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Books > Earth & environment > Earth sciences > Geology & the lithosphere > General
Lying off the south-western tip of Mull, the island of Iona has huge significance as the first important centre of Christianity in Scotland. But the Abbey itself is built upon rocks that tell of events of much greater antiquity: the Lewisian gneisses of western Iona are some of the oldest rocks in the world. Alan McKirdy explores the fascinating geology of the area - in particular the eruption of two major volcanoes around 60 million years ago whose magma chambers formed the spectacular hills and glens of the Ardnamurchan peninsula and Glen More on Mull; and the Ice Age, when glaciers ripped away much of the upper part of the two volcanoes and sandpapered the landscape to create the rounded contours we see today.
Natural Disasters, 12th edition focuses on explaining how the normal processes of Earth concentrate their energies and deal heavy blows to humans and their structures. Students have a natural curiosity about natural disasters and why they occur. This text explains why natural disasters occur by interweaving the themes of Energy sources, Plate tectonics, Climate change, Earth Processes, Geologic time, the complexities of multiple variables operating simultaneously throughout the text.
"Earthquakes and Coseismic Surface Faulting on the Iranian Plateau" is a comprehensive and well-illustrated multi-disciplinary research work that analyzes the human and physical aspects of the active faults and large-magnitude earthquakes since ancient times on the Iranian Plateau. The long-term historical, archaeological, and sociological record of earthquakes discussed here gives insight into earthquake magnitudes, recurrences, fault segmentation, clustering, and patterns of coseismic ruptures from prehistoric times to the present. The first part of the book examines oral traditions and literature of the region concerned with earthquakes, particularly in folklore, epic literature, and theology. The second part assesses dynamic phenomena associated with earthquakes, including active tectonics, archaeoseismicity, and coseismic surface faulting throughout the twentieth century. This work is a valuable technical survey and an essential
reference for understanding seismic hazard analysis and earthquake
risk minimization in earthquake-prone developing and developed
countries throughout the world.
In general, lives of noteworthy accomplishment are led by people with an obvious talent, or more than one. Occasionally, though, someone with no discernible gift whatsoever may distinguish him or herself with a remarkable life. Such cases invite the question of how? How did it happen? With age I have realised that mine is such a life, and, inevitably, I have asked that question. It may happen in cases like this that, as one searches for an answer, one looks for precedents: or even for gifts not inherent in oneself but from outside. I did neither: it came to me unbidden. As I sang, the lines in the hymn resonated so powerfully I could not get away from them: ‘As noiseless let Thy blessings fall as fell Thy manna down.’ That was it. Unobtrusively I had been blessed – again and again and again. A dozy, unsocialised child follows a boringly ordinary course through life until gradually things start to work out for him in increasingly extraordinary ways. The only prize I ever won at school was the Natural History Prize, no academic accolades or colours for any sport. I was rewarded for loving undemanding nature; almost a non-prize. Nearly fifty years later, in a small town I had never visited before I was introduced to the author of a slim volume on the geography of the area. “Not THE Nick Norman,” she asked. I might have blushed. In 1987, aged 42 I had married, and gone on to father two children, one now a top lawyer, the other on a similar trajectory in medicine. Having dreamt of being a farmer, I owned a farm in Franschhoek, which put me in about the most envied group of people in South Africa. After a successful career in mineral exploration in Africa and South America I turned my hand to writing about geology in a way accessible to lay readers. Three best-sellers followed. The Red Sea opened up and the River Jordan stopped flowing, for the Israelites to reach their land of milk and honey. In between, though, there were 40 years in the wilderness. This is my narrative. Yours will be different. Unpack it and you will find blessing after blessing. See how I found mine.
Written by highly qualified Argentine scientists and scholars, this
book focuses on the uninterrupted geological and paleontological
record of Patagonia and Tierra del Fuego since the Miocene-Pliocene
boundary to the arrival of man and modern times. This region is an
outstanding area for research, with significant interest at the
international level. It provides an updated overview of the
scientific work in all related fields with a strong paleoclimatic
approach. Patagonia has also been a sort of a "paleoclimatic
bridge" between the Antarctic Peninsula and the more northerly land
masses, since the final opening of the Drake Passage in the middle
Miocene. Timely and comprehensive, "The Late Cenozoic of Patagonia
and Tierra del Fuego" is the only monograph book written in
English.
Foraminiferal cultures now serve as tools for researching biological, environmental, and geological topics. However, the biological backgrounds, in particular the natural histories of foraminifera, largely remain unclear. It is also true that the different techniques used in different subdisciplines are a setback to fully understanding the subject. Taken together, these factors prevent progress in experimental approaches to foraminiferal studies. This book aims to share and exchange knowledge between researchers from different subdisciplines, and the book should interest not only foraminiferal researchers but also scientists who are working with marine organisms to explore questions in relation to biology, geology, and oceanography.
Terrestrial mass movements (i.e. cliff collapses, soil creeps,
mudflows, landslides etc.) are severe forms of natural disasters
mostly occurring in mountainous terrain, which is subjected to
specific geological, geomorphological and climatological
conditions, as well as to human activities. It is a challenging
task to accurately define the position, type and activity of mass
movements for the purpose of creating inventory records and
potential vulnerability maps. Remote sensing techniques, in
combination with Geographic Information System tools, allow
state-of-the-art investigation of the degree of potential mass
movements and modeling surface processes for hazard and risk
mapping. Similarly, through statistical prediction models, future
mass-movement-prone areas can be identified and damages can to a
certain extent be minimized. Issues of scale and selection of
morphological attributes for the scientific analysis of mass
movements call for new developments in data modeling and
spatio-temporal GIS analysis.
The author argues that, after five decades of debate about the interactive of solar wind with the magnetosphere, it is time to get back to basics. Starting with Newton's law, this book also examines Maxwell's equations and subsidiary equations such as continuity, constitutive relations and the Lorentz transformation; Helmholtz' theorem, and Poynting's theorem, among other methods for understanding this interaction.
This book is intended to be the most complete and up-to-date guide to the geology and fossils of the New Forest, providing a wealth of information of interest to both the amateur fossil collector and the professional geologist. It includes some 200 field photographs, palaeogeographic maps, digitised borehole/outcrop logs, and geological cross sections. Also included is a tour of the regional geological evolution of southern England since the Permian Period (-280 million years ago), based on deep boreholes and coastal exposures, including the world-famous Jurassic coast of Dorset and east Devon. The author discusses the petroleum geology of southern England and the New Forest and gives a detailed overview of the stratigraphy of the Hampshire Basin, followed by related aspects of economic geology within this area, including ironstones, freshwater aquifers, geothermal energy, sand, clay and peat resources. Finally, there is an up-to-date and complete account of the principal fossil localities, together with a comprehensive gallery of photographs with accompanying descriptions of the most abundant fossils within the New Forest National Park.
Coal and Peat Fires: A Global Perspective is a compelling collection of research conducted by scientists and engineers around the world. The first of four volumes in the collection, Coal - Geology and Combustion, features chapters that discuss the origin of coal and coal fires; mining and use of coal; combustion and coal petrology; environmental and health impacts of coal fires; combustion by-products; geochemical, geophysical, and engineering methodologies for studying coal fires; the control, extinguishment, and political implications of coal fires; and much more.
This thesis presents an impressive summary of the potential to use passive seismic methods to monitor the sequestration of anthropogenic CO2 in geologic reservoirs. It brings together innovative research in two distinct areas - seismology and geomechanics - and involves both data analysis and numerical modelling. The data come from the Weyburn-Midale project, which is currently the largest Carbon Capture and Storage (CCS) project in the world. James Verdon's results show how passive seismic monitoring can be used as an early warning system for fault reactivation and top seal failure, which may lead to the escape of CO2 at the surface.
This reference presents a comprehensive description of flow through porous media and solutions to pressure diffusion problems in homogenous, layered, and heterogeneous reservoirs. It covers the fundamentals of interpretation techniques for formation tester pressure gradients, and pretests, multiprobe and packer pressure transient tests, including derivative, convolution, and pressure-rate and pressure-pressure deconvolution. Emphasis is placed on the maximum likelihood method that enables one to estimate error variances in pressure data along with the unknown formation parameters. Serves as a training manual for geologists, petrophysicists, and
reservoir engineers on formation and pressure transient
testing
The female authors highlighted in this monograph represent a special breed of science writer, women who not only synthesized the science of their day (often drawing upon their own direct experience in the laboratory, field, classroom, and/or public lecture hall), but used their works to simultaneously educate, entertain, and, in many cases, evangelize. Women played a central role in the popularization of science in the 19th century, as penning such works (written for an audience of other women and children) was considered proper "women's work." Many of these writers excelled in a particular literary technique known as the "familiar format," in which science is described in the form of a conversation between characters, especially women and children. However, the biological sciences were considered more "feminine" than the natural sciences (such as astronomy and physics), hence the number of geological "conversations" was limited. This, in turn, makes the few that were completed all the more crucial to analyze. |
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