Most geologic and geomorphologic features emerged on a deltaic plain resulted from the interplay of marine, land and river, of which are some have the potential to be a geoheritage site, this is called a geomorphosite. Over time, human impact due to settlements on the geomorphosite, reshaped and transformed the site to geoarcheomorphosite. The Great Pelusium, or Tell El-Farama, which is located along the Tineh Plain at the NE extreme of the Nile Delta between the third and fifth c. AD, is classified as a geoarcheomorphosite. The location includes several geomorphosites, such as the accreted coastal ridges, which record Late Holocene sea level changes. It also includes traces of the flash flood on the Pelusiac branch during the eighth c. AD, with the fluvial flood plain, natural levee, and crevasse splays, on which the Great Pelusium, Tell El-Luli, Tell El-Fadah, and Tell El-Makhzan were constructed. Recently, the area subjected to a hub development project, which may represent anthropogenic hazards that threaten the Great Pelusium. This study aims to quantify the potential anthropogenic hazards. The change detection shows that in 1984 the area of the geoarcheomorphosites was 424.8 km², representing approximately 67.1% of the Tineh Plain, in addition to the sand dune area of 75 km², representing 11.8%. In 2018, the area saw agricultural activities, fish farms, and an urban expansion that covered approximately 244.2 km², representing 38% of the Tineh Plain. The construction of a new hub in the Suez Canal corridor and the addition of a new community of one million people in an area of 164 km², representing 30.3% of the plain, will add more pressure on the geodiversity. A conservation plan is recommended in the form of sustainable development to save an important area of geoheritage in Egypt and convert the area into a tourism destination.

中文翻译：

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埃及尼罗河三角洲东北部Tineh平原强烈城市化压力下的地貌变质岩

由于海洋，陆地和河流的相互作用而在三角洲平原上出现的大多数地质和地貌特征，其中一些有可能成为地质遗迹，这被称为地貌遗址。随着时间的流逝，由于定居在地貌上的人类影响，将其重塑并转变为地貌。大Pe（Tell El-Farama），位于蒂尼平原上，位于尼罗河三角洲东北角，位于第三和第五个c之间。AD被归类为地质古构造遗址。该位置包括几个地貌岩，例如记录了全新世晚期海平面变化的沿海隆起山脊。它也包括在八世纪期间Pelusiac分支上的山洪泛滥的痕迹。公元，河流泛滥的平原，天然堤坝和裂缝开裂，大Pe对泰勒·卢利说，Tell El-Fadah和Tell El-Makhzan建成。最近，该地区正在进行枢纽开发项目，这可能是威胁大that的人为危险。这项研究旨在量化潜在的人为危害。变化检测表明，1984年地貌变质岩面积为424.8 km。²，约占Tineh平原的67.1％，此外，沙丘面积为75 km ²，占11.8％。在2018年，该地区进行了农业活动，养鱼场和城市扩张，占地约244.2 km ²，占Tineh平原的38％。在苏伊士运河走廊上建设新的枢纽，并在164 km ²的面积（占平原的30.3％）中增加一百万人口的新社区，这将给地球多样性带来更多压力。建议以可持续发展的形式制定保护计划，以保存埃及重要的地质遗迹地区并将其转变为旅游目的地。