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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. -
Formal and Informal Networks of Knowledge and Etheldred Benett's
Journal of Literature and Science Volume 8, No. 1 (2015) ISSN 1754-646X Susan Pickford, “Social Authorship, Networks of Knowledge”: 69-85 “I have no pleasure in collecting for myself alone”:1 Social Authorship, Networks of Knowledge and Etheldred Benett’s Catalogue of the Organic Remains of the County of Wiltshire (1831) Susan Pickford As with many other fields of scientific endeavour, the relationship between literature and geology has proved a fruitful arena for research in recent years. Much of this research has focused on the founding decades of the earth sciences in the early- to mid-nineteenth century, with recent articles by Gowan Dawson and Laurence Talairach-Vielmas joining works such as Noah Heringman’s Romantic Rocks, Aesthetic Geology (2003), Ralph O’Connor’s The Earth on Show: Fossils and the Poetics of Popular Science, 1802-1856 (2007), Virginia Zimmerman’s Excavating Victorians (2008) and Adelene Buckland’s Novel Science: Fiction and the Invention of Nineteenth-Century Geology (2013), to explore the rhetorical and narrative strategies of writings in the early earth sciences. It has long been noted that the most institutionally influential early geologists formed a cohort of eager young men who, having no tangible interests in the economic and practical applications of their chosen field, were in a position to develop a passionately Romantic engagement with nature, espousing an apocalyptic rhetoric of catastrophes past and borrowing epic imagery from Milton and Dante (Buckland 9, 14-15). However, as Buckland further notes, this argument – though persuasive as far as it goes – fails to take into account the broad social range of participants in the construction of early geological knowledge. -
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. -
The Wyley History of the Geologists' Association in the 50 Years 1958
THE WYLEY HISTORY OF THE GEOLOGISTS’ ASSOCIATION 1958–2008 Leake, Bishop & Howarth ASSOCIATION THE GEOLOGISTS’ OF HISTORY WYLEY THE The Wyley History of the Geologists’ Association in the 50 years 1958–2008 by Bernard Elgey Leake, Arthur Clive Bishop ISBN 978-0900717-71-0 and Richard John Howarth 9 780900 717710 GAHistory_cover_A5red.indd 1 19/08/2013 16:12 The Geologists’ Association, founded in 1858, exists to foster the progress and Bernard Elgey Leake was Professor of Geology (now Emeritus) in the diffusion of the science of Geology. It holds lecture meetings in London and, via University of Glasgow and Honorary Keeper of the Geological Collections in the Local Groups, throughout England and Wales. It conducts field meetings and Hunterian Museum (1974–97) and is now an Honorary Research Fellow in the School publishes Proceedings, the GA Magazine, Field Guides and Circulars regularly. For of Earth and Ocean Sciences in Cardiff University. He joined the GA in 1970, was further information apply to: Treasurer from 1997–2009 and is now an Honorary Life Member. He was the last The Executive Secretary, sole editor of the Journal of the Geological Society (1972–4); Treasurer (1981–5; Geologists’ Association, 1989–1996) and President (1986–8) of the Geological Society and President of the Burlington House, Mineralogical Society (1998–2000). He is a petrologist, geochemist, mineralogist, Piccadilly, a life-long mapper of the geology of Connemara, Ireland and a Fellow of the London W1J 0DU Royal Society of Edinburgh. He has held research Fellowships in the Universities of phone: 020 74349298 Liverpool (1955–7), Western Australia (1985) and Canterbury, NZ (1999) and a e-mail: [email protected] lectureship and Readership at the University of Bristol (1957–74). -
So6 NATURE (SEPTEMBER 22, T904
so6 NATURE (SEPTEMBER 22, t904 Is Selenium Radio-active? THE HEART OF SKYE.' lT occurred to me recently that a possible ·method of deciding between the two hypotheses which have been THIS volume of detailed rock-description, raising brought forward to explain radio-activity, namely, that of in its successive chapters questions of profound atomic degradation (Rutherford and Soddy, Ramsay, &c.) interest in philosophic geology, proves that the Geo and that of molecular change (Armstrong and Lowry, Proc. logical Survey of the United Kingdom is confident Roy. Soc., 1903), lay in attempting to realise radio-activity that the scientific spirit should permeate its public in the case of an element well known to undergo molecular work. None of the rocks dealt with possesses at pre change readily, but with an atomic weight small enough sent an economic value; most of the area is untraversed to exclude the probability of an atomic instability such as by roads, and the exposures are not to be sought in is assumed for radium and thorium. Such an element is quarries, but in rain-swept uplands, or high on selenium (at. wt. .79), which suggested itself to me as a desolate mountain-walls. Yet no detail is regarded suitable material to experiment with because, under the as unimportant; the surveyor, for months together, influence of light, it undergoes a remarkable alteration in its electrical resistance and E.M.F. of contact, suggesting leads a life as hard and remote as that of an Alaskatt an allotropic change of an altogether unusual character. pioneer; and the result is a book in which the daily As this change, whatever be its real nature, occurs almost difficulties are concealed, while an array of facts is instantaneously (Bellati and Romanese, A tti R. -
Persp V1n2 Final4pdf
MODERN SCIENCE AND THE SEARCH FOR TRUTH Brian Tonks—Department of Physics have pondered the question, “What is truth?” for many years. My I intellectual journey has convinced me that truth comes in many ways through a variety of sources. I began my schooling believing that scientists were searching for the truth, but my undergraduate training included classes in the history and philosophy of science that disillusioned me towards the scientific process. Then my service in the United States Navy showed me the practical utility of scientific principles, and my graduate studies provided real experience in how science really works. For five years I was involved in nearly all facets of the scientific process. My adult life spans the period of the Voyager missions to the outer planets, the Viking, Pathfinder, and Global Surveyor missions to Mars, and the Pioneer and Magellan missions to Venus. These missions demonstrated the power of scientific observation. Before Voyager, we knew little about the outer planets and even less about their satellites. Even in the largest ground-based telescopes, these appeared as mere pinpoints of light. Voyager revealed them as real worlds with actual, albeit bizarre, geology. Years of speculation were dispelled in a relative moment, reminding me of the Prophet Joseph Smith’s state- ment, “Could you gaze into heaven five minutes, you would know more than you would by reading all that was written on the subject” (History I have come full of the Church, 6:50). I have come full circle, believing today that science is an important source of truth. -
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…. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
The Critique of the Principle of Uniformitarianism and the Analysis
The Critique ofthe Principle ofUniformitarianism and the Analysis of High School Earth Science Textbooks Ho Jang Song and Hui Soo An Department ojEarth Science Education, Seoul National University Although uniformitarianism is widely recognized as the basic principle upon which the structure of historical geology has been erected, a closer investigation on the basis of present scientific knowledge and the philosophy of science reveals some of its invalid aspects. The concept of uniformitarianism wasdeveloped in a dual concept in Lyellian days. Substantive uniformitarianism (a testable theory of geologic change postulating uniformity of rates or material conditions) is false, ambiguous and stifling to hypotheses formation. Methodological uniformitarianism (a procedural principle asserting that former changes of the Earth's surface may be explained by reference to causes now in operation) belongs to the defmition of science and is not unique to geology. Moreover, it also has some methodological defects in forming bold and novel working hypotheses. Methodological uniformitarianism today should take the form of a much older and more general scientific principle: Occam's Razor, the principle of simplicity. Accordingly, substantive uniformitarianism, an incorrect theory, should be abandoned. Methodological uniformi tarianism, now a superfluous term, should be best confined to the historical roles in geology. In this connection, the presentation of uniformitarianism in high school textbooks was analyzed. It was revealed that text books were riddled with false and misleading statements as to what uniformi tarianism means. Since uniformitarianism, as presented in many textbooks, is in direct contradiction to the philosophy of Inquiry learning, it is important to rethink the direction of uniformitarianism presentation in Earth Science curriculum development. -
Article James Croll – Aman‘Greater Far Than His Work’ Kevin J
Earth and Environmental Science Transactions of the Royal Society of Edinburgh,1–20, 2021 Article James Croll – aman‘greater far than his work’ Kevin J. EDWARDS1,2* and Mike ROBINSON3 1 Departments of Geography & Environment and Archaeology, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen AB24 3UF, UK. 2 McDonald Institute for Archaeological Research and Scott Polar Research Institute, University of Cambridge, Cambridge, UK. 3 Royal Scottish Geographical Society, Lord John Murray House, 15–19 North Port, Perth PH1 5LU, UK. *Corresponding author. Email: [email protected] ABSTRACT: Popular and scholarly information concerning the life of James Croll has been accumu- lating slowly since the death in 1890 of the self-taught climate change pioneer. The papers in the current volume offer thorough assessments of topics associated with Croll’s work, but this contribution seeks to provide a personal context for an understanding of James Croll the man, as well as James Croll the scho- lar of sciences and religion. Using archival as well as published sources, emphasis is placed upon selected components of his life and some of the less recognised features of his biography.These include his family history, his many homes, his health, participation in learned societies and attitudes to collegiality, finan- cial problems including the failed efforts to secure a larger pension, and friendship. Life delivered a mix- ture of ‘trials and sorrows’, but it seems clear from the affection and respect accorded him that many looked upon James Croll as a ‘man greater far than his work’. KEY WORDS: Croil–Croyle–Croll, family history, friendship, health, homes, income, learned societies, pension. -
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.