Sacramento Valley Symposium and Guidebook
Author | : Raymond V. Ingersoll |
Publisher | : |
Total Pages | : 232 |
Release | : 1990 |
Genre | : Science |
ISBN | : |
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Author | : Raymond V. Ingersoll |
Publisher | : |
Total Pages | : 232 |
Release | : 1990 |
Genre | : Science |
ISBN | : |
Author | : Eldridge M. Moores |
Publisher | : Geological Society of America |
Total Pages | : 507 |
Release | : 1999-01-01 |
Genre | : Science |
ISBN | : 0813723388 |
Author | : Donald R. Prothero |
Publisher | : CRC Press |
Total Pages | : 404 |
Release | : 2024-03-21 |
Genre | : Science |
ISBN | : 1003838065 |
California has some of the most distinctive and unique geology in the United States. It is the only state with all three types of plate boundaries, an extraordinary history of earthquakes and volcanoes, and many rocks and minerals found nowhere else. The Golden State includes both the highest and lowest points in the continental US and practically every conceivable geological feature known. This book discusses not only the important geologic features of each region in California but also the complex geologic four-dimensional puzzle of how California was assembled, beginning over two billion years ago. The author provides an up-to-date and authoritative review of the geology and geomorphology of each geologic province, as well as recent revelations of the tectonic history of California’s past. There are separate chapters on some of California’s distinctive geologic resources, including gold, oil, water, coastlines, and fossils. An introductory section describes basic rock and mineral types and fundamental aspects of plate tectonics, so that students and other readers can make sense of the bizarre, wild, and crazy jigsaw puzzle that is California's geological history. In this second edition, the book has an entirely new final section, “California’s Environmental Hazards and Challenges,” with new chapters on California’s landslides, air and water pollution, renewable energy, and the future of climate change in California. Key Features Thoroughly updates the market-leading textbook on California's geology Is written by an author with 30 years of teaching geology and leading field trips in California Introduces California's unique geological history Covers fundamentals of geology Characterizes specific geographical regions of California Describes major geological resources of California Summarizes the paleontology of California Reviews the likely impact of climate change on California's environment Related Titles Hollocher, K. A Pictorial Guide to Metamorphic Rocks in the Field (ISBN 978-11380-2630-8) Glavovic, B. et al. Climate Change and the Coast: Building Resilient Communities (ISBN 978-04154-6487-1)
Author | : Raymond V. Ingersoll |
Publisher | : Geological Society of America |
Total Pages | : 768 |
Release | : 2017-12-28 |
Genre | : Science |
ISBN | : 0813725402 |
Through a remarkable combination of intellect, self-confidence, engaging humility, and prodigious output of published work, William R. Dickinson influenced and challenged three generations of sedimentary geologists, igneous petrologists, tectonicists, sandstone petrologists, archaeologists, and other geoscientists. A key figure in the plate-tectonic revolution of the 1960s and 1970s, he explained how the distribution of sediments on Earth's surface could be traced to tectonic processes, and is widely recognized as a founder of modern sedimentary basin analysis. This volume consists of 31 chapters related to Dickinson's research interests; many of the authors are his former students, their students, and their students' students, demonstrating his continuing profound influence. The papers in this volume are an impressive tribute to the depth and breadth of Bill Dickinson's contributions to the geosciences.
Author | : Andrew Miall |
Publisher | : Elsevier |
Total Pages | : 626 |
Release | : 2008-12-03 |
Genre | : Science |
ISBN | : 0080929362 |
In recent years there have been rapid strides in our understanding of plate-tectonic processes, many developments in methods of basin analysis, and the accumulation of much new surface and subsurface geological and geophysical data. Projects such as COCORP (in the United States) and Lithoprobe (in Canada) have provided essential insights into the deep crustal structure of the continent. Synthesis of all the available information about North America's geological regions has not been attempted systematically since the "Decade of North American Geology project undertaken by the Geological Society of America and the Geological Survey of Canada nearly twenty years ago. The book commences with a summary of the Phanerozoic geological history of the United States and Canada, illustrated with a suite of new paleogeographic maps, and tying in each of the subsequent regional chapters by the inclusion of numerous cross-references. This followed by a set of fifteen regional syntheses of the principal tectonic regions of the United States and Canada, focusing on the stratigraphic and tectonic history of the major sedimentary basins. Most of these chapters have been contributed by specialists, drawing on their own research, and providing interpretive summaries of a type not previously attempted. - Up-to-date synthesis of the sedimentary/tectonic history of the major areas of the United States and Canada - Up-to-date references - Many new color maps
Author | : California. Division of Mines and Geology |
Publisher | : |
Total Pages | : 236 |
Release | : 2000 |
Genre | : Geology |
ISBN | : |
Author | : Stephan Alan Graham |
Publisher | : Pacific Section Society of Economic Paleontologists & Mineralogists |
Total Pages | : 76 |
Release | : 1993 |
Genre | : Science |
ISBN | : |
Author | : Colin F. Williams |
Publisher | : |
Total Pages | : 214 |
Release | : 1983 |
Genre | : Argillite |
ISBN | : |
Phosphatic concretions occur within diatomite in the upper part of the Miocene Monterey Formation near Lompoc, Calif. Absence of disruption of fine laminar bedding in the associated sediment by the concretions shows that they formed after complete compaction of the enclosing sediment.The concretions exhibit a strongly concentric color, chemical, and mineralogic zonation. Many of them are composed of a nucleus in which vivianite is the dominant mineral. Amorphous ferric phosphate, mitridatite, and francolite are the dominant phosphatic phases in successive layers toward the surface of the concretions. Cd and As contents increase tenfold from the nucleus outward, reaching a maximum of 2,000 ppm, whereas Ni content, with a maximum of 720 ppm, and Co content show the opposite trend. This mineralogy and elemental composition favor accretion under conditions of continuously increasing Eh and pH, during uplift into the fresh-ground-water zone of the terrestrial environment. Shale-normalized rare-earth-element patterns, however, suggest a marine source for the elements biogenic debris consisting of opal-A, organic matter, and carbonates of the enclosing sediment.