Eastern Desert in the context of "Coptos"

In Egypt, the Western Desert 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, although both are part of the broader Libyan desert in North Africa. The Western Desert is mostly rocky desert, save for an area of sandy desert, known as the Great Sand Sea, lying to the west and extending across the Libyan border.The desert covers an area of 680,650 km (262,800 sq mi) which is two-thirds of the land area of the country. 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.

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.

Egyptians (Arabic: مِصرِيُّون, romanized: Miṣriyyūn, IPA: [mɪsˤrɪjˈjuːn]; Egyptian Arabic: مَصرِيِّين, romanized: Maṣriyyīn, IPA: [mɑsˤɾɪjˈjiːn]; Coptic: ⲣⲉⲙⲛ̀ⲭⲏⲙⲓ, romanized: remenkhēmi) are an ethnic group native to the Nile Valley in Egypt. Egyptian identity is closely tied to geography. The population is concentrated in the Nile Valley, a small strip of cultivable land stretching from the First Cataract to the Mediterranean and enclosed by desert both to the east and to the west. This unique geography has been the basis of the development of Egyptian society since antiquity.

The daily language of the Egyptians is a continuum of the local varieties of Arabic; the most famous dialect is known as Egyptian Arabic or Masri. Additionally, a sizable minority of Egyptians living in Upper Egypt speak Sa'idi Arabic. Egyptians are predominantly adherents of Sunni Islam with a small Shia minority and a significant proportion who follow native Sufi orders. A considerable percentage of Egyptians are Coptic Christians who belong to the Coptic Orthodox Church, whose liturgical language, Coptic, is the most recent stage of the ancient Egyptian language and is still used in prayers along with Egyptian Arabic.

The Triakontaschoinos (Greek: Τριακοντάσχοινος, "Land of the Thirty Schoinoi"), Latinized as Triacontaschoenus, was a geographical and administrative term used in the Greco-Roman world for the part of Lower Nubia between the First and Second Cataracts of the Nile, which formed a buffer zone between Egypt and later Rome on the one hand and Meroë on the other hand. The northern part of this area, stretching from the First Cataract south to Maharraqa, was known as the Dodekaschoinos or Dodecaschoenus (Δωδεκάσχοινος, "Land of the Twelve Schoinoi"). In the Ptolemaic and Roman periods the Dodekaschoinos was often annexed to Egypt or controlled from it, and the rest of the Triakontaschoinos sometimes was as well.

In 275 or 274 BC, Ptolemy II (r. 283–246 BC) sent an army to Nubia, and defeated the Kingdom of Kush. The expedition pursued several objectives: on the one hand, it curbed Kushite power, which had been steadily expanding for the past century, and helped secure Ptolemaic rule against the native Egyptians of Upper Egypt, who might be tempted to seek Kushite aid in their revolts. In addition, the expedition secured the Ptolemies' control of the supply route for African elephants, which played a crucial role as war elephants in their conflicts with the rival Seleucid Empire, that monopolized access to the larger Indian elephants. As a result of this campaign, the area between the First and Second Cataracts of the Nile, which also included the valuable gold mines of the Eastern Desert, was annexed to Egypt and became later known as Triakontaschoinos.

Thebes (Arabic: طيبة, Ancient Greek: Θῆβαι, Thēbai), known to the ancient Egyptians as Waset, was an ancient Egyptian city located along the Nile about 800 kilometers (500 mi) south of the Mediterranean. Its ruins lie within the modern Egyptian city of Luxor. Thebes was the main city of the fourth Upper Egyptian nome (Sceptre nome) and was the capital of Egypt for long periods during the Middle Kingdom and New Kingdom eras. It was close to Nubia and the Eastern Desert, with its valuable mineral resources and trade routes. It was a religious center and the most venerated city during many periods of ancient Egyptian history.

The site of Thebes includes areas on both the eastern bank of the Nile, where the temples of Karnak and Luxor stand and where the city was situated; and the western bank, where a necropolis of large private and royal cemeteries and funerary complexes can be found. In 1979, the ruins of ancient Thebes were classified by UNESCO as a World Heritage Site.

The Mokattam (Arabic: المقطم  [elmoˈʔɑtˤ.tˤɑm], also spelled Muqattam), also known as the Mukattam Mountain or Hills, is the name of an Eastern Desert plateau as well as the district built over it in the Southern Area of Cairo, Egypt.

The Blemmyes (Ancient Greek: Βλέμμυες or Βλέμυες, Blémues [blé.my.es], Latin: Blemmyae) were an Eastern Desert people who appeared in written sources from the 7th century BC until the 8th century AD. By the late 4th century, they had occupied Lower Nubia and established a kingdom. From inscriptions in the temple of Isis at Philae, a considerable amount is known about the structure of the Blemmyan state.

The Blemmyes are usually identified as one of the components of the archaeological X-Group culture that flourished in Late Antiquity. Their identification with the Beja people who have inhabited the same region since the Middle Ages is generally accepted.

Itbāy (Arabic: اطبيه) or ʿAtbāy is a region of southeastern Egypt and northeastern Sudan. It is characterized by a chain of mountains, the Red Sea Hills, running north–south and parallel with the Red Sea. The hills separate the narrow coastal plain from the Eastern Desert.