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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-1945</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Изменение морского края дельты Нила по историческим данным (VІ в. до н.э.- ХХ в. н.э.)</article-title><trans-title-group xml:lang="en"><trans-title>Changes of the offshore margin of the Nile delta according to historical evidences (VI-XX centuries AC)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Науар</surname><given-names>А. Х.</given-names></name><name name-style="western" xml:lang="en"><surname>Nawar</surname><given-names>A. H.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Леонтьев</surname><given-names>О. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Leontyev</surname><given-names>O. K.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1978</year></pub-date><pub-date pub-type="epub"><day>15</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>81</fpage><lpage>88</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Науар А.Х., Леонтьев О.К., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Науар А.Х., Леонтьев О.К.</copyright-holder><copyright-holder xml:lang="en">Nawar A.H., Leontyev O.K.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/1945">https://geomorphology.igras.ru/jour/article/view/1945</self-uri><abstract><p>Comparative studies of geographical (mainly cartographical) data on the Nile delta from antique manuscripts, mediaeval Arabian geographical works and descriptions dated from the XVII -beginning of the XIX centuries A. C. reveal main trends of the offshore delta evolution throughout the historical time. Results of the studies suggest, first, gradual elimination of the delta channels (from 7 at Herodotus time to 2 at present); second, drying western flank of the delta and increasing humidity of the eastern flank. The channels atrophy is likely due to increasing usage of the Nile water for irrigation purposes; western flank drying and eastern flank wetting may result from differentiated tectonics and changes of the flow pattern within the delta.</p></abstract><trans-abstract xml:lang="en"><p>Comparative studies of geographical (mainly cartographical) data on the Nile delta from antique manuscripts, mediaeval Arabian geographical works and descriptions dated from the XVII -beginning of the XIX centuries A. C. reveal main trends of the offshore delta evolution throughout the historical time. Results of the studies suggest, first, gradual elimination of the delta channels (from 7 at Herodotus time to 2 at present); second, drying western flank of the delta and increasing humidity of the eastern flank. The channels atrophy is likely due to increasing usage of the Nile water for irrigation purposes; western flank drying and eastern flank wetting may result from differentiated tectonics and changes of the flow pattern within the delta.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
