DOCSLIB.ORG

Be River, Czech Labe, One of the Major Waterways of Central Europe

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Be River, Czech Labe, One of the Major Waterways of Central Europe be River, Czech Labe, one of the major waterways of central Europe. It runs from the Czech Republicthrough Germany to the North Sea, flowing generally to the northwest. The river rises on the southern side of the Krkonoše (Giant) Mountains near the border of the Czech Republic and Poland. It then makes a wide arc across Bohemia (northwestern Czech Republic) and enters eastern Germany about 25 miles (40 kilometres) southeast of Dresden. For the remainder of its course it flows through Germany. Above Hamburg the Elbe splits into two branches; these rejoin farther downstream, and the river then broadens into its estuary, the mouth of which is at Cuxhaven, where it flows into the North Sea. Elbe River, cehă Labe, unul dintre cele mai importante căile navigabile din Europa Centrală. Se ruleaza din Republica Cehă prin Germania la Marea Nordului, care curge în general, la nord-vest. Râul se ridică de pe latura de sud a Krkonoše (gigant) Munț ii in apropiere de frontiera Republica Cehă și Polonia. Apoi face un arc larg peste Bohemia (nord-vestul Republica Cehă) și intră în Germania de Est la aproximativ 25 mile (40 km) sud-est de Dresda. Pentru restul cursului său curge prin Germania. Deasupra Hamburg Elba se imparte in doua ramuri; acestea reuni mai departe în aval, iar râul apoi extinde în estuar, gura, care este la Cuxhaven, în cazul în care se varsă în Marea Nordului. IMAGES QUIZZES LISTS The total length of the Elbe is 724 miles (1,165 kilometres), of which roughly one-third flows through the Czech Republic and two-thirds through Germany. Its total drainage area is 55,620 square miles (144,060 square kilometres). Major tributaries are the Vltava (Moldau), Ohře (Eger), Mulde, and Saale rivers, all of which join it from the left, and the Iser, Schwarze (“Black”) Elster, Havel, and Alster rivers from the right. Lungimea totală a Elba este 724 mile (1165 km), din care aproximativ o treime curge prin Republica Cehă și două treimi prin Germania. Suprafaț a sa totală este de drenaj 55,620 mile pătrate (144,060 km patrati). Afluenț i majore sunt Vltava (Moldau), Ohře (Eger), Mulde, iar râurile Saale, toate din care aceasta adera pe partea stângă, și Iser, Schwarze ("Black") Elster, Havel, iar Alster râuri din dreap Physical features Physiography The Elbe is formed by the confluence of numerous headwater streams in the KrkonošeMountains a few miles from the Polish-Czech frontier. It flows south and west, forming a wide arc for about 225 miles in the Czech Republic to its confluence with the Vltava at Mělník and is joined 18 miles downstream by the Ohře. Elba este format din confluenț a a numeroase fluxuri afluent din KrkonošeMountains câ ț iva kilometri de frontiera polono-ceh. Curge spre sud și vest, formând un arc larg de aproximativ 225 mile în Republica Cehă la confluenț a acestuia cu Vltava la Mělník și este îmbinată 18 mile în aval de Ohře. It then cuts to the northwest through the picturesque Elbe Sandstone Mountains, and, in a gorge four miles long, it enters Germany. Between Dresden and Magdeburg the Elbe receives many long tributaries, of which all except the Schwarze Elster are left-bank streams. These are the Mulde and the Saale and its tributaries—including the Weisse (“White”) Elster, the Unstrut, and the Ilm. These left-bank tributaries rise in the Ore Mountains or the Thuringian Forest and form the drainage basin of the middle Elbe, with its geographic foci in Halle and Leipzig. Apoi taie la nord-vest, prin munț ii pitore ș ti Gresie Elbe, și, într-un defileu patru mile lungime, acesta intră Germania. Între Dresda si Magdeburg Elba primeș te multe afluen ț i lungi, din care toate, cu excepț ia Schwarze ELSTER sunt fluxuri stânga-bancare. Acestea sunt Mulde și Saale și afluen ț ii săi, inclusiv-Weisse ("alb") Elster, Unstrut, și ILM. Aceste afluen ț i de stânga-bancare creș te în Mun ț ii Metaliferi Pădurea Turingiei sau și formează bazinul hidrografic al Elbei mijloc, cu focare geografică în Halle și Leipzig. Halle is on the Saale, just below the confluence of the Weisse Elster; Leipzig lies at the confluence of the Pleisse and the Weisse Elster. Below Magdeburg the Elbe receives most of its water from its right bank. Most of these tributaries rise in the uplands of Mecklenburg. The river enters the North German Plain at Riesa, 25 miles below Dresden; below Riesa it meanders in a wide floodplain and has some abandoned loops. Dikes begin there and continue as far as the confluence of the Mulde. Halle este pe Saale, chiar sub confluenț a Weiße Elster; Leipzig se află la confluen ț a a Pleiße și Weisse Elster. Sub Magdeburg Elba primeste cea mai mare parte a apei de la banca dreapta. Cele mai multe dintre aceste afluenț i cre ș te în zonele înalte de Mecklenburg. Râul intră în nord Câmpia german la Riesa, 25 mile de mai jos Dresda; de mai jos Riesa se meandre într-o zonă inundabilă larg și are unele bucle abandonate. Diguri începe acolo și continuă până la confluenț a Mulde. Between Wittenberg and Dessau the east–west valley floor narrows to five miles in width, and hilly land rises to the north (the Fläming Heath) and south. From Dessau to Magdeburg the floodplain widens, and dikes have been constructed continuously down to the sea. In its course below Magdeburg the floodplain is two miles wide down to the confluence with the Havel. The river keeps to the left of its floodplain and sometimes cuts into the low hills on its banks. Între Wittenberg și Dessau vale podeaua est-vest se îngustează la cinci mile în lă ț ime, și terenuri deluroase se ridica la nord (The Flaming Heath) și sud. De la Dessau a Magdeburg luncii lărgeș te, iar digurile au fost construite în mod continuu până la mare. În cursul sub Magdeburg luncii este de două km lăț ime până la confluen ț a cu Havel. Râul păstrează la stânga de lunca sale și, uneori, taie în dealurile joase de pe malurile sale. Below the confluence with the Havel the river flows southeast–northwest; the floodplain widens and has distributaries and backwaters often flanked by low sandy hills (geest). Reclaimed salt marshes begin at Lauenburg. Above Hamburg—which the Elbe transverses in two arms, the Norder Elbe and the Süder Elbe—the floodplain is eight miles wide but narrows to four miles between the sandy geest of Schleswig-Holstein and the Lüneburg Heath. The estuary proper of the Elbe (Unterelbe) extends from Hamburg to Cuxhaven, a distance of about 55 miles. It varies in width from one to two miles, but much of it is occupied by mud flats and sandbanks. The main channel is buoyed and dredged. At high tide the channel has a depth of some 53 feet (16 metres). The south or left bank is low and marshy and the river has sandbanks; the right bank is steep below Hamburg, but farther downstream there are marshes, diked and drained, that are intensively cultivated. The great port city of Hamburg grew up on the Alster River on low sandy hills above the marshes. The modern port facilities have spread to the low-lying south bank of the Elbe. Hydrology The flow of water in the Elbe varies considerably with the amount of precipitation and thawing in its drainage basin. At Dresden the discharge rate averaged 11,200 cubic feet (317 cubic metres) per second in the period 1931–75, but the rate varied from a minimum of 800 cubic feet to a maximum of 118,700. At Neu-Darchau, about 140 miles above the mouth, the discharge rate was 24,700 cubic feet per second in the period 1926–65, with extremes of 5,100 and 127,700. These great variations sometimes hinder navigation. Although there are dams on the upper Elbe in the Czech Republic and at Geesthacht, Ger., and large dams have been built on the Vltava and on the Saale in the Thuringian Forest, these are not sufficient to control the water level of the Elbe. Debitul de apă în Elba variază considerabil cu cantitatea de precipitaț ii și topirea în bazinul hidrografic al acesteia. La Dresda rata de descărcare de gestiune medie 11200 de metri cubi (317 metri cubi pe secundă) în perioada 1931-1975, dar rata a variat de la un minim de 800 de metri cubi la un maxim de 118700. La Neu-Darchau, aproximativ 140 mile deasupra gurii, rata de descărcare de gestiune a fost 24700 de metri cubi pe secundă, în perioada 1926-1965, cu extreme de 5100 și 127700. Aceste varia ț ii mari împiedică uneori de navigare. De ș i există baraje pe cursul superior al Elba în Republica Cehă și în Geesthacht, Ger., Și baraje mari au fost construite pe Vltava și pe Saale în Pădurea Turingiei, acestea nu sunt suficiente pentru a controla nivelul de apă din Elba. The lower course of the Elbe is tidal as far as the dam at Geesthacht, above Hamburg, where the river flow periodically reverses its direction. The average tide at Hamburg is about eight feet. However, during storms the water may rise much higher, occasionally even flooding parts of the city. Cursul inferior al Elba este mareelor în ceea ce barajul de la Geesthacht, peste Hamburg, în cazul în care debitul râului inversează periodic direcț ia sa. Valul medie la Hamburg este de aproximativ opt metri. Cu toate acestea, în timpul furtunilor apa poate creș te mult mai mare, uneori chiar inundaț ii păr ț i ale ora ș ului.
Load more

Recommended publications
  • The Stamps of the German Empire
    UC-NRLF 6165 3fi Sfifi G3P6 COo GIFT OF Lewis Bealer THE STAMPS OF THE GERMAN STATES By Bertram W. H. Poole PART I "Stamps of the German Empire" BADEN MECKLENBURG-SCHWERIN BAVARIA MECKLENBURG-STREUTZ BERGEDORF OLDENBURG BREMEN PRUSSIA BRUNSWICK SAXONY HAMBURG SCHLESWIG-HOISTEIN HANOVER LUBECK WURTEMBERG HANDBOOK NUMBER 6 Price 35c PUBLISHED BY MEKEEL-SEVERN-WYLIE CO. BOSTON, MASS. i" THE STAMPS OF THE GERMAN EMPIRE BY BERTRAM W. H. POOLE AUTHOR OF The Stamps of the Cook Islands, Stamp Collector's Guide, Bermuda, Bulgaria, Hong Kong, Sierra Leone, Etc. MEKEEL-SEVERN-WYLIE CO. HANDBOOK No. 6 PUBLISHED BY MEKEEL-SEVERN-WYLIE CO. BOSTON, MASS. GIFT OF FOREWORD. In beginning this series of articles little is required in the way of an intro- ductory note for the title is lucid enough. I may, however, point out that these articles are written solely for the guidance of the general collector, in which category, of course, all our boy readers are included. While all im- portant philatelic facts will be recorded but little attention will be paid to minor varieties. Special stress will be laid on a study of the various designs and all necessary explanations will be given so that the lists of varieties appearing in the catalogues will be plain to the most inexperienced collector. In the "refer- ence list," which will conclude each f chapter, only > s.ucji s. arfif>s; Hifl >e in- cluded as may; ie,'con&tfJdrekt ;"e,ssntial" and, as such,' coming 'within 'the scope of on the.'phJlaJtetist'lcoUeetijig' ^ene^l" lines. .V.
    [Show full text]
  • Offenbach, 30 January 2015 – Frequent Weather Systems Coming in from the West Brought Varied Weather to Germany in January 2015
    The weather in Germany in January 2015 Year of record temperatures in 2014 followed by a much too warm January 2015 Offenbach, 30 January 2015 – Frequent weather systems coming in from the west brought varied weather to Germany in January 2015. Everything was included, from spring-like warmth with record temperatures and severe storms to brief wintry interludes. Overall, the month was very mild with high precipitation and little sunshine. This is what the initial analysis by the Deutscher Wetterdienst (DWD) of data from its around 2,000 weather stations shows. Periods of spring-like warmth with record temperatures Following on from the year of 2014, which was the warmest since records began, January 2015, too, saw a positive temperature anomaly. At 2.1 degrees Celsius (°C), the average temperature was 2.6 degrees higher than the international reference value for 1961 to 1990 of -0.5°C. Compared to the warmer period 1981 to 2010, the deviation was +1.7°C. The influence of high pressure prevailed at the start of the month, but brought weather with little cloud cover only to the south. This caused the temperature over the snow cover existing there to fall and give hard frosts. Leutkirch-Herlazhofen in the Württemberg part of the Allgäu recorded the lowest temperature in January with -15.2°C in the night to 1 January. After that, lively westerly winds, which generally brought very mild air masses, prevailed under the influence of low pressure during the first twenty days of the month. On 10 January, the storm depression ‘Felix’ brought spring-like warmth to Germany.
    [Show full text]
  • 2.14 Mean Annual Climatic Water Balance
    2.14 Mean Annual Climatic Water Balance The climatic water balance (CWB) is defined as the difference between precipitation depth Baltic Sea. The whole lowland regions of Mecklenburg-Vorpommern (Mecklenburg-Western and the depth of potential evapotranspiration at a given site during a certain time period. Pomerania), Brandenburg, Sachsen-Anhalt (Saxony-Anhalt), and Sachsen (Saxony) have negative summer half-year balances, with average values sometimes drastically below In general climatology, climate classifications are usually based on the weather elements “air - 100 mm. The highest deficits in the summer half-year show values below -300 mm. In sum- temperature” and “precipitation depth”, from which e. g. the description of the aridity of the mers with abundant rainfall, positive half-year balances may be recorded too, what was the climate is derived, the so-called aridity index. However, in the context of water-resources case in about one third of the years in the series 1961–1990. management and hydrology, the climatic water balance is better suitable for the hydroclimatic characterisation of sites, areas or periods, because the (hydro-)climatic conditions are The period with mean negative monthly balances in the inland lowlands lasts from April to described directly by means of the water-balance effective elements “precipitation” or “poten- September/October. The highest monthly balance deficits below -100 mm are recorded in the tial evapotranspiration” in the dimension “mm”. Dependent on whether precipitation depth or months from May to July. Negative monthly balances may occur throughout the year, potential evapotranspiration depth prevails in the considered period, the climatic water provided dry weather prevails.
    [Show full text]
  • Wolf to the German State of Lower Saxony EXPEDITION REPORT
    EXPEDITION REPORT Expedition dates: 23 June – 6 July 2018 Report published: May 2019 Love / hate relationships: Monitoring the return of the wolf to the German state of Lower Saxony EXPEDITION REPORT Love / hate relationships: Monitoring the return of the wolf to the German state of Lower Saxony Expedition dates: 23 June – 06 July 2018 Report published: May 2019 Authors: Peter Schütte Wolf commissioner Matthias Hammer (editor) Biosphere Expeditions 1 © Biosphere Expeditions, a not-for-profit conservation organisation registered in Australia, England, France, Germany, Ireland, USA Member of the United Nations Environment Programme's Governing Council & Global Ministerial Environment Forum Member of the International Union for the Conservation of Nature ABSTRACT This report details wolf (Canis lupus lupus) active monitoring fieldwork by Biosphere Expeditions in collaboration with the State Wolf Bureau of the German state of Lower Saxony and local wolf commissioners. Field work was conducted from 23 June to 6 July 2018 in two one-week long groups comprising twelve citizen scientists. The aim of the expedition was to collect samples for DNA and dietary analyses. This was done by sending small groups into the field to search for scat samples. 24 citizen scientists took part in the expedition, 16 from Germany or its immediate neighbour states (67%) with two of them (8%) from Lower Saxony, three people each from North America and the United Kingdom (12.5%), as well as one person each from Iceland and Australia (4%). Before commencement of field work, which was exclusively conducted on public paths and bridleways, citizen scientists were trained for 1.5 days in sample detection, sampling and data collection techniques.
    [Show full text]
  • Deutschland 83 Is Determined to Stake out His Very Own Territory
    October 3, 1990 – October 3, 2015. A German Silver Wedding A global local newspaper in cooperation with 2015 Share the spirit, join the Ode, you’re invited to sing along! Joy, bright spark of divinity, Daughter of Elysium, fire-inspired we tread, thy Heavenly, thy sanctuary. Thy magic power re-unites all that custom has divided, all men become brothers under the sway of thy gentle wings. 25 years ago, world history was rewritten. Germany was unified again, after four decades of separation. October 3 – A day to celebrate! How is Germany doing today and where does it want to go? 2 2015 EDITORIAL Good neighbors We aim to be and to become a nation of good neighbors both at home and abroad. WE ARE So spoke Willy Brandt in his first declaration as German Chancellor on Oct. 28, 1969. And 46 years later – in October 2015 – we can establish that Germany has indeed become a nation of good neighbors. In recent weeks espe- cially, we have demonstrated this by welcoming so many people seeking GRATEFUL protection from violence and suffer- ing. Willy Brandt’s approach formed the basis of a policy of peace and détente, which by 1989 dissolved Joy at the Fall of the Wall and German Reunification was the confrontation between East and West and enabled Chancellor greatest in Berlin. The two parts of the city have grown Helmut Kohl to bring about the reuni- fication of Germany in 1990. together as one | By Michael Müller And now we are celebrating the 25th anniversary of our unity regained.
    [Show full text]
  • Scottish Geographical Magazine the Origin And
    This article was downloaded by: [University of Ulster Library] On: 04 January 2015, At: 03:58 Publisher: Routledge Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Scottish Geographical Magazine Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/rsgj19 The origin and development of heather Moorland Dr. W. G. Smith Published online: 27 Feb 2008. To cite this article: Dr. W. G. Smith (1902) The origin and development of heather Moorland, Scottish Geographical Magazine, 18:11, 587-597, DOI: 10.1080/00369220208733402 To link to this article: http://dx.doi.org/10.1080/00369220208733402 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content. This article may be used for research, teaching, and private study purposes.
    [Show full text]
  • The Geography of Germany: Lessons for Teaching the Five Themes of Geography
    DOCUMENT RESUME ED 460 910 SO 029 411 AUTHOR Blankenship, Glen; Tinkler, D. William TITLE The Geography of Germany: Lessons for Teaching the Five Themes of Geography. Social Studies, Grades 9-12. Update 1997/1998. INSTITUTION Inter Nationes, Bonn (Germany).; Goethe House, New York, NY. PUB DATE 1998-00-00 NOTE 105p.; Transparency 7 is not available from ERIC. For earlier version, see ED 396 972. AVAILABLE FROM National Council for the Social Studies, NCSS Publications, P.O. Box 2067, Waldorf, 'MD 20604-2067. Tel: 800-683-0812 (Toll Free); Fax: 301-843-0159; e-mail: [email protected]; Web site: http://www.ncss.org/home/ncss. PUB TYPE Guides Classroom Teacher (052) EDRS PRICE MF01/PC05 Plus Postage. DESCRIPTORS Area Studies; Civics; Cultural Education; Culture; Foreign Countries; *Geographic Concepts; *Geographic Location; *Geographic Regions; Geography; *Geography Instruction; High Schools; *Human Geography; Maps; Multicultural Education; Physical Geography; Social Studies; World Geography; World History IDENTIFIERS *Germany ABSTRACT This packet contains five lessons related to the five themes of geography: location; place; human-environment interaction; movement; and region. The lessons are designed to support the teaching of courses in world geography, U.S. government/civics, and economics from a comparative U.S./German perspective. Lessons include:(1) "Location of Germany on the Earth's Surface"; (2) "Physical and Human Characteristics of Germany"; (3) "The Interaction of the German People and Their Environment";(4) "Cultural Diversity in
    [Show full text]
  • 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.
    [Show full text]
  • Late Cretaceous to Paleogene Exhumation in Central Europe – Localized Inversion Vs
    https://doi.org/10.5194/se-2020-183 Preprint. Discussion started: 11 November 2020 c Author(s) 2020. CC BY 4.0 License. Late Cretaceous to Paleogene exhumation in Central Europe – localized inversion vs. large-scale domal uplift Hilmar von Eynatten1, Jonas Kley2, István Dunkl1, Veit-Enno Hoffmann1, Annemarie Simon1 1University of Göttingen, Geoscience Center, Department of Sedimentology and Environmental Geology, 5 Goldschmidtstrasse 3, 37077 Göttingen, Germany 2University of Göttingen, Geoscience Center, Department of Structural Geology and Geodynamics, Goldschmidtstrasse 3, 37077 Göttingen, Germany Correspondence to: Hilmar von Eynatten ([email protected]) Abstract. Large parts of Central Europe have experienced exhumation in Late Cretaceous to Paleogene time. Previous 10 studies mainly focused on thrusted basement uplifts to unravel magnitude, processes and timing of exhumation. This study provides, for the first time, a comprehensive thermochronological dataset from mostly Permo-Triassic strata exposed adjacent to and between the basement uplifts in central Germany, comprising an area of at least some 250-300 km across. Results of apatite fission track and (U-Th)/He analyses on >100 new samples reveal that (i) km-scale exhumation affected the entire region, (ii) thrusting of basement blocks like the Harz Mountains and the Thuringian Forest focused in the Late 15 Cretaceous (about 90-70 Ma) while superimposed domal uplift of central Germany is slightly younger (about 75-55 Ma), and (iii) large parts of the domal uplift experienced removal of 3 to 4 km of Mesozoic strata. Using spatial extent, magnitude and timing as constraints suggests that thrusting and crustal thickening alone can account for no more than half of the domal uplift.
    [Show full text]
  • Leipzig New Lake Land
    LEIPZIG NEW LAKELAND LAND IN MOTION 1 Maritime atmosphere at Zöbigker Marina Welcome to Leipzig New Lakeland ! By 2015, the flooding of opencast mines around the city of Leipzig in central Germany will have created nearly 70 square kilometres of new lakes – and a wealth of leisure opportunities. Visitors can already enjoy various adrenaline sports on water and on land, as well as fun and relaxation for the whole family, not to mention a wide variety of culture. Join the local Schladitz family as they discover Leipzig New Lakeland – Land in Motion. 2 Black gold Leipzig New Lakeland has a proud mining heritage. And with its industrial past still very much in evidence, there are some fascinat- ing discoveries to be made. page 4 In the pink Sports enthusiasts are always on the look-out for attractive facilities in the right surroundings for their favourite activities. They’re spoilt for choice in Leipzig New Lakeland! page 6 Green surroundings Get away from your daily routine – and get back to nature! Leipzig New Lakeland’s the place to recharge your batteries in the company of family and friends. page 8 Colourful history HierHistorical wurden spectacles Geschichten and placesgeschrie - ben.where Historische famous writers, Spektakel philosophers, und Ausflügeartists and zu composers Wirkungsstätten once lived nam - hafterand worked Dichter, make Denker Leipzig und New Künstler Lake - machenland a cultural das Leipziger treasure Neuseenland trove. zur Schatzkammer. page 10 Play the blues Art and music are part and parcel of Leipzig New Lakeland. After your days out, take in first-rate perfor- mances in the evenings.
    [Show full text]
  • A New Basal Sphenacodontid Synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany
    A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany JÖRG FRÖBISCH, RAINER R. SCHOCH, JOHANNES MÜLLER, THOMAS SCHINDLER, and DIETER SCHWEISS Fröbisch, J., Schoch, R.R., Müller, J., Schindler, T., and Schweiss, D. 2011. A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany. Acta Palaeontologica Polonica 56 (1): 113–120. A new basal sphenacodontid synapsid, represented by an anterior portion of a mandible, demonstrates for the first time the presence of amniotes in the largest European Permo−Carboniferous basin, the Saar−Nahe Basin. The new taxon, Cryptovenator hirschbergeri gen. et sp. nov., is autapomorphic in the extreme shortness and robustness of the lower jaw, with moderate heterodonty, including the absence of a greatly reduced first tooth and only a slight caniniform develop− ment of the second and third teeth. Cryptovenator shares with Dimetrodon, Sphenacodon, and Ctenospondylus, but nota− bly not with Secodontosaurus, enlarged canines and a characteristic teardrop outline of the marginal teeth in lateral view, possession of a deep symphyseal region, and a strongly concave dorsal margin of the dentary. The new find shows that sphenacodontids were present in the Saar−Nahe Basin by the latest Carboniferous, predating the record of sphenacodontid tracks from slightly younger sediments in this region. Key words: Synapsida, Sphenacodontidae, Carboniferous, Saar−Nahe Basin, Germany. Jörg Fröbisch [[email protected]], Department of Geology, The Field Museum, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA and [joerg.froebisch@mfn−berlin.de], Museum für Naturkunde Leibniz−Institut für Evolu− tions− und Biodiversitätsforschung an der Humboldt−Universität zu Berlin, Invalidenstr.
    [Show full text]
  • Hydrogen Strategy for North Germany
    Ministries of Economics and Transport of the North German Coastal States Bremen, Hamburg, Mecklenburg-Western Pomerania, Lower Saxony and Schleswig-Holstein HYDROGEN STRATEGY FOR NORTH GERMANY 7 November 2019 Hydrogen Strategy for North Germany Summary The Hydrogen Strategy for North Germany is the result of close cooperation of a number of Federal States and of comprehensive and constructive involvement of active players from the areas of business, research and administration. Unique characteristics of North Germany Compared to other regions, North Germany features unparalleled locational advantages for establishing a ‘green’ hydrogen economy: great generating capacity for onshore and offshore wind-generated electricity with further expansion potential, underground formations for storing hydrogen, seaports whose import terminals are going to play a decisive role as logistics and business hubs, when it comes to importing and distributing green hydrogen and synthetic energy carriers, as well as for using hydrogen and exporting hydrogen-related technology and components, maritime enterprises and scientific expertise, as well as industry sectors with significant experience in handling hydrogen. Additional know-how is being generated in the six North German “Regulatory Sandboxes for the Energy Revolution”. Based on their economic policy, the North German States are able to offer attractive location perspectives for local companies and companies willing to settle in the area, to ensure that value is created, and that high-quality jobs are preserved in the region and new ones are created. They are going to encourage innovation and economic growth and therefore strengthen North Germany as a business location. By establishing a green hydrogen economy, the States are thus also going to continue their existing ambitious economic policies.
    [Show full text]