Prealpine Plant Species Polygala Chamaebuxus
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Present-Day Uplift of the European Alps Evaluating Mechanisms And
Earth-Science Reviews 190 (2019) 589–604 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Invited review Present-day uplift of the European Alps: Evaluating mechanisms and models T of their relative contributions ⁎ Pietro Sternaia, ,1, Christian Sueb, Laurent Hussonc, Enrico Serpellonid, Thorsten W. Beckere, Sean D. Willettf, Claudio Faccennag, Andrea Di Giulioh, Giorgio Spadai, Laurent Jolivetj, Pierre Vallac,k, Carole Petitl, Jean-Mathieu Nocquetm, Andrea Walpersdorfc, Sébastien Castelltorta a Département de Sciences de la Terre, Université de Genève, Geneva, Switzerland b Chrono-Environnement, CNRS, Université de Bourgogne Franche-Comté, Besançon, France c Université Grenoble Alpes, CNRS, IRD, IFSTAR, ISTERRE, Université Savoie Mont Blanc, Grenoble 38000, France d Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Bologna, Italy e Institute for Geophysics, Department of Geological Sciences, Jackson School of Geosciences, The University Texas at Austin, Austin, TX, USA f Erdwissenschaften, Eidgenössische Technische Hochschule Zürich (ETH), Zurich, Switzerland g Dipartimento di Scienze, Università di Roma III, Rome, Italy h Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Pavia, Italy i Università degli Studi di Urbino “Carlo Bo”, Urbino, Italy j Sorbonne Université, Paris, France k Institute of Geological Sciences, Oeschger Center for Climate Research, University of Bern, Switzerland l Geoazur, IRD, Observatoire de la Côte d'Azur, CNRS, Université de Nice Sophia-Antipolis, Valbonne, France m Institut de Physique du Globe de Paris, Paris, France ARTICLE INFO ABSTRACT Keywords: Recent measurements of surface vertical displacements of the European Alps show a correlation between vertical European Alps velocities and topographic features, with widespread uplift at rates of up to ~2–2.5 mm/a in the North-Western Vertical displacement rate and Central Alps, and ~1 mm/a across a continuous region from the Eastern to the South-Western Alps. -
Maps of Aegidius Tschudi
146 The Alpin~ Maps of Aegidius Tschudi. We arrived at 4.30 at the tents and after hot drinks soon recovered our strength. Also Kesar's eyesight became normal again. At 7.30 we arrived down at Camp I, evacuated everything to the Base Camp on 22nd, and on 27th arrived at Tapoban. p ACHMARHI, INDIA, C.P. 2-10-33. DEAR DocTOR LoNGSTAFF, The mistake about times was due to my carelessness in the account I sent you. I suppose I did not look it through with thoroughness. The actual times were these: Left Camp II (ca. 19,000 ft.) . 7.45 A.M. At the site we meant to have Camp III (about 11.15 , 21,000 ft.) 11.30 " Summit 2.45 P.M. • • • • • • • • 2.52 " ' Camp III ' (ca. 21,000 ft.) . 4.30 " • . 5.00 '' Camp II . • • • . .. 6.00 " ' Camp I (ca. 17,000 ft.) • • . 7.30 '' This gives my times: Of. [T. G. L.] ' A.J.' 24, 120 : Up: 4500 ft. in 7 hrs. 6000 ft. in 10 hrs. 650 ft. per hour. 600 ft. per hr. Down : 6500 ft. in 4! hrs. 7000 ft. in 3 hrs. 1440 ft. per hour. 2333 ft. per hr. These times are incI uding rests. Ditto. p. R. OLIVER . • [Lieut. Oliver followed our 1907 route except perhaps at the commencement. There is no doubt at all that he attained the summit, which is the first (N.) . small flattish dome : the very slightly lower and corniched S. top, across a small gap, would have been invisible in such weather. -
Climatotherapy and Medical Effects at High Altitude Sulden
Climatotherapy and medical eff ects at high altitude Sulden am Ortler 1 Contents The Sulden Study 4 Sulden is precious 6 The fountain of youth effect 7 Gushing source of life 8 Fit, slim and healthy 9 Height training 10 Best stimulating climate 11 Testimonials 12, 13 Environmental contribution from Sulden 14 Project description 2010-2011 Setting of location and project development with Prof DDr. A. Schuh 2012 Concept development of a study on the medical effect of high-altitude locations 2013-2014 Implementation of a pilot study, evaluation and publication of the results The project „Climatotherapy and medical effects in high-altitude locations - Sulden am Ortler“, fascicle number 2/308/2010, was supported by • the Unione europea - Fondo sociale europeo, • the Ministero del lavoro e delle Politiche Sociali and • the Ufficio sociale europeo - Provincia autonoma di Bolzano. www.puremountainsulden.com © Vinschgau Marketing/Frieder Blickle, Ferienregion Ortler/Frieder Blickle 2 3 „A healthy metabolism in Sulden“ Univ. Prof. Dr. Christian Wiedermann The Sulden study Head of the Academic Leptin and triglyceride levels in the blood of people with metabolic Teaching Department for Internal Medicine syndrome: results of a comparative pilot study on a 2-week hiking holiday of Innsbruck Medical at 1,900m or 300m above sea level. University at Bolzano A slight decrease in the oxygen concentration in breathing air Central Hospital possibly strengthens the health-promoting effect of physical exercise for the reduction of risk factors for heart attack and stroke. In autumn 2013, a pilot study was conducted with the purpose of investigating the impact of a 2-week hiking holiday on typical risk factors measurable in the blood in people with metabolic syndrome, whereby exactly the same exercise programme at a low altitude (300m) was compared with training at altitude (Sulden, 1900m). -
The Supreme Discipline of Mountaineering
The Supreme Discipline of Mountaineering To what heaven would it lead me to climb a mountain that flew? Christoph Ransmayr, “The Flying Mountain” MMM Corones on Kronplatz – between the Gader Valley, Olang and the Puster Valley – is the final act in the Messner Mountain Museum project (which comprises a total of six facilities). On the edge of South Tyrol’s mountain plateau with the most spectacular views, in the unique museum architecture created by Zaha Hadid, I present the crowning of traditional mountaineering. Kronplatz offers views beyond the borders of South Tyrol to all points of the compass: from the Lienz Dolomites in the east to the Ortler in the west, from the Marmolada in the south to the Zillertal Alps in the north. The museum is a mirror of the world of my childhood - the Geislerspitzen, the central buttress of the Heiligkreuzkofel (the most difficult climb in my whole life) and the glaciated granite mountains of the Ahrn Valley. On Kronplatz I present the development of modern mountaineering and 250 years of progress with regard to the equipment. I speak of triumphs and tragedies on the world’s most famous peaks – the Matterhorn, Cerro Torre, K2 – and the depiction of our activity, however contradictory it may seem. As in my other museums, I shed light on alpinism with the help of relics, thoughts, works of art (pictures and sculptures) and by reflecting the outside mountain backcloth in the interior of MMM Corones. As the storyteller of traditional mountaineering, it is not my intention to judge or dramatise but simply to condense human experience of a world that is my world, of the 250-year-old contest between man and the mountain. -
In Memoriam 115
IN MEMORIAM 115 • IN MEMORIAM CLAUDE WILSON 1860-1937 THE death of Claude Wilson within a few weeks of attaining his seventy-seventh birthday came as a terrible shock to his many friends. Few of us even knew that he was ill, but in the manner of his passing none can regret that there was no lingering illness. We can but quote his own words in Lord Conway's obituary: 'the best we can wish for those that we love is that they may be spared prolonged and hopeless ill health.' His brain remained clear up to the last twenty-four hours and he suffered no pain. The end occurred on October 31. With Claude Wilson's death an epoch of mountaineering comes to an end. He was of those who made guideless and Alpine history from Montenvers in the early 'nineties, of whom but Collie, Kesteven, Bradby, ~olly and Charles Pasteur still survive. That school, in which Mummery and Morse were perhaps the most prominent examples, was not composed of specialists. Its members had learnt their craft under the best Valais and Oberland guides; they were equally-proficient on rocks or on snow. It mattered little who was acting as leader in the ascent or last man in the descent. They were prepared to turn back if conditions or weather proved unfavourable. They took chances as all mountaineers are forced to do at times but no fatal accidents, no unfortunate incidents, marred that great page of Alpine history, a page not confined to Mont Blanc alone but distributed throughout the Western Alps. -
The Eastern Alps: Result of a Two-Stage Collision Process
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Mil. Cteto-r. Goo GOG. ISSN 02hl 7-193 92 11999; 117 13-1 Wen Jui 2000 The Eastern Alps: Result of a two-stage collision process FRANZ NEUBAUER1, JOHANN GENSER1, ROBERT HANDLER1 8 Figures Abstract The present structure and the Late Paleozoic to Recent geological evolution of the Alps are reviewed mainly with respect to the distribution of Alpidic, metamorphic overprints of Cretaceous and Tertiary age and the corresponding ductile structure. According to these data, the Alps as a whole, and the Eastern Alps in particular, are the result of two independent Alpidic collisional orogenies: The Cretaceous orogeny formed the present Austroaipine units sensu lato (extending from bottom to top of the Austroaipine unit s. str., the Meliata unit, and the Upper Juvavic unit) including a very low- to eclogite-grade metamorphic overprint. The Eocene-Oligocene orogeny resulted from an oblique continent-continent collision and overriding of the stable European continental lithosphere by the combined Austroalpine/Adriatic continental microplate. A fundamental difference seen in the present-day structure of the Eastern and Central/ Western Alps resulted as the Austroaipine units with a pronounced remnants of a Oligocene/Neogene relief are mainly exposed in the Eastern Alps, in contrast to the Central/Western Alps with Penninic units, which have been metamorphosed during Oligocene. Exhumation of metamorphic crust, formed during Cretaceous and Tertiary orogenies, arose from several processes including subvertical extrusion due to lithospheric indentation, tectonic unroofing and erosional denudation. Original paleogeographic relationships were destroyed and veiled by late Cretaceous sinistral shear, Oligocene-Miocene sinistral wrenching along ENE-trending faults within eastern Austroaipine units and the subsequent eastward lateral escape of units exposed within the central axis of the Alps. -
Ivrea Mantle Wedge, Arc of the Western Alps, and Kinematic Evolution of the Alps–Apennines Orogenic System
Swiss J Geosci DOI 10.1007/s00015-016-0237-0 Ivrea mantle wedge, arc of the Western Alps, and kinematic evolution of the Alps–Apennines orogenic system 1 1 1 2 Stefan M. Schmid • Eduard Kissling • Tobias Diehl • Douwe J. J. van Hinsbergen • Giancarlo Molli3 Received: 6 June 2016 / Accepted: 9 December 2016 Ó Swiss Geological Society 2017 Abstract The construction of five crustal-scale profiles related to the lateral indentation of the Ivrea mantle slice across the Western Alps and the Ivrea mantle wedge towards WNW by some 100–150 km. (4) The final stage of integrates up-to-date geological and geophysical informa- arc formation (25–0 Ma) is associated with orogeny in the tion and reveals important along strike changes in the Apennines leading to oroclinal bending in the southern- overall structure of the crust of the Western Alpine arc. most Western Alps in connection with the 50° counter- Tectonic analysis of the profiles, together with a review of clockwise rotation of the Corsica-Sardinia block and the the existing literature allows for proposing the following Ligurian Alps. Analysis of existing literature data on the multistage evolution of the arc of the Western Alps: (1) Alps–Apennines transition zone reveals that substantial exhumation of the mantle beneath the Ivrea Zone to shal- parts of the Northern Apennines formerly suffered Alpine- low crustal depths during Mesozoic is a prerequisite for the type shortening associated with an E-dipping Alpine sub- formation of a strong Ivrea mantle wedge whose strength duction zone and were backthrusted to the NE during exceeds that of surrounding mostly quartz-bearing units, Apenninic orogeny that commences in the Oligocene. -
ALPINE NOTES. Date of the ALPINE CLUB OBITUARY: Election
Alpine Notes . 381 The Triglav 'N. Face' is between 700 and 800 rrL high in t hat portion traversed by the ' Jug' route, and for the first three parts of the route it is almost sheer. Great smooth slabs, occurring in successive series, constitute the special and characteristic difficulty. The climb occupied 16 hours in all. F . S. C. ALPINE NOTES. Date of THE ALPINE CLUB OBITUARY: Election Allport, D . W. • • • • • • • 1875 Colgrove, J. B . • • • • • • • 1876 Morse, Sir George H. • • • • • • 1887 Holmes, .Alfred • • • • • • • 1894 Shea, C. E .. • • • • • • • 1896 Nicholson, L. D . • • • • • • 1902 Candler, H. • • • • • • • 1905 Collin, T. • • • • • • • • 1907 Schofield, J . W. • • • • • • 1907 Drake, Canon F. W. • • • • • • 1908 Kidd, Canon J. H . • • • • • • 1921 Morshead, Lt.-Col. H. T. • • • • • 1922 Painter, A. R. • • • • • • • 1923 Wright, W. A. • • • • • • • 1925 Peto, R . H . K . • • • • • • • 1929 THE CLOSING OF THE ITALIAN ALPS. If a little easier in fre _quented districts during t he height of summer, there are no real signs of improvement in the general situation, which continues to be unsatisfactory. During the C.A.I. Congress at Botzen, the President announced that 18 passes, hitherto closed, would be open between t he Stelvio and Pontebba in 1932. The S.A.C. and letters of t he REv. W. A. B. CooLIDGE. The Librarian of the S.A.C. Central Library, Zurich, requests us to announce that, ' together with the Alpine portion of Mr. Coolidge's library, the S.A.C. has collected during the course of the year, in their library at Zurich, many letters belonging to that distinguished mountaineer. It is true that Mr. -
Alpine Adventures 2019 68
RYDER WALKER THE GLOBAL TREKKING SPECIALISTS ALPINE ADVENTURES 2019 68 50 RYDER WALKER ALPINE ADVENTURES CONTENTS 70 Be the first to know. Scan this code, or text HIKING to 22828 and receive our e-newsletter. We’ll send you special offers, new trip info, RW happenings and more. 2 RYDERWALKER.COM | 888.586.8365 CONTENTS 4 Celebrating 35 years of Outdoor Adventure 5 Meet Our Team 6 Change and the Elephant in the Room 8 Why Hiking is Important – Watching Nature 10 Choosing the Right Trip for You 11 RW Guide to Selecting Your Next Adventure 12 Inspired Cuisine 13 First Class Accommodations 14 Taking a Closer Look at Huts 15 Five Reasons Why You Should Book a Guided Trek 16 Self-Guided Travel 17 Guided Travel & Private Guided Travel EASY TO MODERATE HIKING 18 Highlights of Switzerland: Engadine, Lago Maggiore, Zermatt 20 England: The Cotswolds 22 Isola di Capri: The Jewel of Southern Italy NEW 24 French Alps, Tarentaise Mountains: Bourg Saint Maurice, Sainte Foy, Val d’Isère 26 Sedona, Arches & Canyonlands 28 Croatia: The Dalmatian Coast 28 30 Engadine Trek 32 Scotland: Rob Roy Way 34 Montenegro: From the Durmitor Mountain Range to the Bay of Kotor 36 New Mexico: Land of Enchantment, Santa Fe to Taos NEW 38 Slovakia: Discover the Remote High Tatras Mountains NEW MODERATE TO CHALLENGING HIKING 40 Heart of Austria 42 Italian Dolomites Trek 44 High Peaks of the Bavarian Tyrol NEW 46 Sicily: The Aeolian Islands 48 Rocky Mountain High Life: Aspen to Telluride 50 New Brunswick, Canada: Bay of Fundy 52 Via Ladinia: Italian Dolomites 54 Dolomiti di -
On the Disequilibrium Response and Climate Change Vulnerability of the Mass-Balance Glaciers in the Alps
Journal of Glaciology On the disequilibrium response and climate change vulnerability of the mass-balance glaciers in the Alps Article Luca Carturan1,2, Philipp Rastner3 and Frank Paul3 Cite this article: Carturan L, Rastner P, Paul F 1Department of Land, Environment, Agriculture and Forestry, University of Padova, Viale dell’Università 16, 35020, (2020). On the disequilibrium response and Legnaro, Padova, Italy; 2Department of Geosciences, University of Padova, Via Gradenigo 6, 35131, Padova, Italy climate change vulnerability of the mass- and 3Department of Geography, University of Zurich, Winterthurerstr. 190, 8057 Zurich, Switzerland balance glaciers in the Alps. Journal of Glaciology 66(260), 1034–1050. https://doi.org/ 10.1017/jog.2020.71 Abstract Received: 21 December 2019 Glaciers in the Alps and several other regions in the world have experienced strong negative mass Revised: 28 July 2020 balances over the past few decades. Some of them are disappearing, undergoing exceptionally Accepted: 31 July 2020 negative mass balances that impact the mean regional value, and require replacement. In this First published online: 9 September 2020 study, we analyse the geomorphometric characteristics of 46 mass-balance glaciers in the Alps Key words: and the long-term mass-balance time series for a subset of nine reference glaciers. We identify climate change; glacier mass balance; glacier regime shifts in the mass-balance time series (when non-climatic controls started impacting) monitoring; mountain glaciers and develop a glacier vulnerability index (GVI) as a proxy for their possible future development, based on criteria such as hypsometric index, breaks in slope, thickness distribution and elevation Author for correspondence: Luca Carturan, E-mail: [email protected] change pattern. -
Fabian Lächler Optimization of Regionalized Precipitation with Radar and Rain Gauge Data for Trentino-Alto Adige
Fabian Lächler Optimization of Regionalized Precipitation with Radar and Rain Gauge Data for Trentino-Alto Adige MASTER’S THESIS Submitted to the Institute of Geography, University of Innsbruck In partial fulfilment of requirements for the degree Master Advisors: Univ.-Prof. Dr. Ulrich Strasser Ass. Prof. Dr. Thomas Marke September 2017 Abstract The accurate measurement of rainfall is an important prerequisite for various applications of meteorology, hydrology and their subsections. The reliable detection of precipitation fields is difficult, particularly in mountainous regions. To provide the best possible measurement, rain gauge and precipitation radar data are combined in state-of-the-art weather models. However, these state-of- the-art methods have only been extensively used for a short period of time. For the study area, which is mostly located in the central eastern Alps in the Italian federal state Trentino-Alto Adige, no radar data from Gantkofel mountain had been integrated between 2004 and 2009. Therefore the aim of this master thesis was to develop a state-of-the-art algorithm which calculates retrospective precipitation fields for the years from 2004 to 2009. The algorithm, which is strongly orientated towards the INCA model developed by ZAMG (Haiden et al., 2011), computes a weighted combination of rain gauge and radar data. It takes into account the reduced visibility of radar in mountainous areas. Furthermore the elevation dependence of precipitation is considered. Three evaluation methods were selected to determine the accuracy of the developed model. Firstly, image differencing between the self- developed and the INCA model without the Gantkofel radar was carried out. -
An Overview of Glacier Lakes in the Western Italian Alps from 1927 To
Geogr. Fis. Dinam. Quat. DOI 10.4461/GFDQ.2016.39.19 39 (2016). 203-214, 9 figg., 3 tabb. CRISTINA VIANI (*), MARCO GIARDINO (*,**), CH RISTIAN GLHUG E (***), LUIGI PEROTTI (*,**) & GIO VANNI MORTARA (**) AN OVERVIEW OF GLACIER LAKES IN THE WESTERN ITALIAN ALPS FROM 1927 TO 2014 BASED ON MULTIPLE DATA SOURCES (HISTORICAL MAPS, ORTHOPHOTOS AND REPORTS OF THE GLACIOLOGICAL SURVEYS) ABSTRT AC : VIANI C., GIARDINO M., HUGLG E C., PEROTTI L. & MOR- Alps (Monte Rosa Group). Moreover, in a dedicated database, we collect- TARA G., An overview of glacier lakes in the Western Italian Alps form ed information (descriptions, photos, maps) about glacier lakes from the 1927 to 2014 based on multiple data sources (historical maps, orthophotos reports of the annual glaciological surveys published by the Italian Gla- and reports of the glaciological surveys). (IT ISSN 0391-9839, 2016) ciological Committee (CGI) since 1928. Finally, we reported two cases of glacier lakes at the Tzére Glacier (Monte Rosa Group, Pennine Alps) Since the end of the Little Ice Age (LIA, ca. 1850 AD) a general and at the Ban Glacier (Monte Leone-Blinnenhorn Chain, Lepontine and progressive retreat of glaciers started in the European Alps, causing Alps), in order to demonstrate the importance of integrating data from a important environmental changes in this high mountain region. The ap- diversity of sources (historical maps, orthophotos and reports of the gla- pearance of glacier lakes is one of the most evident environmental effects ciological surveys) for better detailed reconstructions of the condition of in the Alps as well as in newly deglaciated areas worldwide.