DOCSLIB.ORG

Emergency Hospital' S Suggested by Skiba

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Emergency Hospital' S Suggested by Skiba \ Newspaper Devoted , , the Community Intereat ( Fairly, Clearly Local Coverage And Impartially Each Week Complete News Pirtiirei >l XXXIX-NO. 29 CARTERET, N. J., FRIDAY, OCTOBlfc *!, I960 This Corner. Parade U.S.M.R^Emergenc> y Hospital' Details Honors 9 s Suggested by Skiba; Kllioit. THeposkv Get Gold Watches or •-•«*** (Jive Program for Bonds at Dinner h'le Hallo ween F«>te Held las! Mi;hi Favors Early Study CARTERET - Robert El- (See Plotun- on liot Hiid Joseph Teleposky co- CARTERE_T Irluiinnon of the annual Hal-I employees" tf US Mpfils RP ,Iii«T,ni parade sponsored by the fining Co, received gold Vatr.1, Ueformalion Services Set WoilldAsk jCin-teret. Recreation Depart-|es Or U.S. Bonds at the annual 1 |m,.m. tn be held Sunday after- , 25-Year Dinner laM niKh! T ! innon, October 30 today Ut-\MnmT was held at thr Kli/a- |...nin,T<l that thr assembly ferth-Cartwt Hotel Eli7«belh By Council of Churches Group Get iimint. for the parade this year; - ™[ John Towers CARTERET Thr Car- Ice will be led by laymen of , * !is ...e Cartrrr. Shopping Cen- , ,. „ *"'; ager presidPd 0V(1 Council of Churches the participating churches of '^dunfT,R°0SeVelt Ave: monies «nd made the present,, will sponsor a Reformation the council. TIIP theme for mi-. All bands, groups and| , J •» tlon of awards 0 (| Service of Worship to be hold the rvmliiR is "The' Priest- All Data ^legations are requested to as- • p | , ^ Tne em ll)ypps who r( in the First Presbyterian hood of All Believers." l-cemblr there not later than! , „ awards WPrr fts Church on Wednesday eve- Thomas Pox. a lay lender CARTKRET - Mayor Stept*. 1:30 P. M, sn that the parade: and an employee of Bell Tele- mny start, promptly at 2 P. M. ! ning. October 26. at 8:00 P.M. n Skiba las Midlae l K The entile Thr parade route will be as'- ° ' ' t> « s . Alfredo the sermon. 'follows: start at Carteret Shop- Paiva, John Batista, Ithought should be given to th« establishment of a hospital In IpinR Center to Roosevelt Ave- Truch, Joseph Kllyk, Charles Carteret. Inue, down Roosevelt Avenue toKahora, B e n v i n d o Matrin, Stephen Ronyak, Michael Ko- Dolan Suggests He Rfiki the project could fat HI sV WITH (AMPAH1N fhoto 'how •Pershing Avenue, right on Per- Installation is i Frank Barrdird. center, candidate for Mayor, John Konci. left, and vacs, Julius Oensi. Louis Strat- an "emergency hospital" lor * in \l icltnllnski. r(«ht. for Connrll shing Avenue to Carteret Ave- •II. Miming from picture Is William Grrrnwald. Candida** f«r a«*.•...<>.• nue, left on Carteret Avenue, ton, Gary Sohayda: Anthony Drive Here to start, Mayor Sklba said he re- then left to Roosevelt Avenue, Foytlin: Stephen LeWky: Mi'- Held by New alizes what such a program right on Roosevelt Avenue to chael BlRdt. Jozsrf Mnuiar, -would entail, but expressed th* tan. Honors Republicans Hit 1 - Party (;h h WomePershinn g Avenue, right on Per-Adam Boranowski. Tony Russo Build Hospital hope that it could come Into ure Avenue to Carteret Ave- Steve Moravek, George Little! PostofJ.W.V. being provided a non-partisan Michael Kursak; Joseph Nas- CARTERET — A — 'group was behind it to raltt nue, , lefeftt on Carteret Avenue on hospital CARTERET New officers | ^ I Slremiau; iSyslem; Need 'Watchdog' Assemble Gifts j library side to Cypress St., right enough flmds make u on Cypress St. to Washington CARTERET Frank I. In vl( of p tity lor an extended period Avenue, left on Washington cslzmadia, Stephen Me- Mayor Edward J. Dolan urRed!jewlsh War Veterans I '» * increase in Bareford. Republican candi- of tl«e. We think all will Avenue to Carteret High School zey, James Rpsko. Stephen,at Wednesday night's Third avor Stenhm, 4kih. « .population here, the need of Danku, John Peter. M n n The Middle- date for' mayor in a state- agree that because of theFor Missions stadium where the awards will r Pa-District Democratic Women's.JZ L *^ti^L ^".^I'^ch a hospital is clearly wi- •••.:\ BHr Association ment luted "today" In behalf ! wmplete control exercised by be made. ' the .. th cl s CARTERET — Church ser- Joseph Gurney, miaster of name such a committee to ex- :ii,:li: honored Emll of himself and the other can- ; "."»" ^f' °« ^ List Entrlcf body. Councilman Alexander! HM».«. »„ tu nsm ti i-«. *rth an active Interest in tces at The First Presbyterian i plore nil angles. He said there n( 7 Cook* Avenue Church will be held at 9 -.30 i To date tne lowing en- attended. i ,MI of hi* 50th an- sr, about $75,000 in a hospital A. M. this Sunday. The minis- trants in the parade have been ,i' member of the ter will preach the sermon, "To- received: bands, Carteret High;mnk 1, STorkr^m^<=rat,c SS^^/STS^^^^ ™*^ ash, John Barbarczuk, Walterjbas hall^the Middlesex CountyrV «,..» .i,,, i,,. i „„„„>„.. was donated at thr end ol I! School, St. Mary's High School, wnaa the nl ncn o ! gether for Christ." There is Kielman, Frnri Koeble', Josephi prosecutor expressed hihis hope * i, . w» !!»l «{«"k«. | j • mimi was pretexted t^resU of the community. WorW War whnl CaltRn a nursery ln the manse during Jr. Elks Drum and Bugle Corps, i.,i..,u r>-_:-. r^-..- - • 'jj^ a hospital project 1 Mr, Bareford said there are ™W The borough Cathol^ Vf*r[sM to iwM a hospital. MMIII' »t the dinner Mr. Bareford declared that ! the 11:00 service. Church Melrose Drum and BUKIP Corps, assisted In the cere- f the association held | many deficiencies existing in St PatrlcllB be started in the near future., nie"8rraTsin"g"thelr'coiovs'with! QidS Rvittm on the local level, voters j Carteret which require cor- School meets at 9:30 with clas-i Cadets, Barron- Pasipanki. and John Kereluik. mO H IK Manor, Metuchen. should not be swayed by a s He told the gathering thatlti,05e Of the JWV as a gpsturej Cpimcil agai rejected two DW| rection. He felt that efficient ses for all. On Sunday after-! j£* ' Woodbridge Post 4410 Port Beading '.ition «u nude by party labels. He said: VFW, Madonna CYO Drum & public Interest has increaseincr d of of U11JK, . !for paving of Poplar Street, j management of borough af- noon at 3:30 the Jr. and Jr. HI Manuel Perez. Frank Sosnow- fFellowship meets, and in theiBuRle Corp- Boy Scollt Tro°P Ma UO „•„- *...— other'speakers included Ber-I^oimcllman Thomas Milik felt K,iplan. an attorney of j -R wilt be generally agreed | fairs through wjund budget- «ki, Steve Pasztor, Prank Bino, i (evening at 7:30 the Sr. Hi Fel-|82; floals' Lions club> Shore- local Demociatic candidates na].d Abrams. another pn fiRurefi submitted were that a one-party system has | ary practices call for an ac- Walter Osyf, Stephen Nagy, had been questioned on the e)iMSStvt> u aB ihc love and reapact lownhip meets. crest Civic Club: Carteret Wom- tionnl commander of the JWV,- * decided to re-. deprived our citizens here of ' tlvc minority on the Council. Robert Woodward and John number of thr ta<r": en's Club; St. Joseph's School, WssibiUty of a hospital byiEdwar(1 fw..*W*. The the benefit of representatives j Running with Mr. Bare- On Tuesday evening, Octo- Alach. be Middlesex said St. Mary'g High School. Girl ™member,rss o:tof thhe PkParkviei wCi Civiic Cminty prescutor „„.. „,..„ Products * would act *t watchdogs I ford are Chester Wlelgolinslcl j*»er 36. the Women's Associa- 1 Scout Troop 190. ^ EVan- Club «t Us Octolper 3rd-meeting.;^^, wl wn lost,,.bd (l, nfk** of the New yorfc on wl *•' over borough aftdns and John Konci for'cotincii \^" " h«ve . fr,.,„„.„»•. ui im. tit atrrtn-1 gelicai - Lutlieran uy Nicholas Babftsky', Michael At that trme"Mayor'Stephen commander ' ie&'tSMf, and C and William Gi»enwaia, can- |«wtnw at 8:00 MKThej will 1 1 a h8d iM club Schcol: drill teama. Naval Re- 'Lompcyx)mpcy. Amandlo Damas,TDamas,"FriBrtti7i f r , merabers, Other officers installed were Hopelawn 40.42s. "••«t to t-;! :-Jb ,liWt-d to ,.«.t; rV.,, „ e. i u- didaU' for reelection as tax packages and gifts for 1 serve Drill team from Perth Tnmnpv A m » „ H i« nnm.', tnat the money In the hospitaliiivinir Levit:/ .wiinv IM™m »J fwo bids for sewer cleaning ... <m *« iiv age oV. troi of an> governmental en- tuinessor. the children of the mission sta- senior vice com- Amboy, All Girl Rifiettes from ordered tabled. One cam* tions assigned to the associa- bl et 0 tot uwdfA or iisideru of New Brunswick, Candleiers Stephen Katko, Stephen Shaf- "* .J , ™, f' ' 'v>^ com m a n4 er ; Sidney from Fred Hryrkh Little Palls, tion. A list of the items needed from Newark. In addition the H.u Association, is as follows: clothing, toys, fer. Julius Horvath. ;a Hospital. The fund holds an Hwbst, adjutant and patrioticiasking $3 400 and the other following will participate tn dalD offlrel •ived for many years^Andre; w Charara (larteret Pupils and jewelry for 11, 12, and 13 Elizabeth ' o?h S!, V°i, 'J' ': Arthur Bauchner. quar-lfrom Robinson Pipe Cleaning; groups, Carteret Fire Dept., S kllla h8d rBedtheresldcnts •<•• of I he Committee Joao Carvallo Antnnin rn t ( . }; ,termaster; Nathan Jacoby,,co., CannonstuuK, Pa., for $3,- year olds; girls' dresses; boys' Port Reading Fire Dept., Ocean- Joao caivallo, Antonio Go-^o try to seek personal pledges chaplain; Summer Weener, 700. :<-..(l Grievances. pajamas; 3 wool skirts for mez, George Under, John Vi- port Fire Dept.,- Columbus Harold • of the Rites Saturday In Trenton Tour girls, size 14; 2 boys' sweaters, School, St.
Load more

Recommended publications
  • Full-Waveform Inversion of Gpr Data from the Thur River Aquifer
    FULL-WAVEFORM INVERSION OF GPR DATA FROM THE THUR RIVER AQUIFER Published in Near Surface Geophysics: Klotzsche, A., van der Kruk, J., Meles, G. A., Doetsch, J., Maurer, H., and Linde, N., 2010, Full-waveform inversion of cross- hole ground-penetrating radar data to characterize a gravel aquifer close to the Thur River, Switzerland: Near Surface Geophysics, 8, 635-649. 0 Full-waveform inversion of GPR data from the Thur River aquifer ABSTRACT Crosshole radar tomography is a useful tool for mapping shallow subsurface electrical properties viz. dielectric permittivity and electrical conductivity. Common practice is to invert crosshole radar data with ray-based tomographic algorithms using first arrival traveltimes and first cycle amplitudes. However, the resolution of conventional standard ray-based inversion schemes for crosshole ground penetrating radar (GPR) is limited because only a fraction of the information contained in the radar data is used. The resolution can be improved significantly by using a full-waveform inversion that considers the entire waveform, or significant parts thereof. A recently developed 2-D time-domain vectorial full-waveform crosshole radar inversion code has been modified in the present study by allowing optimized acquisition setups that reduce the acquisition time and computational costs significantly. This is achieved by minimizing the number of transmitter points and maximizing the number of receiver positions. The improved algorithm was employed to invert crosshole GPR data acquired within a gravel aquifer (4 - 10 m depth) in the Thur valley, Switzerland. The simulated traces of the final model obtained by the full-waveform inversion fit the observed traces very well in the lower part of the section and reasonably well in the upper part of the section.
    [Show full text]
  • Stocking Measures with Big Salmonids in the Rhine System 2017
    Stocking measures with big salmonids in the Rhine system 2017 Country/Water body Stocking smolt Kind and stage Number Origin Marking equivalent Switzerland Wiese Lp 3500 Petite Camargue B1K3 genetics Rhine Riehenteich Lp 1.000 Petite Camargue K1K2K4K4a genetics Birs Lp 4.000 Petite Camargue K1K2K4K4a genetics Arisdörferbach Lp 1.500 Petite Camargue F1 Wild genetics Hintere Frenke Lp 2.500 Petite Camargue K1K2K4K4a genetics Ergolz Lp 3.500 Petite Camargue K7C1 genetics Fluebach Harbotswil Lp 1.300 Petite Camargue K7C1 genetics Magdenerbach Lp 3.900 Petite Camargue K5 genetics Möhlinbach (Bachtele, Möhlin) Lp 600 Petite Camargue B7B8 genetics Möhlinbach (Möhlin / Zeiningen) Lp 2.000 Petite Camargue B7B8 genetics Möhlinbach (Zuzgen, Hellikon) Lp 3.500 Petite Camargue B7B8 genetics Etzgerbach Lp 4.500 Petite Camargue K5 genetics Rhine Lp 1.000 Petite Camargue B2K6 genetics Old Rhine Lp 2.500 Petite Camargue B2K6 genetics Bachtalbach Lp 1.000 Petite Camargue B2K6 genetics Inland canal Klingnau Lp 1.000 Petite Camargue B2K6 genetics Surb Lp 1.000 Petite Camargue B2K6 genetics Bünz Lp 1.000 Petite Camargue B2K6 genetics Sum 39.300 France L0 269.147 Allier 13457 Rhein (Alt-/Restrhein) L0 142.000 Rhine 7100 La 31.500 Rhine 3150 L0 5.000 Rhine 250 Doller La 21.900 Rhine 2190 L0 2.500 Rhine 125 Thur La 12.000 Rhine 1200 L0 2.500 Rhine 125 Lauch La 5.000 Rhine 500 Fecht und Zuflüsse L0 10.000 Rhine 500 La 39.000 Rhine 3900 L0 4.200 Rhine 210 Ill La 17.500 Rhine 1750 Giessen und Zuflüsse L0 10.000 Rhine 500 La 28.472 Rhine 2847 L0 10.500 Rhine 525
    [Show full text]
  • Karte Der Erdbebenzonen Und Geologischen Untergrundklassen
    Karte der Erdbebenzonen und geologischen Untergrundklassen 350 000 KARTE DER ERDBEBENZONEN UND GEOLOGISCHEN UNTERGRUNDKLASSEN FÜR BADEN-WÜRTTEMBERG 1: für Baden-Württemberg 10° 1 : 350 000 9° BAYERN 8° HESSEN RHEINLAND- PFALZ WÜRZBUR G Die Karte der Erdbebenzonen und geologischen Untergrundklassen für Baden- Mainz- Groß- Main-Spessart g Wertheim n Württemberg bezieht sich auf DIN 4149:2005-04 "Bauten in deutschen Darmstadt- li Gerau m Bingen m Main Kitzingen – Lastannahmen, Bemessung und Ausführung üblicher Freudenberg Erdbebengebieten Mü Dieburg Ta Hochbauten", herausgegeben vom DIN Deutsches Institut für Normung e.V.; ub Kitzingen EIN er Burggrafenstr. 6, 10787 Berlin. RH Alzey-Worms Miltenberg itz Die Erdbebenzonen beruhen auf der Berechnung der Erdbebengefährdung auf Weschn Odenwaldkreis Main dem Niveau einer Nicht-Überschreitenswahrscheinlichkeit von 90 % innerhalb Külsheim Werbach Großrinderfeld Erbach Würzburg von 50 Jahren für nachfolgend angegebene Intensitätswerte (EMS-Skala): Heppenheim Mud Pfrimm Bergst(Bergstraraßeß) e Miltenberg Gebiet außerhalb von Erdbebenzonen Donners- WORMS Tauberbischofsheim Königheim Grünsfeld Wittighausen Gebiet sehr geringer seismischer Gefährdung, in dem gemäß Laudenbach Hardheim des zugrunde gelegten Gefährdungsniveaus rechnerisch die bergkreis Höpfingen Hemsbach Main- Intensität 6 nicht erreicht wird Walldürn zu Golla Bad ch Aisch Lauda- Mergentheim Erdbebenzone 0 Weinheim Königshofen Neustadt Gebiet, in dem gemäß des zugrunde gelegten Gefährdungsniveaus Tauber-Kreis Mudau rechnerisch die Intensitäten 6 bis < 6,5 zu erwarten sind FRANKENTHAL Buchen (Odenwald) (Pfalz) Heddes-S a. d. Aisch- Erdbebenzone 1 heim Ahorn RHirschberg zu Igersheim Gebiet, in dem gemäß des zugrunde gelegten Gefährdungsniveaus an der Bergstraße Eberbach Bad MANNHEIM Heiligkreuz- S c Ilves- steinach heff Boxberg Mergentheim rechnerisch die Intensitäten 6,5 bis < 7 zu erwarten sind Ladenburg lenz heim Schriesheim Heddesbach Weikersheim Bad Windsheim LUDWIGSHAFEN Eberbach Creglingen Wilhelmsfeld Laxb Rosenberg Erdbebenzone 2 a.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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 ..........................................
    [Show full text]
  • Case Study Rhine
    International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR International Commission for the Hydrology of the Rhine Basin Erosion, Transport and Deposition of Sediment - Case Study Rhine - Edited by: Manfred Spreafico Christoph Lehmann National coordinators: Alessandro Grasso, Switzerland Emil Gölz, Germany Wilfried ten Brinke, The Netherlands With contributions from: Jos Brils Martin Keller Emiel van Velzen Schälchli, Abegg & Hunzinger Hunziker, Zarn & Partner Contribution to the International Sediment Initiative of UNESCO/IHP Report no II-20 of the CHR © 2009, KHR/CHR ISBN 978-90-70980-34-4 Preface „Erosion, transport and deposition of sediment“ Case Study Rhine ________________________________________ Erosion, transport and deposition of sediment have significant economic, environmental and social impacts in large river basins. The International Sediment Initiative (ISI) of UNESCO provides with its projects an important contribution to sustainable sediment and water management in river basins. With the processing of exemplary case studies from large river basins good examples of sediment management prac- tices have been prepared and successful strategies and procedures will be made accessible to experts from other river basins. The CHR produced the “Case Study Rhine” in the framework of ISI. Sediment experts of the Rhine riparian states of Switzerland, Austria, Germany and The Netherlands have implemented their experiences in this publication.
    [Show full text]
  • 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.
    [Show full text]
  • Reconstruction of Flood Events Based on Documentary Data And
    Hydrol. Earth Syst. Sci., 19, 4149–4164, 2015 www.hydrol-earth-syst-sci.net/19/4149/2015/ doi:10.5194/hess-19-4149-2015 © Author(s) 2015. CC Attribution 3.0 License. Reconstruction of flood events based on documentary data and transnational flood risk analysis of the Upper Rhine and its French and German tributaries since AD 1480 I. Himmelsbach1, R. Glaser1, J. Schoenbein1, D. Riemann1, and B. Martin2 1Physical Geography, Albert-Ludwigs Universität Freiburg, Freiburg, Germany 2CRESAT, University of Haut-Alsace, Mulhouse, France Correspondence to: J. Schoenbein ([email protected]) Received: 1 December 2014 – Published in Hydrol. Earth Syst. Sci. Discuss.: 7 January 2015 Revised: 11 September 2015 – Accepted: 23 September 2015 – Published: 14 October 2015 Abstract. This paper presents the long-term analysis of flood the small rivers in Alsace compared to those on the Baden occurrence along the southern part of the Upper Rhine River side – an interesting fact – especially if the modern European system and of 14 of its tributaries in France and Germany Flood directive is taken into account. covering the period starting from 1480 BC. Special focus is given on the temporal and spatial variations of flood events and their underlying meteorological causes over time. Ex- 1 Introduction amples are presented of how long-term information about flood events and knowledge about the historical aspect of The knowledge about the occurrence of floods in histori- flood protection in a given area can help to improve the un- cal times, their meteorological causes and their distribution derstanding of risk analysis and therefor transnational risk within the (hydrological) year does provide a deeper under- management.
    [Show full text]
  • Tracer Studies of River-Groundwater Interaction Under Hydropeaking Conditions
    Tracer Studies of River-Groundwater Interaction under Hydropeaking Conditions Dissertation Markus W. Fette 2 Dissertation ETH Nr. 16103 Tracer Studies of River-Groundwater Interaction under Hydropeaking Conditions A dissertation submitted to the SWISS FEDERAL INSTITUTE OF TECHNOLOGY ZURICH for the degree of DOCTOR OF NATURAL SCIENCES presented by MARKUS WOLFGANG FETTE Dipl.-Ing., University of Stuttgart born on September 12, 1973 citizen of Germany accepted on recommendation of Prof. Dr. Bernhard Wehrli, examiner Prof. Dr. Pierre Perrochet, co-examiner Prof. Dr. Anton Schleiss, co-examiner Zürich 2005 3 4 Was den Menschen angeht, so glaube ich an das Individuum, nicht aber an den Individualismus. Was die Natur angeht, so glaube ich an das sinnvolle Zusammenspiel ihrer schöpferischen und zerstörerischen Kräfte, nicht aber an deren Manipulierbarkeit zu eigennützigen Zwecken. Was die Musik angeht, so glaube ich an die Töne, nicht aber an die Noten. Was das Geld angeht, so glaube ich an Münzen und Noten und sonst an gar nichts. Was die ewige Liebe angeht, so glaube ich an ihre fortdauernde Renovierbarkeit, nicht aber an ihre Konservierbarkeit. Was die Religion angeht, so glaube ich an Erfahrung, nicht aber an Überzeugungen. Was Antworten auf die letzten Fragen angeht, so glaube ich an den Gedankenstrich, nicht aber an das Ausrufezeichen. Balts Nill, Musiker (Stiller Has) 5 6 Table of Contents T. Table of Contents.......................................................................... 7 A. Acknowledgements ...................................................................
    [Show full text]
  • Flood Risk Along the Upper Rhine Since AD 1480
    Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 12, 177–211, 2015 www.hydrol-earth-syst-sci-discuss.net/12/177/2015/ doi:10.5194/hessd-12-177-2015 © Author(s) 2015. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Hydrology and Earth System Sciences (HESS). Please refer to the corresponding final paper in HESS if available. Flood risk along the upper Rhine since AD 1480 I. Himmelsbach1, R. Glaser1, J. Schoenbein1, D. Riemann1, and B. Martin2 1Physical Geography, Albert-Ludwigs-University Freiburg, Germany 2CRESAT, University of Haut-Alsace, Mulhouse, France Received: 1 December 2014 – Accepted: 9 December 2014 – Published: 7 January 2015 Correspondence to: J. Schoenbein ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 177 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract This paper presents the occurrence, cause and frequency changes of floods, their development and distribution along the southern part of the upper Rhine River and of 14 of its tributaries in France and Germany covering the period from 1480 BC. Special 5 focus is given on the temporal and spatial variations and underlying meteorological causes which show a significant change over space and time. Examples are presented how long-term information can help to improve transnational risk and risk management analysis while connecting single historical and modern extreme events. 1 Introduction 10 The knowledge about the occurrence of floods in historical times, their meteorologi- cal causes and their distribution within the (hydrological) year does provide a deeper understanding of the natural variability of the severity of flood events by providing long- term knowledge about changes in the causes, frequencies and gravities of the floods.
    [Show full text]
  • Intergovernmental Perspective, 1991, V.17 No.4
    ‘commission_ ment in which the Congress declares ists don’t even have to be so clever in everything to be of national interest, fashioning a constitutional justification and then requires the states and lucal because the Supreme Court threw up governments to raise the money and its hands and said to the Congress, do perform the mandates under threat of what you want to do. The Com’t con- civil and, often, criminal annctions. cluded that the Tenth Amendment of- The Constitution has been amend- fers no guidance on where to draw the ed a thousand times over without the line between federal and state power, need to use the cumbersome, constitu- and that the only avenue left for main- tionally provided, amendment process. taining some balance among the gov- The Congress. the Administration, and ernments in our federal system is the courts have ignored the admoni- through the election process. tion of Chief Justice Roger B. “Ikney For the Congress, the end now who said, “If we are at liberty to give old justifies the means, and the Tenth words new meanings—there is no pow- Amendment is dead. When Justice States and cities are having in- er which may not by this mode of con- Robert H. Jackson, in Youn@/own v. creasing difficulty finding the funds struction, be conferred on the general Smvyer (1952), involving President Tru- to provide traditional services and facili- government and denied to the states.” man’s steel plant takeover, stated that ‘Ilrough the Constitution, the states ties —plice, fire, educntion, and tiras- “necessity knows no law,” he was right.
    [Show full text]