Eine Neubetrachtung vonmw-qd „das umgewandte/umgekehrte/abbiegende Wasser“

2020 ◽  
Vol 147 (1) ◽  
pp. 19-29
Author(s):  
Marc Brose
Keyword(s):  
Red Sea ◽  

SummaryThis article takes a fresh at the geographical term mw-qd, usually transcribed as “inverted/reverse/encircling water” (or the like) and often identified with the river Euphrates in Mesopotamia or the Red Sea or a part of it. After an overview of the attestations of the term, the former ideas of the researchers and the discussion of grammatical and lexical details, a new effort tries to show that there would have been at least two or three locations bearing this name: the region on the Upper Nile in Nubia between the Fourth Cataract and Kurgus, where the Nile takes a characteristic bend in its course, further a region on the northern coastal area of the Red Sea, perhaps the region of Qoseir, and at last a river in Asia, perhaps the Euphrates.

2015 ◽  
Vol 3 (3) ◽  
pp. 165-176
Author(s):  
Essam Abdelsalam Gouda

This paper analysis the tourism development on the Red Sea in Egypt (west bank) and the needed ongoing action toward a sustainable approach. It addresses, at the first, the development's evolution occurred in the coastal area, the environmental effects it left, and how to minimize those impacts in the future. The second main point is dealing with the most important issues that hinder the achievement of sustainable tourism development on the Red Sea coast and how we can overcome them in the future.


Author(s):  
A. G. Al-Zubieri ◽  
R. A. Bantan ◽  
R. Abdalla ◽  
S. Antoni ◽  
T. A. Al-Dubai ◽  
...  

<p><strong>Abstract.</strong> Jazan city is a fast-growing coastal city in the southern part of Saudi Arabia, Red Sea. Recently, it has encountered quick industrial development activities. To monitor these activities, the changes in coastal zone morphology explore over the last 30 years (1987&amp;ndash;2017) using GIS and remote sensing techniques. Four satellite images (TM and ETM) acquired during these intervals were performed. Furthermore, a development and growth of the city were created based on direct digitizing from Google Earth Pro to identify the extension and expansion of the area of study during this period. The magnitudes of erosion, deposition, and landfilling at differential scales through the period of study were determined using photo-interpretation on the changes of surface area and the extension of the city landward. The results illustrated remarkable changes and shifting of shoreline seaward along the coast and extending of dwelling zone in the city. Erosion and accretion take place mostly in the earlier interval (1987&amp;ndash;2000) in some parts of the coast followed by landfilling occurring in the northern and middle parts of the coastal area in the interval (2000&amp;ndash;2013). However, the magnitudes were different from interval to interval. The relative changes were 14.33, 58.56, and 27.11&amp;thinsp;% at the periods from 1987&amp;ndash;2000, 2000&amp;ndash;2013, and 2013&amp;ndash;2017, respectively. However, dwelling zone extended dramatically from 23.31&amp;thinsp;km<sup>2</sup> in 1987, to 25.32&amp;thinsp;km<sup>2</sup> in 2000, 63.37&amp;thinsp;km<sup>2</sup> in 2013, and to reach 67.90&amp;thinsp;km<sup>2</sup> in 2017. These changes probably attributed to human activities in the coastal area due to construct a new economic city in the northern part during the period between 2003 and 2013 along with different socio-economic activities. The tidal flat in front of the city is shrunk due to this landfilling. This landfilling has been destructed a wide range of mangrove ecozones and possibly impacted the biotics in the area.</p>


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