ICOLS-2011 Information
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Ergebnisse Der Detailstrukturkartierung
Oberirdische Gewässer Band 38 Niedersächsischer Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz Detailstrukturkartierung ausgewählter Fließgewässer in Niedersachsen und Bremen Ergebnisse 2010 bis 2014 Oberirdische Gewässer Band 38 Niedersächsischer Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz Detailstrukturkartierung ausgewählter Fließgewässer in Niedersachsen und Bremen Ergebnisse 2010 bis 2014 Herausgeber: Niedersächsischer Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz (NLWKN) Direktion Am Sportplatz 23 26506 Norden Bearbeitung: Dipl.-Biol. Kuhn, Ulrike – Bremen i. A. des NLWKN Begleitende Arbeitsgruppe Abée, Eva – NLWKN – GB III Meppen; Bellack, Eva – NLWKN – GB III Hannover-Hildesheim; Baumgärtner, Manfred – NLWKN – GB III Stade; Fricke, Dr. Diethard – NLWKN – GB III Lüneburg; Pinz, Dr. Katharina – NLWKN – GB III Lüneburg; Datentechnik und GIS Betreuung Kuckluck, Bettina – NLWKN – GB III Lüneburg; Weber, Dirk – NLWKN – GB III Hannover-Hildesheim; Titelbilder: Links oben – Soeste (Kiesgeprägter Tieflandbach), Ems Links unten – Mühlenfleet (Küstenmarschgewässer), Weser Rechts – Holzminde (Mittelgebirgsbach), Weser 1. Auflage 2015: 1000 Exemplare Stand Dezember 2015 Schutzgebühr: 5,00 € zzgl. Versandkosten Bezug: Niedersächsischer Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz (NLWKN) Veröffentlichungen Göttinger Chaussee 76 30453 Hannover Online verfügbar unter: www.nlwkn.niedersachsen.de (→ Service → Veröffentlichungen/Webshop) Inhalt 1 Einführung und Zielsetzung ................................................................................................................................ -
Guest Information English
English Guest information dfgdfgd Location and how to get here Bus The city is well-connected and situated in the tri-city Central bus station (ZOB), Bahnhofstraße, area Bremen, Hanover and Hamburg; the well-develo- station forecourt ped infrastructure allows a comfortable arrival from City bus all directions. Allerbus, Verden-Walsroder Eisenbahn (VWE), Tel. (0)4231 92270, www.allerbus.de, www.vwe-verden.de VBN-PLUS shared taxi Tel. (0)4231 68 888 Regional bus Hamburg Verkehrsverbund Bremen/Niedersachsen (VBN), A27 Tel. (0)421 596059, www.vbn.de A29 Taxi A28 Bremen A1 Taxi Böschen Tel. (0)4231 66160 or 69001 Taxi Kahrs Tel. (0)4231 82906 A7 Taxi Köhler Tel. (0)4231 5500 Taxi Sieling Tel. (0)4231 930000 Verden A27 Car parks The city of Verden has a car park routing system taking Weser Aller A1 you safely and comfortably into the city centre. Car park P 1, multi-storey car parks P 3 and ‘Nordertor‘ are recommended if you want to visit the shopping street Hannover and the historic old town. Caravan park Conrad-Wode-Straße 15 spaces up to a length of max. 12 m GPS coordinates: E = 9° 13‘ 42“ N = 52° 55‘ 32“ Marina of the Verden motor boat club International telephone code for Germany: 0049 Höltenwerder 2 Connections Car rental Motorway A27 (Hanover-Bremen) Hertz Federal road B215 (Rotenburg/Wümme-Minden) Marie-Curie-Straße 4, Tel. (0)4231 965015 Airports Access to the attractions and sights of the city Bremen 40 km Before you reach the city centre, the tourist information Hanover 80 km system and the parking information system will direct Hamburg 125 km you to the attractions, sights, hotels and car parks. -
How Britain Unified Germany: Geography and the Rise of Prussia
— Early draft. Please do not quote, cite, or redistribute without written permission of the authors. — How Britain Unified Germany: Geography and the Rise of Prussia After 1815∗ Thilo R. Huningy and Nikolaus Wolfz Abstract We analyze the formation oft he German Zollverein as an example how geography can shape institutional change. We show how the redrawing of the European map at the Congress of Vienna—notably Prussia’s control over the Rhineland and Westphalia—affected the incentives for policymakers to cooperate. The new borders were not endogenous. They were at odds with the strategy of Prussia, but followed from Britain’s intervention at Vienna regarding the Polish-Saxon question. For many small German states, the resulting borders changed the trade-off between the benefits from cooperation with Prussia and the costs of losing political control. Based on GIS data on Central Europe for 1818–1854 we estimate a simple model of the incentives to join an existing customs union. The model can explain the sequence of states joining the Prussian Zollverein extremely well. Moreover we run a counterfactual exercise: if Prussia would have succeeded with her strategy to gain the entire Kingdom of Saxony instead of the western provinces, the Zollverein would not have formed. We conclude that geography can shape institutional change. To put it different, as collateral damage to her intervention at Vienna,”’Britain unified Germany”’. JEL Codes: C31, F13, N73 ∗We would like to thank Robert C. Allen, Nicholas Crafts, Theresa Gutberlet, Theocharis N. Grigoriadis, Ulas Karakoc, Daniel Kreßner, Stelios Michalopoulos, Klaus Desmet, Florian Ploeckl, Kevin H. -
Naturräumlich-Ökologische Analyse Der Flechtenflora Von Deutschland
624 Herzogia 28 (2) Teil 2, 2015: 624 – 653 Naturräumlich-ökologische Analyse der Flechtenflora von Deutschland Ulf Schiefelbein*, Florian Jansen, Birgit Litterski & Volkmar Wirth Zusammenfassung: Schiefelbein, U., Jansen, F., Litterski, B. & Wirth, V. 2015. Naturräumlich-ökologische Analyse der Flechtenflora von Deutschland. – Herzogia 28: 624 – 653. Die Flechtenflora von Deutschland wird auf der Grundlage der Angaben von Wirth et al. (2013; Die Flechten Deutschlands) analysiert, wobei Naturräume die geografische Basis für die Analysen bilden. Bewertet werden Artendiversität, Exklusivität des Arteninventars, substratspezifische Eigenschaften (Substratbindung, pH-Werte und Nährstoffgehalt/Eutrophierung der besiedelten Substrate) und klimatische Faktoren (Licht, Luftfeuchte). Die artenreichs- ten Naturräume sind nach den Bayerischen Alpen, dem Schwarzwald und Odenwald-Spessart die ebenfalls sehr nieder- schlagsreichen Naturräume Eifel, Weserbergland, Harz, Fränkische Alb, Sauerland und Bayerisch-Böhmischer Wald. Die artenärmsten Landschaften liegen überwiegend im südlichen Teil des Nordostdeutschen Tieflandes. Die Exklusivität des Arteninventars eines Naturraumes wird als Anzahl der Arten, die in Deutschland nach 1950 nur in einem bis zwei Naturräumen nachgewiesen wurden, definiert. In der gesamten Bundesrepublik sind es 638 Arten, davon kommen die meisten in den Bayerischen Alpen, im Schwarzwald, Bayerischen Wald, Odenwald-Spessart und in der Schwäbischen Alb vor. Im gesamten Deutschland überwiegen die Gesteinsbewohner (47,6 % des Gesamtarteninventars), -
Lower Saxony and Northern Hesse, NW Germany)
Quaternary Science Journal GEOZON SCIENCE MEDIA Volume 60 / Number 1 / 2011 / 27–46 / DOI 10.3285/eg.60.1.02 ISSN 0424-7116 E&G www.quaternary-science.net Spatial analysis of loess and loess-like sediments in the Weser- Aller catchment (Lower Saxony and Northern Hesse, NW Germany) Bianca Wagner Abstract: A spatial compilation and visualization of loess parameters was carried out for the Pleistocene loess and loess-like sediments in the Weser-Aller catchment (southern Lower Saxony and northern Hesse, NW Germany), one of the loess regions of Central Europe. As far as available, data about main loess characteristics like thickness, granulometry and stratigraphy were combined for the first time with spatial information extracted from maps. Data storage and analysis in a geographical information system (GIS) permitted creation of large-scale thematic loess maps. The loess thickness map displays an increase of the thickness in valleys and basins and from north to south. The granulometry map presents main granulometrical facies types of the loess cover. Furthermore, several loess locations with unusual thickness were identified and their special geological and geomorphological conditions are discussed. In summary, the loessic sediments in the northern part of the study area are of Upper Weichselian age, whereas in the south- ern upland regions incomplete or detailed Weichselian loess sequences were identified. In conclusion, highly detailed maps of regional loess-property patterns can be created even if only heterogeneous historically published data are taken into account. [Räumliche Analyse von Lössen und löss-ähnlichen Sedimenten im Weser-Aller-Einzugsgebiet (Süd-Niedersachsen und Nord-Hessen, NW-Deutschland)] Kurzfassung: Eine räumliche Kompilation und Darstellung von Löss-Parametern wurde für die pleistozänen Lösse und löss-ähnlichen Sedi- mente im Weser-Aller-Einzugsgebiet (Süd-Niedersachsen und Nordhessen, NW-Deutschland), einer der Lössregionen in Mit- teleuropa, durchgeführt. -
EGU2009-2158-3, 2009 EGU General Assembly 2009 © Author(S) 2009
Geophysical Research Abstracts, Vol. 11, EGU2009-2158-3, 2009 EGU General Assembly 2009 © Author(s) 2009 Catastophic flooding origin of channel systems and streamlined hills in the Münsterland Embayment, NW Germany J. Meinsen (0,1), N. Landmeyer (0), A. Weitkamp (0), and J. Winsemann (0) (0) Leibniz Universität Hannover, Institut für Geologie, Callinstrasse 30, 30167 Hannover, Germany , (1) [email protected] During the Early Saalian glaciation numerous glacial lakes formed at the southern margin of the Scandinavian Ice Sheet. Ice-damming of the Upper Weser Valley led to the formation of glacial Lake Weser. During the maximum lake-level highstand of approximately 200 m a.s.l. the lake covered an area of at least 1700 km2 with more than 100 km3 water stored in the lake basin. The spillway system was through a series of valleys in the Teutoburger Wald Mountain over an altitude range of 40-215 m a.s.l., through which the proglacial lake drained southwestward into the Münsterland Embayment. The lake drained catastrophically into the Münsterland Embayment as the western ice dam failed, releasing up to 70 km3 of water within a few days. The drainage routes are characterized by the occurrence of streamlined hills, oversteepened channels and trench-like incised valleys, cut into bed rock and older Quaternary deposits. Streamlined hills occur in front of two lake overspills and are 6-12 m high, 600-3000 m long, and 300-1000 m wide, forming fan-shaped arrays of hills, covering an area of approximately 200 or 300 km2, respectively. Most of these hills trend NE-SW and have quadrilateral, elongate to lemniscate shapes with a common width to length ratio between 1:2 to 1:4. -
Travel Planner 2017
Travel Planner 2017 FÜRSTENBERG Castle Complex For groups and travel operators NEW OPENING Museum with Visitors’ Workshop OPENING MARCH 2017 Museum Visitors’ Workshop Workshops Manufactory Store Castle Café and Restaurant FÜRSTENBERG Castle complex combining the traditional and the modern The charm of the FÜRSTENBERG castle complex lies in the combination of yesterday and today. Here, the historic Weser Renaissance castle; there, the modern manufactory, setting new standards in porcelain production with its premium collections. The castle complex offers an extraordi- nary experience to culture enthusiasts and weekend visitors of all ages. The views of the Weser valley from the pano- ramic terrace are simply breathtaking. “Historical windows” – information posts Inhaltsverzeichnis Seite on the site – explain the history of the Museum 4 castle and the manufactory with pictures Guided tours 5 and diagrams. The new porcelain museum Visitors’ Workshop 6 uniquely demonstrates the fascinating Workshops 7 transformation in sophisticated dining Manufactory Store 8 from 1747 to today. Exclusive manufac- Castle Café and Restaurant 9 tured porcelain can be purchased in the General information 10 adjacent Manufactory Store. A meal or Entrance fees 10 snack in the Lottine café & restaurant Around Fürstenberg 11 rounds off the visit. Site map, Imprint 12 4 | FÜRSTENBERG | Travel planner for groups and travel operators The new museum in the castle Opening March 2017 A first-rate historical monument with modern interior design, designs. A modern-day projection shows how decoration can presenting the most extensive range of Fürstenberg porcelain in change the character of a piece of white porcelain. Impressive an innovatively designed exhibition – even in the castle‘s new portrayals of dining culture from the past and present provide an museum, the traditional and the modern blend harmoniously. -
Inland Shipping in Northern Germany: Two Case Studies”
#IWTS 2.0: “Mobilizing small waterway transport potentials” Of Containers and Feedstuff - Inland Shipping in Northern Germany: Two Case Studies Page. 0 “#IWTS 2.0: Mobilising small waterway transport potentials” https://northsearegion.eu/iwts20 Lay out cover by: Maritieme Akademie Harlingen. Cover photo: Claudia Behrend/bremenports GmbH & Co. KG This document is published within the #IWTS 2.0 project, click here, an INTERREG Vb project of the North Sea Region as one of the material for WP 5. Author Dr. Lars Stemmler bremenports GmbH & Co. KG (bremenports) Version: 1.0 of 28.04.2020 “#IWTS 2.0: Mobilising small waterway transport potentials” https://northsearegion.eu/iwts20 Of Containers and Feedstuff - Inland Shipping in Northern Germany: Two Case Studies” TABLE OF CONTENTS Of Containers and Feedstuffs – Inland Shipping in Northern Germany ................................................................. 4 From Ship to Shed: Feedstuffs Imports by Barge ....................................................................................................... 5 The supply chain ........................................................................................................................................................ 5 The role of inland shipping ....................................................................................................................................... 5 Review questions ...................................................................................................................................................... -
Evidence for Active Tilting of the NW-German Basin from Correlations Between fluvial Landscape and Geological Subground
Int J Earth Sci (Geol Rundsch) (2005) 94: 66–93 DOI 10.1007/s00531-004-0446-z ORIGINAL PAPER Thore Szeder Æ Frank Sirocko Evidence for active tilting of the NW-German Basin from correlations between fluvial landscape and geological subground Received: 12 November 2003 / Accepted: 16 September 2004 / Published online: 27 January 2005 Ó Springer-Verlag 2005 Abstract The catchment basin of the River Hunte about 2,640 km2. The well is on the southern slope of (Lower Saxony, NW-German Basin) was studied on a the German Middle Mountain range (‘‘Wiehengebirge’’) mesoscale (length of 90 km) to investigate the influ- at 150 m a.s.l.. ence of the geological subground on modern morphol- The River Hunte reaches the North German plain ogy. A Geo Information System (GIS) was used to after a distance of 8 km, at a height of about 50 m calculate linear correlation coefficients between the a.s.l.. After a distance of 37 km, the river reaches depth of geological strata (Base Zechstein to Base the Lake Du¨ mmer. Near the town Barnstorf (Fig. 2), the Quaternary) and the height of the modern landscape River Hunte enters the hilly and undulating area of (Holocene Alluvial Plain, Lower Weichselian Terrace, the ‘‘Cloppenburger and Wildeshauser Geest’’, formed catchment basin and watershed). High linear correlation by the glacial deposits of the Saalian glaciation. North coefficients between the Base of Tertiary and the height of the town Oldenburg, the River Hunte reaches the of the modern topography (catchment basin [r2=0.87], marshy area of the River Weser. -
Pioneers of Modern Geography: Translations Pertaining to German Geographers of the Late Nineteenth and Early Twentieth Centuries Robert C
Wilfrid Laurier University Scholars Commons @ Laurier GreyPlace 1990 Pioneers of Modern Geography: Translations Pertaining to German Geographers of the Late Nineteenth and Early Twentieth Centuries Robert C. West Follow this and additional works at: https://scholars.wlu.ca/grey Part of the Earth Sciences Commons, and the Human Geography Commons Recommended Citation West, Robert C. (1990). Pioneers of Modern Geography: Translations Pertaining to German Geographers of the Late Nineteenth and Early Twentieth Centuries. Baton Rouge: Department of Geography & Anthropology, Louisiana State University. Geoscience and Man, Volume 28. This Book is brought to you for free and open access by Scholars Commons @ Laurier. It has been accepted for inclusion in GreyPlace by an authorized administrator of Scholars Commons @ Laurier. For more information, please contact [email protected]. Pioneers of Modern Geography Translations Pertaining to German Geographers of the Late Nineteenth and Early Twentieth Centuries Translated and Edited by Robert C. West GEOSCIENCE AND MAN-VOLUME 28-1990 LOUISIANA STATE UNIVERSITY s 62 P5213 iiiiiiiii 10438105 DATE DUE GEOSCIENCE AND MAN Volume 28 PIONEERS OF MODERN GEOGRAPHY Digitized by the Internet Archive in 2017 https://archive.org/details/pioneersofmodern28west GEOSCIENCE & MAN SYMPOSIA, MONOGRAPHS, AND COLLECTIONS OF PAPERS IN GEOGRAPHY, ANTHROPOLOGY AND GEOLOGY PUBLISHED BY GEOSCIENCE PUBLICATIONS DEPARTMENT OF GEOGRAPHY AND ANTHROPOLOGY LOUISIANA STATE UNIVERSITY VOLUME 28 PIONEERS OF MODERN GEOGRAPHY TRANSLATIONS PERTAINING TO GERMAN GEOGRAPHERS OF THE LATE NINETEENTH AND EARLY TWENTIETH CENTURIES Translated and Edited by Robert C. West BATON ROUGE 1990 Property of the LfhraTy Wilfrid Laurier University The Geoscience and Man series is published and distributed by Geoscience Publications, Department of Geography & Anthropology, Louisiana State University. -
Brandenburg Niedersachsen Sachsen Thüringen
4375000 4400000 4425000 4450000 4475000 4500000 4525000 4550000 4575000 4600000 Legende Vorläufige Bewertung des Hochwasserrisikos gemäß Art. 4, 5 HWRM-RL Wahrenberg (HW2002) 5875000 5875000 ! (! PFRA - Orte vergangener und zukünftig zu erwartender signifikanter Hochwasserereignisse A ! l a Elbe von Havel bis Geesthacht nd (Art. 4, HWRM-RL) APSFR - Gewässerstrecken, von denen ein potenziell signifikantes Hochwasserrisiko ausgeht Salzwedel (HW2007) Seehausen (HW1909) (Art. 5, HWRM-RL) !! Al te D Salzwedel (HW1941) Bombeck (Osterwohle) (HW1998) u m ! Havelberg (HW1981) m !!! e z ! e it ! m J l g um e Ha ä D e ve J Klein-Damerow (HW1981) er t l ue Gewässereinzugsgebietsgrenze el z !! Ne ! Ilmenau/Este/Seeve ed e ! lzw Dosse-Jäglitz Jeetze - Seege Sa se ie B Grenze Flusseinzugsgebiete Elbe - Weser (gemäß WRRL) 5850000 5850000 Aller/Quelle Grenze der Planungseinheiten (gemäß WRRL) Rhin e d l i Rhin M G Schollene (HW1981) r Milde-Biese-Aland ü t z Administrative Grenze e ! r! Kalbe (HW1998) V o r f ! l ! u t e Landesgrenze Sachsen-Anhalt U r c h Stendal (HW1994) t e e b l !! E Sonstiges Tangermünde (HW2002) r Gewässernetz DLM1000 (Berichtsnetz der HWRM-RL und der WRRL) 5825000 5825000 ge an !! T te ig in re Ve e m m Klitsche (HW1981) e r t Milde-Biese-Aland Name der Planungseinheit s t! p! u a H Magdeburg (HW2002) Ort und Jahr eines signifikanten Hochwassers der Vergangenheit (Art. 4 HWRM-RL) Tanger Untere Havel Brandenburg h c a Bode Gewässer, von dem ein potenziell signifikantes Hochwasserrisiko ausgeht (Art. 5 HWRM-RL) B r e Elbe von Saale bis Havel n e Ohre h Parchen (HW2007) c r a P !- ! Kartenhintergrund: Topographische Übersichtskarte 1:250.000, Digitales Geländemodell DGM10 m i Weferlingen (HW1981) e h h O c Niedersachsen ! u Planunterlage auf der Basis amtlicher Geobasisdaten vom "[Geobasisdaten] © LVermGeo LSA (www.lvermgeo.sachsen-anhalt.de) / 10008". -
DOCUMENT RESUME ED 384 553 SO 024 877 AUTHOR Blankenship, Glen; Tinkler, D. William TITLE the Geography of Germany: Lessons
DOCUMENT RESUME ED 384 553 SO 024 877 AUTHOR Blankenship, Glen; Tinkler, D. William TITLE The Geography of Germany: Lessons for Teaching the Five Themes of Geography. PUB DATE 93 NOTE 95p.; For related volume of social studies lessons, see SO 024 876. PUB TYPE Guides Classroom Use Teaching Guides (For Teacher) (052) EDRS PRICE MF01/PC04 Plus Postage. DESCRIPTORS Area Studies; Elementary Secondary Education; Foreign Countries; Fundamental Concepts; *Geographic Concepts; Geographic Location; *Geography; *Geography Instruction; History; Human Geography; Physical Geography; Social Studies; Teaching Guides; Teaching Methods; Western Civilization IDENTIFIERS *Germany ABSTRACT This activity guide contains five lessons. Lesson 1 deals with "Location of Germany on the Earth's Surface" with two activities:(1) "Germany's Location in the World"; and (2) "Germany's Location in Europe." Lesson 2 is on the "Physical and Human Characteristics of Germany" with four activities on:(1) "Physical Features of Germany";(2) "Germany's Population Pyramid"; (3) " Population Density in Germany"; and (4) "Population Distribution in Germany." Lesson 3 addresses "The Interaction of the German People and Their Environment" with four activities: (1) "Land Use in Germany";(2) "Industrial Areas in Germany"; (3) "Pollution in Germany"; and (4) "The Environment." Lessc- 4 highlights "Movement and Diversity in Germany" with two activities:(1) "Foreigners in Germany"; and (2) "Immigration to Germany." Lesson 5 develops the theme of "German Unification and Regional Changes" with aix activities: (1) "Regions in Germany";(2) "German Unification"; (3) "Opening the Berlin Wall";(4) "East German Perspectives on Unification, Part A";(5) "East German Perspectives on Unification, Part B"; and (6) "World Press Views on Unification." Complete handouts and instruc'tions accompany the lessons.