Outside the areas of Nile silt deposits, the nature of such cultivable soil as exists depends upon the availability of the water supply and the type of rock in the area. Almost one-third of the total land surface of Egypt consists of Nubian sandstone, which extends over the southern sections of both the Eastern and Western deserts. Limestone deposits of Eocene age (i.e., some 35 to 55 million years old) cover a further one-fifth of the land surface, including central Sinai and the central portions of both the Eastern and Western deserts. The northern part of the Western Desert consists of limestone dating from the Miocene Epoch (25 to 5 million years ago). About one-eighth of the total area, notably the mountains of the Sinai, the Red Sea, and the southwest part of the Western Desert, consists of ancient igneous and metamorphic rocks.
The silt, which constitutes the present-day cultivated land in the delta and the Nile valley, has been carried down from the Ethiopian Highlands by the Nile’s upper tributary system, consisting of the Blue Nile and the ?A?barah rivers. The depth of the deposits ranges from more than 30 feet (10 metres) in the northern delta to about 22 feet (7 metres) at Asw?n. The White Nile, which is joined by the Blue Nile at Khartoum, in Sudan, supplies important chemical constituents. The composition of the soil varies and is generally more sandy toward the edges of the cultivated area. A high clay content makes it difficult to work, and a concentration of sodium carbonate sometimes produces infertile black-alkali soils. In the north of the delta, salinization has produced the sterile soils of the so-called bar?r? (“barren”) regions.
Egypt lies within the North African desert belt; its general climatic characteristics, therefore, are low annual precipitation and a considerable seasonal and diurnal (daily) temperature range, with sunshine occurring throughout the year. In the desert, cyclones stir up sandstorms or dust storms, called khamsins (Arabic: “fifties,” as they are said to come 50 days per year), which occur most frequently from March to June; these are caused by tropical air from the south that moves northward as a result of the extension northeastward of the low-pressure system of Sudan. A khamsin is accompanied by a sharp increase in temperature of 14 to 20 °F (8 to 11 °C), a drop in relative humidity (often to 10 percent), and thick dust; winds can reach gale force.
The climate is basically biseasonal, with winter lasting from November to March and summer from May to September, with short transitional periods intervening. The winters are cool and mild, and the summers are hot. Mean January minimum and maximum temperatures show a variation between 48 and 65 °F (9 and 18 °C) in Alexandria and 48 and 74 °F (9 and 23 °C) at Asw?n. The summer months are hot throughout the country’s inland, with mean midday high temperatures in June ranging from 91 °F (33 °C) at Cairo to 106 °F (41 °C) at Asw?n. Egypt enjoys a very sunny climate, with some 12 hours of sunshine per day in the summer months and between 8 and 10 hours per day in winter. Extremes of temperature can occur, and prolonged winter cold spells or summer heat waves are not uncommon.
Humidity diminishes noticeably from north to south and on the desert fringes. Along the Mediterranean coast the humidity is high throughout the year, but it is highest in summer. When high humidity levels coincide with high temperatures, oppressive conditions result.
Precipitation in Egypt occurs largely in the winter months; it is meagre on average but highly variable. The amount diminishes sharply southward; the annual average at Alexandria is about 7 inches (175 mm), Cairo has about 1 inch (25 mm), and Asw?n receives virtually nothing—only about 0.1 inch (2.5 mm). The Red Sea coastal plain and the Western Desert are almost without precipitation. The Sinai Peninsula receives somewhat more precipitation: the northern sector has an annual average of about 5 inches (125 mm).