"Kathleen O' Neal & Michael W. Gear - People 5 - People Of The Sea" - читать интересную книгу автора (O'Neal Kathleen)projects on which he had worked in California. Sierra Adare spent many
hours locating and ordering books and articles--not to mention running front-line defense in difficult times. Michael Seidman is never far from our thoughts. Linda Quinton, Ralph Arnote, Yolanda Rodriguez, John DelGaizo, Maria Melilli, Natalie Farsi, Rae Lindsay and Ellisa Mitchell deserve special thanks for their superb work on our behalf. And Harriet McDougal continues to be the heartbeat of this series. Her talent and caring oversight keep it, and us, going. Last, our readers should be aware that the opinions expressed by the characters in this book are not necessarily those of the authors! Foreword During the last Ice Age (the Pleistocene epoch), the Pacific coast, from Vancouver to Southern California, was a very different place than it is today. The Sierra Nevada mountain range in California underwent extensive glaciation. In the region between Lake Tahoe and Yosemite, an ice cap three thousand feet deep stretched eighty miles long and forty miles wide. The Merced drainage, the San Joaquin River drainage and the fields and glaciers. A coniferous forest of Douglas fir, cypress, giant redwoods and pines thrived along the coast--where now there is only chaparral. East of the Sierras, the glacial climate spawned enormous inland lakes. Honey Lake in California and Pyramid Lake in Nevada are tiny remnants of Lake Lahontan, which covered forty-three thousand square miles and was five hundred feet deep. Lake Bonneville, of which the Great Salt Lake is a vestige, was twice the size of Lake Lahontan. Because so much of the earth's water was tied up in glaciers and lakes, the world's sea levels dropped approximately two hundred and eighty feet. The Pacific shoreline extended ten to thirty miles farther west than at present. Familiar places such as San Francisco Bay did not exist. The Channel Islands, off the coast of Santa Barbara, were one long island, seventy-eight miles long by twenty miles wide, that stretched to within seven miles of the mainland. The great North American glaciers--the Cordilleran and Laurentide ice sheets, which covered most of Canada and scooped out the Great Lakes--began rapid melting about eighteen thousand years ago. But between ten and twelve thousand years ago, the Sierra Nevada mountains were locked in a glacial advance. Called the Tioga glaciation, it depressed sea surface temperatures, cooled the air |
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