Publisher's Note: Products purchased from Third Party sellers are not guaranteed by the publisher for quality, authenticity, or access to any online entitlements included with the product. A compendium of knowledge and technology relating to scour processes in all earth materials Structures built in or near rivers and other channels can be vulnerable to scour around their foundations. If the depth of the scour becomes significant, the stability of the foundations may be endangered, with a consequent risk of damage or failure of the structure. There have been several bridge failures, resulting in transport disruption, economic loss and, on occasion, loss of life. The factors influencing scour are complex and vary according to the type of structure. Protection for preventing scour needs to be designed to withstand the flow forces imposed on them and have to be practical to build and install, while minimizing adverse environmental effects. This book covers the entire Scour Technology area and is prepared by one of the leading experts on the subject.

This encyclopedia, which constitutes a wide ranging and authoritative collection of academic articles, covers the sedimentological aspects of sediments and sedimentary rocks. As such the encyclopedia provides a comprehensive, one-volume reference work for students and faculty in universities, and for professionals in geology and allied disciplines (geography, engineering, environmental studies), as well as informed lay readers.

"Rivers and Floodplains" is concerned with the origin, geometry, water flow, sediment transport, erosion and deposition associated with modern alluvial rivers and floodplains, how they vary in time and space, and how this information is used to interpret deposits of ancient rivers and floodplains. There is specific reference to the types and lifestyles of organisms associated with fluvial environments, human interactions with rivers and floodplains, associated environmental and engineering concerns, as well as the economic aspects of fluvial deposits, particularly the modeling of fluvial hydrocarbon reservoirs and aquifers. Methods of studying rivers and floodplains and their deposits are also discussed. Although basic principles are emphasized, many examples are detailed.

Particular emphasis is placed on how an understanding of the nature of modern rivers and floodplains is required before any problems concerning rivers and floodplains, past or present, can be addressed rationally.

"Rivers and Floodplains" is designed as a core text for senior undergraduate and graduate students studying modern or ancient fluvial environments, particularly in earth sciences, environmental sciences and physical geography, but also in civil and agricultural engineering. College teachers, researchers, and practising professionals will also find the book an invaluable reference.
Presents a process-based approach, which is relevant to modern curricula.
Discusses methods of studying rivers and floodplains and their deposits.
Provides many detailed examples throughout the text.
Emphasises the basic principles of this subject.
As the first synthesis of this entire field, it will be a must-have for all students studying modern or ancient fluvial environments.
Teachers, researchers and practising professionals will find this an invaluable reference tool.

"Rivers and Floodplains" will also be of interest to geologists, geographers and engineers.

The last decade has been a period of rapid advances in glacier hydrology and hydrochemistry. These have resulted from the application of new technologies to the direct observation of englacial and subglacial drainage systems via boreholes, from theoretical advances and from increased interactions between fieldworkers and modellers. This collection of papers captures the spirit of these advances highlighting new methodologies, the change in character of hydrological models from lumped conceptual models to physically based, distributed models, and the changing role of field studies in glacier hydrological investigations. Major themes identified in the book are: approaches to defining the structure of drainage systems in cold and temperate glaciers; investigations of the linkages between surface and subsurface components of these systems, and of hydraulic interactions between different elements of subglacial systems; seasonal changes in drainage system properties at local and glacier wide scales; controls on meltwater quality; the integration of field and modelling studies; and problems of scaling up results from studies of valley glaciers to the ice sheet scale.

Students taking undergraduate degrees in geography, ecology, earth science, and environmental science frequently take an introductory unit in Physical Geography. Some will have not done any geography since their early teens, while others have more recent knowledge. This range of backgrounds can be challenging for both the instructor and the student, this primer aims to help. A primer is a readable introduction to a subject, more technical than a piece of popular science, but less detailed than a specialist textbook. It aims to give the reader a platform in a subject with which they may be unfamiliar, so that they can proceed simultaneously, or sequentially, to more advanced texts and information. Ideally the primer should have something for those without any knowledge, while also challenge and entertaining those who do. Not quite bedtime reading, but a step in that direction. Our Dynamic Earth introduces students to the Earth's origins, to plate tectonics, atmospheric and oceanographic circulation, as well as to a range of Earth surface processes. Idea to get you started in your studies.

Geosequestration involves the deep geological storage of carbon dioxide from major industrial sources, providing a potential solution for reducing the rate of increase of atmospheric concentrations of carbon dioxide and mitigating climate change. This volume provides an overview of the major geophysical techniques and analysis methods for monitoring the movement and predictability of carbon dioxide plumes underground. Comprising chapters from eminent researchers, the book is illustrated with practical examples and case studies of active projects and government initiatives, and discusses their successes and remaining challenges. A key case study from Norway demonstrates how governments and other stake-holders could estimate storage capacity and design storage projects that meet the requirements of regulatory authorities. Presenting reasons for embracing geosequestration, technical best practice for carbon management, and outlooks for the future, this volume provides a key reference for academic researchers, industry practitioners and graduate students looking to gain insight into subsurface carbon management.

The ice mountains of the Karakoram are among the world's greatest natural treasures. At 8611 metres (28,251 ft), K2 is the second tallest mountain on Earth. There are three other mountains in the range that top 8000 metres (26,247 ft) - Gasherbrum I, Broad Peak and Gasherbrum II - and more than 60 peaks above 7000 metres (22,966 ft). Extending in a south-easterly direction from the north-eastern tip of Afghanistan and spanning the borders of Pakistan, India and China, the Karakoram is part of a complex of ranges in Central Asia that includes the Hindu Kush to the west and the Himalayas to the south-east. These mountains, however, are distinctive. This is the most glaciated region on the planet outside the Arctic and Antarctic. But while most of the world's great peaks are almost blanketed in snow and ice, the Karakoram is an exception: the mountains are so vertical that they rapidly shed snow, leaving their bold, jagged outlines of black granite glistening in the sun. The name of the range comes from the Turkic term for 'black rock' or 'black gravel'. The well-known landscape photographer Colin Prior was initially inspired to visit the Karakoram in his early twenties: in his local library he picked up the book In the Throne Room of the Mountain Gods (1977) by the American climber and photographer Galen Rowell, and was instantly captivated by images of the sharp, fractured peaks and vast glaciers. His first trip to the Karakoram came in the mid-1990s, and he has been passionate about these mountains ever since. Prior's new book is the result of six expeditions he has made to the Gilgit-Baltistan region of north-east Pakistan over the last six years. Because the region is so remote, there are no established base camps, and each expedition requires careful planning and miles of trekking with a large team of guides, porters and ponies to carry the equipment and provisions. There are regular rock falls and perilous snow-covered crevasses to contend with. The reward for Prior is what he calls the ultimate mountain landscape: 'The scenery is graphic, with towers, minarets and cathedrals of rock.' This beautifully produced volume showcases the breathtaking beauty of the Karakoram in some 130 duotone and colour photographs. The images are largely arranged to follow Prior's progress up the glaciers, and are accompanied by well-chosen quotations from accounts of historical expeditions to the region. A selection of 'making of' images at the end of the book highlights the challenges of documenting the most exceptional mountain range in the world.

Rock Weathering and Landform Evolution brings together a series of important studies on rock weathering by leading researchers, and illustrates the diversity of approaches and techniques that are currently being used by geomorphologists to study weathering processes and responses. The book commences with a number of research studies and review chapters on weathering processes and weathered products. This is followed by several discussions of the weathering of cut or dressed rock in urban and coastal environments. Contributors then examine the application of weathering and weathering rates to the dating of deposits or rock surfaces. The final section of the book comprises studies of the relationship between weathering and landforms in a variety of climatic environments. The contributions included in this book cover a wide range of topics and demonstrate the many advances that are being made by researchers investigating rock weathering. Some of the studies deal with state-of-the-art technology, others the very traditional geomorphological skills of observation and deductive reasoning, backed up as necessary by statistical analysis. This volume is the first collection of papers on weathering published for many years, and provides a wealth of information not just to geomorphologists but also to geologists, engineers, architects and archaeologists.

This book is in response to the growing demand from academics and the general public for state-of-the-art research in permafrost science and, in particular, information about its impacts on infrastructure and ecosystems. It brings together research from diverse but highly complementary scientific disciplines to illuminate the main physical, chemical and biological processes occurring in permafrost systems and identifies the possible mechanisms controlling fluxes of energy and matter at various scales. Taken together, the 8 chapters of this book provide a comprehensive, up-to-date description and analysis of the basic geomorphological, physical, hydrological, chemical and biological aspects of permafrost-affected ecosystems, their interaction with other components of the landscape and their impact on human life and infrastructure.

The Anthropocene is a major new concept in the Earth sciences and this book examines the effects on geomorphology within this period. Drawing examples from many different global environments, this comprehensive volume demonstrates that human impact on landforms and land-forming processes is profound, due to various driving forces, including: use of fire; extinction of fauna; development of agriculture, urbanisation, and globalisation; and new methods of harnessing energy. The book explores the ways in which future climate change due to anthropogenic causes may further magnify effects on geomorphology, with respect to future hazards such as floods and landslides, the state of the cryosphere, and sea level. The book concludes with a consideration of the ways in which landforms are now being managed and protected. Covering all major aspects of geomorphology, this book is ideal for undergraduate and graduate students studying geomorphology, environmental science and physical geography, and for all researchers of geomorphology.

Weathering is an important phenomenon of the geochemical cycle as it contributes to the relief formation. It corresponds to a general term applied to physical and chemical changes suffered by rocks as a consequence of their exposition to different conditions of humidity and temperature. In this book, the authors present topical research in the study of the types, processes and effects of weathering. Topics discussed include the use of weathering indices in rock research; geomorphic processes in the last glacial age; understanding chemical weathering in affecting the Earth's surface; weathering of dimensional granite stones used as cladding and the weathering process and desert pavement development.

In 1830-33, Charles Lyell laid the foundations of evolutionary biology with Principles of Geology, a pioneering book that Charles Darwin took with him on the Beagle. Volume 1 discusses the effects on the Earth's crust of climate change, running water, volcanic eruptions and earthquakes, and supports James Hutton's theory of uniformitarianism, now a guiding principle of geology. Volume 2 (1832) focuses on plants and animals, their distribution, diffusion, migrations and adaptation to changing habitats, and considers the theories of Lamarck, while Volume 3 periodises sedimentary and volcanic rock formations and considers the marine fossil record. The books are generously illustrated and thoroughly indexed. Lyell writes with infectious enthusiasm, conveying the excitement of his fieldwork and discoveries in this landmark book, which remains of interest to geologists and historians of science alike.

Sandstones form the backdrop to some of the world's most spectacular scenery, and are found all over the planet and in all climates. Following on from the authors' successful 1992 book, this is the only volume that considers sandstone landforms from a truly global perspective. It describes the wide variety of landforms that are found in sandstone, and discusses the role of lithological variation, chemical weathering and erosional processes in creating these features, with examples drawn from around the world. Climatic and tectonic constraints on the development of sandstone landscapes are also considered. This volume provides a comprehensive assessment of the literature from publications in a range of languages, and is illustrated with over 130 photographs of sandstone features from every continent. It presents a holistic account of sandstone terrain for researchers and graduate students in a variety of fields including geography, geomorphology, sedimentology and geomechanics.

Geomorphological landforms and processes exert a strong influence on surface engineering works, yet comparatively little systematic information on geomorphology is available to engineers. This book presents a worldwide view of geomorphology for engineers and other professionals on the near-surface engineering problems associated with the various landscapes. This new and completely revised edition has additional chapters with an improved format and is broadly divided into three parts.;The first part is concerned with the major factors which control the materials, form and processes on the Earth's surfaces. The second part deals with the geomorphological processes which help shape land surfaces and influence their engineering characteristics and the final part covers environments and landscapes, including some specialist chapters. Each chapter is written by leading authorities on the subject and is both self-contained and referenced with other chapters as appropriate to make a balanced whole.;Readership: practitioners and academics in civil, geotechnical, foundation engineering, soil and rock mechanics, and engineering geology.; Practitioners, postgraduate and advanced undergraduates

'Outstanding Academic Title' Choice, magazine of the Association of College & Research Libraries, American Library Association.Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision - where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin.The most obvious mountain belts today - the Himalayas, the Alps and the Andes, for example - are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion.The presently active mountain belts are arranged in three separate systems: the Alpine-Himalayan ranges, the circum-Pacific belt and the mid-ocean ridges. Much of the Alpine-Himalayan belt is relatively well known, but large parts of the circum-Pacific and ocean-ridge systems are not nearly as familiar, but contain equally impressive mountain ranges despite large parts being partly or wholly submerged.This book takes the reader along the active mountain systems explaining how plate tectonic processes have shaped them, then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It is aimed at those with an interest in mountains and in developing an understanding of the geological processes that create them.

Allow yourself to be taken back into deep geologic time when strange creatures roamed the Earth and Western North America looked completely unlike the modern landscape. Volcanic islands stretched from Mexico to Alaska, most of the Pacific Rim didn't exist yet, at least not as widespread dry land; terranes drifted from across the Pacific to dock on Western Americas' shores creating mountains and more volcanic activity. Landscapes were transposed north or south by thousands of kilometers along huge fault systems. Follow these events through paleogeographic maps that look like satellite views of ancient Earth. Accompanying text takes the reader into the science behind these maps and the geologic history that they portray. The maps and text unfold the complex geologic history of the region as never seen before. Winner of the 2021 John D. Haun Landmark Publication Award, AAPG-Rocky Mountain Section

Recent studies indicate that - due to climate change - the Earth is undergoing rapid changes in all cryospheric components, including polar sea ice shrinkage, mountain glacier recession, thawing permafrost, and diminishing snow cover. This book provides a comprehensive summary of all components of the Earth's cryosphere, reviewing their history, physical and chemical characteristics, geographical distributions, and projected future states. This new edition has been completely updated throughout, and provides state-of-the-art data from GlobSnow-2 CRYOSAT, ICESAT, and GRACE. It includes a comprehensive summary of cryospheric changes in land ice, permafrost, freshwater ice, sea ice, and ice sheets. It discusses the models developed to understand cryosphere processes and predict future changes, including those based on remote sensing, field campaigns, and long-term ground observations. Boasting an extensive bibliography, over 120 figures, and end-of-chapter review questions, it is an ideal resource for students and researchers of the cryosphere.

Computational models are invaluable in understanding the complex effects of physical processes and environmental factors which interact to influence landform evolution of geologic time scales. This book provides a holistic guide to the construction of numerical models to explain the co-evolution of landforms, soil, vegetation and tectonics, and describes how the geomorphology observable today has been formed. It explains the science of the physical processes and the mechanics of how to solve them, providing a useful resource for graduates studying geomorphology and sedimentary and erosion processes. It also emphasises the methods for assessing the relative importance of different factors at field sites, enabling researchers to select the appropriate processes to model. Integrating a discussion of the fundamental processes with mathematical formulations, it guides the reader in understanding which processes are important and why; and creates a framework through which to study the interaction of soils, vegetation and landforms over time.

Based on four decades of research by Professor Andrew Goudie, this volume provides a state-of-the-art synthesis of our understanding of desert geomorphology. It presents a truly international perspective, with examples from all over the world. Extensively referenced and illustrated, it covers such topics as the importance of past climatic changes, the variability of different desert environments, rock breakdown, wind erosion and dust storm generation, sand dunes, fluvial and slope forms and processes, the role of the applied geomorphologist in desert development and conservation, and the Earth as an analogue for other planetary bodies. This book is destined to become the classic volume on arid and semi-arid geomorphology for advanced students and researchers in physical geography, geomorphology, Earth science, sedimentology, environmental science, and archaeology.

"Understanding Sea-Level Rise and Variability" identifies the major impacts of sea-level rise, presents up-to-date assessments of past sea-level change, thoroughly explores all of the factors contributing to sea-level rise, and explores how sea-level extreme events might change. It identifies what is known in each area and what research and observations are required to reduce the uncertainties in our understanding of sea-level rise so that more reliable future projections can be made. A synthesis of findings provides a concise summary of past, present and future sea-level rise and its impacts on society.

Key Features: Book includes contributions from a range of international sea level experts Multidisciplinary Four color throughout Describes the limits of our understanding of this crucial issue as well as pointing to directions for future research

The book is for everyone interested in sea-level rise and its impacts, including policy makers, research funders, scientists, students, coastal managers and engineers.

Additional resources for this book can be found at: http: //www.wiley.com/go/church/sealevel.

"Retreat of mountain glaciers ranks alongside sea level rise and extermination of species as one of the greatest threats posed by continued global warming. The authoritative picture painted in "Darkening Peaks" should help bring humanity to its senses and to spur the actions needed."--James E. Hansen, NASA Goddard Institute for Space Studies
"This important and timely book elucidates how glacier retreat is affecting physical, biological, and human systems simultaneously. The authors' perspectives from mountain regions worldwide provide key insights at both global and local scales."--Cynthia Rosenzweig, Earth Institute, Columbia University
"From an impressive range of disciplinary perspectives and geographic locations, Darkening Peaks provides a refreshing look at the real complexities involved with the causes and consequences of environmental change."--Roger A. Pielke, Jr., author of "The Honest Broker: Making Sense of Science in Policy and Politics"
"Glaciers play a major role in teaching us about our planet's past, and in warning us about its future. They inspire fear, awe, and fascination. Whatever your interest in glaciers, you will find this rich, broadly ranging volume exciting."--Jared Diamond, author of "Guns, Germs, and Steel" and "Collapse"
""Darkening Peaks" is a dazzling fusion of hard science, historical narrative, and cultural context that outlines social responses for coping with our changing environment."--Stephen H. Schneider, Intergovernmental Panel on Climate Change
"Combining the latest research results from the social and natural sciences, "Darkening Peaks" succeeds in giving a timely and detailed account of the cultural perceptions, scientificobservations, trends, impacts, and responses associated with glacial retreat. Highly recommended."--John Schellnhuber CBE, Chief Science Advisor to the German government and Director, Potsdam Institute for Climate Impact Research

Ice Sheets and Late Quaternary Environmental Change provides a detailed account of the temporal and spatial distribution of ice sheets during the last ice age, and how these ice masses interacted with the environment. This is the first book in 20 years to detail the sizes of ice sheets during the last glaciation and the first to discuss their role in past climate change.
Arranged in two parts, the first part provides the tools required for evaluating past ice sheets while the second part uses these tools to establish the size, extent and dynamics of late Quaternary ice sheets. Assuming no prior knowledge of Quaternary Science, the discussion progresses from the basic principles of how and why ices ages occur, to the interpretation of proxy records of past climate and ocean change.
Instructive accounts of how the geological record can be used as evidence of former ice sheet behaviour and a discussion on the role of numerical models in understanding interaction between ice sheets, oceans and the atmosphere are included in this book. Details of former ice sheets are presented by geographical region along with a number of critical new theories on their size and behaviour.
This book would appeal to 2nd/3rd year students of Quaternary Science, most University Geography, Earth Science or Geology departments, as well as researchers and academics in Quaternary Science.

"I've seen the Sudan, traveled in South and Central America and been all over Europe, but I've never seen what I've been able to see on this tour [of the Loess Plateau, China]."
-Ed Skidmore, soil scientist, Wind
Erosion Research Unit of the Agricultural Research Service, USDA, Manhattan, Kansas

Overpopulation is at the core of most environmental problems. The impacts of continued growth-with world population reaching 6 billion in October 1999-are felt in most parts of the world. China, the most populous nation, illustrates many of the pivotal problems-and solutions.
Although China faces the same effects of overpopulation as the rest of the world, it still feeds over a billion people on a tillable area that allows about one tenth of a hectare per person. The country's efforts to tie together soil and water conservation, dryland farming, and economic development have been largely successful. Soil Erosion and Dryland Farming explores these trials and the lessons learned from them.
Copublished with the Soil and Water Conservation Society, this exhaustive text consists of the rewritten proceedings from the Society's conference held in Yangling, Shaanxi, China. It covers dryland farming systems and soil water management, environmental quality and sustainability, and erosion control techniques as they relate primarily to Mainland China. With additional global examples and a balance between conceptual and applied studies, it covers some of the most progressive work in soil erosion control and dryland farming from around the world.
Soil exposure while land lies fallow is one of the greatest risks in dryland farming. New procedures and kinds of tillage help control erosion and improve water intake. Soil Erosion and Dryland Farming presents these techniques and technologies to give you a forward-looking perspective into the field, as well as the larger problem of tailoring food production to sustain the population.