Thomas Goebel – författare

Between 1898 and 1918, many American states introduced the initiative, referendum, and recall - known collectively as direct democracy. Most interpreters have seen the motives for these reform measures as purely political, but Thomas Goebel demonstrates that the call for direct democracy was deeply rooted in antimonopoly sentiment. Frustrated with the governmental corruption and favoritism that facilitated the rise of monopolies, advocates of direct democracy aimed to check the influence of legislative bodies and directly empower the people to pass laws and abolish trusts. But direct democracy failed to achieve its promises: corporations and trusts continued to flourish, voter turnout rates did not increase, and interest groups grew stronger. By the 1930s, it was clear that direct democracy favored large organizations with the financial and organizational resources to fund increasingly expensive campaigns. Recent years have witnessed a resurgence of direct democracy, particularly in California, where ballot questions and propositions have addressed such volatile issues as gay rights and affirmative action. In this context, Goebel's analysis of direct democracy's history, evolution, and ultimate unsuitability as a grassroots tool is particularly timely.

This is the first of two volumes devoted to earthquakes and multi-hazards around the Pacific Rim. The circum-Pacific seismic belt is home to roughly 80% of the world’s largest earthquakes, making it the ideal location for investigating earthquakes and related hazards such as tsunamis and landslides. Gathering 16 papers that cover a range of topics related to multi-hazards, the book is divided into three sections: earthquake physics, earthquake simulation and data assimilation, and multi-hazard assessment and earthquake forecasting models. The first section includes papers on laboratory-derived rheological parameters as well as seismic studies in the Gulf of California and China. In turn, the second section includes papers on improvements in earthquake simulators as well as the statistical methods used to evaluate their performance, automated methods for determining fault slip using near-field interferometric data, variabilities in earthquake stress drops in California, and the use of social media data to supplement physical sensor data when estimating local earthquake intensity. The final section includes a paper on probabilistic tsunami hazard assessment, several papers on time-dependent seismic hazard analysis around the Pacific Rim, and a paper on induced and triggered seismicity at the Geysers geothermal field in California. Rapid advances are being made in our understanding of multi-hazards, as well as the range of tools used to investigate them. This volume provides a representative cross-section of how state-of-the-art knowledge and tools are currently being applied to multi-hazards around the Pacific Rim. The material here should be of interest to scientists involved in all areas of multi-hazards, particularly seismic and tsunami hazards. In addition, it offers a valuable resource for students in the geosciences, covering a broad spectrum of topics related to hazard research.

In addition to laboratory rock friction experiments, the second section examines earthquake source models for the 2016 MW 6.6 Aketao earthquake in Eastern Pamir and two earthquakes in Eastern Taiwan, along with strong ground motion studies of the 2008 MW 7.9 Wenchuan, China earthquake.