Relevant bibliographies by topics / 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 'Alps'

Author: Grafiati
Published: 4 June 2021
Last updated: 21 September 2024

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Journal articles on the topic "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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Maeland, Johan A., Jan E. Afset, Randi V. Lyng, and Andreas Radtke. "Survey of Immunological Features of the Alpha-Like Proteins of Streptococcus agalactiae." Clinical and Vaccine Immunology 22, no. 2 (December 24, 2014): 153–59. http://dx.doi.org/10.1128/cvi.00643-14.

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ABSTRACTNearly allStreptococcus agalactiae(group B streptococcus [GBS]) strains express a protein which belongs to the so-called alpha-like proteins (Alps), of which Cα, Alp1, Alp2, Alp3, Rib, and Alp4 are known to occur in GBS. The Alps are chimeras which form mosaic structures on the GBS surface. Both N- and C-terminal stretches of the Alps possess immunogenic sites of dissimilar immunological specificity. In this review, we have compiled data dealing with the specificity of the N- and C-terminal immunogenic sites of the Alps. The majority of N-terminal sites show protein specificity while the C-terminal sites show broader cross-reactivity. Molecular serotyping has revealed that antibody-based serotyping has often resulted in erroneous Alp identification, due to persistence of cross-reacting antibodies in antisera for serotyping. Retrospectively, this could be expected on the basis of sequence analysis results. Some of the historical R proteins are in fact Alps. The data included in the review may provide a basis for decisions regarding techniques for the preparation of specific antisera for serotyping of GBS, for use in other approaches in GBS research, and for decision making in the context of GBS vaccine developments.
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Leroux, Erick. "The great crossing of the Alps or move your Alps (GTA)." Worldwide Hospitality and Tourism Themes 10, no. 2 (April 9, 2018): 236–43. http://dx.doi.org/10.1108/whatt-12-2017-0080.

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Purpose The purpose of this study is to highlight the Grande Traversée des Alpes or – Move your Alps (GTA) which can be regarded as one of the first organizations to promote sustainable tourism in the Alps. Design/methodology/approach The study is based on a case study of the GTA. Findings The GTA is a key case study for understanding stakeholders’ management and sustainable tourism in the Alps. Originality/value There has been insufficient attention given in the literature to the role of the GTA, especially given its importance in the promotion of sustainable tourism in the Alps.
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Zhao, Zuotao, Fanrong Kong, and Gwendolyn L. Gilbert. "Reverse Line Blot Assay for Direct Identification of Seven Streptococcus agalactiae Major Surface Protein Antigen Genes." Clinical and Vaccine Immunology 13, no. 1 (January 2006): 145–49. http://dx.doi.org/10.1128/cvi.13.1.145-149.2006.

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ABSTRACT We developed a multiplex PCR-based reverse line blot hybridization assay (mPCR/RLB) to detect the genes encoding members of the family of variable surface-localized proteins of Streptococcus agalactiae (group B streptococcus [GBS]), namely, Bca (Cα), Rib, Epsilon (Epsilon/Alp1/Alp5), Alp2, Alp3, and Alp4, and the immunoglobulin A binding protein, Bac (Cβ). We used the assay to identify these genes in a collection of well-characterized GBS isolates and reference strains. The results showed that mPCR/RLB avoids the common problems of cross-reaction and nontypability associated with protein typing using antisera. It is as sensitive as, but more practical than, separate gene-specific PCRs and would be suitable for large molecular epidemiological studies of GBS.
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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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Price, Martin F. "Alpenatlas—Atlas des Alpes—Atlante delle Alpi—Atlas Alp—Mapping the Alps: Society—Economy—Environment." Mountain Research and Development 29, no. 3 (August 1, 2009): 292. http://dx.doi.org/10.1659/mrd.mm057.

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Tretow-Fish, Tobias Alexander Bang, and Md Saifuddin Khalid. "Methods for Evaluating Learning Analytics and Learning Analytics Dashboards in Adaptive Learning Platforms: A Systematic Review." Electronic Journal of e-Learning 21, no. 5 (December 19, 2023): 430–49. http://dx.doi.org/10.34190/ejel.21.5.3088.

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This research paper highlights and addresses the lack of a systematic review of the methods used to evaluate Learning Analytics (LA) and Learning Analytics Dashboards (LAD) of Adaptive Learning Platforms (ALPs) in the current literature. Addressing this gap, the authors built upon the work of Tretow-Fish and Khalid (2022) and analyzed 32 papers, which were grouped into six categories (C1-6) based on their themes. The categories include C1) the evaluation of LA and LAD design and framework, C2) the evaluation of user performance with LA and LAD, C3) the evaluation of adaptivity, C4) the evaluation of ALPs through perceived value, C5) the evaluation of Multimodal methods, and C6) the evaluation of the pedagogical implementation of ALP’s LA and LAD. The results include a tabular summary of the papers including the categories, evaluation unit(s), methods, variables and purpose. While there are numerous studies in categories C1-4 that focus on the design, development, and impact assessment of ALP's LA and LAD, there are only a few studies in categories C5 and C6. For the category of C5), very few studies applied any evaluation methods assessing the multimodal features of LA and LADs on ALPs. Especially for C6), evaluating the pedagogical implementation of ALP's LA and LAD, the three dimensions of signature pedagogy are used to assess the level of pedagogy evaluation. Findings showed that no studies focus on evaluating the deep or implicit structure of ALP's LA. All studies examine the structural surface dimension of learning activities and interactions between students, teachers, and ALP's LA and LAD, as examined in categories C2-C5. No studies were exclusively categorized as a C6 category, indicating that all studies evaluate ALP's LA and LAD on the surface structure dimension of signature pedagogy. This review highlights the lack of pedagogical methodology and theory in ALP's LA and LAD, which are recommended to be emphasized in future research and ALP development and implementation.
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Simmel, Georg. "The Alps." Qualitative Sociology 16, no. 2 (1993): 179–84. http://dx.doi.org/10.1007/bf00989749.

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Palmisani, E., M. Miano, T. Lanza, P. Terranova, M. Lanciotti, S. Zanardi, E. Facchini, et al. "PF351 ALPS DISEASE AND ALPS PHENOTYPE: DISTINCT ENTITIES?" HemaSphere 3, S1 (June 2019): 127. http://dx.doi.org/10.1097/01.hs9.0000559616.91240.a0.

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Seif, Alix E., Catherine S. Manno, Cecilia Sheen, Stephan A. Grupp, and David T. Teachey. "Identifying autoimmune lymphoproliferative syndrome in children with Evans syndrome: a multi-institutional study." Blood 115, no. 11 (March 18, 2010): 2142–45. http://dx.doi.org/10.1182/blood-2009-08-239525.

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Abstract Autoimmune lymphoproliferative syndrome (ALPS) is a disorder of abnormal lymphocyte survival caused by dysregulation of the Fas apoptotic pathway. Clinical manifestations of ALPS include autoimmune cytopenias, organomegaly, and lymphadenopathy. These findings overlap with Evans syndrome (ES), defined by presence of at least 2 autoimmune cytopenias. We hypothesized a subset of patients with ES have ALPS and tested 45 children at 22 institutions, measuring peripheral blood double-negative T cells (DNTs) and Fas-mediated apoptosis. ALPS was diagnosed in 47% of patients tested. Markedly elevated DNTs (≥ 5%) were a strong predictor of ALPS (positive predictive value = 94%), whereas no patients with DNTs less than 2.5% had ALPS on apoptosis testing. Severity of cytopenias and elevated immunoglobulin levels also predicted ALPS. This is the largest published series describing children with ES and documents a high rate of ALPS among pediatric ES patients. These data suggest that children with ES should be screened for ALPS with DNTs.
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Dissertations / Theses on the topic "Alps"

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Stacher, Susanne. "Dreamland Alps. L'architecture alpine au prisme du sublime." Thesis, Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLV070.

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La thèse interroge la manière dont la notion de sublime influence la définition de l’architecture construite dans les Alpes, depuis la naissance du tourisme jusqu’à aujourd’hui.La première partie traite de la façon dont au début du XVIIIe siècle, les Alpes sont devenues le topos d'une nouvelle perception de la nature qui se cristallise dans la notion de sublime. Entre effroi et fascination, ce terme engage une expérience de la limite. C’est à la recherche de cette sensation que les voyageurs se rendaient dans les Alpes. Peu de temps après des montagnes artificielles ont été construites dans les villes, d'abord en tant que symbole de la liberté pendant la Révolution française, ensuite comme panoramas illusionnistes, jusqu'aux parcs d'attractions du XIXe siècle.Les parties qui suivent analysent de quelle façon le sublime donne corps à différents types d’architectures. Tandis que les grand-hôtels alpins mettaient en scène la vue sur le panorama des montagnes pour contempler le spectacle de la nature sauvage, les architectures cristallines sont l’expression de visions utopiques. Au cours du XIXe siècle, l'intérêt pour la nature sauvage se transfère sur des éléments singuliers de la nature, particulièrement sur le soleil qui devient en tant que thérapie un véritable mythe. Ceci se manifeste dans les divers « mouvements de réforme de vie », tout comme dans les affiches publicitaires des sanatoriums. Les Alpes étaient considérées comme un « paysage thérapeutique », et comme un territoire idéal pour l'éducation. Différentes institutions religieuses et politiques y ont construit des colonies d'enfants, provocant entre eux une véritable lutte d'appropriation idéologique.Mais les Alpes étaient aussi le territoire idéal pour jouir de l'ivresse du mouvement et du vertige depuis que l’accès en était rendu possible par un réseau de plus en plus dense de téléphériques et de refuges, où l'architecture met en scène l'expérience de la limite du sublime. Avec l’émergence du tourisme de masse, ce n'était plus la nature qui était considérée comme sublime, mais la technique qui permettait de la dominer.L’analyse de l’architecture alpine à travers le prisme du sublime amène en conclusion à un état des lieux du tourisme alpin aujourd’hui où est mise en évidence la radicalité des prises de position. À travers ces présentations, les différentes figures du sublime ouvrent ainsi à une réflexion sur les constructions futures dans la continuité d’une pensée visionnaire, où s’articule le rapport entre l’homme et la nature
The thesis questions in which way the sublime has influenced the architecture built in the Alps, from the beginning of tourism until today.The first part shows how the Alps became in the beginning of the 18th century the topos of a new perception of nature, which crystallized in the notion of the sublime. Situated between terror and enthusiasm, this term implies an experience of the limit. Longing for this sensation, the travelers went to the Alps. A little later, mountains were constructed artificially in the cities, first as a symbol for liberty during the French Revolution, then in form of illusionist panorama-paintings, up to factice Swiss sceneries in amusement-parks in the end of the 19th century. This induced a flood of tourists, transforming the Alps into a “Dreamland”, for different kind of dreams.The main part analyses in which way the sublime became the guiding principle for various architectures: While the alpine grand-hotel framed the scenery by panoramic windows in order to contemplate the wilderness outside, crystalline architectures are conceived out of utopic visions, looking for a harmonious world. In the end of the 19th century the focus on the “wild nature” was transferred on to singular elements of nature, especially the sun, which (being considered as a remedy) became a real myth. This becomes evident in the “Live Reform”-groups, as well as in the advertisements for sanatoriums. The Alps were considered as a “therapeutic landscape”, as well as an ideal territory for education. Numerous children-colonies have been built by different religious and political institutions, leading to a fight about the appropriation of the children; the ideological differences became visible in the architectural typologies. But the Alps were also considered as an ideal territory to experiment the sensation of giddiness and speed. This became possible by the increasing net of cable-cars and sport-hotels, where cantilevers emphasized the experience of the limit (inherent to the sublime). With the upcoming mass tourism it was not anymore the wild nature which was considered as sublime, but the technic, which dominates nature.The analysis of the alpine architecture through the prism of the sublime leads to an observation of the actual alpine tourism, emphasizing the radicalism of the various phenomena throughout history. The different figures of the sublime open towards a reflection about the future constructions, in the continuity of a visionary relationship between man and nature
Die Dissertation hinterfragt auf welche Weise das Erhabene die Architektur in den Alpen beeinflusst hat, vom Beginn des Tourismus an bis heute. Im ersten Abschnitt wird aufgezeigt, wie die Alpen zu Beginn des 18. Jahrhunderts zum Topos einer neuartigen Naturbetrachtung wurden, die sich im Begriff des Sublimen (Erhabenen) kristallisierte. Zwischen Schrecken und Faszination angesiedelt, liegt diesem Gefühlszustand eine Grenzerfahrung zugrunde. Auf der Suche nach diesem Gemütszustand, suchten Reisende sehnsuchtsvoll die Welt der Berge auf; diese wurde alsbald in künstlicher Form in den Städten rekonstruiert, vom Freiheitssymbol der Französischen Revolution angefangen, über illusionistische Panoramabilder, bis hin zum Vergnügungspark im 19.Jh. Die daraufhin einsetzende Reiseflut verwandelte die Alpen in ein Land, in dem ganz unterschiedliche Träume projiziert wurden. In den folgenden Kapiteln wird untersucht, inwiefern das Sublime bei den unterschiedlichen Architekturen als Leitmotiv erscheint: Während beim alpinen Grandhotel die Aussicht auf das Panorama inszeniert wurde, um das Spektakel der „wilden Natur“ zu betrachten, standen bei den Kristallarchitekturen utopische-visionäre Gedanken im Vordergrund. Der Fokus auf die wilde Natur verlagerte sich gegen Ende des 19. Jahrhunderts auf einzelne Naturelemente, insbesondere auf die Sonne, die als Heilmittel zum Mythos erhoben wurde. Dies kommt sowohl in den Lebensreformgruppen zum Ausdruck, als auch auf den Werbeplakaten für Sanatorien. Die Alpen fungierten als „therapeutische Landschaft“ und wurden auch als idealer Ort der Erziehung angesehen. Verschiedene religiöse und politische Institution errichteten Kinderkolonien, wobei sich ein wahrer ideologischer „Kampf um das Kind“ entspann, der architektonisch gesehen zu sehr unterschiedlichen Resultaten führte. Die Alpen waren aber auch ein ideales Territorium, um den Rausch der Bewegung auszuleben. Dies wurde durch ein immer dichter werdendes Netz von Seilbahnen, Sporthotels und Hütten ermöglicht, wobei die Grenzerfahrung des Sublimen architektonisch bewusst inszeniert wurde. Mit dem aufkommenden Massentourismus wurde nicht mehr die wilde Natur, sondern die Technik als erhaben angesehen, die es ermöglichte, die Berge zu dominieren. Die Analyse der alpinen Architektur durch das Prisma des Sublimen führt uns zum Schluss zu einer Betrachtung des heutigen alpinen Tourismus im Spiegel des Wandels des Erhabenen-Begriffs, wobei die Radikalität der verschiedenen Phänomene hervorgehoben wird. Die unterschiedlichen Figuren des Erhabenen öffnen somit ein Nachdenken über das zukünftige Bauen in den Alpen, in der Kontinuität einer bestimmen Beziehung zwischen dem Menschen und der Natur
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Perucchetti, Laura. "Physical barriers, cultural connections : a reconsideration of the metal flow at the beginning of the metal age in the Alps." Thesis, University of Oxford, 2015. https://ora.ox.ac.uk/objects/uuid:e7da4d42-f41b-407f-9e75-6c5bc6b24132.

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This thesis considers the early copper and copper-alloy metallurgy of the entire Circum-Alpine region. It introduces a new approach to the interpretation of chemical composition data sets, which has been applied to a comprehensive regional database for the first time. An extensive use of GIS has been applied to investigate the role of topography in the distribution of metal and to undertake spatial and geostastical analysis that may highlight patterns of distribution of some specific key compositional element. The Circum-Alpine Chalcolithic and Early Bronze Age show some distinctively different patterns of metal use, which can be interpreted through changes in mining and social choices. But there are also some signs of continuity, in particular those which respect the use of major landscape features such as watersheds and river systems. Interestingly, the Alpine range does not act as a north-south barrier, as major differences in composition tend to appear on an east-west axis. Conversely, the river system seems to have a key role in the movement of metal. Geostastical analyses demonstrate the presence of a remelting process, applicable also in the case of ingots; evidence that opens new and interesting questions about the role of ingots and hoards in the distribution of metal at the beginning of the Metal Age. New tools and new analysis may also be useful to identify zones where there was a primary metal production and zones where metal was mostly received and heavily manipulated.
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Merle, Anthony. "Le piémont géographique : essai pour une approche au prisme des interspatialités : étude croisée entre terrains alpin (Alpes franco-suisses) et carpatique (Roumanie)." Thesis, Université Grenoble Alpes (ComUE), 2015. http://www.theses.fr/2015GREAA021/document.

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Si la montagne est un objet qui n'a cessé d'accompagner la discipline géographique et ses évolutions, la question des seuils de la montagne est toujours restée relativement marginale. Pourtant, un intérêt croissant pour ces espaces est à noter. De nombreux concepts animant la discipline (interface, interspatialités, espaces intermédiaires…) poussent à reconsidérer ces espaces flous, au seuil de « l'espèce d'espace » ou catégorie spatiale qu'est la montagne. C'est dans ce cadre qu'est menée cette étude croisée entre terrain des Alpes du Nord franco-suisses et terrain des Carpates roumaines. Ce seuil de la montagne, appelé ici piémont, ne saurait émerger selon des critères exclusivement physiques ou topographiques qui n'ont plus lieu d'être au sein d'une discipline toujours plus ancrée dans les sciences humaines. Le piémont peut alors être défini comme l'espace sur lequel se déploie un ensemble de fonctions dites « piémontines ». Ce sont ces fonctions qu'il s'agit ici de saisir, de définir, afin d'en identifier les acteurs et d'en expliquer les dynamiques spatiales et temporelles. Ce sont aussi les logiques territoriales et métropolitaines qui sont à interroger, puisque ces fonctions « piémontines » peuvent constituer autant d'occasions de développement, de rapprochements mais aussi de concurrences entre territoires et/ou entre métropoles. Par conséquent, ce sont également la genèse et le fonctionnement des territorialités et, plus spécifiquement, des processus d'urbanisation et de métropolisation qui sont obligatoirement envisagés lorsque l'on s'intéresse à ces fonctions « piémontines ». Enfin, l'étude croisée permet, au moins dans une certaine mesure, d'envisager la comparaison, malgré tous les écueils et limites que celle-ci présente. Les paradoxes émergeant de cette volonté de comparaison constituent alors autant d'éléments susceptibles de mieux saisir ce que peuvent être les seuils de la montagne, mais aussi de proposer une approche renouvelée de ces terrains d'étude
If the mountain is an object that has continued to support the geographical discipline and its developments, the issue of thresholds the mountain has remained relatively marginal. Yet a growing interest in these areas is noteworthy. Many concepts animating discipline (interface, interspatialités, intermediate spaces ...) push to reconsider these blurred areas, the threshold of "the kind of space" or spatial category what the mountain. It is in this context what this crossover study conducted between land North of the Alps in France and Switzerland and field of Romanian Carpathians. This threshold of the mountain foothills called here, can not emerge as exclusively physical or topographical criteria that have longer relevant in an increasingly rooted in the humanities discipline. The foothills can then be defined as the space on which deploys a set of functions called "foothill's functions". It is these features that this is to capture, define, in order to identify the players and explain the spatial and temporal dynamics. These are also the territorial logic and metropolitan which are to be questioned, as these "foothill's functions" can be as many development opportunities, but also of reconciliation competition between territories and / or between cities. Therefore, it is also the genesis and operation of territoriality and, specifically, the process of urbanization who must be considered when we look at these "foothill's functions". Finally, crossover study allows, at least to some extent, to consider the comparison, despite all the pitfalls and limitations that it presents. Emerging paradoxes of this comparison will then constitute elements that may better understand what can be the thresholds of the mountain, but also to propose a new approach to study these courses
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Martínez, Granado Pablo. "Inversion Tectonics in the Alpine Foreland, Eastern Alps (Austria)." Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/435684.

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In this thesis, the 3D structure and kinematics of the locally and mildly inverted Lower Austria Mesozoic Basin beneath the Alpine-Carpathian fold-and-thrust belt is described. This study has been carried out by the integrative interpretation of 2D and 3D seismic surveys, well and geophysical logs data and gravity maps. A basin-scale, 3D structural model has been carried out, focused on the sub-thrust and foreland zones. The Late Eocene to Early Miocene Alpine–Carpathian fold-and-thrust belt resulted from the subduction of the European plate beneath the Adriatic one, and the subsequent continental collision between both plates. The Alpine–Carpathian foredeep and fold-and-thrust belt recorded the long-lasting involvement of the European crystalline basement in several deformation events: from late Variscan transtension, to Jurassic rifting, and Cretaceous to Neogene shortening. In this thesis, two additional basement fault reactivation events have been defined in relation to the Alpine-Carpathian Cenozoic shortening: an extensional reactivation event related to the bending of the European plate coeval with Egerian to Karpatian (ca. 28–16 Ma) thin-skinned thrusting; followed by the selective positive inversion of the basement faults in the sub-thrust and in the foreland during Karpatian to Badenian times (ca. 16-12.5 Ma). The flexural bending of the European plate and the associated extensional fault reactivation were promoted by high lateral gradients of lithospheric strength in addition to the slab pull forces associated with subduction. Delamination of the European lithosphere during the final stages of collision around Karpatian times (ca. 16 Ma) promoted a large-wavelength uplift and an excessive topographic load. This topographic load was compensated by broadening the orogenic wedge through the compressional reactivation of the inherited fault array in the Euroepan plate beneath and ahead of the thin-skinned thrust system. Ultimately, collapse and deep burial of the Alpine-Carpathian tectonic wedge took place by the formation of the Pannonian basins system. To gain further insights in the deformational processes in sub-thrust and foreland settings, sandbox analogue models of brittle and brittle-viscous sand wedges have been carried out. The models aimed testing the influence of different topographic loads (i.e., thrust wedges) on the sub-thrust inversion of extensional basins, as well as the influence of the initial orientation of the extensional basins, and the presence or absence of weak detachment layers. Segmented half-graben basins -striking at 90º, 45º and 15º to the extension direction- were created first, and then shortened using different angles for the basal detachment and topographic slope. A shallow layer of viscous polymer over the half- graben basin was included in one of the models. The experiments were analysed using time-lapse photography, topography laser scans and image-based 3D voxels. The modelling results indicate a deformation sequence characterised by layer-parallel compaction, fault reactivation, thrust propagation and related folding. Fault reactivation and basin inversion were associated with layer-parallel compaction accomplished by slip along the basal detachment, prior to and in between pulses of thrusting. The results of the sandbox analogue models reveal a fundamental control imposed by the vertical load of the tectonic wedge and its integrated strength profile in the inversion of sub-thrust basins. Small vertical loads or strong gradients of vertical load have revealed as fundamental factors aiding in the inversion of buried, sub-thrust basins. The integrated strength profile resulted from the combination of inherited, strain-softened fault zones, as well as the presence or absence and distribution of weak, viscous horizons. The results of the sandbox models carried out indicate that the vertical load, its gradient over the sub-thrust basins and the inherited, strain-softened faults, are more important than the obliquity between the direction of shortening and the orientation of pre-existing fault systems. As indicated by the results of sandbox analogue models, the recurrent and long-lasting frictional reactivation of the Lower Austria basement fault array may have been favoured by fault-weakening mechanisms, as well as by steep gradients of vertical loads generated by thin-skinned out- of-sequence stacking of the Rhenodanubian Flysch located south of the inverted basement fault array.
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Käestle, Emanuel David. "High-resolution ambient-noise and earthquake surface-wave tomography of the Alps Apennines and Dinarides." Electronic Thesis or Diss., Paris 6, 2017. http://www.theses.fr/2017PA066307.

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La collision alpine a créé des structures complexes comme des chaînes de montagnes très arqués et des interactions compliquées entre les slabs subduits. La polarité de subduction est inversée à la transition entre les Alpes et les Apennins et les Alpes et les Dinarides. Le fait que la plaque Adria subducte en même temps vers l'ouest et vers l'est avec un fort pendage, presque verticalement, suggèrent une flexion importante de cette plaque. Notamment, si on considère de plus la proposition qu'Adria subducte aussi vers le nord sous les Alpes de l'est, ce qui est toujours sujet de discussion. Des déchirures dans le slab adriatique sous les Dinarides du nord à plus de 150 km de profondeur et sous les Apennins à moins de 200 km, pourraient être des signes d'une forte tension et, en conséquence, un détachement de la plaque adriatique. La plaque européenne pourrait aussi avoir subi plusieurs déchirures le long des Alpes. Cette hypothèse sujette à débat nécessite de nouveaux modèles tomographiques. Le modèle tomographique présenté dans cette thèse se base sur les vitesses de phase des ondes de surface pour donner un modèle 3-D à haute résolution des vitesses de cisaillement de la surface jusqu'à 200 km de profondeur. Ce modèle est unique de par sa haute résolution dans le manteau lithosphérique où des modèles antérieurs montrent de fortes incertitudes. Afin d'imager la croûte et le manteau supérieur en même temps, une combinaison des données de vitesses de phase des ondes de surface mesurés à partir des bruits ambiants ainsi que des séismes est utilisée dans cette thèse.Pour tester la validité de cette procédure, une comparaison détaillée des mesures de vitesses de phases et des structures imagées avec les deux méthodes est présentée. De l’analyse résulte un faible biais qui montre des vitesses plus élevées avec les données se basant sur des séismes par rapport aux données se basant sur le bruit ambiant. En comparant avec des travaux antérieurs, il est apparu que ce biais est dû à une différence méthodologique. Plusieurs paramètres qui pourraient influencer les mesures du bruit ambiant sont testés numériquement. Une cause unique n'a pu être identifiée. L'explication la plus probable pour le biais est une combinaison entre différentes sensibilités des méthodes aux structures et l'influence des modes supérieurs. Néanmoins, l'écart est suffisamment faible par rapport aux variations structurales pour être négligé.Un modèle final de vitesse de cisaillement de la région alpine est obtenu avec une résolution latérale d'environ 25 km dans la croûte peu profonde. Les tests synthétiques donnent une résolution approximative de profondeur estimée à 2 km près de la surface et de 5 km à la profondeur du Moho. Dans le manteau supérieur, la résolution baisse rapidement mais les structures principales des panneaux plongeants restent bien imagées jusqu'à une profondeur de 200 km le long des Alpes et des Apennins.La partie crustale du modèle donne des informations à haute résolution sur la taille et la profondeur des bassins sédimentaires et du corps d’Ivrée ainsi que sur la profondeur et la structure du Moho. Ce modèle de vitesses de cisaillement est le premier montrant autant de détails et couvrant les Alpes entières, il est proposé que le modèle pourrait servir comme référence pour la région.Le modèle montre les limites des zones de subduction et les régions de basses vitesses asthénosphèriques montants sous les bassins Ligure et pannonien. Des structures connues comme les déchirures de slabs sous les Apennins et les Dinarides sont imagés. Des découvertes supplémentaires ont été mises en évidence : une petite zone de faible vitesse qui coupe la lithosphère au nord des Dinarides est interprété comme l'expression d'une grande faille décrochante
The plate collision in the Alps and adjacent orogens has created a complex picture of highly arcuate mountain belts and complicated interactions of subduction slabs. The subduction polarity is reversed from European to Adriatic subduction in the transition of the Alps to the Apennines and to the Dinarides. The subduction of Adria both to the west and east and the almost vertical dip of the slabs implies an important flexure of this plate. Even more so if one considers the proposed subduction of Adria also to the north under the eastern Alps, which is still a matter of discussion. Gaps in the Adriatic slab under the northern Dinarides, below 150~km depth and in the southern Apennines above 200~km may be signs of the stresses and the consequent tearing that the Adriatic plate is exposed to.Also the European plate has supposedly undergone one or several break-offs all along the Alpine arc. Especially in the eastern and western Alps it is still an open question whether the European slab is detached below the lithosphere. New tomographic models are thus needed.The herein presented tomographic model is based on surface-wave phase velocities and gives a picture of the shear-velocity structure from the surface to 200 km depth. It is the first high-resolution shear-velocity model of the entire Alpine crust and upper mantle. It is also unique in its good resolution in the lithospheric mantle, where previous body-wave models are subject to high uncertainties. In order to be able to image both crust and upper mantle, a combination of ambient-noise and earthquake-based phase-velocity measurements is used in the present thesis.The validity of this approach is tested by a detailed comparison of the phase-velocity measurements and the structures that are imaged from each method individually. A small bias between the methods results in slightly elevated velocities from earthquake measurements. By comparison with earlier works it appears that this bias is due to methodological differences. Several effects that may influence the ambient-noise records are tested with synthetic experiments, but no unique cause is found. The most likely explanation for the bias between the two methods is a combination of different structural sensitivities and the influence of higher modes. Nevertheless, the discrepancy is sufficiently small with respect to the structural variations that the bias can be neglected.A final shear-velocity model of the Alpine region is obtained which has a lateral resolution in the shallow crust of approximately 25 km. From synthetic tests, the average depth resolution is estimated to be 2~km close to the surface and 5 km for the Moho depth. In the upper mantle the resolution decreases significantly, but main slab structures are well imaged in the central Alps and the Apennines down to the bottom of the model at 200 km depth.Highlights of the crustal part of the model are size and depth of sedimentary basins, the Ivrea body and the Moho structure. Being the first shear-velocity model of this detail and extend it is proposed to serve as reference for the Alps
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Menard, Gilles. "Structure et cinématique d'une chaîne de collision : les Alpes occidentales et centrales." Grenoble 1, 1988. http://www.theses.fr/1988GRE10018.

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La chaine alpine est un domaine a croute epaissie pour lequel le deplacement impose aux limites est absorbe alternativement par deux mecanismes de raccourcissement. Le premier correspond au glissement d'ecailles crustales sur des discontinuites, le second a une deformation interne des ecailles quand les glissements se bloquent. Ce modele s'applique egalement aux deformations actuelles et permet d'integrer aussi bien les donnees sur la sismicite (mecanismes au foyer) que sur les mouvements verticaux (surrection actuelle)
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7

Käestle, Emanuel David. "High-resolution ambient-noise and earthquake surface-wave tomography of the Alps Apennines and Dinarides." Thesis, Paris 6, 2017. http://www.theses.fr/2017PA066307/document.

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La collision alpine a créé des structures complexes comme des chaînes de montagnes très arqués et des interactions compliquées entre les slabs subduits. La polarité de subduction est inversée à la transition entre les Alpes et les Apennins et les Alpes et les Dinarides. Le fait que la plaque Adria subducte en même temps vers l'ouest et vers l'est avec un fort pendage, presque verticalement, suggèrent une flexion importante de cette plaque. Notamment, si on considère de plus la proposition qu'Adria subducte aussi vers le nord sous les Alpes de l'est, ce qui est toujours sujet de discussion. Des déchirures dans le slab adriatique sous les Dinarides du nord à plus de 150 km de profondeur et sous les Apennins à moins de 200 km, pourraient être des signes d'une forte tension et, en conséquence, un détachement de la plaque adriatique. La plaque européenne pourrait aussi avoir subi plusieurs déchirures le long des Alpes. Cette hypothèse sujette à débat nécessite de nouveaux modèles tomographiques. Le modèle tomographique présenté dans cette thèse se base sur les vitesses de phase des ondes de surface pour donner un modèle 3-D à haute résolution des vitesses de cisaillement de la surface jusqu'à 200 km de profondeur. Ce modèle est unique de par sa haute résolution dans le manteau lithosphérique où des modèles antérieurs montrent de fortes incertitudes. Afin d'imager la croûte et le manteau supérieur en même temps, une combinaison des données de vitesses de phase des ondes de surface mesurés à partir des bruits ambiants ainsi que des séismes est utilisée dans cette thèse.Pour tester la validité de cette procédure, une comparaison détaillée des mesures de vitesses de phases et des structures imagées avec les deux méthodes est présentée. De l’analyse résulte un faible biais qui montre des vitesses plus élevées avec les données se basant sur des séismes par rapport aux données se basant sur le bruit ambiant. En comparant avec des travaux antérieurs, il est apparu que ce biais est dû à une différence méthodologique. Plusieurs paramètres qui pourraient influencer les mesures du bruit ambiant sont testés numériquement. Une cause unique n'a pu être identifiée. L'explication la plus probable pour le biais est une combinaison entre différentes sensibilités des méthodes aux structures et l'influence des modes supérieurs. Néanmoins, l'écart est suffisamment faible par rapport aux variations structurales pour être négligé.Un modèle final de vitesse de cisaillement de la région alpine est obtenu avec une résolution latérale d'environ 25 km dans la croûte peu profonde. Les tests synthétiques donnent une résolution approximative de profondeur estimée à 2 km près de la surface et de 5 km à la profondeur du Moho. Dans le manteau supérieur, la résolution baisse rapidement mais les structures principales des panneaux plongeants restent bien imagées jusqu'à une profondeur de 200 km le long des Alpes et des Apennins.La partie crustale du modèle donne des informations à haute résolution sur la taille et la profondeur des bassins sédimentaires et du corps d’Ivrée ainsi que sur la profondeur et la structure du Moho. Ce modèle de vitesses de cisaillement est le premier montrant autant de détails et couvrant les Alpes entières, il est proposé que le modèle pourrait servir comme référence pour la région.Le modèle montre les limites des zones de subduction et les régions de basses vitesses asthénosphèriques montants sous les bassins Ligure et pannonien. Des structures connues comme les déchirures de slabs sous les Apennins et les Dinarides sont imagés. Des découvertes supplémentaires ont été mises en évidence : une petite zone de faible vitesse qui coupe la lithosphère au nord des Dinarides est interprété comme l'expression d'une grande faille décrochante
The plate collision in the Alps and adjacent orogens has created a complex picture of highly arcuate mountain belts and complicated interactions of subduction slabs. The subduction polarity is reversed from European to Adriatic subduction in the transition of the Alps to the Apennines and to the Dinarides. The subduction of Adria both to the west and east and the almost vertical dip of the slabs implies an important flexure of this plate. Even more so if one considers the proposed subduction of Adria also to the north under the eastern Alps, which is still a matter of discussion. Gaps in the Adriatic slab under the northern Dinarides, below 150~km depth and in the southern Apennines above 200~km may be signs of the stresses and the consequent tearing that the Adriatic plate is exposed to.Also the European plate has supposedly undergone one or several break-offs all along the Alpine arc. Especially in the eastern and western Alps it is still an open question whether the European slab is detached below the lithosphere. New tomographic models are thus needed.The herein presented tomographic model is based on surface-wave phase velocities and gives a picture of the shear-velocity structure from the surface to 200 km depth. It is the first high-resolution shear-velocity model of the entire Alpine crust and upper mantle. It is also unique in its good resolution in the lithospheric mantle, where previous body-wave models are subject to high uncertainties. In order to be able to image both crust and upper mantle, a combination of ambient-noise and earthquake-based phase-velocity measurements is used in the present thesis.The validity of this approach is tested by a detailed comparison of the phase-velocity measurements and the structures that are imaged from each method individually. A small bias between the methods results in slightly elevated velocities from earthquake measurements. By comparison with earlier works it appears that this bias is due to methodological differences. Several effects that may influence the ambient-noise records are tested with synthetic experiments, but no unique cause is found. The most likely explanation for the bias between the two methods is a combination of different structural sensitivities and the influence of higher modes. Nevertheless, the discrepancy is sufficiently small with respect to the structural variations that the bias can be neglected.A final shear-velocity model of the Alpine region is obtained which has a lateral resolution in the shallow crust of approximately 25 km. From synthetic tests, the average depth resolution is estimated to be 2~km close to the surface and 5 km for the Moho depth. In the upper mantle the resolution decreases significantly, but main slab structures are well imaged in the central Alps and the Apennines down to the bottom of the model at 200 km depth.Highlights of the crustal part of the model are size and depth of sedimentary basins, the Ivrea body and the Moho structure. Being the first shear-velocity model of this detail and extend it is proposed to serve as reference for the Alps
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8

Eremin, Katherine. "Metamorphic conditions within the Eclogite Zone, Tauern Window, Austria." Thesis, University of Cambridge, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321481.

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Peel, F. J. "Structural evolution of the Vanoise Massif (French Alps)." Thesis, University of Oxford, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.370320.

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Ghiselli, A. "Interaction of geomorphology and tectonics in the evolution of the Orobic Alps (central Southern Alps)." Doctoral thesis, Università degli Studi di Milano, 2008. http://hdl.handle.net/2434/60326.

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Although numerical and physical models clearly demonstrated the dynamic coupling of tectonic evolution with surface processes, the landscape is still often interpreted as the result of the climatic action only. Valley patterns in mountain areas are often related to glacial and fluvial erosion, without considering the influence of structures. The aim of this work is to find out the relationships between tectonics and geomorphology to get an evolutionary model of the Orobic Alps (Central Southern Alps, Italy). The structural model is based on previous authors’ works, cross-sections (traditional and balanced) and interpretation of existing data. This analysis allowed the reconstruction of the alpine deformation phases and of the relative chronology of structures. Geomorphology and Quaternary geology field-data, aerial photos-DEMs interpretation and evaluations of the erosion rates gave informations on the landscape evolution. Sandbox experiments helped to understand the linkage between structures and morphologies, kinematic and erosion. The integration of structural and geomorphological analysis showed the close relationship between valley evolution and tectonics. The contemporaneous evolution of valleys and relieves has been demonstrated: the initial valley pattern was created during the alpine deformation phases together with the structures. Weathering and gravity acted during and after the orogenesis dismantling part of the relief. Rivers and glaciers played a minor role, mainly transporting and depositing the debris previously produced, rather then actively eroding the valleys. Therefore, the Orobic Alps landscape is mostly inherited by the structural shaping of the surface during the alpine deformation phases.
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Books on the topic "Alps"

1

Hans, Mayer, and Arbeitsgemeinschaft Alpen-Adria, eds. Alps Adria. Motovun: Motovun, 1986.

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Lee, Stephen. The Alps. London: Batsford, 1991.

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Michelin, ed. French Alps. Clermont-Ferrand: Michelin, 1998.

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Allsop, David. Swiss Alps. Lincolnwood, Ill: Passport Books, 1993.

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1917, Mason Stanley b., ed. The alps. Dübendorf: De Clivo Press, 1987.

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Harvey, Edwards, and Spring Ira, eds. 100 hikes in the Alps. 2nd ed. Seattle: Mountaineers, 1992.

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George, Mills, ed. Walking Austria's Alps: Hut to hut. Seattle: Mountaineers, 1988.

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Keith, Sugden, ed. Ancient pathways in the Alps. London: Philip, 1988.

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Dana, Krista. Alps Pocket Adventures. Hobe Sound: Hunter Publishing, 2007.

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Sandford, Robert W. The Canadian Alps. Banff, Alta., Canada: Altitude Pub., 1990.

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Book chapters on the topic "Alps"

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Beniston, Martin. "Alps." In Encyclopedia of Earth Sciences Series, 35–38. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_16.

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Paul, Frank, Yves Arnaud, Roberto Ranzi, and Helmut Rott. "European Alps." In Global Land Ice Measurements from Space, 439–63. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-540-79818-7_20.

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Kellerer-Pirklbauer, Andreas, Isabelle Gärtner-Roer, Xavier Bodin, and Luca Paro. "European Alps." In Periglacial Landscapes of Europe, 147–224. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-14895-8_9.

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Psaras, Marios. "Alps: Of Hauntology." In The Queer Greek Weird Wave, 155–84. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-40310-6_6.

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Sattler, Katrin. "The Southern Alps." In Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, 9–16. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-35074-5_2.

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Füreder, Leopold, Aurelia Ullrich-Schneider, and Thomas Scheurer. "Alps Freshwater, Europe." In Climate and Conservation, 129–43. Washington, DC: Island Press/Center for Resource Economics, 2012. http://dx.doi.org/10.5822/978-1-61091-203-7_11.

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Anderson, Ben. "Constructing the Alps." In Cities, Mountains and Being Modern in fin-de-siècle England and Germany, 99–138. London: Palgrave Macmillan UK, 2020. http://dx.doi.org/10.1057/978-1-137-54000-3_4.

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Kybett, Susan Maclean. "Beyond the Alps." In Bonnie Prince Charlie, 21–41. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003211686-2.

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Carrer, Francesco. "Archaeology of the Alps." In Encyclopedia of Global Archaeology, 834–46. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-30018-0_3492.

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Carrer, Francesco. "Archaeology of the Alps." In Encyclopedia of Global Archaeology, 1–12. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-51726-1_3492-1.

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Conference papers on the topic "Alps"

1

Hornby, Gregory S. "ALPS." In the 8th annual conference. New York, New York, USA: ACM Press, 2006. http://dx.doi.org/10.1145/1143997.1144142.

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Lazik, Patrick, Niranjini Rajagopal, Oliver Shih, Bruno Sinopoli, and Anthony Rowe. "ALPS." In SenSys '15: The 13th ACM Conference on Embedded Network Sensor Systems. New York, NY, USA: ACM, 2015. http://dx.doi.org/10.1145/2809695.2809727.

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Karri, Ramesh, and Alex Orailoğlu. "ALPS." In the 24th annual international symposium. New York, New York, USA: ACM Press, 1991. http://dx.doi.org/10.1145/123465.123490.

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Hu, Yitao, Xiaochen Liu, Suman Nath, and Ramesh Govindan. "ALPS." In UbiComp '16: The 2016 ACM International Joint Conference on Pervasive and Ubiquitous Computing. New York, NY, USA: ACM, 2016. http://dx.doi.org/10.1145/2971648.2971674.

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Koehler, Christian, Nikola Banovic, Ian Oakley, Jennifer Mankoff, and Anind K. Dey. "Indoor-ALPS." In UbiComp '14: The 2014 ACM Conference on Ubiquitous Computing. New York, NY, USA: ACM, 2014. http://dx.doi.org/10.1145/2632048.2632069.

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Szabó, Gábor. "ELI-ALPS." In the 19th ACM SIGSOFT symposium and the 13th European conference. New York, New York, USA: ACM Press, 2011. http://dx.doi.org/10.1145/2025113.2025117.

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Massó, Eduard, David B. Tanner, and Karl A. van Bibber. "Spin-Two ALPs." In AXIONS 2010: Proceedings of the International Conference. AIP, 2010. http://dx.doi.org/10.1063/1.3489554.

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Zhao, Chen, Zhenya Zhou, and Dake Wu. "Empyrean ALPS-GT." In ICCAD '20: IEEE/ACM International Conference on Computer-Aided Design. New York, NY, USA: ACM, 2020. http://dx.doi.org/10.1145/3400302.3415762.

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Koç, Cansu, Gonca Kaçar, Simge Özel Çınar, Suheyla Ocak, Nihan Burtecene, and Tiraje Celkan. "297 Lymphoma or ALPS?" In 10th Europaediatrics Congress, Zagreb, Croatia, 7–9 October 2021. BMJ Publishing Group Ltd and Royal College of Paediatrics and Child Health, 2021. http://dx.doi.org/10.1136/archdischild-2021-europaediatrics.297.

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Elstermann, Matthes, and Jivka Ovtcharova. "Sisi in the ALPS." In the 10th International Conference. New York, New York, USA: ACM Press, 2018. http://dx.doi.org/10.1145/3178248.3178262.

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Reports on the topic "Alps"

1

Jordan, David V., Paul L. Reeder, Lindsay C. Todd, Glen A. Warren, Kathleen R. McCormick, Daniel L. Stephens, Bruce D. Geelhood, James M. Alzheimer, Shannon L. Crowell, and William A. Sliger. Advanced Large Area Plastic Scintillator Project (ALPS): Final Report. Office of Scientific and Technical Information (OSTI), February 2008. http://dx.doi.org/10.2172/925718.

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Jordan, David V., Bruce D. Geelhood, Paul L. Reeder, Daniel L. Stephens, Richard A. Craig, and Justin I. McIntyre. Progress Report on the Advanced Large-Area Plastic Scintillators (ALPS) Project. Office of Scientific and Technical Information (OSTI), May 2003. http://dx.doi.org/10.2172/15010207.

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Bergmann, Nicolas. Preserving Nature through Film: Wilderness Alps of Stehekin and the North Cascades, 1956-1968. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.973.

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Reeder, Paul L., Daniel L. Stephens, David V. Jordan, Richard A. Craig, and Bruce D. Geelhood. Progress Report for the Advanced Large-Area Plastic Scintillator (ALPS) Project: FY 2003 Final. Office of Scientific and Technical Information (OSTI), November 2003. http://dx.doi.org/10.2172/15010549.

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Alexander, Timothy, and Ole Seehausen. Diversity, distribution and community composition of fish in perialpine lakes. "Projet Lac" synthesis report. Eawag, 2021. http://dx.doi.org/10.55408/eawag:24051.

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Projet Lac was a large project conducted by Eawag and the University of Bern to quantitatively survey, for the first time, whole-lake fish communities in the large and deep lakes in and around the European Alps using multiple, standardised sampling methods. Starting in 2010, in total 35 lakes were investigated across Switzerland, Italy, France, Germany and Austria, with more than 106 fish species recorded. This report brings together key findings, compares fish communities among lakes, investigates their relationship to environmental parameters, and provides an overview of drivers of biodiversity and community structure in this important ecosystem.
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Hutton, A., J. Uberti, and M. Thomson. The ALPN HTTP Header Field. RFC Editor, August 2015. http://dx.doi.org/10.17487/rfc7639.

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De Waele, Arnout, Janne Vaes, Pim Van Reempts, and Nathalie Casteels. Erfgoed als hefboom. Brussel: agentschap Onroerend Erfgoed, April 2024. http://dx.doi.org/10.55465/yioe4857.

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Rietra, R. P. J. J., P. G. Dijk, and J. P. van t Hull. Bodem als indicator : bodemkenmerken als indicator voor nitraat in grondwater. Wageningen: Wageningen Environmental Research, 2022. http://dx.doi.org/10.18174/574940.

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Waters, A., and W. Brown. ALS Performance Summary - Update. Office of Scientific and Technical Information (OSTI), September 2004. http://dx.doi.org/10.2172/15014619.

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Tamura, ed. ALS Activity Report 2004. Office of Scientific and Technical Information (OSTI), July 2005. http://dx.doi.org/10.2172/877330.

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