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Mixed, and National Arms THE SECOND sort of unprofitable arms are auxiliaries, by whom I mean, troops brought to help and protect you by a potentate whom you summon to your aid; as when in recent times, Pope Julius II observing the pitiful behaviour of his mercenaries at the enterprise of Ferrara, betook himself to auxiliaries, and arranged with Ferdinand of Spain to be supplied with horse and foot soldiers. 1 Auxiliaries may be excellent and useful soldiers for themselves, but are always hurtful to him who calls them in; for if they are defeated, he is undone, if victorious, he becomes their prisoner. Ancient histories abound with instances of this, but I shall not pass from the example of Pope Julius, which is still fresh in mens minds. It was the height of rashness for him, in his eagerness to gain Ferrara, to throw himself without reserve into the arms of a stranger. Nevertheless, his good fortune came to his rescue, and he had not to reap the fruits of his ill-considered conduct. For after his auxiliaries were defeated at Ravenna, the Swiss suddenly descended and, to their own surprise and that of every one else, swept the victors out of the country, so that, he neither remained a prisoner with his enemies, they being put to flight, nor with his auxiliaries, because victory was won by other arms than theirs. The Florentines, being wholly without soldiers of their own, brought ten thousand French men-at-arms to the siege of Pisa, thereby incurring greater peril than at any previous time of trouble. To protect himself from his neighbours, the Emperor of Constantinople summoned ten thousand Turkish soldiers into Greece, who, when the war was over, refused to leave, and this was the beginning of the servitude of Greece to the Infidel. 2 Let him, therefore, who would deprive himself of every chance of success, have recourse to auxiliaries, these being far more dangerous than mercenary arms, bringing ruin with them ready made. For they are united, and wholly under the control of their own officers; whereas, before mercenaries, even after gaining a victory, can do you hurt, longer time and better opportunities are needed; because, as they are made up of separate companies, raised and paid by you, he whom you place in command cannot at once acquire such authority over them as will be injurious to you. In short, with mercenaries your greatest danger is from their inertness and cowardice, with auxiliaries from their valour. Wise Princes, therefore, have always eschewed these arms, and trusted rather to their own, and have preferred defeat with the latter to victory with the former, counting that as no true victory which is gained by foreign aid. 3 I shall never hesitate to cite the example of Cesare Borgia and his actions. He entered Romagna with a force of auxiliaries, all of them French men-at-arms, with whom he took Imola and Forli. But it appearing to him afterwards that these troops were not to be trusted, he had recourse to mercenaries from whom he thought there would be less danger, and took the Orsini and Vitelli into his pay. But finding these likewise while under his command to be fickle, false, and treacherous, he got rid of them, and fell back on troops of his own raising. And we may readily discern the difference between these various kinds of arms, by observing the different degrees of reputation in which the Duke stood while he depended upon the French alone, when he took the Orsini and Vitelli into his pay, and when he fell back on his own troops and his own resources; for we find his reputation always increasing, and that he was never so well thought of as when every one perceived him to be sole master of his own forces. 4 I am unwilling to leave these examples, drawn from what has taken place in Italy and in recent times; and yet I must not omit to notice the case of Hiero of Syracuse, who is one of those whom I have already named. He, as I have before related, being made captain of their armies by the Syracusans, saw at once that a force of mercenary soldiers, supplied by men resembling our Italian condottieri, was not serviceable; and as he would not retain and could not disband them, he caused them all to be cut to pieces, and afterwards made war with native soldiers only, without other aid. 5 And here I would call to mind a passage in the Old Testament as bearing on this point. When David offered himself to Saul to go forth and fight Goliath the Philistine champion, Saul to encourage him armed him with his own armour, which David, so soon as he had put it on, rejected, saying that with these untried arms he could not prevail, and that he chose rather to meet his enemy with only his sling and his sword. In a word, the armour of others is too wide, or too strait for us; it falls off us, or it weighs us down. 6 Charles VII, the father of Louis XI, who by his good fortune and valour freed France from the English, saw this necessity of strengthening himself with a national army, and drew up ordinances regulating the service both of men-at-arms and of foot soldiers throughout his kingdom. But afterwards his son, King Louis, did away with the national infantry, and began to hire Swiss mercenaries. Which blunder having been followed by subsequent Princes, has been the cause, as the result shows, of the dangers into which the kingdom of France has fallen; for, by enhancing the reputation of the Swiss, the whole of the national troops of France have been deteriorated. For from their infantry being done away with, their men-at-arms are made wholly dependent on foreign assistance, and being accustomed to co-operate with the Swiss, have grown to think they can do nothing without them. Hence the French are no match for the Swiss, and without them cannot succeed against others. 7 The armies of France, then, are mixed, being partly national and partly mercenary. Armies thus composed are far superior to mere mercenaries or mere auxiliaries, but far inferior to forces purely national. And this example is in itself conclusive, for the realm of France would be invincible if the military ordinances of Charles VII had been retained and extended. But from want of foresight men make changes which relishing well at first do not betray their hidden venom, as I have already observed respecting hectic fever. Nevertheless, the ruler is not truly wise who cannot discern evils before they develop themselves, and this is a faculty given to few. 8 If we look for the causes which first led to the overthrow of the Roman Empire, they will be found to have had their source in the employment of Gothic mercenaries, for from that hour the strength of the Romans began to wane and all the virtue which went from them passed to the Goths. And, to be brief, I say that without national arms no Princedom is safe, but on the contrary is wholly dependent on Fortune, being without the strength that could defend it in adversity. And it has always been the deliberate opinion of the wise, that nothing is so infirm and fleeting as a reputation for power not founded upon a national army, by which I mean one composed of subjects, citizens, and dependents, all others being mercenary or auxiliary. 9 The methods to be followed for organizing a national army may readily be ascertained, if the rules above laid down by me, and by which I abide, be well considered, and attention be given to the manner in which Philip, father of Alexander the Great, and many other Princes and Republics have armed and disposed their forces. 10 CONTENTS · BOOK CONTENTS · BIBLIOGRAPHIC RECORD PREVIOUSNEXT Search Amazon: Click here to shop the Bookstore.Welcome · Press
russia history
On adventure travel vacation Imperfection of adventure travel vacation Geological Record On adventure travel vacation Sudden Appearance of Groups of Allied Species in adventure travel vacation Lowest Known Fossiliferous Strata THERE is another and allied difficulty, which is much more serious. I allude to adventure travel vacation manner in which species belonging to several of adventure travel vacation main divisions of adventure travel vacation animal kingdom suddenly appear in adventure travel vacation lowest known fossiliferous rocks. Most of adventure travel vacation arguments which have convinced me that all adventure travel vacation existing species of adventure travel vacation same group are descended from a single progenitor, apply with equal force to adventure travel vacation earliest known species. For instance, it cannot be doubted that all adventure travel vacation Cambrian and Silurian trilobites are descended from some one crustacean, which must have lived long before adventure travel vacation Cambrian age, and which probably differed greatly from any known animal. Some of adventure travel vacation most ancient animals, as adventure travel vacation Nautilus, Lingula, &c., do not differ much from living species; and it cannot on our theory be supposed, that these old species were adventure travel vacation progenitors of all adventure travel vacation species belonging to adventure travel vacation same groups which have subsequently appeared, for they are not in any degree intermediate in character. 1 Consequently, if adventure travel vacation theory be true, it is indisputable that before adventure travel vacation lowest Cambrian stratum was deposited, long periods elapsed, as long as, or probably far longer than, adventure travel vacation whole interval from adventure travel vacation Cambrian age to adventure travel vacation present day; and that during these vast periods adventure travel vacation world swarmed with living creatures. Here we encounter a formidable objection; for it seems doubtful whether adventure travel vacation earth, in a fit state for adventure travel vacation habitation of living creatures, has lasted long enough. Sir W. Thompson concludes that adventure travel vacation consolidation of adventure travel vacation crust can hardly have occurred less than 20 or more than 400 million years ago, but probably not less than 98 or more than 200 million years. These very wide limits show how doubtful adventure travel vacation data are; and other elements may have hereafter to be introduced into adventure travel vacation problem. Mr. Croll estimates that about 60 million years have elapsed since adventure travel vacation Cambrian period, but this, judging from adventure travel vacation small amount of organic change since adventure travel vacation commencement of adventure travel vacation Glacial epoch, appears a very short time for adventure travel vacation many and great mutations of life, which have certainly occurred since adventure travel vacation Cambrian formation; and adventure travel vacation previous 140 million years can hardly be considered as sufficient for adventure travel vacation development of adventure travel vacation varied forms of life which already existed during adventure travel vacation Cambrian period. It is, however, probable, as Sir William Thompson insists, that adventure travel vacation world at a very early period was subjected to more rapid and violent changes in its physical conditions than those now occurring; and such changes would have tended to induce changes at a corresponding rate in adventure travel vacation organisms which then existed. 2 To adventure travel vacation question why we do not find rich fossiliferous deposits belonging to these assumed earliest periods prior to adventure travel vacation Cambrian system, I can give no satisfactory answer. Several eminent geologists, with Sir R. Murchison at their head, were until recently convinced that we beheld in adventure travel vacation organic remains of adventure travel vacation lowest Silurian stratum adventure travel vacation first dawn of life. Other highly competent judges, as Lyell and E. Forbes, have disputed this conclusion. We should not forget that only a small portion of adventure travel vacation world is known with accuracy. Not very long ago M. Barrande added another and lower stage, abounding with new and peculiar species, beneath adventure travel vacation then known Silurian system; and now, still lower down in adventure travel vacation Lower Cambrian formation, Mr. Hicks has found in South Wales beds rich in trilobites, and containing various molluscs and annelids. The presence of phosphatic nodules and bituminous matter, even in some of adventure travel vacation lowest azoic rocks, probably indicates life at these periods; and adventure travel vacation existence of adventure travel vacation Eozoön in adventure travel vacation Laurentian formation of Canada is generally admitted. There are three great series of strata beneath adventure travel vacation Silurian system in Canada, in adventure travel vacation lowest of which adventure travel vacation Eozoön is found. Sir W. Logan states that their united thickness may possibly far surpass that of all adventure travel vacation succeeding rocks, from adventure travel vacation base of adventure travel vacation palæozoic series to adventure travel vacation present time. We are thus carried back to a period so remote, that adventure travel vacation appearance of adventure travel vacation so-called primordial fauna (of Barrande) may by some be considered as a comparatively modern event. The Eozoon belongs to adventure travel vacation most lowly organised, of all classes of animals, but is highly organised for its class; it existed in countless numbers, and, as Dr. Dawson has remarked, certainly preyed on other minute organic beings, which must have lived in great numbers. Thus adventure travel vacation words, which I wrote in 1859, about adventure travel vacation existence of living beings long before adventure travel vacation Cambrian period, and which are almost adventure travel vacation same with those since used by Sir W. Logan, have proved true. Nevertheless, adventure travel vacation difficulty of assigning any good reason for adventure travel vacation absence of vast piles of strata rich in fossils beneath adventure travel vacation Cambrian system is very great. It does not seem probable that adventure travel vacation most ancient beds have been quite worn away by denudation, or that their fossils have been wholly obliterated by metamorphic action, for if this had been adventure travel vacation case we should have found only small remnants of adventure travel vacation formations next succeeding them in age, and these would always have existed in partially metamorphosed condition. But adventure travel vacation descriptions which we possess of adventure travel vacation Silurian deposits over immense territories in Russia and in North America, do not support adventure travel vacation view, that adventure travel vacation older a formation is, adventure travel vacation more invariably it has suffered extreme denudation and metamorphism. 3 The case at present must remain inexplicable; and may be truly urged as a valid argument against adventure travel vacation views here entertained. To show that it may hereafter receive some explanation, I will give adventure travel vacation following hypothesis. From adventure travel vacation nature of adventure travel vacation organic remains which do not appear to have inhabited profound depths, in adventure travel vacation several formations of Europe and of adventure travel vacation United States; and from adventure travel vacation amount of sediment, miles in thickness, of which adventure travel vacation formations are composed, we may infer that from first to last large islands or tracts of land, whence adventure travel vacation sediment was derived, occurred in adventure travel vacation neighbourhood of adventure travel vacation now existing continents of Europe and North America. This same view has since been maintained by Agassiz and others. But we do not know what was adventure travel vacation state of things in adventure travel vacation intervals between adventure travel vacation several successive formations; whether Europe and adventure travel vacation United States during these intervals existed as dry land, or as a submarine surface near land, on which sediment was not deposited, or as adventure travel vacation bed of anand unfathomable sea. 4 Looking to adventure travel vacation existing oceans, which are thrice as extensive as adventure travel vacation land, we see them studded with many islands; but hardly one truly oceanic island (with adventure travel vacation exception of New Zealand, if this can be called a truly oceanic island) is as yet known to afford even a remnant of any palæozoic or secondary formation. Hence we may perhaps infer, that during adventure travel vacation palæozoic and secondary periods, neither continents nor continental islands existed where our oceans now extend; for had they existed, palæozoic and secondary formations would in all probability have been accumulated from sediment derived from their wear and tear; and these would have been at least partially upheaved by adventure travel vacation oscillations of level, which must have intervened during these enormously long periods. If then we may infer anything from these facts, we may infer that, where our oceans now extend, oceans have extended from adventure travel vacation remotest period of which we have any record; and on adventure travel vacation other hand, that where continents now exist, large tracts of land have existed, subjected no doubt to great oscillations of level, since adventure travel vacation Cambrian period. The coloured map appended to my volume on coral reefs, led me to conclude that adventure travel vacation great oceans are still mainly areas of subsidence, adventure travel vacation great archipelagoes still areas of oscillations of level, and adventure travel vacation continents areas of elevation. But we have no reason to assume that things have thus remained from adventure travel vacation beginning of adventure travel vacation world. Our continents seem to have been formed by a preponderance, during many oscillations of level, of adventure travel vacation force of elevation; but may not adventure travel vacation areas of preponderant movement have changed in adventure travel vacation lapse of ages? At a period long antecedent to adventure travel vacation Cambrian epoch, continents may have existed where oceans are now spread out; and clear andoceans may have existed where our continents now stand. Nor should we be justified in assuming that if, for instance, adventure travel vacation bed of adventure travel vacation Pacific Ocean were now converted into a continent we should there find sedimentary formations in a recognisable condition older than adventure travel vacation Cambrian strata, supposing such to have been formerly deposited; for it might well happen that strata which had subsided some miles nearer to adventure travel vacation centre of adventure travel vacation earth, and which had been pressed on by an enormous weight of super-incumbent water, might have undergone far more metamorphic action than strata which have always remained nearer to adventure travel vacation surface. The immense areas in some parts of adventure travel vacation world, for instance in South America, of naked metamorphic rocks, which must have been heated under great pressure, have always seemed to me to require some special explanation; and we may perhaps believe that we see in these large areas, adventure travel vacation many formations long anterior to adventure travel vacation Cambrian epoch in a completely metamorphosed and denuded condition. 5 The several difficulties here discussed, namelythat, though we find in our geological formations many links between adventure travel vacation species which now exist and which formerly existed, we do not find infinitely numerous fine transitional forms closely joining them all together;the sudden manner in which several groups of species first appear in our European formations;the almost entire absence, as at present known, of formations rich in fossils beneath adventure travel vacation Cambrian strata,are all undoubtedly of adventure travel vacation most serious nature. We see this in adventure travel vacation fact that adventure travel vacation most eminent palæontologists, namely Cuvier, Agassiz, Barrande, Pictet, Falconer, E. Forbes, &c., and all our greatest
adventure travel vacation
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