Orson Card - 27 Short Stories

"I heard it," he said. She leaned closer to him, her voice a whisper. "Do you dream, these days?"

"Many dreams. But the only ones that come true are the ones I dream in daylight."

"Ah," she sighed. "My sleep is also silent." She seemed distant, sad, distracted. Sam also; then, as if by conscious decision, he brightened, smiled, spoke cheerfully. "I have grandchildren now."

"And a wife you love," she said, reflecting his brightening mood. "I have grandchildren, too." Then she became wistful again. "But no husband. Just memories of an angel."

"Will I see Quetzalcoatl?" "No," she said, very quickly. A decision she had long since made and would not reconsider. "It would not be good for you to meet face to face, or stand side by side. Quetzalcoatl also asks that in the next election, you refuse to be a candidate."

"Have I displeased him?" asked Sam.

"He asks this at my advice," she said. "It is better, now that his face will be seen in this land, that your face stay behind closed doors." Sam nodded. "Tell me," he said. "Does he look like the angel?" "He is as beautiful," she said. "But not as pure." They embraced each other and wept. Only for a moment. Then her men lifted her back

into her litter, and Sam returned with Carpenter to the helicopter. They never met again.

In retirement, I came to visit Sam, full of questions lingering from his meeting with Virgem America. "You knew each other," I insisted. "You had met before." He told me all this story then.

That was thirty years ago. She is dead now, he is dead, and I am old, my fingers slapping these keys with all the grace of wooden blocks. But I write this sitting in the shade of a tree on the brow of a hill, looking out across woodlands and orchards, fields and rivers and roads, where once the land was rock and grit and sagebrush. This is what America wanted, what it bent our lives to accomplish. Even if we took twisted roads and got lost or injured on the way, even if we came limping to this place, it is a good place, it is worth the journey, it is the promised, the promising land.

CardKemal Akyazi grew up within a few miles of the ruins of Troy; from his boyhood home above Kumkale he could see the waters of the Dardanelles, the narrow strait that connects the waters of the Black Sea with the Aegean. Many a war had been fought on both sides of that strait, one of which had produced the great epic of Homer's ILIAD

This pressure of history had a strange influence on Kemal as a child. He learned all the tales of the place, of course, but he also knew that the tales were Greek, and the place was of the Greek Aegean world. Kemal was a Turk; his own ancestors had not come to the Dardanelles until the fifteenth century. He felt that it was a powerful place, but it did not belong to him. So the ILIAD was not the story that spoke to Kemal's soul. Rather it was the story of Heinrich Schliemann, the German explorer who, in an era when Troy had been regarded as a mere legend, a myth, a fiction, had been sure not only that Troy was real but also where it was. Despite all scoffers, he mounted an expedition and found it and unburied it. The old stories turned out to be true

In his teens Kemal thought it was the greatest tragedy of his life that Pastwatch had to use machines to look through the the millennia of human history. There would be no more Schliemanns, studying and pondering and guessing until they found some artifact, some ruin of a long-lost city, some remnant of a legend made true again. Thus Kemal had no interest in joining Pastwatch. It was not history that he hungered for--it was exploration and discovery that he wanted, and what was the glory in finding the truth through a machine

So, after an abortive try at physics, he studied to become a meteorologist. At the age of eighteen, heavily immersed in the study of climate and weather, he touched again on the findings of Pastwatch. No longer did meteorologists have to depend on only a few centuries of weather measurements and fragmentary fossil evidence to determine long-range patterns. Now they had accurate accounts of storm patterns for millions of years. Indeed, in the earliest years of Pastwatch, the machinery had been so coarse that individual humans could not be seen. It was like time-lapse photography in which people don't remain in place long enough to be on more than a single frame of the film, making them invisible. So in those days Pastwatch recorded the weather of the past, erosion patterns, volcanic eruptions, ice ages, climatic shifts

All that data was the bedrock on which modern weather prediction and control rested. Meteorologists could see developing patterns and, without disrupting the overall pattern, could make tiny changes that prevented any one area from going completely rainless during a time of drought, or sunless during a wet growing season. They had taken the sharp edge off the relentless scythe of climate, and now the great project was to determine how they might make a more serious change, to bring a steady pattern of light rain to the desert regions of the world, to restore the prairies and savannahs that they once had been. That was the work that Kemal wanted to be a part of

Yet he could not bring himself out from the shadow of Troy, the memory of Schliemann. Even as he studied the climatic shifts involved with the waxing and waning of the ice ages, his mind contained fleeting images of lost civilizations, legendary places that waited for a Schliemann to uncover them

His project for his degree in meteorology was part of the effort to determine how the Red Sea might be exploited to develop dependable rains for either the Sudan or central Arabia; Kemal's immediate target was to study thedifference between weather patterns during the last ice age, when the Red Sea had all but disappeared, and the present, with the Red Sea at its fullest. Back and forth he went through the coarse old Pastwatch recordings, gathering data on sea level and on precipitation at selected points inland. The old TruSite I had been imprecise at best, but good enough for counting rainstorms

Time after time Kemal would cycle through the up-and-down fluctuations of the Red Sea, watching as the average sea level gradually rose toward the end of the Ice Age. He always stopped, of course, at the abrupt jump in sea level that marked the rejoining of the Red Sea and the Indian Ocean. After that, the Red Sea was useless for his purposes, since its sea level was tied to that of the great world ocean

But the echo of Schliemann inside Kemal's mind made him think: What a flood that must have been

What a flood. The Ice Age had locked up so much water in glaciers and ice sheets that the sea level of the whole world fell. It eventually reached a low enough point that land bridges arose out of the sea. In the north Pacific, the Bering land bridge allowed the ancestors of the Indies to cross on foot into their great empty homeland. Britain and Flanders were joined. The Dardanelles were closed and the Black Sea became a salty lake. The Persian Gulf disappeared and became a great plain cut by the Euphrates. And the Bab al Mandab, the strait at the mouth of the Red Sea, became a land bridge

But a land bridge is also a dam. As the world climate warmed and the glaciers began to release their pent-up water, the rains fell heavily everywhere; rivers swelled and the seas rose. The great south-flowing rivers of Europe, which had been mostly dry during the peak of glaciation, now were massive torrents. The Rhone, the Po, the Strimon, the Danube poured so much water into the Mediterranean and the Black Sea that their water level rose at about the same rate as that of the great world ocean

The Red Sea had no great rivers, however. It was a new sea, formed by rifting between the new Arabian plate and the African, which meant it had uplift ridges on both coasts. Many rivers and streams flowed from those ridges down into the Red Sea, but none of them carried much water compared to the rivers that drained vast basins and carried the melt-off of the glaciers of the north. So, while the Red Sea gradually rose during this time, it lagged far, far behind the great world ocean. Its water level responded to the immediate local weather patterns rather than to worldwide weather