Figure 2. Landform Regions in Albania
A low coastal belt extends from the northern boundary southward to about Vlore. It averages less than ten miles deep but widens to about thirty miles in the Elbasan area. In its natural state it is characterized by low scrub vegetation, varying from barren to dense. There are large areas of marshland and other areas of bare eroded badlands. Where elevations rise slightly and precipitation is regular—in the foothills of the central uplands, for example—the land is excellent. Marginal land is being reclaimed wherever irrigation is possible.
The land itself is of recent geological origin. It has been, and is being, created by sediments from the many torrents that erode the interior mountains. New alluvial deposits tend to be gravelly, without humus, and require many years before sufficient vegetation to make them fertile can be established. The sedimentation process, moreover, raises river channels above the level of the nearby terrain. Channels change frequently, devastating areas that have not been stabilized and creating marshes in others by blocking off the drainage. Road builders are confronted with difficult and constantly changing conditions.
Rainfall is heavy during the winter and is infrequent to nonexistent during nearly half the year. Mosquitoes thrive in the hot, humid, and marshy land. Only since about 1930 have there been effective measures to control malaria. Before then no extensive working of areas near the marshes could be seriously considered. For these reasons the coastal zone, in addition to supporting few people, has until relatively recently acted as a barrier, hindering, rather than encouraging, contact with the interior.
Coastal hills descend abruptly to Ionian Sea beaches along the Albanian Riviera from Vlore Bay southward to about Sarande. The 500- and 1,000-foot contour lines are within a mile or so of the water along nearly the entire distance. In the northern portion a 4,000-foot ridge is frequently only two to three miles inland. South of Sarande is another small area of coastal lowlands fronting on the Ionian Sea and separated from the Greek island of Corfu (Kerkira) by a mile-wide channel. Climate and soil conditions permit the cultivation of citrus fruits in this southernmost area of Albania.
Central Uplands
The central uplands region extends south from the Drin River valley, which marks the southern boundary of the North Albanian Alpine area, to the southern mountains. It is an area of generally lower mountain terrain immediately east of the lowlands. In the north, from the Drin River to the vicinity of Elbasan, it constitutes an area about twenty miles wide. It narrows to practically nothing in the vicinity of Elbasan, then widens into a broader triangular shape with its base against the southern mountains. Earth shifting along the faultline that roughly defines the western edge of the central uplands causes frequent and occasionally severe earthquakes. Major damage occurred over wide areas in 1967 and 1969.
Softer rocks predominate in the uplands. The most extensive are flysch, a soft crumbly rock that is usually sandstone but frequently contains shales, sandy limestones, and marl. This type of formation erodes rapidly and is the basis of much of the poor alluvial lowland soil. The ridges of the uplands are extensions of the Dalmatian coastal range that enters Albania from Yugoslavia. Elevations are generally moderate, between 1,000 and 3,000 feet with a few reaching above 5,000 feet.
Serpentine Zone