The nature of the soil and climate of Morocco are not unlike those of Spain and Portugal; and though Morocco does not materially differ from other parts of Barbary, its greater extent of coast on the Atlantic, along which the tradewind of the north coast blows nine months out of twelve, and its loftier ridges of the Atlas, so temper its varied surface of hill and plain and vast declivities that, together with the absence of those marshy districts which in hot climates engender fatal disease, this country may be pronounced, excepting perhaps Tunis, the most healthy in all Africa.
In the northern provinces, the climate is nearly the same as that of Spain; in the southern there is less rain and more of the desert heat, but this is compensated for by the greater fertility in the production of valuable staple articles of commerce. Nevertheless, Morocco has its extremes of heat and cold, like all the North African coast.
The most striking object of this portion of the crust of the globe, is the vast Atlas chain of mountains [15], which traverses Morocco from north-east to south-west, whose present ascertained culminating point, Miltsin, is upwards of 15,000 feet above the level of the sea, or equal to the highest peaks of the Pyrenees. The Maroquine portion of the Atlas contains its highest peaks, which stretch from the east of Tripoli to the Atlantic Ocean, at Santa Cruz; and we find no mountains of equal height, except in the tenth degree of North latitude, or 18,000 miles south, or 30,000 south, south-east. The Rif coast has a mountainous chain of some considerable height, but the Atlantic coast offers chiefly ridges of hills. The coasts of Morocco are not much indented, and consequently have few ports, and these offer poor protection from the ocean.
The general surface of Morocco presents a large ridge or lock, with two immense declivities, one sloping N.W. to the ocean, with various rivers and streams descending from this enormous back-bone of the Atlas, and the other fulling towards the Sahara, S.E., feeding the streams and affluents of Wad Draha, and other rivers, which are lost in the sands of the Desert. This shape of the country prevents the formation of those vast Sebhahas, or salt lakes, so frequent in Algeria and the south of Tunis. We are acquainted