The Smart City Develops on Geology: Comparing Rome and Naples
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Planetary Geology (Part of Chapter 9): General Processes Affecting the Terrestrial Planets (And the Moon)
Planetary Geology (part of Chapter 9): General Processes Affecting the Terrestrial Planets (and the Moon) Many geological features on planetary surfaces are shaped by processes within the planet’s interior. The interior of a terrestrial world is divided into three layers of differing densities and chemical compositions: core of high-density metal, mantle of moderate- density rock, and crust of low-density rock. Although we see molten rock (lava) coming out of the Earth, only a thin layer near the top of the mantle is partially molten. However, the solid rock within planets can flow like a liquid over periods of millions of years at speeds of around 1 cm per year. The crust and very top part of the mantle do not deform or flow easily, they are called the lithosphere. The thickness of a planet’s lithosphere affects how easily it can be fractured and rearranged into mountains and valleys, and how easily lava can be erupted onto the surface. Interior heat causes geological activity. Terrestrial worlds were heated during their formation due to accretion and differentiation, and are still heated today by radioactive decay. They are slowly cooling down, with heat moving up through the mantle by convection, up through the crust by conduction, and radiating out to space. Larger planets retain heat for longer than smaller planets, so larger planets are more geologically active. If a rapidly-rotating planet contains a layer of electrically conducting fluid, such as a liquid metal core, then it will have a magnetic field. This magnetic field can protect its atmosphere from the solar wind. -
GEOLOGY What Can I Do with This Major?
GEOLOGY What can I do with this major? AREAS EMPLOYERS STRATEGIES Some employment areas follow. Many geolo- gists specialize at the graduate level. ENERGY (Oil, Coal, Gas, Other Energy Sources) Stratigraphy Petroleum industry including oil and gas explora- Geologists working in the area of energy use vari- Sedimentology tion, production, storage and waste disposal ous methods to determine where energy sources are Structural Geology facilities accumulated. They may pursue work tasks including Geophysics Coal industry including mining exploration, grade exploration, well site operations and mudlogging. Geochemistry assessment and waste disposal Seek knowledge in engineering to aid communication, Economic Geology Federal government agencies: as geologists often work closely with engineers. Geomorphology National Labs Coursework in geophysics is also advantageous Paleontology Department of Energy for this field. Fossil Energy Bureau of Land Management Gain experience with computer modeling and Global Hydrogeology Geologic Survey Positioning System (GPS). Both are used to State government locate deposits. Consulting firms Many geologists in this area of expertise work with oil Well services and drilling companies and gas and may work in the geographic areas Oil field machinery and supply companies where deposits are found including offshore sites and in overseas oil-producing countries. This industry is subject to fluctuations, so be prepared to work on a contract basis. Develop excellent writing skills to publish reports and to solicit grants from government, industry and private foundations. Obtain leadership experience through campus organi- zations and work experiences for project man- agement positions. (Geology, Page 2) AREAS EMPLOYERS STRATEGIES ENVIRONMENTAL GEOLOGY Sedimentology Federal government agencies: Geologists in this category may focus on studying, Hydrogeology National Labs protecting and reclaiming the environment. -
Biosphere 2 (B2) PI: Katerina Dontsova, Phd Co-PI: Kevin Bonine, Phd Sponsors: National Science Foundation Research Experiences for Undergraduates (NSF REU) Program
Biosphere 2 (B2) PI: Katerina Dontsova, PhD Co-PI: Kevin Bonine, PhD Sponsors: National Science Foundation Research Experiences for Undergraduates (NSF REU) Program BIOSPHERE 2 (B2) Kierstin Acuña The effect of nanochitosan on piñon pine (Pinus edulis) seedling mortality in heatwave conditions University of Maryland, Environmental Science and Policy Mentor: Dr. Dave Breshears, Jason Field and Darin Law – School of Natural Resources and the Environment Abstract Semiarid grasslands worldwide are facing woody plant encroachment, a process that dramatically alters carbon and nutrient cycling. This change in plant types can influence the function of soil microbial communities with unknown consequences for soil carbon cycling and storage. We used soils collected from a five-year passive warming experiment in Southern, AZ to test the effects of warming and substrate availability on microbial carbon use. We hypothesized that substrate addition would increase the diversity of microbial substrate use, and that substrate additions and warming would increase carbon acquisition, creating a positive feedback on carbon mineralization. Community Level Physiological Profiling (CLPP) of microbial activity was conducted using Biolog EcoPlateTMassays from soils collected in July 2018, one week after the start of monsoon rains. Two soil types common to Southern AZ, were amended with one of four treatments (surface juniper wood chips, juniper wood chips incorporated into the soil, surface biochar, or a no-amendment control) and were randomly assigned to a warmed or ambient temperature treatment. We found that surface wood chips resulted in the highest richness and diversity of carbon substrate use with control soils yielding the lowest. Substrate use was positively correlated with the total organic carbon but not with warming. -
Weathering, Erosion, and Susceptibility to Weathering Henri Robert George Kenneth Hack
Weathering, erosion, and susceptibility to weathering Henri Robert George Kenneth Hack To cite this version: Henri Robert George Kenneth Hack. Weathering, erosion, and susceptibility to weathering. Kanji, Milton; He, Manchao; Ribeira e Sousa, Luis. Soft Rock Mechanics and Engineering, Springer Inter- national Publishing, pp.291-333, 2020, 9783030294779. 10.1007/978-3-030-29477-9. hal-03096505 HAL Id: hal-03096505 https://hal.archives-ouvertes.fr/hal-03096505 Submitted on 5 Jan 2021 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. Published in: Hack, H.R.G.K., 2020. Weathering, erosion and susceptibility to weathering. 1 In: Kanji, M., He, M., Ribeira E Sousa, L. (Eds), Soft Rock Mechanics and Engineering, 1 ed, Ch. 11. Springer Nature Switzerland AG, Cham, Switzerland. ISBN: 9783030294779. DOI: 10.1007/978303029477-9_11. pp. 291-333. Weathering, erosion, and susceptibility to weathering H. Robert G.K. Hack Engineering Geology, ESA, Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente Enschede, The Netherlands e-mail: [email protected] phone: +31624505442 Abstract: Soft grounds are often the result of weathering. Weathering is the chemical and physical change in time of ground under influence of atmosphere, hydrosphere, cryosphere, biosphere, and nuclear radiation (temperature, rain, circulating groundwater, vegetation, etc.). -
Planetary Geology GEOLOGY 307 Spring 2018 Tuesday & Thursday 9:30 -10:50 A.M
Planetary Geology GEOLOGY 307 Spring 2018 Tuesday & Thursday 9:30 -10:50 a.m. C. M. Bailey Office- McStreet Hall 215 x12445 [email protected] Preamble Space, the Final Frontier! Although the Earth provides a rich tapestry for geologists, other planetary bodies in our Solar System are equally worthy of study. Many of the same processes that operate on Earth modify these worlds, but each planet is unique in many respects. Planetary bodies also contain a record of the solar system’s history. The goals of this course include a better understanding of the processes that operate on distant worlds, gaining insight into how the Solar System has changed through time, and thinking about the future opportunties in planetary science. This class will not simply be a tour of the planets, nor will it attempt to answer all the questions normally dealt with in Astronomy and Cosmology courses. We will start from observations and use a judicious amount of mathematics, physics, and chemistry to achieve our goals. At semester’s end we hope you will have developed an understanding of the Solar System, a sense for the new and exciting discoveries in planetary science, as well as an appreciation of the important questions still to be answered. Week Dates Topic Readings 1 Jan. 18 Planetary Geology Introduced WHOOPS! Ch. 1 2 Jan. 23, 25 Planetary Geology Introduced Ch. 1 The Universe: matter, stars, planets, and life- oh my! 3 Jan. 30, Feb. 1 Celestial Mechanics Ch. 2 Ch. 5, pg. 64-67 4 Feb. 6, 8 Solar System Formation Meteorites are Mighty Important 5 Feb. -
Geomorphology and Environmental Geology the Luckiamute Watershed, Central Coast Ranggge, Oregon
Geomorphology and Environmental Geology the Luckiamute Watershed, Central Coast Ranggge, Oregon Greenbelt Land Trust Luckiamute Watershed Council Western Oregon University Field Guide May 10, 2014 123 37.5 123 30 123 22.5 123 15 Dallas West Salem 5 4 44 52.5 Monmouth te ckiamu Little Lu e g n 3 a R Falls 1 City Independence y e 2 l l Pee r a r Helmick e V e Dee iv iv R Sta te e R ut m Park 44 45 ia 99W ck Lu s g n i K 223 k e t e r s C a p o a o C S 44 37.5 Corvallis 34 Albany Blodgett Wren e t Luckiamute Watershed t e Boundary m N la Western Oregon Univ. il 20 W Field Trip Stop Philomath 5 0 5 km Prepared By: Steve Taylor, Ph.D., Professor of Geology Earth and Physical Science Department Chair, Division of Natural Sciences and Mathematics Western Oregon University Monmouth, Oregon 97361 Email: [email protected] Table of Contents TOPIC PAGE Introduction 1-6 Physiographic Setting 7-12 Tectonic Setting 13-16 Bedrock Geology 17-23 Geomorphology Regional Overview 24-28 Geomorphic Research Results 29-35 Vegetation and Invasive Plant Distribution Introduction 36-41 Methodology 42 Invasive Research Results 43-52 Field Trip Stop Summaries and Maps Helmick State Park 55-60 NOTE: Selected pages omitted / recycled from a previous field trip. Field Trip Introduction •People •Introductions •Organizations •Western Oregon University (Earth Science) •Luckiamute Watershed Council •Greenbelt Land Trust •Background •Luckiamute Watershed – Focus of 2001 WOU Environmental Science Institute Course •Undergraduate Science Majors •Pre-service Science Education Majors -
Engineering Geology and Seismology for Public Schools and Hospitals in California
The Resources Agency California Geological Survey Michael Chrisman, Secretary for Resources Dr. John G. Parrish, State Geologist Engineering Geology and Seismology for Public Schools and Hospitals in California to accompany California Geological Survey Note 48 Checklist by Robert H. Sydnor, Senior Engineering Geologist California Geological Survey www.conservation.ca.gov/cgs July 1, 2005 316 pages Engineering Geology and Seismology performance–based analysis, diligent subsurface for Public Schools and Hospitals sampling, careful reading of the extensive geologic in California literature, thorough knowledge of the California Building Code, combined with competent professional geological work. by Robert H. Sydnor Engineering geology aspects of hospital and public California Geological Survey school sites include: regional geology, regional fault July 1, 2005 316 pages maps, site-specific geologic mapping, geologic cross- sections, active faulting, official zones of investigation Abstract for liquefaction and landslides, geotechnical laboratory The 446+ hospitals, 1,400+ skilled nursing facilities testing of samples, expansive soils, soluble sulfate ±9,221 public schools, and 109 community college evaluation for Type II or V Portland-cement selection, campuses in California are regulated under California and flooding. Code of Regulations, Title 24, California Building Code. Seismology aspects include: evaluation of historic These facilities are plan–checked by senior–level seismicity, probabilistic seismic hazard analysis of Registered Structural Engineers within the Office of earthquake ground–motion, use of proper code terms Statewide Health Planning and Development (OSHPD) (Upper–Bound Earthquake ground–motion and Design– for hospitals and skilled nursing facilities, and the Basis ground–motion), classification of the geologic Division of the State Architect (DSA) for public schools, subgrade by shear–wave velocity to select the correct community colleges, and essential services buildings. -
Principles of Engineering Geology Principles of Engineering Geology
PRINCIPLES OF ENGINEERING GEOLOGY PRINCIPLES OF ENGINEERING GEOLOGY P. B. ATTEWELL and I. W. FARMER University of Durham LONDON CHAPMAN AND HALL A Halsted Press Book JOHN WILEY & SONS, INC., NEW YORK First published 1976 by Chapman and Hall Ltd 11 New Fetter Lane, London EC4P 4EE © 1976 J. E. Attewell and L. C. Attewell Sriftcover reprillt rifthe hardcover 1ft editiolt 1976 Typeset by Preface Ltd, Salisbury, Wilts Fletcher & Son Ltd, Norwich ISBN-13: 978-94-009-5709-1 e-ISBN-13: 978-94-009-5707-7 DOl: 10.1007/978-94-009-5707-7 All rights reserved. No part of this book may be reprinted, or reproduced or utilized in any form or by any electronic, mechanical or other means, now known or hereafter invented, including photocopying and recording, or in any information storage and retrieval system, without permission in writing from the Publisher. Distributed in the U.S.A. by Halsted Press, a Division of John Wiley & Sons, Inc., New York Library of Congress Cataloging in Publication Data Attewell, P B Principles of engineering geology. 1. Engineering geology. I. Farmer, Ian William, joint author. II. Title. TA705.A87 1975 624'151 75-20012 Contents Preface xi Symbols xvii Composition of Rocks 1 1.1 Origin and geological classification of rocks 1 1.2 Rock forming minerals 7 1.3 Clay minerals 16 1.4 Base exchange and water adsorption in clay minerals 20 1.5 Mineralogical identification 25 2 Rock Particles and Particle Systems 30 2.1 Rock particle classification 30 2.2 Typical rock particle systems 33 2.3 Physical properties of particulate systems -
A Geologist Views the Environment
ILLINOIS STATE GEOLOGICAL SURVEY 3 3051 00005 3805 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/geologistviewsen42frye EGN 42 557 I16e no. 42 c. 1 ENVIRONMENTAL GEOLOGY NOTES FEBRUARY 1971 • NUMBER 42 A GEOLOGIST VIEWS THE ENVIRONMENT John C. Frye ILLINOIS STATE GEOLOGICAL SURVEY JOHN C. FRYE, Chief • Urbana 61801 A GEOLOGIST VIEWS THE ENVIRONMENT' John C. Frye When the geologist considers the environment, and particularly when he is concerned with the diversified relations of man to his total physical environment, he takes an exceptionally broad and long-term view. It is broad because all of the physical features of the earth are the subject matter of the geologist. It is long term because the geologist views the environment of the moment as a mere point on a very long time-continuum that has witnessed a succession of physical and biological changes—and that at present is dynam- ically undergoing natural change. Let us first consider the time perspective of the geologist, then consider the many physical factors that are important to man's activity on the face of the earth, and, third, turn our attention to specific uses of geologic data for the maintenance or development of an environment that is compatible with human needs. THE LONG VIEW The earth is known to be several billion years old, and the geologic record of physical events and life-forms on the earth is reasonably good for more than the most recent 500 million years. Throughout this span of known time the environment has been constantly changing— sometimes very slowly, but at other times quite rapidly. -
Mars Field Geology, Biology, and Paleontology Workshop, Summary
MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston, Houston, Texas LPI Contribution No. 968 MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston Edited by Nancy Ann Budden Lunar and Planetary Institute Sponsored by Lunar and Planetary Institute National Aeronautics and Space Administration Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 968 Compiled in 1999 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautcis and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This volume may be cited as Budden N. A., ed. (1999) Mars Field Geology, Biology, and Paleontology Workshop: Summary and Recommendations. LPI Contribution No. 968, Lunar and Planetary Institute, Houston. 80 pp. This volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling. _________________ Cover: Mars test suit subject and field geologist Dean Eppler overlooking Meteor Crater, Arizona, in Mark III Mars EVA suit. PREFACE In November 1998 the Lunar and Planetary Institute, under the sponsorship of the NASA/HEDS (Human Exploration and Development of Space) Enterprise, held a workshop to explore the objectives, desired capabilities, and operational requirements for the first human exploration of Mars. -
Burlington House Fire Safety Information
William Smith Meeting 2015 (Part 2) 5 November 2015 200 Years and Beyond: The future of geological mapping Contents Page 2 Acknowledgements Page 3 Conference Programme Page 5 Speaker Biographies and Abstracts Page 29 Poster Abstracts Page 40 Burlington House Fire Safety Information Page 41 Ground Floor Plan of the Geological Society, Burlington House @geolsoc #wsmith15 #williamsmith200 Page 1 William Smith Meeting 2015 (Part 2) 5 November 2015 200 Years and Beyond: The future of geological mapping WELCOME FROM THE CONVENORS In 1815 William Smith published the first edition of his Geological Map of England and Wales. Smith’s map made a seminal contribution to the understanding of the ground beneath our feet and, by showing the location of coal, iron ore, clays and other raw materials, helped fuel the industrial revolution. Two hundred years on, the demands for spatial knowledge about our geological environment and its resources and hazards have become ever more diverse and pressing. Nevertheless, many of the motivators, approaches and principles pioneered by William Smith survive in the geological maps, models and information systems of today. The History of Geology Group and the British Geological Survey have worked together to convene two William Smith meetings at the Geological Society in 2015 to celebrate this landmark anniversary. The first, very successful meeting in April 2015, convened by HOGG, chronicled the history and development of the geological map from its earliest beginnings to the digital maps of today. This second meeting, convened by the BGS, looks to the future of geological mapping, and to the grand challenges for geoscience that will motivate the ‘William Smiths’ of tomorrow. -
Popularizing Geological Education Among Civil Engineering Students Chen Xiang-Jun1,A and Zhou Ying2
JOURNAL OF GEOSCIENCE EDUCATION 60, 228–233 (2012) Popularizing Geological Education Among Civil Engineering Students Chen Xiang-jun1,a and Zhou Ying2 ABSTRACT The sustainable development of an economy and a society cannot be realized without the help of modern geoscience. Engineering geology knowledge is necessary on a civil engineering construction site to ensure the construction work goes smoothly. This paper first discusses the importance of geoscience, especially the study of engineering geology. Then, the current Chinese engineering geology course for civil engineering students is summarized. The engineering geology course at Shijiazhuang Tiedao University is described in detail, including its history, its content, and some teaching tactics for the course. The paper closes with an evaluation of the effects of the teaching tactics. Ó 2012 National Association of Geoscience Teachers. [DOI: 10.5408/10-207.1] Key words: engineering geology, civil engineering IMPORTANCE OF GEOLOGICAL STUDY geological science can tell humans how to exploit and utilize On 19 June 2007, Chinese Prime Minister Wen Jia-bao, resources reasonably, reduce consumption of resources, who is also a geologist, expounded on the importance of reduce environmental damage, and prevent geological geological study when he talked with officials of the hazards. The harmony between Earth and humans funda- International Union of Geological Sciences. The prime mentally depends on the progress of geology. Improving the minister said he believes that the tasks of modern geoscience, level of geological research can help humans face the which is closely connected with the economy, society, and challenges of energy scarcity, environment destruction, environment, are to support the sustainable development of natural disasters, and so on.