NATURE 203 Such a Construction Will Be Exceedingly Glad That So Ex• Has, Regarded As a Whole, a Unity and Perfection Which Perienced
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Case Study Skyway Mont Blanc, Courmayeur (IT)
Skyway Mont Blanc Case study Skyway Mont Blanc, Courmayeur (IT) Client: Funivie Monte Bianco AG, Courmayeur (IT) Architect: STUDIO PROGETTI Architect Carlo Cillara Rossi, Genua (IT) General contractor: Doppelmayr Italia GmbH, Lana Project completion: 2015 Products: FalZinc®, foldable Aluminium with a pre-weathered zinc surface Skyway Mont Blanc Mont Blanc, or ‘Monte Bianco’ in Italian, is situated between France and Italy and stands proud within The Graian Alps mountain range. Truly captivating, this majestic ‘White Mountain’ reaches 4,810 metres in height making it the highest peak in Europe. Mont Blanc has been casting a spell over people for hundreds of years with the first courageous mountaineers attempting to climb and conquer her as early as 1740. Today, cable cars can take you almost all of the way to the summit and Skyway Mont Blanc provides the latest and most innovative means of transport. Located above the village of Courmayeur in the independent region of Valle d‘Aosta in the Italian Alps Skyway Mont Blanc is as equally futuristic looking as the name suggests. Stunning architectural design combined with the unique flexibility and understated elegance of the application of FalZinc® foldable aluminium from Kalzip® harmonises and brings this design to reality. Fassade und Dach harmonieren in Aluminium Projekt der Superlative commences at the Pontal d‘Entrèves valley Skyway Mont Blanc was officially opened mid- station at 1,300 metres above sea level. From cabins have panoramic glazing and rotate 2015, after taking some five years to construct. here visitors are further transported up to 360° degrees whilst travelling and with a The project was developed, designed and 2,200 metres to the second station, Mont speed of 9 metres per second the cable car constructed by South Tyrolean company Fréty Pavilion, and then again to reach, to the journey takes just 19 minutes from start to Doppelmayr Italia GmbH and is operated highest station of Punta Helbronner at 3,500 finish. -
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. -
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. -
CAHIER D'architecture HAUTE Maurienne
CAHIER D’ARCHITECTURE Haute MaurieNNE / VANOISE Toute rénovation ou construction nouvelle va marquer l’espace de façon durable. Des paysages de caractère Chaque paysage possède un trait distinctif ou, mieux, une personnalité susceptible de susciter familiarité ou étrangeté. La Haute Maurienne présente un habitat très groupé en fond de vallée, le long de l’Arc et des voies de passage (col du Mont-Cenis, Petit Mont-Cenis et Iseran) pour libérer les prés de cultures et de fauche. Au-delà, le paysage est étagé, déterminé en cela par le relief et l’activité humaine : torrents, cultures, forêts, alpages, sommets, Parc national de la Vanoise. Depuis la fin du XXe siècle, l’usage de la montagne pour les sports d’hiver a bouleversé l’ancienne polarité et la montagne est désormais parcourue été comme hiver. Pour plus de précisions, se référer page 6 du document général. m k l j km N 0 1 Cartes IGN au 1 : 25 000 n° 3432 ET, 3532 OT, 3531 ET, 3532 ET, 3433 ET, 3534 OT et 3633 ET réduites à l’échelle du 1 : 150 000 © IGN - Paris - autorisation n° 9100 Reproduction interdite 46 Voilà nos paysages que des générations ont soigneusement construits et entretenus par leur savoir-faire, pour mieux y vivre. 10. Pays de Modane 12. Pays du Mont-Cenis Cette entité transversale marque le seuil de la Haute Maurienne. Elle est La haute vallée de l’Arc, de Lanslebourg à Lanslevillard, constitue un cadrée en rive droite (adret) par les sommets majestueux et glaciers du second seuil, délimité à l’amont par le col de La Madeleine. -
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. -
Bumble Bees of the Susa Valley (Hymenoptera Apidae)
Bulletin of Insectology 63 (1): 137-152, 2010 ISSN 1721-8861 Bumble bees of the Susa Valley (Hymenoptera Apidae) Aulo MANINO, Augusto PATETTA, Giulia BOGLIETTI, Marco PORPORATO Di.Va.P.R.A. - Entomologia e Zoologia applicate all’Ambiente “Carlo Vidano”, Università di Torino, Grugliasco, Italy Abstract A survey of bumble bees (Bombus Latreille) of the Susa Valley was conducted at 124 locations between 340 and 3,130 m a.s.l. representative of the whole territory, which lies within the Cottian Central Alps, the Northern Cottian Alps, and the South-eastern Graian Alps. Altogether 1,102 specimens were collected and determined (180 queens, 227 males, and 695 workers) belonging to 30 species - two of which are represented by two subspecies - which account for 70% of those known in Italy, demonstrating the particular value of the area examined with regard to environmental quality and biodiversity. Bombus soroeensis (F.), Bombus me- somelas Gerstaecker, Bombus ruderarius (Mueller), Bombus monticola Smith, Bombus pratorum (L.), Bombus lucorum (L.), Bombus terrestris (L.), and Bombus lapidarius (L.) can be considered predominant, each one representing more than 5% of the collected specimens, 12 species are rather common (1-5% of specimens) and the remaining nine rare (less than 1%). A list of col- lected specimens with collection localities and dates is provided. To illustrate more clearly the altitudinal distribution of the dif- ferent species, the capture locations were grouped by altitude. 83.5% of the samples is also provided with data on the plant on which they were collected, comprising a total of 52 plant genera within 20 plant families. -
From Valmy to Waterloo: France at War, 1792–1815
Copyright material from www.palgraveconnect.com - licensed to Universitetsbiblioteket i Tromsoe - PalgraveConnect - 2011-03-08 - PalgraveConnect Tromsoe i - licensed to Universitetsbiblioteket www.palgraveconnect.com material from Copyright 10.1057/9780230294981 - From Valmy to Waterloo, Marie-Cecile Thoral War, Culture and Society, 1750–1850 Series Editors: Rafe Blaufarb (Tallahassee, USA), Alan Forrest (York, UK), and Karen Hagemann (Chapel Hill, USA) Editorial Board: Michael Broers (Oxford, UK), Christopher Bayly (Cambridge, UK), Richard Bessel (York, UK), Sarah Chambers (Minneapolis, USA), Laurent Dubois (Durham, USA), Etienne François (Berlin, Germany), Janet Hartley (London, UK), Wayne Lee (Chapel Hill, USA), Jane Rendall (York, UK), Reinhard Stauber (Klagenfurt, Austria) Titles include: Richard Bessel, Nicholas Guyatt and Jane Rendall (editors) WAR, EMPIRE AND SLAVERY, 1770–1830 Alan Forrest and Peter H. Wilson (editors) THE BEE AND THE EAGLE Napoleonic France and the End of the Holy Roman Empire, 1806 Alan Forrest, Karen Hagemann and Jane Rendall (editors) SOLDIERS, CITIZENS AND CIVILIANS Experiences and Perceptions of the Revolutionary and Napoleonic Wars, 1790–1820 Karen Hagemann, Gisela Mettele and Jane Rendall (editors) GENDER, WAR AND POLITICS Transatlantic Perspectives, 1755–1830 Marie-Cécile Thoral FROM VALMY TO WATERLOO France at War, 1792–1815 Forthcoming: Michael Broers, Agustin Guimera and Peter Hick (editors) THE NAPOLEONIC EMPIRE AND THE NEW EUROPEAN POLITICAL CULTURE Alan Forrest, Etienne François and Karen Hagemann -
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. -
Geochemistry of Some Hp-Metavolcanics from Western Alps Metaophiolites
Acta Mineralogica-Petrographica, Szeged. XXX, 55—65,1989 GEOCHEMISTRY OF SOME HP-METAVOLCANICS FROM WESTERN ALPS METAOPHIOLITES I. KUBOVICS and ABDHL AAL M. ABDEL-KARIM Department of Petrology and Geochemistry, Lóránd Eötvös University ABSTRACT Ophiolite metavolvanics from Monviso, Arc valley and Montgenévre in the Piedmont Zone of the Western Alps are geochemically investigated and compared with data obtained from oceanic crust. Belonging to the Zermatt-Saas and Combin (Monviso and Arc valley) units they are charac- terized by HP-facies metamorphism including eclogite-facies metabasalts and garnet-bearing glauco- phanites that underwent into greenschist-facies metamorphism. Few metavolcanics (Montgenévre) are partly escaped from ocean-floor metamorphism, but they are overprinted by Alpine deformation. They show a large variation in the bulk rock geochemistry and roughly compare to MORB and a few of them show an IAT character. Their geochemical characters prevalently similar to that of oceanic ridge basalts and they show abyssal tholeiitic differentiation trend. KEYWORDS: HP-Facies metavolcanics, Geochemistry, metamorphic evolution, Peidmont Zone, Western Alps metaophiolite. INTRODUCTION * The HP-metamorphism had an effect on large bodies of the pre-Alpine conti- nental and organic crust in the Western Alps. During the Cretaceous, most of the oceanic crust (now represented by the Piedmont ophiolite nappe) and some parts of both continental margins underwent blueschist to eclogitic conditions that are followed by the greenschist facies conditions (LOMBARDO, 1988). The geochemistry of the metavolcanics from the Western Alps have been sub- jected to various studies ; previous researches had carried out from Monviso in Cottain Alps (LOMBARDO et al., 1978, NISIO, 1985, NISIO and LARDEAUX, 1987, COMPAGNONI et al., 1988), Arc valley in the Zermatt-Saas zone (BOCQUET, 1974, DAL PIAZ et al., 1981; DEN TEX, 1987; LEARDI et al., 1986) and from Chenaillet in Montgenévre (MÉVEL, 1975, LEWIS and SMEWING, 1980, BERTRAND et al., 1981, 1982, 1987). -
Travaux Scientifiques Du Parc National De La Vanoise
MINISTÈRE DÉLÉGUÉ ISSN 0180-961 X CHARGÉ DE L'ENVIRONNEMENT DIRECTION DE LA PROTECTION DE LA NATURE Travaux scientifiques du Parc National de la Vanoise Recueillis et publiés sous la direction de C. PAIRAUDEAU Directeur du Parc National Tome XVI 1988 Cahiers du Parc National de la Vanoise 135, rue du Docteur-Julliand B.P. 705, 73007 CHAMBÉRY Cedex (France) ISSN 0180-961 X Parc National de la Vanoise, Chambéry, France, 1988 COMPOSITION DU COMITE SCIENTIFIQUE DU PARC NATIONAL DE LA VANOISE Président honoraire : M. Philippe TRAYNARD, Président honoraire de l'Institut National Polytechnique de Gre- noble. Président: M. Denys PRADELLE, Architecte-Urbaniste, Chambéry. Viœ-Présidents : M. Philippe LEBRETON, Professeur à l'Université Claude Bernard Lyon l. M. André PALLUEL-GUILLARD, Maître Assistant à l'Université de Savoie, Chambéry. Membres du Comité: M. Roger BUVAT, Membre de l'Académie des Sciences, Professeur Honoraire à l'Univer- site de Marseille. M. Marc BOYER, Maître de Conférence à l'Université Lyon 2. M. Raymond CAMPAN, Professeur à l'Université Paul Sabatier, Toulouse. M. Yves CARTON, Maître de Recherches, C.N.R.S., Gif-sur-Yvette. M. Louis CHABERT, Professeur à l'Université Lyon 2. M. Charles DEGRANGE, Professeur à l'Université Joseph Fourier, Grenoble. M. René DELPECH, Professeur honoraire à l'Institut National Agronomique Paris-Gri- gnon. M. Philippe DREUX, Professeur à l'Université Pierre et Marie Curie, Paris. M. Bernard FANDRE, Administrateur Délégué du C.N.R.S., Grenoble. R.P. Robert FRITSCH, Président de la Société d"Histoire Naturelle de la Savoie. M. Louis Jean CACHET, Conservateur Adjoint au Musée Savoisien, Chambéry. -
Long-Wavelength Late-Miocene Thrusting in the North Alpine Foreland: Implications for Late Orogenic Processes
Solid Earth, 11, 1823–1847, 2020 https://doi.org/10.5194/se-11-1823-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes Samuel Mock1, Christoph von Hagke2,3, Fritz Schlunegger1, István Dunkl4, and Marco Herwegh1 1Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland 2Institute of Geology and Palaeontology, RWTH Aachen University, Wüllnerstrasse 2, 52056 Aachen, Germany 3Department of Geography and Geology, University of Salzburg, Hellbrunnerstrasse 34, 5020 Salzburg, Austria 4Geoscience Center, Sedimentology and Environmental Geology, University of Göttingen, Goldschmidtstrasse 3, 37077 Göttingen, Germany Correspondence: Samuel Mock ([email protected]) Received: 17 October 2019 – Discussion started: 27 November 2019 Revised: 24 August 2020 – Accepted: 25 August 2020 – Published: 13 October 2020 Abstract. In this paper, we present new exhumation ages 1 Introduction for the imbricated proximal molasse, i.e. Subalpine Mo- lasse, of the northern Central Alps. Based on apatite .U−Th−Sm/=He thermochronometry, we constrain thrust- Deep crustal processes and slab dynamics have been con- driven exhumation in the Subalpine Molasse between 12 and sidered to influence the evolution of mountain belts (e.g. 4 Ma. This occurs synchronously to the main deformation in Davies and von Blanckenburg, 1995; Molnar et al., 1993; the adjacent Jura fold-and-thrust belt farther north and to the Oncken et al., 2006). However, these deep-seated signals late stage of thrust-related exhumation of the basement mas- may be masked by tectonic forcing at upper-crustal levels sifs (i.e.