Online Encyclopedia

BALKAN PENINSULA

Online Encyclopedia
Originally appearing in Volume V03, Page 258 of the 1911 Encyclopedia Britannica.
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BALKAN PENINSULA  , the most easterly of the three large peninsulas which form the
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southern extremities of the
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European continent . Its
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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
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Italian . Its
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northern boundary stretches from the
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Kilia mouth of the Danube to the Adriatic Sea near Fiume, and is generally regarded as marked by the courses of the rivers Danube, Save and Kulpa . On the E. it is bounded by the Black Sea, the Sea of Marmora, and the
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Aegean; on the S. by the Mediterranean; on the W. by the Ionian Sea and the Adriatic . With the exception of the Black Sea coast and the Albanian littoral, its shores are considerably indented and flanked by groups of islands . The Peninsula in its general
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contour resembles an inverted
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pyramid or triangle, terminating at its
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apex in a subsidiary peninsula, the Peloponnesus or Morea . Its
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surface is almost entirely mountainous, the only extensive plains being those formed by the valleys of the Danube and Maritza, and the basin of
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Thessaly drained by the Salambria (ancient Peneus) . The Danubian plain, lying, for the most
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part, outside the Peninsula, is enclosed, on the north, by the Carpathians; and on the south by the Balkans, from which the Peninsula derives its name . These ranges form together the
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great semicircular mountain-chain, known as the anti-Dacian
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system, through which the Danube finds a passage at the Iron Gates . The other mountain-systems display great complexity of formation; beginning with the Dinaric
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Alps and the parallel ranges of Bosnia, they run, as a
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rule, from north-west to south-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
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Montenegro and
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Albania, continued by the
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Pindus range and the heights of
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Acarnania and
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Aetolia . The
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principal summits are
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Olympus (9794 ft.), overlooking the Gulf of 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 Bulgaria (chain of Dospat, 8562); Smolika in the Pindus range (8445); • Dormitor in northern Montenegro (8294); Kaimakchalan in central
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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, Scutari and Iannina . The
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climate is more severe than that of the
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sister peninsulas, and the temperature is liable to sudden changes . The winter, though short, is often intensely cold, especially in the Danubian plain and in
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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
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Greece . The autumn weather is generally
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fine and clear . Geology.—Broadly speaking, the
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Balkan Peninsula may be divided into four areas which geologically are distinct . There is a central region, roughly triangular in shape, with its
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base resting upon the emeeyW5 e,, ..

End of Article: BALKAN PENINSULA
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