The Rhine River
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Johannes Fröhlinger: „The Return of the Deutschland Tour on Roads I Know – It Could Hardly Be Better”
Johannes Fröhlinger: „The return of the Deutschland Tour on roads I know – it could hardly be better” Johannes Fröhlinger is one of the most experienced German pros in the peloton. The 32-year-old with Team Sunweb has just ended his 11th year as a pro cyclist and extended his contract through 2019. The native of Gerolstein is a cornerstone of his team as its road captain. With his cycling roots in the Eifel, Fröhlinger feels especially good on the challenging rolling terrain. Trier is your second home: You grew up barely 500 kilometers away from Trier. Your family lives in Trier and you spend a lot of time in the region. Now the Deutschland Tour is coming to Trier in the first year of its new life. Your first reaction? “That was fantastic news. My first thought was immediately: I have to be there. On the same day I told my team of my wish to include that in the season planning. Hopefully it will work out. Race days for us German riders on our native soil have been drastically reduced over the last decade. At the last Deutschland Tour in 2008, I was at the start. Starting again in the race and then riding on familiar roads, that could hardly be better for me personally.” You know the terrain of the Moselle valley as well as the distinctive climbs in the Eifel and Hunsrück like you know the back of your hand. What can your colleagues in the peloton and especially the fans of the Deutschland Tour look forward to? “The region offers an incredible variety of roads. -
Castles Along the Rhine & Moselle, 5 Days
CASTLES ALONG THE RHINE & MOSELLE Private Escorted Tour April 1 - October 20, 2021 - Departure any day 5 days / 4 nights: 1 night in Frankfurt, Liebenstein Castle, Ehrenburg Castle, Trier, Heidelberg Accommodation Meals Tours Transportation Transfer Not included 4* hotels in each city Breakfast daily in Tours throughout as Car or minival during entire tour. Arrival and City taxes in hotels each city. per itinerary. departure transfers to be paid on site English speaking guide during Admissions to entire tour. castles included Wine tasting Rates 2021 US$ per Person Day by Day Itinerary Day 1: The tour begins in Frankfurt and follows the Rhine to Rudesheim. Enjoy a sightseeing Hotel Class & Dates Twin Single tour of Rudesheim’s old historic center. Next we embark on a cruise and sail along the Rhine River, the Lorelei Valley. Disembark at Kamp-Bornhofen and ascend to Liebenstein 4* Hotel Castle, which towers high above the village and offers a beautiful view of the Rhine. April 1 - October 20 $3,569 $3,924 Accommodation in this 13th century castle. The rooms have been beautifully restored in medieval style. *Based on minimum 2 people traveling Day 2: After breakfast, travel to the ancient Roman city of Koblenz, one of the oldest cities in together. Germany. Then continue to the “Deutsches Eck” or German Corner, where the Moselle meets the Rhine. Cross the river in a panoramic cable car for a spectacular view. Visit the Liebenstein ← Frankfurt Ehrenbreitstein Fort, the second largest fort in Europe. Then continue along the Moselle ← river and the Ehrbachtal Valley. Ascend to Ehrenburg Castle for the Night. -
World War Ii in Europe
“THEIR SACRIFICE, OUR FREEDOM” WORLD WAR II IN EUROPE War in Europe Lesson Plans Recommended Level: High School Time Required: 5 Days Introduction This unit covers the European Theater. Preceding these lessons, the students have covered the rise of dictators and identified Hitler, Mussolini and Stalin. These lessons begin with Hitler’s seizure of territories and end with V-E Day in Europe, and covers five days. Part 1 of the video gives an excellent introduction or review of the steps leading to World War II. It is used as a review of foreign policy in the 1930’s through the Allied invasion of Africa and Sicily. Part 2 covers from D-Day to V-E Day and may also be used as an introduction or review. It is used as an introduction of U.S. troops fighting in Europe. Along with excellent video, eyewitness accounts and commentaries are presented by our veterans giving the added value of thoughts and details on what it was like to be there at that time and place. Materials • Video – “Their Sacrifice, Our Freedom: World War II in Europe” • Internet resources • Map of European Theater • Art supplies and poster board Unit Goals After completing this unit, students will be able to: 1. Label and identify Hitler’s seizure of territories in 1930’s 2. Identify participants in the Munich Conference and understand the effects of appeasement. 3. Describe U.S. neutrality efforts in the 1930’s. 4. Identify Churchill and Roosevelt and the goals of the Atlantic Charter. 5. List effects of the fall of France on U.S. -
EMS INFORMATION BULLETIN Nr 144
16/07/2021 EMSR517 – Flood in Western Germany EMSR518 – Flood in Belgium EMSR519 – Flood in Switzerland EMSR520 – Flood in The Netherlands EMS INFORMATION BULLETIN Nr 144 THE COPERNICUS EMERGENCY MANAGEMENT SERVICE The Copernicus Emergency Management Service forecasts, notifies, and monitors devastating floods in Germany, Netherlands, Belgium and Switzerland CEMS flood forecasting and notifying in Germany On 9 and 10 July, flood forecasts by the European Flood Awareness System (EFAS) of the Copernicus Emergency Management Service indicated a high probability of flooding for the Rhine River basin, affecting Switzerland and Germany. Subsequent forecasts also indicated a high risk of flooding for the Meuse River basin, affecting Belgium. The magnitude of the floods forecasted for the Rhine River basin increased significantly in this period. The first EFAS notifications were sent to the relevant national authorities starting on 10 July and, with the continuously updated forecasts, more than 25 notifications were sent for specific regions of the Rhine and Meuse River basins in the following days until 14 July. Figure: EFAS flood forecast from 12.07.2021 00:00 UTC Providing early and current maps of flooded areas On 13 July, the CEMS Rapid Mapping component was activated to map the ongoing floods in parts of Western Germany (EMSR517 Mapping Website , EMSR517 Activation Viewer). As a flood peak was foreseen on 16 July for segments of other rivers, CEMS preemptively acquired satellite images of the vulnerable area through Pre-Tasking on 14 July. These early images informed ensuing activations by the CEMS Rapid Mapping component based on the EFAS forecasts for areas in Belgium, Netherlands, Germany, Switzerland and France. -
River Cruises Cover
2 2018 EUROPEAN RIVER CRUISE COLLECTION The relaxing 0 way to cruise r w The Dutch and Belgian Waterways, We are also voyaging to the Channel The Main, Rhine & I Moselle Rivers " " " " " " " " " " " " " " " " " Welcome to the 2018 Hebridean River Cruise Collection Relaxing, informative, sociable and stimulating – just some of the words which can be used to describe a Hebridean river cruise in Europe. A cruise holiday with Hebridean is like no other, with meticulous attention to the finest details and an elegant charm that is simply unique. Travelling effortlessly to some of Europe’s finest towns and cities, every one of our itineraries will allow you to uncover the soul and make up of each destination. In the style of a 1930’s club, Royal Crown is elegant and understated, with its spacious panoramic lounge containing comfortable sofas and armchairs, and a single sitting restaurant which serves a mix of British and continental cuisine. So put your feet up and choose your Hebridean river cruise from this enticing selection and then relax, safe in the knowledge that Hebridean Island Cruises will be looking after you on a journey which is going to transport you back in time to the Golden Age of cruising. We look forward to seeing you in 2018. Ken Charleson Managing Director Contents The Hebridean Difference 2-3 The Hebridean Connection 4 The Faces of Hebridean 5 Life On Board with Hebridean 6-7 Dining and Cuisine with a Hebridean Influence 8-9 Going Ashore with Hebridean 10-11 Hebridean’s Renowned Guest Speakers 12-13 Itineraries 14-21 Grand River Voyages of Europe 22-23 Good Connections 24 Royal Crown Deck Plans 25 Royal Crown Cabins 26-27 General Information 28-29 Conditions of Business 30-34 Booking Form 35 Map of European Rivers 38 Moselle Valley The Hebridean Difference Genuinely fully-inclusive cruises Hebridean river cruises are fully-inclusive; not an empty promise but a Hebridean pledge to ensure that you have a carefree holiday both on board and ashore. -
International Cooperation on the River Rhine
International cooperation on the river Rhine Maarten Hofstra Unesco‐IHE/Water Governance Centre NL The Rhine river basin The Rhine = 3rd biggest European river 200.000 km² Outline •The Rhine: some chracteristics •The Netherlands as a downstream country •Early cooperation in the Rhine basin •Water pollution •Difficulties and conflicts •Flood protection •Ecological restauration •What makes cooperation work Cooperation in the Rhine basin Dutch border with: ‐Switzerland ‐Germany ‐France ‐Luxembourg ‐Netherlands The Rhine river basin Inhabitants Coblence – CIPR 58 Mio. Drinking water for 20 million people Main stream 1233 km Navigable 825 km from Basel/ Rheinfelden – Rotterdam RIZA RIZA Some hydrological characteristics of the Rhine Mean discharge Lobith: 2.200 m3/s Minimum in January Lowest discharge: 620 m3/s (1947, November) Extreme flood 1926, January: 12.600 m3/s Flood 1995, January: ca 12.000 m3/s Height difference Rotterdam‐Basel: 260 m The Netherlands as a downstream country International cooperation: Shipping on the River Rhine 1815: Congres of Vienna ‐ Free shipping ‐ Central committee for the River Rhine 1831 Act of Mainz 1868 Act of Mannheim 1963 Convention of Strassbourg International cooperation on prevention of pollution After World War 2: Pollution of the river leading to poor water quality International Commission for the Protection of the Rhine (ICPR) Switzerland, France, Germany, Luxemburg, Netherlands, European Community Established 1950 Confirmed 1963 Rhine action programme 1987 New Rhine Treaty 1‐1‐2003: Rhine 2020 ICPR: -
The Waffen-SS in Allied Hands Volume Two
The Waffen-SS in Allied Hands Volume Two The Waffen-SS in Allied Hands Volume Two: Personal Accounts from Hitler’s Elite Soldiers By Terry Goldsworthy The Waffen-SS in Allied Hands Volume Two: Personal Accounts from Hitler’s Elite Soldiers By Terry Goldsworthy This book first published 2018 Cambridge Scholars Publishing Lady Stephenson Library, Newcastle upon Tyne, NE6 2PA, UK British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library Copyright © 2018 by Terry Goldsworthy All rights for this book reserved. No part of this book may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior permission of the copyright owner. ISBN (10): 1-5275-0858-7 ISBN (13): 978-1-5275-0858-3 All photographs courtesy of the US National Archives (NARA), Bundesarchiv and the Imperial War Museum. Cover photo – An SS-Panzergrenadier advances during the Ardennes Offensive, 1944. (German military photo, captured by U.S. military photo no. HD-SN-99-02729; NARA file no. 111-SC-197561). For Mandy, Hayley and Liam. CONTENTS Preface ...................................................................................................... xiii VOLUME ONE Introduction ................................................................................................. 1 The rationale for the study of the Waffen-SS ........................................ 1 Sources of information for this book .................................................... -
Collected Sequence of the Rhine and Nahe Terraces at Bingen
Results of recent Terrace Research in the Middle Rhine Valley Fig. 1.: Downstream Correlation Diagram of River-Terraces in the Lower Nahe & Upper Middle Rhine Valley. Fig. 2 & Tab. 1: Collected Sequence of the Rhine and Nahe Terraces at Bingen-Trechtingshausen Downstream Correlation Diagram of River Terraces in the Lower Nahe & Upper Middle Rhine Valley correlated with Pollen Records and Marine Isotope Stages. Collected Terrace- MIS Elevation of Assumed Difference Incision at Lower Nahe Valley Upper Middle Rhine Valley Lower Lahn Valley Age Palaeomagnetic Marine Isotope Stages (MIS) Mean Temp.°C Sequence Base NW-European Age labels Terr. Base Mean in Age Collected 18 Nahe / Rhein LowerGÖRG Nahe(1984) Valley Upper PMiddleREUSS, BURGER & SRhineIEGLER (2015) Valley Lower ALahnNDRES & SEWERING Valley(1983); (Ma) Record (Ma) (δ OOcean‰) in July (Pollen) (m a.s.l.) Stages (Ma) Nahe / Nahe/Rhine Age Nahe/Rhine Sequence 5 4 0° 10° 20° SEWERING (1993) tRh 11.2 78 Rhine (No.) (m a.s.l.) (Ma) (Ma) Nahe/Rhine GÖRG (1984) PREUSS, BURGER & SIEGLER (2015) ANDRES & SEWERING (1983); 2 tRh 11.1 81 Weichselian (mm/a) 4 tRh 10 84 SEWERING (1993) 6 Eemian tNa 12. 1 75 0,00 0,01 0,30 tRh 9. 90 Saalian tNa 11.2 1-2 78 0,01 0,01 0,30 8 tRh 8.2 94 tNa 11.1 2 81 0,02 0,04 0,08 10 tRh 8.1 101 Holsteinian tNa 10. 4 84 0,06 0,08 0,08 12 tRh 7.4 108 Elsterian tRh 7.3 114 tNa 9. 6 90 0,14 0,11 0,04 Elevation m a.s.l. -
Olympiatauben Mit Züchter 404.Xlsx
regionareiseVver z-nr ReiseVereinigungen_na S_GSMT_name pr pkt t-nat t-ver t-jahr t-nr t-gescRegionalverbaende_name 404 10 5 6 Gießen Nord Göhler, E.+Th. 3 22640 6680 17 0097 Lahn-Sieg-Dill 404 10 5 6 Gießen Nord Göhler, E.+Th. 3 20314 6680 17 0181 Lahn-Sieg-Dill 404 10 6 11 Gießen Nord Kostka ,Bernhard 3 27048 6914 17 0103 Lahn-Sieg-Dill 404 10 6 11 Gießen Nord Kostka ,Bernhard 3 26817 6914 17 0101 Lahn-Sieg-Dill 404 10 6 11 Gießen Nord Kostka ,Bernhard 3 25402 6914 17 0157 Lahn-Sieg-Dill 404 10 6 11 Gießen Nord Kostka ,Bernhard 3 19550 6914 17 0134 Lahn-Sieg-Dill 404 10 12 3 Gießen Nord Schwarz, Klaus 3 25485 3725 17 0278 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 28582 4695 17 1313 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 28154 4695 17 1326 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 27608 6680 17 0388 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 27589 4695 17 1301 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 27580 4695 17 1374 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 26983 4695 17 1333 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 26748 4695 17 1025 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 26576 6680 17 0333 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 25652 4695 17 1316 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 25494 4695 17 1343 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 24906 4695 17 1321 Lahn-Sieg-Dill 404 10 16 1 Gießen Nord Jochum Benjamin 3 24721 0986 17 0116 Lahn-Sieg-Dill 404 -
Marble from the Lahn
Marble from the Lahn A historical project on the quarrying of stone Quarrying is also part of mining. Stones, chalk, sand and gravel may at first glance seem less valuable, and quarries less interesting. However, these materials were and still are an essential component of our civilization. There would be no flour without millstones, no pottery without clay, no castles without stones, and no modern roads without road metal. This is why the department of mining history also deals with this important industry. Following on from the work of Christoph Bartels (slate villages) and Meinrad Pohl (millstones, tuff and trass from the volcanic eastern Eifel region), the plan is to investigate a further example from the industry within the framework of a dissertation project. This time the focus is on a type of stone which was used for building and decoration, the so-called “Nassau marble” or “Lahn marble”. From a geologist’s point of view this is a cuttable, polishable limestone, formed about 380 million years ago from a tropical reef. The deposits are part of the Rhenish Massif (Rheinisches Schiefergebirge) and extend over a strip approx. 60 km long on both sides of the Lahn. “Lahn marble” was quarried and processed from the 16th century (if not earlier) until the 1970s. Evidence of a highly developed “Lahn marble” industry can be found in a multitude of churches and palaces, public and private buildings, town squares and facades. The spectrum ranges from the mighty tombstones in the Mainz cathedral to the splendid Baroque staircase of the Würzburg Residenz and the sumptuous decoration of some of Wiesbaden’s villas and hotels. -
Middle and Upper Pleistocene Fluvial Evolution of the Meurthe and Moselle Valleys in the Paris Basin and the Rhenish Massif ⅲ
Quaternaire, 16, (3), 2005, p. 201-215 MIDDLE AND UPPER PLEISTOCENE FLUVIAL EVOLUTION OF THE MEURTHE AND MOSELLE VALLEYS IN THE PARIS BASIN AND THE RHENISH MASSIF Ⅲ Stéphane CORDIER*, Manfred FRECHEN**, Dominique HARMAND*** and Monique BEINER**** ABSTRACT The terrace systems of the River Meurthe (Me), and the River Moselle (M) downstream from the present Moselle-Meurthe confluence are composed of eight stepped alluvial terraces (Me8-M8 to Me1-M1), situated at less than 90 m above the modern floodplain Me0-M0. Morphological, mineralogical and petrographical studies evidence that the oldest five terraces (Me8-M8 to Me4-M4) were formed by the “Palaeo-Meurthe”, while the Upper Moselle flowed towards the Meuse valley. Downstream from the confluence, the three youngest alluvial terraces (Me3-M3 to Me1-M1) contain crystalline sediments from the Upper Moselle basin; they have been formed since the Upper Moselle capture, dated about 250-270 ka before present. IRSL and radiocarbon datings provide independent absolute age control for these post-capture terraces, which respectively correlate with the end of the Saalian (Me3-M3) and the Weichselian (Me2-M2 and Me1-M1). The constant relative height of the terraces between France, Luxemburg and Germany gives evidences that there was no differenciated tec- tonic movements along the valley since at least the capture. A cyclic evolution scheme for the formation of the terraces is presented. The main gravel sedimentation occurred during cold periods (pleniglacial and late glacial phases), with a minor erosive period at the beginning of late glacial periods. Major incision occurs at the warm-to-cold transition. Key-words: Meurthe and Moselle valleys, alluvial terraces, alluvial sequences, IRSL datings, heavy minerals, Upper and Middle Pleistocene. -
Results of Recent Terrace Research in the Middle Rhine Valley
Results of Recent Terrace Research in the Middle Rhine Valley A lot of questions concerning the sequence of terraces in the Middle Rhine Valley as well as their genetic dependence on geological, geomorphological and climatic processes remain insufficiently answered. So far, three issues in particular have required further examination: -The phenomenon of the horizontal consistency ("Horizontalkonstanz") of the main terraces cannot be explained coherently. -Studies from adjoining valleys of the Nahe and Lahn rivers, have identified larger numbers of terraces within the upper terrace group (ANDRES & SEWERING 1983; GÖRG 1984; SEWERING 1993). -Unsolved problems concerning the positions and ages of the older (äHT) and younger (jHT) main terraces. Given these problems, we started re-mapping the terraces of the Upper Middle Rhine Valley by conducting numerous borehole drillings. Our results, which we combined with the findings presented in previous studies, demonstrate the existence of a total of 28 alluvial sediment bodies in the valleys of the rivers Nahe and Rhine between Bad Kreuznach, Bingen and Boppard (GÖRG 1984; PREUSS 1983; ANDRES & PREUSS 1983; PREUSS, BURGER & SIEGLER 2015). For the Lower Middle Rhine Valley we mainly used the publications of BIBUS (1980), HOSELMANN (1994) AND BOENIGK & HOSELMANN (2003). For the Moselle and Lahn CORDIER et al. (2006, 2014) and SEWERING (1993) provided helpful insights. Further information was obtained from FUCHS et al. (1983), BIBUS & SEMMEL (1977)AND SEMMEL (2009). .The Downstream Correlation Diagram (DCD) of river terraces in the Lower Nahe and Upper Middle Rhine Valley (see Fig. 1) contains 28 alluvial sediment bodies. They were identified at key locations with more than 720 borehole drillings, many of them in clusters, which in most cases reached the rockbed of the river terraces.