Imenrt-Crrapelle ^American (Cemetery Nnb Jhemortal

Total Page:16

File Type:pdf, Size:1020Kb

Imenrt-Crrapelle ^American (Cemetery Nnb Jhemortal IMenrt-Crrapelle ^American (Cemetery nnb JHemortal The American Battle Monuments Commission 1986 The Guardian Angel 3 JCmrt-COjapeUe (Cemetery anb iHemnnal LOCATION follow Aachen highway east approxi­ mately 1 mile/1.6 km, then turn right The Henri-Chapelle Cemetery and on Aubel Road 7.5 miles/12 km to Memorial lies 2 miles northwest of the Hagelstein, thence left on N-18 to the village of Henri-Chapelle which is on cemetery or by Autoroute E-5, Liege the main highway from Liege, Bel­ or Aachen to the Battice exit and then gium to Aachen, Germany (18 miles/ turn right on N-3 to Henri-Chapelle. 29 km from Liege or 10 miles/16 km from Aachen). It can be reached by HOURS train from Paris (Gare du Nord — 5V2 hours), from Brussels (2 hours) The cemetery is open daily to the and Liege, Belgium, or from Germany public as shown below: via Aachen, to Welkenraedt, Bel­ SUMMER (16 March-30 September) gium, where taxicab service to the 9:00 a.m.-6:00 p.m. — weekdays cemetery, 4V2 miles distant, is avail­ 10:00 a.m.-6:00 p.m. — Saturdays, able. To reach the cemetery by auto­ Sundays and holidays mobile, follow N-3 from Liege or WINTER (1 October-15 March) Aachen to the road fork in Henri- 9:00 a.m.-5:00 p.m. — weekdays Chapelle, thence northwest on N-18 10:00 a.m.-5:00 p.m. — Saturdays, to the cemetery; or, from Margraten Sundays and holidays Entrance Pylons 4 Aerial View of Cemetery When the cemetery is open to the launched a powerful counterattack in public, a staff member is on duty in an attempt to split the Allied forces the Visitors' Room to answer ques­ and isolate the U.S. Third Army. tions and escort relatives to grave and Resisting vigorously, Allied ground memorial sites (except between noon and air forces not only stopped the and 3:00 p.m. on weekends and holi­ attacking enemy but threatened him days). with complete encirclement. Thor­ oughly defeated after suffering great HISTORY losses, the enemy beat a hasty retreat across the Seine River. Following the successful landings on Rapid exploitation of this victory the beaches of Normandy on 6 June resulted in swift Allied advances far 1944, the Allies slowly but relentlessly exceeding expectations. On the left fought their way inland to expand the flank, the Canadian First Army drove beachhead. Then on 25 July, after a along the coast reaching the Nether­ paralyzing air bombardment, the lands frontier and liberating Ostend U.S. First Army launched the attack and Bruges early in September, while southward to break out. Joining the the British Second Army advanced assault a few days later, the U.S. rapidly through central Belgium liber­ Third Army on the right flank thrust ating Brussels on 3 September and southward along the coast while the Antwerp the following day. The Brit­ British and Canadians advanced on ish Second Army then moved to join the left flank. with the Canadian First Army astride When the breakout occurred, the Netherlands frontier. Allied planners had expected the In the center of the advance, the enemy to withdraw and re-establish a U.S. First Army freed Liege in eastern defense at the line of the Seine River Belgium on 8 September and con­ to the northeast. Instead, the enemy tinued northeastward toward the Ger- 3 Location of Cemetery Features man city of Aachen, while at the same and the French First Army which time liberating Luxembourg. On the extended Allied lines to the Swiss bor­ right, the U.S. Third Army swept der, resistance was organized around across France to reach the Moselle heavily fortified cities forming strong- River and make contact with the points in front of the Siegfried Line. In troops of the U.S. Seventh Army the north, the defenders utilized to ad­ advancing from the beaches of south­ vantage against the British and Cana­ ern France, where they had landed on dians the barriers formed by the ex­ 15 August. tensive canal and river systems. On 17 Patrols of the U.S. First Army September, a valiant combined air­ crossed the German frontier in the borne-ground assault in the Nether­ Ardennes area on 11 September. The lands intended to outflank the north next day, elements of the U.S. First end of the enemy line, achieved only Army crossed the frontier near partial success as it failed to seize Aachen and moved eastward toward crossings of the lower Rhine. the Siegfried Line, where strong resist­ For the next three months, intensive ance was encountered immediately. fighting produced only limited gains Almost simultaneously, progress against fierce opposition. During this slowed all along the advancing Allied period, the principal Allied offensive line as opposition stiffened. The effort was concentrated in the center retreating enemy had at last stabilized of the enemy line where some of the its line of defense. most bitter fighting of the war The Siegfried Line formed the core occurred in the battle to capture the of resistance at the center of the en­ city of Aachen, the first large German emy defenses. To the south in front of city to be captured by the Allies, and the U.S. Third and Seventh Armies, penetrate the Siegfried Line. Finally, 6 encircled in mid-October after savage vade Germany itself. During Febru­ house-to-house fighting, Aachen fell ary and March, with the aid and on 31 October. Meanwhile, the U.S. assistance of fighters and medium Ninth Army organized at Brest in bombers, the first step was success­ Brittany, moved into the lines on the fully completed and heavy losses were right flank of the U.S. First Army. To inflicted on the enemy. Because of the south, the U.S. Third and Seventh those losses, the subsequent crossing Armies continued to advance slowly, of the Rhine did not meet with the vi­ as the U.S. Seventh Army forced the olent opposition that had been antici­ enemy back into the Vosges Moun­ pated. Working together, Allied tains. ground and air forces swept victori­ On 4 November, the U.S. First ously across Germany, bringing the Army began the difficult struggle war in Europe to a conclusion on 8 through the dense woods of the May 1945. Hurtgen Forest. Shortly thereafter, the U.S. Ninth Army was shifted to SITE the U.S. First Army's left flank. Then, on 16 November preceded by a mas­ The cemetery, 57 acres in area, lies on sive air bombardment, the two armies the crest of a ridge affording an excel­ attacked together opening a wide gap lent view to the east and west. The in the Siegfried Line. By 1 December, memorial is visible from Highway N- the Roer River line was reached. On 3 several miles away. Highway N-18 the right, the city of Metz was cap­ separates the overlook to the north­ tured by the U.S. Third Army on 22 west from the rest of the cemetery. November, although the last fort The site was liberated on 12 Sep­ defending that city did not surrender tember 1944 by troops of the U.S. 1st until 13 December. The greatest terri­ Infantry Division. A temporary ceme­ torial gains, however, came in the tery was established on 28 September south where the U.S. Seventh Army 1944 two or three hundred yards to penetrated the Vosges Mountains to the north of the present site which was liberate the city of Strasbourg on 23 selected because of its more attractive November as French troops on the setting. Here rest 7,989 of our military extreme right flank liberated Mul- Dead, most of whom gave their lives house. in the repulse of the German counter- offensive in the Ardennes or during The Schelde estuary was finally the advance into, and across, Ger­ cleared of the enemy by the Canadian many during the fall and winter of First Army and the great port city of 1944 and the spring of 1945. Others Antwerp became available on 28 No­ were lost in air operations over the vember to supply the Allied armies. region. The cemetery and memorial Suddenly on 16 December 1944, the were completed in 1960. Allied advance was interrupted when the enemy launched in the Ardennes its final major counteroffensive of the ARCHITECTS war, with a second major assault on Architects for the cemetery and me­ New Year's Eve in Alsace to the south. morial were Holabird, Root and After furious fighting in bitterly cold Burgee of Chicago, Illinois. The land­ weather these last enemy onslaughts scape architect was Franz Lipp of were halted and the lost ground Chicago. regained. The Allies then developed their plan for final victory. GENERAL LAYOUT The first step of the plan was to clear all enemy from west of the To the west of Highway N-18 where it Rhine; the subsequent step was to in­ crosses the reservation is the overlook 7 area with its flagstaff. From the west paved with gray St. Gothard granite end of this area a wide view is from Switzerland. afforded over the broad valley of the Berwinne streamlet (which lies in the THE COLONNADE sector of advance of the U.S. 1st In­ fantry Division) and the ridges On the 48 faces of the 24 pylons and beyond. The roadway on the over­ the 4 faces of the engaged pylons at look is lined with linden trees. the ends of the colonnade are en­ East of the highway is the memo­ graved the seals of the wartime 48 rial; there are parking areas at both States, 3 territories and the District of the north and south ends.
Recommended publications
  • L'église De L'abbaye Cistercienne Notre-Dame Du Val-Dieu
    UNIVERSITE DE LIEGE Faculté de Philosophie & Lettres L’église de l’abbaye cistercienne Notre-Dame du Val-Dieu Mémoire présenté par Jérôme Eeckhout en vue de l’obtention du grade de licencié en Histoire de l’Art et Archéologie Année académique 1998-1999 1 REMERCIEMENTS Cette étude n’aurait pu être réalisée sans le concours de nombreuses personnes. Je tiens à remercier Monsieur Patrick Hoffsummer, directeur de ce mémoire, ainsi que Messieurs Albert Lemeunier et Benoît Van den Bossche, lecteurs. Leurs remarques avisées ont précisé et orienté de manière judicieuse mes recherches et mes analyses. L’organisation de ce travail doit également beaucoup aux conseils méthodologiques qu’ils m’ont donnés. Ma plus grande reconnaissance s’adresse à Dom Bernard Kaul (†), Père André Meys, Frère Benoît, et Frère Albéric. Le soutien qu’ils ont manifesté à mon égard m’a permis de travailler dans les meilleures conditions. Qu’ils soient remerciés pour leur bienveillance, pour les nombreuses informations reçues et pour les kilomètres parcourus avec moi dans l’abbaye. Que messieurs et mesdames les conservateurs de musées et de dépôts d’archives ainsi que les propriétaires d’œuvres veuillent trouver ici l’expression de ma gratitude : Monsieur Albert Lemeunier, du Musée d’Art religieux et d’Art mosan à Liège, Madame Marie-Paule Deblanc- Magnée, du Musée des Beaux-Arts à Verviers, Monsieur Alfred Minke, des Archives de l’Etat à Eupen, ainsi que le Docteur et Madame José Vieillevoye-Henrotay. De précieuses remarques ont été fournies par Madame Terryl N. Kinder lors de sa visite au Val-Dieu durant l’été 1998.
    [Show full text]
  • Visé Sint-Martens Voeren Laurent BARCHY Et Jean-Marc MARION
    34/7-8 34/7-8 OEREN S - V ARTEN -M INT - S É S VI E V LICATI XP E NOTICE VISÉ SINT-MARTENS VOEREN CARTE GÉOLOGIQUE DE LA WALLONIE ÉCHELLE : 1/25 000 NOTICE EXPLICATIVE DIRECTION GÉNÉRALE OPÉRATIONNELLE DE L’AGRICULTURE, DES RESSOURCES NATURELLES ET DE L’ENVIRONNEMENT CARTE GÉOLOGIQUE DE WALLONIE : 1/25 000 Plus d'infos concernant la carte géologique de Wallonie : http://geologie.wallonie.be [email protected] Un document édité par le Service public de Wallonie, Direction générale de l’Agriculture, des Ressources naturelles et de l’Environnement. Dépôt légal : D/2017/11802/03 Éditeur responsable : Brieuc Quévy, Directeur général, DGARNE - Avenue Prince de Liège, 15 - B-5100 Namur. Reproduction interdite. SPW | Éditions, CARTES N° vert : 1718 (informations générales) - 1719 (germanophones) Site : www.wallonie.be VISÉ SINT-MARTENS VOEREN Laurent BARCHY et Jean-Marc MARION Université de Liège Département de Géologie Paléontologie animale et humaine Sart-Tilman, B 18, B-4000 Liège Photographie de couverture : carrière de Visé, stratotype du Viséen Zones G et H de la carrière illustrée à la fig. 5 page 15 Cliché : J-M Marion NOTICE EXPLICATIVE 2017 Dossier complet déposé : décembre 2006 Accepté pour publication : novembre 2007 CARTE VISÉ - ST-MARTENS - VOEREN 34/7-8 RÉSUMÉ Située à cheval sur l'extrême nord de la province de Liège, le Limbourg belge et le Limbourg néerlandais, la portion de territoire couverte par la carte peut-être divisée en trois régions : la plaine alluviale de la Meuse, la région des terrasses de la Meuse et le Pays fouronnais qui est le prolongement nord du Pays de Herve.
    [Show full text]
  • Armies and Ecosystems in Premodern Europe: the Meuse Region, 1250–1850
    WCP ARMIES AND ECOSYSTEMS IN PREMODERN EUROPE THE MEUSE REGION, 1250–1850 Using the ecosystem concept as his starting point, the author examines the complex relationship between premodern armed forces and their environ- and Conflict in War ment at three levels: landscapes, living beings, and diseases. The study focuses Societies Premodern on Europe’s Meuse Region, well-known among historians of war as a battle- ground between France and Germany. By analyzing soldiers’ long-term inter- actions with nature, this book engages with current debates about the eco- ARMIES AND ECOSYSTEMS IN PREMODERN EUROPE IN PREMODERN logical impact of the military, and provides new impetus for contemporary armed forces to make greater effort to reduce their environmental footprint. “This is an impressive interdisciplinary study, contributing to environmental history, the history of war and historical geography. The book advances an original and intriguing argument that armed forces have had a vested interest in preserving the environments and habitats in which they operate, and have thus contributed to envi- ronmental conservation long before this became a popular cause of wider humanity. The work will provide a template for how this topic can be researched for other parts of the world or for other time periods.” Peter H. Wilson, Chichele Professor of the History of War, University of Oxford War and Confl ict in Premodern Societies is a pioneering series that moves away from strategies, battles, and chronicle histories in order to provide a home for work that places warfare in broader contexts, and contributes new insights ARMIES AND ECOSYSTEMS on everyday experiences of confl ict and violence.
    [Show full text]
  • Low Flow Regionalisation in the Walloon Region
    Low flow regionalisation in the Walloon region September 2012 Title Low flow regionalisation in the Walloon region Authors Maud Grandry, Arnaud Verstraete, Sébastien Gailliez, Aurore Degré Date September 2012 Lead partner ULg Gembloux Agro-Bio Tech Partners involved ULg Gembloux Agro-Bio Tech Work package 1 Action 3 AMICE Adaptation of the Meuse to the Impacts of Climate Evolutions is an INTERREG IVB North West Europe Project (number 074C). Climate change impacts the Meuse basin creating more floods and more droughts. The river managers and water experts from 4 countries of the basin join forces in this EU-funded transnational project to elaborate an innovative and sustainable adaptation strategy. The project runs lasts from 2009 through 2012. To learn more about the project visit: www.amice-project.eu The NWE INTERREG IV B Programme The Programme funds innovative transnational actions that lead to a better management of natural resources and risks, to the improvement of means of communication and to the reinforcement of communities in North-West Europe. To learn more about the programme visit www.nweurope.eu 2 Table of contents 1. Introduction..................................................................................................................... 4 2. Hydrological data .......................................................................................................... 4 3. Frequency analysis....................................................................................................... 6 4. Calculation of the
    [Show full text]
  • Dalhem 42/3-4
    DALHEM-HERVE 42/3-4 DALHEM HERVE 42/3-4 NOTICE EXPLICATIVE CARTE GEOLOGIQUE DE WALLONIE CARTE GEOLOGIQUE DE WALLONIE : 1/25.000 ECHELLE : 1/25.000 NOTICE EXPLICATIVE DALHEM-HERVE Laurent BARCHY & Jean-Marc MARION Université de Liège Service de paléontologie animale et humaine Sart-Tilman, B 18, B-4000 Liège Photographie de couverture : Mine de Blégny-Trembleur et son terril avec en avant-plan les fruitiers hautes tiges typiques du Pays de Herve NOTICE EXPLICATIVE 2000 Dépôt légal : D/2000/5322/64 Carte Dalhem-Herve n° 42-3/4 Résumé Située dans le nord de la province de Liège, la portion de territoire couverte par la carte montre des contrastes importants; ils sont liés à la constitution de son socle et résul- tent aussi de processus géomorphologiques. Trois régions peu- vent être définies : la plaine alluviale de la Meuse, la région des terrasses et la dépression d'Aubel, dans le Pays de Herve. Le sous-sol est constitué par des dépôts paléozoïques qui affleurent dans les vallées et qui s'étagent, avec quelques lacunes, depuis le Silurien (reconnu dans plusieurs sondages) jusqu'au Westphalien. Ces dépôts sont recouverts en discor- dance par les terrains sub-horizontaux d'âge crétacé supérieur et tertiaire et enfin, par les alluvions quaternaires. Du point de vue structural, l'histoire de ces dépôts com- porte d'abord une déformation synsédimentaire dévono-dinan- tienne liée à une tectonique de blocs. Vient ensuite l'orogenèse varisque, au cours de laquelle les dépôts ont été faillés (failles précoces ou plats-crains) puis plissés et de nouveau faillés (che- vauchements).
    [Show full text]
  • Final Report | 31/12/2013 (Revision | 31/03/2014)
    1. LP3LP Landscape Policy for the Three Countries Park Targeted Analysis 2013/2/21 Final Report | 31/12/2013 (Revision | 31/03/2014) Main Report ESPON 2013 1 This report presents the final results of a Targeted Analysis conducted within the framework of the ESPON 2013 Programme, partly financed by the European Regional Development Fund. The partnership behind the ESPON Programme consists of the EU Commission and the Member States of the EU27, plus Iceland, Liechtenstein, Norway and Switzerland. Each partner is represented in the ESPON Monitoring Committee. This report does not necessarily reflect the opinion of the members of the Monitoring Committee. Information on the ESPON Programme and projects can be found on www.espon.eu The web site provides the possibility to download and examine the most recent documents produced by finalised and ongoing ESPON projects. This basic report exists only in an electronic version. © ESPON & the LP3LP TPG, 2014. Printing, reproduction or quotation is authorised provided the source is acknowledged and a copy is forwarded to the ESPON Coordination Unit in Luxembourg. ESPON 2013 2 List of authors Prof. Dr. Frank Lohrberg Timo Matti Wirth Anja Brüll RWTH Aachen University (Lead Partner) Chair of landscape architecture Jakobstraße 2 52056 Aachen Germany Marc Nielsen Alain Coppens Prof. Marie-Françoise Godart Université libre de Bruxelles (Project Partner) 50 av. F. D. Roosevelt CP 130/02 B-1050 Brussels Belgium External expert - Alain Malherbe (CREAT-UCL) Annet Kempenaar Dr. Marlies Brinkhuijsen Fiona Morris Wageningen Universiteit (Project Partner) Droevendaalsesteeg 3 36708 PB Wageningen Netherlands ESPON 2013 3 Table of contents 1.
    [Show full text]
  • On the Lateglacial and Postglacial Vegetation of South Limburg (Netherlands)
    On the lateglacial and postglacial vegetation of South Limburg (Netherlands) C.R. Janssen (Botanical Museum and Herbarium, State University, Utrecht) (received May 20th, 1960) CONTENTS chapter i. Introduction 2 chapter n. Geological Structure 3 chapter m. Peat Deposits 6 chapter rv. Present Aspect ofthe Vegetation 13 chapter v. Materials and Methods 18 chapter vi. The Bogs 20 Benzenrade 21 Ravensbos 23 Groenebeemden 24 Wolffsheid 25 Moorveld 26 Noorbeek 26 Sijlerbeek 27 Klimmen 27 Hulsberg 27 Leiffenderven 28 Brommelen 35 Nuth 38 Anselerbeek 40 Rimburg 41 Cortenbach, Voerendaal 44 Brunssum 48 Discussion of the vegetation of the bogs 51 chapter vii. Discussion of the Zones 53 Zone i, ii and in 59 Zone rv 62 Zone v 63 Zone and vi vn 66 . Zone vni 71 Zone ix 80 Zone x 84 Discussion Individual chapter vm. of some Constituents of theVegeta- tion 92 chapter ix. Relations to the History of Human Occupation 102 .... CHAPTER X. ZONATTON AND DATING 104 1 2 C. R. JANSSEN CHAPTER I INTRODUCTION The history of the vegetation found in the southern part of the of to now unknown. This is province Limburg was up practically partly due to the scarcity of peat sediments which makes this region with other of the unattractive to palynologists. Compared parts Netherlands South Limburg shows in its soil as well as in its climate a particular character. The soil in the area investigated by us consists of limestone and of loess. For that reason and also on account of its somewhat different climate its vegetation presently differs conspic- uously from that found in the other parts of the Netherlands.
    [Show full text]
  • Dénombrement Du Limbourg
    BE-A0523_715466_715459_FRE Inventaire des archives du comité du dénombrement et du cadastre du Limbourg (Duché de Limbourg, pays de Dalhem, de Fauquemont (Valkenburg) et de Rolduc (`s- Hertogenrade) / Bruno Dumont Het Rijksarchief in België Archives de l'État en Belgique Das Staatsarchiv in Belgien State Archives in Belgium This finding aid is written in French. 2 Dénombrement du Limbourg DESCRIPTION DU FONDS D'ARCHIVES:............................................................................7 Consultation et utilisation..............................................................................................8 Conditions d'accès............................................................................................................8 Conditions de reproduction...............................................................................................8 Caractéristiques matérielles et contraintes techniques.................................................8 Instruments de recherche................................................................................................8 Recommandations pour l'utilisation................................................................................8 Contenu et structure....................................................................................................10 Contenu...........................................................................................................................10 Sélections et éliminations..............................................................................................11
    [Show full text]
  • The Thermal Spring of Elven- Schans-Navagne In
    THE THERMAL SPRING OF ELVEN- The subsurface is composed of turbiditic limestones of SCHANS-NAVAGNE IN MOELINGEN Upper Viséan age, attaining easily 500 m in thickness. (VOEREN-FOURONS) AND ITS GEO- All these beds dip 30° East, probably resulting from a transpressional bulge over the southern Border Fault LOGICAL ORIGIN (`faille bordière') of the Brabant Massif which must NEW INSIGHTS AS A RESULT OF GEOLOGICAL follow here a NNE-SSW direction along the west mar- RECONNAISSANCE FOR A GAS PIPELINE gin of the Meuse river valley incision. The Visé-Puth subsidence basin, located in between the Border and Michiel DUSAR' Anticlinaal-Oranje fault systems, accomodated thick carbonate sequences derived from a shallow, highly 1. Geological Survey of Belgium, Jennerstraat 13, B-1000 productive carbonate platform near Visé and deposited Brussel as seasonal(?) mudflows on the unstable slope. Pervasive silicification affected these beds in and around The originally artesian thermal well of Elvenschans- karst solution structures developed during different Navagne served for the water supply of the medieval emersion phases from the base Namurian onwards. moat Elvenschans, later Spanish bastion Navagne, over- Tropical weathering during the Cretaceous installed a looking the Meuse river. A farmhouse De Schans was 100 m deep paleosol on the silicites, characterised by a later built on the ruins of the historic site. bleached kaolinised upper zone and an black carbo- The thermal well is located on the lower terrace of the naceous lower zone. Late Cretaceous to Tertiary tilting Meuse river, above the highest flood level. The arte- and subsequent erosion finally resulted in variable sian nature (which gradually disappeareded since a new depths to relative unaltered but karstified limestones, water production well tapped the same aquifer at 15 m silicites, black and white paleosols.
    [Show full text]
  • CROSSBORDER INTEGRATION BETWEEN the NETHERLANDS and BELGIUM the Case of Water Quality in the Meuse River Basin
    CROSSBORDER INTEGRATION BETWEEN THE NETHERLANDS AND BELGIUM The case of water quality in the Meuse River Basin Angeliki Karydi Master Thesis Nijmegen School of Management Radboud University MA Environment and Society Studies 0 1 CROSSBORDER INTEGRATION BETWEEN THE NETHERLANDS AND BELGIUM The case of water quality in the Meuse River Basin Colophon Author: Angeliki Karydi Student number: s1025954 Word Count: 28000 Internal supervisor: Daan Boezeman, Radboud University Nijmegen External supervisor: Noud Kuijpers, ProgrammaBureau Maas University: Radboud University Nijmegen Faculty: School of Management Degree: MA Environment and Society Studies Course: Master Thesis Date: 22.08.2019 2 Contents Summary ................................................................................................................................................. 5 CHAPTER 1 ........................................................................................................................................... 8 1.1 INTRODUCTION ......................................................................................................................... 8 1.2 PROBLEM STATEMENT ............................................................................................................ 8 1.3 SOCIETAL AND SCIENTIFIC RELEVANCE ........................................................................... 10 1.4 RESEARCH AIM AND RESEARCH QUESTION ..................................................................... 11 1.5 READING STRUCTURE...........................................................................................................
    [Show full text]
  • An Evaluation of Restocking Practice and Demographic Stock Assessment Methods for Cryptic Juvenile European Eel in Upland Rivers
    sustainability Article An Evaluation of Restocking Practice and Demographic Stock Assessment Methods for Cryptic Juvenile European Eel in Upland Rivers Billy Nzau Matondo 1,* , Jean-Philippe Benitez 1 , Arnaud Dierckx 1, Xavier Rollin 2 and Michaël Ovidio 1 1 Laboratory of Fish Demography and Hydroecology, Biology of Behaviour Unit, Freshwater and Oceanic science Unit of Research-FOCUS, University of Liège, 22 Quai E. Van Beneden, B-4020 Liège, Belgium; [email protected] (J.-P.B.); [email protected] (A.D.); [email protected] (M.O.) 2 DGO3-DNF-Fisheries Service, Public Service of Wallonia, 5100 Jambes, Belgium; [email protected] * Correspondence: [email protected]; Tel.: +32-4-3669227 Received: 26 November 2019; Accepted: 2 February 2020; Published: 5 February 2020 Abstract: Restocking of the critically endangered European eel Anguilla anguilla is widespread, but it is rarely scientifically evaluated. Methods used to assess its associated performance by estimating the survival rate and implement restocking for maximum recruitment in rivers have not yet been investigated. Based on two glass eel restocking events using a single release site/point and multiple sites per river performed in upland rivers (>340 km from the North Sea), the recruitment success of stocked eels was scientifically evaluated during a 3-year study using multiple capture-mark-recapture methods and mobile telemetry. We compared the observed data with the data estimated from the Telemetry, De Lury and Jolly-Seber stock assessment methods. For recruitment data, Telemetry was very close to Jolly-Seber, an appropriate stock assessment method for open populations. Using the best model of Jolly-Seber, survival probability was higher (>95%) in both restocking practices, but recruitment yields were higher and densities of stocked eels were lower in multiple sites compared to a single site.
    [Show full text]
  • Carte Hydrogéologique De Dalhem - Herve DALHEM - HERVE
    DALHEM - HERVE 42/3-4 Notice explicative CARTE HYDROGÉOLOGIQUE DE WALLONIE Echelle : 1/25 000 Photos couverture © SPW-DGARNE(DGO3) Fontaine de l'ours à Andenne Forage exploité Argilière de Celles à Houyet Puits et sonde de mesure de niveau piézométrique Emergence (source) Essai de traçage au Chantoir de Rostenne à Dinant Galerie de Hesbaye Extrait de la carte hydrogéologique de Dalhem - Herve DALHEM - HERVE 42/3-4 Ingrid RUTHY, Alain DASSARGUES Université de Liège Sart-Tilman - Bâtiment B52 B-4000 Liège (Belgique) NOTICE EXPLICATIVE 2008 Première édition : Mai 2003 Actualisation partielle : Janvier 2008 Dépôt légal –D/2008/12.796/1 - ISBN : 978-2-8056-0058-6 SERVICE PUBLIC DE WALLONIE DIRECTION GENERALE OPERATIONNELLE DE L'AGRICULTURE, DES RESSOURCES NATURELLES ET DE L'ENVIRONNEMENT (DGARNE-DGO3) AVENUE PRINCE DE LIEGE, 15 B-5100 NAMUR (JAMBES) - BELGIQUE I. INTRODUCTION ............................................................................................................ 4 II. CADRE GEOGRAPHIQUE, HYDROGRAPHIQUE ET GEOMORPHOLOGIQUE..................................................................................................... 5 III. CADRE GEOLOGIQUE.............................................................................................. 7 III.1 CADRE GEOLOGIQUE REGIONAL................................................................................. 7 III.2 CADRE GEOLOGIQUE DE LA CARTE ............................................................................ 8 III.2.1 CADRE LITHO-STRATIGRAPIQUE ................................................................................
    [Show full text]