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See also: form the See also: southern extremities of the See also: European continent
.
Its See also: area, 184,779 sq. m., is about 35,000 sq. m. less than that of the Iberian Peninsula, but more than twice that of the See also: Italian
.
Its See also: northern boundary stretches from the See also: Kilia mouth of the Danube to the Adriatic See also: Sea near Fiume, and is generally regarded as marked by the courses of the See also: rivers Danube, Save and Kulpa
.
On the E. it is bounded by the Black Sea, the Sea of Marmora, and the See also: Aegean; on the S. by the Mediterranean; on the W. by the Ionian Sea and the Adriatic
.
With the exception of the Black Sea See also: coast and the Albanian littoral, its shores are considerably indented and flanked by See also: groups of islands
.
The Peninsula in its general See also: contour resembles an inverted See also: pyramid or triangle, terminating at its See also: apex in a subsidiary peninsula, the See also: Peloponnesus or Morea
.
Its See also: surface is almost entirely mountainous, the only extensive plains being those formed by the valleys of the Danube and Maritza, and the See also: basin of See also: Thessaly drained by the Salambria (See also: ancient Peneus)
.
The Danubian plain, lying, for the most See also: part, outside the Peninsula, is enclosed, on the See also: north, by the Carpathians; and on the See also: south by the Balkans, from which the Peninsula derives its name
.
These ranges form together the See also: great semicircular See also: mountain-chain, known as the See also: anti-Dacian See also: system, through which the Danube finds a passage at the Iron See also: Gates
.
The other mountain-systems display great complexity of formation; beginning with the Dinaric See also: Alps and the parallel ranges of Bosnia, they run, as a See also: rule, from north-west to south-See also: east; the great chain of Rhodope traverses the centre of the Peninsula, throwing out spurs towards the Black Sea and the Aegean; farther west are the lofty Shar Dagh and the mountains of See also: Montenegro and See also: Albania, continued by the See also: Pindus range and the heights of See also: Acarnania and See also: Aetolia
.
The See also: principal summits are See also: Olympus (9794 ft.), overlooking the Gulf of See also: Salonica; Musalla (9631) and Popova Shapka (8855), both in the Rhodope system; Liubotrn in the Shar Dagh (8989); Elin, in the Perin Planina (8794); Belmeken in southern See also: Bulgaria (chain of Dospat, 8562); Smolika in the Pindus range (8445); • Dormitor in northern Montenegro (8294); Kaimakchalan in central See also: Macedonia (8255);and Kiona in Aetolia (8235)
.
Owing to the distribution of the mountain-chains, the principal rivers flow in an easterly or south-easterly direction; the Danube falls into the Black Sea; the Maritza, Mesta, Struma (Strymon), Vardar and Salambria into the Aegean
.
The only considerable rivers flowing into the Adriatic are the Narenta, Drin and Viossa . The principal lakes are those of Ochrida, Prespa,See also: Scutari and Iannina
.
The See also: climate is more severe than that of the See also: sister peninsulas, and the temperature is liable to sudden changes
.
The winter, though See also: short, is often intensely cold, especially in the Danubian plain and in See also: Thrace, the rigorous climate of which is frequently alluded to by the Latin poets
.
Bitter north-easterly winds prevail in the spring, and snow is not uncommon even in the low-lying districts of See also: Greece
.
The autumn weather is generally See also: fine and clear
.
Geology.—Broadly speaking, the See also: Balkan Peninsula may be divided into four areas which geologically are distinct
.
There is a central region, roughly triangular in shape, with its See also: base resting upon the
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