Celebrating the Age of the Earth
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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…. -
An Investigation Into the Graphic Innovations of Geologist Henry T
Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School 2003 Uncovering strata: an investigation into the graphic innovations of geologist Henry T. De la Beche Renee M. Clary Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Education Commons Recommended Citation Clary, Renee M., "Uncovering strata: an investigation into the graphic innovations of geologist Henry T. De la Beche" (2003). LSU Doctoral Dissertations. 127. https://digitalcommons.lsu.edu/gradschool_dissertations/127 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. UNCOVERING STRATA: AN INVESTIGATION INTO THE GRAPHIC INNOVATIONS OF GEOLOGIST HENRY T. DE LA BECHE A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Curriculum and Instruction by Renee M. Clary B.S., University of Southwestern Louisiana, 1983 M.S., University of Southwestern Louisiana, 1997 M.Ed., University of Southwestern Louisiana, 1998 May 2003 Copyright 2003 Renee M. Clary All rights reserved ii Acknowledgments Photographs of the archived documents held in the National Museum of Wales are provided by the museum, and are reproduced with permission. I send a sincere thank you to Mr. Tom Sharpe, Curator, who offered his time and assistance during the research trip to Wales. -
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. -
The Geological Revolution: Deep Time and the Age of the Earth
Lecture 6: The Geological Revolution: Deep Time and the Age of the Earth Astronomy 141 – Winter 2012 This lecture explores the geological revolution that revealed the antiquity of the Earth. Understanding the age of the Earth requires having a conception of a beginning for the Earth. Historical and Physical age estimates give different answers. Geological discoveries uncovered the deep history of the Earth, and developed techniques for reading that history. The Earth is 4.54 ± 0.05 Billion Years old, measured by radiometric age dating of meteorites, the oldest Earth rocks, and Moon rocks. In order for “what is the age of the Earth?” to make sense, you must conceive of a beginning. Two ways people have conceived of time: Cyclical Time: Earth has no beginning or end, only repeated cycles of birth, death, and rebirth/renewal. Linear Time: Earth has a past beginning & will have a future end. On human scales, time appears to be cyclical Natural cycles around us: Cycle of day & night Monthly cycle of moon phases Yearly cycle of the seasons Generational cycle of birth, life, and death... Examples: Hinduism & Buddhism posit cyclical time Plato’s 72,000 year cycle: 36,000 Golden Age followed by a 36,000 age of disorder & chaos. Linear Time posits a definite beginning in the past, and an eventual ending in the future. Judaism provides an example of linear time: Past divine creation of the Earth (Genesis) Promised end of times. Christianity & Islam adopted this idea: See history as fulfillment, not growth. No change in the world, except decay from past perfection (“fall from grace”). -
Redacted Thesis (PDF, 12Mb)
Victorian Egyptology and the Making of a Colonial Field Science, 1850 – 1906 by Meira Gold Wolfson College Department of History and Philosophy of Science This thesis is submitted for the degree of Doctor of Philosophy Date of Submission: December 2019 Declaration This thesis is the result of my own work and includes nothing which is the outcome of work done in collaboration except as declared in the Preface and specified in the text. It is not substantially the same as any that I have submitted, or, is being concurrently submitted for a degree or diploma or other qualification at the University of Cambridge or any other University or similar institution except as declared in the Preface and specified in the text. I further state that no substantial part of my thesis has already been submitted, or, is being concurrently submitted for any such degree, diploma or other qualification at the University of Cambridge or any other University or similar institution except as declared in the Preface and specified in the text. It does not exceed the prescribed word limit for the History and Philosophy of Science Degree Committee. Abstract Victorian Egyptology and the Making of a Colonial Field Science, 1850-1906 Meira Gold This dissertation provides a new account of the origins of archaeological fieldwork in the Nile Delta. It considers how practitioners from diverse disciplinary backgrounds circulated knowledge about the built environment of pharaonic ruins: monuments, architecture, burials, and soil mounds that remained in situ. I trace the development of Egyptology from an activity that could be practiced long-distance through a network of informants to one that required first-hand field experience. -
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. -
Leonard Horner: a Portrait of an Inspector of Factories
BERNICE MARTIN LEONARD HORNER: A PORTRAIT OF AN INSPECTOR OF FACTORIES Leonard Horner was the most impressive and influential of the first English factory inspectors. For 26 years from 1833 to 1859 he adminis- tered the Factory Act mainly in the textile district of Lancashire. His work and that of his colleagues in the Factory Department made a success of this major experiment in legislative intervention in industry and despite the gloomy predictions of their early opponents they did not ruin the British economy in the process. The first generation of Inspectors laid the foundation for successive extensions of the Factory Act so that by the end of the 19th century working conditions and hours of labour for women and children were under legal regulation in all the major branches of manufacturing industry. Horner was ac- knowledged by his contemporaries to be the major figure among the early Inspectors; he even had the singular honour of being praised by Marx in Capital. This short biography will concentrate on Horner's work as Inspector of Factories since this is undoubtedly his major achievement. However it will also be concerned with other aspects of his life and interests, both because these have some importance in their own right and also in order to examine the extent to which Horner's life and thought form a coherent whole. Finally, an assessment will be made of Horner's place in social reform and in the development of English economic and social policy in the 19th century. I HORNER'S EARLY LIFE AND CAREER1 Leonard Horner was born in Edinburgh in 1785. -
Hutton's Uniformitarianism
BYU Studies Quarterly Volume 23 Issue 1 Article 4 1-1-1983 Hutton's Uniformitarianism Jess R. Bushman Follow this and additional works at: https://scholarsarchive.byu.edu/byusq Recommended Citation Bushman, Jess R. (1983) "Hutton's Uniformitarianism," BYU Studies Quarterly: Vol. 23 : Iss. 1 , Article 4. Available at: https://scholarsarchive.byu.edu/byusq/vol23/iss1/4 This Article is brought to you for free and open access by the Journals at BYU ScholarsArchive. It has been accepted for inclusion in BYU Studies Quarterly by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Bushman: Hutton's Uniformitarianism huttonssuttonsHuttons uniformitarianism jess R bushman uniformitarianism or cause and effect is a very important and basic concept in geology the heart of the concept is that there is order and regularity in the operation or functioning of natural laws this consistency is what gives significance to cause and effect pat- terns what we see happening today helps us to identify the results of natural processes which were active millions of years ago we observe ripple marks being formed by wave action on beaches today when we see similar ripple marks in ancient sandstone we use cause and effect or uniformitarianism to suggest that the ripple marked sandstones were once part of an ancient beach the geologist as he studies natural processes at work and sees how long it takes to produce soil from solid rock or for a glacier to carve a U shaped valley is convinced -
Leonard Horner in Bonn and Liu Tungsheng in Beijing Tic
Open Geosci. 2018; 10:925–931 Research Article Ian Smalley* and Slobodan B. Markovic An enthusiasm for loess: Leonard Horner in Bonn and Liu Tungsheng in Beijing https://doi.org/10.1515/geo-2018-0073 tic. Liu followed determinedly in these footsteps; a great Received Jan 10, 2018; accepted Dec 18, 2018 scholar, and a great enthusiast. Loess scholarship needs careful and precise investigation Abstract: Liu Tungsheng featured on the list of twelve no- and reporting but it also needs a broad sweep of enthusi- table loess investigators prepared for the great LoessFest asm, an appreciation of loess for the extraordinary mate- meeting, held in Heidelberg and Bonn in 1999. He fully de- rial that it is. served his position on this list of eminent loess scholars; in fact it might be argued that his was the major contri- Keywords: Loess, loess investigation, loess enthusiasm, bution. His contribution was a true paradigm shift in the Leonard Horner, Liu Tungsheng world of loess investigation. Obruchev and Richthofen had produced an earlier paradigm shift when they propagated the idea that loess deposits form by aeolian deposition- a “The thick silt sediment in North China deposited by the wind paradigm shift away from the earlier Lyellian idea of la- during the dry period of the Quaternary period is unique in many custrine or fluvial deposition. But that was a fairly simple aspects. Its great thickness, wide distribution, complex develop- ment history, rich fossil contents and the characteristic topogra- shift, a tweak of the sedimentological event structure. Liu, phy it shows make it unequalled as compared with the loess de- and his co-workers in China, produced a new vision, a new posits in other parts of the world.” way of looking at loess, not so much a paradigm shift as a Liu & Chang 1964 p.523 [12] paradigm enlargement. -
Charles Darwin and John Herschel*
432 South African Journal of Science 105, November/December 2009 Research Articles Charles Darwin and John Herschel* B. Warner The influence of John Herschel on the philosophical thoughts of Charles Darwin, both through the former’s book, Natural Philosophy, and through their meeting in 1836 at the Cape of Good Hope, is discussed. With Herschel having himself speculated on evolution just a few months before he met Darwin, it is probable that he stimulated at least the beginnings of the latter’s lifelong work on the subject. : evolution, Cape of Good Hope, Charles Darwin, John Herschel He never talked much, but every word which he uttered was worth listening to. Charles Darwin, about Sir John Herschel His Majesty’s Ship Beagle, commanded by Captain Robert Fitz- Roy and carrying Charles Robert Darwin as the naturalist on board, arrived in Simon’s Bay on 31 May 1836 on the final stage of a voyage around the world that had taken four and a half years and had still another six months to go. One of FitzRoy’s duties was to check the accuracy of 22 marine chronometers, destined for use by the Royal Navy; the presence of the Royal Observatory in Cape Town gave him the finest opportunity to carry this out, with the result that the Beagle stayed in port for Charles Darwin as a young man.Watercolour by George Richmond, after the return 18 days—longer than at any other port during the circumnaviga- of the Beagle. tion (they stayed for five weeks in the Galapagos, but island- hopped). -
Sir Charles Lyell, Bart., M.A., D.C.L., Ll.D., P.K.B., P.L.S., V.P
142 Obituary—Sir Charles Lyell. OBITTTABT. SIR CHARLES LYELL, BART., M.A., D.C.L., LL.D., P.K.B., P.L.S., V.P. OEOL. SOC. LOND. ON Monday, 22nd February, at his residence in Harley Street, and in his seventy-eighth year, Sir Charles Lyell passed peacefully from amongst us, after a long life of scientific labour, to his honoured rest. To the outside world it may seem strange that the death of a man who was neither statesman, soldier, nor public orator, should arouse our sympathies so strongly, or that he should be so highly esteemed all over the world; but geologists know well what Lyell has done for them since he published the first volume of " The Principles of Geology " in 1830. It is in the character of historian and philosophical expo- nent of geological thought that Lyell has achieved so much for our science; nor can we fail to remember that those clear and advanced views, for which he became so justly celebrated, were advocated by him forty-five years ago, at a time when scientific thought was still greatly trammelled by a strong religious bias, and men did not dare to openly avow their belief in geological discoveries nor accept the only deductions which could be drawn from them. It was no small service which Lyell rendered to us when he publicly maintained that, in reasoning on geological data, it was impossible to restrict geologists to the limits of the Mosaic cosmogony, or to adopt for the past ages of geological time the chronology of Archdeacon Ussher. -
Front Matter (PDF)
THE QUARTERLY OF THE GEOLOGICAL SOCIETY OF LONDO5 EDITED BY THE ASSISTANT-SECRETARY OF THE GEOLOGICAL SOCIETY VOLUME THE FOURTEENTH. 1858. PART THE FIRST. PROCEEDINGS OF THE GEOLOGICAL SOCIETY. LONDON LONGMAN, BKOWN, GREEN, LONGMANS, AND ROBERTS. PARIS :--FRIED. KLINCKSIECK, 11 RUE DE LILLE; BAUDRY, 9 RUE DU COQ, PRES LE LOUVRE ; LEIPZIG, T. O. 'WEIGEL. SOLD AL~O AT THE APARTMENTS OF THE SOCIETY. MDCCCLVIII. OF THE OFFICERS OF THE GEOLOGICAL SOCIETY OF LONDON. Elected February 19, 1858. Professor John Phillips, M.A., LL.D., F.R.S. i~fc~re~f~mt~. John J. Bigsby, M.D. Hugh Falconer, M.D., F.R.S. Leonard Horner, Esq., F.R.S.L. & E. Sir R. I. Murchison, G.C.St.S,, F.R.S. & L.S. ~r Thomas Davidson, Esq., F.R.S. Warington W. Smyth, Esq., M.A., F.R.S. ~oreign ~creta~. WiUiam John Hamilton, Esq., F.R.S. grea~urrr. Joseph Prestwieh, Esq., F.R.S. John J. Bigsby, M.D. Prof. N. S. Maskelyne, M.A. W. J. Broderip, Esq., M.A., F.R.S. & L.S. John C. Moore, Esq., M.A., F.R.S. Prof. Charles Daubeny, M.D., F.R.S. & L.S. Sir R. I. Murchison, G.C.St.S., F.R.S. & Thomas Davidson, Esq., F.R.S. L.S. Hugh Falconer, M.D., F.R.S. Robert W. Mylne, Esq. Thomas F. Gibson, Esq. Prof. John Phillips, M.A., LL.D., F.R.S. R. A. Godwin-Austen, Esq., B.A., F.R.S. Major-General Portlock, LL.D., F.R.S.