Hidden places you never imagine it is on the earth
Crastlr lake
Black westersn
The Western Desert of Egypt is an area of the Sahara that lies west of the river Nile, up to the Libyan border, and south from the Mediterranean Sea to the border with Sudan. It is named in contrast to the Eastern Desert which extends east from the Nile to the Red Sea. The Western Desert is mostly rocky desert, though an area of sandy desert, known as the Great Sand Sea, lies to the west against the Libyan border. The desert covers an area of 680,650 km2 (262,800 sq mi) which is two-thirds of the land area of the country.[1] Its highest elevation is 1,000 m (3,300 ft) in the Gilf Kebir plateau to the far south-west of the country, on the Egypt-Sudan-Libya border. The Western Desert is barren and uninhabited save for a chain of oases which extend in an arc from Siwa, in the north-west, to Kharga in the south. It has been the scene of conflict in modern times, particularly during the Second World War.
Quartz-rich sand from the Western Desert near Sakkara, Egypt.
Administratively the Western Desert is divided between various governorates; in the north and west, the Matrouh Governorate administers the area from the Mediterranean south to approx 27°40′ N latitude, and the New Valley Governorate from there to the Sudan border, while in the east parts of the Western Desert lie in the Giza, Fayyum, Beni Suef, and Minya Governorates
Moses mountain
Geography
Travel through the night to Mount Sinai to climb the mountain at night to see the sunrise from atop Moses’ Mountain. The descent after dawn to visit one of the oldest Christian monasteries in the world, St. Catherine, built around the site of the Burning Bush.
The region is described by one writer as “a plateau standing on average some 500 feet [150 m] above sea level, barren, rubble- and boulder-strewn, dark brown in colour, occasionally dotted with scrub, and, at first sight, flat”. He also states that little of the area conforms to “the romantic view… the Hollywood scenery of wind-formed dunes with occasional oases fringed with palm” (although such areas do exist in the Sand Sea where dunes are sculpted into fantastic shapes); the area is also the location of a series of oases created where the land dips sufficiently to meet the aquifer. These lie in an arc from Siwa in the north-west near the Libyan border, to Bahariya, Farafra, Dakhla, then Kharga in the south. East of Siwa lies the Qattara Depression, a low-lying area dotted with salt marsh and extending 310 km (190 mi) west to east and 135 km (84 mi) north to south. Further to the east, near the Nile, another depression gives rise to the Fayyum Oasis, a heavily populated area separate from the main Nile valley.
To the south, beyond the Bahariya oasis lies the Black Desert, an area of black volcanic hills and dolerite deposits. Beyond this, north of Farafra, lies the White Desert, an area of wind-sculpted chalk rock formations, which give the area its name. To the south of Kharga the plateau rises towards the Gilf Kebir, an upland region lying astride the Egypt-Sudan border and home to pre-historic sites such as the Cave of Swimmers.
In the south-west, near the point where the borders of Libya, Sudan and Egypt meet, is an area of desert glass, thought to have been formed by a meteorite strike at Kebira, over the border in Libya.
The Great Sand Sea is a roughly lung-shaped area of sandy desert lying astride the border with Libya, 320 km (200 mi) inland from the Mediterranean. The sea is divided by a long peninsula of rocky desert along the border, leaving the eastern lobe in Egypt and the western in Libya, where it is called the Calanshio desert. On the Egyptian side it was known historically as the “Libyan Desert”, taking its name from Ancient Libya, which lay between the Nile and Cyrenaica. With the formation of the state of Libya, the term “Western Desert” has come to describe the part of the Sahara in Egypt.
Boundaries
To the Ancient Greeks, the term Libya described the whole Saharan littoral west of the Nile to the Atlas Mountains. In Roman times, the term Libya was limited to Cyrenaica and the region between there and Egypt, organized as the provinces of Libya Superior and Libya Inferior. The term Libyan Desert then applied to the area to the south of these provinces. This became a misnomer during colonial times when Cyrenaica and the land to the west was organized as the Italian colony of Libya in 1911, and the term Western Desert used to describe the area within Egypt became more common.
Playfair described the Western Desert of 1940 as 390 km (240 mi) wide (i.e. from the Nile to the Libyan border) and 240 km (150 mi) from the Mediterranean to the latitude of Siwa Oasis, while the region to the south was referred to as the Inner Desert.However, during the Second World War the term Western Desert came to apply not only to the coastal desert of Egypt but also to the area fought over in Libya, ranging beyond the Egypt-Libya border to Gazala, Cyrenaica and even El Agheila.
The contemporary use of the term refers to the entire desert in Egypt west of the Nile.
Caprtic water
Cats grave
Blue hole
Dwone city
The submerged Palace of Cleopatra; an Underwater Heritage in Alexandria.
Antirhodos was an island in the eastern harbor of Alexandria, Egypt. Antirhodos existed until the year 365 when a massive earthquake believed to have been the biggest in the Ancient Mediterranean, sent off a wave of destruction that reached as far as the shores of Spain. The site now lies underwater, near the seafront of modern Alexandria, at a depth of approximately five metres (16 ft).
In 1996, underwater archaeology in the harbour of Alexandria conducted by Franck Goddio located the island and found that it was on the opposite side of the harbour from where it was placed by Strabo. Goddio uncovered the remains of a relatively modest (90 metres by 30 metres) marble-floored palace, believed to have been Cleopatra’s royal quarters. Cleopatra VII Philopator (69 BC-30 BC) was queen of the Ptolemaic Kingdom of Egypt from 51 to 30 BC, and its last active ruler. The remains on the island do not seem to date from later than the Ptolemaic period, suggesting the palace may have been abandoned soon after Cleopatra’s death and the absorption of Egypt into the Roman Republic
Egyptian animals
