Bridge Technology and Historical Scholarship
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Response of Drainage Systems to Neogene Evolution of the Jura Fold-Thrust Belt and Upper Rhine Graben
1661-8726/09/010057-19 Swiss J. Geosci. 102 (2009) 57–75 DOI 10.1007/s00015-009-1306-4 Birkhäuser Verlag, Basel, 2009 Response of drainage systems to Neogene evolution of the Jura fold-thrust belt and Upper Rhine Graben PETER A. ZIEGLER* & MARIELLE FRAEFEL Key words: Neotectonics, Northern Switzerland, Upper Rhine Graben, Jura Mountains ABSTRACT The eastern Jura Mountains consist of the Jura fold-thrust belt and the late Pliocene to early Quaternary (2.9–1.7 Ma) Aare-Rhine and Doubs stage autochthonous Tabular Jura and Vesoul-Montbéliard Plateau. They are and 5) Quaternary (1.7–0 Ma) Alpine-Rhine and Doubs stage. drained by the river Rhine, which flows into the North Sea, and the river Development of the thin-skinned Jura fold-thrust belt controlled the first Doubs, which flows into the Mediterranean. The internal drainage systems three stages of this drainage system evolution, whilst the last two stages were of the Jura fold-thrust belt consist of rivers flowing in synclinal valleys that essentially governed by the subsidence of the Upper Rhine Graben, which are linked by river segments cutting orthogonally through anticlines. The lat- resumed during the late Pliocene. Late Pliocene and Quaternary deep incision ter appear to employ parts of the antecedent Jura Nagelfluh drainage system of the Aare-Rhine/Alpine-Rhine and its tributaries in the Jura Mountains and that had developed in response to Late Burdigalian uplift of the Vosges- Black Forest is mainly attributed to lowering of the erosional base level in the Back Forest Arch, prior to Late Miocene-Pliocene deformation of the Jura continuously subsiding Upper Rhine Graben. -
Quaternary Glaciation History of Northern Switzerland
Quaternary Science Journal GEOzOn SCiEnCE MEDiA Volume 60 / number 2–3 / 2011 / 282–305 / DOi 10.3285/eg.60.2-3.06 iSSn 0424-7116 E&G www.quaternary-science.net Quaternary glaciation history of northern switzerland Frank Preusser, Hans Rudolf Graf, Oskar keller, Edgar krayss, Christian Schlüchter Abstract: A revised glaciation history of the northern foreland of the Swiss Alps is presented by summarising field evidence and chronologi- cal data for different key sites and regions. The oldest Quaternary sediments of Switzerland are multiphase gravels intercalated by till and overbank deposits (‘Deckenschotter’). Important differences in the base level within the gravel deposits allows the distin- guishing of two complex units (‘Höhere Deckenschotter’, ‘Tiefere Deckenschotter’), separated by a period of substantial incision. Mammal remains place the older unit (‘Höhere Deckenschotter’) into zone MN 17 (2.6–1.8 Ma). Each of the complexes contains evidence for at least two, but probably up-to four, individual glaciations. In summary, up-to eight Early Pleistocene glaciations of the Swiss alpine foreland are proposed. The Early Pleistocene ‘Deckenschotter’ are separated from Middle Pleistocene deposition by a time of important erosion, likely related to tectonic movements and/or re-direction of the Alpine Rhine (Middle Pleistocene Reorganisation – MPR). The Middle-Late Pleistocene comprises four or five glaciations, named Möhlin, Habsburg, Hagenholz (uncertain, inadequately documented), Beringen, and Birrfeld after their key regions. The Möhlin Glaciation represents the most extensive glaciation of the Swiss alpine foreland while the Beringen Glaciation had a slightly lesser extent. The last glacial cycle (Birrfeld Glaciation) probably comprises three independent glacial advances dated to ca. -
The Flood Events of 1993/1994 and 1995 in the Rhine River Basin
Destructive Water: Water-Caused Natural Disasters, their Abatement and Control (Proceedings of the Conference held at Anaheim, California, June 1996). IAHS Publ. no. 239, 1997. 21 The flood events of 1993/1994 and 1995 in the Rhine River basin H. ENGEL Federal Institute of Hydrology, Kaiserin-Augusta-Anlagen 15-17, D-56068 Koblenz, Germany Abstract The causes of the Rhine floods of 1993/1994 and 1995 are described and compared with those of historic events. Information is given on damages and about consequences drawn at national and international levels. GENERAL BACKGROUND The flood events of 1993/1994 and 1995 and their underlying causes were media topics for weeks. Today, discussions continue as to why these floods were more frequent and their flood peaks higher. The main arguments are anthropogenic interference with nature. GEOGRAPHICAL-HYDROLOGICAL OVERVIEW In a comparison with the river basins of Amazonas or Mississippi-Missouri (7.2 x 106 km2 and 3.2 x 106 km2, respectively), the Rhine basin (Fig. 1) with its area of some 190 000 km2 appears less spectacular. However, the Rhine is one of the rivers with the highest streamflow in Europe and has little seasonal variation in discharge. Moreover, the River Rhine is one of the busiest waterways in the world. Nine states share the Rhine basin and about 50 million people live there. With about 100 000 km2, Germany has the greatest land area within the basin. The 1320 km-long course of the river is divided into six major stretches: (a) the Alpine Rhine and (b) the High Rhine, which are -
Council CNL(14)23 Annual Progress Report on Actions Taken
Agenda Item 6.1 For Information Council CNL(14)23 Annual Progress Report on Actions Taken Under Implementation Plans for the Calendar Year 2013 EU – Germany CNL(14)23 Annual Progress Report on Actions taken under Implementation Plans for the Calendar Year 2013 The primary purposes of the Annual Progress Reports are to provide details of: • any changes to the management regime for salmon and consequent changes to the Implementation Plan; • actions that have been taken under the Implementation Plan in the previous year; • significant changes to the status of stocks, and a report on catches; and • actions taken in accordance with the provisions of the Convention These reports will be reviewed by the Council. Please complete this form and return it to the Secretariat by 1 April 2014. The annual report 2013 is structured according to the catchments of the rivers Rhine, Ems, Weser and Elbe. Party: European Union Jurisdiction/Region: Germany 1: Changes to the Implementation Plan 1.1 Describe any proposed revisions to the Implementation Plan and, where appropriate, provide a revised plan. Item 3.3 - Provide an update on progress against actions relating to Aquaculture, Introductions and Transfers and Transgenics (section 4.8 of the Implementation Plan) - has been supplemented by a new measure (A2). 1.2 Describe any major new initiatives or achievements for salmon conservation and management that you wish to highlight. Rhine ICPR The 15th Conference of Rhine Ministers held on 28th October 2013 in Basel has agreed on the following points for the rebuilding of a self-sustainable salmon population in the Rhine system in its Communiqué of Ministers (www.iksr.org / International Cooperation / Conferences of Ministers): - Salmon stocking can be reduced step by step in parts of the River Sieg system in the lower reaches of the Rhine, even though such stocking measures on the long run remain absolutely essential in the upper reaches of the Rhine, in order to increase the number of returnees and to enhance the carefully starting natural reproduction. -
Der Rhein Eine Reise
Elke Heidenreich Fotografie Tom Krausz Der Rhein Eine Reise | Bilder | Geschichten Zu des Rheins gestreckten Hügeln, hochgesegneten Gebreiten, Auen, die den Fluss bespiegeln, weingeschmückten Landesweiten möget, mit Gedankenflügeln, ihr den treuen Freund begleiten. Johann Wolfgang von Goethe, 1814 Inhalt Alles fließt 13 Der Rhein und ich 17 Die Quellen 25 Der junge Rhein 39 Der Rhein wird erwachsen 51 Ein letztes Aufbäumen 61 Es wird ungemütlich 69 Basel 77 Die Schiffsreise beginnt 87 Der Rhein kriegt ein Korsett 95 Der Rhein als Zankapfel 99 Straßburg 103 Seele und Charakter 111 Das Rheingold 115 Speyer 123 Worms, Nibelungen, Luther – das ganze Programm 135 Erst noch richtig Dreck, dann aber wirklich Wein 145 Mainz und Wiesbaden 159 Die Burgen 165 Die Loreley 179 Die Germania und die Drosselgasse 187 Mein Köln 199 Drachenfels und Rolandseck 211 Das Ruhrgebiet 225 Der Niederrhein 235 Wieder zuhause oder: Peking 249 Anhang 251 Hamburg Bremen Nordsee Amsterdam Ijssel Rotterdam Rhein 13 Maas Nimwegen Lippe Xanten Holland Duisburg Ruhr Deutschland Alles fließt Düsseldorf Wupper Köln uf unserer Reise entlang des Rheins sahen und erlebten Belgien Sieg A wir vor allem eins: »Alles fließt.« Das hat der antike grie- Bonn chische Philosoph Heraklit gesagt, panta rhei, alles fließt. Rhea, Lahn die Fließende – sie war eine Titanin und die Gemahlin ihres Rhein Bruders Kronos, mit dem sie gemeinsam den ewigen Fluss der Koblenz Zeit und der Generationen bestimmte. Wiesbaden »Man kann nicht zweimal in denselben Fluss steigen«, auch Main das sagte Heraklit. Ja, man sieht auch nicht zweimal denselben Bingen Mainz Fluss. Weil alles fließt, verändert sich alles, und so sehen, so Luxem- Mosel sahen wir den Vater Rhein mit unseren Augen, der Fotograf Tom burg Worms Krausz und ich, die Erzählerin. -
Rare Earth Elements As Emerging Contaminants in the Rhine River, Germany and Its Tributaries
Rare earth elements as emerging contaminants in the Rhine River, Germany and its tributaries by Serkan Kulaksız A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geochemistry Approved, Thesis Committee _____________________________________ Prof. Dr. Michael Bau, Chair Jacobs University Bremen _____________________________________ Prof. Dr. Andrea Koschinsky Jacobs University Bremen _____________________________________ Dr. Dieter Garbe-Schönberg Universität Kiel Date of Defense: June 7th, 2012 _____________________________________ School of Engineering and Science TABLE OF CONTENTS CHAPTER I – INTRODUCTION 1 1. Outline 1 2. Research Goals 4 3. Geochemistry of the Rare Earth Elements 6 3.1 Controls on Rare Earth Elements in River Waters 6 3.2 Rare Earth Elements in Estuaries and Seawater 8 3.3 Anthropogenic Gadolinium 9 3.3.1 Controls on Anthropogenic Gadolinium 10 4. Demand for Rare Earth Elements 12 5 Rare Earth Element Toxicity 16 6. Study Area 17 7. References 19 Acknowledgements 28 CHAPTER II – SAMPLING AND METHODS 31 1. Sample Preparation 31 1.1 Pre‐concentration 32 2. Methods 34 2.1 HCO3 titration 34 2.2 Ion Chromatography 34 2.3 Inductively Coupled Plasma – Optical Emission Spectrometer 35 2.4 Inductively Coupled Plasma – Mass Spectrometer 35 2.4.1 Method reliability 36 3. References 41 CHAPTER III – RARE EARTH ELEMENTS IN THE RHINE RIVER, GERMANY: FIRST CASE OF ANTHROPOGENIC LANTHANUM AS A DISSOLVED MICROCONTAMINANT IN THE HYDROSPHERE 43 Abstract 44 1. Introduction 44 2. Sampling sites and Methods 46 2.1 Samples 46 2.2 Methods 46 2.3 Quantification of REE anomalies 47 3. Results and Discussion 48 4. -
Fische, Krebse Und Muscheln Im Kanton Aargau UM W E L T AA R G
Sondernummer 16 Januar 2004 UMWE L T AARGAU im KantonAargau Fische, KrebseundMuscheln Finanzdepartement Abteilung Wald Umwelt- Lokale Natur Raum Ressourcen Gesundheit Stoffe Abfall Luft Boden Wasser Allgemeines bildung Agenda 21 Landschaft Altlasten Lärm Gewässer IMPRESSUM Sondernummer aus der UMWELT AARGAU zum Thema Fische, Krebse und Muscheln im Kanton Aargau Autoren Roland Brogli Regierungsrat, Vorsteher Finanzdepartement Dr. Werner Dönni AquaPlus, Elber Hürlimann Niederberger, 6300 Zug Dr. Arno Stöckli Abteilung für Umwelt, Sektion Gewässer und Betriebsabwasser Dr. Thomas Stucki Abteilung Wald, Sektion Jagd und Fischerei Dr. Heinrich Vicentini Fisch- und Gewässerökologie 8055 Zürich Dr. Peter Voser Abteilung Wald, Sektion Jagd und Fischerei Fischfotos: Michel Roggo, Wildlife Photo- graphy, 1700 Fribourg Redaktion und Produktion Dr. Peter Voser Abteilung Wald, Sektion Jagd und Fischerei Telli-Hochhaus 5004 Aarau Tel. 062 835 28 50 Fax 062 835 28 59 e-mail: [email protected] Nachdruck Mit Quellenangabe erwünscht. Belegexemplare bitte an die Sektion Jagd und Fischerei schicken Papier Gedruckt auf hochwertigem Recyclingpapier. Titelbild: Revitalisierter Abschnitt des Holz- bachs, Villmergen, sowie Strömer, Edel- krebs, Fischzucht, Grosse Teichmuschel und Elektrische Kontrollabfischung Hier finden Sie Informationen über Jagd und Fischerei im Kanton Aargau www.ag.ch/jagd_fischerei www.ag.ch Hier finden Sie die Ausgaben von UMWELT AARGAU unter Baudeparte- ment, Umwelt, in elektronischer Form Umweltinformation Kanton Aargau Sondernummer 16 2004 Januar Vorwort AARGAU Im Aargau fliessen vier grosse Flüsse der Fische, Krebse und Muscheln ist nung im Bereich des Artenschutzes, der Schweiz zusammen. Unser Kanton eine Daueraufgabe. Wassertiere sind des qualitativen und quantitativen Ge- weist zudem ein Bachsystem mit einer auch wichtige Indikatoren für die Ge- wässerschutzes, des Wasserbaus und Länge von mehr als 1900 km offenen wässerqualität insgesamt. -
Extreme Flood Events on the River Aare 1
Extreme flood events on the River Aare 1 Key findings and results of the EXAR project Extreme flood events on the River Aare Key findings and results of the EXAR project 2 Extreme flood events on the River Aare Key findings and results of the EXAR project Contents 4 The EXAR project provides an important basis for decision-making in order to better protect the population and key infrastructure on the River Aare from flooding in the future. 7 By combining different models and simulation programs, the ex- perts were able to determine the peak discharges of the Aare over a period of almost 300,000 years. 10 Because of the much longer time horizon, the flood peaks on the Aare can be significantly higher than previously expected in the case of extremely rare events. For example, upstream of the point where it joins the Rhine, discharge values of over 7,000 cubic metres per second are possible, around 12 times the average discharge. 14 In the drainage basin, there are six key sites capable of influencing the flow behaviour of the Aare supra-regionally. Highly unlikely dam failures could flood large areas of the Seeland with several metres of water. 19 EXAR provides detailed hazard assessments for five locations, including the sites of the nuclear power plants on the Aare. They show that flooding is possible, especially in the case of structural failures and blockages by large wood. 28 The expert assessments, calculations and simulations of natural processes and technical structural failures are subject to uncertain- ties. Although only an approximation to real events is possible, EXAR will help to improve the assessment of flood hazard on the Aare. -
Internationally Coordinated Management Plan 2015 for the International River Basin District of the Rhine
Internationally Coordinated Management Plan 2015 for the International River Basin District of the Rhine (Part A = Overriding Part) December 2015 Imprint Joint report of The Republic of Italy, The Principality of Liechtenstein, The Federal Republic of Austria, The Federal Republic of Germany, The Republic of France, The Grand Duchy of Luxemburg, The Kingdom of Belgium, The Kingdom of the Netherlands With the cooperation of the Swiss Confederation Data sources Competent Authorities in the Rhine river basin district Coordination Rhine Coordination Committee in cooperation with the International Commission for the Protection of the Rhine (ICPR) Drafting of maps Federal Institute of Hydrology, Koblenz, Germany Publisher: International Commission for the Protection of the Rhine (ICPR) Kaiserin-Augusta-Anlagen 15, D 56068 Koblenz P.O. box 20 02 53, D 56002 Koblenz Telephone +49-(0)261-94252-0, Fax +49-(0)261-94252-52 Email: [email protected] www.iksr.org Translation: Karin Wehner ISBN 978-3-941994-72-0 © IKSR-CIPR-ICBR 2015 IKSR CIPR ICBR Bewirtschaftungsplan 2015 IFGE Rhein Contents Introduction .................................................................................. 6 1. General description .............................................................. 8 1.1 Surface water bodies in the IRBD Rhine ................................................. 11 1.2 Groundwater ...................................................................................... 12 2. Human activities and stresses .......................................... -
Analysis of Overdeepened Valleys Using the Digital Elevation Model of the Bedrock Surface of Northern Switzerland
Swiss J Geosci (2010) 103:375–384 DOI 10.1007/s00015-010-0043-z Analysis of overdeepened valleys using the digital elevation model of the bedrock surface of Northern Switzerland Peter Jordan Received: 6 March 2008 / Accepted: 7 June 2010 / Published online: 30 November 2010 Ó Swiss Geological Society 2010 Abstract Based on surface and borehole information, are divided into several sub-basins, indicating a multiphase together with pre-existing regional and local interpretations, evolution of the valleys. Some of the swells or barriers a 7,150 square kilometre Raster Digital Elevation Model separating the sub-basins coincide with known late LGM (DEM) of the bedrock surface of northern Switzerland was retreat stages. In the Suhre valley, an old fluvial valley floor constructed using a 25 m cell size. This model represents a with restricted overdeepened sections is documented. further important step in the understanding of Quaternary sediment distribution and is open to a broad field of appli- Keywords Quaternary cover Á Bedrock surface Á cation and analysis, including hydrogeological, geotech- Overdeepened valleys Á DEM Á GIS nical and geophysical studies as well as research in the field of Pleistocene landscape evolution. An analysis of the overdeepened valleys in the whole model area and, more Introduction specifically in the Reuss area, shows that, in most cases, overdeepening is restricted to the areas covered by the Last Motivation Glaciation Maximum (LGM). However, at various locations relatively narrow overdeepened valleys outreach the tongue A well established knowledge of the bedrock surface basins and the LGM ice shield limits. Therefore, an earlier geometry and the thickness and spatial distribution of and further-reaching glacial event has probably contributed unconsolidated rock is of fundamental interest for a wide significantly to the overdeepening of these valleys. -
SEBA Gene Conservation Units (EUFORGEN) Proposal for Selction of Candidate Gene Conservation Units (GCU) for Scattered Broadleav
SEBA Gene conservation units (EUFORGEN) page 1 / 2 Proposal for selction of candidate gene conservation units (GCU) for scattered broadleaves in Switzerland attrib Record ID Entry Latin species name Bewertu Notes on qualification Type of Canton Region Municipality Forest Provenance Notes on location Notes on Type of ex situ National Notes on juristic Longitude Latitude Digita Altitude Main river River last levelTotal area Total area Year(s) of Number Average Genotype Average number Average Share in Type of marker(s) Notes on ute Numb ng pot. population Region responsable Conservation Registration aspects X coordinate Y coordinate lizatio (m) tributary stand (ha) region establish of number s of trees (nr/ha) number of total basal genetic er GCU 1 structure partners Unit Number n of (ha) ment genotype of ramets originate trees (nr/ha) area (%) information Phase in situ GIS s per from ## ID_rec ID_id ID_nr ID_spec_name QU_pro QU_note LO_pop_typ LO_kt LO_reg LO_muni LO_for LO_prov LO_note LO_partner_not JU_exSitu_type JU_nat_nr JU_note SI_lon_X SI_lon_Y SI_di SI_alt SI_river_mai SI_river_lastl ST_stand ST_regio ST_date ST_geno ST_rame ST_regio ST_spec_dens ST_spec_d ST_spec_s GE_markers_type GE_note 603 IN-ACEPL-CHE-03 3 Acer platanoides 1 high regional density, population size C region GL Nordalpen Region Glarner Unterland (5 0 Swiss Northern 0 0 0 0 0 728000 219500 (Y) 420- Rhein Linth, Limmat 0 78 km2 0000 10'000 >2 >1 - 0 and quality (SEBA1) due to the Gemeinden): Bilten, Niederunren, Alps 1000 influence of Foehn (warm and dry wind Oberurnen, -
Formation and Evolution of the Lower Terrace of the Rhine River in the Area of Basel
1661-8726/09/020307-15 Swiss J. Geosci. 102 (2009) 307–321 DOI 10.1007/s00015-009-1325-1 Birkhäuser Verlag, Basel, 2009 Formation and evolution of the Lower Terrace of the Rhine River in the area of Basel STÉPHANE KOCK 1, PETER HUGGENBERGER 2, FRANK PREUSSER 3 PHILIPPE RENTZEL 4 & ANDREAS WETZEL 2 Key words: River Rhine, fluvial deposits, fluvial terraces, Pleistocene, optical dating, river incision ABSTRACT The response of fluvial systems to tectonic activity and climate change during deposited during two periods (30–15 ka and 13–11 ka), which correlate with the Late Pleistocene influenced sedimentary processes and hence the condi- two cold climatic phases, representing the Last Glaciation of the Alps and the tions of river terraces formation. The northern Alpine foreland is well adapted Younger Dryas. These ages underline that main incision of the Lower Ter- for such studies due to the high sediment input and the variety of depositional race braidplain in the area of Basel is restricted to post Younger Dryas times, environments. This study focuses on sediments of a part of the Rhine River in as sediments of that age (13–11 ka) are found atop the highest levels. From the area of Basel, at the Border between Switzerland, Germany and France. then on, a flight of cut-terraces were formed with minor re-accumulation due A detailed evolution of the Lower Terrace is inferred from sedimentological, to Holocene flood events. These findings demonstrate that the surface of a geomorphologic and pedological observations as well as historical documents, terrace does not always represent the age of sediment aggradation, and this and calibrated using different dating methods (optically stimulated lumines- should be remembered when using terraces to reconstruct the tectonic history cence, uranium series disequilibrium, radiocarbon).