THE IBERIAN PENINSULA 669 the sea have been few. Where coastal plains exist, they are usually narrow, and mountains or the abrupt edge of the plateau render con- tacts with the interior very difficult. The major portion of the popula- tion consequently had little interest in or knowledge of the sea. Even during the days of Iberian supremacy, and at the period when trade routes were most favorable, such maritime activities as were carried on seem to have been the result of a conscious effort rather than a natural growth. Only the people of the Portuguese plain have main- tained an interest in the sea, and this consists largely in carrying on coastal trade. This lack of commercial interests and development has isolated the peoples of the peninsula culturally and economically, and has made it difficult for them to take advantage of such favorable locational factors as have existed. CLIMATE The location of the peninsula causes most of it to be within the dry horse latitudes and trades in the summer, and within the prevailing westerly belt in the winter. Rainfall is accordingly seasonal, coming largely during the autumn and winter. A deficiency of rainfall charac- terizes most of the land, and limits agriculture. In this the peninsula would seem to conform with the other Mediterranean lands. But in spite of the fact that the sea forms seven-eighths of the boundaries of the peninsula, bordering mountains and an average elevation of some 2200 feet restrict the moderating influence of the water, and give the greater part of the land a continental climate. Thus, in contrast to most Mediterranean lands, it is a region of extremes in temperature. How- ever, relief and latitude cause the peninsula to be divided into four climatic zones, each of which has a distinct influence on vegetation and human development. The highlands of the north and the northwest have a climate en- tirely different from the rest of the peninsula. Cool summers and mild winters, with heavy and evenly distributed rainfall, favor forest growth, the raising of forage crops, and dairying. The climate and the resulting types of agriculture thus resemble those of northwestern Europe. This same type of climate extends south along the western seaboard as far as central Portugal. The "meseta" or plateau which occupies about three-fourths of the peninsula has an< extreme continental climate, with light rainfall coming mostly during the winter. The rainfall is a little heavier in the northwestern portion of the plateau, and here is located the great