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Books > Earth & environment > Earth sciences > Geology & the lithosphere > Historical geology
Trace metals play key roles in life - all are toxic above a threshold bioavailability, yet many are essential to metabolism at lower doses. It is important to appreciate the natural history of an organism in order to understand the interaction between its biology and trace metals. The countryside and indeed the natural history of the British Isles are littered with the effects of metals, mostly via historical mining and subsequent industrial development. This fascinating story encompasses history, economics, geography, geology, chemistry, biochemistry, physiology, ecology, ecotoxicology and above all natural history. Examples abound of interactions between organisms and metals in the terrestrial, freshwater, estuarine, coastal and oceanic environments in and around the British Isles. Many of these interactions have nothing to do with metal pollution. All organisms are affected from bacteria, plants and invertebrates to charismatic species such as seals, dolphins, whales and seabirds. All have a tale to tell.
Learn how the deep history of nature became a dominant paradigm of historical thinking, through a study of landscapes of India. Winner of the BSHS Pickstone Prize by the British Society for the History of Science In the nineteenth century, teams of men began digging the earth like never before. Sometimes this digging-often for sewage, transport, or minerals-revealed human remains. Other times, archaeological excavation of ancient cities unearthed prehistoric fossils, while excavations for irrigation canals revealed buried cities. Concurrently, geologists, ethnologists, archaeologists, and missionaries were also digging into ancient texts and genealogies and delving into the lives and bodies of indigenous populations, their myths, legends, and pasts. One pursuit was intertwined with another in this encounter with the earth and its inhabitants-past, present, and future. In Inscriptions of Nature, Pratik Chakrabarti argues that, in both the real and the metaphorical digging of the earth, the deep history of nature, landscape, and people became indelibly inscribed in the study and imagination of antiquity. The first book to situate deep history as an expression of political, economic, and cultural power, this volume shows that it is complicit in the European and colonial appropriation of global nature, commodities, temporalities, and myths. The book also provides a new interpretation of the relationship between nature and history. Arguing that the deep history of the earth became pervasive within historical imaginations of monuments, communities, and territories in the nineteenth century, Chakrabarti studies these processes in the Indian subcontinent, from the banks of the Yamuna and Ganga rivers to the Himalayas to the deep ravines and forests of central India. He also examines associated themes of Hindu antiquarianism, sacred geographies, and tribal aboriginality. Based on extensive archival research, the book provides insights into state formation, mining of natural resources, and the creation of national topographies. Driven by the geological imagination of India as well as its landscape, people, past, and destiny, Inscriptions of Nature reveals how human evolution, myths, aboriginality, and colonial state formation fundamentally defined Indian antiquity.
As in the original edition of 1988, this book covers the principles and practice of argon isotopic dating, a technique that has been used to determine the numerical age of the Earth. The greater precision of the 40Ar/39Ar method allows scientists to test smaller geological samples than its precursor, the K-Ar method, which required a comparison of different elements. The new edition will incorporate new developments made in 40Ar/39Ar application over the last decade, made possible by advances in lasers and mass spectrometry.
'A lyrical meditation on landscapes and cities, vivid reportage and a memoir. And also a beautifully realised and moving read.' Financial Times 'A beguiling mix of history, geology, folklore and memoir that captivated me from the first page.' Lara Maiklem, author of Mudlarking 'Tom Chivers brings a poet's sensibility to this book about the hidden parts of the capital, mixing the past with the present, the known with the unknown and his personal story with social history and geology.' Bernardine Evaristo, author of Girl, Woman, Other What secrets lie beneath a city? Tom Chivers follows hidden pathways, explores lost islands and uncovers the geological mysteries that burst up through the pavement and bubble to the surface of our streets. From Roman ruins to a submerged playhouse, from an abandoned Tube station to underground rivers, Chivers leads us on a journey into the depths of the city he loves. A lyrical interrogation of a capital city, a landscape and our connection to place, London Clay celebrates urban edgelands: in-between spaces where the natural world and the metropolis collide. Through a combination of historical research, vivid reportage and personal memoir, it will transform how you see London, and cities everywhere. 'Tom Chivers, with the forensic eye of an investigator, the soul of a poet, is an engaging presence; a guide we would do well to follow.' Iain Sinclair, author of The Last London
This third edition of Reconstructing Quaternary Environments has been completely revised and updated to provide a new account of the history and scale of environmental changes during the Quaternary. The evidence is extremely diverse ranging from landforms and sediments to fossil assemblages and geochemical data, and includes new data from terrestrial, marine and ice-core records. Dating methods are described and evaluated, while the principles and practices of Quaternary stratigraphy are also discussed. The volume concludes with a new chapter which considers some of the key questions about the nature, causes and consequences of global climatic and environmental change over a range of temporal scales. This synthesis builds on the methods and approaches described earlier in the book to show how a number of exciting ideas that have emerged over the last two decades are providing new insights into the operation of the global earth-ocean-atmosphere system, and are now central to many areas of contemporary Quaternary research.
The resolution of the sixty-year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth science. This four-volume treatise on the continental drift controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary theory. Based on extensive interviews, archival papers and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. This second volume provides the first extensive account of the growing paleomagnetic case for continental drift in the 1950s and the development of apparent polar wander paths that showed how the continents had changed their positions relative to one another, more or less as Wegener had proposed. Paleomagnetism offered the first physical measure that continental drift had occurred and helped determine the changing latitudes of the continents through geologic time.
The resolution of the sixty-year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth science. This four-volume treatise on the continental drift controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary theory. Based on extensive interviews, archival papers and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. This third volume describes the expansion of the land-based paleomagnetic case for drifting continents and recounts the golden age of marine geology and geophysics. Fuelled by the Cold War, US and British workers led the way in making discoveries and forming new hypotheses, especially about the origin of oceanic ridges. When first proposed, seafloor spreading was just one of several competing hypotheses about the evolution of ocean basins.
The resolution of the sixty-year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth science. This four-volume treatise on the continental drift controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary theory. Based on extensive interviews, archival papers and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. This fourth volume explains the discoveries in the mid 1960s which led to the rapid acceptance of seafloor spreading theory and how the birth of plate tectonics followed soon after with the geometrification of geology. Although plate tectonics did not explain the cause or dynamic mechanism of drifting continents, it provided a convincing kinematic explanation that continues to inspire geodynamic research to the present day.
The archipelagos of Orkney and Shetland are the products of some of the most dramatic events which have occurred in the Earth's history. The Shetlands are the eroded roots of a vast mountain range that once soared to Himalayan heights and extended from Scandinavia to the Appalachians. Around 65 million years ago, this mighty chain was split asunder by the shifting of the Earth's tectonic plates, and the North Atlantic Ocean was formed. In earlier times, the area was occupied by a huge freshwater lake - Lake Orcadie - which existed for almost 10 million years and was home to a wide range of primitive species of fish. Later, during the last Ice Age, the area was completely submerged beneath ice sheets which left an indelible mark on the landscapes of both island groups. This book tells the incredible geological story of the most northerly outposts of the British Isles.
This book provides a new look at the climatic history of the last 2.6 million years during the ice age, a time of extreme climatic fluctuations that have not yet ended. This period also coincides with important phases of human development from Neanderthals to modern humans, both of whom existed side by side during the last cold stage of the ice age. The ice age has seen dramatic expansions of glaciers and ice sheets, although this has been interspersed with relatively short warmer intervals like the one we live in today. The book focuses on the changing state of these glaciers and the effects of associated climate changes on a wide variety of environments (including mountains, rivers, deserts, oceans and seas) and also plants and animals. For example, at times the Sahara was green and colonized by humans, and Lake Chad covered 350,000 km2 larger than the United Kingdom. What happened during the ice age can only be reconstructed from the traces that are left in the ground. The work of the geoscientist is similar to that of a detective who has to reconstruct the sequence of events from circumstantial evidence. The book draws on the specialisms and experience of the authors who are experts on the glacial history of the Earth. Readership: Undergraduate and postgraduate students studying the Quaternary, researchers, and anyone interested in climate change, environmental change and geology. The book provides a rich collection of illustrations and photographs to help the readers at all levels visualise the dramatic consequences of glacier expansions during the Ice Age.
The Small Isles comprise the Inner Hebridean islands of Rum, Eigg, Canna and Muck. The landscapes, rocks and fossils of these beautiful, remote islands tells of a drama involving erupting volcanoes, an ancient ecosystem that included dinosaurs and an ancient desert landscape. The geological history stretches back 3 billion years to the earliest events recorded on Earth. All four islands owe their origin to a group of three adjacent volcanoes that were active around 60 million years ago. Rum is the eroded remains of the magma chamber of one of these volcanoes. Eigg and Muck are part of the lava field that extends north from the Mull volcano and Canna lies towards the southern extent of the lavas that flowed from the Skye volcano. The final event that left a mark on these islands was the Ice Age that started around 2.4 million years ago. Its effect on the landscape was profound. The thick cover of erosive ice shaped the contours of the land into the hills and glens that we are familiar with today.
The written history and archaeological records of Central Scotland takes us back to Pictish times some 5,000 years ago. The geology of the area stretches back a further 400 million years. The oldest rocks are found near Lesmahagow and in the Pentland Hills. Known geologically as 'inliers'- small areas of rocks from an older age, surrounded by younger strata - these strata have yielded some of the oldest fish on earth and are highly prized for what they tell us about early life on the planet. Rocks of the Old Red Sandstone and the succeeding Carboniferous era underlie the rest of Central Scotland in almost equal measure. Explosive volcanic rocks, thick layers of lava, desert sandstones, limestones and productive coal measures make up this bedrock patchwork. Then, sometime later, a covering of ice, some two kilometres thick, blanketed the landscape. It sandpapered and burnished the bedrock into the familiar scenes we see today - our matchless Scottish landscape. The coal and iron ore which lay beneath the ground between Edinburgh and Glasgow provided the raw materials that drove the Industrial Revolution in Scotland, and the early focus on understanding the rocks beneath our feet was unsurprisingly initially concentrated on the most useful minerals resources.
Take a learning journey through billions of years of Earth history This indispensable guide to the fundamentals of geology is the ideal way to introduce yourself to all the basics, from rocks, minerals, and fossil fuels to earthquakes, volcanoes, and plate tectonics. Using quick quizzes and self-tests to reinforce key concepts, Geology carefully walks you through billions of years of Earth history. Illustrated with more than one hundred specially commissioned illustrations and fifty photographs that help clarify difficult concepts, this easy-to-follow book is an interactive resource for anyone interested in learning more about our planet. Whether you are new to geology or want to refresh and update your knowledge, the proven self-teaching guide approach will allow you to work at your own pace, check your progress, and learn more about this fascinating field of study.
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.
Illustrated with 200 barn sketches, diagrams, and maps, this book takes you on a journey through the St Croix River Valley. It grounds you in the geography, geology and biology of the region and introduces you to its original inhabitants, the Dakota and Ojibwe peoples, European explorers, fur traders and loggers and the settlers that followed them. It is a celebration of regional diversity and architectural expression through a single type of building - the barn.
This book describes the geological setting of Iran throughout geological history, referring to paleogeography and general geodynamics. Also, all structural units, faults, tectonic phases and orogeny occurred in the geology of Iran have been evaluated. Magmatic and metamorphic rocks along with ophiolitic complexes have extensive outcrops in Iran, and these rocks with Precambrian age constitute its basement. Study and identification of such rocks not only throws light on the geodynamic issues of Iran but also helps in recognition of the mode of formation and evolution of the sedimentary basins located within various structural divisions of the country. Moreover, the majority of metallic and non-metallic mineral deposits are associated either directly or indirectly with magmatic, and at time metamorphic, rocks. In the Magmatism and Metamorphism parts, it is tried to thoroughly consider the various aspects of the igneous rocks, whether intrusive, extrusive or young volcanoes, from the point of view of petrography, geochemistry and geodynamics. In addition, the major intrusive bodies of Iran have been presented along with their petrologic and chronologic specifications in tables, mentioning the bibliographic resources.
A beautful book for anyone interested in exploring the history of trade in maps. Trade is the lifeblood of nations. It has provided vital goods and wealth to countries and merchants from the ancient Egyptians who went in search of gold and ivory to their 21st-century equivalents trading high-tech electronic equipment from the Far East. In this beautiful book, more than 70 maps give a visual representation of the history of World Commerce, accompanied by text which tells the extraordinary story of the merchants, adventurers, middle-men and monarchs who bought, sold, explored and fought in search of profit and power. The maps are all works of art, witnesses to history, and have a fascinating story to tell. The maps include * Catalhoeyuk Plan, c. 6200BC * Babylonian Map of the World, c. 600BC * Stone Map of China, 1136 * Hereford Mappa Mundi, c. 1300 * Buondelmonti Map of Constantinople, c. 1420 * The Waldseemuller Map, 1507 * James Rennell Map of Hindoostan, 1782 * Air Age Map, 1945 * Johns Hopkins Covid-19 Dashboard, 2020
The book provides the first comprehensive and thematic treatment of micropalaeontology and its applications in petroleum exploration. The first part deals with pure micropalaeontology, and the second part with the principles and practices of applied micropalaeontology and sequence stratigraphy. Case histories of applications in a range of geographic, geologic, and stratigraphic settings are given.
Discover one of the Scottish Enlightenment's brightest stars. Among the giants of the Scottish Enlightenment, the name of James Hutton is overlooked. Yet his Theory of the Earth revolutionised the way we think about how our planet was formed and laid the foundation for the science of geology. He was in his time a doctor, a farmer, a businessman, a chemist yet he described himself as a philosopher - a seeker after truth. A friend of James Watt and of Adam Smith, he was a polymath, publishing papers on subjects as diverse as why it rains and a theory of language. He shunned status and official position, refused to give up his strong Scots accent and vulgar speech, loved jokes and could start a party in an empty room. Yet much of his story remains a mystery. His papers, library and mineral collection all vanished after his death and only a handful of letters survive. He seemed to be a lifelong bachelor, yet had a secret son whom he supported throughout his life. This book uses new sources and original documents to bring Hutton the man to life and places him firmly among the geniuses of his time.
Serpentinites, a major source of both ornamental facing stone in architecture and asbestos, are considered enigmatic rocks due to their apparent complexity. Yet studying serpentinites and the processes that form them is essential to understanding the formations in the Earth's tectonic plates. This book presents the geological history of serpentinites, from detailed descriptions and photographs in outcrop and under the microscope, to models describing the distribution of serpentine minerals and the formation of chrysotile-asbestos deposits. Students pursuing research topics in serpentinites or Earth scientists investigating tectonic processes in mid-ocean ridges will find this a useful reference book.
The Earth that sustains us today was born out of a few remarkable,
near-catastrophic revolutions, started by biological innovations
and marked by global environmental consequences. The revolutions
have certain features in common, such as an increase in the
complexity, energy utilization, and information processing
capabilities of life. This book describes these revolutions,
showing the fundamental interdependence of the evolution of life
and its non-living environment. We would not exist unless these
upheavals had led eventually to 'successful' outcomes - meaning
that after each one, at length, a new stable world emerged.
This book outlines the development and perspectives of the Anthropocene concept by Paul J. Crutzen and his colleagues from its inception to its implications for the sciences, humanities, society and politics. The main text consists primarily of articles from peer-reviewed scientific journals and other scholarly sources. It comprises selected articles on the Anthropocene published by Paul J. Crutzen and a selection of related articles, mostly but not exclusively by colleagues with whom he collaborated closely. * In the year 2000 Nobel Laureate Paul J. Crutzen proposed the Anthropocene concept as a new epoch in Earth's history * Comprehensive collection of articles on the Anthropocene by Paul J. Crutzen and his colleagues* Unique primary research literature and Crutzen's comprehensive bibliography* Paul Crutzen's scientific investigations into human influences on atmospheric chemistry and physics, the climate and the Earth system, leading to the conception of the Anthropocene* Reflections on the Anthropocene and its implications* Bibliometric review of the spread of the use of the Anthropocene concept in the Natural and Social Sciences, Humanities and Law
DUST is unmistakably a major book in the making. This is a book with an extraordinary global story to tell, but - and - also with an ethical argument to advance. - Robert Macfarlane __________ Four-and-a-half billion years ago, Planet Earth was formed from a vast spinning nebula of cosmic dust, the detritus left over from the birth of the sun. Within the next hundred years, human life on swathes of the earth's surface will also end, in a haze of heat, drought and, again, dust. Dust is the legacy of twentieth-century progress and a profound threat to life in the twenty-first. And yet it's something we hardly ever consider - so small and so mundane as to be beyond the threshold of thought. All of history is recorded in the dust we create: the pollution we make, the fires we start, the chemicals we use, the volcanos that erupt. Now, for the first time DUST will examine this substance and reveal it's importance and the fascinating stories it has.
This is a book about an ocean that vanished six million years ago - the ocean of Tethys. Named after a Greek sea nymph, there is a sense of mystery about such a vast, ancient ocean, of which all that remains now are a few little pools, like the Caspian Sea. There were other great oceans in the history of the Earth - Iapetus, Panthalassa - but Tethys was the last of them, vanishing a mere moment (in geological terms) before Man came on the scene. Once Tethys stretched across the world. How do we know? And how could such a vast ocean vanish? The clues of its existence are scattered from Morocco to China. This book tells the story of the ocean, from its origins some 250 million years ago, to its disappearance. It also tells of its impact on life on Earth. The dinosaurs were just beginning to get going when Tethys formed, and they were long dead by the time it disappeared. Dorrik Stow describes the powerful forces that shaped the ocean; the marine life it once held and the rich deposits of oil that life left behind; the impact of its currents on environment and climate. It is rarely realized how very important oceans are to climate and environment, and therefore to life on Earth. The story of Tethys is also a story of extinctions, and floods, and extraordinary episodes such as the virtual drying up of the Mediterranean, before being filled again by a dramatic cascade of water over the straits of Gibralter. And in the telling of that story, we also learn how geologists put together the clues in rocks and fossils to discover Tethys and its history.
This book gives a comprehensive view of the strengths and limits of the interdisciplinary methods that work together to form the geohistorical approach to geographical and geological sciences. The geohistorical approach can be synthetically defined as a multi- and interdisciplinary approach that uses techniques and perspectives, mainly from geography, history, and natural sciences, to examine topics that inform the space-time knowledge of environment, territory, and landscape. The boundary between the application of physical and human science methods is large and hazy. This volume exists at this boundary and offers an approach that utilizes both historical data (from both physical and human records) and GIScience (e.g. GIS, cartography, GPS, remote sensing) to investigate the evolution of the environment, territory and landscape through both space and time. The first objective of this volume is to define the term geohistorical approach. An entire chapter focuses on a review of the main disciplines that connect geography and history, a review of the terms environment, territory, and landscape as objects of study of this approach, and the definition and importance of the geohistorical approach. The second goal is to describe the methods used in the geohistorical approach. Eight chapters present the key methods also using examples of applications from the international context, offering an awareness of the potentials, limitations and accuracy of each method, with particular focus on the integration of methods. The third goal is to provide case studies to demonstrate the use and integration of geohistorical methods from both original material and published research. A final chapter is dedicated to an interdisciplinary case study from the Venetian Plain (Italy), providing an example of the integration of almost all methods described in the book. |
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