “granular coesite” identifiable both with optical petrography and with micro-Raman spectroscopy. The coesite+glass occurs only within former silica amygdules, which is also the first report of high-pressure polymorphs forming from a shocked secondary mineral. Detailed petrography and NMR spectroscopy suggest that the coesite crystallized directly from a localized SiO2 melt, as the result of complex interactions between the shock wave and these vesicle fillings. INTRODUCTION Although there is no direct observation of nonshock stishovite in nature, a possible post-stishovite phase may High-Pressure SiO2 Phases be a large component of subducting slabs and the core- mantle boundary (Lakshtanov et al. 2007), and Silica (SiO2) polymorphs are some of the simplest stishovite likely occurs in the deep mantle if basaltic minerals in terms of elemental chemistry, yet they are slabs survive to depth. -
The Ancient Meteorite Crater at Holleford Ontario by Leo Enright
Firefox https://starlightcascade.ca/tourism/holleford/HollefordCrater.php The Ancient Meteorite Crater at Holleford Ontario by Leo Enright Aerial photo of Holleford Meteorite Crater. Holleford Crater, an interesting and very ancient meteorite impace feature, is named after the tiny village located partly within its boundaries. It is a circular depression about 30 meters deep and 2.35 km in diameter, located at latitude 44 deg 47 minutes north, longitude 76 deg 38 minutes west, about 27 km north-north-west of Kingston, Ontario. Although several farms had been maintained at the site for over 100 years, its discovery and confirmation as a meteorite impace site dates only to the mid-1950's. The 1950's research was led by Canadian scientists from the Dominion Observatory in Ottawa, and the project that led to its discovery was the result of the discovery of two other meteorite impace sites, the New Quebec Crater amd the crater at Brent, Ontario. First identification of the feature was a result of a 1955 study of 200,000 aerial photographs of areas of the Canadian Shield conducted by the Dominion Observatory under the direction of Dr. Carlyle S. Beals, the Dominion Astronomer at the time. Subsequently, the research program included a study of the surface geology by the Geologic Survey of Canada, and a series of four geophysical studies, namely (1) magnetic observations of the area, (2) seismic studies which proved consistent with the theory that it was an impact site, (3) gravity studies which also proved consistent with the impact theory, and (4) a diamond drilling program in which 3 holes were drilled.