Canals and Harbors in the Time of Giza Pyramid-Building by Mark Lehner
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Cambridge Archaeological Journal 15:2, 2005
Location of the Old Kingdom Pyramids in Egypt Miroslav Bârta The principal factors influencing the location of the Old Kingdom pyramids in Egypt are reconsidered. The decisive factors influencing their distribution over an area of c. eighty kilometres were essentially of economic, géomorphologie, socio-political and unavoidably also of religious nature. Primary importance is to be attributed to the existence of the Old Kingdom capital of Egypt, Memphis, which was a central place with regard to the Old Kingdom pyramid fields. Its economic potential and primacy in the largely redistribution- driven state economy sustained construction of the vast majority of the pyramid complexes in its vicinity. The location of the remaining number of the Old Kingdom pyramids, including many of the largest ever built, is explained using primarily archaeological evidence. It is claimed that the major factors influencing their location lie in the sphere of general trends governing ancient Egyptian society of the period. For millennia, megaliths and monumental arts were pyramids see Edwards 1993; Fakhry 1961; Hawass commissioned by the local chieftains and later by the 2003; Lehner 1997; Stadelmann 1985; 1990; Vallogia kings of Egypt. The ideological reasons connected 2001; Verner 2002; Dodson 2003). The reasons that may with the construction and symbolism of the pyra be put forward to explain their location and arrange mids were manifold, and in most cases obvious: the ment are numerous but may be divided into two basic manifestation of power, status and supremacy over groups: practical and religious. It will be argued that the territory and population, the connection with the whereas the general pattern in the distribution of the sacred world and the unlimited authority of the rulers pyramid sites may be due mainly to practical reasons, (O'Connor & Silverman 1995). -
Was the Function of the Earliest Writing in Egypt Utilitarian Or Ceremonial? Does the Surviving Evidence Reflect the Reality?”
“Was the function of the earliest writing in Egypt utilitarian or ceremonial? Does the surviving evidence reflect the reality?” Article written by Marsia Sfakianou Chronology of Predynastic period, Thinite period and Old Kingdom..........................2 How writing began.........................................................................................................4 Scopes of early Egyptian writing...................................................................................6 Ceremonial or utilitarian? ..............................................................................................7 The surviving evidence of early Egyptian writing.........................................................9 Bibliography/ references..............................................................................................23 Links ............................................................................................................................23 Album of web illustrations...........................................................................................24 1 Map of Egypt. Late Predynastic Period-Early Dynastic (Grimal, 1994) Chronology of Predynastic period, Thinite period and Old Kingdom (from the appendix of Grimal’s book, 1994, p 389) 4500-3150 BC Predynastic period. 4500-4000 BC Badarian period 4000-3500 BC Naqada I (Amratian) 3500-3300 BC Naqada II (Gerzean A) 3300-3150 BC Naqada III (Gerzean B) 3150-2700 BC Thinite period 3150-2925 BC Dynasty 1 3150-2925 BC Narmer, Menes 3125-3100 BC Aha 3100-3055 BC -
The Iconography of the Princess in the Old Kingdom 119 Vivienne G
THE OLD KINGDOM ART AND ARCHAEOLOGY PROCEEDINGS OF THE CONFERENCE HELD IN PRAGUE, MAY 31 – JUNE 4, 2004 Miroslav Bárta editor Czech Institute of Egyptology Faculty of Arts, Charles University in Prague Academia Publishing House of the Academy of Sciences of the Czech Republic Prague 2006 OOKAApodruhéKAApodruhé sstrtr ii–xii.indd–xii.indd 3 99.3.2007.3.2007 117:18:217:18:21 Contributors Nicole Alexanian, James P. Allen, Susan Allen, Hartwig Altenmüller, Tarek El Awady, Miroslav Bárta, Edith Bernhauer, Edward Brovarski, Vivienne G. Callender, Vassil Dobrev, Laurel Flentye, Rita Freed, Julia Harvey, Salima Ikram, Peter Jánosi, Nozomu Kawai, Jaromír Krejčí, Kamil O. Kuraszkiewicz, Renata Landgráfová, Serena Love, Dušan Magdolen, Peter Der Manuelian, Ian Mathieson, Karol Myśliwiec, Stephen R. Phillips, Gabriele Pieke, Ann Macy Roth, Joanne M. Rowland, Regine Schulz, Yayoi Shirai, Nigel Strudwick, Miroslav Verner, Hana Vymazalová, Sakuji Yoshimura, Christiane Ziegler © Czech Institute of Egyptology, Faculty of Arts, Charles University in Prague, 2006 ISBN 80-200-1465-9 OOKAApodruhéKAApodruhé sstrtr ii–xii.indd–xii.indd 4 99.3.2007.3.2007 117:18:217:18:21 Contents Foreword ix Bibliography xi Tomb and social status. The textual evidence 1 Nicole Alexanian Some aspects of the non-royal afterlife in the Old Kingdom 9 James P. Allen Miniature and model vessels in Ancient Egypt 19 Susan Allen Presenting the nDt-Hr-offerings to the tomb owner 25 Hartwig Altenmüller King Sahura with the precious trees from Punt in a unique scene! 37 Tarek El Awady The Sixth Dynasty tombs in Abusir. Tomb complex of the vizier Qar and his family 45 Miroslav Bárta Die Statuen mit Papyrusrolle im Alten Reich 63 Edith Bernhauer False doors & history: the Sixth Dynasty 71 Edward Brovarski The iconography of the princess in the Old Kingdom 119 Vivienne G. -
Reconstructing an Extreme Flood from Boulder Transport and Rainfall–Runoff
Global and Planetary Change 70 (2010) 64–75 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Reconstructing an extreme flood from boulder transport and rainfall–runoff modelling: Wadi Isla, South Sinai, Egypt Alan E. Kehew a,⁎, Adam Milewski a, Farouk Soliman b a Geosciences Dept., Western Michigan Univ., Kalamazoo, MI 49008, USA b Geology Department, Faculty of Science, Suez Canal University, Ismailia, Egypt article info abstract Article history: The Wadi Isla drainage basin, a narrow steep bedrock canyon and its tributaries, rises near the highest elevations Accepted 6 November 2009 of the Precambrian Sinai massif on the eastern margin of the tectonically active Gulf of Suez rift. The basin area Available online 17 November 2009 upstream from the mountain front is 191 km2 and downstream the wadi crosses a broad alluvial plain to the Red Sea. Stream-transported boulders within the lower canyon (up to 5 m in diameter) and in a fan downstream Keywords: indicate extremely high competence. In one reach, a 60-m-long boulder berm, ranging in height from 3 to 4 m, lies palaeoflood along the southern wall of the canyon and contains boulders 2–3 m in diameter. Boulder deposits beyond the Sinai rainfall–runoff model mouth of the canyon generally appear to be less than several metres thick and are composed of imbricated, well- boulder transport sorted boulders. The last flood that deposited these boulders is believed to have been a debris torrent with a low flash floods content of fines. Mean intermediate diameter decreases from about 1.5 m just beyond the mouth of the canyon, where the channel width expands to 300 m, to about 0.5 m downstream to the point at which the valley is no longer confined on its south side. -
Wadi Ar Rumah the Earth Longest Dry Watershed Analysis System Using Remote Sensing Thermal Data
WADI AR RUMAH THE EARTH LONGEST DRY WATERSHED ANALYSIS SYSTEM USING REMOTE SENSING THERMAL DATA Sultan Ibn Sultan Al Qassim University P.O.Box 6688. Al Qassim 51452, College of Agricultur, Saudi Arabia. Tel: +96663342440, Fax: +96663340366 E-mail: [email protected] Abstract Wadi Ar Rumah watershed system analysis combining both the information in the Advanced Very High Resolution Radiometer (AVHRR) visible/near-infrared bands in terms of Normalized Difference Vegetation Index (NDVI) and in the thermal-infrared bands in terms of Land Surface Temperature (LST) is presented. The analysis is based in the LST-NDVI feature space. This permits characterizing the distribution and evolution of the different regions according to their vegetation and watershed systems. The Pathfinder AVHRR Land (PAL) data analysis has been carried out to investigate the changes in the biophysical characteristics of land cover and the water system pattern. The PAL data corresponds to the month of February for the years of 1997, 1998 and 1999. The Arabian Peninsula in general was selected as the area of study due to its high environmental diversity. Wadi Ar Rumah was especially selected because it was flooded by heavy precipitation during end of 1997 to beginning of 1998. Precipitation saturated the ground surface soil and kept the wet condition for a time. This work proved the wadi AR RUMAH as the earth longest watershed drainage system in our plant. Keywords: Watershed system, desert vegetation, AVHRR, NDVI, LST. 1. Introduction water, Solar radiation, and vegetation govern natural environment in the Arabian Peninsula. This research examines whether space observations are useful on the site to study the phenomena of the region. -
366 Water in Deserts
Geo Factsheet www.curriculum-press.co.uk Number 366 Water in Deserts Figure 1 The global distribution of deserts ● The sparsity of vegetation cover means that there is The action of flowing water, both in the present and past, is, and has an absence of plant roots. Humus in the soils is limited; been, important in shaping desert landscapes. Rainfall quantities in existing soils are compact and infiltration is limited. deserts are low overall but rainfall events that do occur can have a ● Interception is minimal. The rainfall hits the ground marked influence on the landscape. Many landforms in deserts are and dislodges fine, loose particles, moving them by rain shaped by the action of rivers and the water that flows into and / or splash. They can resettle and become lodged in any pore through the region. Figure 1 shows the global distribution of deserts. spaces that did exist in the soil, acting to ‘plug’ the gaps and create a top soil layer which has reduced permeability. Rainfall in deserts Such soils can only allow rainwater to infiltrate at a rate Desert regions can be classed as hyper-arid, arid or semi-arid of around a few mm per hour, so any excess rainfall will depending on the average annual precipitation that they receive: build up on, and flow over, the ground surface. Hyper-arid zones have a mean annual precipitation value of less than 100mm; Arid zones have an annual rainfall total of less than 250 mm; Semi-arid areas have an average annual precipitation of 250-500 mm. -
A Low Cost Approach for Wadi Flow Diversion
~ low cost approach for wadi flow diversion G. L. Silva and M. L. Makin Overseas Development Natural Resources Institute Surbiton, UK 1. Introduttion The whole system comprised 25 canals, fed by low A study of the land and wlUer resources of the Wadi Rima rubble and brushwoOd deflectors. and some ten earth bar coastal plain (YAR) was undertaken between 1974 and rages (aqm) in the downstream reach where spates had 1977 by the Land Resources Division (LRD)aspartofthe generally lost momentum. Ideally. the canal iQUlkes were British Technical Assi$tance programme (Makin, 1977). set in the wadi bank on the outer side of bends to enhance One of the majorproposalsemanating from that study was the collection offlood recessiOn and base flows. the intake for reSlNcturing the traditional system of spate diversion heads being open and uncontrolled., The wadi is partially and irrigation. ' incised within an elevated alluvial fan. so each canal is The Yemen coastal plain ('Tihamah') comprises ex capable of commanding extensive areas without heading tensiveatluvial fans and terraces flanking the mountains of up. the interior. Lying close to sea level, the plain is hotanddry The area irrigated in any one season with single to triple withashon,erratiesnmmerrainyseason,andevaporation waterings averaged about 6 700 ha out of an estimated exceeding 2 500 mm per year. Mean annual rainfall4e 8 000 ha; some distant fields might only be irrigated once creases frOm 3S0mm atthefootofthemounqUns,tobelow or twice in a decade. Other areas have been deprived of 100 mm on the Red Sea coast. In general, only low yields water through the illegal development of new irrigation; ofdrought-tolerantcropsareproducedandwaterresources here increasing numbers of people claim rights to wadi ate intensively exploited for irrigation, the principallimi water. -
Vulnerability of Soils in the Watershed of Wadi El Hammam to Water Erosion (Algeria) 5
DOI: 10.1515/jwld-2015-0001 © Polish Academy of Sciences, Committee for Land Reclamation JOURNAL OF WATER AND LAND DEVELOPMENT and Environmental Engineering in Agriculture, 2015 J. Water Land Dev. 2015, No. 24 (I–III): 3–10 © Institute of Technology and Life Science, 2015 PL ISSN 1429–7426 Available (PDF): http://www.itp.edu.pl/wydawnictwo/journal;http://www.degruyter.com/view/j/jwld Received 25.10.2014 Reviewed 10.02.2015 Accepted 13.03.2015 Vulnerability of soils A – study design B – data collection in the watershed of Wadi El Hammam C – statistical analysis D – data interpretation E – manuscript preparation to water erosion (Algeria) F – literature search Mohamed GLIZ1) ABDEF, Boualem REMINI2) ADEF, Djamel ANTEUR4) ABE, Mohammed MAKHLOUF3) AEF 1) University of Mascara, Department of Agronomy, BP305, Mascara 29000, Algeria; e-mail: [email protected] 2) University of Blida, Department of Water Science, Blida 9000, Algeria; e-mail: [email protected] 3) University of Saida, Department of Biology, Saida 2000, Algeria; e-mail: [email protected] 4) University of Sidi-bell-abbes, Department of Mechanics, Sidi-bel-Abbes 22000, Algeria; e-mail: md [email protected] For citation: Gliz M., Remini B., Anteur D., Makhlouf M. 2015. Vulnerability of soils in the watershed of Wadi El Ham- mam to water erosion (Algeria). Journal of Water and Land Development. No. 24 p. 3–10 Abstract Located in the north west of Algeria, the watershed of Wadi El Hammam is threatened by water erosion that has resulted the silting of reservoirs at cascade: Ouizert, Bouhanifia and Fergoug. The objective of this study is to develop a methodology using remote sensing and geographical information systems (GIS) to map the zones presenting sensibility of water erosion in this watershed. -
Giza Plateau Mapping Project. Mark Lehner
GIZA PLATEAU MAPPING PROJECT GIZA PLATEAU MAPPING PROJECT Mark Lehner Ancient Egypt Research Associates (AERA) Season 2017: The Old and the New This year AERA team members busied themselves with the old and very new in research. I had the opportunity to return to some of my earliest work at the Sphinx, thanks to a grant from the American Research Center in Egypt (ARCE) Antiquities Endowment Fund (AEF) for the Sphinx Digital Database. This project will digitize, conserve, and make available as open source the archive from the 1979–1983 ARCE Sphinx Project, for which Dr. James Allen was project director and I was field director. My work at the Sphinx started three years earlier, in 1977, with Dr. Zahi Hawass, so that makes it exactly forty years ago.1 Search for Khufu We launched a new initiative, directed by Mohsen Kamel and Ali Witsell, to explore the older layers of the Heit el-Ghurab (“Wall of the Crow,” HeG) site. In some areas we have seen an older, different layout below what we have so far mapped, which dates to Khafre and Men- kaure. We believe that the older phase settlement and infrastructure, which was razed and rebuilt, served Khufu’s building of the Great Pyramid. The discovery in 2013, and publication this year, of the Journal of Merer2 piques our interest all the more in the early phase of Heit el-Ghurab. Pierre Tallet and a team from the Sorbonne and the French Institute in Cairo discovered the inscribed papyri at Wadi el-Jarf on the west- ern Red Sea Coast, in a port facility used only in the time of Khufu. -
FLOOD ANALYSIS and MITIGATION for PETRA AREA in JORDAN By
FLOOD ANALYSIS AND MITIGATION FOR PETRA AREA IN JORDAN By Radwan A. Al-Weshah1 and Fouad El-Khoury2 ABSTRACT: Petra is located in the southwest region of Jordan about 200 km south of Amman, between the Dead Sea and the Gulf of Aqaba. Petra was carved in sandstone canyons by the Nabatean over 2,000 years ago. Today the city is a major tourist attraction, its monuments being considered the jewels of Jordan. Floods pose a serious threat to the tourist activities in Petra as well as to the monuments themselves. In this paper, a ¯ood analysis model developed and calibrated for the Petra catchment is described. Using the model, ¯ood ¯ows and volumes are estimated for storm events of various return periods. To alleviate the impact of ¯oods on tourism in Petra, several ¯ood mitigation measures are proposed. The impact of these measures on ¯ood peak¯ow and volume is evaluated. These include afforestation, terracing, construction of check and storage dams, and various combinations of these measures. The ¯ood simulation model predicts that the measures can reduce ¯ood peak- ¯ows and volumes by up to 70%. INTRODUCTION was an extreme event, probably with a 100-year return period. During this extreme event, the intense and sudden rainfall The Petra region is located in the southwest of Jordan, be- caused ¯ood water to ¯ow from all wadis into the main wadi tween the Dead Sea and the Gulf of Aqaba. It lies in the upstream of the Siq. The ¯ood carried a huge sediment load Sherah Mountains overseeing Wadi Araba in the Jordan Rift of loose silt and sand which blocked most of the hydraulic Valley, at latitude of 30Њ 20Ј North and longitude of 35Њ 27Ј structures in the wadi. -
Akhet Khufu : Archaeo-Astronomical Hints at a Common Project of the Two Main Pyramids of Giza, Egypt
Akhet Khufu : archaeo-astronomical hints at a common project of the two main pyramids of Giza, Egypt. Giulio Magli Dipartimento di Matematica del Politecnico di Milano P.le Leonardo da Vinci 32, 20133 Milano, Italy. e-mail [email protected] The architectural complexes composed by the two main pyramids of Giza together with their temples are investigated from an inter-disciplinary point of view, taking into account their astronomical alignments as well as their relationships with the visible landscape. Combining already known facts together with new clues, the work strongly supports the idea that the two complexes were conceived as parts of a common project. 1. Introduction The Giza Plateau overlooks today’s city of Cairo, Egypt. Here, in a short period of time (certainly comprised between 2600 and 2450 b.C.) during the so called Old Kingdom , the expert workmen and architects of the pharaohs of the IV Egyptian Dynasty constructed for their rulers two pyramids which are, still today, among the most remarkable achievements of the whole human history. We shall call these pyramids Giza 1 and Giza 2; with side lengths of 230.3 and 215 meters, and heights of 146.6 and 143.5 meters respectively, Giza 1 and Giza 2 are by far greater than the third famous pyramid present on the Plateau, the tomb of the pharaoh Menkaure. This pyramid indeed hardly reaches 65 meters in height and is, therefore, much smaller also of the three pyramids constructed about 100 years before by the pharaoh Snefru in the sites of Meidum and Dahshur, south of Giza, all of which reach an height of more than 90 meters. -
Gram Vol. 11 No.2
VOL. 11 NO.2 GRAM Winter 2011 ANCIENT EGYPT RESEARCH ASSOCIATES ISSN 1944-0014 Groundbreaking Archaeology Front … Double-Decker Dorms The galleries of the Lost City of the Pyramids Digging Again may have been covered with great barrel vaults. 2 Here, in this reconstruction, the front wall is Seeds and Skeletons: Training Egypt’s stripped away to show the galleries with lofts nestled under the vaults. The workers relax on Archaeological Scientists two levels. Read inside about how Günter Heindl 4 developed the vault hypothesis. See the back On the Cusp of a New Dynasty 10 cover for a view of the rear of the gallery. 7 http://www.aeraweb.org Season 2011: The Lost City of the Pyramids: The Mystery of Standing Wall Island Digging Again In 2004, at the southern edge of the site, we discovered the “standing wall,” so-called because we found this fieldstone wall rising unusually about five feet above the ruin Last year we took a break from excavation surface. Standing Wall forms the northern end of ES1 and ES2, two large enclosures to devote our time to studies and analysis of stone walls flanked on two sides by deep sand-filled depressions that sink more in our Giza Field Laboratory and to the than three feet below the floor level of the Western Town district immediately to Analysis and Publication Field School the north. The depressions leave the enclosures standing like an island. (see AERAGRAM 11-11). This season we are During the 2004 season we did not find the southern end of the western wall of back in the field again.