Relevant bibliographies by topics / Western Alps

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Western Alps'

Author: Grafiati
Published: 4 June 2021
Last updated: 4 May 2024

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Journal articles on the topic "Western Alps"

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Kvam, Augusta I., Rooyen T. Mavenyengwa, Andreas Radtke, and Johan A. Maeland. "Streptococcus agalactiae Alpha-Like Protein 1 Possesses Both Cross-Reacting and Alp1-Specific Epitopes." Clinical and Vaccine Immunology 18, no. 8 (June 8, 2011): 1365–70. http://dx.doi.org/10.1128/cvi.05005-11.

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ABSTRACTMost isolates of group B streptococci (GBS) express an alpha-like protein (Alp), Cα (encoded bybca), Alp1 (also called epsilon;alp1), Alp2 (alp2), Alp3 (alp3), Alp4 (alp4), or R4/Rib (rib). These proteins are chimeras with a mosaic structure and with antigenic determinants with variable immunological cross-reactivities between the Alps, including Alp1 and Cα cross-reactivity. This study focused on antigenic domains of Alp1, studied by using rabbit antisera in immunofluorescence, Western blotting, and enzyme-linked immunosorbent assay (ELISA)-based tests and whole cells of GBS or trypsin-extracted and partially purified antigens from the strains A909 (serotype Ia/Cα, Cβ) and 335 (Ia/Alp1). Alp1 and Cα shared an antigenic determinant, Alp1/Cα common, not harbored by other Alps, probably located in the Alp1 and Cα repeat units, as these units are nearly identical in genomic sequence. An antigenic Alp1 determinant was Alp1 specific and was most likely located in the N-terminal unit of Alp1 in which an Alp1-specific primer site for PCR is also located. In addition, Alp1 possessed a domain with low immunogenicity which cross-reacted immunologically with Alp2 and Alp3, with unknown location in Alp1. Alp1 was partially degraded by trypsin during antigen extraction but with the antigenic domains preserved. The results indicate that Cα and Alp1 are immunologically related in the same manner that R4 (Rib) and Alp3 are related. The domain called Alp1 specific should be important in GBS serotyping as a surface-anchored serosubtype marker. The Alp1/Cα common determinant may be of prime interest as an immunogenic domain in a GBS vaccine.
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Michl, Thomas, Stefan Huck, Peter Haase, and Burkhard Büdel. "Genetic Differentiation among Populations of Cicerbita alpina (L.) Wallroth (Asteraceae) in the Western Alps." Zeitschrift für Naturforschung C 62, no. 9-10 (October 1, 2007): 747–56. http://dx.doi.org/10.1515/znc-2007-9-1019.

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In this study we analyzed the genetic population structure of the hygrophilous tall-herb Cicerbita alpina in the western Alps because this group of mountain plants is underrepresented in the biogeographical literature. AFLP (amplified fragment length polymorphism) fingerprints of 40 samples were analyzed from four populations situated in a transect from the southwestern Alps to the eastern part of the western Alps and one population from the Black Forest outside the Alps. Two genetic groups can be distinguished. The first group (A) comprises the populations from the northern and eastern parts of the western Alps, and the second group (B) comprises the populations from the southwestern Alps and the Black Forest. Group A originates most likely from at least one refugium in the southern piedmont regions of the Alps. This result provides molecular evidence for a humid climate at the southern margin of the Alps during the Würm glaciation. Group B originates presumably from western or northern direction and we discuss two possible scenarios for the colonization of the Alps, i. e. (1) long-distance dispersal from southwestern refugia and (2) colonization from nearby refugia in the western and/or northern Alpine forelands. The study demonstrates that the target species harbours considerable genetic diversity, even on a regional scale, and therefore is a suitable model for phylogeographic research.
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Perrone, G., P. Cadoppi, S. Tallone, and G. Balestro. "Post-collisional tectonics in the Northern Cottian Alps (Italian Western Alps)." International Journal of Earth Sciences 100, no. 6 (April 2, 2010): 1349–73. http://dx.doi.org/10.1007/s00531-010-0534-1.

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Carrapa, Barbara, Jan Wijbrans, and Giovanni Bertotti. "Episodic exhumation in the Western Alps." Geology 31, no. 7 (2003): 601. http://dx.doi.org/10.1130/0091-7613(2003)031<0601:eeitwa>2.0.co;2.

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Ricou, L. E., and A. W. B. Siddans. "Collision tectonics in the Western Alps." Geological Society, London, Special Publications 19, no. 1 (1986): 229–44. http://dx.doi.org/10.1144/gsl.sp.1986.019.01.13.

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Gillet, Ph, P. Choukroune, M. Ballèvre, and Ph Davy. "Thickening history of the Western Alps." Earth and Planetary Science Letters 78, no. 1 (May 1986): 44–52. http://dx.doi.org/10.1016/0012-821x(86)90171-8.

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Nguyen, Hai Ninh, Philippe Vernant, Stephane Mazzotti, Giorgi Khazaradze, and Eva Asensio. "3-D GPS velocity field and its implications on the present-day post-orogenic deformation of the Western Alps and Pyrenees." Solid Earth 7, no. 5 (September 21, 2016): 1349–63. http://dx.doi.org/10.5194/se-7-1349-2016.

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Abstract. We present a new 3-D GPS velocity solution for 182 sites for the region encompassing the Western Alps, Pyrenees, and southern France. The velocity field is based on a Precise Point Positioning (PPP) solution, to which we apply a common-mode filter, defined by the 26 longest time series, in order to correct for network-wide biases (reference frame, unmodeled large-scale processes, etc.). We show that processing parameters, such as troposphere delay modeling, can lead to systematic velocity variations of 0.1–0.5 mm yr−1 affecting both accuracy and precision, especially for short (< 5 years) time series. A velocity convergence analysis shows that minimum time-series lengths of ∼ 3 and ∼ 5.5 years are required to reach a velocity stability of 0.5 mm yr−1 in the horizontal and vertical components, respectively. On average, horizontal residual velocities show a stability of ∼ 0.2 mm yr−1 in the Western Alps, Pyrenees, and southern France. The only significant horizontal strain rate signal is in the western Pyrenees with up to 4 × 10−9 yr−1 NNE–SSW extension, whereas no significant strain rates are detected in the Western Alps (< 1 × 10−9 yr−1). In contrast, we identify significant uplift rates up to 2 mm yr−1 in the Western Alps but not in the Pyrenees (0.1 ± 0.2 mm yr−1). A correlation between site elevations and fast uplift rates in the northern part of the Western Alps, in the region of the Würmian ice cap, suggests that part of this uplift is induced by postglacial rebound. The very slow uplift rates in the southern Western Alps and in the Pyrenees could be accounted for by erosion-induced rebound.
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Winterle, Alberto. "Leggere le Alpi / Reading the Alps." Regionalità e produzione architettonica contemporanea nelle Alpi, no. 1 ns, november 2018 (November 15, 2018): 202–6. http://dx.doi.org/10.30682/aa1801v.

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Living a place means first of all reading it, understanding it, assimilating it. This is even more evident in the case of a particular natural environment where the possibilities of land use are limited. Looking at a map of the Alps, it becomes clear how the morphology has conditioned the methods of settlement and exploitation of the places. In an attempt to read and interpret the transformation of the Alpine territories, the Architetti Arco Alpino association has initiated a review of projects, from which it emerges that today there exist very different cultural, political, social and economic contexts. The result are two almost opposite phenomena. In some places the mountains have been abandoned, which has led to the risk of losing their important architectural heritage. The interventions are therefore aimed at enhancing the existing structures and constructing new buildings capable of becoming a reference for the redevelopment of entire villages. In other places, a harmonic balance between human presence and territory has been largely exceeded. Here, the objective is to put a stop to further land development, aiming to enhance the quality of the existing buildings and implementing an aesthetic and formal research that is capable of becoming an economic value and an element of cultural identification. Taking into account the various “cultural horizons” and reference regions, it becomes clear that South Tyrol has historically maintained close ties with North Tyrol and the neighbouring Swiss cantons. Contemporary architecture is commonly seen as an asset today, not only among experts, but also among the general population. On the other hand, the relations with Austria’s and Slovenia’s Eastern Alpine territories have less effect. The research seems to be the work of a limited number of professionals. In the Western Alps, cross-border relations with France and Switzerland have a stronger cultural and linguistic root, but perhaps the presence of large massifs difficult to cross has prevented a closer relationship and a dissemination of common construction methods. Crossing national and international administrative boundaries, the Alps can continue to be a place of passage, of confrontation and of cultural, linguistic, economic and also architectural exchange.
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Pšenička, Josef, Stanislav Opluštil, Ausonio Ronchi, and Zbyněk Šimůnek. "Revision of the Pennsylvanian Flora from Val Sanagra in Western Part of the Southern Alps (Italy)." Folia Musei rerum naturalium Bohemiae occidentalis. Geologica et Paleobiologica 46, no. 1-2 (December 1, 2012): 31–79. http://dx.doi.org/10.2478/fbgp-2013-0003.

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Abstract The Pennsylvanian flora from the Alpe Logone/Val Sanagra locality in the Western Lombardy (Southern Alps, Italy) last underwent a taxonomic study in the mid 20th century. The main problem is generally poor preservation of the plant remains, which makes their identification problematic. Despite this, the authors have identified 43 fossil species from this locality. Based on the sedimentary context of this paleoflora, we assume that the Val Sanagra sediments were deposited in a continental setting, in a fluvial environment with a well-developed and vegetated floodplain where where clastic substrates would locally and occasionally change into peat swamp. The common presence of rhytidolepis and sub-rhytidolepis sigillarias, as well of Eusphenopteris neuropteroides, Lobatopteris miltonii, Mariopteris latifolia, Paripteris linguaefolia, Pecopteris microphylla, Alethopteris sp. (cf. grandinii) indicates that the flora from the Val Sanagra locality spans the interval between the Duckmantian and Bolsovian (middle Moscovian), and thus represents one of the oldest Pennsylvanian floras of the Southern Alps.
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Carcaillet, Christopher, and Olivier Blarquez. "Glacial refugia in the south‐western Alps?" New Phytologist 222, no. 2 (February 7, 2019): 663–67. http://dx.doi.org/10.1111/nph.15673.

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Dissertations / Theses on the topic "Western Alps"

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Ustaszewski, Michaela. "Active tectonics in the central and western Swiss Alps /." [S.l.] : [s.n.], 2007. http://www.zb.unibe.ch/download/eldiss/07ustaszewski_m.pdf.

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Maurer, Hansruedi Maurer Hansruedi Maurer Hansruedi. "Seismotectonics and upper crustal structure in the western swiss alps /." Zürich, 1993. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=10268.

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Hubbard, Bryn Pugh. "Basal ice facies and their formation in the western Alps." Thesis, University of Cambridge, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239624.

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Marucco, Francesca. "Spatial population dynamics of recolonizing wolves in the western Alps." Diss., [Missoula, Mont.] : The University of Montana, 2009. http://etd.lib.umt.edu/theses/available/etd-10092009-140452.

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Bowtell, Sophie Ann. "Geochronological and geochemical studies of Zermatt-Saas Fee Ophiolite, Western Alps." Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305487.

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BADINO, FEDERICA. "Holocene vegetation and climate variability as recorded in high-altitude mires (western Italian Alps)." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2016. http://hdl.handle.net/10281/131067.

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Climate variability during the Holocene (the last 11700 calendar yr b2k) is relatively subtle whether compared with the higher amplitude characterizing the last glacial period. Nonetheless, several proxy data (e.g. pollen, plant macrofossils, glacier length variations), indicate detectable changes in temperature and/or moisture during this period. Retreating glaciers may uncover peat sequences that were once ice-buried. Palynological analysis of those organic deposits provides information on plant communities colonization in proglacial areas as well as long-distance vegetations signal. The aim of this study is to investigate the potential of high-altitude pollen records for vegetation history and climate reconstruction during the Holocene in the south-western Italian Alps. The study sites are located in the Rutor Glacier area (La Thuile Valley). Within this thesis, modern (a) and past (b) vegetation and climate conditions have been analyzed using different methodologies; a) Modern pollen rain, vegetation, climate and terrain parameters have been collected at 27 sampling sites placed along an altitudinal gradient from the village of Morgex (983 m asl) to the Rutor Glacier forefield (2668 m asl). This altitudinal training set has been designed (i) to provide a robust modern reference for reliable palaeoenvironmental and quantitative interpretations of past changes in vegetation composition; (ii) to integrate the newly-obtained pollen spectra into a large, continental dataset of modern pollen samples (EMPD - European Modern Pollen Database) for quantitative climate reconstructions. b) New paleoecological, stratigraphical and geochronological data have been obtained from peat deposits (Lac dans la Roche peat bog, 2594 m asl) and integrated with the well-known buried peat sequences exposed at 2510 m asl by the '80es Rutor Glacier retreat. The result is a composite paleoecological record covering most of the Holocene. At the base of the composite sequence, meltwater glacier sediments testify to the early Holocene development of a proglacial lake, before Abies alba expansion in the western Italian Alps. These sediments bear the palynological evidence of a primary plant succession testifying to an ecological mechanism of colonization on deglaciated terrains. Moreover, macrofossil analysis highlighted the local presence of alpine dwarf - shrubland species (e.g. Salix cfr. foetida). Pinus cembra occurs rather densely in the alpine belt from ca. 8000 yrs cal. BP, representing the beginning of the Holocene thermal maximum in the high Alps. Between 8000 - 4000 yrs cal. BP timberline was higher than today. A radiocarbon age obtained from a Pinus cembra wood fragment suggests the occurrence of pines as high as ca. 2600 m asl at around 5650 yrs cal BP. The dated wood fragment cannot have been long-distance transported, thus it indicates the presence of this species in situ. Moreover, paleobotanical insights and comparison with climate threshold of modern treeline (ca. 9,3° C at 2400 m asl), suggest a positive treeline shift of almost 150 m. Preliminary pollen-inferred Tjul reconstructions show higher values (up to 2 - 3°C) than today for this interval. At around 4000 yrs cal. BP Picea abies and Alnus viridis started to expand. A progressive natural/climatic driven decline of Pinus cembra took place. Pollen inferred Tjul shows a decreasing trend between 2900 – 2000 yrs cal BP and possibly a short-lived cold event starting at ca. 1140 yrs cal. BP, pre-dating the onset of the LIA (Little Ice Age). A subsequent arolla pine forests reduction can be attributed to LIA glacier advance (max occurred between 1751 – 1864 AD), which is testified in the upper part of the sequence by fluvioglacial deposits.
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Parish, M. "Tectonic evolution of the Western French Alps around St. Jean de Maurienne." Thesis, University of Oxford, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.371553.

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Ashruf, Tahira Nicole <1990&gt. "The Moho reflectivity from ambient seismic noise autocorrelations beneath the Western Alps." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2022. http://amsdottorato.unibo.it/10491/1/Thesis30Sept_TahiraNicoleAshruf.pdf.

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The lower crustal structure beneath the Western Alps -- including the Moho -- bears the signature of past and present geodynamic processes. It has been the subject of many studies until now. However, its current knowledge still leaves significant open questions. In order to derive new information, independent from previous determinations, here I wish to address this topic using a different method --- ambient seismic noise autocorrelation --- that is for the first time applied to reveal Moho depth in the Western Alps. Moho reflections are identified by picking reflectivity changes in ambient seismic noise autocorrelations. The seismic data is retrieved from more than 200 broadband seismic stations, from the China--Italy--France Alps (CIFALPS) linear seismic network, and from a subset of the AlpArray Seismic Network (AASN). The automatically-picked reflectivity changes along the CIFALPS transect in the southwestern Alps show the best results in the 0.5--1 Hz frequency band. The autocorrelation reflectivity profile of the CIFALPS transect shows a steeper subduction profile,~55 to ~70 km, of the European Plate underneath the Adriatic Plate. The dense spacing of the CIFALPS network facilitates the detection of lateral continuity of crustal structure, and of the Ivrea mantle wedge reaching shallow crustal depths in the southwestern Alps. The data of the AASN stations are filtered in the 0.4--1 and 0.5--1 Hz frequency bands. Although the majority of the stations give the same Moho depth for the different frequency bands, the few stations with different Moho depths shows the care that has to be taken when choosing the frequency band for filtering the autocorrelation stacks. The new Moho depth maps by using the AASN stations are a compilation of the first and second picked reflectivity changes. The results show the complex crust-mantle structure with clear differences between the northwestern and southwestern Alps.
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Kassem, Osama Mohamed Kaoud. "Finite-strain analysis in orthogneiss of the Gran Paradiso massif, Western Alps, Italy." [S.l.] : [s.n.], 2005. http://deposit.ddb.de/cgi-bin/dokserv?idn=97595749X.

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Chambers, Alan Frederick. "Kinematics of the frontal Himalayan thrust belt, Pakistan, and the external western Alps, France." Thesis, Imperial College London, 1992. http://hdl.handle.net/10044/1/11281.

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Books on the topic "Western Alps"

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Jozef, Vozár, IGCP Project 176--Paleozoic Geodynamic Domains and their Alpidic Evolution in the Tethys., International Geological Correlation Programme, Geologický ústav Dionýza Štúra, and Slovak Geological Conference (5th : 1990 : Bratislava, Slovakia 0., eds. Western Carpathians, eastern Alps, Dinarides. Bratislava: Dionýz Štúr Institute of Geology, 1992.

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I.G.C.P. 235 Excursion to the Alps. (1988 Turin-Genoa). Geological framework of the Western Alps: Field meeting on highecologitic reequilibrium in the Western Alps. [Genoa]: [IGCP Project 235], 1988.

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Dodgshon, Robert. Farming Communities in the Western Alps, 1500–1914. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-16361-7.

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Isaia, Marco. Aracnidi sotterranei delle Alpi occidentali italiane =: Subterranean arachnids of the western Italian Alps. Torino: Museo regionale di scienze naturali, 2011.

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Neillands, Robin. Eighth Army: From the Western Desert to the Alps, 1939-1945. London: John Murray, 2004.

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Venturini, Guido. Geology, geochemistry, and geochronology of the inner central Sesia zone, western Alps, Italy. Lausanne, Suisse: Section des sciences de la terre, Institut de géologie et paléontologie, Université de Lausanne, 1995.

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Nina, Shoumatoff, ed. The Alps: Europe's mountain heart. Ann Arbor: University of Michigan Press, 2001.

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Marylou, Reifsnyder, and Sierra Club, eds. Adventuring in the Alps: France, Switzerland, Germany, Austria, Liechtenstein, Italy, Slovenia. 2nd ed. San Francisco: Sierra Club Books, 1999.

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Marylou, Reifsnyder, and Sierra Club, eds. Adventuring in the Alps: The Sierra Club travel guide to the Alpine regions of France, Switzerland, Germany, Austria, Liechtenstein, Italy, and Yugoslavia. San Francisco: Sierra Club Books, 1986.

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Beccaro, Paola. Radiolarian biostratigraphy of middle-upper Jurassic pelagic siliceous successions of Western Sicily and the Southern Alps (Italy). Lausanne, Suisse: Institut de Géologie et Paléontologie, Université de Lausanne, 2006.

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Book chapters on the topic "Western Alps"

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Armand, Fabio. "Werewolves in the Western Alps." In Werewolf Legends, 261–83. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-06082-3_11.

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Nicolich, R. "Crop-Ecors Activity in the Western Alps." In Joint Interpretation of Geophysical and Geological Data Applied to Lithospheric Studies, 189–92. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3590-0_11.

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Bausch, Thomas. "Managing hybrid destinations: challenges and lessons from the Alps." In Tourism marketing in Western Europe, 108–26. Wallingford: CABI, 2021. http://dx.doi.org/10.1079/9781789248753.0006.

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Abstract Using the example of the Alps, it was shown that hybridity in tourism touches primarily three marketing fields: (a) Product. Because of attractions that change their character and level of appeal throughout the year or are linked to yearly events and habits, the perception of the core elements of the destination's image varies; (b) Communication. The hybridity of the product implies the need to address different target groups, as the changing focus of the destination image attracts different, often disjunctive or mutually exclusive, consumer groups; and (c) Pricing. Similar to all fields of consumption, an increasing polarization between low cost or bargain trips and high priced luxury travelling can be found. Some travellers prefer either lowcost or luxury travelling, while others change their expenditure from trip to trip.
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Kochan, Lionel. "Beyond the Rhine and Over the Alps." In The Making of Western Jewry, 1600–1819, 267–74. London: Palgrave Macmillan UK, 2004. http://dx.doi.org/10.1057/9780230800021_17.

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Gentile, Luca, Walter Sartor, Giuseppe Rachino, and Paulo Rachino. "Uranium and radon in the Italian Western Alps." In IFMBE Proceedings, 682–84. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03902-7_196.

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Stampfli, G. M., and R. H. Marchant. "Geodynamic evolution of the Tethyan margins of the Western Alps." In Deep Structure of the Swiss Alps, 223–39. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_17.

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Marchant, R. H., and G. M. Stampfli. "Crustal and lithospheric structure of the Western Alps: geodynamic significance." In Deep Structure of the Swiss Alps, 326–37. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_24.

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Escher, A., J. C. Hunziker, M. Marthaler, H. Masson, M. Sartori, and A. Steck. "Geologic framework and structural evolution of the western Swiss-Italian Alps." In Deep Structure of the Swiss Alps, 205–21. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9098-4_16.

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de Graciansky, P. C. "Basement-Cover Relationship in the Western Alps Constraints for Pre-Triassic Reconstructions." In Pre-Mesozoic Geology in the Alps, 7–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 1993. http://dx.doi.org/10.1007/978-3-642-84640-3_2.

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Butler, Robert W. H. "The Geometry of Crustal Shortening in the Western Alps." In Tectonic Evolution of the Tethyan Region, 43–76. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2253-2_3.

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Conference papers on the topic "Western Alps"

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Deville, É., and W. Sassi. "Integrated maturity modelling in thrust belts - Cases histories in the Western Alps." In 58th EAEG Meeting. Netherlands: EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201409119.

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Macagno, Sara, Luca Degiorgis, and Massimo Santarelli. "H2 &#38; RENEWABLE ENERGY: A CASE STUDY IN NORTH-WESTERN ITALIAN ALPS." In HYSYDAYS. Connecticut: Begellhouse, 2023. http://dx.doi.org/10.1615/hysydays2005.510.

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Rahmonov, T., and S. Ermakov. "VARIETY OF LANGUAGES IN SWITZERLAND." In Manager of the Year. FSBE Institution of Higher Education Voronezh State University of Forestry and Technologies named after G.F. Morozov, 2022. http://dx.doi.org/10.34220/my2021_258-261.

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Switzerland is located at the junction of western, central and southern Europe, is landlocked and borders Italy to the south, France to the west, Germany to the north, and Austria and Liechtenstein to the east. The country is geographically divided between the Alps, the Swiss plateau and the Jura, covering a total area of 41,285 km². While the Alps occupy most of the territory, Switzerland’s population of approximately 8.5 million people is mainly concentrated on the plateau, where the largest cities are located, including two global ones – Zurich and Geneva. Switzerland is at the crossroads of Germanic and Romance Europe and has four main linguistic and cultural regions: German, French, Italian and Romansh.
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Marchisio, M., A. Bianchi, X. Bodin, P. Ciuffi, L. D‘Onofrio, D. Fabre, M. Pappalardo, A. Ribolini, S. Sartini, and P. Schoneich. "Application of Electrical Resistivity Tomography on Glaciers and Rock-Glaciers in the Western Alps." In Near Surface 2005 - 11th European Meeting of Environmental and Engineering Geophysics. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.13.p033.

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Chen, Anxia, Zhen Zeng, Zicong Xiao, Yi-Xiang Chen, Fang Huang, and Xiaofeng Gu. "Modification of fluids in subduction channel: Evidence from barium isotopes of western Alps whiteschis." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.5495.

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Kempf, Elias Dominik, and Jörg Hermann. "HYDROGEN INCORPORATION AND RETENTION IN METAMORPHIC OLIVINE FROM THE ECLOGITE FACIES ZERMATT-SAAS SERPENTINITES (WESTERN ALPS)." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320377.

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Gerbaldo, Paolo. "TRAVELS THROUGH THE WESTERN ALPS IN THE AGE OF GRAND TOUR: ALBANIS BEAUMONT FROM CUNEO TO NICE." In 5th SGEM International Multidisciplinary Scientific Conferences on SOCIAL SCIENCES and ARTS SGEM2018. STEF92 Technology, 2018. http://dx.doi.org/10.5593/sgemsocial2018/2.2/s08.051.

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Ulrich, Michelle, Daniela Rubatto, Jörg Hermann, Francesca Piccoli, and Cees-Jan De Hoog. "Tracking fluid flow in subducted serpentinites of the Zermatt-Saas HP-ophiolite (Western Alps) using oxygen isotopes." In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.14088.

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Bruno, F., L. Levato, and F. Marillier. "High-resolution seismic reflection, EM and electrokinetic SP applied to landslide studies: "Le Boup" landslide (Western Swiss Alps)." In 4th EEGS Meeting. European Association of Geoscientists & Engineers, 1998. http://dx.doi.org/10.3997/2214-4609.201407175.

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Bienveignant, Dorian, Yann Rolland, Martin Huraut, Adrien Vezinet, Matthias Bernet, Stéphane Schwartz, Arjan De-Leeuw, Thierry Dumont, and Antonin Bilau. "Clacite U-Pb dating in the Western Alps: State of the art and new perspectives for constraining Alpine geodynamics." In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.19391.

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Reports on the topic "Western Alps"

1

Belz, Markus, Svenja Höner, Claudia Kruse, Sebastian Rolfsmeier, and Merle Schroer. Mobilitätsmanagement an der Goethe-Universität Frankfurt am Main, Campus Westend. Goethe-Universität, Institut für Humangeographie, December 2014. http://dx.doi.org/10.21248/gups.35594.

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Die Goethe-Universität ist einer der größten Verkehrserzeuger der Stadt Frankfurt. Der Bericht zum Mobilitätsmanagement stellt zunächst die drängendsten Herausforderungen an der Goethe-Universität exemplarisch für den größten Campus, den Campus Westend, dar. Anschließend werden Maßnahmen zur Verbesserung der Situation abgeleitet und hinsichtlich ihrer Wirkung, ihrer zeitlichen Realisierung und der notwendigen Kosten abgeschätzt. Übergreifend wird die Einführung eines institutionalisierten Mobilitätsmanagements für die Goethe-Universität vorgeschlagen. Damit können – in enger Abstimmung mit weiteren städtischen Akteuren – Maßnahmen zu einer sowohl effizienteren als auch umweltfreundlicheren und sicheren Gestaltung des Verkehrs von Studierenden und Beschäftigten umgesetzt werden.
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2

Schubert, Steffi. Universität in Bewegung. Goethe-Universität, Institut für Humangeographie, August 2016. http://dx.doi.org/10.21248/gups.39466.

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Die Goethe-Universität befindet sich seit einigen Jahren in einem deutlichen Wandel. Der Campus Westend wird zum Zentralcampus ausgebaut und auch personell wächst die Goethe-Universität. Fast 47.000 Studierende und mehr als 5.000 Beschäftigte (Stand Herbst 2014) studieren und arbeiten an den Campussen. Die Goethe-Universität ist damit einer der bedeutendsten Verkehrserzeuger in Frankfurt, da nahezu täglich über 50.000 Personen ihren Studien- oder Arbeitsplatz an der Goethe-Universität erreichen müssen und auch zwischen den verschiedenen Standorten pendeln. Das folgende Arbeitspapier befasst sich mit der Mobilität der Studierenden und der Beschäftigten der Goethe-Universität, die mittels zweier Online-Befragungen erhoben und analysiert wurden. Es werden die zentralen Erkenntnisse bezüglich der vorhandenen Mobilitätsressourcen und wohnungsnahen Mobilitätsangebote, des Verkehrsverhaltens hinsichtlich der Häufigkeit, Dauer und Länge von Wegen zu und zwischen den Campussen und der Nutzung von Verkehrsmitteln, den Einstellungen zu den verschiedenen Verkehrsmitteln und die Nutzungsbereitschaft bezüglich optionaler Mobilitätsangebote der Universität vorgestellt. Abschließend wird ein Resümee über den durch die Universität erzeugten Verkehr gezogen und auf Basis umfassender zielgruppenspezifischer Erkenntnisse werden Vorschläge zur Entzerrung, Verlagerung und Optimierung für ein universitäres Mobilitätsmanagement entwickelt.
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3

Ali Khogali, Sophie, Aileen Behnel, Johann Kalbhenn, Patrick Kunz, and Lara Sophie Wilhelmi. Auswirkungen fahrradfreundlicher Infrastruktur auf Gewerbetreibende : eine qualitative Untersuchung zum Einfluss einer Fahrradstraße auf Gewerbetreibende am Beispiel des Frankfurter Grüneburgwegs. Goethe-Universität, Institut für Humangeographie, Arbeitsgruppe Mobilitätsforschung, December 2023. http://dx.doi.org/10.21248/gups.69039.

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Im Rahmen des Maßnahmenpakets zur Förderung fahrradfreundlicher Infrastruktur wurde der Frankfurter Grüneburgweg zur Fahrradstraße umgebaut. Mit Fokus auf Gewerbetreibende wurde zwischen März und April 2023 eine Studie zu den Auswirkungen der Fahrradstraße auf dem Grüneburgweg im Frankfurter Westend durchgeführt. Insgesamt wurden 12 Interviews mit ortsansässigen Einzelhandel- und Gastronomiebetreiber:innen geführt. Im Zentrum standen dabei die Auswirkungen der Fahrradstraße auf die geschäftlichen Aktivitäten sowie Einflussfaktoren der Akzeptanz solcher Maßnahmen. Es konnte herausgearbeitet werden, dass die Fahrradstraße aus Sicht der ansässigen Gewerbetreibenden einen negativen Einfluss auf die Erreichbarkeit des Grüneburgwegs hat. Dies geht laut den befragten Gewerbetreibenden mit Umsatzverlusten, einem Rückgang an Kund:innen und Problemen mit der Warenlieferung einher. Ferner wird von einigen Gewerbetreibenden kritisiert, nicht rechtzeitig seitens der Stadt über den Umbau informiert worden zu sein und kein Mitspracherecht bei der Gestaltung der Fahrradstraße zu haben. Die von vielen Gewerbetreibenden wahrgenommenen Auswirkungen auf ihre geschäftlichen Aktivitäten, ihre Einbeziehung in den Planungs- und Umbauprozess sowie ihr eigenes Mobilitätsverhalten sind zentrale Einflussfaktoren für die Akzeptanz der Fahrradstraße. Die Ergebnisse zeigen, dass viele Gewerbetreibende zwar eine positive Einstellung zur Fahrradstraße haben, jedoch den Grüneburgweg nicht als einen geeigneten Standort für eine Fahrradstraße halten. Aus den Ergebnissen lässt sich schließen, dass für künftige Umgestaltungen besonders auf eine gute Kommunikation der Stadt mit den Gewerbetreibenden geachtet werden muss.
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