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Title: Cleopatra

Author: Jacob Abbott

Release Date: February 8, 2004 [eBook #10992] Most recently updated: July 11, 2012

Language: English

***START OF THE PROJECT GUTENBERG EBOOK CLEOPATRA***

E-text prepared by Ted Garvin, Terry Gilliland, and Project Gutenberg Distributed Proofreaders

Makers of History

CLEOPATRA BY JACOB ABBOTT

[Illustration: CLEOPATRA.]

PREFACE

Of all the beautiful women of history, none has left us such convincing proofs of her charms as Cleopatra, for the tide of Rome's destiny, and, therefore, that of the world, turned aside because of her beauty. Julius Caesar, whose legions trampled the conquered world from Canopus to the Thames, capitulated to her, and Mark Antony threw a fleet, an empire and his own honor to the winds to follow her to his destruction. Disarmed at last before the frigid Octavius, she found her peerless body measured by the cold eye of her captor only for the triumphal procession, and the friendly asp alone spared her Rome's crowning ignominy.

TABLE OF CONTENTS CHAPTER I. THE VALLEY OF THE NILE II. THE PTOLEMIES III. ALEXANDRIA IV. CLEOPATRA'S FATHER V. ACCESSION TO THE THRONE VI. CLEOPATRA AND CAESAR VII. THE ALEXANDRINE WAR VIII. CLEOPATRA A QUEEN IX. THE BATTLE OF PHILIPPI X. CLEOPATRA AND ANTONY XI. THE BATTLE OF ACTIUM XII. THE END OF CLEOPATRA ILLUSTRATIONS CLEOPATRA MEETING OF CLEOPATRA AND ANTONY CLEOPATRA TESTING THE POISON UPON THE SLAVES

[Illustration: Map—'Scene of CLEOPATRA'S HISTORY']

CHAPTER I. THE VALLEY OF THE NILE.

The parentage and birth of Cleopatra.—Cleopatra's residence in Egypt.—Physical aspect of Egypt.—The eagle's wings and science.—Physical peculiarities of Egypt connected with the laws of rain.—General laws of rain.—Causes which modify the quantity of rain.—Striking contrasts.—Rainless regions.—Great rainless region of Asia and Africa.—The Andes.—Map of the rainless region.—Valley of the Nile.—The Red Sea.—The oases.—Siweh.—Mountains of the Moon.—The River Nile.—Incessant rains.—Inundation of the Nile.—Course of the river.—Subsidence of the waters.—Luxuriant vegetation.—Absence of forests.—Great antiquity of Egypt.—Her monuments.—The Delta of the Nile.—The Delta as seen from the sea.—Pelusiac mouth of the Nile.—The Canopic mouth.—Ancient Egypt.—The Pyramids.—Conquests of the Persians and Macedonians.—The Ptolemies.—Founding of Alexandria.—The Pharos.

The story of Cleopatra is a story of crime. It is a narrative of the course and the consequences of unlawful love. In her strange and romantic history we see this passion portrayed with the most complete and graphic fidelity in all its influences and effects; its uncontrollable impulses, its intoxicating joys, its reckless and mad career, and the dreadful remorse and ultimate despair and ruin in which it always and inevitably ends.

Cleopatra was by birth an Egyptian; by ancestry and descent she was a Greek. Thus, while Alexandria and the Delta of the Nile formed the scene of the most important events and incidents of her history, it was the blood of Macedon which flowed in her veins. Her character and action are marked by the genius, the courage, the originality, and the impulsiveness pertaining to the stock from which she sprung. The events of her history, on the other hand, and the peculiar character of her adventures, her sufferings, and her sins, were determined by the circumstances with which she was surrounded, and the influences which were brought to bear upon her in the soft and voluptuous clime where the scenes of her early life were laid.

Egypt has always been considered as physically the most remarkable country on the globe. It is a long and narrow valley of verdure and fruitfulness, completely insulated from the rest of the habitable world. It is more completely insulated, in fact, than any literal island could be, inasmuch as deserts are more impassable than seas. The very existence of Egypt is a most extraordinary phenomenon. If we could but soar with the wings of an eagle into the air, and look down upon the scene, so as to observe the operation of that grand and yet simple process by which this long and wonderful valley, teeming so profusely with animal and vegetable life, has been formed, and is annually revivified and renewed, in the midst of surrounding wastes of silence, desolation, and death, we should gaze upon it with never-ceasing admiration and pleasure. We have not the wings of the eagle, but the generalizations of science furnish us with a sort of substitute for them.

The long series of patient, careful, and sagacious observations, which have been continued now for two thousand years, bring us results, by means of which, through our powers of mental conception, we may take a comprehensive survey of the whole scene, analogous, in some respects, to that which direct and actual vision would afford us, if we could look down upon it from the eagle's point of view. It is, however, somewhat humiliating to our pride of intellect to reflect that long-continued philosophical investigations and learned scientific research are, in such a case as this, after all, in some sense, only a sort of substitute for wings. A human mind connected with a pair of eagle's wings would have solved the mystery of Egypt in a week; whereas science, philosophy, and research, confined to the surface of the ground, have been occupied for twenty centuries in accomplishing the undertaking.

It is found at last that both the existence of Egypt itself, and its strange insulation in the midst of boundless tracts of dry and barren sand, depend upon certain remarkable results of the general laws of rain. The water which is taken up by the atmosphere from the surface of the sea and of the land by evaporation, falls again, under certain circumstances, in showers of rain, the frequency and copiousness of which vary very much in different portions of the earth. As a general principle, rains are much more frequent and abundant near the equator than in temperate climes, and they grow less and less so as we approach the poles. This might naturally have been expected; for, under the burning sun of the equator, the evaporation of water must necessarily go on with immensely greater rapidity than in the colder zones, and all the water which is taken up must, of course, again come down.

It is not, however, wholly by the latitude of the region in which the evaporation takes place that the quantity of rain which falls from the atmosphere is determined; for the condition on which the falling back, in rain, of the water which has been taken up by evaporation mainly depends, is the cooling of the atmospheric stratum which contains it; and this effect is produced in very various ways, and many different causes operate to modify it. Sometimes the stratum is cooled by being wafted over ranges of mountains, sometimes by encountering and becoming mingled with cooler currents of air; and sometimes, again, by being driven in winds toward a higher, and, consequently, cooler latitude. If, on the other hand, air moves from cold mountains toward warm and sunny plains, or from higher latitudes to lower, or if, among the various currents into which it falls, it becomes mixed with air warmer than itself, its capacity for containing vapor in solution is increased, and, consequently, instead of releasing its hold upon the waters which it has already in possession, it becomes thirsty for more. It moves over a country, under these circumstances, as a warm and drying wind. Under a reverse of circumstances it would have formed drifting mists, or, perhaps, even copious showers of rain.

It will be evident, from these considerations, that the frequency of the showers, and the quantity of the rain which will fall, in the various regions respectively which the surface of the earth presents, must depend on the combined influence of many causes, such as the warmth of the climate, the proximity and the direction of mountains and of seas, the character of the prevailing winds, and the reflecting qualities of the soil. These and other similar causes, it is found, do, in fact, produce a vast difference in the quantity of rain which falls in different regions. In the northern part of South America, where the land is bordered on every hand by vast tropical seas, which load the hot and thirsty air with vapor, and where the mighty Cordillera of the Andes rears its icy summits to chill and precipitate the vapors again, a quantity of rain amounting to more than ten feet in perpendicular height falls in a year. At St. Petersburg, on the other hand, the quantity thus falling in a year is but little more than one foot. The immense deluge which pours down from the clouds in South America would, if the water were to remain where it fell, wholly submerge and inundate the country. As it is, in flowing off through the valleys to the sea, the united torrents form the greatest river on the globe—the Amazon; and the vegetation, stimulated by the heat, and nourished by the abundant and incessant supplies of moisture, becomes so rank, and loads the earth with such an entangled and matted mass of trunks, and stems, and twining wreaths and vines, that man is almost excluded from the scene. The boundless forests become a vast and almost impenetrable jungle, abandoned to wild beasts, noxious reptiles, and huge and ferocious birds of prey.

Of course, the district of St. Petersburg, with its icy winter, its low and powerless sun, and its twelve inches of annual rain, must necessarily present, in all its phenomena of vegetable and animal life, a striking contrast to the exuberant prolificness of New Grenada. It is, however, after all, not absolutely the opposite extreme. There are certain regions on the surface of the earth that are actually rainless; and it is these which present us with the true and real contrast to the luxuriant vegetation and teeming life of the country of the Amazon. In these rainless regions all is necessarily silence, desolation, and death. No plant can grow; no animal can live. Man, too, is forever and hopelessly excluded. If the exuberant abundance of animal and vegetable life shut him out, in some measure, from regions which an excess of heat and moisture render too prolific, the total absence of them still more effectually forbids him a home in these. They become, therefore, vast wastes of dry and barren sands in which no root can find nourishment, and of dreary rocks to which not even a lichen can cling.

The most extensive and remarkable rainless region on the earth is a vast tract extending through the interior and northern part of Africa, and the southwestern part of Asia. The Red Sea penetrates into this tract from the south, and thus breaks the outline and continuity of its form, without, however, altering, or essentially modifying its character. It divides it, however, and to the different portions which this division forms, different names have been given. The Asiatic portion is called Arabia Deserta; the African tract has received the name of Sahara; while between these two, in the neighborhood of Egypt, the barren region is called simply the desert. The whole tract is marked, however, throughout, with one all-pervading character: the absence of vegetable, and, consequently, of animal life, on account of the absence of rain. The rising of a range of lofty mountains in the center of it, to produce a precipitation of moisture from the air, would probably transform the whole of the vast waste into as verdant, and fertile, and populous a region as any on the globe.

[Illustration: VALLEY OF THE NILE]

As it is, there are no such mountains. The whole tract is nearly level, and so little elevated above the sea, that, at the distance of many hundred miles in the interior, the land rises only to the height of a few hundred feet above the surface of the Mediterranean; whereas in New Grenada, at less than one hundred miles from the sea, the chain of the Andes rises to elevations of from ten to fifteen thousand feet. Such an ascent as that of a few hundred feet in hundreds of miles would be wholly imperceptible to any ordinary mode of observation; and the great rainless region, accordingly, of Africa and Asia is, as it appears to the traveler, one vast plain, a thousand miles wide and five thousand miles long, with only one considerable interruption to the dead monotony which