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Coordinates: 27°00′N 30°00′E / 27.000°N 30.000°E / 27.000; 30.000 The geography of Egypt
Egypt
relates to two regions: North Africa and Southwest Asia. Egypt
Egypt
has coastlines on the Mediterranean Sea, the River Nile
Nile
and the Red Sea. Egypt
Egypt
borders Libya
Libya
to the west, the Gaza Strip
Gaza Strip
and Israel
Israel
to the northeast, and Sudan
Sudan
to the south. Egypt
Egypt
has an area of 1,001,449 km2 (386,662 mi2). The longest straight-line distance in Egypt
Egypt
from north to south is 1,024 km (636 mi), while that from east to west measures 1,240 km (771 mi). More than 2,900 km (1800 mi) of coastline on the Mediterranean Sea, the Gulf of Suez, the Gulf of Aqaba, and the gulf shore

Contents

1 Governorates 2 Natural regions

2.1 Nile
Nile
Valley and Delta 2.2 Western Desert 2.3 Eastern Desert 2.4 Sinai
Sinai
Peninsula

3 Urban and rural areas 4 Extreme points 5 Notes 6 References 7 External links

Governorates[edit] Main article: Governorates of Egypt Egypt
Egypt
is divided into 27 governorates, which include two city-governorates: Alexandria
Alexandria
( Alexandria
Alexandria
Governorate) and Cairo ( Cairo
Cairo
Governorate). There are nine governorates of Lower Egypt
Egypt
in the Nile Delta
Nile Delta
region, ten of Upper Egypt
Egypt
along the Nile
Nile
river south from Cairo
Cairo
to Aswan
Aswan
and five frontier governorates covering Sinai
Sinai
and the deserts that lie west and east of the Nile
Nile
rive Natural regions[edit]

Egypt's topography.

Egypt
Egypt
is predominantly desert. 35,000 km2 - 3.5% - of the total land area is cultivated and permanently settled. Most of the country lies within the wide band of desert that stretches eastwards from Africa's Atlantic Coast across the continent and into southwest Asia. Egypt's geological history has produced four major physical regions:

Nile
Nile
Valley and Nile
Nile
Delta Western Desert
Desert
(from the Nile
Nile
west to the Libyan border) Eastern Desert
Desert
(extends from the Nile
Nile
Valley all the way to the Red Sea coast) Sinai
Sinai
Peninsula

Despite covering only about 6.5% of the total area of Egypt; the Nile Valley and Nile Delta
Nile Delta
are the most important regions, being the country's only cultivable regions and supporting about 99% of the population. The Nile
Nile
valley extends approximately 800 km from Aswan
Aswan
to the outskirts of Cairo. The Nile
Nile
Valley is very cool and known as Upper Egypt, while the Nile Delta
Nile Delta
region is known as Lower Egypt. Steep rocky cliffs rise along the banks of the Nile
Nile
in some stretches, while other areas along the Nile
Nile
are flat, with space for agricultural production. In the past, flooding of the Nile
Nile
during the summer provided silt and water to make agriculture possible on land that is otherwise very dry. Since construction of the Aswan
Aswan
Dam, agriculture in the Nile
Nile
valley depends on irrigation. The Nile
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.[1] Nile
Nile
Valley and Delta[edit]

Nile
Nile
delta, and the entire course of the Nile

Main articles: Nile
Nile
and Nile
Nile
Delta The Nile
Nile
Valley and Delta, the most extensive oasis on earth, was created by the world's longest river and its seemingly inexhaustible sources. Without the topographic channel that permits the Nile
Nile
to flow across the Sahara, Egypt
Egypt
would be entirely desert. The length within Egypt
Egypt
of the River Nile
Nile
in its northwards course from three central African sources – the White Nile, the Blue Nile, and the Atbara
Atbara
– totals some 1,600 km. The White Nile, which begins at Lake Victoria
Lake Victoria
in Uganda, supplies about 28% of the Nile's Egyptian waters. In its course from Lake Victoria to Juba
Juba
in South
South
Sudan, the White Nile's channel drops more than 600 m. In its 1,600-km course from Juba
Juba
to Khartoum, Sudan's capital, the river descends just 75 m. In South
South
Sudan, the White Nile passes through the Sudd, a wide, flat plain covered with swamp vegetation and slows almost to the point of stagnation. The Blue Nile, which originates at Lake Tana
Lake Tana
in Ethiopia, provides on average some 58% of the Nile's Egyptian waters. 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 muddy, while that closer to the western bank, and coming from the White Nile, is clearer. The much shorter Atbarah River, which also originates in Ethiopia, joins the main Nile
Nile
north of Khartoum
Khartoum
between the fifth and sixth cataracts (areas of steep rapids) and provides about 14% of the Nile's waters in Egypt. During the low-water season, which runs from January to June, the Atbarah shrinks to a number of pools. But, in late-summer, when torrential rains fall on the Ethiopian Highlands, the Atbarah provides 22% of the Nile's flow. The Blue Nile
Nile
has a similar pattern. It contributes 17% of the Nile's waters in the low-water season and 68% during the high-water season. In contrast, the White Nile
Nile
provides only 10% of the Nile's waters during the high-water season but contributes more than 80% during the low-water period. Thus, before the Aswan
Aswan
High Dam was completed in 1971, the White Nile
Nile
watered the Egyptian stretch of the river throughout the year, whereas the Blue Nile, carrying seasonal rain from Ethiopia, caused the Nile
Nile
to overflow its banks and deposit a layer of fertile mud over adjacent fields. The great flood of the main Nile
Nile
usually occurred in Egypt
Egypt
during August, September, and October, but it sometimes began as early as June at Aswan
Aswan
and often did not completely wane until January. The Nile
Nile
enters Egypt
Egypt
a few kilometers north of Wadi Halfa, a Sudanese town that was completely rebuilt on high ground when its original site was submerged in the reservoir created by the Aswan
Aswan
High Dam. As a result of the dam's construction, the Nile
Nile
actually begins its flow into Egypt
Egypt
as Lake
Lake
Nasser, which extends southwards from the dam for 320 km to the border and for an additional 158 km within Sudan. Lake
Lake
Nasser's waters fill the area through Lower Nubia (Upper Egypt
Egypt
and northern Sudan) within the narrow canyon between the cliffs of sandstone and granite created by the flow of the river over many centuries. Below Aswan
Aswan
the cultivated floodplain strip widens to as much as twenty km. North of Isna (160 km north of Aswan), the plateau on both sides of the valley rises to as much as 550 m above sea level; at Qina (some 90 km north of Isna) the 300-m limestone cliffs force the Nile
Nile
to change course towards the southwest for about 60 km before it turns northwest for about 160 km to Asyut. Northward from Asyut, the escarpments on both sides diminish, and the valley widens to a maximum of 22 km. At Cairo, the Nile
Nile
spreads out over what was once a broad estuary, subsequently filled by silt deposits to form what is now a fertile, fan-shaped delta some 250 km wide at its seaward extremity and extending about 160 km from north to south. The Nile Delta
Nile Delta
covers approximately 22,000 km2 (roughly equivalent in area to that of Massachusetts). According to historical accounts from the first century AD, seven branches of the Nile
Nile
once ran through the delta. According to later accounts, the Nile
Nile
had, by around the twelfth century, just six branches. Since then, nature and man have closed all but two main outlets: the east branch, Damietta
Damietta
(also seen as Dumyat; 240 km long), and the west branch, Rosetta
Rosetta
(235 km long). 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
Nile
delta embraces a series of salt marshes and lakes, the most notable among which are Idku, Al Burullus, and 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. The timing and the amount of annual flow were always unpredictable. Measurements of annual flows as low as 1.2 billion m3 and as high as 4.25 billion m3 have been recorded. For centuries Egyptians
Egyptians
attempted to predict and take advantage of these flows and thereby moderate the severity of floods. The construction of dams on the Nile, particularly the Aswan
Aswan
High Dam, transformed the mighty river into a large and predictable irrigation ditch. Lake
Lake
Nasser, the world's largest artificial lake, has enabled planned use of the Nile
Nile
regardless of the amount of rainfall in Central Africa
Central Africa
and East Africa. The dams have also affected the Nile Valley's fertility, which was dependent for centuries not only on the water brought to the arable land but also on the materials left by the water. Researchers have estimated that beneficial silt deposits in the valley began about 10,000 years ago. The average annual deposit of arable soil through the course of the river valley amounted to some nine metres. Analysis of the flow revealed that 10.7 million tons of solid matter passed Cairo
Cairo
each year. Today the Aswan
Aswan
High Dam obstructs most of this sediment, now retained in Lake
Lake
Nasser. The reduction in annual silt deposits has contributed to rising water tables and increasing soil salinity in the Delta, the erosion of the river's banks in Upper Egypt, and the erosion of the alluvial fan along the shore of the Mediterranean Sea. Western Desert[edit] Main article: Western Desert
Desert
(Egypt) The Western Desert
Desert
covers an area of some 700,000 km2, thereby accounting for around two-thirds of Egypt's total land area. This immense desert to the west of the Nile
Nile
spans the area from the Mediterranean Sea
Mediterranean Sea
southwards to the Sudanese border. The desert's Jilf al Kabir Plateau, at a mean altitude of some 1000 m, constitutes an exception to the uninterrupted territory of basement rocks covered by layers of horizontally bedded sediments forming a massive plain or low plateau. The Great Sand Sea
Great Sand Sea
lies within the desert's plain and extends from the Siwa Oasis
Siwa Oasis
to Jilf al Kabir. Escarpments (ridges) and deep depressions (basins) exist in several parts of the Western Desert, and no rivers or streams drain into or out of the area. The government has considered the Western Desert
Desert
a frontier region and has divided it into two governorates at about the twenty-eighth parallel: Matruh to the north and New Valley (Al Wadi al Jadid) to the south. There are seven important depressions in the Western Desert, and all are considered oases except the largest, Qattara, the water of which is salty. The Qattara
Qattara
Depression, which includes the country's lowest point, encompasses 19,605 square kilometers (7,570 sq mi), which is similar to the size of Lake
Lake
Ontario. It is largely below sea level and is 133 meters (436 ft) below sea level at the lowest. Badlands, salt marshes, and salt lakes cover the sparsely inhabited Qattara
Qattara
Depression. Limited agricultural production, the presence of some natural resources, and permanent settlements are found in the other six depressions, all of which have fresh water provided by the Nile
Nile
or by local groundwater. The Siwah Oasis, close to the Libyan border and west of Qattara, is isolated from the rest of Egypt
Egypt
but has sustained life since ancient times. The Siwa's cliff-hung Temple of Amun was renowned for its oracles for more than 1,000 years. Herodotus
Herodotus
and Alexander the Great
Alexander the Great
were among the many illustrious people who visited the temple in the pre-Christian era. The other major oases form a topographic chain of basins extending from the Faiyum Oasis
Oasis
(sometimes called the Fayyum Depression) which lies 60 kilometers (37 mi) southwest of Cairo, south to the Bahariya, Farafirah, and Dakhilah oases before reaching the country's largest oasis, Kharijah. A brackish lake, Birket Qarun, at the northern reaches of Al Fayyum Oasis, drained into the Nile
Nile
in ancient times. For centuries sweet water artesian wells in the Fayyum Oasis have permitted extensive cultivation in an irrigated area that extends over 1,800 square kilometers (695 sq mi). Eastern Desert[edit]

A large plume of Saharan Desert
Desert
dust (light brownish pixels) blown across Libya
Libya
and Egypt
Egypt
northward over the Mediterranean Sea
Mediterranean Sea
toward the Middle East, on February 2, 2003.

Main article: Eastern Desert The topographic features of the desert region east of the Nile
Nile
differ from those to the west of the Nile. The Eastern Desert
Desert
is relatively mountainous. The elevation rises abruptly from the Nile, and a downward-sloping plateau of sand gives way within 100 km to arid, defoliated, rocky hills running north and south between the Sudan border and the Delta. The hills reach elevations of more than 1,900 m. The region's most prominent feature is the easterly chain of rugged mountains, the Red Sea
Red Sea
Hills, which extend from the Nile
Nile
Valley eastward to the Gulf of Suez
Suez
and the Red Sea. This elevated region has a natural drainage pattern that rarely functions because of insufficient rainfall. It also has a complex of irregular, sharply cut wadis that extend westward toward the Nile. The desert environment extends all the way to the Red Sea
Red Sea
coast. Sinai
Sinai
Peninsula[edit]

Mount Catherine
Mount Catherine
in Sinai, Egypt's highest point.

The Sinai Peninsula
Sinai Peninsula
is a triangular-shaped peninsula, about 61,100 km2 in area (slightly smaller than the U.S. state
U.S. state
of West Virginia). Similar to the desert, the peninsula contains mountains in its southern sector that are a geological extension of the Red Sea Hills, the low range along the Red Sea
Red Sea
coast that includes Mount Catherine (Jabal Katrinah), the country's highest point, at 2,642 m above sea-level. The Red Sea
Red Sea
may have been named after these mountains, which are red. The southern side of the peninsula has a sharp escarpment that subsides after a narrow coastal shelf that slopes into the Red Sea
Red Sea
and the Gulf of Aqaba. The elevation of Sinai's southern rim is about 1,000 m. Moving northward, the elevation of this limestone plateau decreases. The northern third of Sinai
Sinai
is a flat, sandy coastal plain, which extends from the Suez
Suez
Canal into the Gaza Strip
Gaza Strip
and Israel. Before the Israeli military occupied Sinai
Sinai
during the June 1967 War (Arab-Israeli war, also known as the Six-Day War), a single Egyptian governorate administered the whole peninsula. By 1982 after all of Sinai
Sinai
was returned to Egypt, the central government divided the peninsula into two governorates. North Sinai
Sinai
has its capital at Al Arish and the South
South
Sinai
Sinai
has its capital in Artt Turkishy. The abundance of life in the Sinai Peninsula
Sinai Peninsula
may not be immediately apparent. This again has its roots in the way in which the animals of the desert have adapted to life here. Many species, mammals especially, but also reptiles and even birds such as owls, are nocturnal. They spend the daylight hours in the relative cool of burrows, under boulders or in crevices and cracks in the rock. Many of these creatures will only be apparent from their tracks and trails or from a fleeting glimpse of a diminutive gerbil, or zig-zigging hare, in the car headlights at night. Even those animals that do brave the heat of the day are normally only active in the early morning or evening. With only sparse vegetation in which to hide, many desert species rely on camouflage as protection. Some, like the desert lark or the gerbils, are coloured in browns and beiges and russets to match the landscape. Others, such as Burton's Carpet Viper or the Sinai
Sinai
Leopard are strikingly patterned, but when seen against their natural desert backdrop that pattern breaks up the outline of the animal and it becomes difficult to distinguish. Even such large animals as the Nubian Ibex can be very hard to see against a cliff face as their initial response to a threat is to freeze. Unless they move they are virtually impossible to find. The few desert inhabitants that are boldly marked, generally in black and white ( like the Wheatears ), can be mistaken for a shadow. Very few of the desert animals are brightly coloured, one prominent exception in St Catherine being the bright blue Sinai
Sinai
Agama. In this case the objective is to be seen as the male agama is holding a territory against other males. Urban and rural areas[edit] In the 1970 census, 57 percent of Egypt's population was counted as rural, including those residing in agricultural areas in the Nile Valley and Delta, as well as the much smaller number of persons living in desert areas. Rural areas differ from the urban in terms of poverty, fertility rates, and other social factors. Agriculture
Agriculture
is a key component of the economy in rural areas, though some people are employed in the tourist industry or other non-farm occupations. In 1992, the percentage of Egypt's population employed in agriculture was 33 percent. The agricultural industry is dependent on irrigation from the Nile
Nile
river.[2] Extreme points[edit] This is a list of the extreme points of Egypt, the points that are farther north, south, east or west than any other location.

Northernmost point – unnamed headland immediately north-west of Sidi Barrani, Matruh Governorate Easternmost point – Ras Hadarba (Cape Elba), Red Sea
Red Sea
Governorate* Southernmost point - Jabal Bartazuga on the Sudanese border, Red Sea Governorate ** Westernmost point - unnamed point on the border with Libya
Libya
immediately east of the ruin of Qasr al Qarn in Libya, Matruh Governorate * Ras Hadarba lies within the Hala'ib triangle
Hala'ib triangle
which is claimed by Sudan
Sudan
but occupied by Egypt. If it is excluded, then Egypt's easternmost point is the Ras Banas peninsula on the mainland or, including islands, Mukawwa Island ** Egypt's southernmost point lies in the Bir Tawil
Bir Tawil
region, an area that is commonly included as part of Egypt
Egypt
but is not claimed by it. If this area is excluded then Egypt
Egypt
has no southernmost point, its southern border being formed by the 22nd parallel north.

Notes[edit]

^ Rosalie, David (1997). "The Geography and Historical Background". Pyramid Builders of Ancient Egypt: A Modern Investigation of Pharaoh's Workforce. Routledge. p. 14.  ^ Hopkins, Nicholas and Kirsten Westergaard (1998). Directions of Change in Rural Egypt. American University in Cairo. pp. 2–4. 

References[edit]

 This article incorporates public domain material from the Library of Congress Country Studies website http://lcweb2.loc.gov/frd/cs/.  This article incorporates public domain material from the CIA World Factbook website https://www.cia.gov/library/publications/the-world-factbook/index.html.

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