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Статті в журналах з теми "La vallée du M’Goun"

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Автор: Grafiati

Опубліковано: 7 липня 2024

Оновлено: 7 липня 2024

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1

Ait Omar, Toufik, Yahia El Khalki, Aude Nuscia Taïbi, and Mustapha El Hannani. "Les géopatrimoines de la partie nord-est du géoparc régional du M'Goun (Maroc) : représentations sociales et valorisation géotouristique." Géo-Regards 14, no. 1 (2021): 157–73. http://dx.doi.org/10.33055/georegards.2021.014.01.157.

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La partie nord-est du géoparc régional du M’Goun, appartenant en grande partie à l’Atlas de Béni Mellal, est un territoire montagnard qui présente une géodiversité remarquable. De nombreux géosites constituent une réelle ressource territoriale qui devrait être activée pour la promotion du géotourisme. Cet article vise à identifier les géosites à forte renommée sociale dans la partie nord-est du géoparc régional du M’Goun en se basant sur une enquête par questionnaire qui a permis de mettre en évidence les représentations sociales des acteurs territoriaux. Les géosites identifiés ont également été évalués. Enfin, ce travail met l’accent sur le rôle des associations locales pour la promotion du géotourisme et pour la géoconservation.

2

Barbier, Emmanuel. "Nanteuil-en-Vallée (Charente). Abbaye de Nanteuil-en-Vallée." Archéologie médiévale, no. 49 (December 20, 2019): 282–83. http://dx.doi.org/10.4000/archeomed.25170.

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3

Cooper, Danielle Chavy, and Jean-Claude Forêt. "La vallée perdue." World Literature Today 63, no. 1 (1989): 66. http://dx.doi.org/10.2307/40145056.

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4

Potte-Bonneville, Mathieu, and Ariane Chottin. "habiter la vallée." Vacarme 42, no. 1 (2008): 58. http://dx.doi.org/10.3917/vaca.042.0058.

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5

Green, M., and Chantal Chawaf. "La vallée incarnate." World Literature Today 59, no. 2 (1985): 242. http://dx.doi.org/10.2307/40141476.

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6

Marcoux, Nancy, Lucien Tessier, and Yves Bégin. "Répartition estivale du dioxyde d'azote et de l'ozone dans une vallée alpine, Chamonix, France." Géographie physique et Quaternaire 52, no. 2 (October 2, 2002): 255–64. http://dx.doi.org/10.7202/004848ar.

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Résumé Au cours de l'été 1995, la distribution des concentrations atmosphériques en dioxyde d'azote (NO 2 ) et enozone (O 3 ) a été analysée dans une vallée alpine (Chamonix, France). Sur 8 km, du fond de la vallée (1 020 m) à 2 000 m d'altitude, 42 sites répartis selon une maille de 1 km 2 ont fait l'objet de trois échantillonnages passifs hebdomadaires, du 17 juillet au 7 août 1995. Des mesures en continu des concentrations en NO 2 et en O3 effectuées simultanément sur deux des sites ont permis de vérifier les résultats obtenus par l'échantillonnage passif. Les concentrations en NO 2 s'atténuent graduellement du sud-ouest au nord-est suivant l'axe de la vallée, passant de 50,3 à 9,9 [.mu]g/m 3 . Par contre, elles diminuent rapidement avec l'altitude (de 27,3 [.mu]g/m 3 au fond de la vallée à 3,2 [.mu]g/m 3 à 2 000 m d'altitude). Les concentrations maximales sont relevées à proximité des zones de concentration du trafic routier: route principale (26 000 véhicules par jour), route d'accès au tunnel du Mont-Blanc (7 000 v/j) et aires de stationnement. L'ozone est en concentration maximale en altitude (125 [.mu]g/m 3 ) et diminue graduellement vers le fond de la vallée (67,1 [.mu]g/m 3 ). Le resserrement de la vallée dans la partie nord-est conduit à l'augmentation des concentrations dans cette zone. Le climat (turbulences de l'air, phénomènes d'inversion thermique), les phénomènes photochimiques et la configuration de la vallée sont les facteurs expliquant ce patron de distribution des concentrations en NO 2 et en O 3 dans la vallée.

7

Mori, Masahiro. "La vallée de l’étrange." Gradhiva, no. 15 (May 16, 2012): 26–33. http://dx.doi.org/10.4000/gradhiva.2311.

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8

Ayeb, Habib. "La vallée du Nil." Maghreb - Machrek N° 138, no. 4 (January 4, 1992): 64–73. http://dx.doi.org/10.3917/machr1.138.0064.

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9

Bellaoui, Ahmed. "La vallée du Zat." Téoros: Revue de recherche en tourisme 24, no. 1 (2005): 42. http://dx.doi.org/10.7202/1071109ar.

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10

Kleinhubbert, Guido, and Baptiste Touverey. "La vallée des morts." Books N° 117, no. 1 (December 7, 2021): 48–50. http://dx.doi.org/10.3917/books.117.0048.

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11

Proulx, Marc-Urbain. "Enjeux dans la Vallée." Revue Organisations & territoires 17, no. 3 (September 1, 2008): 3–4. http://dx.doi.org/10.1522/revueot.v17n3.446.

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12

Brassard, Diane, and Marc-Urbain Proulx. "Interaction dans la Vallée." Revue Organisations & territoires 17, no. 3 (September 1, 2008): 13–26. http://dx.doi.org/10.1522/revueot.v17n3.448.

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13

Hermant, Maxence. "Étienne de La Vallée." Revue de l'art N° 161, no. 3 (March 1, 2008): 29–39. http://dx.doi.org/10.3917/rda.161.0029.

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14

Triganon, A., M. Dzikowski, J. P. Novel, M. Dray, G. M. Zuppi, and A. Parriaux. "Échanges napperivière en vallée alpine : quantification et modélisation (Vallée d'Aoste, Italie)." Canadian Journal of Earth Sciences 40, no. 5 (May 1, 2003): 775–86. http://dx.doi.org/10.1139/e03-017.

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A mathematical model is applied to the Aoste Valley (Italy), which is a good example of the hydrological workings of alluvial rock basin aquifers in mountainous regions. The course of the Dorea Baltea follows the valley, which between the altitudes of 500 and 600 m is dominated by summits reaching more than 3000 m. The lacustrine- and fluviatile-type sedimentary deposits are accompanied by several alluvial cones that, due to their varying nature, confer very diverse hydrodynamic characteristics to the land. In this particular context, the source and drainage of the Dorea control the hydrodynamics of the aquifers and influence the spatial dispersion of the physicochemical properties of the groundwater. The model also led to quantify and determine the zones and types of exchanges with the river. Simulation of lowering the water table in the river showed the variable sensitivity of the water table piezometry with various spatial impacts. Finally, the streamaquifer impact is highlighted by the spatial evolution of the sulphate contents coming from deep lateral sources. Taking into account the streamaquifer exchanges in an underground-flow mathematical model gives a better understanding of the workings of the valley aquifers and thus their management, especially for the development of watercourses in mountainous regions.[Journal translation]

15

Harris, D. James, A. Carolina Varela-Pereira, J. Filipe Faria, Abderrahim S’Khifa, Diana Vasconcelos, Jonathon C. Marshall, and Tahar Slimani. "New localities and lineages of the Atlas dwarf lizard Atlantolacerta andreanskyi identified using mitochondrial DNA markers." Herpetozoa 36 (May 4, 2023): 129–34. http://dx.doi.org/10.3897/herpetozoa.36.e103068.

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Atlantolacerta andreanskyi (Werner, 1929) is an endemic lizard from the High Atlas Mountains region of Morocco. A previous molecular assessment of this species using mitochondrial and nuclear DNA markers uncovered extensive genetic diversity with seven lineages indicative of a species complex. A morphological assessment of six of these lineages did not establish simple diagnostic features, and proposed these should be considered as a cryptic species, while highlighting the need for greater sampling across the range. In this study, we sampled 8 individuals from 5 previously unsampled localities and carried out genetic analyses to compare these populations to the known variation. Phylogenetic reconstruction based on mitochondrial DNA markers (12S rRNA and ND4) corroborates the previously described lineages and identified a new one. Interestingly, the two samples that account for this newly identified lineage have been collected from distinct localities – M’goun and Toumliline – that form a sister taxon to the population of Jbel Azourki.

16

Krasniqi, Xh Z. "Applications of the deferred de la Vallée Poussin means of Fourier series." Asian-European Journal of Mathematics 14, no. 10 (April 14, 2021): 2150179. http://dx.doi.org/10.1142/s1793557121501795.

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In this paper, we have proved four theorems on deferred generalized De la Vallée Poussin summability of Fourier series. Some results obtained previously by others, pertaining to generalized De la Vallée Poussin summability of Fourier series, are particular cases of ours.

17

VanCour, Shawn, and Chloe Patton. "From Songfilms to Telecomics: Vallée Video and the New Market for Postwar Animation." Animation 15, no. 3 (November 2020): 207–28. http://dx.doi.org/10.1177/1746847720964886.

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From 1948–1952, Rudy Vallée, a successful performer whose career spanned radio, film, recorded music and stage entertainment, expanded his operations into the burgeoning US television market with the launch of his independent production company, Vallée Video. One of hundreds of forgotten companies that arose during this period to meet growing demand for programming content, Vallée Video offers an important case study for understanding animation workers’ role in postwar television production. Drawing on corporate records and films preserved in the Rudy Vallée Papers at California’s Thousand Oaks Library and the UCLA Film and Television Archive, the authors’ analysis documents Vallée’s use of freelance artists and external animation houses for work ranging from camera effects for illustrated musical shorts to animated commercials and original cartoon series. These productions demonstrate the fluid movement of animation labor from theatrical film to small screen markets and participated in larger aesthetic shifts toward minimalist drawing styles and limited character animation that would soon dominate mid-20th century US television.

18

Schulz, O., and C. de Jong. "Snowmelt and sublimation: field experiments and modelling in the High Atlas Mountains of Morocco." Hydrology and Earth System Sciences 8, no. 6 (December 31, 2004): 1076–89. http://dx.doi.org/10.5194/hess-8-1076-2004.

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Abstract. Snow in the High Atlas Mountains is a major source for freshwater renewal and for water availability in the semi-arid lowlands of south-eastern Morocco. Snowfall- and snow-ablation monitoring and modelling is important for estimating potential water delivery from the mountain water towers to the forelands. This study is part of GLOWA-IMPETUS, an integrated management project dealing with scarce water resources in West Africa. The Ameskar study area is located to the south of the High Atlas Mountains, in their rain shadow. As a part of the M’Goun river basin within the upper Drâa valley, the study area is characterised by high radiation inputs, low atmospheric humidity and long periods with sub-zero temperatures. Its altitude ranges between 2000 m and 4000 m, with dominant north- and south-facing slopes. Snowfall occurs mainly from November to April but even summit regions can become repeatedly devoid of snow cover. Snow cover maps for the M’Goun basin (1240 km2) are derived from calculations of NDSI (Normalized Difference Snow Index) from MODIS satellite images and snow depth is monitored at four automatic weather stations between 2000–4000 m. Snowfall events are infrequent at lower altitudes. The presence of snow penitentes at altitudes above 3000 m indicates that snow sublimation is an important component of snow ablation. Snow ablation was modelled with the UEB Utah Energy Balance Model (Tarboton and Luce, 1996). This single layer, physically-based, point energy and mass balance model is driven by meteorological variables recorded at the automatic weather stations at Tounza (2960 m) and Tichki (3260 m). Data from snow pillows at Tounza and Tichki are used to validate the model’s physical performance in terms of energy and water balances for a sequence of two snowfall events in the winter of 2003/4. First UEB modelling results show good overall performance and timing of snowmelt and sublimation compared to field investigations. Up to 44% of snow ablation is attributed to snow sublimation in typical winters with subzero temperatures and low atmospheric humidity at an altitude of 3000 m. At altitudes below 3000 m snowmelt generally dominates over sublimation. Unfortunately, the highest altitude zones suffer long periods with direct water loss into the atmosphere by sublimation in the course of which they cannot contribute to direct runoff or groundwater formation in the southern High Atlas Mountains. Keywords: sublimation, snow ablation modelling, energy balance model, High Atlas Mountains

19

Guillot, Florence. "Auzat (Ariège). Vallée de Soulcem." Archéologie médiévale, no. 45 (December 1, 2015): 294. http://dx.doi.org/10.4000/archeomed.8159.

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20

Meyer, Philippe. "Dans cette vallée de larmes." Commentaire Numéro77, no. 1 (1997): 160. http://dx.doi.org/10.3917/comm.077.0160.

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21

Lebaillif, Sylvain. "Une vallée industrieuse : Fontaine-Guérard." Études Normandes 54, no. 3 (2005): 35–38. http://dx.doi.org/10.3406/etnor.2005.1602.

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22

Nicolle, Hervé. "Qu’elle était verte ma vallée." Revue des mondes musulmans et de la Méditerranée, no. 133 (June 8, 2013): 227–38. http://dx.doi.org/10.4000/remmm.8118.

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23

Allain, Jean-Marie. "Une vallée urbaine : la Sambre." Les Annales de la recherche urbaine 30, no. 1 (1986): 89–98. http://dx.doi.org/10.3406/aru.1986.1240.

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24

Perron, Marco. "Enquête toponymique en Vallée d'Aoste." Nouvelle revue d'onomastique 15, no. 1 (1990): 115–20. http://dx.doi.org/10.3406/onoma.1990.1052.

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25

Cornelius, Nathalie G. "La vallée par Bernard Minier." French Review 94, no. 3 (2021): 274–75. http://dx.doi.org/10.1353/tfr.2021.0065.

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26

Benhessa, Ghislain, and Nathalie Bittinger. "Qu’elle était verte ma vallée." Esprit Janvir-févrir, no. 1 (2018): 192. http://dx.doi.org/10.3917/espri.1801.0192.

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27

Ghesquière, Emmanuel. "Des feux dans la vallée." Revue archéologique de l'Ouest, no. 26 (December 31, 2009): 312–13. http://dx.doi.org/10.4000/rao.941.

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28

Blanchard, Maxime. "L’aliénation tranquille:C.R.A.Z.Y.de Jean-Marc Vallée." Contemporary French and Francophone Studies 13, no. 1 (January 2009): 71–79. http://dx.doi.org/10.1080/17409290802606846.

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29

Esi, Ayhan. "Statistical Summability through de la Vallée-Poussin Mean in Probabilistic Normed Spaces." International Journal of Mathematics and Mathematical Sciences 2014 (2014): 1–5. http://dx.doi.org/10.1155/2014/674159.

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Two concepts—one of statistical convergence and the other of de la Vallée-Poussin mean—play an important role in recent research on summability theory. In this work we define a new type of summability methods and statistical completeness involving the ideas of de la Vallée-Poussin mean and statistical convergence in the framework of probabilistic normed spaces.

30

Muller, Emmanuel. "La vallée de la Thur (Haut-Rhin) : aperçu sur les structures industrielles d'une vallée vosgienne." Revue Géographique de l'Est 32, no. 2 (1992): 105–25. http://dx.doi.org/10.3406/rgest.1992.2222.

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31

Schmitz, Jean. "Évolution contrastée de l’agro-pastoralisme dans la Vallée du fleuve Sénégal (Delta et Moyenne Vallée)." Natures Sciences Sociétés 3, no. 1 (January 1995): 54–58. http://dx.doi.org/10.1051/nss/19950301054.

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32

Kchikach, Nisrine, Hassan Ibouh, Abderrahim Benali, Anas Charbaoui, and Abdelhafid El Alaoui El Fels. "Digital Promotion of Geoheritage along a Tourist Route in M’Goun UNESCO Geopark (Central High Atlas, Morocco) and Visitor Typology Analysis." Geosciences 14, no. 6 (May 23, 2024): 141. http://dx.doi.org/10.3390/geosciences14060141.

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In the digital era, highlighting the heritage resources of a mountainous region involves describing and advertising them to promote their visibility and attractiveness. Previous studies mainly assess the natural resources of such regions through a multi-indicator descriptive evaluation. This study aims to develop an effective evaluation of such indicators along the main tourist route of the M’Goun UNESCO Global Geopark, located in the central High Atlas of Morocco. The implementation of an experiential method to assess the tourism characteristics of this region is a notable aspect of our study. It includes analyzing the criteria for choosing this destination by segmenting tourists’ consumption experiences. Statistical data analysis has identified five dimensions of destination choice and four visitor groups. Additionally, we created an interactive map and made it accessible online to promote the natural geoheritage of this region. This article proposes to discuss the findings of this research and their applicability in terms of tourism destination management and decision-making, which can assist local governments in allocating tourism resources and land use rationally.

33

Labelle, Claude, and Pierre J. H. Richard. "Histoire Postglaciaire de la Végétation dans la Région de Mont-Saint-Pierre, Gaspésie, Québec." Géographie physique et Quaternaire 38, no. 3 (November 29, 2007): 257–74. http://dx.doi.org/10.7202/032567ar.

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RÉSUMÉLes analyses pollinique et macrofossile de sédiments de deux lacs des environs de Mont-Saint-Pierre (Gaspésie), l'un dans la vallée côtière, l'autre sur le plateau, permettent de reconstituer l'histoire postglaciaire de la végétation dans deux situations physiographiques contrastées. Seul le plateau a été colonisé par une végétation initiale de type toundra (> 10 400 ans BP), pendant que la vallée était encore en partie ennoyée par la mer de Goldthwait. L'afforestation du plateau fut caractérisée d'abord par des populations de Picea sp., accompagné de Populus sp. et Larix laricina, puis par un envahissement progressif par Abies balsamea et Betula papyrifera. La baisse de la représentation pollinique de l'aulne vert (Alnus cf. crispa), maximale durant l'afforestation, paraît être un indicateur assez fidèle de la fermeture de la couverture forestière. Cette phase se termine vers 9000 ans BP sur le plateau. Le rythme de l'afforestation a été différent dans la vallée. Des taxons héliophiles s'y sont maintenus plus longtemps, ce qui peut être relié à l'activité des versants abrupts qui flanquent la vallée. Malgré des variations de l'abondance relative des arbres, la sapinière à bouleau blanc a sans doute occupé le plateau depuis 9000 ans BP environ. Par contre, la végétation de la vallée s'est passablement modifiée jusque vers 5000 à 4500 ans BP, par la migration successive de Betula alleghaniensis, de Pinus strobus, de Fraxinus nigra, dAcer saccharum et d'Ulmus americana. L'implantation progressive de ces arbres relativement thermophiles est à l'origine de la diversité du paysage actuel de la vallée. Ces reconstitutions permettent d'écarter l'hypothèse de Dansereau (1944) selon laquelle les érablières à Acer saccharum de la Gaspésie seraient des groupements hérités de l'optimum climatique de l'Holocène moyen, au cours duquel les érablières auraient été largement répandues sur le territoire. Les données montrent que ces érablières datent de l'Holocène Supérieur, la migration d'Acer saccharum ayant sans doute été freinée par des barrières topo-climatiques entraînant une discontinuité prononcée des habitats pouvant accueillir cette espèce.

34

Schaeben, H. "The de la Vallée Poussin Standard Orientation Density Function." Textures and Microstructures 33, no. 1-4 (January 1, 1999): 365–73. http://dx.doi.org/10.1155/tsm.33.365.

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The de la Vallée Poussin standard orientation density function νκ(ω)=C(κ)cos⁡2κ(ω/2) is discussed with emphasis on the finiteness of its harmonic series expansion which, advantageously distinguishes it from other known standard functions. Given its halfwidth, the de la Vallée Poussin standard orientation density function allows, for example, to tabulate the degree of series expansion into harmonics required for its exact representation.

35

Youssef, Gharnit, Moujane Abdelaziz, Outourakht Aboubakre, Aziz Hasib, and Abdelali Boulli. "Impact of climate and demographic changes on the vegetation of the M’goun Geopark UNESCO of Morocco (1984-2021)." Investigaciones Geográficas, no. 81 (January 26, 2024): 225–43. http://dx.doi.org/10.14198/ingeo.25433.

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The primary goal of this study is to identify changes in the vegetation cover of the geopark M’goun region of Morocco, as a sample area to track the Moroccan vegetation status, and the crucial factors that influenced its evolution between 1984 and 2021. The NDVI (Normalized Difference Vegetation Index) method has been used, combined with supervised classification manipulated with the Google Earth Engine and through statistical analysis using R, together with field trips and Google Earth records for supervised classification. The percentage of vegetation density, made up of oak groves, Matorrals, red juniper, and thuja, in addition to a highly biodiverse cover, displays a declining trend. Medium-cover vegetation decreased by 29.5%, dense vegetation decreased considerably by 70.9%, and low-cover vegetation saw a minimal decline of 0.02%. As a result, dense and medium vegetation are being replaced by bare lands or poor-quality cover formed by sparse plants and solitary trees. In addition, precipitation increased slightly, showing an irregular trend, with average minimum and maximum temperatures rising by +1.7°C and +1.4°C, respectively. Furthermore, the population increased by 84.47%. Statistical analysis showed that the most important parameters affecting medium and dense vegetation cover are temperatures (Tmin and Tmax) and population density, as evidenced by the strong correlation between them. In contrast, sparse vegetation cover showed less correlation due to its heterogeneity. However, precipitation played a minimal role in vegetation evolution. Change detection maps revealed a significant negative impact on vegetation cover. This degradation was localized in the southern part of the area of study, where, according to the demographic density map, the majority of the population resides. Deforestation continues due to the lifestyle and economic activities of the local population. These factors, combined with climate change, are exerting large-scale pressure on the forest throughout the geopark.

36

Chomette, Guy-Pierre. "La Vallée de Ferghana, poudrière environnementale." Les Cahiers de l'Orient 89, no. 1 (2008): 113. http://dx.doi.org/10.3917/lcdlo.089.0113.

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37

Bétemps, Alexis. "Rimailles de clocher en Vallée d'Aoste." Le Monde alpin et rhodanien. Revue régionale d’ethnologie 16, no. 3 (1988): 41–49. http://dx.doi.org/10.3406/mar.1988.1381.

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38

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Claude, Viviane, and André Guillerme. "La vallée de l'Orge. 1880-1977." Les Annales de la recherche urbaine 30, no. 1 (1986): 78–88. http://dx.doi.org/10.3406/aru.1986.1239.

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Ghesquiere, Emmanuel. "Écouché (Orne). Vallée de l’Udon 2." Archéologie médiévale, no. 42 (December 1, 2012): 192. http://dx.doi.org/10.4000/archeomed.10803.

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Triolet, Laurent. "Nanteuil-en-Vallée (Charente). La Robinetrie." Archéologie médiévale, no. 41 (December 1, 2011): 208–9. http://dx.doi.org/10.4000/archeomed.11867.

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Pépin, M. "Fièvre de la vallée du Rift." Médecine et Maladies Infectieuses 41, no. 6 (June 2011): 322–29. http://dx.doi.org/10.1016/j.medmal.2010.12.010.

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Usher, Michael B. "The Vallée de Mai, Praslin, Seychelles." Environmental Conservation 20, no. 4 (1993): 356–58. http://dx.doi.org/10.1017/s0376892900023572.

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Thibaudier, Viviane. "« La vallée où poussent les âmes »." Cahiers jungiens de psychanalyse 137, no. 1 (2013): 27. http://dx.doi.org/10.3917/cjung.137.0027.

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Ferreira, Rui A. C. "Fractional de la Vallée Poussin inequalities." Mathematical Inequalities & Applications, no. 3 (2019): 917–30. http://dx.doi.org/10.7153/mia-2019-22-62.

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47

Bertolucci, Bernardo. "Le cavalier de la vallée solitaire." 1895, no. 95 (October 1, 2021): 152–57. http://dx.doi.org/10.4000/1895.9002.

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Harzoune, Mustapha. "Soufiane Khaloua, La Vallée des Lazhars." Hommes & migrations, no. 1344 (January 1, 2024): 183. http://dx.doi.org/10.4000/hommesmigrations.17042.

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Ferraroni, Roberto. "Cécile Vallée, Ananda Devi écrivaine mauricienne." Studi Francesi 202 (LXVIII | I) (2024): 238–39. http://dx.doi.org/10.4000/11wln.

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50

Kinj, Ahmed, Mohammad Ali, and Suleiman Mahmoud. "Approximation Properties of de la Vallée-Poussin sums in Morrey spaces." Sultan Qaboos University Journal for Science [SQUJS] 22, no. 2 (January 28, 2018): 89. http://dx.doi.org/10.24200/squjs.vol22iss2pp89-95.

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Анотація:

In this paper, we investigate the problem of the deviation of a function from its de la Vallée-Poussin sums of Fourier series in Morrey spaces defined on the unite circle in terms of the best approximation to . Moreover, approximation properties of de la Vallée-Poussin sums of Faber series in Morrey-Smirnov classes of analytic functions, defined on a simply connected domain bounded by a curve satisfying Dini's smoothness condition are obtained.