This monograph provides state-of-the-art theoretical and computational findings from investigations on physical and chemical dissolution front instability problems in porous media, based on the author s own work. Although numerical results are provided to complement theoretical ones, the focus of this monograph is on the theoretical aspects of the topic and those presented in this book are applicable to a wide range of scientific and engineering problems involving the instability of nonlinear dynamic systems. To appeal to a wider readership, common mathematical notations are used to derive the theoretical solutions. The book can be used either as a useful textbook for postgraduate students or as a valuable reference book for computational scientists, mathematicians, engineers and geoscientists."

The subject of this book is the methodology and results of integrated geophysical investigations in the Caucasian region, mainly interpretation of magnetic and gravity anomalies with utilization of a huge petrophysical database for the evaluation of geological structure and mineral resources. Relative voluminous geophysical data are useful for the Earth Sciences researchers interested in the Caucasian region (and adjacent and similar regions) characterized by complicated geological structure, inclined magnetization (polarization), uneven topography and mountain/sea transition. Examination of geophysical fields verified by super-deep wells drilling indicates that magmatic rocks of the Lesser Caucasus are extended northward under thick sedimentary cover of the Kura Depression up to the Greater Caucasus. These rocks form hidden petroleum-bearing traps of a newly identified type. On the basis of geophysical studies (mainly inexpensive magnetic and electric methods), a new copper-polymetallic province in the Greater Caucasus has been revealed. a newly developed integrated approach and special information-statistical techniques for processing and interpretation of geophysical data facilitate detection of important geological features, e.g. hidden intersections of linear structures that control location of large commercial ore and oil-and-gas deposits, as well as focuses of dangerous geodynamic events at a depth. Numerous illustrations (including colour) elucidate different problems and solutions on various scales and in diverse geological-geophysical environments. Many aspects of this book have been presented at the teaching courses for bachelors, masters and doctors at the Tel-Aviv University (Tel Aviv, Israel) and Ben-Gurion University (Be'er-Sheva, Israel). Benefits to readers are predetermined by the combination of the authors many-years personal experience in the geophysical studies of Azerbaijan and other regions of the Caucasus with the authors' knowledge of the modern level of geophysics in the world.

This beautifully illustrated 2007 volume describes the entire flora and fauna of the famous Lower Cretaceous Crato Formation of Brazil - one of the world's most important fossil deposits, exhibiting exceptional preservation. A wide range of invertebrates and vertebrates are covered, including extended sections on pterosaurs and insects. Two chapters are devoted to plants. Many of the chapters include descriptions of new species and re-descriptions and appraisals of taxa published in obscure places, rendering them available to a wider audience. Fossil descriptions are supported by detailed explanations of the geological history of the deposit and its tectonic setting. Drawing on expertise from around the world and specimens from the most important museum collections, this book forms an essential reference for researchers and enthusiasts with an interest in Mesozoic fossils.

Secord gives a dazzlingly detailed account of this scientific trench warfare and its social consequences. One ends up with a marvellous feeling for the major taxonomic enterprises in Darwin's younger day: mapping, ordering, conquering 'taming the chaos" of the strata. All of these of course had social and imperial ramifications; and Secord mentions geology's moral appeal (in supporting a divinely-stratified Creation) to a beleaguered elite intent on subduing the lower orders.

Originally published in 1990.

The Princeton Legacy Library uses the latest print-on-demand technology to again make available previously out-of-print books from the distinguished backlist of Princeton University Press. These paperback editions preserve the original texts of these important books while presenting them in durable paperback editions. The goal of the Princeton Legacy Library is to vastly increase access to the rich scholarly heritage found in the thousands of books published by Princeton University Press since its founding in 1905.

Comprising the first definitive account of the geological and palaeometeorological studies made by the British geologist, Frederic W. Harmer (1835-1924) this book contributes a previously missing chapter to the history of science. The main objective of the author is to ensure that the scientific work of Harmer, which unfortunately has been widely neglected or forgotten, becomes more generally known and acknowledged. The balance of this deficiency will be redressed by bringing to light in this volume his contributions to the history of science to an audience of academic and lay readers of the current literature.

First published in 1943, this was the last book of the eminent botanist and geologist Sir Albert Seward, who completed the manuscript three days before his death in 1941. The book was intended to be a useful and simply worded guide to geology for the general reader. Seward wished to emphasise the attraction which an understanding of geology could afford to anyone who enjoys a walk over the countryside. After a preliminary survey of the essentials of geology, the book then proceeds as a series of journeys through the British Isles, bringing the geological history and features of various regions under review.

The advent of accessible student computing packages has meant that geophysics students can now easily manipulate datasets and gain first-hand modeling experience - essential in developing an intuitive understanding of the physics of the Earth. Yet to gain a more in-depth understanding of physical theory, and to develop new models and solutions, it is necessary to be able to derive the relevant equations from first principles. This compact, handy book fills a gap left by most modern geophysics textbooks, which generally do not have space to derive all of the important formulae, showing the intermediate steps. This guide presents full derivations for the classical equations of gravitation, gravity, tides, earth rotation, heat, geomagnetism and foundational seismology, illustrated with simple schematic diagrams. It supports students through the successive steps and explains the logical sequence of a derivation - facilitating self-study and helping students to tackle homework exercises and prepare for exams.

Sir Roderick Impey Murchison (1792-1871) was an influential Scottish geologist best known for his classification of Palaeozoic rocks into the Silurian system. After early military experience in the Peninsular War, he resigned his commission; a chance meeting with Sir Humphrey Davy led him subsequently to pursue a scientific career. The Silurian System, published in 1839, was a highly influential study, which established the oldest contemporary classification of fossil-bearing strata. Murchison was appointed President of the Royal Geographical Society in 1843. These volumes, first published in 1875, use information taken from Murchison's private journals and correspondence. Archibald Geikie (1835-1924) provides a detailed account of his mentor's life and work in the context of geology as a developing science in the early nineteenth century, and provides a fascinating insight into the life and work of this eminent Victorian geologist. Volume 1 describes Murchison's early life and geological studies until 1842.

Sir Roderick Impey Murchison (1792-1871) was an influential Scottish geologist best known for his classification of Palaeozoic rocks into the Silurian system. After early military experience in the Peninsular War, he resigned his commission; a chance meeting with Sir Humphrey Davy led him subsequently to pursue a scientific career. The Silurian System, published in 1839, was a highly influential study, which established the oldest contemporary classification of fossil-bearing strata. Murchison was appointed President of the Royal Geographical Society in 1843. These volumes, first published in 1875, use information taken from Murchison's private journals and correspondence. Archibald Geikie (1835-1924) provides a detailed account of his mentor's life and work in the context of geology as a developing science in the early nineteenth century, and provides a fascinating insight into the life and work of this eminent Victorian geologist. Volume 2 describes his later life, from 1843 to 1871.

This biography, edited by the writer and critic Peter Bayne (1830 1896), was published in 1844. Miller (1802 1856), a Scottish geologist, palaeontologist and evangelical Christian, is best known for his geological arguments for the existence of God. Miller sought to demonstrate the accuracy of the biblical creation story by demonstrating that the seven days of creation correspond to seven geological periods. Volume 1 covers Miller's early life, family, education and apprenticeship as a stonemason, and includes a selection of letters, both private and public, including two that expound his developing views on religion. The work is a key source for the life and thought of this fascinating nineteenth-century man whose life was marked by a passionate commitment to both science and religion and the ongoing attempt to reconcile the two. It will invigorate and entertain the modern-day reader.

This biography, edited by the writer and critic Peter Bayne (1830 1896), was published in 1844. Miller (1802 1856), a Scottish geologist, palaeontologist and evangelical Christian, is best known for his geological arguments for the existence of God. Miller sought to demonstrate the accuracy of the biblical creation story by demonstrating that the seven days of creation correspond to seven geological periods. Volume 2 covers Miller's developing intellectual life and religious ideas; his publications; his marriage and the birth and loss of children; and his own tragic death after a long history of mental illness. The work is a key source for the life and thought of this fascinating nineteenth-century man whose life was marked by a passionate commitment to both science and religion and the attempt to reconcile the two. It will invigorate and entertain the modern-day reader.

George Poulett Scrope (1797 1876) was a British geologist who studied at Cambridge, where his teachers included Adam Sedgwick, and who became a close colleague of Charles Lyell. As an undergraduate he developed a lifelong fascination with volcanos, inspired by visits to Vesuvius and Etna. After graduating in 1821 he spent six months exploring extinct volcanos of the Massif Central in France, and he returned to Naples to witness the 1822 eruption of Vesuvius. In 1825 he published Considerations on Volcanos (also reissued in this series), and in 1826 he was elected a Fellow of the Royal Society. His pioneering work on France was originally published in 1827 as Memoir on the Geology of Central France and later revised for the 1858 edition reissued here. It contains detailed descriptions and illustrations of volcanos, and argues that the concept of geological time is important for the understanding of mineralogy and volcanism.

The geologist Richard Dixon Oldham (1858 1936) published the second edition of Geology of India in 1892 for the Geological Survey of India. The work is a thoroughgoing revision of the first edition of the same manual compiled by H. M. Medlicott (1829 1905) and W. T. Blanford (1832 1905), published in 1879. It contains one of the earliest and most important geological surveys of India. Owing to an increase in available data since the first edition, descriptions of the rock formations of the country are arranged chronologically. This edition is particularly important for the data on, and discussion of, the age and origins of the Himalayas. It includes other chapters on metamorphic and crystalline rocks, fossils, vegetation, volcanic regions, geological history, and rock formation. It is a key work of nineteenth-century geology which remains relevant for geologists studying the subcontinent today.

John Playfair (1748-1819) was a Scottish mathematician and geologist best known for his defence of James Hutton's geological theories. He attended the University of St Andrews, completing his theological studies in 1770. In 1785 he was appointed joint Professor of Mathematics at the University of Edinburgh, and in 1805 he was elected Professor of Natural Philosophy. This highly influential book, first published in 1802, contains Playfair's clarification and summary of Hutton's geological concepts. Playfair concisely explains Hutton's theories on erosion and geothermal heat in rock formation and the concept of uniformitarianism in geology, illustrating these theories with his own precise observations on different types of rock strata. The clarity of Playfair's explanations was instrumental in popularising Hutton's geological theories, many of which are now recognised as key principles of modern geology. Playfair's strident defence of Hutton's ideas formed part of a controversial debate between Hutton's supporters and his detractors.

Geological Evolution of Antarctica is a collection of papers presented at the Fifth International Symposium on Antarctic Earth Sciences, held under the auspices of the Scientific Committee on Antarctic Research (SCAR) at Robinson College, Cambridge, 23 28 August 1987. Contributors were invited to address problems related to the tectonic evolution of the Antarctic crust and the palaeoenvironmental evolution of Antartica since the Late Mesozoic. One hundred and seventy two papers and posters were presented, of which one hundred and fifteen are included in this volume. Papers dealing with the crustal development of Antarctica are divided into major geographical areas and arranged in chronostratigraphic order. The first four sections in this group cover the craton, the Transantarctic Mountains, Weddell Sea-Ross Sea region and the Pacific margin; the last addresses aspects of Gondwana break-up. A final group of papers discusses some of the environmental changes arising from the break-up of Gondwana.

KEY BENEFIT: Living With Earth: An Introduction to Environmental Geology is ideal for readers with little or no scientific background, fostering a better understanding of how they interact with Earth and how their actions can affect Earth's environmental health. The informal, friendly presentation is organized around a few unifying perspectives: how the various Earth systems interact with one another; how Earth affects people (creating hazards but also providing essential resources); and how people affect Earth. Greater emphasis is placed on environment and sustainability than on geology. Essential scientific foundations are presented-but the ultimate goal is to connect students proactively to their role as stakeholders in Earth's future.
What Does "Living with Earth" Mean? Earth Systems; The Dynamic Geosphere and Plate Tectonics; Geosphere Materials; Earthquakes; Volcanoes; Rivers and Flooding; Unstable Land; Changing Coasts; Water Resources; Soil Resources; Mineral Resources; Energy Resources; Atmosphere Resources and Climate Change; Managing People's Environmental Impact.
MARKET: A reader-friendly reference for those who wish to learn more about human-Earth system interaction.

Shows the bedrock geology. Information for superficial deposits may be omitted or shown only in outline.

A. C. Seward (1863 1941) was an eminent English geologist and botanist who pioneered the study of palaeobotany. After graduating from St John's College, Cambridge, in 1886 Seward was appointed a University Lecturer in Botany in 1890. In 1898 he was elected a Fellow of the Royal Society, and was appointed Professor of Botany in 1906. These volumes, published to great acclaim between 1898 and 1919, provide a detailed discussion and study of an emerging science. In the early nineteenth century, research and critical literature concerning palaeobotany was scattered across disciplines. In these volumes Seward synthesised and revised this research and also included a substantial amount of new material. Furnished with concise descriptions of fossil plants, detailed figures and extensive bibliographies these volumes became the standard reference for palaeobotany well into the twentieth century. Volume 1, published in 1898, contains an overview of palaeobotany with systematic descriptions of fossil plants.

A. C. Seward (1863 1941) was an eminent English geologist and botanist who pioneered the study of palaeobotany. After graduating from St John's College, Cambridge, in 1886 Seward was appointed a University Lecturer in Botany in 1890. In 1898 he was elected a Fellow of the Royal Society, and was appointed Professor of Botany in 1906. These volumes, published to great acclaim between 1898 and 1919, provide a detailed discussion and study of an emerging science. In the early nineteenth century, research and critical literature concerning palaeobotany was scattered across disciplines. In these volumes Seward synthesised and revised this research and also included a substantial amount of new material. Furnished with concise descriptions of fossil plants, detailed figures and extensive bibliographies these volumes became the standard reference for palaeobotany well into the twentieth century. Volume 2, first published in 1910, contains systematic descriptions of fossil ferns.

A. C. Seward (1863 1941) was an eminent English geologist and botanist who pioneered the study of palaeobotany. After graduating from St John's College, Cambridge, in 1886 Seward was appointed a University Lecturer in Botany in 1890. In 1898 he was elected a Fellow of the Royal Society, and was appointed Professor of Botany in 1906. These volumes, published to great acclaim between 1898 and 1919, provide a detailed discussion and study of an emerging science. In the early nineteenth century, research and critical literature concerning palaeobotany was scattered across disciplines. In these volumes Seward synthesised and revised this research and also included a substantial amount of new material. Furnished with concise descriptions of fossil plants, detailed figures and extensive bibliographies these volumes became the standard reference for palaeobotany well into the twentieth century. Volume 3, first published in 1917, contains systematic descriptions of fossil seed plants.

A. C. Seward (1863 1941) was an eminent English geologist and botanist who pioneered the study of palaeobotany. After graduating from St John's College, Cambridge, in 1886 Seward was appointed a University Lecturer in Botany in 1890. In 1898 he was elected a Fellow of the Royal Society, and was appointed Professor of Botany in 1906. These volumes, published to great acclaim between 1898 and 1919, provide a detailed discussion and study of an emerging science. In the early nineteenth century, research and critical literature concerning palaeobotany was scattered across disciplines. In these volumes Seward synthesised and revised this research and also included a substantial amount of new material. Furnished with concise descriptions of fossil plants, detailed figures and extensive bibliographies these volumes became the standard reference for palaeobotany well into the twentieth century. Volume 4, first published in 1919, contains systematic descriptions of fossil ginkgoales and coniferales.

Growth of population, communication and interdependence among countries has sharpened the impact of natural disasters. Not only have calamities and miseries been given wider publicity, but the realization has grown that through rational study and foresight much can be done to mitigate these hazards to life and social wellbeing. In this book we present a summary account of hazards which nowadays are usually classified as geological: earthquakes, faulting, tsunamis, seiches, vol canoes, avalanches, rock and soil slides, differential settlement and liquefaction of soil, and inundation. The book is aimed first at the general reader who is interested in studying the history of such hazards and examining ways that risk can be reduced even if all dangers cannot be eliminated. We also hope that the book will be useful to college students in introductory courses in geology, engineering, geography, country and urban planning, and in environmental studies. We have tried to bring out for the students the problems that remain to be solved.