Geoheritage, a National Inventory in France De Wever, P
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Cantal Pêche Guide 2018
Cantal Pêche Guide 2018 Fédération Départementale de Pêche 14 Allée du Vialenc - Aurillac Tél. 04 71 48 19 25 www.cantal-peche.com Sommaire Mot du Président MOT DU PRÉSIDENT P RENDRE SA CARTE DE PÊCHE DANS LE CANTAL Tarifs cartes de pêche 2018 .....................................................................................................................................................P 6-7 ADHEREZ au Club Halieutique Interdépartemental ......................................................P 8-9 Dépositaires du département ...........................................................................................................................................P 10-11 OU PECHER DANS LE CANTAL Bassins Cère et Lot ......................................................................................................................................................................................P 12-17 Bassins Dordogne et Maronne ........................................................................................................................................P 18-23 Bassins Rhue et Alagnon ..............................................................................................................................................................P 24-27 Bassins Truyere et Bes .........................................................................................................................................................................P 28-33 LEC S A TIONS DE LA FEDERATION EN 2017 Actions de promotion et sensibilisation .....................................................................................................P -
The Volcanic Region of Auvergne
THE VOLCANIC REGION OF AUVERGNE. By CANON T. G. BOKNEY, D.Se., LL.D.. F.R.S., etc., late Professor of Geology in University College, London. (Read July stll, 190L) UVERGNE, SO far as my experience goes, is the most A interesting region in France, if not in Europe. It can teach the geological student more about the natural history of volcanoes than the Eifel, or even than the neighbourhood of Naples, though not a single vent is now in action. Impressive as Vesuvius must be during an eruption, we have then to con template it from a respectful distance, so that, although I would gladly have witnessed this, I probably learnt more from being able to stand on the crater rim. Auvergne offers to our examination a wonderful series of preparations, the handiwork of nature, illustrative of the anatomy of a volcano, from crater-cones as perfect as that of Monte Nuovo to ruins as complete as those on the Fifeshire coast. These will principally attract your attention during your visit, but they do not exhaust the geological interests of the region. The volcanic cones rise from a great upland plateau-a huge insular mass of ancient, and to a large extent, crystalline rocks surrounded by Secondary and later strata. Depressions in this plateau were occupied towards the middle of the Tertiary era by extensive lakes, which were gradually filled up by beds of sand stone, marls and freshwater limestones, the earlier of which are contemporaneous with the Headon, Bembridge and Hamstead beds of our country. You will frequently come across sections of them, especially on the western flank of the broad valley of the Allier, sealed up sometimes under sheets of basalt. -
AUV0078 Nom : Plomb Du Cantal Région : Auvergne Confidentialité : Public Nombre D'étoiles : ** Typologie : Site Naturel De Surface Géosite
ID : AUV0078 Nom : Plomb du Cantal Région : Auvergne Confidentialité : Public Nombre d'étoiles : ** Typologie : Site naturel de surface Géosite Résolution : 76,265 m/pixel Entités administratives et cartographiques Département(s) Commune(s) N° Département N°INSEE Commune (15) Cantal 15025 ALBEPIERRE-BREDONS 15192 SAINT-JACQUES-DES-BLATS Carte(s) topographique(s) au 1 / 25 000 Carte(s) géologique(s) au 1 / 50 000 N° Carte N° Carte 2435E MURAT.PLOMB DU CANTAL 0788 MURAT Carte(s) marine(s) (non renseigné) Contact pour le site Nom : SAEM Super Lioran Développement Adresse : Gare du téléphérique - Le Lioran Code postal : 15300 Ville : Laveissière Description physique Description physique : Point culminant du Cantal avec 1855 m, le Plomb du Cantal a une forme de bosse hémisphérique de 140 m de diamètre qui chapeaute une longue ligne de crête qui borde le flanc sud de la vallée de l’Alagnon et de la Cère. Le Plomb du Cantal se dresse en bordure d'un cirque d'origine glaciaire qui entaille un important empilement de coulées de laves trachyandésitiques. Les affleurements qui jalonnent les derniers mètres du sentier permettent d’observer des prismes de basanite inclinés. Superficie : 83 hectares Etat actuel : Bon / Bon état général Commentaire : Une table d’orientation située vers le nord donne un aperçu des ensembles volcaniques qui forment le coeur du Cantal.Un panorama se déploie des Pyrénées ou des Alpes par temps très clair. Usage(s) (non renseigné) Collection(s) (non renseigné) Accessibilité au site Accessibilité : Facile Libre Périodicité ouverture : Annuelle Autorisation préalable : Non Site payant : Non Itinéraire d'accès : Depuis la station de ski du Super Lioran, un chemin de grande randonnée de 3,8 km (GR4) permet d'atteindre en deux heures le sommet du Plomb, accessible également à partir des villages et des hauts plateaux basaltiques. -
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19 -
Chromite Crystal Structure and Chemistry Applied As an Exploration Tool
Western University Scholarship@Western Electronic Thesis and Dissertation Repository February 2015 Chromite Crystal Structure and Chemistry applied as an Exploration Tool Patrick H.M. Shepherd The University of Western Ontario Supervisor Dr. Roberta L. Flemming The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Patrick H.M. Shepherd 2015 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Shepherd, Patrick H.M., "Chromite Crystal Structure and Chemistry applied as an Exploration Tool" (2015). Electronic Thesis and Dissertation Repository. 2685. https://ir.lib.uwo.ca/etd/2685 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Western University Scholarship@Western University of Western Ontario - Electronic Thesis and Dissertation Repository Chromite Crystal Structure and Chemistry Applied as an Exploration Tool Patrick H.M. Shepherd Supervisor Roberta Flemming The University of Western Ontario Follow this and additional works at: http://ir.lib.uwo.ca/etd Part of the Geology Commons This Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in University of Western Ontario - Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. Chromite Crystal Structure and Chemistry Applied as an Exploration Tool (Thesis format: Integrated Article) by Patrick H.M. -
Fiche Imprimable 1.05-Massif Du Cantal
AtlAs prAtique des pAysAges d’Auvergne / fichE ensemble de paysage Les hautes terres 1 MASSIf DU CANTAL 05 « Dans les monts d’Auvergne, le massif 1. SITUATION Les unités de paysages qui composent cet en- du Cantal a une place toute spéciale. semble : 1.05 A Crêtes du Cantal / 1.05 B Pla- L’ensemble de paysages du Massif du Cantal nèze de St-Flour / 1.05 C Planèze de Cézens / Avec deux mille sept cents kilomètres occupe la partie centrale du département 1.05 D Plateau de Noalhac / 1.05 E Plateau de carré, plus de cinquante kilomètres auquel il a donné son nom. Il correspond à la Pailherols / 1.05 F Plateau du Coyan / 1.05 G de diamètre, c’est le plus vaste édifice zone centrale du volcan et aux vallées qui l’ont Montagnes de Saint Jean-de-Dône / 1.05 H volcanique unitaire de toute l’Europe... disséquée et en partie démantelée. Même s’ils Plateau de Girgols / 1.05 I Plateau de Legal / ne sont pas directement «lisibles» sur le ter- 1.05 J Plateau de Malgorce / 1.05 K Volcan du Sans compter d’autres plateaux qui rain, rien n’imposant dans les paysages l’image puy Violent / 1.05 L Planèze de Salers / 1.05 M forment comme des satellites de la que l’on se fait habituellement d’un volcan, les Planèze de Trizac / 1.05 N Plateau de la Font- montagne principale : le Cézallier, phénomènes volcaniques sont à l’origine des Sainte / 1.05 O Planèze du Limon / 1.05 P Bois l’Aubrac ». -
Thirty-Fourth List of New Mineral Names
MINERALOGICAL MAGAZINE, DECEMBER 1986, VOL. 50, PP. 741-61 Thirty-fourth list of new mineral names E. E. FEJER Department of Mineralogy, British Museum (Natural History), Cromwell Road, London SW7 5BD THE present list contains 181 entries. Of these 148 are Alacranite. V. I. Popova, V. A. Popov, A. Clark, valid species, most of which have been approved by the V. O. Polyakov, and S. E. Borisovskii, 1986. Zap. IMA Commission on New Minerals and Mineral Names, 115, 360. First found at Alacran, Pampa Larga, 17 are misspellings or erroneous transliterations, 9 are Chile by A. H. Clark in 1970 (rejected by IMA names published without IMA approval, 4 are variety because of insufficient data), then in 1980 at the names, 2 are spelling corrections, and one is a name applied to gem material. As in previous lists, contractions caldera of Uzon volcano, Kamchatka, USSR, as are used for the names of frequently cited journals and yellowish orange equant crystals up to 0.5 ram, other publications are abbreviated in italic. sometimes flattened on {100} with {100}, {111}, {ill}, and {110} faces, adamantine to greasy Abhurite. J. J. Matzko, H. T. Evans Jr., M. E. Mrose, lustre, poor {100} cleavage, brittle, H 1 Mono- and P. Aruscavage, 1985. C.M. 23, 233. At a clinic, P2/c, a 9.89(2), b 9.73(2), c 9.13(1) A, depth c.35 m, in an arm of the Red Sea, known as fl 101.84(5) ~ Z = 2; Dobs. 3.43(5), D~alr 3.43; Sharm Abhur, c.30 km north of Jiddah, Saudi reflectances and microhardness given. -
New Mineral Names*
American Mineralogist, Volume 97, pages 2064–2072, 2012 New Mineral Names* G. DIEGO GATTA,1 FERNANDO CÁMARA,2 KIMBERLY T. TAIT,3,† AND DMITRY BELAKOVSKIY4 1Dipartimento Scienze della Terra, Università degli Studi di Milano, Via Botticelli, 23-20133 Milano, Italy 2Dipartimento di Scienze della Terra, Università di degli Studi di Torino, Via Valperga Caluso, 35-10125 Torino, Italy 3Department of Natual History, Royal Ontario Museum, 100 Queens Park, Toronto, Ontario M5S 2C6, Canada 4Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia IN THIS ISSUE This New Mineral Names has entries for 12 new minerals, including: agardite-(Nd), ammineite, byzantievite, chibaite, ferroericssonite, fluor-dravite, fluorocronite, litochlebite, magnesioneptunite, manitobaite, orlovite, and tashelgite. These new minerals come from several different journals: Canadian Mineralogist, European Journal of Mineralogy, Journal of Geosciences, Mineralogical Magazine, Nature Communications, Novye dannye o mineralakh (New data on minerals), and Zap. Ross. Mineral. Obshch. We also include seven entries of new data. AGARDITE-(ND)* clusters up to 2 mm across. Agardite-(Nd) is transparent, light I.V. Pekov, N.V. Chukanov, A.E. Zadov, P. Voudouris, A. bluish green (turquoise-colored) in aggregates to almost color- Magganas, and A. Katerinopoulos (2011) Agardite-(Nd), less in separate thin needles or fibers. Streak is white. Luster is vitreous in relatively thick crystals and silky in aggregates. Mohs NdCu6(AsO4)3(OH)6·3H2O, from the Hilarion Mine, Lavrion, Greece: mineral description and chemical relations with other hardness is <3. Crystals are brittle, cleavage nor parting were members of the agardite–zálesíite solid-solution system. observed, fracture is uneven. Density could not be measured Journal of Geosciences, 57, 249–255. -
GRECO G : Massif Central
Grande région écologique G Massif central Sarthe Loiret Yonne ANGERS Loir-et-Cher ¯ Maine-et-Loire Nièvre Indre-et- Côte-d'Or Loire NEVERS Cher Vienne CHÂTEAUROUX Saône-et- Indre Vendée Loire POITIERS MOULINS NIORT Allier Deux-Sèvres GUÉRET Creuse Charente- Maritime Loire Ain Puy-de-Dôme LIMOGES Rhône Haute- CLERMONT- FERRAND ANGOULÊME Vienne LYON Charente Isère SAINT-ÉTIENNE Corrèze TULLE Haute-Loire Gironde Dordogne Cantal LE PUY- G11 Châtaigneraie du Centre et de l'Ouest EN-VELAY VALENCE G12 Marches du Massif central AURILLAC Ardèche G13 Plateaux limousins Lot Lozère PRIVAS G21 Plateaux granitiques ouest du Massif central Lot-et- MENDE Drôme Garonne G22 Plateaux granitiques du centre Aveyron Ardèche du Massif central RODEZ Vaucluse G23 Morvan et Autunois Tarn-et- LandesG30 Massif central volcanique Garonne Gard G41 Bordure Nord-Est du Massif central AVIGNON G42 Monts du Vivarais et du Pilat Gers ALBI G50 Ségala et Châtaigneraie auvergnate NÎMES G60 Grands Causses Tarn Hérault TOULOUSE Bouches- G70 Cévennes Haute- MONTPELLIER du-Rhône G80 Haut-Languedoc et Lévézou Garonne G90 Plaines alluviales et piémonts Aude Méditerranée du Massif centralHautes- Pyrénées- Limite de départementPyrénées CARCASSONNE Atlantiques 05025 km Limite de GRECO Ariège Sources : BD CARTO® IGN, BD CARTHAGE® IGN Agences de l'Eau. Les SER de la GRECO G : Massif Central La GRECO G : Massif central est un collines, plaines et vallées, il occupe Par leur ressemblance climatique et massif hercynien de moyenne mon- environ un sixième (85 000 km²) géologique avec la Châtaigneraie tagne, culminant à 1 886 m au Puy de la superfi cie de la France et est limousine, les hauteurs de Gâtine de Sancy, aux reliefs arrondis, limité situé entièrement dans le domaine (Deux-Sèvres) y ont été rattachées, par le Bassin aquitain à l’ouest, biogéographique atlantique, en si bien que la GRECO regroupe le Bassin parisien au nord, la val- limite d’infl uences continentales à 14 sylvoécorégions (SER). -
The Iberian Variscan Orogen
CHAPTER 1 THE IBERIAN VARISCAN OROGEN Aerial view of the tectonic repetition of limestone beds in the Láncara Formation, Primajas duplex structure of the Esla thrust (photo by J.L. Alonso) Martínez Catalán, J.R. Aller, J. Alonso, J.L. Bastida, F. Rocks of Upper Proterozoic to Carboniferous age - forming the Variscan or Hercynian orogen - crop out widely in the western part of the Iberian Peninsula, in what is called the Iberian or Hesperian Massif. These deformed rocks, often metamorphosed and intruded by different types of granitoids, were witness to the great mountain range formed in the late Paleozoic, basically in the Late Devonian and Carboniferous (between 370 and 290 million years ago), by the convergence and collision of two major continents: Laurasia and Gondwana. The Iberian Massif constitutes a geological framework of global interest. It is unique due to the continuity of its exposures and because it displays excellent records allowing the analysis of continental crust features, the tectonic, metamorphic and magmatic evolution of orogens, and therefore provides enormously relevant data about the lithospheric dynamics during the latest Precambrian and the Paleozoic. The Variscan orogen forms the basement of the Figure 1. Scheme showing the position of the Iberian Iberian Peninsula and of most of western and central Peninsula in relation to the Appalachians and the Europe. A crustal basement is the result of an orog- Caledonian and Variscan belts. Modified from eny, that is, the consequence of a deep remobilization Neuman and Max (1989). of the continental crust caused by the convergence of plates, and is associated to uplift and the creation of relief. -
World Geomorphological Landscapes
World Geomorphological Landscapes Series Editor: Piotr Migoń For further volumes: http://www.springer.com/series/10852 Monique Fort • Marie-Françoise André Editors Landscapes and Landforms o f F r a n c e Editors Monique Fort Marie-Françoise André Geography Department, UFR GHSS Laboratory of Physical CNRS UMR 8586 PRODIG and Environmental Geography (GEOLAB) University Paris Diderot-Sorbonne-Paris-Cité CNRS – Blaise Pascal University Paris , France Clermont-Ferrand , France Every effort has been made to contact the copyright holders of the fi gures and tables which have been reproduced from other sources. Anyone who has not been properly credited is requested to contact the publishers, so that due acknowledgment may be made in subsequent editions. ISSN 2213-2090 ISSN 2213-2104 (electronic) ISBN 978-94-007-7021-8 ISBN 978-94-007-7022-5 (eBook) DOI 10.1007/978-94-007-7022-5 Springer Dordrecht Heidelberg New York London Library of Congress Control Number: 2013944814 © Springer Science+Business Media Dordrecht 2014 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifi cally the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfi lms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifi cally for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. -
Italian Type Minerals / Marco E
THE AUTHORS This book describes one by one all the 264 mi- neral species first discovered in Italy, from 1546 Marco E. Ciriotti was born in Calosso (Asti) in 1945. up to the end of 2008. Moreover, 28 minerals He is an amateur mineralogist-crystallographer, a discovered elsewhere and named after Italian “grouper”, and a systematic collector. He gradua- individuals and institutions are included in a pa- ted in Natural Sciences but pursued his career in the rallel section. Both chapters are alphabetically industrial business until 2000 when, being General TALIAN YPE INERALS I T M arranged. The two catalogues are preceded by Manager, he retired. Then time had come to finally devote himself to his a short presentation which includes some bits of main interest and passion: mineral collecting and information about how the volume is organized related studies. He was the promoter and is now the and subdivided, besides providing some other President of the AMI (Italian Micromineralogical As- more general news. For each mineral all basic sociation), Associate Editor of Micro (the AMI maga- data (chemical formula, space group symmetry, zine), and fellow of many organizations and mine- type locality, general appearance of the species, ralogical associations. He is the author of papers on main geologic occurrences, curiosities, referen- topological, structural and general mineralogy, and of a mineral classification. He was awarded the “Mi- ces, etc.) are included in a full page, together cromounters’ Hall of Fame” 2008 prize. Etymology, with one or more high quality colour photogra- geoanthropology, music, and modern ballet are his phs from both private and museum collections, other keen interests.