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Paleoseismology
Paleoseismology has become an important component of seismic risk analysis, which is mandated for nuclear power plants, dams, waste repositories, and other critical structures. This book is the first in the English language to be devoted solely to paleoseismology. It summarizes the development of the field from the 1960s to the present, encompassing material that is currently widely dispersed in journal articles. Includes a comprehensive review of the techniques currently used in paleoseismology Emphasizes practical methods of data collection and field studies Covers interpretation of field data based on current theory concerning fault segmentation and recurrence cycles Contains more than 170 line drawings and 50 photographs of paleoseismic phenomena
McAlpin(e) Genealogies, 1730-1990
The McAlpin family descends from the royalty of Scotland through Kenneth MacAlpin who united Celtic Scotland. One of his descendants was Alexander McAlpin, Sr. (ca. 1720's-1790) was born in Scotland and immigrated to America in the 1740s. He settled in South Carolina and eventually served in the American army during the revolution. After the war he settled in Wilkes County, Georgia where he died in 1790. He was married two to three times and was the father of twelve children. His many descendants live throughout the United States.
Consensus Preferred Recurrence-interval and Vertical Slip-rate Estimates
This report presents the results of the Utah Quaternary Fault Parameters Working Group (hereafter referred to as the Working Group) review and evaluation of Utah’s Quaternary fault paleoseismic-trenching data. The purpose of the review was to (1) critically evaluate the accuracy and completeness of the paleoseismictrenching data, particularly regarding earthquake timing and displacement, (2) where the data permit, assign consensus, preferred recurrence-interval (RI) and vertical slip-rate (VSR) estimates with appropriate confidence limits to the faults/fault sections under review, and (3) identify critical gaps in the paleoseismic data and recommend where and what kinds of additional paleo...
Post-Provo Paleoearthquake Chronology of the Brigham City Segment, Wasatch Fault Zone, Utah
This Utah Geological Survey Miscellaneous Publication, Post-Provo Paleoearthquake Chronology of the Brigham City Segment, Wasatch Fault Zone, Utah, is the eleventh report in the Paleoseismology of Utah series. This series makes the results of paleoseismic investigations in Utah available to geoscientists, engineers, planners, public officials, and the general public. These studies provide critical information on paleoearthquake parameters such as timing, recurrence, displacement, slip rate, and fault geometry which can be used to characterize potential seismic sources and evaluate the long-term seismic hazard presented by Utah’s Quaternary faults. This report presents the results of the mo...
Post-Bonneville Paleoearthquake Chronology of the Salt Lake City Segment, Wasatch Fault Zone, from the 1999 "Megatrench" Site
This report presents the results of a paleoseismic investigation designed to date a long series of consecutive earthquakes on the Wasatch fault zone and to measure the variability of recurrence times between the events. Geologists have long recognized that the comparatively short average recurrence interval (compared to most other basin-and-range normal faults) between large surface-faulting earthquakes on the Salt Lake City segment of the Wasatch fault zone during mid- to late-Holocene time is potentially anomalous, and possibly affected by the rise and fall of Lake Bonneville. This study extends the paleoearthquake record back to Bonneville time, nearly doubling the previous record, and provides new information on the timing and periodicity of surface faulting on the Salt Lake City segment from the latest Pleistocene through the Holocene. The trench and accompanying auger hole for this study exposed 26 meters of vertical section, roughly four times that of a typical paleoseismic trench on the Wasatch fault zone, hence the name “Megatrench.”
Tectonics
This book is devoted to different aspects of tectonic researches, especially to modern geodynamic processes. Syntheses of recent and earlier works, combined with new results and interpretations, are presented here for diverse tectonic settings. Most of chapters include up-to-date materials of detailed geological-geophysical investigations, which can help more clearly understand the essence of mechanisms of different tectonic processes. Among general problems of tectonics are discussed processes in axes of slow-spreading mid-ocean ridges on example of central part of Mid-Atlantic Ridge and in continental collision zones. Formation of sedimentary basins are considered on examples of Niger Delta, Triassic Cuyana Basin (Argentina), and Mesozoic and Cenozoic basins of the Alpine margin (Tunisia); neotectonic processes examined in Turkey and Morocco; tectonic evolution of the southern margin of Laurasia in the Paleozoic discussed as well as interrelation of western Troms-Lofoten and the Lewisian complexes in the Midle Paleoproterozoic.
Landforms of the Earth
This is a highly illustrated book with each landform being described with the following structure: (1) Main characteristics, including geometric, morphometric and sedimentological features. (2) Genetic processes and controlling factors. (3) Different typologies if applicable. (4) Additional comments related to various relevant aspects such us environmental implications or geographical distribution. Image visualization of landforms is essential for learning geomorphology and stimulating the interest in this field-based subject; a picture is worth a thousand words. Consequently, the book constitutes a valuable educational resource for every university student enrolled in courses related with earth surface processes and landforms (e.g. Geomorphology, Physical Geography, Geology, Geohazards, Environmental Sciences.). The book is also attractive to travellers and people keen on nature who want to know about the terminology and origin of the landforms they encounter in their trips. In many cases, the geomorphological features constitute the main asset of first-class protected areas (e.g., UNESCO World Heritage Sites, National Parks).
