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Добірка наукової літератури з теми "Army of the Pyrenees"

Автор: Grafiati

Опубліковано: 23 вересня 2022

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Статті в журналах з теми "Army of the Pyrenees"

1

Ritaine, Eleanor Cashin. "Harmonising European Private International Law: A Replay of Hannibal's Crossing of the Alps?" International Journal of Legal Information 34, no. 2 (2006): 419–39. http://dx.doi.org/10.1017/s0731126500001542.

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In 218 BC, the Carthaginian general Hannibal (247-182) achieved a most extraordinary feat: he crossed both the Pyrenees Mountains and the Alps with an army of about 38.000 soldiers, 8.000 Cavalry and 37 elephants, aiming to win the Second Punic War by a bold invasion of Italy before the Romans were prepared. Even if his attempts to defeat the Roman legions failed in the end, common lore stills tells the story of the elephants crossing the Col du Mont Genevre in deep snow, setting thus an example of a near impossible achievement for generations to come.

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2

Kosykh, Tatiana. "Africa Begins at the Pyrenees? The Experience of Cross-Cultural Contact of British Soldiers in Andalusia 1810—1812." ISTORIYA 12, no. 7 (105) (2021): 0. http://dx.doi.org/10.18254/s207987840015315-5.

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In the late 18th and early 19th centuries, there was a presentation which was dominated in Britain about romantic Andalusia, which has hidden Islamic heritage of past centuries, and only the most courageous traveler can decide to take in a journey to it. With the beginning of the Napoleonic Wars and the Pyrenean campaign of the French army, everything had changed, and British soldiers became “travelers in red uniforms”. Some of them visited occupied by the French troops Andalusia in 1810—1812. This article attempts to view Andalusia as a “frontier” between Europe and Africa and to reconstruct the image of southwestern Spain in the narratives of British participants of military operations on the Iberian Peninsula. The author analyzes the peculiarities of the relationship of British officers with local inhabitants, as well as with soldiers of the enemy army, the French and the Poles, and reveals the specificity of the British perception of allies and enemies in Andalusia the context of the Spanish War of Independence.

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3

Gordienko, Dmitry O. "«The Peninsular War»: The Anglo-French confrontation in the Pyrenees during the Second Hundred Years’ War (1689–1815)." Izvestiya of Saratov University. New Series. Series: History. International Relations 21, no. 1 (March 25, 2021): 60–66. http://dx.doi.org/10.18500/1819-4907-2021-21-1-60-66.

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The article shows the Anglo-French confrontation on the Iberian Peninsula as an important stage of the Second Hundred years’ War. The example of remote action of the British expeditionary force demonstrates the «English style» of war: the operation of army troops with the active support of the Royal Navy. The author comes to the conclusion that the Pyrenean wars of the beginning of the XIX century have a certain significance in the system of Revolutionary and Napoleonic wars.

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4

Krzyżostaniak, Magdalena. "Rozmówki polsko-hiszpańskie. Problemy językowe i próby ich przezwyciężenia podejmowane przez polskich uczestników hiszpańskiej wojny o niepodległość w świetle materiałów wspomnieniowych." Annales Universitatis Paedagogicae Cracoviensis | Studia Historicolitteraria 21 (December 23, 2021): 75–86. http://dx.doi.org/10.24917/20811853.21.4.

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The article presents selected mechanisms of communication between the Polish participants of the Napoleonic campaign in 1808–1812 and the local population behind the Pyrenees. The sources of information were the memoirs of Polish soldiers fighting on the Iberian Peninsula in the Grande Armée. Even though a significant part of the memoirs focuses on the military aspects of the participation of Poles in the Peninsular War, several do provide a whole spectrum of information about the daily lives of soldiers on foreign ground and many observations regarding the customs of their brothers in arms – mainly the French – as well as the local population. Among the fragments devoted to the non-military aspects of their stay on the Iberian Peninsula, the remarks on the attempts at communication – both verbal and non-verbal – between Poles and Spaniards seem to be particularly interesting. The purpose of this article is to explain why, in many situations, efficient communication could not take place in an intermediary language (French) and how the Polish soldiers dealt with lexical and grammatical structures in the previously unknown Spanish language. It is worth pointing out that language transfer is clearly noticeable – both from the native language of the soldiers (Polish) and from French, which most of Napoleonic soldiers learnt as their first Romance language.

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5

Riggs, Ann R. "Rahner beyond the Pyrenees." Philosophy and Theology 25, no. 2 (2013): 301–9. http://dx.doi.org/10.5840/philtheol201325217.

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6

Newberry, Jacob. "December In The Pyrenees." Iowa Review 41, no. 3 (December 2011): 40–41. http://dx.doi.org/10.17077/0021-065x.7068.

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7

McGRADY, D. "L'AFRIQUE COMMENCE AUX PYRENEES." Notes and Queries 36, no. 4 (December 1, 1989): 485. http://dx.doi.org/10.1093/nq/36.4.485-a.

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8

MCMILLAN, A. A. "Geology in the Pyrenees." Geology Today 1, no. 6 (November 1985): 187–88. http://dx.doi.org/10.1111/j.1365-2451.1985.tb00335.x.

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9

Lemus-Canovas, Marc, Joan Albert Lopez-Bustins, Javier Martín-Vide, Amar Halifa-Marin, Damián Insua-Costa, Joan Martinez-Artigas, Laura Trapero, Roberto Serrano-Notivoli, and José María Cuadrat. "Characterisation of Extreme Precipitation Events in the Pyrenees: From the Local to the Synoptic Scale." Atmosphere 12, no. 6 (May 22, 2021): 665. http://dx.doi.org/10.3390/atmos12060665.

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Mountain systems within the Mediterranean region, e.g., the Pyrenees, are very sensitive to climate change. In the present study, we quantified the magnitude of extreme precipitation events and the number of days with torrential precipitation (daily precipitation ≥ 100 mm) in all the rain gauges available in the Pyrenees for the 1981–2015 period, analyzing the contribution of the synoptic scale in this type of event. The easternmost (under Mediterranean influence) and north-westernmost (under Atlantic influence) areas of the Pyrenees registered the highest number of torrential events. The heaviest events are expected in the eastern part, i.e., 400 mm day−1 for a return period of 200 years. Northerly advections over the Iberian Peninsula, which present a low zonal index, i.e., implying a stronger meridional component, give rise to torrential events over the western Pyrenees; and easterly advections favour extreme precipitation over the eastern Pyrenees. The air mass travels a long way, from the east coast of North America, bringing heavy rainfall to the western Pyrenees. In the case of the torrential events over the eastern Pyrenees, the trajectory of the air mass causing the events in these areas is very short and originates in the Mediterranean Basin. The North Atlantic Oscillation (NAO) index has no influence upon the occurrence of torrential events in the Pyrenees, but these events are closely related to certain Mediterranean teleconnections such as the Western Mediterranean Oscillation (WeMO).

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10

Marie-Claude, Bal, Vannière Boris, Galop Didier, and Rendu Christine. "Fire and human activities on the Pyrenees mountain (Western Pyrenees and Eastern Pyrenees), inferred from pedoanthracological, palynological, micro-charcoal and archaeological data." Forest Ecology and Management 234 (November 2006): S14—S15. http://dx.doi.org/10.1016/j.foreco.2006.08.030.

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Дисертації з теми "Army of the Pyrenees"

1

Baills, Henry. "Le neolithique des pyrenees roussillonnaises." Paris, EHESS, 1991. http://www.theses.fr/1991EHES0303.

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2

Adam, Claire Reid. "Geophysical investigations of the Western Pyrenees." Thesis, University of Bristol, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.357133.

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3

Gilbert, Jennie S. "Late-Hercynian volcanism of the Pyrenees." Thesis, University of Cambridge, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302843.

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4

Condado, Madera Emilio. "Les espagnols et les Cent Mille Fils de Saint Louis à l’époque de l’expédition française de 1823 en Espagne." Thesis, Aix-Marseille, 2021. http://www.theses.fr/2021AIXM0594.

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En 1823, l’intervention militaire de la France, agissant au nom de la Sainte-Alliance, met fin au régime constitutionnel et rétablit sur le trône Ferdinand VII. Cette nouvelle Guerre d’Espagne n’est pas sans susciter de fortes inquiétudes même chez ses plus fervents partisans : dix ans seulement après la désastreuse aventure napoléonienne dans la Péninsule, comment ces Espagnols qui s’étaient levés d’un commun accord contre l’Empereur réagiront-ils ? La haine des Français les poussera-t-elle à prendre de nouveau les armes et à mener cette terrible guérilla ayant fait tant de ravages dans les rangs français ? Pendant que le duc d’Angoulême progressera en Espagne, les journaux royalistes ne tariront pas d’éloges sur ces Français venus libérer leur roi et, leur attribuant toutes les qualités militaires et morales, chantent à l’envi l’entente plus que cordiale qui s’instaure immédiatement entre les sujets de Ferdinand VII et les soldats de Louis XVIII. Au-delà du discours reflété dans les déclarations officielles et la presse, où se situe la réalité ? Les Français exécrés lors du conflit antérieur ont-ils été véritablement accueillis en héros par les Espagnols? Les réactions de la Régence aux dispositions promulguées à Andujar par le duc d’Angoulême laissent deviner que l’entente entre les partisans de Ferdinand VII et le haut commandement français n’a sans doute pas été aussi cordiale qu’on a bien voulu le proclamer. Quant à la fraternisation des Espagnols avec les troupes françaises, a-t-elle été aussi effective qu’on l’a laissé entendre? C’est à toutes ces questions, parfois soulevées, mais jamais véritablement traitées par les historiens que cette thèse prétend répondre
In 1823, the military intervention of France, acting in the name of the Holy Alliance, put an end to the constitutional regime and re-established Ferdinand VII on the throne. From the outset, this new Spanish War was not without its strongest supporters : only ten years after Napoleon's disastrous adventure in the Peninsula, how would the Spaniards, who had risen up in unison against the Emperor, react? Would their Anti-French sentiment drive them to take up arms again and wage the terrible guerrilla warfare that had wreaked such havoc on the French ranks? While the Duke of Angouleme was making progress in Spain, the royalist newspapers were full of praise for these Frenchmen who had come to liberate their king and, attributing all the military and moral qualities to them, sang a more than cordial understanding that was immediately established between the subjects of Ferdinand VII and the soldiers of Louis XVIII. Beyond the rhetoric reflected in official statements and the press, what was the reality? Were the French, who had been hated in the previous conflict, really welcomed as heroes by the Spaniards? The reaction from the Regency to the provisions promulgated at Andujar by the Duke of Angouleme, suggests that the understanding between the supporters of Ferdinand VII and the French high command was probably not as cordial as it was made out to be. As for the fraternisation of the Spaniards with the French troops, was it as effective as it has been suggested? It is to all these questions, sometimes raised but never really treated by historians, that this thesis aims to answer

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5

Garwin, L. J. "Fission track dating and tectonics in the Eastern Pyrenees." Thesis, University of Cambridge, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.373658.

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6

Etchelecou, André. "Demographie et amenagement de l'espace dans les pyrenees occidentales." Paris 8, 1987. http://www.theses.fr/1987PA080149.

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La societe coutumiere dans les pyrenees occidentales etait caracterisee par une forte organisation communautaire, par la primaute de la famille sur l'individu, par l'indivision et l'inalienabilite des biens de famille, par d'importants droits d'usages sur les terres collectives, par des relations privilegiees avec les pyreneens espagnols. L'espace avait une fonction preeminente qui conditionnait l'evolution du peuplement. L'etude des comportements demographiques (fecondite, nuptialite, mortalite, migrations) du xviiie a nos jours, traduit une transition demographique differentielle par rapport a la france, qui revele une resistance durable au changement structurel et culturel impose par la france, jusque vers 1960. Avec l'ere de l'amenagement du territoire pour l'economie touristique (apres 1960), la population paysanne est devenue minoritaire. L'espace est devenu un enjeu pour le pouvoir central, puis pour le pouvoir local avec la decentralisation, et un objet de conflits sur sa fonction (sociale, ecologique, economique). Plus qu'un lieu de travail, la montagne est aujourd'hui un lieu de residence et un lieu de loisirs. L'avenir doit etre envisage avec une double preoccupation: la rationalite dans la gestion economique, et la rationalite pour la preservation de la diversite biologique; ce qui implique des reformes du processus de decision pour l'amenagement de l'espace
The country society in western pyrenees was characterized by a strong communal organization, by family primacy over person, by the coparcenary and inalienability of family's property, by importants rights of user over collectives lands, by preferential relations with spanish pyrenees. Space had a pre-eminent function from which depends the peopling evolution. The study of demographic behaviour (fecundity, marriage-rate, mortality, migrations) from xviiie till nowadays shows a differential demographic transition compared with france which reveals a lasting resistance to imposed cultural and structural change, until the end of 1960. With the territory development era for touristic economy (after 1960) country people is now a minority. The mountain space became a stake for head power, and then, with decentralization, for local power, and an object of conflicts about his fonction (social, ecologic and economic). More than a work place, to-day mountain is a place of abode and leisure. We must look at future with double cares: the rationality in economic administration and rationality for protection of biological diversity; which means reforms of process decision for space development

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7

MILIAN, JOHAN. "PROTECTION DE LA NATURE ET DEVELOPPEMENT TERRITORIAL DANS LES PYRENEES." Phd thesis, Université Toulouse le Mirail - Toulouse II, 2004. http://tel.archives-ouvertes.fr/tel-00009976.

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A l'instar des autres massifs européens, les Pyrénées ont constitué un secteur privilégié pour l'application des générations successives de politiques de protection de la nature. La relation entre celle-ci et les fonctions sociales de la montagne, longtemps appréhendée suivant une lecture antithétique, a été en pratique diversifiée. Dans un contexte d'évolution marqué par l'héritage de la désindustrialisation, la recomposition des systèmes productifs pastoral et forestier et la croissance des économies locales touristiques, les acteurs publics ont progressivement investi la protection de la nature d'objectifs sociaux qui ont complexifié sa mise en œuvre. Elle a ainsi servi de support à la construction de stratégies de recomposition de l'action collective. Des problèmes de coordination et des conflits d'intérêts se posent cependant entre la prise en compte des enjeux écologiques et l'intégration de la protection de la nature à une logique fonctionnalisée de développement territorial.

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8

Tempest, Simon Aaron. "Fluid-rock interaction in ductile shear zones, central-eastern Pyrenees." Thesis, University of Leeds, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303629.

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9

Pedley, Antony. "Eocene foreland basin carbonatae facies, the external Sierras, Spanish Pyrenees." Thesis, Royal Holloway, University of London, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261690.

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This thesis explores the controls on carbonate platform formation in foreland basins through a study of the facies, and depositional architecture, of the Middle Eocene Guara Limestone Formation, from the External Sierras, Northern Spain. The Guara Limestone Formation formed in a ramp environment on the Iberian foreland margin of the South Pyrenean Foreland Basin. The facies are foraminifera and algal limestones, with minor shallow marine siliciclastics. A facies model has been erected indicating 19 facies, grouped into 6 facies associations. Using these facies and associations, the evolution of the platform has been studied. A progradational lime-mud and clastic rich lowstand systems tract marks the initiation of deposition, the lowstand systems tract being deposited during a period of low relative sea level rise. This is overlain by an aggradational and retrogradational, carbonate grain rich, transgressive systems tract. This was deposited as the rate of relative sea level rise increased. Parasequences have been redefined herein to allow successions of a similar stratigraphic hierarchy to be encompassed in the same name. The aggradational section of the platform containing both shallowing and deepening upward parasequences. The deepening upwards parasequences were created by base level rise driven by tectonic subsidence and eustatic sea level rise. The aggradational platform margin indicates that inner-ramp production, even with the absence of coral reefs, was able to keep pace with relative sea level rise. Relative sea level rise was sufficiently rapid to preclude the development of peritidal facies and evaporites, despite suitable arid climatic conditions. Platform retrogradation, in the late transgressive systems tract, and eventual drowning, was caused by a further increase in the rate of relative sea level rise. This was created by an increase in the rate of foreland subsidence due to the formation of antiformal stacks in the Pyrenean Axial Zone to the north. Following drowning, a progradational, clastic and lime-mud rich highstand systems tract developed. Initially the rate of relative sea level rise was rapid during the highstand systems tract, this rate probably decreasing as the sequence boundary is approached. The observed increase through time of the rate of tectonic subsidence is typical of foreland basins, and is in contrast to the exponential decay of subsidence seen in passive margins. A number of other controls can be seen to have affected the Guara Limestone Formation ramp. These may affect any carbonate system; though some may be favoured specifically in foreland basin settings. Tidal action formed a series of grainstones shoals at the shelf margin, tidal effects may be favoured in narrow foreland basins due to tidal amplification, and also the limitation of wave and storm effects due to a restricted fetch. The basin was well circulated, with effective exchange between basin and platform, and salinity was normal to possibly slightly lower than normal. The biota displays a chlorozoan assemblage, but is depleted in corals due to their global decline at this time. Sediment and nutrient input onto the platform was low, leading to a resource limited environment favouring the development of large benthic foraminifera. Localised tectonics, in the form of small scale folding, produced a series of marked effects on the platform, these include: the generation of angular local unconformities, and a variation and narrowing of biofacies belts. In summary, foreland basins may display a complicated interaction between eustatic sea level variation and tectonic subsidence. In contrast to other basin types, this tectonic subsidence increases through time until eventual uplift. This provides a dominant control on the stratal architectures observed. This thesis illustrates, therefore, the potential of the use of such detailed facies and platform models to elucidate both the local, and the regional scale, controls on platform development and basin evolution.

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10

Moss, Jamie. "Tectonic controls on Eocene deltaic architecture, Jaca Basin, Spanish Pyrenees." Thesis, Durham University, 2005. http://etheses.dur.ac.uk/3730/.

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The Jaca Basin lies to the south of the Pyrenean mountain chain, in Spain, and was formed by the Late Cretaceous and Tertiary convergence between the Iberian and European tectonic plates. During the Bartonian (Middle Eocene), sediment flux from the uplifting Pyrenees was deposited in this basin as the Belsué-Atarés Fm. deltaic system. At the same time, southward propagation of deformation from the orogen created a number of emergent thrusts and thrust-related anticlines along the margins of the basin and within the basin itself. The effect that the growth of these kilometre-scale structures had on the coeval marine depositional systems is the focus of this work. Although the effects that uplifting intrabasinal structures have on fluvial systems and the effects that basin margin structures have on marine systems are well covered in the literature, the influence of intrabasinal compressive structures on coeval marine sedimentation has been largely neglected. By undertaking detailed fades, palaeocurrent and compositional analysis of the Belsué-Atarés Fm. deltaics across the Jaca Basin, it has been found that local tectonics had the strongest control on the marine sedimentation. The structurally defined basin margins largely acted as barriers to external depositional systems, causing large parts of the basin to be dominated by marl deposition. However, a total of four structurally controlled low points through the northern and southern basin margins allowed the entry of large volumes of Pyrenean axial zone sediments, beginning at 41.5 Ma. These were composed of silts, sands and pebbles, and formed the axial deltaic system. Once in the basin, a total of ten, kilometre-scale, growing thrust-related anticlines acted as barriers to the progradation of the axial system, causing facies associations to vertically aggrade behind each structure. At 37.5 Ma, after 4 Myr of vertical aggradation, a basin-wide fall in relative sea-level allowed the facies associations to rapidly prograde, breaching the crests of each of the barrier anticlines. The principal controls on the distribution of facies associations through time (sequence development) in the Jaca Basin were therefore local tectonic ones, with relative sea-level being secondary. This finding calls into question the work of the few existing studies into marine intrabasinal growth structures, which tended to use passive margin sequence stratigraphic concepts i.e. assume that relative sea-level was the primary control on sequences. The development of new techniques, such as numerical modelling, is needed before these types of complex geological situations can be fully understood. The results of this work will be of great relevance to basin dynamics and fold kinematics studies, and for hydrocarbon exploration in thrust-top basin settings.

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Книги з теми "Army of the Pyrenees"

1

With Wellington in the Pyrenees: Being an account of the operations between the Allied Army and the French from July 25 to August 2, 1813. London: T. Donovan, 1993.

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2

Greig, David. Pyrenees. London: Faber and Faber, 2005.

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3

1950-, Davies Paul, ed. The Pyrenees. London: B.T. Batsford, 1990.

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4

Jenner, Paul. Discover Pyrenees. 2nd ed. Oxford: Berlitz, 1994.

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5

Lebegue, Antoine. Connaitre les Pyrenees. Bordeaux: Sud-Ouest, 1990.

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6

CIE, MICHELIN ET. Pyrenees, Aquitaine, cote Basque. Paris: Press Michelin, 1986.

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7

Fittko, Lisa. Escape through the Pyrenees. Evanston, Ill: Northwestern University Press, 1991.

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8

Kelly, Tony. Catalonia & the Spanish Pyrenees. 3rd ed. Peterborough: Thomas Cook Pub., 2009.

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9

Stagg, Julia. Last chance in the Pyrenees. London: Hodder & Stoughton, 2015.

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10

1952-, Smith Christine, and Buckley Jonathan, eds. The Pyrenees: The rough guide. London: Harrap-Columbus, 1990.

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Частини книг з теми "Army of the Pyrenees"

1

Esdaile, Charles J. "Crisis in the Pyrenees, July–December 1813." In The Duke of Wellington and the Command of the Spanish Army 1812–14, 136–65. London: Palgrave Macmillan UK, 1990. http://dx.doi.org/10.1007/978-1-349-20702-2_6.

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2

Majeste-Menjoulas, C., and P. Debat. "Pyrenees." In Pre-Mesozoic Geology in France and Related Areas, 442–57. Berlin, Heidelberg: Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-84915-2_34.

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3

Ninot, Josep M., Empar Carrillo, and Albert Ferré. "The Pyrenees." In The Vegetation of the Iberian Peninsula, 323–66. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-54784-8_8.

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4

Perratore, Julia. "Crossing the Pyrenees." In The Regional and Transregional in Romanesque Europe, 219–33. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003162827-15.

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MacMaster, Neil. "Across the Pyrenees — David." In Spanish Fighters, 112–15. London: Palgrave Macmillan UK, 1990. http://dx.doi.org/10.1007/978-1-349-21009-1_10.

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6

Messana, Paola. "White Army, Red Army." In Soviet Communal Living, 11–13. New York: Palgrave Macmillan US, 2011. http://dx.doi.org/10.1057/9780230118102_3.

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MacMaster, Neil. "Exodus across the Pyrenees — Consuelo." In Spanish Fighters, 106–11. London: Palgrave Macmillan UK, 1990. http://dx.doi.org/10.1007/978-1-349-21009-1_9.

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8

Casas, J. M., J. J. Álvaro, S. Clausen, M. Padel, C. Puddu, J. Sanz-López, T. Sánchez-García, M. Navidad, P. Castiñeiras, and M. Liesa. "Palaeozoic Basement of the Pyrenees." In The Geology of Iberia: A Geodynamic Approach, 229–59. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10519-8_8.

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Calvet, Marc, Magali Delmas, Yanni Gunnell, and Bernard Laumonier. "Crustal Architecture of the Pyrenees." In Geology and Landscapes of the Eastern Pyrenees, 3–26. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-84266-6_1.

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Imber, Colin. "The Army." In The Ottoman Empire, 1300–1650, 262–94. London: Macmillan Education UK, 2009. http://dx.doi.org/10.1007/978-1-137-01406-1_8.

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Тези доповідей конференцій з теми "Army of the Pyrenees"

1

Tjoeng, A. Y., and R. Loro. "Viscosity Modelling of Pyrenees Crude Oil Emulsions." In SPE Asia Pacific Oil & Gas Conference and Exhibition. Society of Petroleum Engineers, 2016. http://dx.doi.org/10.2118/182326-ms.

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2

Del Rio, M., E. Serrano, I. Rico, and J. J. Tejado. "GPR prospection in the Ossoue glacier (Pyrenees)." In 2012 14th International Conference on Ground Penetrating Radar (GPR). IEEE, 2012. http://dx.doi.org/10.1109/icgpr.2012.6254949.

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3

J. Biteau, J., J. Canerot, P. Mallard, and G. Nesen. "The Main Tectono-sedimentary Domains of the Pyrenees." In 70th EAGE Conference and Exhibition - Workshops and Fieldtrips. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609.20147558.

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4

Biteau, J. J., J. M. Masset, J. J. Biteau, and M. Le Vot. "The Main Tectono-sedimentary Domains of the Pyrenees." In 79th EAGE Conference and Exhibition 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701277.

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5

Le Roux, Gaël, Adrien Claustres, Laure Gandois, Thierry Camboulives, Pilar Durantez, Marie-José Tavella, David Baqué, François De Vleeschouwer, and Anne Probst. "Atmospheric Deposition of Trace Elements over the Central Pyrenees." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1463.

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6

Brockmann, Antony, Guy Duncan, and John A. McDonald. "Hydrocarbon indicators in the Macedon‐Pyrenees Field, Western Australia." In SEG Technical Program Expanded Abstracts 2000. Society of Exploration Geophysicists, 2000. http://dx.doi.org/10.1190/1.1815840.

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V. Lbova, Lyudmila. "Paints in Paleolithic Cultures: From the Pyrenees to Siberia." In Spain: Comparative Studies oт History and Culture. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1247-5-88-95.

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8

Olmedo, Christopher. "Army UHF augmentation." In Space Programs and Technologies Conference and Exhibit. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1993. http://dx.doi.org/10.2514/6.1993-4267.

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"Army cyber institute." In 2016 International Conference on Cyber Conflict (CyCon U.S.). IEEE, 2016. http://dx.doi.org/10.1109/cyconus.2016.7836605.

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"Army cyber institute." In 2017 International Conference on Cyber Conflict (CyCon U.S.). IEEE, 2017. http://dx.doi.org/10.1109/cyconus.2017.8167494.

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Звіти організацій з теми "Army of the Pyrenees"

1

DEPARTMENT OF THE ARMY WASHINGTON DC. Army Programs: Army Energy Program. Fort Belvoir, VA: Defense Technical Information Center, February 1997. http://dx.doi.org/10.21236/ada402036.

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DEPARTMENT OF THE ARMY WASHINGTON DC. Army Programs: Army WARTRACE Program. Fort Belvoir, VA: Defense Technical Information Center, July 1995. http://dx.doi.org/10.21236/ada402044.

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3

DEPARTMENT OF THE ARMY WASHINGTON DC. Army Programs: Army International Affairs Policy. Fort Belvoir, VA: Defense Technical Information Center, April 2000. http://dx.doi.org/10.21236/ada402045.

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4

Berard, Diane L. Army After Next: A Cashless Army? Fort Belvoir, VA: Defense Technical Information Center, April 1999. http://dx.doi.org/10.21236/ada363033.

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DEPARTMENT OF THE ARMY WASHINGTON DC. Army Programs: The Army Respiratory Protection Program. Fort Belvoir, VA: Defense Technical Information Center, February 1990. http://dx.doi.org/10.21236/ada401944.

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6

Vuono, Carl E. Army Programs: Army Long-Range Planning System. Fort Belvoir, VA: Defense Technical Information Center, January 1989. http://dx.doi.org/10.21236/ada401979.

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DEPARTMENT OF THE ARMY WASHINGTON DC. Army Programs: The Army Radiation Safety Program. Fort Belvoir, VA: Defense Technical Information Center, May 1999. http://dx.doi.org/10.21236/ada402034.

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8

McCoy, William H., and Jr. Total Army Force Mix.: Reshaping America's Army. Fort Belvoir, VA: Defense Technical Information Center, April 1996. http://dx.doi.org/10.21236/ada308495.

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9

Cianciolo, Anna, and William R. Bickley. Army Instructors to Army Facilitators - Practical Considerations. Fort Belvoir, VA: Defense Technical Information Center, June 2011. http://dx.doi.org/10.21236/ada547495.

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Riley, Ryan, and John P. Steele. 2009 Center for Army Leadership Annual Survey of Army Leadership (CASAL): Army Civilians. Fort Belvoir, VA: Defense Technical Information Center, June 2010. http://dx.doi.org/10.21236/ada530103.

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