Academic literature on the topic 'Kharga, Egypt (Oasis). Temple of Hibis'

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Journal articles on the topic "Kharga, Egypt (Oasis). Temple of Hibis"

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Sultan, S. A., F. A. M. Santos, and A. Helal. "A study of the groundwater seepage at Hibis Temple using geoelectrical data, Kharga Oasis, Egypt." Near Surface Geophysics 4, no. 6 (March 1, 2006): 347–54. http://dx.doi.org/10.3997/1873-0604.2006008.

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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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Megahed, Hanaa A., Awad Hassoup, Abd El-Hay A. Farrag, and Doaa Wahba. "Modeling the Environmental Hazards of El-Kharga Oasis Sand Dunes, Western Desert of Egypt, using Remote Sensing and GIS Techniques." International Journal of Advanced Remote Sensing and GIS 10, no. 1 (July 19, 2021): 3501–20. http://dx.doi.org/10.23953/cloud.ijarsg.505.

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In this study, an integrated suite of Remote Sensing (RS) data and Geographic Information System (GIS) techniques supported by fieldwork is used to assess the sand dunes movement hazards at El-Kharga Oasis. Digital Elevation Model (DEM) data obtained from the Shuttle Radar Topography Mission (SRTM) and Advanced Spaceborne Thermal Emission and Reflection (ASTER) were integrated with GIS techniques to model the vulnerable locations and to study the terrain characteristics (slope angles and aspects) in the studied area. The risk assessment model output was verified with the field investigations using multi-temporal satellite images recorded between 1990 and 2019. Monthly wind roses showed that the sand drifts in the southeastern direction differed widely from one direction to another depending on the wind direction and velocity. The most important output of the spatial model’s, results was a geo-hazard map that classified the sand dunes hazard zones into low, slight, moderate, and high-risk zones. It is concluded that, the sand dunes pose a serious hazard because of their fast movement and accumulation near the monumental sites, over roads and invading the agricultural fields. The obtained results can serve as a basis for planners and decision-makers to take the necessary precautions and measures to minimize the sand dune hazard’s impact on the monumental sites (e.g., Hibis, El-Nadura, El-Ghueita and El-Zayyan), roads, and the agricultural fields at El-Kharga Oasis and lead to a sustainable development plan. Keywords Environmental Hazards; Sand Dunes Movement; Remote Sensing; Risk Assessment, Egypt
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Atya, M. A., H. Kamei, A. M. Abbas, F. A. Shaaban, A. Gh Hassaneen, M. A. Abd Alla, M. N. Soliman, Y. Marukawa, T. Ako, and Y. Kobayashi. "Complementary integrated geophysical investigation around Al-Zayyan temple, Kharga oasis, Al-Wadi Al-Jadeed (New Valley), Egypt." Archaeological Prospection 12, no. 3 (2005): 177–89. http://dx.doi.org/10.1002/arp.256.

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Marey Mahmoud, Hussein H. "Investigations by Raman microscopy, ESEM and FTIR-ATR of wall paintings from Qasr el-Ghuieta temple, Kharga Oasis, Egypt." Heritage Science 2, no. 1 (2014): 18. http://dx.doi.org/10.1186/preaccept-1329924074106331.

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Kamei, Hiroyuki, Magdy Ahmed Atya, Tareq Fahmy Abdallatif, Masato Mori, and Pasomphone Hemthavy. "Ground-penetrating radar and magnetic survey to the west of Al-Zayyan Temple, Kharga Oasis, Al-Wadi Al-Jadeed (New Valley), Egypt." Archaeological Prospection 9, no. 2 (2002): 93–104. http://dx.doi.org/10.1002/arp.185.

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Mahmoud, Hussein H. Marey. "Investigations by Raman microscopy, ESEM and FTIR-ATR of wall paintings from Qasr el-Ghuieta temple, Kharga Oasis, Egypt." Heritage Science 2, no. 1 (August 29, 2014). http://dx.doi.org/10.1186/s40494-014-0018-x.

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Ismael, Hossam. "Climate Effects on archaeological buildings forming the Roman temples: Dush Temple in El- Kharga Oasis, Western Desert of Egypt as a Case Study." Journal of Geography and Earth Sciences 3, no. 2 (2015). http://dx.doi.org/10.15640/jges.v3n2a4.

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Fassa, Eleni. "Προσκυνήματα στον Σάραπι. Χαρτογραφώντας τους προσκυνηματικούς τόπους του Σαράπιδος στην Αίγυπτο." Τεκμήρια 12 (January 28, 2016). http://dx.doi.org/10.12681/tekmeria.314.

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<p>After the 1971 article of G. Geraci, which gathered together the extensive evidence for Egyptian proskynemata, the practice of proskynema from a regional perspective has not attracted much scholarly attention. The present article presents and studies the documents relating to pilgrimages to Sarapis from the Hellenistic to the Imperial periods. It also places emphasis on the linguistic usage and the variations of the proskynema-expressions as well as their local character. From this analysis Abydos appears as the major centre of pilgrimages to Sarapis. The graffiti carved on the walls of the Memnonion present a lively picture of the activities of pilgrims: they visit the temple, which functions as a dream-oracle, mostly seeking healing or thanking the god for previous successful cures. Pilgrimages to Sarapis left traces of their presence (primarily dedicatory inscriptions) also at the Kharga Oasis, at Philae and as far as Lower Nubia. The literal proskynema to the Sarapieia of Egypt should be associated with the proskynema-formula that was used in letters from at least the 2<sup>nd</sup> century CE. The formula, which indirectly pertains to the literal practice of proskynema, is understood as an expression of affection towards and interest in the recipient. Finally, concerning the evolution of the Sarapis cult in general, the proskynema-evidence confirms the image of Sarapis as a major saviour god and as a personal god, to whom his adherents felt considerably attached.</p>
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Books on the topic "Kharga, Egypt (Oasis). Temple of Hibis"

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Crux-Uribe, Eugene. Hibis temple project. San Antonio: Van Siclen, 1988.

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Book chapters on the topic "Kharga, Egypt (Oasis). Temple of Hibis"

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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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