Greece is a small country, but the variety of its climate is

nevertheless great. Striking differences in the climate of different

localities are produced by the contrasts between mountains and plains,

woodlands and sterile valleys, coasts having a northern or southern

aspect. But even leaving out of sight these local differences, it

may safely be asserted that the varieties of climate which we meet

with in traversing Greece from north to south are scarcely exceeded

in any other region. The mountains of Ætolia, in the north, whose

slopes are covered with beech-trees, remind us of the temperate zone

of Europe, whilst the peninsulas and islands towards the east and

south, with their thickets of fig and olive trees, their plantations

of oranges and lemons, their aloe hedges and rare palm-trees, belong

to the sub-tropical zone. But even neighbouring districts occasionally

{40} differ strikingly as regards climate. In the ancient lake basin

of Bœotia the winters are cold, the summers scorching, whilst the

temperature of the eastern shore of Eubœa is equable, owing to the

moderating influence of sea breezes. Within a narrow compass Greece

presents us with the climates of a large portion of the earth, and

there can be no doubt that this diversity of climate, and the contrasts

of every kind springing from it, must have favourably influenced the

intellectual development of the Hellenes. A spirit of inquiry was

called forth amongst them which reacted upon their commercial tastes

and industrial proclivities.

The diversity of the climate of the land, however, is compensated for,

in Greece, by a uniformity in the climate of the maritime districts. As

in a mountain valley, the winds of the Ægean Sea blow alternately in

contrary directions. During nearly the whole of summer the atmospheric

currents of Eastern Europe are attracted towards the African deserts.

The winds from the north of the Archipelago and Macedonia then speed

the navigator on his voyage to the south, and on many occasions the

conquering tribes of the northern shores of that sea have availed

themselves of them in their improvised attacks upon the inhabitants

of the more southern districts of Asia Minor and of Greece. These

regular northerly currents, known as etesian or annual winds, cease

on the termination of the hot season, when the sun stands above the

southern tropic. They are, moreover, interrupted every night, when

the cool sea air is attracted by the heated surface of the land.

When the sun has set the wind gradually subsides; there is a calm,

lasting a few moments; and then the air begins to move in an inverse

direction—“the land begins to blow,” as the sailors say. Nor is this

regular wind without its counter-current, known as the _embates_, or

propitious south-easterly breeze of which the poets sing. General winds

and breezes, moreover, are deflected from their original directions

in consequence of the configuration of the coast and the direction

of mountain chains. The Gulf of Corinth, for instance, is shut in by

high mountains on the north and the south, and the winds alternately

enter it from the east or west—a phenomenon likened by Strabo to the

breathing of an animal.

The rains, like the winds, deviate in many places from the average,

and whilst the water pours down into some mountain valleys as into a

funnel, elsewhere the clouds drift past without parting with a drop of

their humid burden. Contrasts in the amount of precipitation are thus

added to those resulting from differences of configuration and variety

of climate. As a rule, rain is more abundant on the western shores of

Greece than on the eastern, and this fact accounts for the smiling

aspect of the hills of Elis, as compared with the barren declivities

of Argolis and Attica. Thunder-storms, driven before the winds of the

Mediterranean, likewise recur with greater regularity in the western

portion of the peninsula. In Elis and Acarnania the roll of thunder may

be heard in spring daily, for whole weeks, in the afternoon. No sites

more apposite could have been found for temples dedicated to Jupiter,

the god of lightning.

* * * * *

The ancient inhabitants of the Cyclades, and probably, also, those

of the coasts {41} of Hellas and Asia Minor, had already attained a

considerable amount of culture long before the commencement of our

historical records. This has been proved by excavations made in the

volcanic ashes of Santorin and Therasia. At the time their houses were

buried beneath the ashes, the Santoriniotes had begun to pass from the

age of stone into that of copper. They knew how to build arches of

stone and mortar, they manufactured lime, used weights made of blocks

of lava, wove cloth, made pottery, dyed their stuffs, and ornamented

their houses with frescoes; they cultivated barley, peas, and lentils,

and had begun to trade with distant countries.

We do not know whether these men were of the same race as the Hellenes;

but thus much is certain—that at the earliest dawn of history the

islands and coasts of the Ægean Sea were peopled by various families of

Greeks, whilst the interior of the country and the western shores of

the peninsula were inhabited by Pelasgians. These Pelasgians, moreover,

were of the same stock as the Greeks, and they spoke a language derived

from the same source as the dialects of the Hellenes. Both were Aryans,

and, unless natives of the soil, they must have immigrated into Greece

from Asia Minor by crossing the Hellespont, or by way of the islands

of the Archipelago. The Pelasgians, according to tradition, sprang

from Mount Lycæus, in the centre of the Peloponnesus; they boasted of

being “autochthons,” “men of the black soil,” “children of oaks,” or

“men born before the moon.” All around them lived tribes of kindred

origin, such as the Æolians and the Leleges, and these were afterwards

joined by Ionians and Achæans. The Ionians, who, in a subsequent age,

exercised so great an influence over the destinies of the world, only

occupied the peninsula of Attica and the neighbouring Eubœa. The

Achæans for a long time enjoyed a preponderance, and in the end the

Greek clans collectively became known by that name. Later on, when

the Dorians had crossed the Gulf of Corinth where it is narrowest,

and established themselves as conquerors in the Peloponnesus, the

Amphictyons, or national councils, sitting alternately at Thermopylæ

and Delphi, conferred the name of Hellenes, which was that of a small

tribe in Thessaly and Phthiotis, upon all the inhabitants of the

peninsula and the islands. The name of Greek, which signifies, perhaps,

“mountaineer,” “ancient,” or “son of the soil,” gradually spread

amongst the nation, and in the end became general. The Ionians of Asia

Minor, and the Carians of the Sporades, emulated the Phœnicians by

trading from port to port amongst these half-savage tribes, and, like

bees which convey the fecundating pollen from flower to flower, they

carried the civilisation of Egypt and the East from tribe to tribe.

[Illustration: Fig. 9.—MAINOTE AND SPARTAN.]

Phœnician merchants and Roman conquerors scarcely modified the elements

composing the population of Hellas, but during the age of migrations

barbarians in large numbers penetrated into Greece. For more than two

centuries did the Avares maintain themselves in the Peloponnesus. Then

came the Slavs, aided, on more than one occasion, by the plague in

depopulating the country. Greece became a Slavonia, and a Slavonian

language, probably Servian, was universally spoken, as is proved by

the majority of geographical names. The superstitions and legends {42}

of the modern Greeks, as has been remarked by many authors, are not

simply a heritage derived from the ancient Hellenes, but have become

enriched by phantoms and vampires of Slav invention. The dress of the

Greeks, too, is a legacy of their northern conquerors. But, in spite

of this, the polished language of the Hellenes {43} has regained by

degrees its ancient preponderance, and the race has so thoroughly

amalgamated these foreign immigrants, that it is impossible now to

trace any Servian elements in the population. But hardly had Hellas

escaped the danger of becoming Slav when it was threatened with

becoming Albanian. This occurred during the dominion of Venice. As

recently as the commencement of the present century Albanian was the

dominant language of Elis, Argos, Bœotia, and Attica, and even at the

present day a hundred thousand supposed Hellenes still speak it. The

actual population of Greece is, therefore, a very mixed one, but it is

difficult to say in what proportions these Hellenic, Slav, and Albanian

elements have combined. The Mainotes, or Maniotes, of the peninsula

terminating in Cape Matapan, are generally supposed to be the Greeks of

the purest blood. They themselves claim to be the descendants of the

ancient Spartans, and amongst their strongholds they still point out

one which belonged to “Signor Lycurgus.” Their Councils of Elders have

preserved from immemorial times, and down to the war of independence,

the title of Senate of Lacedæmonia. Every Mainote professes to love

unto death “Liberty, the highest of all goods, inherited from our

Spartan ancestors.” Nevertheless, a good many localities in Maina bear

names derived from the Servian, and these prove, at all events, that

the Slavs resided in the country for a considerable time. The Mainotes

practise the _vendetta_, as if they were Montenegrins. But is not this

a common custom amongst all uncivilised nations?

However this may be, in spite of invasions and intermixture with other

races, the Greeks of to-day agree in most points with the Greeks of

the past. Above all things, they have preserved their language, and

it is truly matter for surprise that the vulgar Greek, though derived

from a rural dialect, should differ so slightly only from the literary

language. The differences, analogous to what may be observed with

respect to the languages derived from the Latin, are restricted almost

to two points, viz. the contraction of non-accentuated syllables and

the use of auxiliary verbs. It was, therefore, easy for the modern

Greeks to purify their language from barbarisms and foreign terms,

and to restore it gradually to what it was in the time of Thucydides.

Nor has the race changed much in its physical features, for in most

districts of modern Greece the ancient types may yet be recognised.

The Bœotian is still distinguished by that heavy gait which made him

an object of ridicule amongst the other Greeks; the Athenian youth

possesses the suppleness, grace of movement and bearing which we admire

so much in the horsemen sculptured on the friezes of the Parthenon; the

Spartan women have preserved that haughty and vigorous beauty which

constituted the charm of the virgins of Doris. As regards morals,

the descent of the modern Hellenes is equally evident. Like their

ancestors, they are fond of change, and inquisitive; as the descendants

of free citizens, they have preserved a feeling of equality; and,

still infatuated with dialectics, they hold forth at all times as

if they were in the ancient market-place, or Agora. They frequently

stoop to flattery: like the ancient Greeks, too, they are apt to rate

intellectual merit above purity of morals. {44} Like sage Ulysses of

the Homeric poem, they well know how to lie and cheat with grace; and

the truthful Acarnanian and the Mainote, who are “slow to promise,

but sure to keep,” are looked upon as rural oddities. Another trait

in the character of the modern and ancient Greeks, and one which

distinguishes them from all other Europeans, is this—that they do not

allow themselves to be carried away by passion, except in the cause of

patriotism. The Greek is a stranger to melancholy: he loves life, and

is determined to enjoy it. In battle he may throw it away, but suicide

is a species of death unknown amongst the modern Greeks, and the more

unhappy they are, the more they cling to existence. They are very

seldom afflicted with insanity.

[Illustration: Fig. 10.—FOREIGN ELEMENTS IN THE POPULATION OF GREECE.]

In spite of the diverse elements which compose it, the Greek

nationality is one of the most homogeneous in Europe. The Albanians,

of Pelasgian descent like the Greeks, do not cede to the latter in

patriotism; and it was they—the Suliotes, Hydriotes, Spezziotes—who

fought most valiantly for national independence. The eight hundred

families of Rumanian or Kutzo-Wallachian Zinzares who pasture

their herds in the hills of Acarnania and Ætolia, and are known as

Kara-Gunis, or “black cloaks,” speak the two languages, and sometimes

marry Greek girls, though they never give their own daughters in

marriage to the Greeks. Haughty and free, they are not sufficiently

numerous to be of any great importance. To foreigners the Greeks are

rather intolerant, and they take no pains to render their stay amongst

them agreeable. The Turks—who were numerous formerly in certain parts

of the Peloponnesus, in Bœotia, and in the {45} island of Eubœa, and

whose presence recalled an unhappy period of servitude—have fled to

a man, and only the fez, the narghile, and the slippers remind us of

their former presence. The Jews, though met with in every town of the

East, whether Slav or Mussulman, dare hardly enter the presence of the

Greeks, who are, moreover, their most redoubtable rivals in matters

of finance: they are to be found only in the Ionian Islands, where

they managed to get a footing during the British Protectorate. In this

same Archipelago we likewise meet with the descendants of the ancient

Venetian colonists, and with emigrants from all parts of Italy. French

and Italian families still form a distinct element of the population

of Naxos, Santorin, and Syra. As to the Maltese porters and gardeners

at Athens and Corfu, they continue for the most part in subordinate

positions, and never associate with the Greeks.

* * * * *

The homogeneous character of the population of Greece does not admit

of that country being divided into ethnological provinces, like

Turkey or Austro-Hungary, but it consists geographically of four

distinct portions. These are (1), continental Hellas, known since the

Turkish invasion as Rumelia, in remembrance of the “Roman” empire of

Byzantium; (2), the ancient Peloponnesus, now called the Morea, perhaps

a transposition of the word “Romea,” or from a Slav word signifying

“sea coast,” and applied formerly to Elis; (3), the islands of the

Ægean Sea; (4), the Ionian Islands. In describing the various portions

of Greece we shall make use, in preference, of the ancient names of

mountains, rivers, and towns; for the Hellenes of our own day, proud of

the glories of the past, are endeavouring gradually to get rid of names

of Slav or Italian origin, which still figure upon the maps of their

country.[13]

II.—CONTINENTAL GREECE.

The Pindus, which forms the central chain of Southern Turkey, passes

over into Greece, and imparts to it an analogous orographical

character. On both sides of this conventional boundary we meet with the

same rocks, the same vegetation, the same landscape features, and the

same races of people. By dividing the Epirus and handing over Thessaly

to the Turks, European diplomacy has paid no attention to natural

features. The eastern portion of the boundary is made to follow the

line of water parting over the range of the lofty Othrys, commanding

the plain of the Sperchius. Westward of the Pindus the boundary {46}

crosses transversely the valley of the Achelous, and the hills which

separate it from the Gulf of Arta.

[Illustration: Fig. 11.—MOUNT PARNASSUS AND DELPHI.]

The isolated summit of Mount Tymphrestus, or Velukhi, which rises where

the grand chain of the Othrys branches off from the Pindus, is not the

culminating point of continental Greece, but it is a centre from which

the principal mountain spurs and rivers radiate. Within its spurs lies

hidden the charming valley of Karpenisi, and an elevated ridge joins

them, towards the south-east, to the most important mountain mass of

modern Greece, viz. the group surmounted by the snow-clad pyramids of

the Vardusia and Khiona, whose slopes are covered with dark firs, and

to the superb Katavothra, the Œta of the ancients, on which Hercules

built his funeral pile. The mountains of Vardusia and Khiona are face

to face with the fine mountain masses of Northern Morea, likewise

wooded and covered with snow during the greater part of the year.

The mountains of Ætolia, to the west of the Velukhi and the Vardusia,

are far less elevated, but they are rugged, and form a veritable chaos

of rocks, savage defiles, and thickets, into which only Wallachian

herdsmen venture. In Southern Ætolia, on the shores of the lakes and

along the rivers, the country is more accessible, but mountains rise

there likewise, and by tortuous ridges they are brought into connection

with the system of the Pindus. Those on the coast of Acarnania,

opposite to the Ionian Islands, are steep, covered with trees and

shrubs; they are the mountains of the “Black Continent” mentioned by

Ulysses. {47} To the east of the Achelous there is another coast

chain, well known to mariners: this is the Zygos, the southern slopes

of which, arid and austere, are seen from off Missolonghi. Still

further to the east another range comes down to the seashore, and,

together with the promontories on the opposite coast of the Morea,

forms the narrow entrance to the Gulf of Corinth. Close to this

entrance, on the Ætolian side, there rises bold Mount Varassova, a huge

block of rock. Local tradition tells us that the Titans endeavoured to

throw this rock into the sea, so that it might form a bridge between

the two coasts; but the rock proved too heavy, and it was dropped where

we now see it.

Towards the Ægean Sea the mountain mass of the Katavothra is continued

by a coast range running in a direction parallel to the mountains of

the island of Eubœa. This range should be described rather as a series

of mountain-groups separated from each other by deep hollows, extensive

depressions, and even by river valleys. These mountains, though low

and intersected by numerous roads, are nevertheless difficult of

access, for their slopes are steep, their promontories abrupt, and

their precipices sudden, and in the times of the ancient Greeks a small

number of men repeatedly defended them against large armies. At one

extremity of this range is the passage of Thermopylæ; at the other, on

the eastern foot of the Pentelicus, the famous plain of Marathon.

The mountain groups on the northern shore of the Gulf of Corinth, and

to the south of Bœotia, may be looked upon as a range running parallel

with that following the channel of Eubœa, but far more beautiful and

picturesque. Every one of its summits recalls the sweet memories of

poetry, or conjures up the image of some ancient deity. To the west we

find ourselves in the presence of “double-headed” Parnassus, to which

fled Deucalion and Pyrrha, the ancestors of the Greeks, and where the

Athenians celebrated their torchlight dances in honour of Bacchus.

From the summits of the Parnassus, which rival in height those of the

Khiona, raising its pyramidal head towards the north-west, nearly the

whole of Greece, with its gulfs, islands, and mountains, lies spread

out below us, from the Thessalian Olympus to the Taygetus, at the

extremity of the Peloponnesus; and close by, at our feet, lies the

admirable basin of Delphi, the place of Peace and Concord, where Greeks

forgot their animosities. The mountain group towards the east next to

Parnassus is quite equal to it. The valleys of the Helicon, the seat of

Apollo and the Muses, are still the most verdant and the most smiling

in all Greece. The eastern slope of the Helicon is more especially

distinguished for its charming beauty, its woods, its verdant pastures,

gardens, and murmuring springs, which contrast most favourably with the

bare and arid plains of Bœotia. If Mount Parnassus may boast of the

Castalian spring, Mount Helicon possesses that of Hippocrene, which

burst forth from the ground when struck by the hoof of Pegasus. The

elongated summit of the Cithæron, the birthplace of Bacchus, joins

the mountains of Southern Bœotia to those of Attica, whose marble has

become famous through the neighbourhood of the city which they shelter.

Mount Parnes rises to the north of Athens; to the east of it, like the

pediment of a temple, rises the Pentelicus, in which are {48} the

quarries of Pikermi, rendered famous through their fossil bones; on the

south appears Mount Hymettus, celebrated for its flowers and its bees.

Farther away, the Laurium, with its rich argentiferous slags, stretches

towards the south-east, and terminates in Cape Sunium, consecrated in

other days to Minerva and Neptune, and still surmounted by fifteen

columns of an ancient temple.

Another isolated mountain group to the south of Attica, and occupying

the entire width of the Isthmus of Megara, served the Athenians as a

rampart of defence against their neighbours of the Peloponnesus. This

is the mountain group of Gerania, the modern Pera Khora.[14] Having

passed beyond it, we find ourselves upon the Isthmus of Corinth,

properly so called, confined between the Gulfs of Athens and of

Corinth. It is a narrow neck of land, scarcely five miles across,

whose arid limestone rocks hardly rise two hundred feet above the sea.

This neutral bit of territory, lying between two distinct geographical

regions, naturally became a place for meetings, festivals, and markets.

The remains of a wall built by the Peloponnesians across the isthmus

may still be traced, as may also the canal commenced by order of Nero.

* * * * *

The limestone mountains of Greece, as well as those of the Epirus and

of Thessaly, abound in lakes, but all the rivers are swallowed up in

“sinks,” or _katavothras_, leaving the land dry and arid. Southern

Acarnania, a portion of which is known as Xeromeros, or the “arid

country,” on account of the absence of running water, abounds in

lake basins of this kind. To the south of the Gulf of Arta, which

may not inaptly be described as a sort of lake communicating with

the sea through a narrow opening, there are several sheets of water,

the remains of an inland sea, silted up by the alluvial deposits of

the Achelous. The largest of these lakes is known to the natives as

Pelagos, or “big sea,” because of its extent and the agitated state of

its waters, which break against its coasts. This is the Trichonius of

the ancient Ætolians. Reputed unfathomable, it is, in truth, very deep,

and its waters are perfectly pure; but they are discharged sluggishly

into another basin far less extensive, and surrounded by pestilential

marshes, and through a turgid stream they even find their way into

the Achelous. The hills surrounding Lake Trichonis are covered with

villages and fields, whilst the locality around the lower lake has

been depopulated by fever. The country, nevertheless, is exceedingly

beautiful to look upon. Hardly have we passed through a narrow gorge,

or _klisura_, of Mount Zygos before we enter upon a bridge over a

mile in length, which a Turkish governor caused to be thrown across

the swamps separating the two lakes. This viaduct has sunk down more

than half its {49} height into the mud, but it is still sufficiently

elevated to enable the eye freely to sweep over the surface of the

waters, and to trace the coasts which bound them. Oaks, planes, and

wild olive-trees intermingle beneath us, their branches hung with

festoons of wild vine, and these, with the blue waters of the lake and

the mountains rising beyond it, form a picture of great beauty.

[Illustration: Fig. 12.—LOWER ACARNANIA.

Scale 1 : 800,000.]

The Earth and its inhabitants, Volume 1: Europe. Greece, Turkey in Europe, Rumania, Servia, Montenegro, Italy, Spain, and Portugal. · 第 5 / 53 段