A metaphor for the black land of the Nile Valley to distinguish it from the red desert land surrounding it. “Magyar,” which meant “draining,” meaning (country), “hidden” or “confined,” and it was derived from the word “puppy” meaning the boundary, or from the word “running” meaning the fence. Then a spatial meme was added to it, and it became “Hungary” and it was written After that, in many forms such as "Hungarian" and "Emger". The ancient Egyptians used it and described one of the hairsPharaoh Senusret III perceived them as "more serious"; Any ward off and that it is more like border walls.
The names with which it is known in many European languages are derived from its Latin name Aegyptus, which in turn is derived from the Greek word Aegyptus, which is due to the inspiration of Homer's imagination in his legend that he composed at a time between 1600 and 1200 BC. The Ptolemies called the term "Aegyptus" on Egypt and its inhabitants inspired the myth of Homer referred to. The Greeks called the Nile and the land of the Nile at the same time Aegyptus, then restricted it to Egypt itself, and the Romans wrote after them Aegyptus
Perhaps the closest possible Egyptian nomenclature to the name Aigoptus and its derivatives is the name of Agbi and its synonyms: Ajeb and Ojib, and Ijb and Akb, and they were all synonyms in which the Egyptian spikes symbolized the eternal water from which the earth emerged, the Nile, the flood, the Lord of the flood, and perhaps the land submerged in the flood as well. The Greeks did not pass the name Aigoptus in later ages from the Nile and the land of the Nile together, after they had modified its writing to what they had pronounced, and after adding at the end the two letters waw and sin, which they used to add to the end of most
The land of Egypt consists of an ancient Arakan core, which is part of the Arab-Nubian bloc, which is part of the African Shield; Which was the heart of the continent of Gondwana in the Archaean era. The African Shield, in all its parts, was exposed to the effects of many factors throughout the ages, so the land of Egypt began to grow towards the north at the expense of the Tethys Sea. And Egypt reached at the end of the third geological time its current area
The features of its surface and coasts were formed as they are now in the fourth time. The Egyptian soil in the Nile Valley and its deltas was formed from the accumulation of Nile silt, which was originally derived from the crumbs of the rocks of the Abyssinia Plateau, which began to be returned to Egypt about 10 thousand years ago. Shallow texture, light sandy clay soil and sandy gravel soil
The current political boundaries of Egypt are very recent, as the oldest boundary agreement dates back to 1899. Before that, it was a frontier, and by virtue of the nature of Egypt's geographic location linking the continents of Asia and Africa; Egypt's borders were expanding and shrinking according to the degree of power of the Egyptian state. The Egyptian land borders are astronomical and geometric, and Egypt is bordering with 4 countries: Palestine (Gaza Strip) and Israel to the northeast, Libya to the west, and Sudan to the south. Today, the Arab Republic of Egypt is bordered on the north by the Mediterranean Sea, with a coastline of 995 km long
The climate of Egypt is affected by several factors, the most important of which are the location, surface features, the general system of pressure, depressions and water bodies. All this helped divide Egypt into several distinct climatic regions. Egypt is located in the arid tropical region with the exception of the northern parties that enter the temperate green zone that has a climate similar to that of a region The Mediterranean climate, which is characterized by hot and dry summer months, and mild in winter, with little rain falling on the coast.
According to the country's astronomical site, its northern extremities are located at the outskirts of the central parades, and the rest of its parts are located within hot and dry tropical shows, where the high sub-tropical pressure and the accompanying falling air control the chances of rain. Also, on the surface, these performances are dominated by dry trade winds, which are characterized by their ability to carry water vapor; Because it heats up as it advances south to the equator.
During the winter season, northern Egypt was overcome by the southeast, northwest, and western winds; Especially the northwest coast and the delta. In Middle and Upper Egypt northern winds prevail. In spring, the westerly winds begin to recede, while the northern winds generally advance. The summer season has a different pattern of surface winds, as the northern winds and their branches dominate in all directions and capture the largest share of wind directions. They are known as trade winds, which are dry winds and are known among the commoners as marine air. The autumn season is considered a transitional period between summer and winter conditions in Egypt, as the northern winds begin to recede and some imbalance in wind distribution may occur.
As for the humidity, it rises in the winter season, especially in the northern part of the country; The average relative humidity reaches 80% in the north of the country, 40% in the far south of the country, and between 60% and 70% on the coasts of the Red Sea and the Sinai Peninsula. In the summer, it decreases in July, and the relative humidity in coastal areas reaches between 60% and 70% in July and August, while it drops to 20% in the far south of the country. In the transitional seasons, which are spring and autumn, the relative humidity is a medium between winter and summer.
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