Американские попаданцы и переносы - общая тема


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80-ый год? Победа нацистов? Нет пути!

Посмотрите на темп строительства американцами атомных бомб. И это в РИ, в мирное время.

Не позднее 55-го Третий Рейх можно будет переименовывать в Рейх Радиоактивный. Если они раньше не капитулируют.

Не зря Триша хотел запретить ядерки ;)))

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Ну, если исключить СССР, оно так и будет...

Ну да. Война на истощение (действительно, без ЯО, конечно)

Старый Мольтке, когда войны на истощение казались забытыми, предсказывал "новую 7-летнию и новую 30-ти летнюю войну".

"Новая 7-ми летняя" это ПМВ, конечно, хотя закончилась быстрее (но если ГВ в России считать и турок, то примерно так и выходит)

А "новая 30-летняя" - тут 2 варианта. Или ХВ (тут чуть больше получилось, от 35-ти до 40-ка лет)

Или - ПМВ и ВМВ считать вместе, как "немцы и часть центральной Европы против англо-французов, русских и американцев". Тут 31 год ровно

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Наши заклепщики такое любят.

449_300.jpg

полный размер:

449_original.jpg

Это не то, что вы подумали, а вторжение на Землю Сатурно-Марсианского Альянса в XXI веке.

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Были и оптимисты.

Например, один автор в Astounding за 42 год спрашивает: "Сможет ли Япония уже в этом году уничтожить Гитлера?"

И продолжает: "Нет, я не имею в виду японский народ, японских лидеров или японскую военную мощь. Я имею в виду японскую землю в прямом смысле этого слова. В Японии началось извержение вулкана, которое может так засорить атмосферу, что о русской зиме 1941 года Гитлер будет вспоминать с теплотой. В этот раз нацисты вымерзнут окончательно!"

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Дык это самое... Если мороз будет такой сильный и устойчивый, что вермахт вымерзнет, то СССР тоже кранты наступят, да и северным штатам не поздоровится. Так что автор не знал об атмосферной циркуляции или был скрытым конфедератом. (Вариант: верил в сверхчеловеческую морозоустойчивость и неприхотливость русских и янки).

А вообще удивительно - это ж идея "ядерной зимы", практически. И где? В дешёвом журнальчике 1942 года.

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Самое высшее звание - лейтенант. Хайнлайна надо было пригласить

Зачем? Роберт Энсон уже к тому времени отставник, а Джон Кэмпбелл уже со всеми ими имет контракты в "Астаундинг": и с Азимовым, и дель Реем, и с Хайнлайном, и со Старджоном, ван Вогтом, а одновременно держит на поводке и Генри Каттнера, и Спрэга де Кампа, и Клиффорда нашего Саймака. Один одного краше! Вехи в НФ того времени намечал именно Астаундинг, а Эмейзинг сториз писали для широких масс. Рядовые, капралы, сержанты и лейтененты. Повторюсь: генералы все были у Кэмпбелла. :)

А вообще удивительно - это ж идея "ядерной зимы", практически. И где? В дешёвом журнальчике 1942 года.

Да, идея родилась раньше, чем о ней подумал даже Эйнштейн. :) Круто. Но Астаундинг времен Кэмпбелла - это почитай солидное издание. :) Это вам не Эмейзинг какой-то там. :)

А кстати, кто-то смотрел еще докарпентеровскую экранизацию "Кто ты?" (1951 года) под названием "The Thing From Another World"?

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кто-то смотрел еще докарпентеровскую экранизацию "Кто ты?" (1951

Видел как-то раз, у нас по кабелю часто классику показывают, иногда очень редкую. Но что-то не впечатлило, и в памяти не отложилось.

это ж идея "ядерной зимы", практически. И где?

Там много нам открытий чудных!

Вариант: верил в сверхчеловеческую морозоустойчивость и неприхотливость русских и янки).

Примерно так.

Поскольку статья совсем короткая, кидаю сюда целиком:

VULCAN: Ice King

By Malcolm Jameson

Vulcan, God of Fire and volcanoes, isn't the sort of being you'd ordinarily associate with the world's worst—and coldest—weather. But he's responsible—as Jameson shows!

Illustrated by Fax

It would be the height of irony if this coming winter Japan should annihilate Hitler and Nazi-dom. If it is done—and it may very well be—it will be done without intention or malice; even unwittingly. For by Japan is meant Japan, not its rulers, its armed might, or its people, but the island of Honshu itself—an inanimate thing of rock and soil. Islands before this have wrecked empires, and there are signs now—summer, 1942—that it is about to be done again. Asamayama is reported to have erupted! Will Hitler, who but recently complained of the unfairness of last winter's cold, freeze outright next? He well may. That will depend upon the magnitude of Mount Asama's action—let us pray that the violence of its explosion was of the first order. For only that will freeze over the Baltic, exterminate the invaders of Russia, and reduce the fuel-impoverished inhabitants of Germany to shivering wretches whose only thought is to obtain warmth at any cost.

Extravagant? Fantastic? Not at all. We are too prone to think of volcanic catastrophes in terms of local disaster. While such explosions do wipe out entire populations and level cities to the ground, the aftermath of them is far more widespread than that. Eruptions of terrific violence—the kind that in the course of a few seconds vomit millions of cubic yards of stones, bombs and cinders into the high heavens—cause darkness to fall upon all the regions around, and thermometers to tumble the world over. The latter effect is, as often as not, the more serious, since it affects more people and is more persistent. The desolation wreaked in the immediate vicinity of the restless mountain may be done in a matter of hours, after which there is peace. The blizzards and gloom that are spread over all mankind may endure for months and years. It is those byproducts which we hope that Asama will endow us with in this particular year. For Asama is the king of ice makers. It is conceivable that a score of Asamas, erupting in stately rotation like the firing of the massive cylinders of a Gargantuan motor, could start another glacial age.

Possibly Asama first exerted itself in modern times in the year 1707. Of its identity there is no certainty, as Japan at that time was closed to all outsiders except a handful of Portuguese missionaries, but there is little doubt that an "unknown Japanese volcano" was the chief culprit responsible for the extraordinarily cold years 1708 and 1709. Two other volcanoes participated, Vesuvius and Santorin—on Thera, in the Aegean—but judging from Asama's subsequent performance later in the century, their role was probably a minor one. The results were these: following the triple eruptions of 1707 there was bitter cold all over Europe and in the colonies of North America for two years. The River Thames and the Adriatic froze; there was ten feet of snow in Spain and Portugal. Even the summer of 1709 was cold and rainy.

This was not a freak performance, though it is the first time that a Japanese volcano is mentioned in connection with European or American harsh winters. From the days of the destruction of Pompeii the literature of the times reveals that bitter weather usually followed in the wake of violent eruptions. Hecla, in Iceland, was an occasional offender, being charged with the cold winters of 1637 and 1694. 1695 was a bad year, too, with long and severe cold followed by a chilly summer, but that was due to the activity of an East Indian trio of craters—Celebes, Amboina, and Gunong Api. Europe's own Vesuvius went into eruption in December, 1631, almost equaling its performance in 79 A. D. It threw up dust clouds to the height of forty-eight kilometers, and the resultant murk brought intense cold in its train. The following year was marked by destructive snows, a short summer, and again early frosts and more snow. While it was yet early fall—October 4th—a detachment of soldiers froze to death between Montpellier and Baziers, which is in the south of France and close to the Mediterranean.*

(* The instances cited above and hereafter are selected from a table correlating volcanic activity with unusually severe winters in the chapters on "Vulcanism as a Factor in Climatic Control," "Physics of the Air," W. J. Humphreys, published by the Franklin Institute, 1920. The writer is deeply indebted to this work for what appears herein, and much else. It is highly recommended to anyone desiring a good grounding in its subject.)

From 1707 to 1783 there were several instances of volcanoes bringing snow and ice to the world, but it was not until the latter year that another really major eruption occurred. And that, when it did come, was the most frightful and devastating on record. When Asama exploded in 1783 the damage it did to Japan was vast, but it also spread intense cold and dimmed the skies over all the world. This state of affairs endured for three years, assisted no doubt by the concurrent explosion of Skaptar Jokull, in Iceland, and prolonged by one of Vesuvius in 1785.

Benjamin Franklin, in May, 1784, wrote:

During several of the summer months of the year 1783, when the effects of the Sun's rays to heat the Earth in these Northern regions should have been the greatest, there existed a constant fog over all Europe and a great part of North America. This fog was of a permanent nature ; it was dry, and the rays of the Sun seemed to have little effect toward dissipating it, as they easily do a moist fog arising from the water. They were indeed rendered so faint in passing through it that, when collected in the focus of a burning glass, they would scarce kindle brown paper. Of course, their summer effect in heating the Earth was exceedingly diminished.

Hence the surface was early frozen.

Hence the first snows remained on it unmelted, and received constant additions.

Hence perhaps the winter of 1783-4 was more severe than any that happened for many years.

The cause of this universal fog is not yet ascertained. Whether it was adventitious to this Earth, and merely a smoke ball proceeding from the consumption by fire of one of those great burning balls or globes which we happen to meet with in our course round the Sun, and which are sometimes seen to kindle and be destroyed in passing our atmosphere, and whose smoke might be attracted and retained by our Earth; or whether it was the vast quantity of smoke, long continuing to issue during the summer from Hecla, Iceland, and that other volcano which arose out of the sea near that island, which smoke might be spread by various winds over the northern part of the world, is yet uncertain.

It seems, however, worthy the inquiry, whether other hard winters, recorded in history, were preceded by similar permanent and widely extended summer fogs.

This excerpt has been quoted at length because it gives both a description of the effects of extreme volcanic action, whatever its point of origin, and hits closely at the explanation of them. Franklin was a shrewd and observant man, and the bulk of his surmises and speculations have since been confirmed by the findings of science. The fog he spoke of was Asama's volcanic dust, a potent obstacle to the Sun's rays.

As a virtually solo performance, the great blast of Asama of 1783 is supreme. For a full century no other single mountain approached in ferocity its outbreak of that date. Nevertheless, in the interim a very interesting phenomenon occurred —the coldest and most sustained period of misery in the annals of man. It was due, not to the terrific explosion of one virulent mountain, but to the activities of a group of them acting seriatim. This series of eruptions was initiated in the year 1812 —the one that ruined Napoleon—by Soufriere on St. Vincent. On April 30th, just when Bonaparte was about to launch his ill-fated attack on Russia, Soufriere—not to be confused with the mountain of the same name on neighboring St. Lucia, or Grand Soufriere on Guadaloupe—blew off. That it was bitterly cold in northern Europe during the winter that followed no one needs be told. Though Napoleon may have blundered, and granting that Kutusoff's Cossacks did their work well, adequate credit is due the smoky frost giant of the West Indies.

Soufriere's blowoff was only the beginning. Two years later mighty Mayon, one of the more murderous of Luzon's many explosive cones, thundered into eruption, so there was no relenting of the frigid weather. But worse was yet to come. On April 7, 1815, Tomboro let go with appalling violence, killing fifty-six thousand persons at one stroke. For three days darkness prevailed for three hundred miles around, so vast was the quantity of ash and dust heaved up by the mountain. And Tomboro, being situated on Sumbawa, which lies between Java and Timor and therefore in the midst of a hotbed of craters, jolted many of those into activity by its blast.

It is not to be wondered at, then, once the relation between Vulcan's fires and iciness is conceded, that the succeeding year should break all records for bleak chilliness. The period 1812-16 culminated in what is variously known as "the year without a summer" "poverty year" or, in the quaint American idiom of the day, "eighteen-hundred and froze-to-death." It was in that year of 1816 that snow lay unmelted throughout the summer in districts as far south as the Ohio, and when the current seasonal illness for August was frostbite, not sunstroke.

In the six decades subsequent to that pinching year there were nine other major eruptions, but none of sufficient violence to cause more than a single winter of undue inclemency. Their listing is omitted here for the sake of brevity, but the fact that each of them was trailed by much lower temperatures than was reasonable to expect adds to the already impressive accumulation of evidence of the linkage between vulcanism and cold. It was in 1883 that Asama's runner-up for the volcanic championship made its bid for fame. Krakatoa, between Java and Sumatra, tore itself asunder in a blast second only to that of the old master in 1873. Thousands of people were killed; titanic forces were unleashed. The mountain itself and the islet on which it stood disappeared, and tidal waves of such size and force as to be perceptible as far away as Cape Horn were set up. The amount of volcanic dust ejected was prodigious, and it is estimated that much of it was hurled to the incredible height of eighty kilometers.

A few months later an Alaskan volcano went into violent eruption, adding its not insignificant contribution to the dust of the stratosphere. For the next several years there was unseasonable cold and harsh winters, but by way of amelioration the Earth was treated to gorgeous sunsets everywhere, colored by the dusty atmosphere. Often by day the reddish-brown corona known as Bishop's ring could be seen surrounding the sun, which itself shone feebly as through a veil—corresponding to the phenomenon remarked upon by Franklin the year after Asama. And then, just as the dust clouds were about to settle, New Zealand's Tarawera, far in the south, belatedly exploded in 1886, prolonging the period. All the winters from 1883 to 1886 were severe, and old New Yorkers still speak with awe of the great blizzard of '88, though that may have been from other causes.

The great trio of ice giants—Asama, Krakatoa, and Tomboro—are aided and abetted by many lesser members of their tribe. Bogosiof and Awoe gave us the hard winters of 1890-91-92; Pelee, Santa Maria, and Colima, the ones of 1902-03. Greater than these was our own Alaskan Katmai, which erupted with immense violence in 1912, throwing out a vast amount of cinders and ash, and darkening and denuding the country for hundreds of miles around. It was on account of its action that the winter of 1912-13 was so biting. Heavy snows fell far south—in Texas, Mexico, and some in the desert States. That was the year that icicles hung from Los Angeles buildings, and the orange planters burned smudges in their groves night and day in the effort to save them. (Outraged Angelenos please consult the record before sitting down to write.)

There it is, a convincing list. Well, not quite. It also happens that there have been many severe winters preceded by no volcanic activity whatever. Also many volcanoes have erupted without appreciable effect on the weather except immediately and locally. The above list admittedly is one of selected coincidences, but with the difference that it is wonderfully consistent—there is a common denominator somewhere. And about forty years ago scientists set out to find out what it was.

Climate, as distinct from weather, is made up of a number of things. Roughly speaking. they may be divided into two classes, local factors, and general ones. The local factors are more apparent and more readily understood. Thus, the climate of Greenland differs from that of Sumatra chiefly because of difference in latitude; that of California from that of Nevada, though the States are sitting side by side, a difference due to the existence of a high mountain range between them, shutting the inner State off from the moist air of the sea. The altitude of Mexico City makes it cool, while Vera Cruz, nearby at sea level, has typical tropical climate. And so on.

The exterior factor affects them all together—cooling or heating more or less equally from pole to pole. That factor—I use the singular for convenience—is insolation—the measure of the intensity of solar radiation as received at the outer edge of the atmosphere. Insolation itself is affected by a number of factors, but the complexity of them is of scant interest to the majority of us who live down here on the surface of the Earth. It varies from time to time within a range of about ten percent due to diurnal irregularities and a number of cyclical ones. Solar activity, solar distance, perihelion phase—which has a period of about twenty-one thousand years—and other changes of far greater periods all enter. The only one we feel, as a rule, is the variation due to the sunspot cycle, which has a period of between ten and eleven years. For obscure reasons we receive less heat from the Sun when sunspots are most numerous than when they are few. Thus, in the main, every eleven years we should expect several winters in a row that are rather more severe than the average, followed by increasingly milder years, until we come to the middle of the cycle where we have fairly warm winters for a year or so. It is this feature that gives meaning to Humphreys' comparative table of eruptions and succeeding cold weather. The cold winters he lists as "discrepancies." That is, they came at a time in the sunspot cycle when they should normally be warm. And they were experienced all over the world; not locally from identifiable special conditions prevailing. Curves of pyrheliometric values kept since 1882 come down invariably when a big volcano goes into action. It was apparent that there must be a connection. What was it that volcanoes did to make things cold?

To take one last look at the general observational data before seeing what answer the physicists found, let's mention a few of the salient discrepancies noted. After Asama's great outbreak mean temperatures tumbled two degrees Centigrade. That may not seem much, but a two-degree drop in mean temperature, if prolonged indefinitely, would give rise to a mild glacial age, since it would lower the snow line about a thousand feet. This drop occurred in a year when there were very few sunspots—about twelve. In like manner, the year 1811 was one of minimum sunspots—the fewest ever observed, zero, to be exact, if I read the curve correctly. Yet Soufriere, despite the indications calling for an exceptionally mild winter, did what it did to the Grand Army of France. Tomboro, on the other hand, blew off at one of the sunspot peaks, when cold weather was to be expected, though the number of spots was low for a maximum, being but forty-five. The very exceptional sequel of "the year without a summer" could certainly not be attributed to such a few sunspots.*

(* Curiously enough, the only ''discrepancy" listed by Humphreys of opposite sign to the ones being discussed was the year 1778. which was inexplicably warm. That year the greatest number of sunspots ever observed were counted—one hundred and fifty! No volcanoes were involved. He is at a loss to account for the absence of icy weather unless the solar constant jumped unaccountably for a short time.)

The explanation of why volcanic eruptions impair the warmth of the Earth is simple—like all other scientific explanations, once a score or more of hard-working scientists have given years to piecing the jigsaw puzzle together for us and boiling the answer down to a phrase or so. It is the high-flung dust that does it, by reflecting and scattering the incoming solar radiation, while at the same time not barring the escape of terrestrial radiation of heat.

Thoughtful men from Franklin's time, or perhaps earlier, had noticed the connection and suggested the answer.. But the argument post hoc ergo propter hoc has never met with much respect in scientific circles. The scientists wanted to know, not what, but how and why. Mathematics had to back up empyrical knowledge. Their earlier attempts to find justification for the action of the dust as a filter of radiation produced a disappointing answer. Rock dust, they computed—for rock it must be—would absorb terrestrial radiation and reradiate it, thereby raising the mean temperature slightly rather than otherwise.

Later it was suggested that a lot might depend upon the size and shape of the rocky fragments. Ascertaining the size of particles of a cloud hanging fifty kilometers overhead would seem to be quite a chore, but Pernter tackled the job and gave us a formula for it. He approached it by starting with the Bishop's rings. Those are about ten degrees wide and have an outer radius of twenty-three degrees. From that and the known laws of diffraction of sunlight he arrived at something under two microns as the dimensions of the particles.

Since volcanic dust is known to be often in the form of thin-shelled bubbles, or fragments of such bubbles, both their tiny size and nature made them far more efficient reflectors and scatterers of the short-waved solar radiation than of the longer-waved terrestrial radiation, the ratio being thirty to one, about. The obvious result would be that so long as the veil of dust persisted, a fifth or more of incoming solar heat would be shut out while virtually none of the escaping Earth heat would be shut in—a sort of inverse hothouse effect. So long as that prevailed, the equilibrium of heat normally maintained between incoming and outgoing radiation would be upset and the Earth rapidly cooled.

But even high, wind-borne dust falls if given time. Other computations were made as to the rates of fall. The various factors are many, but the rough answer is that dust ejected far up into the stratosphere will require from one to three years to settle, depending upon its fineness and initial height. Some dust is as small as half a micron in diameter. So far, theory amply jibes with observed facts. Terrific eruptions do create cold. Perhaps, now that we have balloons capable of exploring the air, when next there is such an explosion more direct data can be gathered.

It is worth noting, also, that the dust is a better reflector of oblique rays than of those falling nearly normal, and, therefore, the chilling effect is the more pronounced in the higher altitudes, thus steepening the interzonal temperature gradients. This gives rise to gales, rains and snows which accelerate the cooling process in the middle latitudes. One is tempted to speculate on the effects of a long, continued series of scattered volcanic explosions, since the situation of the volcano has no bearing whatever on the consequences. They are world-wide in every case in which the dust reaches the stratosphere, where the high winds spread it evenly all over the world. Humphreys has computed that the mean temperature of the Earth has been a half of a degree © lower since 1750 than it would have been had there been no volcanic activity ; four or five times the amount of activity we have experienced could easily start another ice age. We should be thankful, therefore, that eruptions are as infrequent as they are.

By the same token, let's hope, for this year at least, that Asama will give us an encore to the performance of 1783. It will mean shoveling snow for us, shivering and ice-bound rivers, but I think we can take it. The Russians have proved they can; the Nazis have proved that they cannot. So up and at 'em, Asamayama, boy—do your stuff!

И аццкая иллюстрация:

post-23-0-94578500-1347963372_thumb.jpg

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Американский разведчик отправляется на смертельно опасное задание во вражескую Евразию. Задание выполнено. Чудом возвращается домой. А на родине ему и говорят:

- О чем это ты? Америка никогда не воевала с Евразией. Евразия всегда была другом Америки. ;)))

Эдмонд Гамильтон, "Голос завоевателя". 1939 год.

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А теперь немного старой доброй холодной войны.

fantastic_adventures_195203.jpg

Да, это он!

Повесть - полный вынос мозга. Написана по всем стандартам и канонам МТА.

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Летающие соусники как советское оружие - это круто... Маленькие зелёные коммунисты - ещё круче.

(Я в курсе, что такое saucer, если что).

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Товарищи, может ли коммунист быть зеленым? Диалектика учит нас, что...

Повесть начинается с того, что герой переходит границу оккупированной Польши и СССР!!!

Там есть тов.Сталин.

Там есть тов.Берия. Он не просто там есть - он один из главных героев, активно участвует в событиях и лично носится по крышам и подвалам!

Там есть подлые поляки, которые гадят и которые заплатят за свою подлость!

Там есть Валерия Ильинична, еще молодая, но уже мужененавистница и вождь анти-советской оппозиции.

Там есть тупые американцы. В смысле, все американские персонажи поголовно. К сожалению, в самом-самом конце вопреки всей логике они внезапно побеждают. Но мы простим автора - в противном случае рассказ бы не пропустила маккартистская цензура, а умные люди и так все поняли! ;)))

Там есть Красный Падаван. То есть Зеленый Марсианин.

Там есть супер-оружие, которое подарили тов.Сталину для убийства всех пиндосов.

Там даже заклепки и калибры есть. Их немного, но мы простим автора - у него не было под рукой википедии и сотни комментаторов в Самиздате, которые подсказывали ему, куда и что писать. У него даже Worda не было!!!

Клюквы на удивление мало. Очень-очень мало. Почти у всех русских персонажей нормальные русские имена.

Надо тщательно проверить биографию автора. Возможно, он и сам был попаданцем.

Кстати, никто не в курсе - автобус от Слуцка до Бобруйска в 1952-м действительно стоил 6 рублей 50 копеек? ;)))

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Там есть тов.Берия. Он не просто там есть - он один из главных героев, активно участвует в событиях и лично носится по крышам и подвалам!

В одном аглицком детективном рассказике 30 года ЧК возглавляет Азеф. Причем его никто не знает в лицо. Он мастер перевоплощения и лично проводит спецоперации за границей ;)

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Азеф не является МТА-стандартом. ;)

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Азеф не является МТА-стандартом

Все же надо скидку делать - в 30 м - Лаврентий тоже таким не являлся ;)

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Лерой Йеркса, "Пропавшие легионы Карфагена", 1943 г.

Вся армия Ганнибала, плюс Ганнибал собственной персоной, плюс слоны - переносится в Альпы 1943 года, где убивает стрелами, копьями и топтанием толпы нацистских альпийских стрелков. После коротких переговоров с союзниками Ганнибал твердо решает - "Мы на стороне угнетенных!" - и принимается топтать немцев с двойным энтузиазмом...

(В этом месте неумелые эпигоны делают себе харакири).

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(В этом месте неумелые эпигоны делают себе харакири).

О! Наоборот! Расово-чуждый семит сговаривается с наглыми наглосаксами против истинных арийцев (немного ошибающихся в методах). Поэтому армия Святослава, идущая на Болгарию внезапно попадает. И тут НАЧАЛОСЬ!

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Святослава не видел, врать не буду, но какая-то фэнтэзи про средневековую Русь там была. Оно и называлось соответственно - "Жрица летающего черепа".

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Вторая мировая продолжается до 1953, а то и до 1980 (!!!) года!

Оффтоп - а не было ли на форуме АИ с где мировые войны затянулись на десятилетия?

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а не было ли на форуме АИ с где мировые войны затянулись на десятилетия

Есть целая компьютерная игра про мир, где ПМВ длится до 1964 г. и не собирается прекращаться.

http://fai.org.ru/forum/index.php/topic/28641-iron-storm/

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Оффтоп - а не было ли на форуме АИ с где мировые войны затянулись на десятилетия?

Ну, это какбэ классика классик.

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про средневековую Русь там была. Оно и называлось соответственно - "Жрица летающего черепа".

Ошибочка вышла - это не средние века, это опять ВМВ. Очень дружелюбный, комплиментарный и русофильский роман. Единственный прокол - главную героиню зовут Ванья Нильченко.

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"Жрица летающего черепа".

Класс!!!

на картинке выше- какой однако монголоидный Сталин))

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Американский летчик и его товарищ из французской контрразведки преследуют в Северной Африке немецкого шпиона, который украл в Касабланке секретные планы союзников. Залетают втроем в какой-то мутный оазис, неотмеченный на картах, а там стегозавры, птеродактили, неандертальцы, фараоновские египтяне, древние греки, ассирийская армия Ашшурбанипала и пришельцы из Гипербореи 80-го века. 

 

Далеко не все доживут до рассвета. 

 

(С)  Эд Гамильтон, "Ничейная земля, ничейное время", 1943 г.  

 

 

 

 

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товарищ из французской контрразведки

Надеюсь, тема подсоединения телефонных проводов к определенным частям тела раскрыта? Французские контр-эспионаж это дело любили...

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Надеюсь, тема подсоединения телефонных проводов к определенным частям тела раскрыта?

Увы. Француз в рассказе - положительный персонаж, поэтому он никак не может опуститься до пыток. 

 

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