Ruby- and Sapphirine-Bearing Mineral Occurrenc- Es in the Fiskenaesset, Nuuk and Maniitsoq Re- Gions, West Greenland Peter W
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New Minerals Approved in 1998 by The
247 The Canadian Mineralogist Vol. 37, pp. 247-252 (1999) NEW MINERALSAPPROVED IN 1998 BY THE COMMISSIONON NEW MINERALS AND MINERALNAMES. INTERNATIONAL MINERALOGICAL ASSOCIATION JOEL D. GRICE* CanadianMuseum of Nttture,P.O. Box 3443A,Station "D", Ottawa,Ontario KIP 6P4 GIOVANNI FERRARISX* Dipanimentodi ScienzeMineralogiche e Petrologiche,Universitd di Torino,Via ValpergaCaluso 35, I-10125Torino, Italy The information given here is provided by the Commission on New Minerals and Mineral Names (CNMMN), Intemational Mineralogical Association (IMA), for comparative purposesand as a service to mineralogists work- ing on new species.Each mineral is described in the following format: IMA Number Chemical Formula (any relationship to other minerals; structure analysis) Crystal system, spacegroup unit-cell parameters Color; luster; diaphaneity Optical properties Strongestlines in the X-ray powder-diffraction pattern td in A(I)l The namesof these approved speciesare consideredconfidential information until the authors have published their descriptions or releasedinformation themselves.No other information will be releasedby the Commission. 1998Pnoposers IMA No. 98-002 Ca:Ge(OH)6(SO+XCO:).12HzO A memberof IMA No. 98-001 the ettringitegroup; Cu3(AsOa)2.4H2O New structure-type structure OrthorhombiciPnma Hexagonal:P63/m a 5.6906.b t7.06I.c 9.82 A, a 11.056,c 10.629A Bottle green;vitreous; transparent White; vitreous;transparent Biaxial(-), u 1.745,B 1.755,1 1.760,2V(meas)11", Uniaxial(-), to 1.509,e 1.479 2V (calc)70" 8.52(100),3.721(60), 3.221(90), 9.57 (vs), 5. 5 3 (s), 3. 8 3 (s), 3. 56(ms), 3.44(m), 2.7 4(ms), 3.ro2(40), 2.8 r7 (3 5), 2.79 s (3 s), 2.3s0(25) 2.53(m) \ * Chairman, CNMMN. -
The Rutile Deposits of the Eastern United States
THE RUTILE DEPOSITS OF THE EASTERN UNITED STATES. By THOMAS L. WATSON. INTRODUCTION. The titanium-bearing minerals comprise more than 60 distinct species, grouped under a variety of mineral and chemical forms, chiefly as oxides, titanates, titano-silicates, silicates, columbates, and iantalates. These minerals are widely distributed in a variety of associations and in such quantity as to make titanium a relatively abundant element. Clarke* estimates the. amount of titanium in the solid crust of the earth to be 0.44 per cent, equivalent in oxide to 0.73 per cent, the element thus standing in the ninth place in the scale of abundance, next to potassium. Most of the titanium-bearing minerals, however, are rare and are only of scientific interest. The largest concentrations of the element are as oxide (rutile), as iron titanate (ilmenite), and in iron ferrate (magnetite) as intergrown ilmenite. Of these three forms the prin cipal source of the element at present is rutile. The known workable deposits of rutile, however, are extremely few and widely sepa rated, and as the demand for titanium has greatly increased in the last few years it has been necessary for some uses to turn to ilmenite or highly titaniferous magnetites. This paper briefly summarizes present knowledge of the geology of the rutile deposits in the eastern United States and for the sake of comparison discusses several foreign deposits, each of which has produced some rutile. Of the known deposits in the United, States only those in Virginia are of commercial importance. These have been made the subject of a special report 2 by the Virginia Geological Survey, which was preceded by a preliminary paper on the rutile deposits of Amherst and Nelson counties.3 1 Clarke, F. -
Natural Resources in the Nanortalik District
National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 2001 Christain M. Glahder Department of Arctic Environment Data sheet Title: Natural resources in the Nanortalik district Subtitle: An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Arktisk Miljø – Arctic Environment. Author: Christian M. Glahder Department: Department of Arctic Environment Serial title and no.: NERI Technical Report No. 384 Publisher: Ministry of Environment National Environmental Research Institute URL: http://www.dmu.dk Date of publication: December 2001 Referee: Peter Aastrup Greenlandic summary: Hans Kristian Olsen Photos & Figures: Christian M. Glahder Please cite as: Glahder, C. M. 2001. Natural resources in the Nanortalik district. An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Na- tional Environmental Research Institute, Technical Report No. 384: 81 pp. Reproduction is permitted, provided the source is explicitly acknowledged. Abstract: The interview study was performed in the Nanortalik municipality, South Green- land, during March-April 2001. It is a part of an environmental baseline study done in relation to the Nalunaq gold project. 23 fishermen, hunters and others gave infor- mation on 11 fish species, Snow crap, Deep-sea prawn, five seal species, Polar bear, Minke whale and two bird species; moreover on gathering of mussels, seaweed etc., sheep farms, tourist localities and areas for recreation. -
Khmaralite, a New Beryllium-Bearing Mineral Related to Sapphirine: a Superstructure Resulting from Partial Ordering of Be, Al, and Si on Tetrahedral Sites
American Mineralogist, Volume 84, pages 1650–1660, 1999 Khmaralite, a new beryllium-bearing mineral related to sapphirine: A superstructure resulting from partial ordering of Be, Al, and Si on tetrahedral sites JACQUES BARBIER,1,* EDWARD S. GREW,2 PAULUS B. MOORE,3 AND SHU-CHUN SU4 1Department of Chemistry, McMaster University, Hamilton, Ontario, L8S 4M1 Canada 2Department of Geological Sciences, University of Maine 5790 Bryand Center Orono, Maine 04469, U.S.A. 3P.O. Box 703, Warwick, New York,10990, U.S.A. 4Hercules Research Center, 500 Hercules Road, Wilmington, Delaware 19808, U.S.A. ABSTRACT 3+ 2+ Khmaralite, Ca0.04Mg5.46Fe 0.12Fe 1.87Al14.26Be1.43B0.02Si4.80O40, is a new mineral closely related to sapphirine from Khmara Bay, Enderby Land, Antarctica. It occurs in a pegmatite metamorphosed at T ≥ 820 °C, P ≥ 10 kbar. The minerals surinamite, musgravite, and sillimanite associated with khmaralite at Casey Bay saturate it in BeO, and thus its BeO content could be close to the maximum possible. Optically, khmaralite is biaxial (–); at λ = 589 nm, α = 1.725(2), β = 1.740(2), γ = 1.741(2), 2Vmeas = 34.4 (1.8)°, v > r strong, and β b. The weak superstructure reported using electron diffraction has been confirmed by single-crystal X-ray diffraction. The superstructure corresponds to a doubling of the a axis in monoclinic sapphirine-2M (P21/c setting) with the following unit-cell parameters: a = 3 19.800(1), b = 14.371(1), c = 11.254(1) Å, β = 125.53(1)°, Z = 4, Dcalc = 3.61 g/cm . -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote -
The Crystal Structure of Aenigmatite E
THE AMERICAN MINERALOGIST, VOL. 56, MARCH-APRIL, 1971 THE CRYSTAL STRUCTURE OF AENIGMATITE E. CANNILLO AND F. MAZZI, Centro di studio del C.N.R. per la cristal- lografia struturale, Istituto di Mineralogia dell' Universita di Pavia, Italy. AND J. H. FANG, PAUL D. ROBINSON, AND Y. OHYA, Department of Geology, Southern Illinois University, Carbondale, Illinois, U.S.A. ABSTRACT Aenigmatite, Na2Fe.TiSi602Q, is triclinic PI, with a= 10.406(13), b = 10.813(14), c=8.926(6) A, <>= 104° 56'(9), ~=96°52'(11), 1'= 125°19'(6), and Z = 2. The structure was solved, independently and simultaneously, by Patterson syntheses and by the symbolic addition procedure. Three-dimensional refinement with 921 "observed" reflections (photo- graphic data) from a Naujakasik, Greenland, crystal gave RhkZ=0.075 and with 1501 "observed" reflections (counter data) from a Kola, Greenland crystal gave Rhkl=O.072. A distinct pseudo-monoclinic symmetry, based on a cell with parameters: 11m= 12.120, b1O=2X14.815, c1O=1O.406 A, <>10=90°4', ~1O=127°9', 1'10=89°44' (matrix of transforma- tion [011jI22/100j), Z = 8, emphasizes the similarity of its crystal structure with that of sapphirine [(Mg, Alh02(Si, Al)6018, a=11.266, b=14.401, c=9.929 A, ~=125 °46', Z=4, space group P2i!a]. The crystal structure consists of two sets of polyhedral layers parallel to the pseudo- monoclinic (100) plane which alternate along the x*-direction. The first layer is formed by Fe-octahedra, Ti-octahedra and distorted Na-square antiprisms and the second by [Si601s]" chains connected by Fe-octahedra. -
Scoping and Terms of Reference for Social Impact Assessment the Malmbjerg Molybdenum Project, Greenland Resources Inc
Scoping and Terms of Reference for Social Impact Assessment The Malmbjerg Molybdenum Project, Greenland Resources Inc. Submitted to: Greenland Resources Inc. Att. Dr. Ruben Shiffman, President Submitted by: Golder Associates A/S Maglebjergvej 6, DK – 2800 Kongens Lyngby, Denmark +45 70 27 47 57 Proj. no.: 19125166 23.06.2020 23.06.2020 Proj. no.: 19125166 Distribution List Greenland Resources Inc. i 23.06.2020 Proj. no.: 19125166 Table of Contents 1.0 INTRODUCTION ............................................................................................................................................. 5 1.1 The Malmbjerg Molybdenum Project ................................................................................................... 5 1.2 About the Mine company GRI .............................................................................................................. 6 1.3 The Molybdenum Mine Project Location .............................................................................................. 6 2.0 PROJECT DESCRIPTION OF THE MALMBJERG PROJECT ..................................................................... 7 2.1 Project Site Description ........................................................................................................................ 7 2.1.1 Geology and Mineralization ............................................................................................................ 8 2.2 Description of the Mining Project ........................................................................................................ -
Sheep Farming As “An Arduous Livelihood”
University of Alberta Cultivating Place, Livelihood, and the Future: An Ethnography of Dwelling and Climate in Western Greenland by Naotaka Hayashi A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Anthropology ©Naotaka Hayashi Spring 2013 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. Abstract In order to investigate how Inuit Greenlanders in western Greenland are experiencing, responding to, and thinking about recent allegedly human-induced climate change, this dissertation ethnographically examines the lives of Greenlanders as well as Norse and Danes in the course of past historical natural climate cycles. My emphasis is on human endeavours to cultivate a future in the face of difficulties caused by climatic and environmental transformation. I recognize locals’ initiatives to carve out a future in the promotion of sheep farming and tree-planting in southern Greenland and in adaptation processes of northern Greenlandic hunters to the ever-shifting environment. -
Marine Ecology Progress Series 518:107
Vol. 518: 107–121, 2015 MARINE ECOLOGY PROGRESS SERIES Published January 7 doi: 10.3354/meps11087 Mar Ecol Prog Ser FREEREE ACCESSCCESS Eelgrass Zostera marina in subarctic Greenland: dense meadows with slow biomass turnover in cold waters Birgit Olesen1,*, Dorte Krause-Jensen2,3, Núria Marbà4, Peter Bondo Christensen2,3 1Department of Bioscience, Aarhus University, Ole Worms Allé 1, Building 1135, 8000 Aarhus C, Denmark 2Department of Bioscience, Aarhus University, Vejlsøvej 25, 8600 Silkeborg, Denmark 3Arctic Research Centre, Aarhus University, C.F. Møllers Allé 8, 8000 Aarhus C, Denmark 4Department of Global Change Research, IMEDEA (CSIC-UIB), Institut Mediterrani d’Estudis Avancats, Miquel Marques 21, 07190 Esporles (Illes Balears), Spain ABSTRACT: Eelgrass Zostera marina L. is the most dominant seagrass species throughout the temperate northern hemisphere, and knowledge on its distribution and production in relation to climatic conditions is relevant for predicting the future of the meadows. We synthesized past and present information on eelgrass near the northern distribution limit in Greenland, and quantified the biomass, production and reproductive potential of eelgrass populations in 4 widely separated locations of Godthåbsfjorden at 64° N. Eelgrass observations in Greenland date back to 1813; most of the meadows recorded in the past still exist, and new ones were identified. The meadows are relatively small and geographically isolated, typically occurring in inner branches of the fjord sys- tem where summer water temperatures are higher (13 to 15°C) than in the outer part (<10°C). The shoot density (871 to 2045 shoots m−2), aboveground biomass (90 to 327 g dry wt [DW] m−2) and rhizome extension rates (8 to 29 cm yr−1) match levels further south. -
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ENERGY IN THE WEST NORDICS AND THE ARCTIC CASE STUDIES Energy in the West Nordics and the Arctic Case Studies Jakob Nymann Rud, Morten Hørmann, Vibeke Hammervold, Ragnar Ásmundsson, Ivo Georgiev, Gillian Dyer, Simon Brøndum Andersen, Jes Erik Jessen, Pia Kvorning and Meta Reimer Brødsted TemaNord 2018:539 Energy in the West Nordics and the Arctic Case Studies Jakob Nymann Rud, Morten Hørmann, Vibeke Hammervold, Ragnar Ásmundsson, Ivo Georgiev, Gillian Dyer, Simon Brøndum Andersen, Jes Erik Jessen, Pia Kvorning and Meta Reimer Brødsted ISBN 978-92-893-5703-6 (PRINT) ISBN 978-92-893-5704-3 (PDF) ISBN 978-92-893-5705-0 (EPUB) http://dx.doi.org/10.6027/TN2018-539 TemaNord 2018:539 ISSN 0908-6692 Standard: PDF/UA-1 ISO 14289-1 © Nordic Council of Ministers 2018 Cover photo: Mats Bjerde Print: Rosendahls Printed in Denmark Disclaimer This publication was funded by the Nordic Council of Ministers. However, the content does not necessarily reflect the Nordic Council of Ministers’ views, opinions, attitudes or recommendations. Rights and permissions This work is made available under the Creative Commons Attribution 4.0 International license (CC BY 4.0) https://creativecommons.org/licenses/by/4.0 Translations: If you translate this work, please include the following disclaimer: This translation was not produced by the Nordic Council of Ministers and should not be construed as official. The Nordic Council of Ministers cannot be held responsible for the translation or any errors in it. Adaptations: If you adapt this work, please include the following disclaimer along with the attribution: This is an adaptation of an original work by the Nordic Council of Ministers. -
Success and Failure of Reindeer Herding in Greenland
Article based on a lecture presented at the Nordic Conference on Reindeer Research, Kautokeino 13-15 March 1998 Success and failure of reindeer herding in Greenland Christine Cuyler Greenland Institute of Natural Resources, P.O.Box 570, DK-3900 Nuuk, Greenland Abstract: Animal husbandry is a recent innovation in Greenland, specifically reindeer husbandry is less than 50 years old. Reindeer husbandry was first established in mid-west Greenland and later in southern Greenland. The Greenland hunter tradition and culture is, however, still dominant in many communities. During the 1980's and 1990's, the incompatibility of these two traditions resulted in the failure of reindeer husbandry in mid-west Greenland. There were neither herding nor seasonal herd movements. Animals remained year round on the winter range, which was destroyed as lichens were trampled every summer. Without seasonal herd movements both sustainable range use and control of the herd were lost. Today, there are just two semi-domestic reindeer herds left, and both are in southern Greenland. One herd is commercially successful, and the other is under development. In mid-west Greenland, semi-domestic reindeer husbandry officially ended in 1998, and a hunt was initiated to remove the remaining population. Possibly, by the year 2000 any animals left in this region will be considered wild caribou. Key words: Rangifer tarandus, husbandry, herding, Greenland. Introduction Prior to the introduction of the semi-domestic reindeer from Norway, the indigenous west Greenland caribou (Rangifer tarandus groenlandicus) inhabited the west coast of Greenland from Thule in the north-west, 77°N, down to the southern tip of the country, 60°N. -
GEOLOGY of CORUNDUM and EMERALD GEM DEPOSITS : a R EVIEW Gaston Giuliani and Lee A
FEATURE ARTICLES GEOLOGY OF CORUNDUM AND EMERALD GEM DEPOSITS : A R EVIEW Gaston Giuliani and lee A. Groat The great challenge of geographic origin determina - processes), and alluvial (deposited by rivers). Today, tion is to connect the properties and features of indi - most sapphires are produced from gem placers related vidual gems to the geology of their deposits. Similar to alkali basalts, as in eastern Australia or southern geologic environments can produce gems with similar Vietnam, while placers in metamorphic environments, gemological properties, making it difficult to find such as in Sri Lanka (Ratnapura, Elahera) and Mada - unique identifiers. Over the last two decades, our gascar (Ilakaka), produce the highest-quality sap phires. knowledge of corundum and emerald deposit forma - The colluvial Montepuez deposit in Mozam bique pro - tion has improved significantly. vides a huge and stable supply of clean and very high- quality rubies. The mineral deposits are classically separated into pri - mary and secondary deposits. Primary corundum de - Primary emerald deposits are subdivided into two posits are subdivided into two types based on their types based on their geological environment of forma - geological environment of formation: (1) magmatic and tion: (1) tectonic-magmatic-related (Type I) and (2) (2) metamorphic. Magmatic deposits include gem tectonic-metamorphic-related (Type II). Several sub - corundum in alkali basalts as in eastern Australia, and types are defined and especially Type IA, hosted in M- sapphire in lamprophyre and syenite as in Montana UMR, which accounts for about 70% of worldwide (United States) and Garba Tula (Kenya), respectively. production (Brazil, Zambia, Russia, and others).