Darwin As a Geologist – Biographical Reflections
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History of Geology
FEBRUARY 2007 PRIMEFACT 563 (REPLACES MINFACT 60) History of geology Mineral Resources Early humans needed a knowledge of simple geology to enable them to select the most suitable rock types both for axe-heads and knives and for the ornamental stones they used in worship. In the Neolithic and Bronze Ages, about 5000 to 2500 BC, flint was mined in the areas which are now Belgium, Sweden, France, Portugal and Britain. While Stone Age cultures persisted in Britain until after 2000 BC, in the Middle East people began to mine useful minerals such as iron ore, tin, clay, gold and copper as early as 4000 BC. Smelting techniques were developed to make the manufacture of metal tools possible. Copper was probably the earliest metal to be smelted, that is, extracted from its ore by melting. Copper is obtained easily by reducing the green copper carbonate mineral malachite, itself regarded as a precious stone. From 4000 BC on, the use of clay for brick-making became widespread. The Reverend William Branwhite Clarke (1798-1878), smelting of iron ore for making of tools and the ‘father’ of geology in New South Wales weapons began in Asia Minor at about 1300 BC but did not become common in Western Europe until Aristotle believed volcanic eruptions and nearly 500 BC. earthquakes were caused by violent winds escaping from the interior of the earth. Since earlier writers had ascribed these phenomena to The classical period supernatural causes, Aristotle's belief was a By recognising important surface processes at marked step forward. Eratosthenes, a librarian at work, the Greek, Arabic and Roman civilisations Alexandria at about 200 BC, made surprisingly contributed to the growth of knowledge about the accurate measurements of the circumference of earth. -
The Importance of French Transformist Ideas for the Second Volume of Lyell’S Principles of Geology Pietro Corsi
The importance of french transformist ideas for the second volume of lyell’s principles of geology Pietro Corsi To cite this version: Pietro Corsi. The importance of french transformist ideas for the second volume of lyell’s principles of geology. 2004. halshs-00002894 HAL Id: halshs-00002894 https://halshs.archives-ouvertes.fr/halshs-00002894 Preprint submitted on 20 Sep 2004 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. THE BRITISH JOURNAL FOR THE HISTORY OF SCIENCE Vol. II t No. 39 (1978) < 221 > THE IMPORTANCE OF FRENCH TRANSFORMIST IDEAS FOR THE SECOND VOLUME OF LYELL'S PRINCIPLES OF GEOLOGY PIETRO CORSI* RECENTLY there has been considerable revaluation of the development of natural sciences in the early nineteenth century, dealing among other things with the works and ideas of Charles Lyell. The task of interpreting Lyell in balanced terms is extremely complex because his activities covered many fields of research, and because his views have been unwarrantably distorted in order to make him the precursor of various modern scientific positions. Martin Rudwick in particular has contributed several papers relating to Lyell's Principles of geology, and has repeatedly stressed the need for a comprehensive evaluation of Lyell's scientific proposals, and of his position in the culture of his time. -
Natural Theology and Natural History in Darwin’S Time: Design
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ETD - Electronic Theses & Dissertations NATURAL THEOLOGY AND NATURAL HISTORY IN DARWIN’S TIME: DESIGN, DIRECTION, SUPERINTENEDENCE AND UNIFORMITY IN BRITISH THOUGHT, 1818-1876 By Boyd Barnes Dissertation Submitted to the Faculty of the Graduate School of Vanderbilt University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in Religion May, 2008 Nashville, Tennessee Approved: Professor James Hudnut-Beumler Professor Dale A. Johnson Professor Eugene A. TeSelle Professor Richard F. Haglund Professor James P. Byrd William Buckland “The evidences afforded by the sister sciences exhibit indeed the most admirable proofs of design originally exerted at the Creation: but many who admit these proofs still doubt the continued superintendence of that intelligence, maintaining that the system of the Universe is carried on by the force of the laws originally impressed upon matter…. Such an opinion … nowhere meets with a more direct and palpable refutation, than is afforded by the subserviency of the present structure of the earth’s surface to final causes; for that structure is evidently the result of many and violent convulsions subsequent to its original formation. When therefore we perceive that the secondary causes producing these convulsions have operated at successive epochs, not blindly and at random, but with a direction to beneficial ends, we see at once the proofs of an overruling Intelligence continuing to superintend, direct, modify, and control the operation of the agents, which he originally ordained.” – The Very Reverend William Buckland (1784-1856), DD, FRS, Reader in Geology and Canon of Christ Church at the University of Oxford, President of the Geological Society of London, President of the British Association for the Advancement of Science, Dean of Westminster. -
The Geohistorical Time Arrow: from Steno's Stratigraphic Principles To
JOURNAL OF GEOSCIENCE EDUCATION 62, 691–700 (2014) The Geohistorical Time Arrow: From Steno’s Stratigraphic Principles to Boltzmann’s Past Hypothesis Gadi Kravitz1,a ABSTRACT Geologists have always embraced the time arrow in order to reconstruct the past geology of Earth, thus turning geology into a historical science. The covert assumption regarding the direction of time from past to present appears in Nicolas Steno’s principles of stratigraphy. The intuitive–metaphysical nature of Steno’s assumption was based on a biblical narrative; therefore, he never attempted to justify it in any way. In this article, I intend to show that contrary to Steno’s principles, the theoretical status of modern geohistory is much better from a scientific point of view. The uniformity principle enables modern geohistory to establish the time arrow on the basis of the second law of thermodynamics, i.e., on a physical law, on the one hand, and on a historical law, on the other. In other words, we can say that modern actualism is based on the uniformity principle. This principle is essentially based on the principle of causality, which in turn obtains its justification from the second law of thermodynamics. I will argue that despite this advantage, the shadow that metaphysics has cast on geohistory has not disappeared completely, since the thermodynamic time arrow is based on a metaphysical assumption—Boltzmann’s past hypothesis. All professors engaged in geological education should know these philosophical–theoretical arguments and include them in the curriculum of studies dealing with the basic assumptions of geoscience in general and the uniformity principle and deep time in particular. -
Hutton, Kelvin, and the Great Earth Debates. • the Beginnings of Modern Geology “All Natural Processes That Affect the Earth’S Crust (Erosion, Deposition, • Ca
Chapter 1 The Science of Geology An Introduction to Geology • Geology - the science that pursues an understanding of planet Earth • Physical geology - examines the materials composing Earth and seeks to understand the many processes that operate beneath and upon its surface • Historical geology - seeks an understanding of the origin of “If there is an interesting place you want to go, there is Earth and its development interesting geology that you can study there” through time Mersin ophiolite, (Cappadocia, Central Turkey). Turkey The Science of Geology The Science of Geology 1.3: satellite image of Mt. Vesuvius, Italy. • Some historical views • Geology, people, and the environment of the Earth • Many important relationships exist between • Aristotle, 300 BC; people and the natural environment • James Ussher, ca. 1600, ‘Earth was created in Problems and issues 4004 BC;’ addressed by • Catastrophism geology include • Earth’s features formed through • Natural hazards, sudden and violent resources, world changes. ‘The Dog population growth, of and environmental Pompeii’ issues Dwelling in Goreme, Cappadocia The Science of Geology Hutton, Kelvin, and the great Earth debates. • The beginnings of modern geology “All natural processes that affect the Earth’s crust (erosion, deposition, • ca. 1780, James Huton’s volcanic eruptions, faulting, glaciation Theory of the Earth; etc.) operate with the same intensity • Uniformitarianism: “the and under the same set of physical processes that operate constraints now as in the geologic past.” today have operated in “(as to the age of Earth) we see no the past.” vestige of a beginning, no prospect of • a uniformitarian view of an end.” Earth requires a vast These points are incorrect - why? amount of time…. -
William Smith Abstracts
William Smith 1769-1839 Acknowledgements This meeting is a part of a number of events that mark the Bicentennial of the first map published by William Smith. We gratefully acknowledge the support of ARUP for making this meeting possible. Sponsor: CONTENTS Inside Cover Sponsors Acknowledgement Event Programme Page 1 Speaker Abstracts Page 37 Poster Abstracts Page 47 Speaker Biographies Page 57 Burlington House Fire Safety Information Page 58 Ground Floor Plan of the Geological Society, Burlington House William Smith Meeting 2015 200 Years of Smith’s Map 23-24 April 2015 PROGRAMME SPEAKER ABSTRACTS William Smith Meeting 23 April 2015 DAY ONE 1 William Smith's (1769-1839) Searches for a Money-earning Career Hugh Torrens Keele University, Keele, Staffordshire, ST5 5BG, UK email: [email protected] This lecture will concentrate on Smith's, highly complex, early 'career paths'. His first employment was as a land surveyor (1). Then in 1793 he became both, canal surveyor (2), and engineer, (3) to the Somerset Coal Canal (SCC). These had guaranteed him a regular, and known, income. But this suddenly changed, when he was successively dismissed, first as surveyor, then as engineer, in 1799. He now had to find some other means of supporting himself, and the geological revelations, which he knew were so important, that he had uncovered in Somerset. In the mid-1790s, he had done some land drainage and irrigation work (4), for the chairman of the SCC, and immediately after his dismissals, was able to generate an adequate living from such work around Bath, during a period of very high rainfall. -
Press Release
Press Release Issued: Wednesday 12th August 2020 Darwin mentor and geology pioneer Charles Lyell’s archives reunited Fascinating writings of an influential scientist who shaped Charles Darwin’s thinking have become part of the University of Edinburgh’s collections. A rich assortment of letters, books, manuscripts, maps and sketches by Scottish geologist Sir Charles Lyell, have been reassembled at the University Library’s Centre for Research Collections, with the goal of making the collection more accessible to the public. Some 294 notebooks, purchased from the Lyell family following a £1 million fundraising campaign in 2019, form a key part of the collection. Although written in the Victorian era, the works shed light on current concerns, including climate change and threats to biodiversity. Now a second tranche of Lyell material has been allocated to the University by HM Government under the Acceptance in Lieu of Inheritance Tax scheme. These new acquisitions, from the estate of the 3rd Baron Lyell, will join other items that have been part of the University’s collections since 1927. The new archive includes more than 900 letters, with correspondence between Lyell and Darwin, the botanist Joseph Dalton Hooker, the publisher John Murray and Lyell’s wife, Mary Horner Lyell, and many others. It also includes a draft manuscript and heavily annotated editions of Lyell’s landmark book The Principles of Geology and several manuscripts from his lectures. Lyell, who died in 1875, aged 77, mentored Sir Charles Darwin after the latter’s return from his five-year voyage on the Beagle in 1836. The Scot is also credited with providing the framework that helped Darwin develop his evolutionary theories. -
References Geological Society, London, Memoirs
Geological Society, London, Memoirs References Geological Society, London, Memoirs 2002; v. 25; p. 297-319 doi:10.1144/GSL.MEM.2002.025.01.23 Email alerting click here to receive free email alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Geological Society, London, Memoirs or the Lyell Collection Notes Downloaded by on 3 November 2010 © 2002 Geological Society of London References ABBATE, E., BORTOLOTTI, V. & PASSERINI, P. 1970. Olistostromes and olis- ARCHER, J. B, 1980. Patrick Ganly: geologist. Irish Naturalists' Journal, 20, toliths. Sedimentary Geology, 4, 521-557. 142-148. ADAMS, J. 1995. Mines of the Lake District Fells. Dalesman, Skipton (lst ARTER. G. & FAGIN, S. W. 1993. The Fieetwood Dyke and the Tynwald edn, 1988). fault zone, Block 113/27, East Irish Sea Basin. In: PARKER, J. R. (ed.), AGASSIZ, L. 1840. Etudes sur les Glaciers. Jent & Gassmann, Neuch~tel. Petroleum Geology of Northwest Europe: Proceedings of the 4th Con- AGASSIZ, L. 1840-1841. On glaciers, and the evidence of their once having ference held at the Barbican Centre, London 29 March-1 April 1992. existed in Scotland, Ireland and England. Proceedings of the Geo- Geological Society, London, 2, 835--843. logical Society, 3(2), 327-332. ARTHURTON, R. S. & WADGE A. J. 1981. Geology of the Country Around AKHURST, M. C., BARNES, R. P., CHADWICK, R. A., MILLWARD, D., Penrith: Memoir for 1:50 000 Geological Sheet 24. Institute of Geo- NORTON, M. G., MADDOCK, R. -
Archibald Geikie (1835–1924): a Pioneer Scottish Geologist, Teacher, and Writer
ROCK STARS Archibald Geikie (1835–1924): A Pioneer Scottish Geologist, Teacher, and Writer Rasoul Sorkhabi, University of Utah, Salt Lake City, Utah 84108, USA; [email protected] years later, but there he learned how to write reports. Meanwhile, he read every geology book he could find, including John Playfair’s Illustrations of the Huttonian Theory, Henry de la Beche’s Geological Manual, Charles Lyell’s Principles of Geology, and Hugh Miller’s The Old Red Sandstone. BECOMING A GEOLOGIST In the summer of 1851, while the Great Exhibition in London was attracting so many people, Geikie decided instead to visit the Island of Arran in the Clyde estuary and study its geology, aided by a brief report by Andrew Ramsay of the British Geological Survey. Geikie came back with a report titled “Three weeks in Arran by a young geologist,” published that year in the Edinburgh News. This report impressed Hugh Miller so much that the renowned geologist invited its young author to discuss geology over a cup of tea. Miller became Geikie’s first mentor. In this period, Geikie became acquainted with local scientists and pri- vately studied chemistry, mineralogy, and geology under Scottish naturalists, such as George Wilson, Robert Chambers, John Fleming, James Forbes, and Andrew Ramsay—to whom he con- fessed his desire to join the Geological Survey. In 1853, Geikie visited the islands of Skye and Pabba off the coast Figure 1. Archibald Geikie as a young geolo- of Scotland and reported his observations of rich geology, including gist in Edinburgh. (Photo courtesy of the British Geological Survey, probably taken in finds of Liassic fossils. -
Report Case Study 25
EXECUTIVE SUMMARY 1. Brief Description of item(s) 294 manuscript notebooks of the geologist Sir Charles Lyell (1797-1875). In two series: 263 numbered notebooks, 1825-1874, on geology, natural history, social and political subjects; 31 additional notebooks, 1818-1871, with indices. Mostly octavo format. For details see Appendix 1. In good condition. 2. Context The nineteenth century saw public debate about how to conduct science reach new heights. Charles Lyell was a pivotal figure in the establishment of geology as a scientific discipline; he also transformed ideas about the relationship between human history and the history of the earth. Above all, he revealed the significance of ‘deep time’. At a time when the Anglican church dominated intellectual culture, geology was a controversial subject. Lyell played a significant part in separating the practice of science from that of religion. Through his major work, The Principles of Geology, he developed the method later adopted by Darwin for his studies into evolution. Lyell observed natural phenomena at first hand to infer their underlying causes, which he used to interpret the phenomena of the past. The method stressed not only a vast geological timescale, but also the ability of small changes to produce, eventually, large ones. The Principles combined natural history, theology, political economy, anthropology, travel, and geography. It was an immediate success, in Britain, Europe, North America and Australia. Scientists, theologians, leading authors, explorers, artists, and an increasingly educated public read and discussed it. Lyell’s inductive method strongly influenced the generation of naturalists after Darwin. Over the rest of his life, Lyell revised the Principles in the light of new research and his own changing ideas. -
Newsletter of the History of Geology Group of the Geological Society
HOGG Newsletter of the History of Geology Group of The Geological Society Number 68 February 2020 Front cover WILLIAM AUGUSTUS EDMOND USSHER (1849‒1920), the centenary of whose death is remembered this year. Born in County Galway, Ireland in 1849, Ussher joined the Geological Survey of Great Britain (now British Geological Survey) in 1868 and spent his whole career (retiring in 1909) as a field and mapping surveyor. He is best known for his work in the south-west of England (Cornwall, Devon, Somerset), particularly his work on the Devonian, Carboniferous and Triassic strata. In 1894, he was awarded the Geological Society’s Murchison Medal. Many Survey maps and memoirs bear his name as does the Ussher Society founded in 1962 as a focus for geological research in south-west England. Originally published under the title Proceedings of the Ussher Society, its journal was renamed Geoscience in South-West England in 1998. Sources Anon. 1920. Obituary of Mr W. A. E. Ussher. Nature, 105, 144. Anon [R. D. Oldham] 1921. Obituary Proceedings of the Geological Society in Quarterly Journal of the Geological Society, 77, lxxiii‒lxxiv. British Geological Survey. https://www.bgs.ac.uk/discoveringGeology/geologyOfBritain/archives/pioneers/pioneers.cfc?method=search ¤tTab=tab_U Burt, E. 2013. W. A. E. Ussher: an insight into his life and character. Geoscience in South-West England, 13, 165‒171. Dineley, D. L. 1974. W. A. E. Ussher: his work in the south-west. Proceedings of the Ussher Society, 3, 189‒201. House, M. R. 1978. W. A. E. Ussher: his ancestral background. Proceedings of the Ussher Society, 4, 115‒118. -
Catastrophism and Uniformitarianism: Logical Roots and Current Relevance in Geology
Downloaded from http://sp.lyellcollection.org/ by guest on September 29, 2021 Catastrophism and uniformitarianism" logical roots and current relevance in geology VICTOR R. BAKER Department of Hydrology and Water Resources, The University of Arizona, Tucson, AZ 85721-0011, USA Abstract, Catastrophism in the Earth sciences is rooted in the view that Earth signifies its causative processes via landforms, structures and rock. Processes of types, rates and magnitudes not presently in evidence may well be signified this way. Uniformitarianism, in contrast, is a regulative stipulation motivated by the presumed necessity that science achieves logical validity in what can be said (hypothesized) about the Earth. Regulative principles, including simplicity, actualism and gradualism, are imposed a priori to insure valid inductive reasoning. This distinction lies at the heart of the catastrophist versus uniformitarian debates in the early nine- teenth century and it continues to influence portions of the current scientific program. Uniform- itarianism, as introduced by Charles Lyell in 1830, is specifically tied to an early nineteenth century view of inductive inference. Catastrophism involves a completely different form of inference in which hypotheses are generated retroductively. This latter form of logical inference remains relevant to modern science, while the outmoded notions of induction that warranted the doctrine of uniformitarianism were long ago shown to be overly restrictive in scientific practice. The latter should be relegated solely to historical interest in the progress of ideas. On 4 July 1997, the Mars Pathfinder spacecraft Antarctic ice, was interpreted as showing various made a highly successful landing in the Ares Vallis indicators of possible relic biogenic activity region of Mars.