Genghis Khan and the Making of the Modern World - Jack Weatherford [17]
The story of the boy who was destined to become the world’s greatest conqueror began six decades before the Mongol conquest of Bukhara in one of the most remote places in the inner expanse of Eurasia, near the border of modern Mongolia and Siberia. According to legend, the Mongols originated in the mountain forest when Blue-Gray Wolf mated with Beautiful Red Doe on the shores of a great lake. Because the Mongols permanently closed this homeland to outsiders when Genghis Khan died, we have no historical descriptions of it. The names of its rivers and mountains are virtually unknown in the historical literature, and even modern maps give conflicting names to its features, in a great variety of spellings.
This territory of the Mongol clans occupied only a small part in the northeast of the country now known as Mongolia. Most of the country now spreads across a high plateau in north-central Asia, beyond the range of the Pacific Ocean’s moisture-bearing winds that water the lush coastal plains of Asia’s agricultural civilizations. By contrast, the winds that reach the Mongolian plateau mostly blow from the Arctic in the northwest. These winds release what little moisture they carry onto the northern mountains and leave the southern part of the country dry, a terrain known as govi, or to foreigners as the Gobi. Between the harsh Gobi and the moderately watered mountains to the north lie vast stretches of steppe that turn green in the summer if they get rain. It is along these steppes that the herders move in the summer, searching for grass.
Although reaching only about ten thousand feet above sea level, Mongolia’s Khentii Mountain Range consists of some of the oldest mountains on the planet. Unlike the jagged, youthful Himalayas, which can only be ascended with climbing gear, the ancient Khentii Mountains have been smoothed by millions of years of erosion so that, with only moderate difficulty, a horse and rider can reach all but a few of the peaks in summer. Marshes dot their sides; in the long winter, these freeze into a solid mass. The deeper indentations in the mountainsides collect snow and water that freeze into what looks like glaciers in the winter, but in the brief summer, they turn into beautiful lakes of cobalt blue. The spring thaw of ice and snow overflows the lakes and spills off the mountains to form a series of small rivers that flow out onto the steppe that in the best of summers shimmers with grass as green as emeralds, but in the worst of times can remain a burned brown for several consecutive years.
The rivers that flow out of the Khentii Mountains are small and remain frozen for much of the year—even in May, when the ice is usually thick enough to support a team of mounted horses and sometimes even a loaded jeep. The long, broad steppes that stretch out along these small rivers served as the highways for the Mongols toward the various regions of Eurasia. Spurs of this grassland reach west all the way into Hungary and Bulgaria in eastern Europe. To the east, they reach Manchuria and would touch the Pacific Ocean if not barred by a thin ridge of coastal mountains that cut off the Korean Peninsula. On the southern side of the Gobi, the grasslands slowly pick up again and join the heart of the Asian continent, connecting with the extensive agricultural plains of the Yellow River.
Despite the gentle roll of the landscape, the weather can be fierce, and changes abruptly. This is a land of marked extremes, where humans and their animals face constant challenges from the weather. The Mongols say that you can experience all four seasons in a single day in the Khentii. Even in May, a horse might sink into snowbanks so deep