Did the ground just shake? You're not just imagining it, it’s probably an earthquake! An earthquake is a natural phenomenon that cannot be predicted. No instrument can tell when and where an earthquake will happen. So instead of trying to guess, it’s better to be prepared. This book will detail what will happen when an Earthquake happens. Open this book today!
Did the ground just shake? You're not just imagining it, it's probably an earthquake! An earthquake is a natural phenomenon that cannot be predicted. No instrument can tell when and where an earthquake will happen. So instead of trying to guess, it's better to be prepared. This book will detail what will happen when an Earthquake happens. Open this book today!
This is the first book to really make sense of the dizzying array of information that has emerged in recent decades about earthquakes. Susan Hough, a research seismologist in one of North America's most active earthquake zones and an expert at communicating this complex science to the public, separates fact from fiction. She fills in many of the blanks that remained after plate tectonics theory, in the 1960s, first gave us a rough idea of just what earthquakes are about. How do earthquakes start? How do they stop? Do earthquakes occur at regular intervals on faults? If not, why not? Are earthquakes predictable? How hard will the ground shake following an earthquake of a given magnitude? How does one quantify future seismic hazard? As Hough recounts in brisk, jargon-free prose, improvements in earthquake recording capability in the 1960s and 1970s set the stage for a period of rapid development in earthquake science. Although some formidable enigmas have remained, much has been learned on critical issues such as earthquake prediction, seismic hazard assessment, and ground motion prediction. This book addresses those issues. Because earthquake science is so new, it has rarely been presented outside of technical journals that are all but opaque to nonspecialists. Earthshaking Science changes all this. It tackles the issues at the forefront of modern seismology in a way most readers can understand. In it, an expert conveys not only the facts, but the passion and excitement associated with research at the frontiers of this fascinating field. Hough proves, beyond a doubt, that this passion and excitement is more accessible than one might think.
The destructive force of earthquakes has stimulated human inquiry since ancient times, yet the scientific study of earthquakes is a surprisingly recent endeavor. Instrumental recordings of earthquakes were not made until the second half of the 19th century, and the primary mechanism for generating seismic waves was not identified until the beginning of the 20th century. From this recent start, a range of laboratory, field, and theoretical investigations have developed into a vigorous new discipline: the science of earthquakes. As a basic science, it provides a comprehensive understanding of earthquake behavior and related phenomena in the Earth and other terrestrial planets. As an applied science, it provides a knowledge base of great practical value for a global society whose infrastructure is built on the Earth's active crust. This book describes the growth and origins of earthquake science and identifies research and data collection efforts that will strengthen the scientific and social contributions of this exciting new discipline.
This is a discount Black and white version. Some images may be unclear, please see BCCampus website for the digital version.This book was born out of a 2014 meeting of earth science educators representing most of the universities and colleges in British Columbia, and nurtured by a widely shared frustration that many students are not thriving in courses because textbooks have become too expensive for them to buy. But the real inspiration comes from a fascination for the spectacular geology of western Canada and the many decades that the author spent exploring this region along with colleagues, students, family, and friends. My goal has been to provide an accessible and comprehensive guide to the important topics of geology, richly illustrated with examples from western Canada. Although this text is intended to complement a typical first-year course in physical geology, its contents could be applied to numerous other related courses.
At various times in a span of fifteen years, John McPhee made geological field surveys in the company of Eldridge Moores, a tectonicist at the University of California at Davis. The result of these trips is Assembling California, a cross-section in human and geologic time, from Donner Pass in the Sierra Nevada through the golden foothills of the Mother Lode and across the Great Central Valley to the wine country of the Coast Ranges, the rock of San Francisco, and the San Andreas family of faults. The two disparate time scales occasionally intersect—in the gold disruptions of the nineteenth century no less than in the earthquakes of the twentieth—and always with relevance to a newly understood geologic history in which half a dozen large and separate pieces of country are seen to have drifted in from far and near to coalesce as California. McPhee and Moores also journeyed to remote mountains of Arizona and to Cyprus and northern Greece, where rock of the deep-ocean floor has been transported into continental settings, as it has in California. Global in scope and a delight to read, Assembling California is a sweeping narrative of maps in motion, of evolving and dissolving lands.
On March 27, 1964, at 5-36 p.m., the biggest earthquake ever recorded in North America--and the second biggest ever in the world, measuring 9.2 on the Richter scale--struck Alaska, devastating coastal towns and villages and killing more than 130 people in what was then a relatively sparsely populated region. In a riveting tale about the almost unimaginable brute force of nature, New York Times science journalist Henry Fountain, in his first trade book, re-creates the lives of the villagers and townspeople living in Chenega, Anchorage, and Valdez; describes the sheer beauty of the geology of the region, with its towering peaks and 20-mile-long glaciers; and reveals the impact of the quake on the towns, the buildings, and the lives of the inhabitants. George Plafker, a geologist for the U.S. Geological Survey with years of experience scouring the Alaskan wilderness, is asked to investigate the Prince William Sound region in the aftermath of the quake, to better understand its origins. His work confirmed the then controversial theory of plate tectonics that explained how and why such deadly quakes occur, and how we can plan for the next one.
