Results 11 to 20 of about 51 (46)
Three thousand years of river channel engineering in the Nile Valley
Abstract Across a 1000‐km stretch of the River Nile, from the 1st Cataract in southern Egypt to the 4th Cataract in Sudan, many hundreds of drystone walls are located within active channels, on seasonally inundated floodplains or in now‐dry Holocene palaeochannel belts.
Matthew Dalton +4 more
wiley +1 more source
Effects of ancient Egypt hypostyle halls on the thermal environment
The Hypostye Hall in ancient Egyptian temples is a system that uses heat capacity to stabilize the thermal environment, similar to the modern Thermo Active Building System (TABS). Using the Great Temple of Amun at Karnak as an example, the value of Hypostyle Hall will be evaluated using physical simulations in this study.
Eisuke Togashi +2 more
wiley +1 more source
Riley in Cairo: British Art and Egypt in the 1980s
In the early 1980s, Bridget Riley produced a series of paintings distinguished by their use of the same group of colours, said to have been inspired by the vividly preserved painted tombs that she encountered during a visit to Egypt in the winter of 1979–80.
Richard Johns
wiley +1 more source
International Journal of Photoenergy, Volume 7, Issue 2, Page 59-60, 2005.
Klaas A. Zachariasse
wiley +1 more source
VAN SICLEN (C.C.), « Amenhotep II and the Mut Temple Complex at Karnak », VA 3/3, 1987, p. 281-282.
openaire +2 more sources
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Journal of Archaeological Science, 2011
This paper presents the results of a geoarchaeological study undertaken in Upper Egypt, in the western part of the Karnak Temples complex. The geoarchaeological approach helps to better understand the fluvial dynamics of the Nile in the proximity of the Pharaonic site during the late Holocene.
Matthieu Ghilardi
exaly +3 more sources
This paper presents the results of a geoarchaeological study undertaken in Upper Egypt, in the western part of the Karnak Temples complex. The geoarchaeological approach helps to better understand the fluvial dynamics of the Nile in the proximity of the Pharaonic site during the late Holocene.
Matthieu Ghilardi
exaly +3 more sources

