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The face of the Peloponnesus presents outlines somewhat more intricate than those of northern Greece. At first sight the whole land appears one pile of mountains, which, toward the northwest, where it reaches its greatest height, forms a compact mass, pressing close upon the Gulf of Corinth. On the western coast it recedes farther from the sea; towards the centre is pierced more and more by little hollows; and on the south and east is broken by three great gulfs, and the valleys opening into them, which suggested to the ancients the form of a plane leaf, to illustrate that of the peninsula. On closer inspection, the highest summits of this pile, with their connecting ridges, may be observed to form an irregular ring, which separates the central region, Arcadia, from the rest.

The other great divisions of the Peloponnesus are Argolis, Laconia, Messenia, Elis, and Achaia. Argolis, when the name is taken in its largest sense, as the part of the Peloponnesus which is bounded on the land side by Arcadia, Achaia, and Laconia, comprehends several districts, which, during the period of the independence of Greece, were never united under one government, but were considered, for the purpose of description, as one region by the later geographers. It begins on the western side with the little territory of Sicyon, which, beside some inland valleys, shared with Corinth a small maritime plain, which was proverbial among the ancients for its luxuriant fertility. The dominions of Corinth, which also extended beyond the isthmus, meeting those of Megara a little south of the Scironian rocks, occupied a considerable portion of Argolis. The two cities, Sicyon and Corinth, were similarly situated—both commanding important passes into the interior of the peninsula. The lofty and precipitous rock, called the Acrocorinthus, on which stood the citadel of Corinth, though, being commanded by a neighbouring height, it is of no great value for the purposes of modern warfare, was in ancient times an impregnable fortress, and a point of the highest importance.

The plain of Argos, which is bounded on three sides by lofty mountains, but open to the sea, is, for Greece, and especially for the Peloponnesus, of considerable extent, being ten or twelve miles in length, and four or five in width. But the western side is lower than the eastern, and is watered by a number of streams, in which the upper side is singularly deficient. In very ancient times the lower level was injured by excess of moisture, as it is at this day: and hence, perhaps, Argos, which lay on the western side, notwithstanding its advantageous position, and the strength of its citadel, flourished less, for a time, than Mycenæ and Tiryns, which were situate to the east, where the plain is now barren through drought.

A long valley, running southward to the sea, and the mountains which border it on three sides, composed the territory of Laconia. It is to the middle region, the heart of Laconia, that most of the ancient epithets and descriptions relating to the general character of the country properly apply. The vale of Sparta is Homer’s “hollow Lacedæmon,” which Euripides further described as girt with mountains, rugged, and difficult of entrance for a hostile power. The epithet “hollow” fitly represents the aspect of a valley enclosed by the lofty cliffs in which the mountains here abruptly terminate on each side of the Eurotas. The character which the poet ascribes to Laconia,—that it is a country difficult of access to an enemy,—is one which most properly belongs to it, and is of great historical importance. On the northern and the eastern sides there are only two natural passes by which the plain of Sparta can be invaded.

At the northern foot of the Taygetus Mountains begins the Messenian plain, which, like the basin of the Eurotas below Sparta, is divided into two distinct districts, by a ridge which crosses nearly its whole width from the eastern side. The upper of these districts, which is separated from Arcadia by a part of the Lycæan chain, and is bounded towards the west by the ridge of Ithome, the scene of ever memorable struggles, was the plain of Stenyclarus, a tract not peculiarly rich, but very important for the protection and command of the country, as the principal passes, not only from the north, but from the east and west fall into it. The lower part of the Messenian plain, which spreads round the head of the gulf, was a region celebrated in poetry and history for its exuberant fertility; sometimes designated by the title of Macaria, or the Blessed, watered by many streams, among the rest by the clear and full Pamisus. It was, no doubt, of this delightful vale, that Euripides meant to be understood, when, contrasting Messenia with Laconia, he described the excellence of the Messenian soil as too great for words to reach.

The rich pastures on the banks of the Elean Peneus were celebrated in the earliest legends; and an ancient channel, which is still seen stretching across them to the sea, may be the same into which Hercules was believed to have turned the river, to cleanse the stable of Augeas.

When the necessary deduction has been made for the inequalities of its surface, Greece may perhaps be properly considered as a land, on the whole, not less rich than beautiful. And it probably had a better claim to this character in the days of its youthful freshness and vigour. Its productions were various as its aspect: and if other regions were more fertile in grain, and more favourable to the cultivation of the vine, few surpassed it in the growth of the olive, and of other valuable fruits. Its hills afforded abundant pastures: its waters and forests teemed with life. In the precious metals it was perhaps fortunately poor; the silver mines of Laurium were a singular exception; but the Peloponnesian Mountains, especially in Laconia and Argolis, as well as those of Eubœa, contained rich veins of iron and copper, as well as precious quarries. The marble of Pentelicus was nearly equalled in fineness by that of the isle of Paros, and that of Carystus in Eubœa. The Grecian woods still excite the admiration of travellers, as they did in the days of Pausanias,h by trees of extraordinary size. Even the hills of Attica are said to have been once clothed with forests; and the present scantiness of its streams may be owed in a great measure to the loss of the shade which once sheltered them. Herodotusi observes, that, of all countries in the world, Greece enjoyed the most happily tempered seasons. But it seems difficult to speak generally of the climate of a country, in which each district has its own, determined by an infinite variety of local circumstances. Both in northern Greece and the Peloponnesus the snow remains long on the higher ridges; and even in Attica the winters are often severe. On the other hand, the heat of the summer is tempered, in exposed situations, by the strong breezes from the northwest (the etesian winds), which prevail during that season in the Grecian seas; and it is possible that Herodotus may have had their refreshing influence chiefly in view.

Though no traces of volcanic eruptions appear to have been discovered in Greece, history is full of the effects produced there by volcanic agency; and permanent indications of its physical character were scattered over its surface, in the hot springs of Thermopylæ, Trœzen, Ædepsus, and other places. The sea between the Peloponnesus and Crete has been, down to modern times, the scene of surprising changes wrought by the same forces; and not long before the Christian era, a new hill was thrown up on the coast near Trœzen, no less suddenly than the islands near Thera were raised out of the sea. Earthquakes, accompanied by the rending of mountains, the sinking of land into the sea, by temporary inundations, and other disasters, have in all ages been familiar to Greece, more especially to the Peloponnesus. And hence some attention seems to be due to the numerous legends and traditions which describe convulsions of the same kind as occurring still more frequently, and with still more important consequences, in a period preceding connected history; and which may be thought to point to a state of elemental warfare, which must have subsided before the region which was its theatre could have been fitted for the habitation of man. Such an origin we might be inclined to assign to that class of legends which related to struggles between Poseidon and other deities for the possession of several districts; as his contests with Athene (Minerva) for Athens and Trœzen; with the same goddess, or with Hera (Juno) for Argos—where he was said, according to one account, to have dried up the springs, and according to another, to have laid the plain under water; with Apollo for the isthmus of Corinth.b