They believed their country was divided into two distinct geographical sections, the black land the fertile banks of the river Nile and the red land the barren desert that covered the rest of the country. Location The location of ancient Egypt was in North-Eastern Africa, having formed and flourished along the lower portion of the Nile River. It made up most of what is now the modern Arab Republic of Egypt. Ancient Egypt had four main divisions of its land, the first two being the Upper and Lower Egypt.
Steep rocky cliffs rise along the banks of the Nile in some stretches, while other areas along the Nile are flat, with space for agricultural production.
In the past, flooding of the Nile during the summer provided silt and water to make agriculture possible on land that is otherwise very dry. Since construction of the Aswan Damagriculture in the Nile valley depends on irrigation.
The Nile delta consists of flat, low-lying areas. Some parts of the delta are marshy and water-logged, and thus not suitable for agriculture. Other areas of the delta are used for agriculture.
Without the topographic channel that permits the Nile to flow across the SaharaEgypt would be entirely desert. In South Sudan, the White Nile passes through the Sudda wide, flat plain covered with swamp vegetation and slows almost to the point of stagnation.
|Climate In Ancient Egypt||Exploration of Asia During the Early Middle Agesgeographical knowledge in Europe regressed though it is a popular misconception that they thought the world was flatand the simple T and O map became the standard depiction of the world. The trips of Venetian explorer Marco Polo throughout Mongol Empire in the 13th century, the Christian Crusades of the 12th and 13th centuries, and the Portuguese and Spanish voyages of exploration during the 15th and 16th centuries opened up new horizons and stimulated geographic writings.|
|Ancient Egypt - HISTORY||Exploration of Asia During the Early Middle Agesgeographical knowledge in Europe regressed though it is a popular misconception that they thought the world was flatand the simple T and O map became the standard depiction of the world.|
This river has a steeper gradient and therefore flows more swiftly than the White Nile, which it joins at Khartoum. Unlike the White Nile, the Blue Nile carries a considerable amount of sediment. For several kilometres north of Khartoum, water closer to the eastern bank of the river, coming from the Blue Nile, is visibly muddywhile that closer to the western bank, and coming from the White Nile, is clearer.
During the low-water season, which runs from January to June, the Atbarah shrinks to a number of pools. The Blue Nile has a similar pattern. Thus, before the Aswan High Dam was completed inthe White Nile watered the Egyptian stretch of the river throughout the year, whereas the Blue Nile, carrying seasonal rain from Ethiopia, caused the Nile to overflow its banks and deposit a layer of fertile mud over adjacent fields.
The great flood of the main Nile usually occurred in Egypt during August, September, and October, but it sometimes began as early as June at Aswan and often did not completely wane until January. The Nile enters Egypt a few kilometers north of Wadi Halfaa Sudanese town that was completely rebuilt on high ground when its original site was submerged in the reservoir created by the Aswan High Dam.
Below Aswan the cultivated floodplain strip widens to as much as twenty km. According to historical accounts from the first century AD, seven branches of the Nile once ran through the delta.
According to later accounts, the Nile had, by around the twelfth century, just six branches. Since then, nature and man have closed all but two main outlets: Both outlets are named after the ports located at their respective mouths. A network of drainage and irrigation canals supplements these remaining outlets.
In the north, near the coast, the Nile delta embraces a series of salt marshes and lakesthe most notable among which are IdkuAl Burullusand Manzilah. The fertility and productivity of the land adjacent to the Nile depends largely on the silt deposited by floodwaters.
Archaeological research indicates that people once lived at a much higher elevation along the river than they do today, probably because the river was higher or the floods more severe.Egypt’s geography, population, history and military strength have made it highly influential in the region.
Egypt is a democratic republic, although some critics claim that it is not truly democratic. Egypt's geography, population, history, and military strength have made it highly influential in the region.
Egypt is a democratic republic, although some critics claim that it is not truly democratic. Coordinates The geography of Egypt relates to two regions: North Africa and Southwest Egypt has coastlines on the Mediterranean Sea, the River Nile and the Red Sea.
Egypt borders Libya to the west, the Gaza Strip and Israel to the northeast, and Sudan to the south. The geography of Ancient Egypt was an interesting concept from the perspective of the ancient Egyptians themselves.
They believed their country was divided into two distinct geographical sections, the black land (the fertile banks of the river Nile) and the red land (the barren desert that covered the rest of .
The geography of ancient Egypt was dominated, as is today, by the combination of lack of rainfall and the Nile River.
The Greek historian Herodotus called Egypt the "gift of the Nile", since the kingdom owed its survival to the annual flooding of the Nile and the resulting depositing of fertile silt.
Geography. The ancient Egyptians thought of Egypt as being divided into two types of land, the 'black land' and the 'red land'. The 'black land' was the fertile land on the banks of the Nile.