Documentation
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Humid Climate During Deposition of Sapropel 1 in the Mediterranean Sea: Assessing the Influence on the Alps
Global and Planetary Change 71 (2010) 242–248 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Humid climate during deposition of sapropel 1 in the Mediterranean Sea: Assessing the influence on the Alps Christoph Spötl a,⁎, Kurt Nicolussi b, Gernot Patzelt c, Ronny Boch a and Daphne team 1 a Institut für Geologie und Paläontologie, Universität Innsbruck, Innrain 52, 6020 Innsbruck, Austria b Institut für Geographie, Universität Innsbruck, Innrain 52, 6020 Innsbruck, Austria c Patscher Straße 20, 6080 Innsbruck-Igls, Austria article info abstract Article history: Cave and lake isotope records from the circum-Mediterranean realm show anomalously low O isotope values Received 23 January 2009 suggesting high rainfall intensity during the time of sapropel 1 deposition (9.5 to 6.5 ka; all ages are given Accepted 2 October 2009 before the year AD 2000, i.e. b2k), coincident with an interval of conspicuously low sea-surface salinities in Available online 22 October 2009 the entire Mediterranean Sea. Speleothem data from Corchia Cave (Tuscany) currently provide the most precise terrestrial chronology and constrain the wettest interval to ca. 8.2 to 7.3 ka. We have traced this Keywords: Holocene isotopic signal to the north and observe a synchronous isotopic change in stalagmites from southalpine and Alps eastalpine caves, but in opposite direction. We attribute this to a shift in the local moisture balance, i.e. to a palaeoclimate higher proportion of moisture advected from the Mediterranean Sea relative to the otherwise dominant stable isotopes northwesterly air masses in the Alps. -
Good to Know
good to know 2017 Activity Report Hohe Tauern National Park www.hohetauern.at 1 Contents Photo: © HTNP / D. Egger Primula glutinosa: Many so-called Speik grounds in the Tauern mountains derive their name from this purple primrose. Primula glutinosa’s oblanceolate leaves with fine toothing near the tip are minutely glandular and sticky. The plant flowers among curved sedge grasses in July and August. It is endemic to the eastern Alps Publication details: and protected. (Source: Pflanzen. Wissenschaftliche Schriften. 2014. Secretariat of the Hohe Tauern National Park Council. Retailed through book stores: Tyrolia-Verlag) Media owner, editor, and publisher: Hohe Tauern National Park Fund, Carinthia Döllach 14, 9843 Grosskirchheim, Austria Hohe Tauern National Park Fund, Salzburg Gerlos Strasse 18, 5730 Mittersill, Austria Hohe Tauern National Park Fund, Tyrol Kirchplatz 2, 9971 Matrei in Osttirol, Austria Association of the Secretariat of the Hohe Tauern National Park Council Contents Kirchplatz 2, 9971 Matrei in Osttirol, Austria Editorial team and responsible for contents: National Park Directors Peter Rupitsch, Hermann Stotter, Wolfgang Urban Project management and co-ordination: Helene Mattersberger 4 Preface 47 Public Relations Cover picture: Zelokssee lake with views of the Hochschober © HTNP / A. Steinacher 6 Facts & Figures 48 Infrastructure Design: vorauerfriends communications gmbh, Thalheim 8 Looking Back 50 Tourism Graphic design: 08/16 grafik, eva scheidweiler, Lienz – Salzburg 14 National Parks Austria 54 Association of Friends Printed by: Oberdruck GmbH, Stribach 17 International Affairs 56 Organisation 18 Natural Resource Management 64 Budget 24 Science & Research 65 Outlook Translations: Stephen B. Grynwasser, London Publication details 32 Preservation of the Cultural Landscape 66 Contact Despite all due care and attention, misprints and printing errors cannot be excluded. -
Connecting Quartz Fluid Inclusion, Fissure Monazite Age, and Fissure
Gnos et al. Swiss J Geosci (2021) 114:14 https://doi.org/10.1186/s00015-021-00391-9 Swiss Journal of Geosciences ORIGINAL PAPER Open Access Episodes of fssure formation in the Alps: connecting quartz fuid inclusion, fssure monazite age, and fssure orientation data Edwin Gnos1* , Josef Mullis2, Emmanuelle Ricchi3, Christian A. Bergemann4, Emilie Janots5 and Alfons Berger6 Abstract Fluid assisted Alpine fssure-vein and cleft formation starts at prograde, peak or retrograde metamorphic conditions of 450–550 °C and 0.3–0.6 GPa and below, commonly at conditions of ductile to brittle rock deformation. Early-formed fssures become overprinted by subsequent deformation, locally leading to a reorientation. Deformation that follows fssure formation initiates a cycle of dissolution, dissolution/reprecipitation or new growth of fssure minerals enclos- ing fuid inclusions. Although fssures in upper greenschist and amphibolite facies rocks predominantly form under retrograde metamorphic conditions, this work confrms that the carbon dioxide fuid zone correlates with regions of highest grade Alpine metamorphism, suggesting carbon dioxide production by prograde devolatilization reac- tions and rock-bufering of the fssure-flling fuid. For this reason, fuid composition zones systematically change in metamorphosed and exhumed nappe stacks from diagenetic to amphibolite facies metamorphic rocks from saline fuids dominated by higher hydrocarbons, methane, water and carbon dioxide. Open fssures are in most cases oriented roughly perpendicular to the foliation and lineation of the host rock. The type of fuid constrains the habit of the very frequently crystallizing quartz crystals. Open fssures also form in association with more localized strike-slip faults and are oriented perpendicular to the faults. -
VRI-170. Grossenzersdorf, N.O. 6550 B.C. VRI.175. Rutzendorf, N.O
[RADIOCARBON, VOL. 13, No. 1, 1971, P. 126-134] VIENNA RADIUM INSTITUTE RADIOCARBON DATES II HEINZ FELBER Institut fur Radiumforschung and Kernphysik der Osterr, Akademie der Wissenschaften, Vienna, Austria Measurements have continued with the same proportional counter system, the same procedure in sample pretreatment, methane prepara- tion and measurement, and the same age calculation using a half-life of 5568 + 30 yr as described previously (R., 1970, v. 12, p. 298-318). Uncertainties quoted are single standard deviations originating from the statistical nature of radioactive decay including standard, sample, background, and half-life. No C13/C12 ratios were measured. The following list presents most samples of our work in the last year. Sample descriptions have been prepared in cooperation with sub- mitters. ACKNOWLEDGMENTS I have again to express many thanks to I. L. Stein for the excellent work in sample preparation and to E. Pak for the careful work in opera- tion of the dating equipment. SAMPLE DESCRIPTIONS I. GEOLOGY, GEOGRAPHY, SOIL SCIENCE, AND FORESTRY Austria 8500 ± 130 VRI-170. Grossenzersdorf, N.O. 6550 B.C. Oak wood, taken from depth 10 to 12 m below surface (154 m sea level) near Grossenzersdorf (48° 12' N Lat, 160 36' E Long), Lower Austria. Coll. 1969 and subm. by H. Bednar, Inst. f. Holzforschung, Hochschule f. Bodenkultur, Vienna. Comment (H.B.): dating necessary for biologic and technical analysis of wood. 7000 ± 160 VRI.175. Rutzendorf, N.O. 5050 B.C. Wood from layer of main stems of trees ca. 8 m below surface in gravel of river platform "Prater Terrasse" (Danube), Rutzendorf (48° 12' 16" N Lat, 16° 36' 38" E Long), Lower Austria, E of Vienna. -
9781852845681 (Short Code: 568) Publication Date: January 2010 Price: £15.00 Edition: First Author: Allan Hartley Pvc Encapsulated, 256 Pages 17.2Cm X 11.6Cm
TREKKING IN AUSTRIA'S HOHE TAUERN Venediger, Glockner and Reichen Groups ISBN: 9781852845681 (Short Code: 568) Publication Date: January 2010 Price: £15.00 Edition: First Author: Allan Hartley pvc Encapsulated, 256 pages 17.2cm x 11.6cm Situated in the heart of Austria and the Eastern Alps the Hohe Tauern National Park is the largest in Europe and a World Conservation Area, taking in the Tirol, Salzburg and Karnten. The area boasts dramatic valleys headed by scores of peaks and trekkers are well supported by some of the best huts in the Alps. The Park is centred on the Gross Glockner, at 3798m Austria-s highest mountain. Trekking in Austria's Hohe Tauern concentrates on three areas – the little known Reichen Group with its folklore of dwarves and giants, the Venediger Group with its glaciers and finally the Gross Glockner Group taking centre stage. Various hut-to-hut tours are described here, including the new Glockner Round that links seven huts together without having to cross glaciers. • 5 long-distance treks described, including a 10-day traverse across the whole area • alternatives, excursions and ascents of nearby peaks also suggested Key marketing points We can help you • ? Largest National Park in Europe, and a World Conservation Area • Select the best range • ? Five long-distance treks • Keep up to date with new titles • ? Includes Tyrol, Salzburg and Karnten and editions • Organise promotions About the author • Provide shelf display units, In addition to his first loves - Austria and the Alps - Allan Hartley has and spinners for larger ranges climbed across the globe from East Africa to the Falkland Islands, in Nepal • Arrange author talks and Pakistan, the Zagros mountains of Iran and the Hajr Mountains of the and support in-store events Arabian Peninsula. -
Der Tauernfleck-Blockgletscher Im Hollersbachtal
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Nationalpark Hohe Tauern - Wissenschaftliche Mitteilungen Nationalpark Hohe Tauern Jahr/Year: 1993 Band/Volume: 1 Autor(en)/Author(s): Lieb Gerhard Karl, Slupetzky Heinz Artikel/Article: Der Tauernfleck-Blockgletscher im Hollersbachtal (Venedigergruppe, Salzburg, Österreich) 138-146 © Nationalpark Hohe Tauern, download unter www.biologiezentrum.at Wissenschaftliche Mitteilungen aus dem Nationalpark Hohe Tauern _____________________ Bd. 1 (1993):138-146_____________________ Der Tauernfleck-Blockgletscher im Hollersbachtal (Venedigergruppe, Salzburg, Österreich) Gerhard Karl Lieb und Heinz Slupetzky 1 Zusammenfassung Nach allgemeinen Bemerkungen zum Phänomen der Blockgletscher und einigen Informationen über deren Verbreitung in den Hohen Tauern wird die Lage des Tauemfleck-Blockgletschers geomorpholo- gisch (Kar) und geoökologisch (subnivale Stufe) präsentiert. Auf Grund der Formenausstattung, des Bewuchses und der gemessenen Wassertemperaturen wird der Blockgletscher als inaktiv eingestuft. Seine Gesamtfläche beträgt etwa 0.15 km2, der untere Rand der Stirn liegt bei 2.360 m. 2 Summary The "Tauernfleck" rock glacier in the Hollersbach Valley (Venediger group, Salzburg, Austria) After some comments on rock glaciers in general and some informations about their distribution in the Hohe Tauern range the geomorphological (cirque) and geoecological position (subnival zone) of the "Tauernfleck" rock -
Lichenotheca Graecensis, Fasc
- 1 - Lichenotheca Graecensis, Fasc. 23 (Nos 441–480) Walter OBERMAYER* OBERMAYER Walter 2017: Lichenotheca Graecensis, Fasc. 23 (Nos 441– 480). - Fritschiana (Graz) 87: 1–13. - ISSN 1024-0306. Abstract: Fascicle 23 of 'Lichenotheca Graecensis' comprises 40 collections of lichens from the following countries (and ad- ministrative subdivisions): Albania, Australia (New South Wales; Norfolk Island; Queensland; Western Australia), Austria (Carin- thia; Salzburg; Styria; Upper Austria), Germany (Baden-Würt- temberg), Greece (Corfu Island), Spain (Mallorca), Switzerland (Canton of Jura), and U.S.A. (Alaska). Isotypes of Caloplaca dahlii, C. norfolkensis, and Trapeliopsis granulosa var. australis are distributed. TLC-analyses were carried out for Chrysothrix candelaris, Cladonia rei, Hypogymnia physodes (growing on ground), Hypotrachyna revoluta aggregate, Lepra albescens, Le- praria caesioalba, L. crassissima aggregate, Melanohalea exas- perata, Parmotrema arnoldii, Parmotrema reticulatum aggregate, Pycnora sorophora, Ramalina capitata, R. fraxinea, and Trapeli- opsis pseudogranulosa. *Institut für Pflanzenwissenschaften, NAWI Graz, Karl-Franzens- Universität, Holteigasse 6, 8010 Graz, AUSTRIA e-mail: [email protected] Introduction The exsiccata series 'Lichenotheca Graecensis' is distributed on exchange basis to the following 19 public herbaria and to one private collection (herbarium ab- breviations follow http://sweetgum.nybg.org/science/ih/): ASU, B, C, CANB, CANL, E, G, GZU, H, HAL, HMAS, LE, M, MAF, MIN, O, PRA, TNS, UPS, Klaus KALB. A pdf- file of the exsiccata is stored under https://static.uni-graz.at/fileadmin/ nawi- institute/Botanik/Fritschiana/fritschiana-87/lichenotheca-graecensis-23.pdf. A text version can be found under https://homepage.uni-graz.at/de/walter.obermayer/ publications/lichenotheca-graecensis-textfile-of-all-issues/. Label texts originally drafted in a local language have been translated into English by the author. -
36,000 Wood, Fragile Fragments of Oak; Depth 7M, Embedded in Sand Below Gravel in Subsoil Water
[RADIOCARBON, VOL. 17, No. 2, 1975, P. 247-254] VIENNA RADIUM INSTITUTE RADIOCARBON DATES VI HEINZ FELBER Institut fur Radiumforschung and Kernphysik der Osterr Akademie der Wissenschaften, Vienna, Austria Measurements have continued with the same proportional counter system, pretreatment procedure, methane preparation and measurement, and calculation, as described previously (R, 1970, v 12, p 298-318). Un- certainties quoted are single standard deviations originating from stan- dard, sample, background counting rates and half-life. No C13/C12 ratios were measured. The following list presents most samples of our work in the last year. Sample descriptions have been prepared in cooperation with submitters. ACKNOWLEDGMENTS I express many thanks to Ing L Stein for excellent work in sample preparation, and to A Rasocha for careful operation of the dating equip- ment. SAMPLE DESCRIPTIONS I. GEOLOGY, GEOGRAPHY, SOIL SCIENCE, AND FORESTRY A. Austria VRI.322. Wallern, Burgenland >36,000 Wood, fragile fragments of oak; depth 7m, embedded in sand below gravel in subsoil water. Seewinkel between Wallern (470 36' N, 16° 56' E) and Pamhagen, Burgenland. Coil 1971 by Fa Frank, well digger, in Frauenkirchen; subm by H Franz, Hochschule f Bodenkultur, Vienna. Glacier Pasterze series, Karnten Pressed sandy humus from fossil autochthonous soil below 1 to 2m ground moraine. Forefield of glacier Pasterze within lateral moraine from 1856, erosion groove of E Seebach rivulet (47° 03' 48" N, 12° 45' 22" E), Glockner-Group, Hohe Tauern, Carinthia. Site thawed ca 20 yr ago (Patzelt, 1969). Coil 1971 and subm by G Patzelt, Inst Meteorolog Geophys, Univ Innsbruck. General Comment (GP): samples date passage of advancing glacier over fossil soil. -
L Travel Across the Hohe Tauern Along the Route from the Gail Valley
L IUGS Subcomm. Silurian Stratigraphy. Field Meeting 1994: Bibl. Geol. B.-A.. 30/1994. Vienna Travel across the Hohe Tauern along the route from the Gail Valley to Lienz, Iselsberg, Heiligenblut, Hochtor, Bruck (GroGglockner Highway), Zell am See, Kitzbuhel, Kirchberg to Aschau. - A short geological route description. (figs. 17-23) (based on V. HOCK, F. KOLLER and R. SEEMANN 1994 and their figures)1 The Alps are generally subdivided into 4 major zones which from north to south have the following names (see fig. 17): 1. Helvetikum (Helvetic Zone or Unit) 2. Penninikum (Penninic Zone or Unit) 3. Ostalpin (Austroalpine Zone or Unit) 4. Sudalpin (Southalpine Zone or Unit) Distribution and style of deformation of these 4 tectonostratigraphic zones varies in the Alps. Unit 1-3 is thrust towards the north while the Southalpine unit is south directed. In addition, it is separated from the former by the distinct Periadriatic Fault. In comparison with the Western Alps in the Eastern Alps of Austria the Helvetic as well as the Penninic unit are markedly reduced. As far as the Hohe Tauern region is concerned it is surrounded by the overlying Austroalpine unit which forms a higher nappe upon the lowermost tectonic unit, i.e. the Penninic Unit (fig. 18). Due to Neogene uplifting and erosion the latter is exposed as a 120 km long and up to 60 km wide tectonic window - the so-called Tauern Window. In the introductory part of the excursion program the evolution of the Penninic Ocean between stable Europe and the northern promontory of the Adriatic plate was outlined. -
Lichenotheca Graecensis, Fasc
- 1 - Lichenotheca Graecensis, Fasc. 18–20 (Nos 341–400) Walter OBERMAYER* OBERMAYER W. 2011: Lichenotheca Graecensis, Fasc. 18–20 (Nos 341–400). - Fritschiana (Graz) 69: 1–16. - ISSN 1024-0306. Abstract: Fascicles 18, 19, and 20 of Lichenotheca Graecensis comprise 60 collections of lichens from the following countries (and administrative subdivisions): Australia (New South Wales; Victoria), Austria (Carinthia; Salzburg; Styria; Tirol; Upper Austria; Vienna), Canada (British Columbia; Québec), France (Rhône-Alpes), Germany (Baden-Württemberg; Saxony Anhalt), Italy (Emilia-Romagna; Trentino-Alto Adige; Veneto Region), Russia (Buryatia Republic), Slovenia, Switzerland (Valais), and Uruguay (Rio Negro). TLC-analyses were carried out for Alectoria sarmentosa, Buellia arborea, Chrysothrix candelaris, Cladonia fimbriata, Dimelaena oreina (partly chemotype Vb with hypostictic acid), Lecanora marginata, Lecidea atrobrunnea, Lecidea umbonata, Lepraria vouauxii, Protomicarea limosa, and Stereocaulon vesuvianum. Fertile material of rarely fruiting taxa like Alectoria sarmentosa, Candelariella reflexa, Hyperphyscia adglu- tinata, and Seirophora contortuplicata, as well as paratype specimens of Xanthoria coomae (Australia) are included. *Institut für Pflanzenwissenschaften, Karl-Franzens-Universität Graz, Holteigasse 6, 8010 Graz, AUSTRIA, e-mail: [email protected], homepage: http://www.uni-graz.at/walter.obermayer The exsiccata series 'Lichenotheca Graecensis' is distributed on exchange basis to the following 19 public herbaria and to one private collection (herbarium abbreviations follow http://sciweb.nybg.org/science2/IndexHerbariorum.asp): ASU, B, C, CANB, CANL, E, G, GZU, H, HAL, HMAS, LE, M, MAF, MIN, O, PRA, TNS, UPS, Klaus KALB. A text version of Lichenotheca Graecensis can be found under http://www.uni-graz.at/walter.obermayer/li-grz1.htm, a pdf-file is stored under http:// www.uni-graz.at/walter.obermayer/lichenotheca-graecensis-18-20.pdf. -
Abstracts & Field Guides
Berichte der Geologischen Bundesanstalt, 99 11th Workshop on Alpine Geological Studies & th 7 European Symposium on Fossil Algae Abstracts & Field Guides Schladming, Sept. 2013 Redaktion: Ralf Schuster Cover image: Sölk marble from the base of the Weiße Wand, Walchental (Styria, Austria) Impressum: ISSN 1017-8880 Alle Rechte für das In- und Ausland vorbehalten © Geologische Bundesanstalt (GBA) A-1030 Wien, Neulinggasse 38 www.geologie.ac.at Wien, September 2013 Medieninhaber, Herausgeber und Verleger: GBA, Wien Redaktion: Ralf Schuster (Geologische Bundesanstalt) Technische Redaktion; Christoph Janda (Geologische Bundesanstalt) Umschlag Monika Brüggemann-Ledolter Druck: Riegelnik, Offsetschnelldruck, Piaristengasse 19, A-1080 Wien Ziel der „Berichte der Geologischen Bundesanstalt“ ist die Verbreitung wissenschaftlicher Ergebnisse durch die Geologische Bundesanstalt. Die „Berichte der Geologischen Bundesanstalt“ sind im Handel nicht erhältlich. Berichte Geol. B.-A., 99 11th Workshop on Alpine Geological Studies & 7th IFAA Content Organisation & Time Schedule 4 Abstracts Emile Argand Conference (11th Workshop on Alpine Geological Studies) Editorial: Ralf Schuster 9 Abstracts 7th European Symposium on Fossil Algae Editorial: Sigrid Missoni & Hans-Jürgen Gawlick 107 Field guide: General Introduction in the Geology of the Easter Alps Ralf Schuster 121 Field guide Excursion A1: Southern Alps of Slovenia in a nutshell: paleogeography, tectonics, and active deformation Bogomir Celarc, Marko Vrabec, Boštjan Rožič, Polona Kralj, Petra Jamšek Rupnik, -
A Computacional Model to Predict Land-Use and Cover Changes in Mountain Landscapes Cristian Fondevilla Moreu
Nom/Logotip de la Universitat on s’ha llegit la tesi A computacional model to predict land-use and cover changes in mountain landscapes Cristian Fondevilla Moreu Dipòsit Legal: L.1696-2014 http://hdl.handle.net/10803/284853 ADVERTIMENT. L'accés als continguts d'aquesta tesi doctoral i la seva utilització ha de respectar els drets de la persona autora. Pot ser utilitzada per a consulta o estudi personal, així com en activitats o materials d'investigació i docència en els termes establerts a l'art. 32 del Text Refós de la Llei de Propietat Intel·lectual (RDL 1/1996). Per altres utilitzacions es requereix l'autorització prèvia i expressa de la persona autora. En qualsevol cas, en la utilització dels seus continguts caldrà indicar de forma clara el nom i cognoms de la persona autora i el títol de la tesi doctoral. No s'autoritza la seva reproducció o altres formes d'explotació efectuades amb finalitats de lucre ni la seva comunicació pública des d'un lloc aliè al servei TDX. Tampoc s'autoritza la presentació del seu contingut en una finestra o marc aliè a TDX (framing). Aquesta reserva de drets afecta tant als continguts de la tesi com als seus resums i índexs. ADVERTENCIA. El acceso a los contenidos de esta tesis doctoral y su utilización debe respetar los derechos de la persona autora. Puede ser utilizada para consulta o estudio personal, así como en actividades o materiales de investigación y docencia en los términos establecidos en el art. 32 del Texto Refundido de la Ley de Propiedad Intelectual (RDL 1/1996).