Hutton's Uniformitarianism
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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…. -
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. -
Contrastive Empiricism
Elliott Sober Contrastive Empiricism I Despite what Hegel may have said, syntheses have not been very successful in philosophical theorizing. Typically, what happens when you combine a thesis and an antithesis is that you get a mishmash, or maybe just a contradiction. For example, in the philosophy of mathematics, formalism says that mathematical truths are true in virtue of the way we manipulate symbols. Mathematical Platonism, on the other hand, holds that mathematical statements are made true by abstract objects that exist outside of space and time. What would a synthesis of these positions look like? Marks on paper are one thing, Platonic forms an other. Compromise may be a good idea in politics, but it looks like a bad one in philosophy. With some trepidation, I propose in this paper to go against this sound advice. Realism and empiricism have always been contradictory tendencies in the philos ophy of science. The view I will sketch is a synthesis, which I call Contrastive Empiricism. Realism and empiricism are incompatible, so a synthesis that merely conjoined them would be a contradiction. Rather, I propose to isolate important elements in each and show that they combine harmoniously. I will leave behind what I regard as confusions and excesses. The result, I hope, will be neither con tradiction nor mishmash. II Empiricism is fundamentally a thesis about experience. It has two parts. First, there is the idea that experience is necessary. Second, there is the thesis that ex perience suffices. Necessary and sufficient for what? Usually this blank is filled in with something like: knowledge of the world outside the mind. -
1 1 Catastrophism, Uniformitarianism, and a Scientific
1 Catastrophism, Uniformitarianism, and a Scientific Realism Debate That Makes a Difference P. Kyle Stanford ([email protected]) Department of Logic and Philosophy of Science UC Irvine Abstract Some scientific realists suggest that scientific communities have improved in their ability to discover alternative theoretical possibilities and that the problem of unconceived alternatives therefore poses a less significant threat to contemporary scientific communities than it did to their historical predecessors. I first argue that the most profound and fundamental historical transformations of the scientific enterprise have actually increased rather than decreased our vulnerability to the problem. I then argue that whether we are troubled by even the prospect of increasing theoretical conservatism in science should depend on the position we occupy in the ongoing debate concerning scientific realism itself. Acknowledgements I would like to acknowledge useful discussions concerning the material in this paper with Kevin Zollman, Penelope Maddy, Jeff Barrett, Pat Forber, Peter Godfrey-Smith, Steve Shapin, Fred Kronz, John Norton, Michael Weisberg, Jane Maienschein, Julia Bursten, Carole Lee, and Arash Pessian, as well as audiences at the Durham University Conference on Unconceived Alternatives and Scientific Realism, the University of Vienna’s (Un)Conceived Alternatives Symposium, the University of Pittsburgh’s Conference on Choosing the Future of Science, Lingnan University’s ‘Science: The Real Thing?’ Conference, the American Association for the Advancement of Science, Cambridge University, the University of Vienna, the University of Pennsylvania, UC San Diego, the University of Washington, the University of Western Ontario, the Pittsburgh Center for the Philosophy of Science, Washington University in St. Louis, Bloomsburg University, Indiana University, the Universidad Nacional Autónoma de México, and the Australian National University. -
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”). -
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. -
Ctor Vr Tniiosop >F-Phir6
SCIENTIFIC PROGRESS AND THE PROBLEM OF REALISM ABSTRACT SUBMITTElUBMITTEDFC.A F^R. TH, E A\gt&E£OF.TH,.-,_. ^- E DgQRE, E OF ctor V>f-phirr Tniioso6 p Under the Supervision of Mr. Mohammad Muqim DEPARTMENT OF PHILOSOPHY ALIGARH MUSLIM UNIVERSITY ALIGARH-202002 (INDIA) 2005 Abstract Scientific progress is a fact of history. The instances of this fact can be traced from Ptolemy to Copernicus, Newton to Einstein, Wave theor}' of Hght to Corpuscular theory. Priestley to Lavoisier, etc. However, the fact of scientific progress entails an ^enquiry.--irtto the pattern of scientific progress vv'hich pattern further necessitates an examination of the position of truth in the onward march of history of science. For. understanding of the position of truth follows from the understanding of pattern of progress. The present topic : 'Scientific Progress and the Problem of Realism" is an attempt to understand the pattern of scientific progress and the status of truth in the changing scientific or theoretical discourse. However, the pattern of progress depends on the nature of theories. In other words, nature of theories indicates the pattern of progress and, in its turn, the pattern of progress indicates the position of truth in it. Accordingly, the research embodied in this thesis is carried out on the views of five considerably different philosophers of science : Karl R. Popper, Thomas S. Kuhn, hnre Lakatos. Larry Laudan and Stephen Toulmin. The present work is comprised of the following eight chapters : 1. Introduction 2. Understanding Theory and Theory-change 3. The Aim of Progress and the Falsifiable Hypothesis. -
Two Letters from John Herschel to Charles Lyell, 1836-1837 Author(S): Walter F
The Impact of Uniformitarianism: Two Letters from John Herschel to Charles Lyell, 1836-1837 Author(s): Walter F. Cannon Source: Proceedings of the American Philosophical Society, Vol. 105, No. 3 (Jun. 27, 1961), pp. 301-314 Published by: American Philosophical Society Stable URL: http://www.jstor.org/stable/985457 Accessed: 28-06-2018 03:03 UTC REFERENCES Linked references are available on JSTOR for this article: http://www.jstor.org/stable/985457?seq=1&cid=pdf-reference#references_tab_contents You may need to log in to JSTOR to access the linked references. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms American Philosophical Society is collaborating with JSTOR to digitize, preserve and extend access to Proceedings of the American Philosophical Society This content downloaded from 150.135.165.81 on Thu, 28 Jun 2018 03:03:33 UTC All use subject to http://about.jstor.org/terms THE IMPACT OF UNIFORMITARIANISM Two Letters from John Herschel to Charles Lyell, 1836-1837 WALTER F. CANNON Assistant Professor of History, University of California, Berkeley I. INTRODUCTION how new species are generated. Lyell himself CHARLES DARWIN began the Introduction to was too fearful of orthodox Christian opinion to On the Origin of Species by saying that his ob- assert a naturalistic origin of species in the Prin- servations in South America "seemed to throw ciples, especially as he could specify no mechanism whereby such generation could take place. -
Five Decades of Structure: a Retrospective View*
Five Decades of Structure : A Retrospective View * Juan V. MAYORAL Received: 18.6.2012 Final version: 30.7.2012 BIBLID [0495-4548 (2012) 27: 75; pp. 261-280] ABSTRACT: This paper is an introduction to the special issue commemorating the 50th anniversary of the publication of The Structure of Scientific Revolutions by Thomas Kuhn. It introduces some main ideas of Structure , as its change in historical perspective for the interpretation of scientific progress, the role and nature of scientific communities, the incommensurability concept, or the new-world problem, and summarizes some philo- sophical reactions. After this introduction, the special issue includes papers by Alexander Bird, Paul Hoyningen-Huene and George Reisch on different aspects of Kuhn’s work. Keywords: Kuhn; structure; paradigms; normal science; scientific revolutions. RESUMEN: Este artículo es una introducción al número monográfico que conmemora el 50º aniversario de la publi- cación de La estructura de las revoluciones científicas de Thomas Kuhn. En la introducción se presentan algunas de las ideas principales del libro, como su cambio de perspectiva histórica para la interpretación del progre- so científico, el papel y naturaleza de las comunidades científicas, el concepto de inconmensurabilidad o el problema del cambio de mundo, y se resumen algunas reacciones filosóficas a las mismas. Tras la introduc- ción, el número monográfico está compuesto por artículos de Alexander Bird, Paul Hoyningen-Huene y George Reisch que versan sobre diversos aspectos de la obra de Kuhn. Palabras clave: Kuhn; estructura; paradigmas; ciencia normal; revoluciones científicas. 1. Introduction The Structure of Scientific Revolutions ranks high among the most significant books in twentieth-century philosophy of science. -
The Basics of Geomorphology: Key Concepts
THE BASICS OF GEOMORPHOLOGY: KEY CONCEPTS Supporting Website Material This website provides material to supplement the text and is organized by chapter with the complete reference list given at the end. Diagrams and tables that are essential for understanding the text are contained in the book. For each chapter the synopsis is given together with additional material, which includes figures and tables, compiled to amplify the dis- cussion in the text, relevant articles in Progress in Physical Geography, which is an excellent resource to pursue particular themes, and a list of the concepts given in bold from the index (together with the references cited in each chapter). The complete reference list is given at the end. 1 Introduction: Concepts and Geomorphology Any discipline has concepts that are key for its progress. For geomorphol- ogy these need to be explicitly stated and consistently understood for what they are. We set them within the evolving history of geomorphology and the changing techniques and understanding that have been involved. This demonstrates the fashioning surges that have characterized the discipline and which complicate identification of those concepts which endure and which remain basic to the present and future study of geomorphology. Figure 1.1 Grand Canyon (from near Powell Memorial) Table 1.1 Some developments in constructing geomorphology (years in italics refer to use of the word ‘geomorphology’) Year Contribution 1674 Pierre Perrault’s (1608–1680) published book on De l’origine des fontaines, showing precipitation sufficient to sustain the flow of rivers in the Seine basin: probably a foundation for understanding of the hydrological cycle. -
Contributions to the History of Geomorphology and Quaternary Geology: an Introduction
Downloaded from http://sp.lyellcollection.org/ by guest on October 1, 2021 Contributions to the history of geomorphology and Quaternary geology: an introduction DAVID R. OLDROYD1 & RODNEY H. GRAPES2 1School of History and Philosophy, The University of New South Wales, Sydney, NSW 2052, Australia (e-mail: [email protected]) 2Department of Earth and Environmental Sciences, Korea University, Seoul, 136-701, Korea (e-mail: [email protected]) This Special Publication deals with various aspects the Baltic States in 2006, where a great deal of of the histories of geomorphology and Quaternary what the geologist sees consists of Quaternary geology in different parts of the world. Geomor- sediments. However, much of the Earth’s surface phology is the study of landforms and the processes is not formed of these sediments but of older that shape them, past and present. Quaternary rocks exposed at the surface by erosion and struc- geology studies the sediments and associated tural displacement. Here, geomorphology can seek materials that have come to mantle much of answers to questions regarding the past histories of Earth’s surface during the relatively recent Pleisto- these rocks, their subsequent erosion, and present cene and Holocene epochs. Geomorphology, with location and form. Geomorphology also raises its concern for Earth’s surface features and pro- questions, and may provide answers, regarding tec- cesses, deals with information that is much more tonic issues, for example from deformed marine amenable to observation and measurement than is terraces and offset fault systems. In all these the case for most geological work. Quaternary instances, the history of geological and geomor- geology focuses mostly, but not exclusively, on phological investigations can serve to illustrate the Earth’s surficial sedimentary cover, which is both the progress and pitfalls involved in the scien- usually more accessible than the harder rocks of tific understanding of the Earth’s surface and the deeper past.