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1UpTravel - Geography Info and Facts of Countries : . - Albania


Albania Geography and Facts

Location: Southeastern Europe, bordering the Adriatic Sea and Ionian Sea, between Greece and Serbia and Montenegro

Geographic coordinates: 41 00 N, 20 00 E

Map references: Europe

Area:
total: 28,748 sq km
land: 27,398 sq km
water: 1,350 sq km

Area - comparative: slightly smaller than Maryland

Land boundaries:
total: 720 km
border countries: Greece 282 km, The Former Yugoslav Republic of Macedonia 151 km, Serbia and Montenegro 287 km (114 km with Serbia, 173 km with Montenegro)

Coastline: 362 km

Maritime claims:
continental shelf: 200-m depth or to the depth of exploitation
territorial sea: 12 nm

Climate: mild temperate; cool, cloudy, wet winters; hot, clear, dry summers; interior is cooler and wetter

Terrain: mostly mountains and hills; small plains along coast

Elevation extremes:
lowest point: Adriatic Sea 0 m
highest point: Maja e Korabit (Golem Korab) 2,753 m

Natural resources: petroleum, natural gas, coal, chromium, copper, timber, nickel, hydropower

Land use:
arable land: 21%
permanent crops: 5%
permanent pastures: 15%
forests and woodland: 38%
other: 21% (1993 est.)

Irrigated land: 3,410 sq km (1993 est.)

Natural hazards: destructive earthquakes; tsunamis occur along southwestern coast

Environment - current issues: deforestation; soil erosion; water pollution from industrial and domestic effluents

Environment - international agreements:
party to: Biodiversity, Climate Change, Hazardous Wastes, Ozone Layer Protection, Wetlands
signed, but not ratified: none of the selected agreements

Geography - note: strategic location along Strait of Otranto (links Adriatic Sea to Ionian Sea and Mediterranean Sea)



Albania

GEOGRAPHY

Size: 28,750 square kilometers (land area 27,400 square kilometers); slightly larger than Maryland.

Location: Southeastern coast of the Adriatic Sea and the eastern part of the Strait of Otranto, opposite the heel of the Italian boot; between approximately 40° and 43° north latitude.

Topography: A little over 20 percent is coastal plain, some of it poorly drained. Mostly hills and mountains, often covered with scrub forest. The only navigable river is the Bun.

Climate: Mild temperate; cool, cloudy, wet winters with a January low of 5°C; hot, clear, dry summers with a July high of 28°C; interior is cooler and wetter.

Boundaries: Land boundaries total 720 kilometers; borders with Greece 282 kilometers; border with former Yugoslav Republic of Macedonia 151 kilometers; border with Serbia 114 kilometers; border with Montengro 173 kilometers; coastline 362 kilometers.

Data as of April 1992



Albania

Topography

The 70 percent of the country that is mountainous is rugged and often inaccessible. The remainder, an alluvial plain, receives precipitation seasonally, is poorly drained, and is alternately arid or flooded. Much of the plain's soil is of poor quality. Far from offering a relief from the difficult interior terrain, the alluvial plain is often as inhospitable as the mountains. Good soil and dependable precipitation, however, are found in intermontane river basins, in the lake district along the eastern frontier, and in a narrow band of slightly elevated land between the coastal plains and the interior mountains (see fig. 3).

In the far north, the mountains are an extension of the Dinaric Alps and, more specifically, the Montenegrin limestone plateau. Albania's northern mountains are more folded and rugged, however, than most of the plateau. The rivers have deep valleys with steep sides and arable valley floors. Generally unnavigable, the rivers obstruct rather than encourage movement within the alpine region. Roads are few and poor. Lacking internal communications and external contacts, a tribal society flourished in this area for centuries. Only after World War II were serious efforts made to incorporate the people of the region into Albanian national life. A low coastal belt extends from the northern boundary southward to the vicinity of Vlor. On average, it extends less than sixteen kilometers inland, but widens to about fifty kilometers in the Elbasan area in central Albania. In its natural state, the coastal belt is characterized by low scrub vegetation, varying from barren to dense. There are large areas of marshlands 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 highly arable. Marginal land is reclaimed wherever irrigation is possible.

Just east of the lowlands, the central uplands, called ermenik by Albanians, are an area of generally moderate elevations, between 305 and 915 meters, with a few points reaching above 1,520 meters. Shifting along the faultline that roughly defines the western edge of the central uplands causes frequent, and occasionally severe, earthquakes.

Although rugged terrain and points of high elevation mark the central uplands, the first major mountain range inland from the Adriatic is an area of predominantly serpentine rock (which derives its name from its dull green color and often spotted appearance), extending nearly the length of the country, from the North Albanian Alps to the Greek border south of Kor. Within this zone, there are many areas in which sharp limestone and sandstone outcroppings predominate, although the ranges as a whole are characterized by rounded mountains.

The mountains east of the serpentine zone are the highest in Albania, exceeding 2,740 meters in the Mal Korab range. Together with the North Albanian Alps and the serpentine zone, the eastern highlands are the most rugged and inaccessible of any terrain on the Balkan Peninsula.

The three lakes of easternmost Albania, Lake Ohrid, Lake Prespa, and Prespa e Vogl, are remote and picturesque. Much of the terrain in their vicinity is not overly steep, and it supports a larger population than any other inland portion of the country. Albania's eastern border passes through Lake Ohrid; all but a small tip of Prespa e Vogl is in Greece; and the point at which the boundaries of three states meet is in Lake Prespa. Each of the two larger lakes has a total surface areas of about 260 square kilometers, and Prespa e Vogl is about one-fifth as large. The surface elevation is about 695 meters for Lake Ohrid and 855 meters for the other two lakes.

The southern mountain ranges are more accessible than the serpentine zone, the eastern highlands, or the North Albanian Alps. The transition to the lowlands is less abrupt, and the arable valley floors are wider. Limestone, the predominant mineral, is responsible for the cliffs and clear water of the coastline southeast of Vlor. Erosion of a blend of softer rocks has provided the sediment that has caused wider valleys to form in the southern mountain area than those characteristic of the remainder of the country. This terrain encouraged the development of larger landholding, thus influencing the social structure of southern Albania.

Data as of April 1992


Albania

Climate

With its coastline facing the Adriatic and Ionian seas, its highlands backed upon the elevated Balkan landmass, and the entire country lying at a latitude subject to a variety of weather patterns during the winter and summer seasons, Albania has a high number of climatic regions for so small an area. The coastal lowlands have typically Mediterranean weather; the highlands have a Mediterranean continental climate. In both the lowlands and the interior, the weather varies markedly from north to south.

The lowlands have mild winters, averaging about 7° C. Summer temperatures average 24° C, humidity is high, and the weather tends to be oppressively uncomfortable. In the southern lowlands, temperatures average about five degrees higher throughout the year. The difference is greater than five degrees during the summer and somewhat less during the winter.

Inland temperatures are affected more by differences in elevation than by latitude or any other factor. Low winter temperatures in the mountains are caused by the continental air mass that dominates the weather in Eastern Europe and the Balkans. Northerly and northeasterly winds blow much of the time. Average summer temperatures are lower than in the coastal areas and much lower at higher elevations, but daily fluctuations are greater. Daytime maximum temperatures in the interior basins and river valleys are very high, but the nights are almost always cool.

Average precipitation is heavy, a result of the convergence of the prevailing airflow from the Mediterranean Sea and the continental air mass. Because they usually meet at the point where the terrain rises, the heaviest rain falls in the central uplands. Vertical currents initiated when the Mediterranean air is uplifted also cause frequent thunderstorms. Many of these storms are accompanied by high local winds and torrential downpours.

When the continental air mass is weak, Mediterranean winds drop their moisture farther inland. When there is a dominant continental air mass, cold air spills onto the lowland areas, which occurs most frequently in the winter. Because the season's lower temperatures damage olive trees and citrus fruits, groves and orchards are restricted to sheltered places with southern and western exposures, even in areas with high average winter temperatures.

Lowland rainfall averages from 1,000 millimeters to more than 1,500 millimeters annually, with the higher levels in the north. Nearly 95 percent of the rain falls in the winter.

Rainfall in the upland mountain ranges is heavier. Adequate records are not available, and estimates vary widely, but annual averages are probably about 1,800 millimeters and are as high as 2,550 millimeters in some northern areas. The seasonal variation is not quite as great in the coastal area.

The higher inland mountains receive less precipitation then the intermediate uplands. Terrain differences cause wide local variations, but the seasonal distribution is the most consistent of any area.

Data as of April 1992


Albania

PHYSICAL ENVIRONMENT

National Boundaries

Albania, with a total area of 28,750 square kilometers, is slightly larger than the state of Maryland. It shares a 287- kilometer border with the Yugoslav republics of Montenegro and Serbia to the north, a 151-kilometer border with the Former Yugoslav Republic of Macedonia to the north and east, and a 282- kilometer border with Greece to the south and southeast. Its coastline is 362 kilometers long. The lowlands of the west face the Adriatic Sea and the strategically important Strait of Otranto, which puts less than 100 kilometers of water between Albania and the heel of the Italian "boot."

The distinct ethnic character of the Albanian people and their isolation within a generally definable area underscored their demands for independence in the early twentieth century. In some places, however, the mingling of different ethnic groups complicated the determination of national borders. Kosovo, across the northeastern Albanian border, was a Serbian-governed province, although ethnic Albanians made up over 90 percent of its population. Many Albanians still regarded Kosovo's status as an issue. Greeks and Albanians lived in the mountains on both sides of the southeastern Albanian boundary. Neither Greece nor Albania was satisfied with the division of nations effected by their common border.

With the exception of the coastline, all Albanian borders are artificial. They were established in principle at the 1912-13 conference of ambassadors in London. The country was occupied by Italian, Serbian, Greek, and French forces during World War I, but the 1913 boundaries were essentially reaffirmed by the victorious states in 1921. The original principle was to define the borders in accordance with the best interests of the Albanian people and the nationalities in adjacent areas. The northern and eastern borders were intended, insofar as possible, to separate the Albanians from the Serbs and Montenegrins; the southeast border was to separate Albanians and Greeks; the valuable western Macedonia lake district was to be divided among the three states- -Albania, Greece, and Yugoslavia--whose populations shared the area. When there was no compromise involving other factors, borderlines were chosen to make the best possible separation of national groups, connecting the best marked physical features available.

Allowance was made for local economic situations, for example, to prevent separation of a village from its animals' grazing areas or the markets for its produce. Political pressures also were a factor in the negotiations, but the outcome was subject to approval by powers having relatively abstract interests, most of which involved the balance of power rather than specific economic ambitions.

Division of the lake district among three states required that each of them have a share of the lowlands in the vicinity. Such an artificial distribution, once made, necessarily affected the borderlines to the north and south. The border that runs generally north from the lakes, although it follows the ridges of the eastern highlands, stays sixteen to thirty-two kilometers west of the watershed divide. Because negotiators at the London conference declined to use the watershed divide as the northeast boundary of the new state of Albania, a large Albanian population in Kosovo was incorporated into Serbia.

In Albania's far north and the northeast mountainous sections, the border connects high points and follows mountain ridges through the largely inaccessible North Albanian Alps, known locally as Bjeshkt e Namuna. For the most part, there is no natural boundary from the highlands to the Adriatic, although Lake Scutari and a portion of the Bun River south of it were used to mark Albania's northwest border. From the lake district south and southwest to the Ionian Sea, the country's southeast border goes against the grain of the land, crossing a number of ridges instead of following them.

Data as of April 1992



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