Sentient Conceptualisations is about how scientists studying the past understand time in relation to space. Simonetti argues that the feelings for depths and surfaces, arising from the bodily movements and gestures of scientific practice, strongly influence conceptualisations of space and time. With an anthropological eye, Simonetti explores the ways archaeologists and those from related disciplines develop expert knowledge in varied environments. The book draws on ethnographic work carried out with Chilean and Scottish archaeologists, working both on land and underwater, to analyse in depth the visual language of science and what it reveals about the relation between thinking and feeling.

The story of the destruction of Sodom, Gomorrah, and Jericho--three cities situated along a major fault line extending 1,100 kilometers from the Red Sea to Turkey--is the oldest such description in human history. In this book, noted geologists K.O. Emery and David Neev have revisited that story to shed light on what happened there some 4,350 years ago. With all the benefits of modern geological and forensic science techniques at their disposal, the authors explore an area where earthquakes, volcanic activity, variations in the Dead Sea's level, and oscillations between arid and wet climates have affected life there for over 10,000 years. In reviewing the geology, biblical paleogeography, and limnology of the region, the authors have produced fascinating insights into the tectonic and climatic changes that have occurred in the region over the last 6,000 years and how those changes have affected cultural life in the Middle East. The Destruction of Sodom, Gomorrah, and Jericho is the first book to combine modern science and biblical archaeology to produce an authoritative account of the of these three great cities. It will fascinate students and researchers in geology, geophysics, and archaeology alike.

The Noerdlinger Ries and Steinheim Basin, two conspicuous geological structures in southern Germany, were traditionally viewed as somewhat enigmatic but nevertheless definitely volcanic edifices until they were finally recognized as impact craters in the 1960s. The changing views about the origin of the craters mark an important paradigm shift in the Earth sciences, from an Earth-centric approach to a planetary perspective that acknowledged Earth's place in the wider cosmos. Drawing on a range of printed sources, detailed archival material, letters, personal notes, and interviews with veterans of Ries research, Martina Koelbl-Ebert provides a detailed reconstruction, not only of the historical sequence of events throughout the twentieth century, but also of the personal thoughts, emotions and motives of the scientists involved and the social context of their research. She shows that there was a sudden reconnection of German researchers with the international scientific community, particularly with more progressive American researchers, after some twenty-five years of scientific isolation during the build-up to WWII and its aftermath. This reconnection brought about not only a new view of geoscience, but also saved German geology from self-sufficiency and patriotic arrogance by integrating it in an interdisciplinary and international framework. In so doing this book sheds much valuable light on an under-explored but crucial development in the way we understand Earth's history, as well as the way that science functioned during times of conflict.

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.

Although the history of orchards and fruit varieties is of great popular interest, there have been few academic treatments of the subject. This book presents results from a three-year project, 'Orchards East', investigating the history and ecology of orchards in the east of England. Together, the eastern counties of Hertfordshire, Essex, Cambridgeshire and Huntingdonshire, Bedfordshire, Norfolk and Suffolk have a tradition of fruit cultivation comparable in scale to that of the better-known west of England. Drawing on far-reaching archival research, an extensive survey of surviving orchards and biodiversity surveys, the authors tell the fascinating story of orchards in the east since the late Middle Ages. Orchards were ubiquitous features of the medieval and early modern landscape. Planted for the most part for practical reasons, they were also appreciated for their aesthetic qualities. By the seventeenth century some districts had begun to specialise in fruit production - most notably west Hertfordshire and the Fens around Wisbech. But it was only in the 'orchard century', beginning in the 1850s, that commercial production really took off, fuelled by the growth of large urban markets and new transport systems that could take the fruit to them with relative ease. By the 1960s orchards were extensive in many districts but, since then, they have largely disappeared, with significant impacts on landscape character and biodiversity. For well over a century now, orchards have been romanticised as nostalgic elements of a timeless yet disappearing rural world. Even before that, they were embedded in myths of lost Edens, or golden ages of effortless plenty. A key aim of this book is to challenge some of these myths by grounding orchards within a wider range of historical and environmental contexts. Orchards are not timeless, and in some ways our relationship with orchards is a classic example of the 'invention of tradition'. What do our attitudes to this aspect of our heritage tell us about our wider engagement with the past, with nature, and with place?

This book aims to view and to understand Alexander von Humboldt from different perspectives and in varying disciplinary contexts. His contributions addressed numerous topics in the earth but also life sciences-spanning from geo-botany, climatology, paleontology, oceanography, mineralogy, resources, and hydrogeology to links between the environmental impact of humans, erosion, and climate change. From the very beginning, he paved the way for a modern, integrated earth system science approach to decipher, characterize, and model the different forcing factors and their feedback mechanisms. It becomes obvious that Humboldt's holistic approach is far beyond simple description and empiric data collection. As documented and analyzed in the different texts of this volume, he combines observation and analysis with emotions and subjective perceptions in a very affectionate way. However, this publication does not intend to add another encyclopedic text compilation but to observe and critically analyze this unique personalitys relevance in a modern context, particularly in discussing environmental and social key issues in the twenty-first century.

A gripping history of the polar continent, from the great discoveries of the nineteenth century to modern scientific breakthroughs Antarctica, the ice kingdom hosting the South Pole, looms large in the human imagination. The secrets of this vast frozen desert have long tempted explorers, but its brutal climate and glacial shores notoriously resist human intrusion. Land of Wondrous Cold tells a gripping story of the pioneering nineteenth-century voyages, when British, French, and American commanders raced to penetrate Antarctica's glacial rim for unknown lands beyond. These intrepid Victorian explorers-James Ross, Dumont D'Urville, and Charles Wilkes-laid the foundation for our current understanding of Terra Australis Incognita. Today, the white continent poses new challenges, as scientists race to uncover Earth's climate history, which is recorded in the south polar ice and ocean floor, and to monitor the increasing instability of the Antarctic ice cap, which threatens to inundate coastal cities worldwide. Interweaving the breakthrough research of the modern Ocean Drilling Program with the dramatic discovery tales of its Victorian forerunners, Gillen D'Arcy Wood describes Antarctica's role in a planetary drama of plate tectonics, climate change, and species evolution stretching back more than thirty million years. An original, multifaceted portrait of the polar continent emerges, illuminating our profound connection to Antarctica in its past, present, and future incarnations. A deep-time history of monumental scale, Land of Wondrous Cold brings the remotest of worlds within close reach-an Antarctica vital to both planetary history and human fortunes.

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.

Tuzo is the never-before-told story of one of Canada's most influential scientists and the discovery of plate tectonics, a pivotal development that forever altered how we think of our planet. In 1961, a Canadian geologist named John "Jock" Tuzo Wilson (1908-1993) jettisoned decades of strongly held opposition to theories of moving continents and embraced the idea that they drift across the surface of the Earth. Tuzo tells the fascinating life story of Tuzo Wilson, from his early forays as a teenaged geological assistant working on the remote Canadian Shield in the 1920s to his experiences as a civilian-soldier in the Second World War to his ultimate role as the venerated father of plate tectonics. Illuminating how science is done, this book blends Tuzo's life story with the development of the theory of plate tectonics, showing along the way how scientific theories are debated, rejected, and accepted. Gorgeously illustrated, Tuzo will appeal to anyone interested in the natural world around them.

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.

The book deals with the record of important Neoproterozoic to Early Palaeozoic events in southwestern Gondwana, that heralded the Cambrian explosion and the dawn of modern ecosystems. It contains a detailed account of the Neoproterozoic to Cambrian geological record in a poorly-known part of the world, which is at the same time key to understand fundamental processes at the Proterozoic-Cambrian transition. The emphasis is placed on litho-, bio-, chemostratigraphy and magmatism. The palaeoclimatic, tectonic, evolutionary radiation and extinction events and associated mineralizations will be identified and discussed. A synthesis of all data is provided at the end of the book, integrating the data from all cratons and fold belts in southwestern Gondwana. The events will be individualized, their impact discussed and correlations between different successions both within and outside Gondwana proposed.
The book is organized in three sections. Section one is an introduction to the neoproterozoic and Cambrian seen as a time of upheavals, extremes and innovations. Section two comprisesnineteen chapters dealing with theneoproterozoic-Cambrian events in southwestern Gondwana. Section three will provide a synthesis on every major topic, and a critical assessment of the global implications of the presented data.
* The book deals with the record of important Neoproterozoic to Early Palaeozoic events in southwestern Gondwana, that heralded the Cambrian explosion and the dawn of modern ecosystems.
It contains a detailed account of the Neoproterozoic to Cambrian geological record in a poorly-known part of the world, which is at the same time key to understand fundamental processes at the Proterozoic-Cambrian transition. The emphasis is placed on litho-, bio-, chemostratigraphy and magmatism."

SHORTLISTED FOR THE ROYAL SOCIETY SCIENCE PRIZE 2022 'A joyful collision of science, history and nature writing' Helen Gordon, author of Notes from Deep Time Adam Sedgwick was a priest and scholar. Roderick Murchison was a retired soldier. Charles Lapworth was a schoolteacher. It was their personal and intellectual rivalry, pursued on treks through Wales, Scotland, Cornwall, Devon and parts of western Russia, that revealed the narrative structure of the Paleozoic Era, the 300-million-year period during which life on Earth became recognisably itself. Nick Davidson follows in their footsteps and draws on maps, diaries, letters, field notes and contemporary accounts to bring the ideas and characters alive. But this is more than a history of geology. As we travel through some of the most spectacular scenery in Britain, it's a celebration of the sheer visceral pleasure generations of geologists have found, and continue to find, in noticing the earth beneath our feet.

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

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.

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.

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.

This volume presents the latest science on all significant geological and paleontological aspects of the Earth during the Late Triassic Period. Rather than presenting a collection of narrowly focused research papers, the volume consists of a series of peer-reviewed chapters on specific aspects of the Late Triassic world (e.g., tectonics, magmatism, paleobotany, climate, etc.), all authored by experts in the subject of their respective chapters. Each chapter reviews and summarizes the latest findings in these fields and also includes a review of the pertinent literature. The author list is very broadly international and forms a veritable who's who of expertise in these fields. The book is loosely organized to present the physical aspects of Earth during the Late Triassic at the outset, followed by the paleontological aspects. The latter section is further organized to present the record of the marine environment first before moving onto land, with fauna followed by flora. The volume closes with a review of the end-Triassic extinctions.

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.

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.

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.