Relevant bibliographies by topics / Alpine arc

Contents

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

Academic literature on the topic 'Alpine arc'

Author: Grafiati
Published: 5 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "Alpine arc"

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FRY, NORMAN. "Kinematics of the Alpine arc." Nature 341, no. 6243 (1989): 576. http://dx.doi.org/10.1038/341576b0.

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PLATT, J. P. "Kinematics of the Alpine arc." Nature 341, no. 6243 (1989): 576. http://dx.doi.org/10.1038/341576c0.

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Woosaree, J., S. N. Acharya, and B. A. Darroch. "ARC Sentinel spike trisetum." Canadian Journal of Plant Science 85, no. 2 (2005): 403–6. http://dx.doi.org/10.4141/p04-010.

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ARC Sentinel spike trisetum (Trisetum spicatum L.) Richt. (Moss 1992) is a low-growing native grass cultivar developed by the Alberta Research Council Inc. for reclamation and revegetation of disturbed sites at high elevations in the Rocky Mountains of Alberta. This is the first spike trisetum cultivar released in Canada for commercial production. This cultivar is well adapted to grow and produce viable seed during the short growing seasons found in the alpine and sub-alpine regions of the Canadian Rocky Mountains. Field observations indicate that ARC Sentinel spike trisetum can tolerate droug
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Müntener, Othmar, Peter Ulmer, and Jonathan D. Blundy. "Superhydrous Arc Magmas in the Alpine Context." Elements 17, no. 1 (2021): 35–40. http://dx.doi.org/10.2138/gselements.17.1.35.

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Magmatic rocks in the Alps are scarce. What little arc magmatism there was pre-dates the Eurasia–Adria collision at 43–34 Ma but ends at 30–29 Ma. Conversely, geochemical data for magmatic rocks from the Alps resemble that of subduction-related magmatic arcs. A characteristic of Alpine magmatism is the occurrence of relatively deep (80–100 km) super-hydrous (>8 wt% H2O) low-K primary magmas in the east and shoshonitic K-rich magmas in the west. These features are likely related to the absence of vigorous mantle wedge convection. Superhydrous primary magmas undergo extensive crystallizat
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Vouillamoz, Naomi, Christian Sue, Jean-Daniel Champagnac, and Philippe Calcagno. "3D cartographic modeling of the Alpine arc." Tectonophysics 579 (December 2012): 131–43. http://dx.doi.org/10.1016/j.tecto.2012.06.012.

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FRY, NORMAN. "Short Paper: Kinematics of the Alpine arc." Journal of the Geological Society 146, no. 6 (1989): 891–92. http://dx.doi.org/10.1144/gsjgs.146.6.0891.

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PAPANIKOLAOU, D., and P. NOMIKOU. "Tectonic structure and volcanic centers at the eastern edge of the aegean volcanic arc around Nisyros island." Bulletin of the Geological Society of Greece 34, no. 1 (2001): 289. http://dx.doi.org/10.12681/bgsg.17025.

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The recent volcanic activity at the eastern edge of the Aegean Volcanic Arc is limited within a neotectonic graben structure which is developed in an E-W general direction between the alpine basement of Kos Island to the north and the alpine basement of Tilos Island to the south. In between the boundary faults of the neotectonic graben there is an extended volcanic area comprising several individual volcanic centers, which penetrate through the thick post-alpine sedimentary deposits of the graben.
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Lickorish, W. H., M. Ford, J. Bürgisser, and P. R. Cobbold. "Arcuate thrust systems in sandbox experiments: A comparison to the external arcs of the Western Alps." GSA Bulletin 114, no. 9 (2002): 1089–107. http://dx.doi.org/10.1130/0016-7606(2002)114<1089:atsise>2.0.co;2.

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Abstract In the external Western Alps, two regional structural arcs were generated during Tertiary northwest-directed collision between the Apulian indenter and the European passive margin. These arcs, distinguished by their geographic position and their age, are examined by using a new compilation of structural data and comparing these to the results of sandbox-analogue experiments. The principal Western Alpine arc comprises two orthogonal, synchronous thrust systems. In the late Eocene–early Miocene, major shortening (105 km) was toward the northwest to west-northwest, and minor shortening (
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Choukroune, Pierre, Michel Ballèvre, Peter Cobbold, Yann Gautier, Olivier Merle, and Jean-Paul Vuichard. "Deformation and motion in the Western Alpine Arc." Tectonics 5, no. 2 (1986): 215–26. http://dx.doi.org/10.1029/tc005i002p00215.

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Vialon, P., P. Rochette, and G. Ménard. "Indentation and rotation in the western Alpine arc." Geological Society, London, Special Publications 45, no. 1 (1989): 329–38. http://dx.doi.org/10.1144/gsl.sp.1989.045.01.18.

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Dissertations / Theses on the topic "Alpine arc"

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Weston, Peter John. "The origin and kinematics of the Alpine arc." Thesis, University of Oxford, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.253478.

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Marnezy, Alain. "L'Arc et sa vallée : anthropisation et géodynamique d'une rivière alpine dans son bassin versant." Université Joseph Fourier (Grenoble), 1999. http://www.theses.fr/1999GRE10013.

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L'Arc en Maurienne (Savoie) présente à l'état naturel tous les caractères d'une rivière torrentielle à forte pente, à l'hydrologie contrastée, aux transports solides abondants. Depuis le XIX siècle, des interventions anthropiques massives ont transformé profondément le fonctionnement du système fluvial : un endiguement insubmersible sur les deux tiers du cours d'eau, l'assainissement de la basse vallée par colmatage et drainage, des travaux de correction torrentielle dans les bassins versants affluents, le développement des équipements hydroélectriques. Maîtrisé, l'Arc est à l'origine de la tr
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Rosenbaum, Gideon. "Tectonic reconstruction of the Alpine orogen in the western Mediterranean region." Monash University, School of Geosciences, 2003. http://arrow.monash.edu.au/hdl/1959.1/9481.

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Aillères, Laurent. "Structure et cinématique de la zone houillère briançonnaise entre Arc et Isère (Alpes francaises) : apport de l'inversion des données de la déformation finie aux modèles cinématiques classiques." Vandoeuvre-les-Nancy, INPL, 1996. http://docnum.univ-lorraine.fr/public/INPL_T_1996_AILLERES_L.pdf.

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A partir de nouvelles observations structurales, nous proposons un nouveau modèle cinématique pour la Zone Houillère Briançonnaise, située au-dessus du front briançonnais (structure majeure des Alpes occidentales). Ce modèle est conforté par l'inversion des données de déformation finie, interpolées et visualisées à l'aide du modeleur 3D GOCAD (ENSG-LIAD Nancy). Les données de déformation finie ont été acquises par l'utilisation d'algorithmes d'analyse d'images, semi-automatisées au cours de ce travail. L'inversion a été effectuée à l'aide du logiciel FaultPack (Université Rennes 1). Le modèle
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El, Bakili Asmae. "Evolution tectono-metamorphique et chronologique des unités métamorphiques du Rif interne (Beni Bousera, Nord du Maroc)." Thesis, Université Côte d'Azur, 2021. http://www.theses.fr/2021COAZ4034.

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Située à l'extrême-ouest de la Méditerranée occidentale, la chaîne bético-rifaine s’est formée au travers d’une histoire orogénique alpine complexe, impliquant des processus de subduction liés à la convergence entre l’Afrique et l’Eurasie depuis le Crétacé. Une découverte importante de ces quatre dernières décennies d'investigations géologiques, a été la mise en évidence des vestiges d’un événement varisque dans les zones internes de la chaîne. Ces résultats soulignent bien la présence de deux systèmes orogéniques superposés, les zones internes de la chaîne bético-rifaine demeurent donc des zo
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Villermet, Jean-Marc. "Dynamiques et enjeux au sein d'un village de montagne : l'espace Grand Arc - Lauzière, aux portes de la Maurienne (mi XIXe - début XXI e s.)." Thesis, Université Grenoble Alpes (ComUE), 2016. http://www.theses.fr/2016GREAH042.

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Etudier les dynamiques et enjeux au sein d’un village de montagne, en Savoie, engendre une réflexion plus générale sur des questionnements importants de l’époque contemporaine. Jean-Marc Villermet a choisi d’aborder ce sujet pour plusieurs raisons : son attachement à cette région, la proximité des archives, le désir de réactiver le chantier de l’aménagement du territoire en altitude.Il s’intéressa à une région désertée, bien que située dans un espace montagnard réputé pour la qualité de ses sites dans une dimension internationale. Jamais la transformation et les mutations économiques et social
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Beucher, Romain. "Evolution Néogène de l'arc~alpin~sud-occidental: Approches sismotectonique et thermochronologique." Phd thesis, Université Joseph Fourier (Grenoble), 2009. http://tel.archives-ouvertes.fr/tel-00444816.

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Cette thèse cible l'évolution Néogène de la branche sud de l'arc alpin occidental. Une approche multi-méthodes associant études de terrain, sismotectonique et thermochronologie basse température y met en évidence un régime tectonique complexe ainsi qu'une évolution morphologique et structurale originale au sein de l'arc. La fracturation s'organise autour d'un faisceau d'accidents NW-SE, à jeu principalement dextre, accompagnant la courbure de l'arc et commandant structure et morphologie. Par ailleurs, à l'échelle des massifs, une structuration en failles normales conjuguées NE-SW traduit une e
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Marçais, Johanna. "Transferts des polluants organiques persistants de l'atmosphère aux milieux aquatiques de montagne." Thesis, Université Grenoble Alpes (ComUE), 2017. http://www.theses.fr/2017GREAA005/document.

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Les sources d’émissions de polluants organiques persistants (POP) dans l’atmosphère sont relativement bien connues. Une fois dans ce compartiment sous formes gazeuse et/ou particulaire, ces composés sont transportés à plus ou moins longue distance puis éliminés en fonction des conditions météorologiques par dépôts secs (aérosols) ou humides (pluie et neige). L’impact des POP est planétaire, tous les milieux de l’environnement sont touchés et les milieux aquatiques de montagne ne sont pas épargnés. Plusieurs études ont rapportées la présence de Polychlorobiphényles (PCB) et d’Hydrocarbures Arom
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Vuichard, Jean-Paul. "La Marge austro-alpine durant la collision alpine évolution tectonométamorphique de la zône Sesia-Lanzo /." Grenoble 2 : ANRT, 1988. http://catalogue.bnf.fr/ark:/12148/cb376191946.

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Günther, Dagmar. "Alpine Quergänge : Kulturgeschichte des bürgerlichen Alpinismus (1870-1930) /." Frankfurt : Campus Verlag, 1998. http://catalogue.bnf.fr/ark:/12148/cb372027948.

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Books on the topic "Alpine arc"

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Santarosa, Luca. Spazio alpino: Tutela e valorizzazione dei territori dell'Europa alpina. Gangemi, 2006.

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Dumont, Gérard-François. L' arc alpin: Histoire et géopolitique d'un espace européen. Thesis Verlag, 1998.

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1957-, Bell Allison W., ed. AMC field guide to the New England alpine summits. Appalachian Mountain Club Books, 1995.

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Gibelli, Luciano. Incisioni rupestri alpine: Testo in italiano e piemontese. F.lli Pistono, 2001.

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1856-1925, Sargent John Singer, and Metropolitan Museum of Art (New York, N.Y.), eds. John Singer Sargent's Alpine sketchbooks: A young artist's perspective. Metropolitan Museum of Art, 1991.

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Compton, Edward T. Edward Theodore Compton "pittore alpino". Museo nazionale della montagna Duca degli Abruzzi, 1993.

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Langé, Santino. Barocco alpino: Arte e architettura religiosa del Seicento : spazio e figuratività. Jaca book, 1994.

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Ghosh, Swati. Rabindrabhābanāẏa Śāntiniketane ālapanā. Ānanda Pābaliśārsa Prāibheṭa Limiṭeḍa, 2011.

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1927-, Jorio Piercarlo, and Berruti Paolo, eds. La Montagna dei segni: I mondi simbolici dell'arte alpina. Priuli & Verlucca, 1992.

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1949-, Kos Wolfgang, and Kunsthalle Wien, eds. Alpenblick: Die zeitgenössische Kunst und das Alpine : [Ausstellung, Kunsthalle Wien], 31. Oktober 1997 bis 1. Februar 1998 : [Katalog]. Stroemfeld/Roter Stern, 1997.

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Book chapters on the topic "Alpine arc"

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Gravela, Marta. "Prima dei Tuchini. Fedeltà di parte e comunità nelle valli del Canavese (Piemonte, secolo XIV)." In La signoria rurale nell’Italia del tardo medioevo. 3 L’azione politica locale. Firenze University Press, 2021. http://dx.doi.org/10.36253/978-88-5518-427-4.03.

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Famous for the late 14th-century revolt known as Tuchinaggio, the Canavese area, in north-western Piedmont, provides significant information concerning the relationship between lords and subjects in a longer time span. By analysing a wide range of sources (pastoral visitations, chronicles, court and notarial records, statutes), the essay examines the domini-homines dialectic in the first half of the 14th century: in the Canavese Alpine valleys various degrees of institutional consolidation of communities can be outlined, identifying a process of growth common to communities in the entire Alpin
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Svalova, Valentina. "Geothermics and Geodynamics of the Back-Arc Basins of the Alpine and Pacific Belts." In Heat-Mass Transfer and Geodynamics of the Lithosphere. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-63571-8_23.

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Charvet, Jacques, Michel Faure, Martial Caridroit, and André Guidi. "Some Tectonic and Tectogenetic Aspects of SW Japan: An Alpine-Type Orogen in an Island-Arc Position." In Formation of Active Ocean Margins. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4720-7_35.

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DEBELMAS, Jacques. "The Western Alpine Arc : New Data and Hypothesis." In Developments in Geotectonics. Elsevier, 1986. http://dx.doi.org/10.1016/b978-0-444-42688-8.50015-1.

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Lexa, Jaroslav. "Outline of the Alpine Geology and Metallogeny of the Carpatho-Pannonian Region." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.03.

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Abstract Volcanic-hosted ore deposits of the Carpatho-Pannonian region have been well known since the time of the Celtic and Roman empires. These deposits played an important role in the precious-metal, copper and base-metal production of these empires over their long histories. The essential volcanological and geological aspects of these deposits have been recognized only recently thanks to advances in paleovolcanic reconstructions and geotectonic analysis using principles of plate tectonics. Paleovolcanic reconstructions (e.g., Konecný, 1971; Konecný et al., 1995a; Szakács and Seghedi, 1995)
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MUELLER, S., and G. F. PANZA. "Evidence of a Deep-Reaching Lithospheric Root Under the Alpine Arc." In Developments in Geotectonics. Elsevier, 1986. http://dx.doi.org/10.1016/b978-0-444-42688-8.50010-2.

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Demoulin, Alain. "Tectonic Evolution, Geology, and Geomorphology." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0010.

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The present-day major relief features of western Europe are to a great extent determined by the underlying geological structures, either passively or actively. To get a comprehensive picture of their morphological evolution and interrelations, this chapter provides an overview of the spatial and temporal characteristics of the larg-escale tectonic framework of the continent. After having described the west European landscape at the end of the Palaeozoic, to which time the oldest preserved landforms date back, an outline of the Mesozoic and Cenozoic history of the major tectonic domains follows
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Shimabukuro, David H., and Claire Battistella. "Ligurian hyperextended continental margin preserved in an ophiolitic block at Timpa di Pietrasasso, Calabrian Arc, southern Italy." In From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid: Honoring the Career of Walter Alvarez. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2557(10).

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ABSTRACT The Cenozoic accretionary complex in the Calabrian Arc, southern Italy, contains hectometric- to kilometric-scale exposures of basalt, gabbro, and serpentinite that have been interpreted as dismembered fragments of Alpine Tethys ocean crust because of their incomplete nature with respect to the traditional view of a complete ophiolite sequence. We present new geologic mapping, geochemistry, and geochronology of one of these units at Timpa di Pietrasasso near the town of Terranova di Pollino in the Basilicata region that exposes Jurassic Tethyan pillow basalt and chert that are separat
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Kindl, Ulrike. "Die Reise der Madrisa." In Von Salzburg über Ladinien und das Aostatal bis Sizilien Wo sich Geolinguistik, Dialektometrie und Soziolinguistik treffen. Istitut Ladin Micurá de Rü, 2024. http://dx.doi.org/10.54218/festschrift.rb.207-230.

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When the glottologist Graziadio Isaia Ascoli proved the close relationship of the favelle in the Alpine Romance language islands of Grisons, Sella-Ladinia and Friuli in his famous Saggi ladini (1873), he presumed the existence of a formerly unified, closed linguistic area as the common matrix of the now isolated fragmented languages. Tracing this ancient linguistic landscape across the Alpine arc, the article attempts to show a parallel development of Rhaeto-Romanic-Ladin narrative culture, whose astonishing depth of tradition still raises many questions.Using the example of the narrative moti
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Wakabayashi, John, and David H. Shimabukuro. "The contrasting geologic record of inferred “hot” intraoceanic and “cold” continental margin subduction initiation." In From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid: Honoring the Career of Walter Alvarez. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2557(11).

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ABSTRACT Two contrasting field relationships may reflect different tectonic settings of subduction initiation preserved in orogenic belts. “Hot” subduction initiation assemblages include a large ophiolite unit (up to kms thick, extending tens to hundreds of km along strike) with supra subduction zone (SSZ) geochemical affinity that structurally overlies a thin (&amp;lt;500 m thick) sheet of high-pressure (HP), high-temperature (HT), primarily metamafic rocks called a metamorphic sole. The ophiolite generally lacks burial metamorphism and includes variably serpentinized peridotite at its base.
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Conference papers on the topic "Alpine arc"

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Di Gangi, Giorgio, Chiara Maria Lebole, Sergio Enrico Favero Longo, Laura Guglielmone, Gabriele Sartorio, and Samuele Voyron. "Alpine archaeology and everyday life at high altitudes: from the excavation to the laboratory (Orgéres-La Thuile, AO, Italy)." In 2023 IMEKO TC4 International Conference on Metrology for Archaeology and Cultural Heritage. IMEKO, 2023. http://dx.doi.org/10.21014/tc4-arc-2023.156.

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Di Gangi, Giorgio, Chiara Maria Lebole, Sergio Enrico Favero Longo, Laura Guglielmone, Gabriele Sartorio, and Samuele Voyron. "Alpine archaeology and everyday life at high altitudes: from the excavation to the laboratory (Orgéres-La Thuile, AO, Italy)." In 2023 IMEKO TC4 International Conference on Metrology for Archaeology and Cultural Heritage. IMEKO, 2023. http://dx.doi.org/10.21014/10.21014/tc4-arc-2023.156.

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Wallner, B., B. Schenk, M. Brodmann-Maeder, H. Brugger, D. Fries, and P. Paal. "Gender Differences in Hypothermia-associated Coagulopathy in Alpine Multiple Trauma Patients – Combined epidemiological and experimental prospective in-vitro Study." In AIC 2018. Georg Thieme Verlag KG, 2018. http://dx.doi.org/10.1055/s-0038-1675492.

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Sayitqulov, Ilhom. "THE EPIC INTERPRETATION OF THE IMAGE OF AMIR TEMUR IN "TEMURNOMA"." In THE PLACE OF THE ANCESTORS IN THE DEVELOPMENT OF WORLD MILITARY WORK AND MILITARY ART: AS AN EXAMPLE OF LITERARY AND HISTORICAL SOURCES. Alisher Navo'i Tashkent state university of Uzbek language and literature, 2024. http://dx.doi.org/10.52773/tsuull.conf.2024.4.5/jicv7333.

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The article shows the evolution of the character of Amir Temur from a historical figure to an epic hero in the "Temurnoma" war novel. In this process, Amir Temur's life path, military potential and activities, military skills, physical strength and battle motifs were created on the basis of folklore traditions. Also, the characteristics of the system of entrepreneurial ideas in the work are compared with the "alpine system" that forms the basis of heroic epics in folklore. Based on the analysis, the features of the character "Sahibqiran" in fiction are highlighted.
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Liping, Xiong, Liu Yanli, and Shi Danni. "Research on the Tectonic Evolution of the North Africa from Morocco to Libya as the Controlling Factor on the petroleum basins’ Hydrocarbon Accumulation." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2566974-ms.

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ABSTRACT This paper focuses on the tectonic evolution of the North African petroleum basins as the controlling factors on the major basins’ formation, evolution and the hydrocarbon accumulation, analyzing the petroleum enrichment conditions and proposing hydrocarbon accumulation mode. The analysis concludes that the distribution of North Africa Basins is in regular east-west direction, clear depression associates with highland structure. The basins becomes gradually older from the west to the east, corresponding to the Western Paleozoic basin, the Middle part Paleozoic and Mesozoic superimpose
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Yaghoubi, A., M. B. Dusseault, and Y. Leonenko. "Stress Variation Around the Balarud Lineament in the Zagros Fold and Thrust Belt and its Implication for Reservoir Geomechanics." In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0270.

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ABSTRACT We investigate horizontal stress variation in the vicinity of the deep-seated Balarud Lineament in the northern part of Iran's Dezful Embayment in the Zagros Fold and Thrust Belt (ZFTB). Both petrophysical data from drilled oil and gas wells (3-4 km deep) and earthquake focal plane solutions (6 to 25 km deep) are used to constrain the orientation and relative magnitudes of the local and regional stresses. The stress orientations in the sedimentary rock strata and the basement are of two entirely distinct types. In the basement, constant regional NE-SW SHmax orientation is observed in
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Reports on the topic "Alpine arc"

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Birk, Steffen, Christian Griebler, Johannes C. Haas, et al. Impact of extreme hydrological events on the quantity and quality of groundwater in alpine regions – multiple-index application for an integrative hydrogeo-ecological assessment. Verlag der Österreichischen Akademie der Wissenschaften, 2023. http://dx.doi.org/10.1553/ess-integrative-groundwater-assessment.

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Freshwater ecosystems in mountain areas are considered important water resources and biodiversity hotspots that are highly sensitive to changes in climate. The Alpine region is known to be particularly affected by climate change, including changes in hydrological extremes such as droughts and floods, which are expected to become more frequent and intense. Despite the importance of groundwater as a primary water resource, climate change impacts on groundwater quality, including those resulting from hydrological extremes, have been rarely addressed to date. Moreover, groundwater monitoring is cu
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Thurston, Alison, Zoe Courville, Lauren Farnsworth, et al. Microscale dynamics between dust and microorganisms in alpine snowpack. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/40079.

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Dust particles carry microbial and chemical signatures from source regions to deposition regions. Dust and its occupying microorganisms are incorporated into, and can alter, snowpack physical properties including snow structure and resultant radiative and mechanical properties that in turn affect larger-scale properties, including surrounding hydrology and maneuverability. Microorganisms attached to deposited dust maintain genetic evidence of source substrates and can be potentially used as bio-sensors. The objective of this study was to investigate the impact of dust-associated microbial depo
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Powers, Claire, Erin Borgman, Daniel Doak, Erin Borgman, Daniel Doak, and Claire Powers. Climate and species traits shape responses of alpine flora in the US Rocky Mountains to a changing world: Analysis of five GLORIA sites across the southern Rockies. National Park Service, 2024. https://doi.org/10.36967/2306920.

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The Global Observation Research Initiative in Alpine Environments (GLORIA) is a world-wide network of sites dedicated to monitoring changes in alpine flora near mountain tops. In this project we analyzed data collected at 5 sets of GLORIA monitoring sites in the Rocky Mountains of the western USA. Each site was visited between 2 and 4 times in the years spanning 2003 to 2021. These sites include four National Parks (Great Sand Dunes National Park and Preserve, Rocky Mountain National Park, Yellowstone National Park, and Glacier National Park) and one wilderness area in the Pecos Wilderness wit
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Sanders, Suzanne, Jessica Kirschbaum, and Sarah Johnson. Arctic and alpine rare plant population dynamics at Isle Royale National Park: Response to changing lake levels. National Park Service, 2022. http://dx.doi.org/10.36967/nrr-2291496.

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Arctic and alpine rare plant species populate wave-splashed rocky shorelines of Isle Royale National Park, where summer temperatures are moderated by Lake Superior. Using data from the mid-1990s and resurvey data from 1998, 2003, and 2016, we examined trajectories of change in occurrence for 25 species at 28 sites coincident with rising lake levels that followed a period of sustained low levels. We analyzed changes in site occupancy of species individually and by functional, geographic, and microhabitat groupings. We also assessed change in population structure for four focal species: Saxifrag
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Fassnacht, Steven, Kazuyoshi Suzuki, Jessica Sanow, et al. Snow surface roughness across spatio-temporal scales. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/49199.

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The snow surface is at the interface between the atmosphere and Earth. The surface of the snowpack changes due to its interaction with precipitation, wind, humidity, short- and long-wave radiation, underlying terrain characteristics, and land cover. These connections create a dynamic snow surface that impacts the energy and mass balance of the snowpack, blowing snow potential, and other snowpack processes. Despite this, the snow surface is generally considered a constant parameter in many Earth system models. Data from the National Aeronautics and Space Administration (NASA) Cold Land Processe
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Anderson, Madison. Ghosts of the High Country: Photographing Mountain Goats in the Bridger Range of Montana. Montana State University, 2025. https://doi.org/10.15788/1751922782.

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Not only do mountain goats live at the top of the world, but they have also adapted to incredibly harsh climates where few other species are found. After spending time with and observing this particular herd, I’ve learned so much about their mannerisms and personalities. The group dynamic is incredibly complex and operates similarly to how humans participate in these dynamics. Every encounter I have with these special animals gives me a deeper awe and appreciation for how capable and resilient they really are. This herd lives in a harsh, rocky, alpine environment that yields little water and l
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White, Jonathan. OF-21-03 Geologic Map of the Dry Creek Quadrangle, Delta County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2103.ovbr9253.

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The Dry Creek quadrangle, situated on the southern flank of Grand Mesa in Delta County Colorado, features high topographic relief with a 1,246.7-m (4,090 ft) variance between its highest and lowest points. The slopes in the upper third of the map area are part of the southern flank of Grand Mesa and are characterized by higher elevations and hummocky, south-facing slopes where landslide deposits overlay Paleogene to Eocene Green River and Wasatch formations. The upper hummocky terrain transitions southward to cliffy mid-elevation sandstone outcrops of the Upper Cretaceous Williams Fork and Ile
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Butterweck, Gernot, Alberto Stabilini, Benno Bucher, et al. Aeroradiometric measurements in the framework of the swiss exercise ARM23. Paul Scherrer Institute, PSI, 2024. http://dx.doi.org/10.55402/psi:60054.

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The flights of the civil (ARM23c) and military (ARM23m) parts of the exercise were performedbetween June 19th and 23rd and between September 11th and September 15th,respectively. The measuring system RLL001 was employed for all measurements. As usual, during the civil exercise the environs of some of the Swiss nuclear power plants were screened, on behalf of the Swiss Nuclear Safety Inspectorate (ENSI). At the site of the nuclear power plant Gösgen (KKG) with its pressurized water reactor, the activation products of the primary coolant loop are kept in the well shielded reactor building, thus
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Blais-Stevens, A., A. Castagner, A. Grenier, and K D Brewer. Preliminary results from a subbottom profiling survey of Seton Lake, British Columbia. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332277.

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Seton Lake is a freshwater fiord located in southwestern British Columbia, roughly 4 km west of Lillooet and 250 km north-northeast of Vancouver. Located in the Coast Mountains, it is an alpine lake about 22-km long and roughly 1-1.5 km wide. It is separated from nearby Anderson Lake, located to the west, by a large pre-historic rock avalanche deposit at Seton Portage. The lake stands at about 243 m above sea level and is up to about 150 m deep (BC gov., 1953). Water level is controlled by a hydroelectric dam (i.e., Seton dam) located at the eastern end of the lake. Here, the lake drains east
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