DOCSLIB.ORG

Ankogel Group Hochalmspitze 3360 M/Nmv 13

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Ankogel Group Hochalmspitze 3360 M/Nmv 13 ALMA MONS ADVENTURES Austrija – Ankogel Group Hochalmspitze 3360 m/nmv 13-15.08.2021. Hochalmspitze je najviša planina u masivu Ankogel grupe, u okviru nacionalnog parka Hohe Tauern, koja se nalazi u austrijskoj državi Koruška, iznad doline Maltatal. Ovaj vrh često zovui kraljicom parka Hohe Tauern, kao pandan kralju Grosglokneru. Vrh je formiran od granitnih stena, dok na istočnoj i južnoj strani ima glečere. Prvi zvanični uspon izvršio je austrijski planinar Paul Grohmann 1859. godine. VRSTA AKTIVNOSTI: VISOKOGORSTVO VREME I MESTO POLASKA: Novi Sad, petak, 13.08. u 14h od lokomotive kod Železničke stanice VREME I MESTO POVRATKA: Novi Sad, nedelja oko 00:00 h, lokomtiva kod Železničke stanice Petak - polazak iz Novog Sada u 14 časova. Vožnja auto putem kroz Hrvatsku i Sloveniju. Po ulasku u Sloveniju kod graničnog prelaza Bregana, pauza u Marcheu Obrežje. Put dalje nastavljamo prema Kranjskoj gori i mestu Ratače gde se smeštamo u planinarski dom. Očekivani dolazak u dom do 22 časa. Po dolasku u dom smeštaj u sobe, odlazak na spavanje. Subota - ustajanje u 07 časova. Nakon doručka i pakovanja opreme u 08 časova polazak prema austrijskom mestu Villach i nastavak puta prema dolini Maltatal, do parkirališta ispred akomulacione brane Goskarspeicher, koje je udaljeno 105 km. Pre dolaska na parkiralište obilazak slapa Fallbach, koji je najviši u Koruškoj. Očekivani dolazak na parking do 10 časova. Vozilo ostavljamo na parking prostoru i sa svom potrebnom opremom kredemo na stazu do planinarskog doma Gießener Hütte koji se nalazi na 2215 m, do kojeg je potrebno nešto manje od tri sata planinarskom stazom koja ide travnatim predelima, kroz borovu šumu sa visinskom razlikom od 660 m. Neposredno pre dolaska do doma, staza počinje da prelazi preko stenovitih delova. Po dolasku, smeštaj u dom. Ostatak vremena koristimo u pripremi opreme za sutrašnji završni uspon i šetnju oko doma. Odlazak na spavanje u 21 čas. Nedelja – ustanje u 04 časova. Polazak na stazu u 05 časova. Na uspon idemo kružnom stazom preko ferate Detmolder Grat do vrha, a potom se spuštamo do doma. Na ovom delu staza celim delom ide preko granitnih stena, potom ivicom glečera do izlaska na osigurani deo staze čeličnim sajlama. Sa vrha se spuštamo istočnim grebenom preko glečera Trippkees nazad do doma. Za prelazak kružne staze dužine oko 9 potrbno je od 10 do 12 sati hoda, sa visinskom razlikom od 1160 m. Po dolasku u dom odmor, pakovanje stvari i silazak do vozila. Polazak za Novi Sad u koji stižemo u ponedeljak u jutarnjim časovima. OPREMA : planinarski ranac do 40l, lična oprema za visokogorske uspone, planinarske duboke cipele, jakna za zaštitu od vetra, kapa, šešir ili marama, krema za zaštitu od sunca, rezervni veš, planinarski štapovi. Tehnička oprema: dereze, šlem, cepin, alpinistički pojas, četiri karabinera sa navrtkom, dva prusika 6-8 mm, dužine 3 m, ferrata set, rukavice, spravica za osiguranje, prusik za izradu čvora mašar d, jedna gurtna dužine 60-100 cm. INFORMACIJE I PRIJAVE: telefonom ili na mail adresu [email protected] Prilikom prijave dostaviti broj planinarske kartice i naziv planinarskog društva. Na akciji mogu učestvovati isključivo planinari koji su članovi osnovnih planinarskih organizacija učlanjenih u PSS. ORGANIZATOR AKCIJE: Planinarsko društvo Alma Mons Advenutres VODIČ: Siniša Carevid i Đorđe Veselinov, planinarski vodiči PSS MB 689 UIAA. Kontakt telefon 064/11-40-264 Vodič zadržava pravo da u skladu sa Pravilnikom o bezbednom izvoĎenju planinarskih aktivnosti, izmene plan u slučaju vanrednih okolnosti. POSTANITE DEO TIMA AVANTURA POČINJE SA NAMA! .
Load more

Recommended publications
  • 20 Years of Geodetic Monitoring of Dösen Rock Glacier (Ankogel Group, Austria): a Short Review
    Joannea Geol. Paläont. : 7-44 (06) 20 Years of Geodetic Monitoring of Dösen Rock Glacier (Ankogel Group, Austria): A Short Review 20 Jahre geodätischer Beobachtung am Dösener Blockgletscher (Ankogelgruppe, Österreich): Ein kurzer Überblick Viktor KAUFMANN Figures Abstract: This paper gives a condensed account of the geodetic measurements carried out at Dösen rock glacier during the last 0 years (995–05). The measurements were taken on an annual basis in order to determine the mean annual flow velocity of the rock glacier. The long-term monitoring program was interrupted only once, i. e. in 00. The geodetic network comprises 07 observation points located on the rock gla- cier (4 of which have been stabilized with brass bolts) and 7 stable reference points situated in the vicinity of the rock glacier. In 04 traditional surveying using a total station was replaced by satellite-based surveying (real-time kinematic - global naviga- tion satellite systems, RTK-GNSS). The flow velocities obtained reveal very well the kinematic behaviour of Dösen rock glacier over the course of time and are an excellent basis for subsequent climate change studies. The mean annual flow velocity of the fastest points varied between .0 and 5.6 cm/a during the observation period. The highest flow velocities (up to 65.9 cm/a) were recorded for 04–05, confirming the ongoing speed-up of this rock glacier. Zusammenfassung: Dieser Aufsatz gibt einen kurzen Überblick über die geodätischen Messungen, welche am Dösener Blockgletscher im Zeitraum 995–05, also über einen Zeitraum von 0 Jahren hinweg, getätigt wurden. Aus den jährlichen Messungen konnten mittlere jährliche Fließgeschwindigkeiten des Blockgletschers abgeleitet wer- den.
    [Show full text]
  • Final Report
    WP5–Action5.3–Finalreport Thermalandgeomorphicpermafrost responsetopresentandfutureclimate changeintheEuropeanAlps Editors: AndreasKellererͲPirklbauer,GerhardKarlLieb, PhilippeSchoeneich,PhilipDelineandPaoloPogliotti Graz,2011 WP5–Action5.3–Finalreport Thermalandgeomorphicpermafrost responsetopresentandfutureclimate changeintheEuropeanAlps Citationreference KellererͲPirklbauer A., Lieb G.K., Schoeneich P., Deline P., Pogliotti P. eds (2011). Thermal and geomorphic permafrost response to present and future climate change in the European Alps. PermaNETproject,finalreportofAction5.3.OnͲlinepublicationISBN978Ͳ2Ͳ903095Ͳ58Ͳ1,177pp. Downladableon:www.permanetͲalpinespace.eu Editors Andreas KellererͲPirklbauer and Gerhard Karl Lieb, Institute of Geography and Regional Science, UniversityofGraz,Austria(IGRS) PhilippeSchoeneich,InstitutdeGéographieAlpine,UniversitédeGrenoble,France(IGAͲPACTE) PhilipDeline,EDYTEM,UniversitédeSavoie,France(EDYTEM) PaoloPogliotti,Regional AgencyfortheEnvironmentalProtectionoftheAostaValley,Italy(ARPA VdA) Projectreference The PermaNET – Permafrost long term monitoring network (2008Ͳ2011) project is part of the EuropeanTerritorialCooperationandcoͲfundedbytheEuropeanRegionalDevelopmentFund(ERDF) inthescopeoftheAlpineSpaceProgrammewww.alpineͲspace.eu PermaNET–Permafrostresponsetoclimatechange Authors Baroni,Carlo UniversityofPisa(Italy) Bodin,Xavier UniversityJosephFourier,Grenoble(France) Cagnati,Anselmo RegionalAgencyfortheEnvironmentalProtectionofVeneto(Italy) Carollo,Federico E.P.C.EuropeanProjectConsultingS.r.l.(Italy)
    [Show full text]
  • The Dösen Rock Glacier in Central Austria: a Key Site for Multidisciplinary Long-Term Rock Glacier Monitoring in the Eastern Alps______
    Austrian Journal of Earth Sciences Vienna 2017 Volume 110/2 xxx - xxx DOI: 10.17738/ajes.2017.0013 The Dösen Rock Glacier in Central Austria: A key site for multidisciplinary long-term rock glacier monitoring in the Eastern Alps_________________ Andreas KELLERER-PIRKLBAUER1)*), Gerhard Karl LIEB1), & Viktor KAUFMANN2) 1) Department of Geography and Regional Science, Working Group Alpine Landscape Dynamics (ALADYN), University of Graz, Heinrichstrasse 36, 8010 Graz, Austria; 2) Institute of Geodesy, Working Group Remote Sensing and Photogrammetry, Graz University of Technology, Steyrergasse 30, 8010 Graz, Austria; *) Corresponding author, [email protected] KEYWORDS rock glacier; monitoring; flow velocity; geophysics; ground temperature; Dösen Valley Abstract Rock glaciers are distinct landforms in high mountain environments indicating present or past permafrost conditions. Active rock glaciers contain permafrost and creep slowly downslope often forming typical flow structures with ridges and furrows related to compressional forces. Rock glaciers are widespread landforms in the Austrian Alps (c. 4600). Despite the high number of rock gla- ciers in Austria, only few of them have been studied in detail in the past. One of the best studied ones is the 950 m long Dösen Rock Glacier located in the Hohe Tauern Range. This rock glacier has been investigated since 1993 using a whole suite of field- based and remote sensing-based methods. Research focused on permafrost conditions and distribution, surface kinematics, inter- nal structure and possible age of the landform. Results indicate significant ground surface warming of the rock glacier body du- ring the period 2007-2015 accompanied by a general acceleration of the rock glacier surface flow velocity (max.
    [Show full text]
  • Nota Lepidopterologica
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Nota lepidopterologica Jahr/Year: 2010 Band/Volume: 33 Autor(en)/Author(s): Cupedo Frans Artikel/Article: A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) 85-106 ©Societas Europaea Lepidopterologica; download unter http://www.biodiversitylibrary.org/ und www.zobodat.at Nota lepid.33 (1): 85-106 85 A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) Frans Cupedo Processieweg 2, NL-6243 BB Geulle, Netherlands; [email protected] Abstract. A systematic analysis of the geographic variation of both valve shape and wing pattern reveals that the subspecies ofErebia euryale can be clustered into three groups, characterised by their valve shape. The adyte-group comprises the Alpine ssp. adyte and the Apenninian brutiorum, the euryale-group in- cludes the Alpine subspecies isarica and ocellaris, and all remaining extra- Alpine occurrences. The third group (kunz/-group), not recognised hitherto, is confined to a restricted, entirely Italian, part of the south- ern Alps. It comprises two subspecies: ssp. pseudoadyte (ssp. n.), hardly distinguishable from ssp. adyte by its wing pattern, and ssp. kunzi, strongly melanistic and even exceeding ssp. ocellaris in this respect. The ssp. pseudoadyte territory is surrounded by the valleys of the rivers Adda, Rio Trafoi and Adige, and ssp. kunzi inhabits the eastern Venetian pre-Alps, the Feltre Alps and the Pale di San Martino. The interven- ing region (the western Venetian pre-Alps, the Cima d'Asta group and the Lagorai chain) is inhabited by intermediate populations.
    [Show full text]
  • Dupla Graecensia Lichenum (2020, Numbers 1191–1290)
    - 1 - Dupla Graecensia Lichenum (2020, numbers 1191–1290) Walter OBERMAYER* OBERMAYER W. 2020: Dupla Graecensia Lichenum (2020, numbers 1191–1290). - Fritschiana (Graz) 96: 1–28. - ISSN 1024-0306. Abstract: The exsiccata 'Dupla Graecensia Lichenum (2020, numbers 1191–1290)' comprises 100 collections (747 specimens) of lichen dupli- cates from the following 18 countries: Albania (district of Shkodër), Australia (state of Queensland), Austria (states of Carinthia, Salzburg, Styria, Tyrol, Upper Austria, and Vorarlberg), Brazil (states of Mato Grosso and Mato Grosso do Sul), Canada (territory of Nunavut), China (Tibet, province Xizang), Croatia (island of Košljun), Czech Republic (North Bohemia and South Bohemia), Greece (islands of Corfu and Rhodes), Italy (region of Veneto and autonomous region of Trentino - Alto Adige), Nepal, New Zea- land (South Island), Portugal (Madeira Island), Slovenia, Spain (Canary Islands), Switzerland (canton of Bern), Thailand (province of Chumphon), and Venezuela (state of Merida). Isotype specimens of Buellia maun- gatuensis are distributed. TLC-investigations were carried out for 40 issued taxa. * University of Graz, Institute of Biology, Division of Plant Sciences, NAWI Graz, Holteigasse 6, 8010 Graz, AUSTRIA e-mail: [email protected] Introduction The dwarf-exsiccata 'Dupla Graecensia Lichenum' is issued by the herbarium of the Institute of Biology (botany section) of the Karl-Franzens-University, Graz, Austria (international herbarium acronym: GZU). It includes lichens (and sometimes lichenicolous fungi) from all over the world with at least five duplicates of each collection. Each institution receiving a duplicate is cited (at the bottom line of each individual label) with its international herbarium acronym: The herbaria in Canberra (CANB), Graz (GZU), Munich (M), New York (NY), and Uppsala (UPS) are receiving specimens of all distributed numbers continuously.
    [Show full text]
  • Najwyższe Szczyty Austrii
    Najwyższe szczyty Austrii Height Prominence Rank Mountain Range Prominence point (m) (m) Glockner 1 Großglockner 3798 Group 2428 Brenner Pass Hohe Tauern Ötztal Alps 2 Wildspitze 3770 2263 Reschen Pass Weißkamm Ötztal Alps 3 Weißkugel 3739 569 Langtauferer Joch Weißkamm Venediger 4 Großvenediger 3666 Group 1185 Felbertauern Hohe Tauern Ötztal Alps 5 Hintere Schwärze 3628 838 Hochjoch Maine Ridge Ötztal Alps 6 Hinterer Brochkogel 3628 160 Mitterkarjoch Weißkamm Ötztal Alps 7 Similaun 3599 261 Similaunjoch Maine Ridge Ötztal Alps 8 Vorderer Brochkogel 3565 165 Vernagtjoch Weißkamm Glockner 9 Großes Wiesbachhorn 3564 Group 481 Gruberscharte Hohe Tauern Venediger 10 Rainerhorn 3559 Group 153 Rainertörl Hohe Tauern Ötztal Alps 11 Großer Ramolkogel 3550 380 Fanatjoch Maine Ridge Ötztal Alps 12 Schalfkogel 3540 351 Ramoljoch Maine Ridge Ötztal Alps 13 Hochvernagtspitze 3535 299 Taschachjoch Weißkamm Ötztal Alps 14 Watzespitze 3533 489 Ölgrubenjoch Kaunergrat Ötztal Alps 15 Langtauferer Spitze 3529 173 Weißkugeljoch Weißkamm Ötztal Alps 16 Weißseespitze 3518 350 Gepatschferner Weißkamm Ötztal Alps 17 Fineilspitze 3514 504 Niederjoch Maine Ridge Height Prominence Rank Mountain Range Prominence point (m) (m) Zillertal 18 Hochfeiler 3510 Alps 982 East of Hörndljoch Main ridge 19 Zuckerhütl 3507 Stubai Alps 1033 Timmelsjoch Venediger 20 Dreiherrnspitze 3499 Group 581 Obersulzbachtörl Hohe Tauern Eissatel (N of 21 Schrankogel 3497 Stubai Alps 523 Hinterer Daunkopf) Ötztal Alps 22 Fluchtkogel 3497 256 Gepatschjoch Weißkamm Venediger 23 Rötspitze 3496
    [Show full text]
  • Military Mountain Training
    Federal Ministry of Defence and Sports S92011/27-Vor/2014 Supply No. 7610-10147-0714 Manual No. 1002.09 Austrian Armed Forces Field Manual (For Trial) Military Mountain Training Vienna, July 2014 Approval and Publishing Austrian Armed Forces Field Manual (for trial) Military Mountain Training Effective as of 1st December 2014 This Field Manual replaces the “Mountain Operations” Field Manual, parts I – IV, Supply number 7610-10133-0808 Approved: Vienna, 8th July 2014 For the Minister of Defence and Sports (COMMENDA, General) 2 Approval and Publication Austrian Armed Forces Field Manual (For Trial) Military Mountain Training Responsible for the Contents: SALZBURG, 27th June 2014 Chief, Air Staff, Austrian Joint Forces Command (GRUBER, BG) SAALFELDEN, 27th June 2014 Cdr (acting), Mountain Warfare Centre: (RODEWALD, Colonel) 3 PREFACE This Field Manual (FM) for trial (f.t.) serves as a basis for the training and application of mountaineering techniques within the Austrian Armed Forces (AAF) and will be distributed to the units in need of it. It is to be seen as the predecessor of the final version of the same-titled AAF FM, which will be published after the testing phase of this manual. The present FM (f.t.) was developed in cooperation with the German Bundeswehr (Bw) in order to ensure standardized training. In the Bw it is called C2-227/0-0-1550 “Gebirgsausbildung”. This FM (f.t.) is meant to provide knowledge and skills on: - geographical, geological, meteorological, and common basics for military operations in mountainous terrain, - safe and secure movements and survival in mountainous and high mountain regions, – mountain rescue, and – mountaineering equipment, which are preconditions for the accomplishment of military tasks.
    [Show full text]
  • Apatite Fission-Track Evidence for Postmetamorphic Uplift
    ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Jb. Geol. B.-A. ISSN 0016-7800 Band 130 Heft 4 S.571-586 Wien, Dezember 1987 Apatite Fission-Track Evidence for Postmetamorphic Uplift and Cooling History of the Eastern Tauern Window and the Surrounding Austroalpine (Central Eastern Alps, Austria) By HEINZ STAUFENBERG*) With 10 Figures and 1 Table Ostalpen Austroalpin Penninikum Tauernfenster Tauernkristallisalion Radiometrische Altersbeslimmungen Apalit-Spa Itspu ren-A Iter Hebungsraten Abkühlungsgeschichte Contents Zusammenfassung , , ,...... 571 1. I~~;~~ac~:o~'a~d' P~~bl~;'" : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : ~i~ 2. Sampling and Experimental Methods .. , , , , , 574 3. Results . , , , , , , , . , 574 4. Discussion ., , , , " 581 5. ~~~~~u.:li~~~e~~~is' : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : ~:~ References , , " , , , , . , , 585 Zusammenfassung Die Abkühlungsgeschwindigkeiten der Gesteinsserien des Mit Hilfe von 62 Apatit-Spaltspurendatierungen wurde die Tauernpenninikums und des ostalpinen Alkristallins liegen im nach dem Abklingen der spätalpinen Regionalmetamorphose Niedertemperaturbereich (von 100°C bis zur heutigen Oberflä- (Tauernkristallisation) fortschreitende Hebung und Abkühlung chentemperatur) zwischen ca. 4 und 9°e/Ma. des östlichen Tauernfensters und seiner ostalpinen Umrah- Mit Ausnahme
    [Show full text]
  • A New Glacier Inventory for the European Alps from Landsat TM Scenes of 2003: Challenges and Results
    Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2011 A new glacier inventory for the European Alps from Landsat TM scenes of 2003: challenges and results Paul, F ; Frey, H ; Le Bris, R Abstract: Meltwater from glaciers in the European Alps plays an important role in hydropower produc- tion, and future glacier development is thus of economic interest. However, an up-to-date and alpine-wide inventory for accurate assessment of glacier changes or modelling of future glacier development has not hitherto been available. Here we present a new alpine-wide inventory (covering Austria, France, Italy and Switzerland) derived from ten Landsat Thematic Mapper (TM) scenes acquired within 7 weeks in 2003. Combined with the globally available digital elevation model from the Shuttle Radar Topography Mission, topographic inventory parameters were derived for each of the 3770 mapped glaciers, covering 2050km2. The area-class frequency distribution is very similar in all countries, and a mean northerly aspect (NW, N, NE) is clearly favoured (arithmetic counting). Mean glacier elevation is ฀2900 m, with a small dependence on aspect. The total area loss since the previous glacier inventory (acquired around 1970 ±15 years) is roughly one-third, yielding a current area loss rate of ฀2%a–1. Digital overlay of the outlines from the latest Austrian glacier inventory revealed differences in the interpretation of glacier extents that prohibit change assessment. A comparison of TM- derived outlines with manually digitized extents on a high-resolution IKONOS image returned 1.5% smaller glaciers with TM.
    [Show full text]
  • Der Dösener Blockgletscher - Studienkarten Und Bewegungsmessungen 141-162 ARBEITEN AUS DEM INSTITUT FÜR GEOGRAPHIE Band 33 DER KARL-FRANZENS-UNIVERSITÄT GRAZ S
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Arbeiten aus dem Institut für Geographie der Karl- Franzens-Universität Graz Jahr/Year: 1996 Band/Volume: 33_1996 Autor(en)/Author(s): Kaufmann Viktor Artikel/Article: Der Dösener Blockgletscher - Studienkarten und Bewegungsmessungen 141-162 ARBEITEN AUS DEM INSTITUT FÜR GEOGRAPHIE Band 33 DER KARL-FRANZENS-UNIVERSITÄT GRAZ S. 141-162 Beiträge zur Permafrostforschung in Österreich Graz 1996 Der Dösener Blockgletscher - Studienkarten und Bewegungsmessungen von Viktor Kaufmann , Graz mit 6 Abbildungen und 3 Tabellen im Text sowie 5 Kartenbeilagen Zusammenfassung In diesem Beitrag werden erstmals die Ergebnisse von geodätischen und kartographischen Arbeiten über den Dösener Blockgletscher (Dösener Tal, Ankogelgruppe, Kärnten, Lage siehe Luftbildkarte 1:10 000 in diesem Band) dargestellt. Weiters wird ein Überblick über die bisherige Blockgletschervermessung in Österreich gegeben, wobei für den Blockgletscher im Äußeren Hochebenkar (Gurgier Tal, Ötztaler Alpen, Tirol, Lage siehe Lieb 1996: Abb. 1, in diesem Band) die jüngsten Meßergebnisse mitgeteilt werden. Der Äußere Hochebenkar-Blockgletscher ist der in Österreich am zeitlich längsten und am besten beobachtete Blockgletscher. Er nimmt jedoch aufgrund seiner durch die Topographie stark beeinflußten Fließbewegung eine Sonderstellung ein. In Erweiterung des geodätischen und photogrammetrischen Beobachtungsprogrammes für Blockgletscher in Österreich wurde der Dösener Blockgletscher als neues Studienobjekt eingebunden. Die geomorphometrische Studienkarte 1:5000 „Inneres Dösener Tal“ war der Ausgangspunkt für weitere geodätische und kartographische Aktivitäten. Die kartographische Palette umfaßt eine Stereoorthophotokarte 1:30 000, zwei kombinierte Bild-Strichkarten im Maßstab 1:10 000, eine Detailkarte des Dösener Blockgletschers im Maßstab 1:5000, sowie eine thematische Karte der Fließbewegungen am Dösener Blockgletscher im Maßstab 1:5000.
    [Show full text]
  • Permafrost Research in Austria: History and Recent Advances
    Austrian Journal of Earth Sciences Volume 105/2 Vienna 2012 Permafrost Research in Austria: History and recent advances Karl KRAINER1), Andreas KELLERER-PIRKLBAUER2)3), Viktor KAUFMANN3), Gerhard Karl LIEB4), Lothar SCHROTT5) & Helmut HAUSMANN6)7) 1) Institute of Geology and Paleontology, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria; 2) Institute for Earth Sciences, University of Graz, Heinrichstrasse 26, 8010 Graz, Austria; 3) Institute of Remote Sensing and Photogrammetry, Graz University of Technology, Steyrergasse 30, 8010 Graz, Austria; 4) Institute of Geography and Regional Science, University of Graz, Heinrichstrasse 36, 8010 Graz, Austria; 5) Department of Geography and Geology, University of Salzburg, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; 6) Central Institute for Meteorology and Geodynamics/ZAMG, Hohe Warte 38, A-1190 Vienna, Austria; 7) Institute of Geodesy and Geophysics, Vienna University of Technology, Vienna, Austria; Abstract In the Austrian Alps the study of alpine permafrost started during the 1920ies and until about 1980 was mainly concentrated on rock glaciers. Since 1980 the number of publications related to permafrost increased and since the late 1990ies investigation of permafrost has been intensified. This introductory article provides an overview on the history of permafrost research in the Austrian Alps, on current activities including new results and a short outlook for the next years.____________________________________ Current research includes the distribution of rock glaciers and
    [Show full text]
  • The Origin of Hollow Tubes in Alpine Quartz Crystals
    3rd Symposion©Hohe Tauern National ofthe Park; downloadHohe unterTauern www.biologiezentrum.at National Park Conference Volume for Research in Protected Areas pages 245-249 ___________________________ September 15th to 17th, 2005, Castle of Kaprun___________________________ The origin of hollow tubes in Alpine quartz crystals Franz Walter, Karl Ettinger Abstract Needle-like hollow tubes penetrating quartz crystals are a particular inclusion phenomenon of Alpine mineral parageneses. From several locations of the Eastern Alps samples of quartz crystals with hollow tubes were investigated to find the previous mineral forming the tubes. In four samples solid inclusions showing the same crystal morphology like the hollow tubes were identified by X-ray and microprobe as anhydrite, CaS04. The formation and dissolution of anhydrite in the hydrothermal system of Alpine clefts is discussed. Keywords Hollow tubes, quartz, Alpine clefts, anhydrite, Carinthia, Salzburg. Projects: „Mineral documentation ofthe National Park Hohe Tauern": Nr. 21303-68/112-2003; areas Rauris and Stubachtal, Salzburg: duration 2003-2008. Nr. 3RO-ALLG-231/2-2003 area Ankogelgruppe, Zirknitztäler, Carinthia: duration 2003-2008. Project aims: Mineralogical investigations of Alpine mineral parageneses. Introduction The study of inclusions in minerals may reveal important informations about the history of mineral formation. Fluid inclusions are by far the most frequent in quartz and may contain liquids (H20, C 02, heavy hydrocarbons), gas phases (H20, C 02, CH4 and N2) and in saturated saline solutions also solids as for example NaCI and KCl. Their analyses point to the composition of the original liquid from which the quartz crystal was formed. Solid inclusions (minerals) in quartz are characterised as protogenetic (formed before the host quartz), syngenetic (formed at the same time) and epigenetic (formed after deposition ofthe host crystal).
    [Show full text]