Academic literature on the topic 'Kharga, Egypt (Oasis)'

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Journal articles on the topic "Kharga, Egypt (Oasis)"

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McDonald, Mary M. A., Marcia F. Wiseman, Maxine R. Kleindienst, Jennifer R. Smith, Nicholas Taylor, Andrew J. Wreschnig, Anne R. Skinner, and Bonnie A. B. Blackwell. "Did Middle Stone Age Khargan Peoples Leave Structural Features? ‘Site J’, The Forgotten Settlement of the ‘Empty Desert’, Kharga Oasis, Egypt: 1933 and 2011." Journal of African Archaeology 14, no. 2 (January 12, 2016): 155–79. http://dx.doi.org/10.3213/2191-5784-10291.

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G. Caton-Thompson and E. W. Gardner designated new Pleistocene cultural units at Kharga Oasis in the 1930’s: both were originally termed ‘pre-Sebilian’, but were later locally named the ‘Levalloiso-Khargan’ and ‘Khargan’ industries. High on the Bulaq scarp face, a puzzling cluster of stone ‘alignments’ was discovered in 1931–32, with a reported, but discounted, association with ‘Levalloiso-Khargan’ artefacts. Gardner excavated some features in 1933. Members of the Kharga Oasis Prehistory Project relocated ‘Site J’ in January 2011, and verified the reported Khargan associations with the features. In 2008, the project found structural features associated with Khargan artefacts in the northern Gebel Yebsa survey area, confirming earlier finds in the southern oases of Kurkur and Dungul. Evidence there, and that found in Kharga and Dakhleh oases, is now designated as the Khargan Complex. The associated built stone features of the included cultural units appear to be unique in Late Pleistocene Africa, especially at Bulaq.
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Lazaridis, Nikolaos. "“Like Wringing Water from a Stone!” Information Extraction from Two Rock Graffiti in North Kharga, Egypt." Heritage 4, no. 3 (September 7, 2021): 2253–60. http://dx.doi.org/10.3390/heritage4030127.

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In the course of the last ten years, the North Kharga Oasis–Darb Ain Amur Survey team, led by Salima Ikram (American University in Cairo), has been exploring a network of interconnected desert paths in Egypt’s Western Desert, known as Darb Ain Amur. These marked paths run between Kharga Oasis and Dakhla Oasis, linking them to Darb el-Arbain, a notorious caravan route facilitating contacts between Egypt and sub-Saharan Africa since prehistoric times. Ancient travelers using the Darb Ain Amur spent several days in the midst of the Western Desert and were thus forced to use areas around sandstone rock outcrops as makeshift stopovers or camping sites. During these much-needed breaks, ancient travelers identified accessible, inscribable surfaces on the towering sandstone massifs and left on them their personalized markings. In this essay, I examine two short rock graffiti carved by such travelers in a site north of Kharga Oasis, focusing on the types of information one may extract from such ancient epigraphic materials.
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El kady, Marwa, Hassan Shokry, and Hesham Hamad. "Effect of superparamagnetic nanoparticles on the physicochemical properties of nano hydroxyapatite for groundwater treatment: adsorption mechanism of Fe(ii) and Mn(ii)." RSC Advances 6, no. 85 (2016): 82244–59. http://dx.doi.org/10.1039/c6ra14497g.

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SALAMA, Fawzy Mahmoud, Monier Mohammed ABD EL-GHANI, Ahmed Abd El Rahman AMRO, Ali El Saeid GAAFAR, and Ayat Abd El Monem ABD EL-GALIL. "Vegetation Dynamics and Species Diversity in a Saharan Oasis, Egypt." Notulae Scientia Biologicae 10, no. 3 (September 27, 2018): 363–72. http://dx.doi.org/10.15835/nsb10310296.

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The present study provides an analysis of the floristic composition, habitat types, vegetation structure and species diversity, elucidating the role of the environmental factors that affect species distribution in Kharga Oasis, Western Desert, Egypt. The vegetation was sampled from 89 permanently visited stands in 12 sites situated along N - S line transect across the oasis, and extending for about 185 km to cover as much as possible the physiognomic variation in habitats. Four main habitats were recognized and forming concentric zones (from inside to outside): farmlands and date-palm orchards represent the inner zone, the waste-salinized lands (not saltmarshes) in the middle zone, and the surrounding (bounding) desert in the outer zone. A total of 122 species from 35 families and 102 genera represented the flora of the study area. Poaceae, Asteraceae and Fabaceae were the major families, which constituted 47% of the total flora. Classification using Bray-Curtis cluster analysis produced 4 vegetation groups (A - D); each can be linked to a certain habitat. The arrangement of habitat zones along the first DCA axis can be noticed: outer zone (bounding desert), middle zone (waste-salinized lands) and inner zone (arable lands). On the other hand, farmlands and date-palm orchard groups were separated from each other along the second DCA axis. The relationship between the vegetation and soil variables was studied using Canonical Correspondence Analysis (CCA); it was indicated the most important environmental gradients those control the vegetation composition and the distribution pattern of species in Kharga Oasis, which were mainly related to gradients in soil moisture content and fine fractions. The present situation of Kharga Oasis urges the conservation of some old historic wells and the naturally growing open dom-palm forests before vanishing due to high human activities in the area.
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., Mona H. Darwish, and Samir A. Awad . "Plant Fragments from Tufa Deposits (Quaternary), Kharga Oasis, Egypt." Pakistan Journal of Biological Sciences 5, no. 11 (October 15, 2002): 1249–54. http://dx.doi.org/10.3923/pjbs.2002.1249.1254.

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Hossam, Ismael. "The Climate and Its Impacts on Egyptian Civilized Heritage: Ei-Nadura Temple in El- Kharga Oasis, Western Desert of Egypt As a Case Study." Present Environment and Sustainable Development 9, no. 1 (May 1, 2015): 5–32. http://dx.doi.org/10.1515/pesd-2015-0001.

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Abstract Undoubtedly, El-Kharga Oasis monumental sites are considered an important part of our world´s cultural heritage in the South Western Desert of Egypt. These sites are scattered on the floor of the oasis representing ancient civilizations. The Roman stone monuments in Kharga represent cultural heritage of an outstanding universal value. Such those monuments have suffered weathering deterioration. There are various elements which affect the weathering process of stone monuments: climate conditions, shapes of cultural heritages, exposed time periods, terrains, and vegetation around them, etc. Among these, climate conditions are the most significant factor affecting the deterioration Archeological sites in Egypt. El- Kharga Oasis belongs administratively to the New Valley Governorate. It is located in the southern part of the western desert of Egypt, lies between latitudes 22º30'14" and 26º00'00" N, and between 30º27'00" and 30º47'00" E. The area of El Kharga Oasis covers about 7500 square kilometers. Pilot studies were carried out on the EI-Nadura Temple, composed of sandstones originating from the great sand sea. The major objective of this study is to monitor and measure the weathering features and the weathering rate affecting the building stones forming El- Nadora Roman building rocks in cubic cm. To achieve that aims the present study used analysis of climatic data such as annual and seasonal solar radiation, Monthly average number of hours of sunshine, maximum and minimum air temperatures, wind speed, which have obtained from actual field measurements and data Meteorological Authority of El-Kharga station for the period 1941 to 2000 (60 years), and from the period 1941-2050 (110 years) as a long term of temperature data. Several samples were collected and examined by polarizing microscopy (PLM), X-ray diffraction analysis (XRD) and scanning electron microscopy equipped with an energy dispersive X-ray analysis system (SEM-EDX). The results were in agreement with the observed values in the study area. The deterioration of El-Nadora temple is above 45 % of original temple (138-161 BC), these deteriorations have occurred not only due to the age of the structures, but also due to the climate elements. It was found that the climate is the most important elements influencing weathering. El-Nadora temple is highly influenced by wind action because it has built on a hill top 180 meter in hyper arid climate and exposed to wind without any obstruction. Finally, El-Nadora Temple has lost about 42.46 % of its original size, and if the rate of deterioration on those rates will disappear the major landmarks, symbols and inscriptions fully in 2150.
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El-Rawy, Mustafa, and Florimond De Smedt. "Estimation and Mapping of the Transmissivity of the Nubian Sandstone Aquifer in the Kharga Oasis, Egypt." Water 12, no. 2 (February 23, 2020): 604. http://dx.doi.org/10.3390/w12020604.

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The Nubian sandstone aquifer is the only water source for domestic use and irrigation in the Kharga oasis, Egypt. In this study, 46 pumping tests are analyzed to estimate the transmissivity of the aquifer and to derive a spatial distribution map by geostatistical analysis and kriging interpolation. The resulting transmissivity values are log-normally distributed and spatially correlated over a distance of about 20 km. Representative values for the transmissivity are a geometric average of about 400 m2/d and a 95% confidence interval of 100–1475 m2/d. There is no regional trend in the spatial distribution of the transmissivity, but there are local clusters with higher or lower transmissivity values. The error map indicates that the highest prediction accuracy is obtained along the central north-south traffic route along which most agricultural areas and major well sites are located. This study can contribute to a better understanding of the hydraulic properties of the Nubian sandstone aquifer in the Kharga oasis for an effective management strategy.
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El-Naghy, Mohamed, Ahmed El-Shahed, Adel Fathi, and Gamal El Din Ahmed. "ALGAL FLORA OF RICE FIELDS AT EL-KHARGA OASIS, EGYPT." Egyptian Journal of Phycology 5, no. 1 (December 28, 2004): 51–69. http://dx.doi.org/10.21608/egyjs.2004.113986.

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Hewaidy, Abdel Galil A., Gamal M. El Qot, and El Sayed M. Moneer. "Campanian–early Eocene cephalopods from Kharga Oasis, Western Desert, Egypt." Annales de Paléontologie 105, no. 1 (January 2019): 45–61. http://dx.doi.org/10.1016/j.annpal.2018.10.003.

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El-Sayed, Shaimaa Sayed Mohamed, Rabea Radi Abdel Kader, and Ahmed Abo-El Yamin. "Desert Environment Effect on the Deterioration of Ancient Building Materials in Archaeological Buildings (El- Bagawat Tombs, El - Kharga Oasis as an Example)." Britain International of Exact Sciences (BIoEx) Journal 2, no. 2 (May 8, 2020): 476–85. http://dx.doi.org/10.33258/bioex.v2i2.223.

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Environmental changes have severe effect on the deterioration of archaeological buildings, desert environment distinguishes with the climatic changes daily and seasonally , which affect badly on the ancient building materials, air temperature variation, relative humidity and wind are the main factors that cause the materials degradation. This research aims to shed the light on desert environment's effect on ancient building materials at El - Bagawat tombs in El- Kharga oasis – Egypt, these tombs, return to early Coptic era, building materials samples were taken mainly mud bricks and mortars , examined and analyzed by scanning electron microscope (SEM) , EDAX unit attached to SEM and polarizing microscope to study the desert's effect , environmental measures were mentioned also like air temperature degrees , relative humidity percentages and wind's direction and speed. El-Kharga oasis is characterized by climate changes throughout the year, these changes reflect on the degradation of building materials in El-Bagawat tombs like mud bricks and mortars.
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Dissertations / Theses on the topic "Kharga, Egypt (Oasis)"

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Shalaby, M. T. "Problems of adaptation and behavioural change in new rural settlements : A case study in Kharga Oasis, Egypt." Thesis, University of Nottingham, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.373626.

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Crépy, Maël. "Les Paysages du vent : géohistoire et géoarchéologie de la dépression de Kharga (désert Libyque, Égypte) du cinquième siècle avant notre ère à nos jours : 2 500 ans d'interactions entre dynamiques éoliennes et activités humaines dans un milieu hyperaride." Thesis, Lyon, 2016. http://www.theses.fr/2016LYSE2141.

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Dans le désert Libyque (Égypte), l'un des plus arides du monde, l'action du vent trouvant peu de limites, l'ablation et le transport éoliens sont des éléments prégnants de la morphogenèse. Au cœur de ce désert, les oasis de la dépression de Kharga, nées de l'artésianisme et des activités humaines, constituent au contraire, par la profusion de l'eau et de la végétation, des secteurs où les processus de dépôt sont renforcés. L'imbrication entre une région désertique (zone-source de sédiments) et des sites oasiens (zones de dépôt), où s'appliquent des processus opposés, maximise les dynamiques éoliennes et leur impact morphogénétique. Il en découle la formation des paysages du vent, que cette thèse vise à décrire, comprendre et expliquer. Mobilisant des méthodes de géomorphologie, de géoarchéologie, de géohistoire et de sédimentologie, ce travail rend compte de l'impact paysager des interactions entre activités humaines et dynamiques éoliennes depuis la création des oasis il y a 2 500 ans. Il présente un bilan des processus naturels et anthropiques, et aborde la question des conditions de vie des oasiens depuis l'Antiquité.Trois apports principaux résultent de cette recherche :- une typologie des formations constitutives des paysages du vent- une modélisation descriptive du système à leur origine, reposant sur des cycles asynchrones de colonisation et de déprises- un bilan des grandes tendances de l'évolution environnementale et morphogénétique sur le temps long, depuis l'implantation des oasis : les paysages du vent sont nés de la distorsion entre la dégradation environnementale régionale et l'amélioration locale et temporaire des conditions édaphiques résultant des activités humaines
The limiting features of the wind dynamics are scarce in the Western desert of Egypt, one of the most arid areas in the world: eolian ablation and transport are the prevailing factors of the morphogenesis. Born from artesian waters and human activities, the oases of Kharga basin form an area where the deposition processes are stronger thanks to the large amount of water and vegetation. Eolian dynamics, and their morphogenetic impacts, are strengthened by the nesting of oasis sites (deposition areas) in a desert region (sediment source-zone). The landscapes of the wind are thus formed by the juxtaposition of these areas where opposed processes occur. This thesis aims to describe, understand and explain their development.This work based on geomorphology, geoarchaeology, « géohistoire » and sedimentology gives an account on the impacts on the landscapes of the interactions between eolian dynamics and human activities since the creation of the oases 2 500 years ago. It consists in an overview of the natural and anthropogenic processes and an assessment of the living conditions in the oasis since the Antiquity.The three main results of this research are:- a typology of the elements forming the landscapes of the wind;- a descriptive modelisation of the system at stake in their formations, which is based on an asynchronous cycle of colonisation and abandonment of the sites;- an overview of the main patterns of the long-term environmental and morphogenetic evolution since the creation of the oases.This triple contribution shows that the landscapes of the wind are born from the distortion between the regional environmental trend towards degraded conditions and the local and temporary improvements of the edaphic conditions due to human activities
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Books on the topic "Kharga, Egypt (Oasis)"

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North Kharga Oasis Survey: Explorations in Egypt's Western Desert. Peeters Publishers & Booksellers, 2018.

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H, Simmons Alan, and Mandel Rolfe D. 1952-, eds. Prehistoric occupation of a marginal environment: An archaeological survey near Kharga Oasis in the western desert of Egypt. Oxford, England: B.A.R., 1986.

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Book chapters on the topic "Kharga, Egypt (Oasis)"

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El-Rawy, Mustafa, Fathy Abdalla, and Abdelazim M. Negm. "Groundwater Characterization and Quality Assessment in Nubian Sandstone Aquifer, Kharga Oasis, Egypt." In Springer Water, 177–99. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-77622-0_8.

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Ayad, Tamer Hamdy Abd El Latif, and Shujun Ye. "The Economical and Social Impacts of Tourism on Kharga Oasis Local Citizens in Egypt." In Tourism and Hospitality Development Between China and EU, 157–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-35910-1_12.

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Skinner, Anne R., Bonnie A. B. Blackwell, Maxine R. Kleindienst, Jennifer R. Smith, Johanna M. Kieniewicz, Katherine A. Adelsberger, C. S. “Rufus” Churcher, et al. "Reconstructing Paleoenvironments in the Western Desert, Egypt: ESR Dating Freshwater Molluscs from Kharga Oasis." In ACS Symposium Series, 321–64. Washington, DC: American Chemical Society, 2013. http://dx.doi.org/10.1021/bk-2013-1147.ch019.

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Dunand, Françoise, and Roger Lichtenberg. "The Ancient Population of the Kharga Oasis." In The Great Oasis of Egypt, 30–45. Cambridge University Press, 2019. http://dx.doi.org/10.1017/9781108593274.003.

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Colburn, Henry P. "Rural Experiences: The Western Desert." In Archaeology of Empire in Achaemenid Egypt, 95–130. Edinburgh University Press, 2019. http://dx.doi.org/10.3366/edinburgh/9781474452366.003.0003.

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This chapter is concerned with the Dakhla and Kharga Oases in the Western Desert. This was an obscure region, considered by the Egyptians to be outside of Egypt proper. Population there was limited, especially after the Old Kingdom when the artesian wells dried up. This picture changes dramatically under Achaemenid rule. Several temples were established or expanded in the oasis. One of these, the Hibis Temple is the earliest example of the ‘pan-Egyptian’ temples that characterized the Ptolemaic and Roman periods. New towns were built along with these temples, and these towns were supplied with water by means of qanats, an irrigation technology that originated in Iran. The resurgence of the oasis, then, served an imperial purpose, namely to link this important strategic location more closely to centers of imperial power in the Nile valley. But, as the Demotic ostraca from Ain Manawir indicate, this act also created a thriving local economy with ties to the Mediterranean and the production of cash crops, notably castor oil, for export. Once again, the empire’s impact in the oases produced varied consequences.
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Ikram, Salima. "The North Kharga Oasis Darb Ain Amur Survey (NKODAAS): Surveying the Tracks between the Two Oases." In The Great Oasis of Egypt, 135–51. Cambridge University Press, 2019. http://dx.doi.org/10.1017/9781108593274.008.

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Bravard, Jean-Paul. "Water Resources and Irrigation in Two Oases of the Western Desert of Egypt: Kharga and Dakhla." In The Great Oasis of Egypt, 17–29. Cambridge University Press, 2019. http://dx.doi.org/10.1017/9781108593274.002.

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Agut-Labordère, Damien. "What Remains in the Hands of the Gods: Taxation in Kharga Oasis through the Demotic Ostraca (Fifth Century BC to First Century AD)." In The Great Oasis of Egypt, 122–32. Cambridge University Press, 2019. http://dx.doi.org/10.1017/9781108593274.007.

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"Observations on the Paintings of the Exodus Chapel, Bagawat Necropolis, Kharga Oasis, Egypt." In Byzantine Narrative, 233–57. BRILL, 2017. http://dx.doi.org/10.1163/9789004344877_018.

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Kleindienst, Maxine R. "Pleistocene Geoarchaeological Surveys, Kharga Oasis Prehistory Project (KOPP), 2001–2011 plus others, Western Desert of Egypt." In Proceedings of the Ninth International Dakhleh Oasis Project Conference, 37–88. Oxbow Books, 2020. http://dx.doi.org/10.2307/j.ctv138wsg1.8.

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Conference papers on the topic "Kharga, Egypt (Oasis)"

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Tawfik, M. "The concept of sustainable architecture and urbanization in Dakhla and Kharga Oases in Egypt." In ISLAMIC HERITAGE ARCHITECTURE AND ART 2016. Southampton UK: WIT Press, 2016. http://dx.doi.org/10.2495/iha160061.

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"The Concept of Sustainable Architecture and Urbanization in Dakhla and Kharga Oases in Egypt." In International Institute of Engineers. International Institute of Engineers, 2015. http://dx.doi.org/10.15242/iie.e0515038.

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