a.Introduction
Albania republic in southeastern Europe, officially known as the Republic of Albania. It lies along the northwestern edge of the Balkan Peninsula.
Separated from Italy by only 76 km (47 mi) of the Adriatic Sea, Albania, throughout its history, has been occupied by Italian powers expanding eastward into the Balkans or by Balkan powers expanding westward. In the 1500s Albania came under the rule of the Ottoman Empire (centered in what is now Turkey), and did not gain its independence until 1912. From 1944 to 1990 Albania was a staunchly Communist state, and in 1991 Albania began its transition to a democratic state and market economy. The capital and largest city is Tirana.
b.Land and Resources
With a total area of 28,748 sq km (11,100 sq mi), Albania is roughly the size of the state of Massachusetts. The greatest distance from north to south is about 345 km (about 215 mi) and from east to west about 150 km (about 95 mi). Albania is bordered by the Adriatic Sea to the west, Greece to the south, the Former Yugoslav Republic of Macedonia (FYROM) to the east, and Serbia and Montenegro (formerly the Federal Republic of Yugoslavia, or FRY) to the north and northeast. The Yugoslav republics of Montenegro and Serbia lie to the north and northeast.
C. NATURAL REGIONS
Albania is a mountainous country in which about 70 percent of the land lies above 300 m (1,000 ft). Its mountains, which form a broad backbone from northwest to southeast, rise abruptly from the coastal lowlands to elevations of more than 2,400 m (8,000 ft). In the north are the most rugged mountains, where a massive limestone extension of the Dinaric Alps reaches inland for 40 km (25 mi) from nearby Montenegro. In the central uplands lies Mount Korab, the country's highest peak, at 2,764 m (9,068 ft). Strong erosive forces have created bare rock surfaces, deeply incised valleys, and a scarcity of meadowlands in this region. South of the Alps, the uplands are lower and more rounded, extending southeastward in a series of plateaus and ranges that merge with the Pindus Mountains in northern Greece.
The western coastal region consists of low hills and lower reaches of valleys that open onto the coastal plain. This is Albania's most densely populated area and comprises most of the land used for farming. Even here a series of flat areas are interrupted by hill country. Most of the soils are difficult to farm because of drainage and water-supply problems. Only the younger, lighter soils near the many rivers are easily cultivated, but are often flooded as well. Albania is subject to occasional earthquakes.
D. RIVERS AND
Albania's longest river is the Drin, total length 282 km (175 mi), which originates at two headwaters in Serbia and the FYROM and flows through northern Albania. Other major rivers include the Seman, the Shkumbin, and the Aأ³أ¶s (Vjأ¶se). Because most of Albania's rivers flow at high elevations, they are usually mountain torrents by the time they reach the coastal plain. In the mountains, rivers have cut deep gorges with near-vertical walls as high as 90 m (300 ft) above the water. The gorges make irrigation difficult, but are well suited for the huge dams that give Albania and nearby countries cheap hydroelectric power. Along the lower course of the rivers, irrigation is also difficult because sediment-laden streams often break out of their beds and shift channels. Irrigation is feasible only in valley bottoms. Albania also shares three large lakes with neighboring states. Lake Scutari in the north lies partly in Montenegro, Lake Ohrid in the east lies partly in the FYROM, while Lake Prespa in the southeast lies in Albania, the FYROM, and Greece.
E. NATURAL RESOURCES
Albania is rich in natural resources. The southwestern part of the country is well endowed with natural gas and petroleum. The northeastern region has large reserves of mineral deposits including chromium, copper, iron, and nickel. Large deposits of lignite (a soft, brown coal) are found near Tirana, and natural asphalt is mined near Selenic.
F. CLIMATE
Albania's climate varies with topography. The coastal lowlands have a Mediterranean climate with arid, almost cloudless summers featuring high temperatures both day and night. Winters are rainy but mild, and in the southern lowlands freezing temperatures are rare. In the mountains rain falls much more often in summer, and the northern regions experience more humidity than the south. Temperatures may soar in the daytime, but nights are much cooler. In winter the mountains, like the lowlands, are subject to heavy and frequent thunderstorms, but in the mountains storms are accompanied by heavy snow.
The average temperatures in August, the hottest month, range from 17آ° to 31آ°C (63آ° to 88آ°F). In January, the coldest month, they range from 2آ° to 12آ°C (36آ° to 54آ°F). December, the wettest month, has an average rainfall of 211 mm (8.3 in) while the driest months, July and August, receive only 32 mm (1.3 in) of rain. On the coast annual rainfall averages 1,000 mm (40 in), but it may be as great as 2,500 mm (100 in) in the mountains.