Significant advances in geomatics and geomorphology are changing the way in which scientists study complex mountain environments. This book provides a critical treatment and evaluation of these recent developments. With the advent of advanced satellite sensors, high resolution satellite imagery and digital elevation, models now make possible quantitative analysis and modelling of the landscape. So it is becoming ever more important for geoscientists to integrate geomatics into their scientific investigation. This book is a "must" for any researcher actively working in geomatics, geomorphology and mountain systems. It will also be valuable to geologists and resource planners interested in the role of surface processes in complex orogens and resource assessment and sustainable development.

Channelized Rivers Perspectives for Environmental Management Andrew Brookes Environmental Consultant, Reading, UK For centuries engineers have modified river channels in order to control floods, drain land, prevent erosion and improve navigation. The natural shape of many rivers has been dramatically changed, often with dire environmental consequences. This book demonstrates the role fluvial geomorphology can play in the design of river channels, both to lessen environmental impact and to enhance the success of channelization schemes. It considers the physical and biological impacts of channelization, the repercussions downstream and in the adjacent floodplain. Revised procedures and designs are proposed which minimize harsh environmental impacts. The interdisciplinary approach of the book offers river managers the opportunity to make more environmentally sensitive decisions in the course of their work. The book will be of great interest to geomorphologists, biologists and civil engineers working in the water industry.

This book provides a wealth of geomathematical case history studies performed by the author during his career at the Ministry of Natural Resources Canada, Geological Survey of Canada (NRCan-GSC). Several of the techniques newly developed by the author and colleagues that are described in this book have become widely adopted, not only for further research by geomathematical colleagues, but by government organizations and industry worldwide. These include Weights-of-Evidence modelling, mineral resource estimation technology, trend surface analysis, automatic stratigraphic correlation and nonlinear geochemical exploration methods. The author has developed maximum likelihood methodology and spline-fitting techniques for the construction of the international numerical geologic timescale. He has introduced the application of new theory of fractals and multi fractals in the geostatistical evaluation of regional mineral resources and ore reserves and to study the spatial distribution of metals in rocks. The book also contains sections deemed important by the author but that have not been widely adopted because they require further research. These include the geometry of preferred orientations of contours and edge effects on maps, time series analysis of Quaternary retreating ice sheet related sedimentary data, estimation of first and last appearances of fossil taxa from frequency distributions of their observed first and last occurrences, tectonic reactivation along pre-existing schistosity planes in fold belts, use of the grouped jackknife method for bias reduction in geometrical extrapolations and new applications of the theory of permanent, volume-independent frequency distributions.

This re-issue, first published in 1964, is the first of a seminal series analysing the development of the study of landforms, from both the geographical and geological point of view, with especial emphasis upon fluvial geomorphology. Volume 1 treats the subject up to the first important statement of the cycle of erosion by W. M. Davis in 1889, and attempts to identify the most significant currents of geomorphic thought, integrating them into the broader contemporary intellectual frameworks with which they were associated. As well as dealing with such key figures as Werner, De Saussure, Hutton, Playfair, Buckland, lyell, Agassiz, Ramsay, Dana, Peschel, Powell, Gilbert and Davis, attention is also given to many less important contributions by American, British and continental workers. A spirited biographical treatment, attractively set off by contemporary portraits, diagrams and sketches, will make this book of great interest to the historian of science, and indeed to the general reader, as well as to the student and scholar in geomorphology, hydrology and any other earth science.

This book provides a general survey of Geocryology, which is the study of frozen ground called permafrost. Frozen ground is the product of cold climates as well as a variety of environmental factors. Its major characteristic is the accumulation of large quantities of ice which may exceed 90% by volume. Soil water changing to ice results in ground heaving, while thawing of this ice produces ground subsidence often accompanied by soil flowage. Permafrost is very susceptible to changes in weather and climate as well as to changes in the microenvironment. Cold weather produces contraction of the ground, resulting in cracking of the soil as well as breakup of concrete, rock, etc. Thus permafrost regions have unique landforms and processes not found in warmer lands. The book is divided into three parts. Part 1 provides an introduction to the characteristics of permafrost. Four chapters deal with its definition and characteristics, the unique processes operating there, the factors affecting it, and its general distribution. Part 2 consists of seven chapters describing the characteristic landforms unique to these areas and the processes involved in their formation. Part 3 discusses the special problems encountered by engineers in construction projects including settlements, roads and railways, the oil and gas industry, mining, and the agricultural and forest industries. The three authors represent three countries and three language groups, and together have over 120 years of experience of working in permafrost areas throughout the world. The book contains over 300 illustrations and photographs, and includes an extensive bibliography in order to introduce the interested reader to the large current literature. Finalist of the 2019 PROSE Awards.

The surface of the Earth is and always has been in flux, constantly being remodelled by powerful natural forces. This text explores the processes and evidence of change, explaining how to recognize past events in the rocks, guiding through geological time to recreate past landscapes, and illustrating agents of erosion such as water, wind and ice sculpting solid landscapes, rocks amd materials recycling at the Earth's surface, and human impact on global cycles and climate change. This book complements the exhibition entitled "Restless Surface" in the Earth Galleries at the Natural History Museum, London.

This book, first published in 1985, arises from the 14th Binghamton Geomorphology Symposium. The chapters here illustrate the use of models in various areas of research in geomorphology.

The tropics provide the key to understanding much biological and Earth science. This is particularly true for the study of landforms, which in higher latitudes suffer great seasonal contrasts in process intensity and type, and which often in the past underwent the dramatic changes of glaciation and periglaciation. Yet studies in the tropics have shown that the legacy of past climate changes is much more dramatic than was formerly believed. This book, first published in 1985, brings together the variety of evidence about such environmental changes, over a variety of timescales, and sets it against the current knowledge of the nature of geomorphic processes in the tropics.

This unique treatment of geomorphology, first published in 1986, provides a comprehensive work to enable students to see the subject as a whole. Taking the concepts that run through the subject and cut across its standard divisions, the book summarises the history of intellectual debate in geomorphology and then describes modern developments, both pure and applied.

This book, first published in 1986, stems from the 1986 Binghamton Geomorphology Symposium. The topic was chosen because of the advances in the study of aeolian processes and landforms, particularly in the area of desertification, and the papers collected here clearly indicate that their study is not constrained by discipline boundaries but are of interest to geologists, physical geographers, soil scientists, meteorologists and engineers.

Time is a central feature of geomorphological research, and is used in this book (first published in 1977) to provide a conceptual framework within which to consider and compare old and new approaches to the field of geomorphology. The emphasis is on providing not merely a manual of current research but an introduction to isolate ideas and concepts, stimulate critical discussion and examine some of the problems that are involved in dealing with data.

The study of landforms is becoming increasingly scientific. This book, first published in 1971, attempts to do justice to the work done in the last few decades, but strives to avoid a too uncritical acceptance of contemporary trends. The author first examines the fundamental characteristics and basic postulates of geomorphology. He then seeks to define the systematic stages through which the study of the landforms of a given area might proceed. Examples are drawn from a wide geographical range with emphasis on presenting examples of actual observations and measurements. The final section presents concise descriptions of simple and inexpensive methods of acquiring field data in landform study.

In this re-evaluation of the basic postulates of geomorphology, first published in 1982, Alistair Pitty examines the subject within its scientific context, arguing that coherence in geomorphology can be demonstrated despite the many apparent divergences, which should themselves be regarded as poles within a spectrum of opinion. Not least, the particularly geological and geographical aspects of geomorphology are carefully identified and explained within this coherence.

This book, first published in 1985, conveys the flavours of geomorphology and the bases of its ideas. It portrays the positive features of pluralism in geomorphology, and focuses on processes operative and their associated landforms; the distinctive geological settings of karst, volcanicity and tectonic activity; and technological advances.

This book, first published in 1973, focuses on non-urban terrain, and presents a uniquely balanced historical treatment of both the land degradation induced by man and his efforts at conservation, preservation and reclamation.

This book, first published in 1979, collects together a key set of papers from the 10th Binghamton Geomorphology Symposium. They analyse fluvial theory, channel processes, stream adjustments, paleo-adjustments and channel adjustments.

This book, first published in 1982, forms the proceedings volume of the 11th Binghamton Geomorphology Symposium. Chapters cover various coastline phenomena, glacial and periglacial processes, carbonate terrains, and specific applications of geomorphic knowledge and techniques.

This book, first published in 1980, is a timely and comprehensive appraisal of thresholds in geomorphology. The papers, arising from the 9th Binghamton Geomorphology Symposium, form the cornerstone of a subject that is increasingly important in geomorphology. This book analyses the historical background to thresholds and geomorphology, as well as fluvial landforms, hydrogeologic regimes and other processes, and the impact of man.

Whether the project is river engineering, soil mapping for landuse planning, or control of landslides, this volume, first published in 1976, illustrates that the professional partnership between geomorphology and engineering can significantly minimize environmental damage. The papers here were presented at the 7th Binghamton Geomorphology Symposium, and using the broad viewpoint of the planner, much new ground is covered: landfill design, prediction of geomorphic processes and their effects, and minimization of streamflow distortion.

This book, first published in 1986, collects the articles presented to the 16th Binghamton Geomorphology Symposium and is a ground-breaking work in the study of hillslope processes. Hillslope processes are studied in a variety of disciplines other than geomorphology, such as hydrology, pedology, agricultural engineering, civil engineering and engineering geology - the study is truly an interdisciplinary science.

This book, first published in 1989, the proceedings of the 19th Binghamton Geomorphology Symposium, is the first set of essays focused on the history of the subject. The articles analyse the founding precepts of geomorphology, the early pioneers, the formation of a defined discipline, and the present state of the topic.

This book, first published in 1992, contains the proceedings of the 22nd Binghamton Geomorphology Symposium, and highlights the quantity and diversity of periglacial geomorphic research being undertaken in Arctic and alpine environments. The articles explore a variety of geomorphic processes and examine the potential impacts of global change on the nature and extent of permafrost and seasonal ice phenomena.

This book, first published in 1985, is a comprehensive guide to the main ideas in the history of geomorphology. It traces the development of thinking on landforms, with material ranging from the ancient world to the present day. The main areas covered are the Renaissance, the explosive growth of the Natural Sciences in the nineteenth century and the impact of the Second World War. The papers and theories of specialists like James Hutton, John Playfair and W.M. Davies are presented and discussed and the final chapters reflect on future change, based on the past and speculation on possible developments. Balance is maintained between the dual importance and dominance of English and North American contributions to the subject, and quite substantial research was undertaken to provide a more complete approach to some areas hitherto neglected.

This book, first published in 1977, is a concise, fully illustrated introduction to modern geomorphology. Geomorphologists pay much attention to the measurement of present day processes in attempting to develop explanations of landscape evolution, and this book reflects this approach by deliberately emphasising processes in humid environments.

Soils and sediments influence current processes, preserve evidence of past processes, indicate evolutionary phases in landscapes and provide a basis for relative and absolute chronologies. They provide an important key to the integration of short-term process studies and investigation of longer-term landform evolution. This book, first published in 1985, has been arranged to provide wide temporal and spatial coverage, with studies ranging from historic to geologic time scales and micro- to macro-spatial scales. The interdisciplinary nature of the subject is reflected in contributions from soil scientists, engineering geologists, hydrologists and geomorphologists.