Here is a book for everyone who has an interest in how our planet works, what has happened during its 4,550 million year history and what might happen in the future. It tells how Earth scientists study the pattern of events that have shaped the planet and guided the evolution of life on Earth. In clear and simple language it describes how the effects of these events are measured and the careful detective work needed to unravel the extraordinary complexity of Earth history. The latest advances in dating methods, including the detection of regular patterns of global climate change, are explained and illustrated with real case histories. Our environment is unexpectedly unstable.
Dramatic and catastrophic changes in the environment have directed the evolution of life and the rise of Man, and we can expect similar events in the future. If we are to control their effects, we will have to understand what to expect - and what could happen if we try to intervene in the 'natural' development of our home, the Earth.

Examines the various forms of evidence used to establish the history and scale of environmenal changes during the Quaternary. The evidence is extremely diverse, ranging from landforms and sediments to fossil assemblages and isotope ratios, bringing the book fully up to date since its last publication.

In order to understand how climate may vary in the future - whether as a result of human activities or of natural fluctuations - we must first understand how and why it has varied in the past. "Climate Since AD 1500" presents a new perspective on the "Little Ice Age" and of the climate of the 20th century. The editors have gathered together over 50 contributors from all over the world to provide as wide a geographical dimension as possible. Leading scientists in their fields, they present climate and meteorological records of climatic variations available for the last 500 years, including research from several areas not previously recorded in an English language volume. These records include: historical documents; long instrumental records; tree rings and ice core records; records based on worldwide current research. Factors that are potentially important in causing climatic changes are also discussed. A postscript has been added since the previous edition to incorporate new research from the vast range of literature published on the subject in the last two years.

The ''Aral Sea Encyclopedia'' is the first one in the new series of encyclopedias about the seas of the former Soviet Union. Preparing it we faced certain difficulties. The thing is that this encyclopedia is a monument to the sea that is disappearing during our lifetime. The world community considers the situation with the Aral Sea and all changes that occurred in its whereabouts in the recent decades as one of the most serious, if not disastrous anthropogenic environmental crises of the 20th century. Before 1960, this was a water-abundant sea-lake that was fourth among world lakes after the Caspian Sea (USSR, Iran), the Great Lakes (USA, Canada) and Victoria Lake (Africa). This was a real ''pearl'' among the sands of the largest deserts, the Karakums and the Kyzylkums. Navigation between the sea ports Muinak and Aralsk and fisheries famous for the Aral breams, barbells, sturgeons, shemaya, and others were developed here. One could find beautiful recreational zones and beaches here. The deltas of the Amudarya, the major river of Central Asia, and the Syrdarya bringing their waters into the Aral Sea were famous for their biodiversity, fishery, muskrat rearing, reed prod- tion. The local population found occupations related to the water infrastructure.

This volume focuses on approaches towards a better understanding of the geological, hydrogeological and paleoclimatic evolution of Northeast Africa. Among the topics discussed are Phanerozoic interplate dynamics, sedimentology and stratigraphy, and mineral deposits and metallogeny.

Palaeomagnetism, plates, hot spots, trenches and ridges are the subject of this unusual book. Plate Tectonics is a book of exercises and background information that introduces and demonstrates the basics of the subject. In a lively and lucid manner, it brings together a great deal of material in spherical trigonometry that is necessary to understand plate tectonics and the research literature written about it. It is intended for use in first year graduate courses in geophysics and tectonics, and provides a guide to the quantitative understanding of plate tectonics.

This volume contains a range of topics from quaternary vertebrate palaeontology in Argentina and biostratigraphy of uppermost Cenozoic in the Pampas. It determines the ice-rafted lithoclasts by the observation on thin slides, the latter issued from the rock sustratum of the Antarctic continent.

The final report of the 1989 Finnish Work Group 9 of the INQUA on the Genesis and Lithology of Glacial Sediments entitled Glacigenic deposits as indicators of glacial movements and their use for indicator tracing in the search for ore deposits . Emphasizes the significance of extensive application o

This volume is a compilation of papers that deal with palaeoecological aspects of Argentina and Uruguay, and that derive from the special session on the Quaternary of South America at the XIIth INQUA International Congress held in Ottawa in 1987.

For most people, planet Earth's icy parts remain out of sight and out of mind. Yet it is the melting of ice that will both raise sea level and warm the climate further by reducing the white surfaces that reflect solar energy back into space. In effect, our icy places act as the world's refrigerator, helping to keep our climate relatively cool. The Icy Planet lays out carbon dioxide's role as the control knob of our climate over the past 1000 million years, then explores what is happening to ice and snow in Antarctica, the Arctic and the high mountains. Colin Summerhayes takes readers to the world's icy places to see what is happening to its ice, snow, and permafrost. He recounts tales from his own visits to these frozen landscapes, shining a light on some of the wonders he has encountered in his travels. He also brings together pieces of the climate story from different scientific disciplines, and from the past and the present, to illustrate how Earth's climate system works. Utilizing geological records of climate change alongside new technologies in ice coring, Summerhayes crafts a detailed and compelling record of Earth's climate history and examines how that can be used as a window into our future.

Cretaceous Sea Level Rise delves into the question of whether the observed short-term sea-level changes are regional (tectonic) or global (eustatic) and determines their possible relation to climate cycles; to assess the role of feedback mechanisms, i.e. thermal expansion/contraction of seawater, subsidence due to loading by water, changing vegetation of the Earth System and to investigate the relation of sea-level highs and lows to ocean anoxia and oxidation events, represented by black shales and oceanic red beds, and to evaluate the evidence for ephemeral glacial episodes or other climate events. Though research has been, and is being, conducted in these fields since the introduction of sea level cycles and sequence development concepts in the 1970"s, the available information is scattered. Cretaceous Sea Level Rise presents the current understanding and future directions of the research on Cretaceous sea level cycles in a single source, forming a reference work for beginners, graduates and postgraduates who are interested in this subject.

This volume represents the proceedings from a colloquium held in West Germany in 1980 on late and postglacial oscillations of glaciers. The main texts are in German (13), English (8) and French (5) but all have abstracts in the three languages and all the figure captions are similarly translated.

This publication is devoted to the natural feature the Black Sea andits littoral states. At the same time the Azov Sea is also considered here. This region is the focus of many geopolitical, economic, social and environmental issues that involve not only the countries coming out to the Black and Azov Seas, but other world countries, too.

This publication contains over 1500 articles and terms providing descriptions of geographical and oceanographic features, cities, ports, transport routes, marinebiological resources, international treaties, national and international programs, research institutions, historical and archaeological monuments, activities of prominent scientists, researchers, travelers, military commanders, etc. who had relation to the Black Sea.

It includes a multi-century chronology of the events that became the outstanding milestones in the history of development of the Black Sea Azov Sea region."

Thoroughly revised and expanded from the 2012 edition (twice the number of pages, almost double the number of illustrations) this book pays tribute to the man and his diverse works and achievements. James Hutton (1726-1797) was one of the first environmentalists, a man ahead of his time. He developed a grand theory of the Earth in which he tried to make sense of a lifetime of observation and deduction about the way in which our planet functions. For example, he connected temperature with latitude. His measurements, with rudimentary thermometers, of temperature changes between the base and summit of Arthur's Seat, were remarkably accurate and he studied climate data from other parts of the world. A leading figure in the eighteenth-century Scottish Enlightenment, he was also an innovative farmer, successful entrepreneur and a man with endless intellectual curiosity. The year 2026 will be the tercentenary of his birth. There will be many special events leading up to and in that year organised by The James Hutton Institute, Scotland's premier environmental and agricultural research organisation.

A new collection of vibrant essays to inform, stimulate and inspire every nature lover. Times of darkness offer opportunities to reflect. In Mistletoe Winter, Roy Dennis offers his reflections on the natural world from the past year - from the welcome signs of change to the ongoing problems we are posing for nature, and what humankind can and must do about them. As in his companion volume, Cottongrass Summer, Roy Dennis balances his alarm at the crisis confronting the natural world with his own sense of optimism that new generations can make crucial changes for the future. One of our most prominent advocates for our planet and its species, he writes with insight and originality. This volume will provide inspiration and ideas for everyone who cares about our planet and its species.

This English translation of "Istoricheskaya Geotektonika"

Contents: Origin of solar system and formation of planet Earth. Hadean 4.5-4.0 b.y.) stage of development; Early Archaean (4.0-3.5 b.y.): oldest sialic crust of the earth and problems of its formation; Middle and Late Archaean (3.5-2.5 b.y.): granite-greenstone terranes and granulite belts. Formation of mature continental crust; Early Proterozoic: partial destruction and restoration of Pangea; Early Riphean: new stage of destruction and commencement of fragmentation of Pangea I' Middle Riphean: continuation of destruction and break-up of Pangea; Late Riphean: Disintegration of Pangea into Gondwana and Laurasia. Origin of mobile belts against the background of development of plate tectonics; Vendian: consolidation of Gondwana and formation of mobile belts of Laurasia against the background of its disintegration; General features of the structural development of the earth's crust in the Precambrian.

The book gives an overview of the tectonic, geological, potential fields, etc maps of the Arctic that were compiled during geological and geophysical studies conducted in the Arctic over the past 15 years under the International project "Atlas of Geological Maps of the Circumpolar Arctic at a scale of 5M" and presents the results of geological, geophysical, paleogeographic and tectonic studies carried out in the Arctic Ocean and the Eastern Arctic during the implementation of national mapping and scientific programmes and studies intended to provide scientific substantiation for the extension of the continental shelf (ECS). Given its scope, the book will appeal to a wide range of geologists.

In Search of Ancient Tsunamis takes readers on a journey through the science of tsunamis and acts as a "how to" guide in the geology, geomorphology, anthropology, and archaeology of these devastating phenomena. The book draws on examples from around the world and includes numerous personal accounts of field and laboratory experiences. This journey through tsunami science is framed within the search for ancient tsunamis in the northern part of Chile, a desert environment that requires all the skillsets available to the tsunami researcher. This is a region where numerous attempts to find evidence have failed largely due to the hostile environment that refuses to play by the rules. The story is told through the very personal lens of the author with first-hand accounts of the trials and tribulations of fieldwork and local eccentricities, of serendipitous events, and a growing awareness and understanding of a wide variety of techniques that can be applied to the science. The journey is populated with side stories engaging the reader with deeper insights into the countries, study areas, joys and disappointments of carrying out scientific research across the globe. It is both a very personal story as well as an in-depth look at the science involved in an increasingly sophisticated and interdisciplinary search to better understand the true nature of tsunamis. It contains the wisdom of elders, "Eureka" moments of discovery, and a look at the very latest developments of understanding the effects of ancient tsunamis on prehistoric human populations.

Moving away from his earlier belief in a short, catastrophic history of the Earth, this volume shows how Buckland envisages instead progressive change as the Earth gradually cooled as it was prepared for human occupation. Extinct creatures did not die out because they were poorly designed; God loved the dinosaurs and had adapted them to their various circumstances.

Moving away from his earlier belief in a short, catastrophic history of the Earth, Buckland's treatise envisages instead and propounds the theory of a course of progressive change that occurred as the Earth gradually cooled and became ready for human occupation. During this time, the creatures that first walked the Earth did not die out because they were poorly designed; God loved the dinosaurs and had adapted them to their various circumstances.

Here is a book for everyone who has an interest in how our planet works, what has happened during its 4,550 million year history and what might happen in the future. It tells how Earth scientists study the pattern of events that have shaped the planet and guided the evolution of life on Earth. In clear and simple language it describes how the effects of these events are measured and the careful detective work needed to unravel the extraordinary complexity of Earth history. The latest advances in dating methods, including the detection of regular patterns of global climate change, are explained and illustrated with real case histories. Our environment is unexpectedly unstable.
Dramatic and catastrophic changes in the environment have directed the evolution of life and the rise of Man, and we can expect similar events in the future. If we are to control their effects, we will have to understand what to expect - and what could happen if we try to intervene in the 'natural' development of our home, the Earth.

The little-known history of how the Sahara was transformed from a green and fertile land into the largest hot desert in the world The Sahara is the largest hot desert in the world, equal in size to China or the United States. Yet, this arid expanse was once a verdant, pleasant land, fed by rivers and lakes. The Sahara sustained abundant plant and animal life, such as Nile perch, turtles, crocodiles, and hippos, and attracted prehistoric hunters and herders. What transformed this land of lakes into a sea of sands? When the Sahara Was Green describes the remarkable history of Earth's greatest desert-including why its climate changed, the impact this had on human populations, and how scientists uncovered the evidence for these extraordinary events. From the Sahara's origins as savanna woodland and grassland to its current arid incarnation, Martin Williams takes us on a vivid journey through time. He describes how the desert's ancient rocks were first fashioned, how dinosaurs roamed freely across the land, and how it was later covered in tall trees. Along the way, Williams addresses many questions: Why was the Sahara previously much wetter, and will it be so again? Did humans contribute to its desertification? What was the impact of extreme climatic episodes-such as prolonged droughts-upon the Sahara's geology, ecology, and inhabitants? Williams also shows how plants, animals, and humans have adapted to the Sahara and what lessons we might learn for living in harmony with the harshest, driest conditions in an ever-changing global environment. A valuable look at how an iconic region has changed over millions of years, When the Sahara Was Green reveals the desert's surprising past to reflect on its present, as well as its possible future.

This book is a collection of papers presented in the symposia, held in Beijing, on palaeontology and historical geology. The papers deal with different topics, providing information on Palaeobiogeography and Palaeoecology of Asian countries, their faunal content, and fossil preservation.

A Concise Geologic Time Scale: 2016 presents a summary of Earth's history over the past 4.5 billion years, as well as a brief overview of contemporaneous events on the Moon, Mars, and Venus. The authors have been at the forefront of chronostratigraphic research and initiatives to create an international geologic time scale for many years, and the charts in this book present the most up-to-date international standard, as ratified by the International Commission on Stratigraphy and the International Union of Geological Sciences. This book is an essential reference for all geoscientists, including researchers, students, and petroleum and mining professionals. The presentation is non-technical and illustrated with numerous colour charts, maps and photographs.

With the increasing awareness of environmental problems, there is a growing desire for a detailed understanding of superficial deposits in general, and glacial deposits in particular. This is because these sediments have a profound influence on groundwater protection, waste management and nature conservation. They are also of vital importance to civil engineering, because they provide the foundation for, as well as the materials extracted to build our roads and buildings. The greater part of the British Isles was glaciated, at least once, during the Quaternary Era. In the regions subjected to glaciation, glacial deposits underlie much of the present land surface. Although there have been many recent publications on various Quaternary geological topics, the present volume is the first dedicated to a detailed assessment of the glacial deposits of Britain and Ireland. After introductory chapters presenting the glacial history, the sedimentary sequences in 24 critical regions are discussed. These regions include all of Ireland, the glaciated area of Great Britain, and the adjoining offshore region of the North Sea. The controversial evolution of the Irish Sea Basin during the Last Glaciation is discussed from various viewpoints. A collection of 'critical topics' presented in the later part of the book range from the classification of glacigenic landforms and deposits to the results of geophysical, geotechnical and geochemical analyses. The book includes 368 figures, 40 tables and 51 colour photographs, a detailed index and a list of over 1000 references. With 45 contributions by 48 scientists, this volume represents a truly contemporary view of this field of research. Together with its companion volume the Glacial deposits in North-West Europe, this book provides an excellent textbook for the advanced student or the amateur, as well as an indispensible source- and guidebook for the professional scientist.