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few days to a few centuries. If from living we turn to lifeless nature, we encounter again the evidence of brief continuance. The sea is unceasingly remoulding its shores; hard as they are, the mountains are constantly yielding to frost and to rain; here an extensive tract of country is elevated, there depressed. We fail to find any thing that is not undergoing change.

Then forms are in their nature transitory, law is everlasting. If from visible forms we turn to directing law how vast is the difference. We pass from the finite, the momentary, the incidental, the conditioned-to the illimitable, the eternal, the necessary, the unshackled.

assert the con

It is of law that I am to speak in this book. In a The object of world composed of vanishing forms I am to this book is to vindicate the imperishability, the majesty of trol of law in law, and to show how man proceeds, in his human affairs. social march, in obedience to it. I am to lead my reader, perhaps in a reluctant path, from the outward phantasmagorial illusions which surround us, and so ostentatiously obtrude themselves on our attention, to something that lies in silence and strength behind. I am to draw his thoughts from the tangible to the invisible, from the limited to the universal, from the changeable to the invariable, from the transitory to the eternal; from the expedients and volitions so largely amusing the life of man, to the predestined and resistless issuing from the fiat of God.

CHAPTER II.

OF EUROPE: ITS TOPOGRAPHY AND ETHNOLOGY.

ITS PRIMITIVE MODES OF THOUGHT. AND THEIR ROGRESSIVE VARIATIONS, MANIFESTED IN THE GREEK AGE OF CREDULITY.

Description of Europe: its Topo raph. Meteorolo y an secular Geological Movements. - Their Effect on its In a tants.

Its Ethnology determined through its ocabulor.es.

Comparative Theology of Greece; the Stage of Sorcery, the Anthropo entric Stage. - Becomes conne tel with false Geography and Astronomy.- Heaven, the Earth, the Under World Orig n. ont nous Variat on and I'rogress of Greek Theology.-It ntroduces Ionic Philosophy.

Decline of Greek Theology. o cas oned by the Advan e o G ogra hy and Philosophical rit cism. Se ess on of Poets, i h loso hers, istorians

-Abortive publ.c Attempts to sustain it.- Duration of its Decline. Its Fall.

EUROPE is geographically a peninsula, and historically a dependency of Asia.

It is constructed on the western third of a vast mountain axis, which reaches in a broken and Description of irregular course from the Sea of Japan to the Europe. Bay of Biscay. On the flanks of this range, peninsular slopes are directed toward the south, and extensive plateaus to the north. The culminating point in Europe is Mont Blanc, 16,000 feet above the level of the sea. The axis of elevation is not the axis of figure; the incline to the south is much shorter and steeper than that to the north. The boundless plains of Asia are prolonged through Germany and Holland. An army may pass from the Pacific to the Atlantic Ocean, a distance of more than six thousand miles, without encountering any elevation of more than a few hundred feet. The descent from Asia

The great path-zone.

into Europe is indicated in a general manner by the mean elevation of the two continents above the level of the sea; that for Asia being 1132 feet, that for Europe 671. Through the avenue thus open to them, the Oriental hordes have again and again precipitated themselves on the West. With an abundance of springs and head-waters, but without any stream capable of offering a serious obstacle, this tract has a temperature well suited to military movements. It coincides generally with the annual isothermal line of 50°, skirting the northern boundary beyond which the vine ceases to grow, and the limiting region beyond which the wild boar does not pass.

Exterior and

Constructed thus, Europe is not only easily accessible from Asia, a fact of no little moment in its interior acces- ancient history, but it is also singularly accessibility. sible interiorly, or from one of its parts to another. Still more, its sea-line is so broken, it has so many intrusive gulfs and bays, that, its surface considered, its maritime coast is greater than that of any other continent. In this respect it contrasts strikingly with Africa. Europe has one mile of coast-line for every 156 square miles of surface, Africa has only one for every 623. This extensive maritime contact adds, of course, greatly to its interior as well as exterior accessibility.

Distribution

The mean annual temperature of the European countries on the southern slope of the mountain axis is from 60' to 70° F., but of those to the north the heat gradually declines, until, at the extreme limit on the shores of Zembla, the ground is perpetually frozen. As on other parts of the globe, the climate does not correspond to the latitude, but is disturbed by several of heat in causes, among which may be distinguished the Europe. great Atlantic current -- the Gulf Stream coming from America-and the Sahara Desert. The latter gives to the south of Europe an unduly high heat, and the former to Ireland, England, and the entire west a genial temperature. Together they press into higher latitudes the annual isothermal lines. If in Europe there are no deserts, there are none of those impenetrable forests seen in tropical countries. From the westerly shores of

Portugal, France, and Ireland, the humidity diminishes as we pass to the east, and, indeed, if we advance into Asia, it disappears in the desert of Gobi. There are no vast homogeneous areas as in Asia, and therefore there is no widespread uniformity in the races of men.

But not only is the temperature of the European continent elevated by the Gulf Stream and the south-west wind, its luxuriance of vegetation depends on them; for luxuriance of vegetation is determined, among other things, by the supply of rain. A profusion of And the quanwater gives to South America its amazing forests; tity of rain. a want inflicts on Australia its shadeless trees, with their shrunken and pointed leaves. With the diminished moisture the green gardens of France are replaced in Gobi by ligneous plants covered with a gray down. Physical circumstances control the vegetable as well as the animal world.

The westerly regions of Europe, through the influence of the south-west wind, the Gulf Stream, and their mountain ranges, are supplied with abundant rains, and have a favourable mean annual temperature; but as we pass to the eastern confines the number of rainy days diminishes, the absolute annual quantity of rain and snow is less, and the mean annual temperature is lower. On the Atlantic face of the mountains of Norway it is perpetually raining: the annual depth of water is there 82 inches; but on the opposite side of those mountains is only 21 inches. For similar reasons, Ireland is moist and green, and in Cornwall the laurel and camellia will bear a winter exposure.

There are six maximum points of rain-Norway, Scot land, South-western Ireland and England, Portugal, North-eastern Spain, Lombardy. They respectively correspond to mountains. In general, the amount of rain diminishes from the equator toward the poles; but it is greatly controlled by the disturbing influence of elevated ridges, which in many instances far more than compensate for the effects of latitude. The Alps exercise an influence over the meteorology of all Europe.

Not only do mountains thus determine the absolute quantity of rain, they also affect the number of rainy days VOL. I.-3

in a year. The occurrence of a rainy season depends on the amount of moisture existing in the air; and hence its frequency is greater at the Atlantic sea-board than in the interior, where the wind arrives in a drier state, much of its moisture having been precipitated by the mountains The number forcing it to a great elevation. Thus, on the of rainy days; eastern coast of Ireland it rains 208 days in a year; in England, about 150; at Kazan, 90; and in Siberia only 60 days.

In

When the atmospheric temperature is sufficiently low, the condensed water descends under the form of snow. general, the annual depth of snow and the number of snowy days increase toward the north. In Rome the and of snowy snowy days are 14; in Venice, 5; in Paris, 12; days. in St. Petersburgh, 171. Whatever causes interfere with the distribution of heat must influence the precipitation of snow. among such are the Gulf Stream and local altitude. Hence, on the coast of Portugal, snow is of infrequent occurrence; in Lisbon it never snowed from 1806 to 1811.

Such facts teach us how many meteorological contrasts Europe presents, how many climates it contains. Necessarily it is full of modified men.

Vibrations of

If we examine the maps of monthly isothermals, we observe how strikingly those lines change, bethe other coming convex to the north as summer approaches, mal lines. and concave as winter. They by no means observe a parallelism to the mean, but change their flexures, assuming new sinuosities. In their absolute transfer they move with a variable velocity, and through spaces far from insignificant. The line of 50° F., which in January passes through Lisbon and the south of the Morea, in July has travelled to the north shore of Lapland, and incloses the White Sea. As in some grand musical instrument, the strings of which vibrate, the isothermal lines of Europe and Asia beat to and fro, but it takes a year for them to accomplish one pulsation.

All over the world physical circumstances control the human race. They make the Australian a savage; incapacitate the negro, who can never invent an alphabet or an arithmetic, and whose theology never passes beyond

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