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User Guide: Soil Parent Material 1 Kilometre Dataset
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive User Guide: Soil Parent Material 1 kilometre dataset. Environmental Modelling Internal Report OR/14/025 BRITISH GEOLOGICAL SURVEY ENVIRONMENTAL Modelling INTERNAL REPORT OR/14/025 User Guide: Soil Parent Material 1 kilometre dataset. The National Grid and other Ordnance Survey data © Crown Copyright and database rights 2012. Ordnance Survey Licence R. Lawley. No. 100021290. Keywords Contributor/editor Parent Material, Soil,UKSO. B. Rawlins. National Grid Reference SW corner 999999,999999 Centre point 999999,999999 NE corner 999999,999999 Map Sheet 999, 1:99 000 scale, Map name Front cover Soil Parent Material 1km dataset. Bibliographical reference LAWLEY., R. USER GUIDE: SOIL PARENT Material 1 Kilometre dataset. 2012. User Guide: Soil Parent Material 1km dataset.. British Geological Survey Internal Report, OR/14/025. 20pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, email [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NERC 2014. All rights reserved Keyworth, Nottingham British Geological Survey 2012 BRITISH GEOLOGICAL SURVEY The full range of our publications is available from BGS shops at British Geological Survey offices Nottingham, Edinburgh, London and Cardiff (Welsh publications only) see contact details below or shop online at www.geologyshop.com BGS Central Enquiries Desk Tel 0115 936 3143 Fax 0115 936 3276 The London Information Office also maintains a reference collection of BGS publications, including maps, for consultation. -
Lecture 13: Earth Materials
Earth Materials Lecture 13 Earth Materials GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Hooke’s law of elasticity Force Extension = E × Area Length Hooke’s law σn = E εn where E is material constant, the Young’s Modulus Units are force/area – N/m2 or Pa Robert Hooke (1635-1703) was a virtuoso scientist contributing to geology, σ = C ε palaeontology, biology as well as mechanics ij ijkl kl ß Constitutive equations These are relationships between forces and deformation in a continuum, which define the material behaviour. GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Shear modulus and bulk modulus Young’s or stiffness modulus: σ n = Eε n Shear or rigidity modulus: σ S = Gε S = µε s Bulk modulus (1/compressibility): Mt Shasta andesite − P = Kεv Can write the bulk modulus in terms of the Lamé parameters λ, µ: K = λ + 2µ/3 and write Hooke’s law as: σ = (λ +2µ) ε GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Young’s Modulus or stiffness modulus Young’s Modulus or stiffness modulus: σ n = Eε n Interatomic force Interatomic distance GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Shear Modulus or rigidity modulus Shear modulus or stiffness modulus: σ s = Gε s Interatomic force Interatomic distance GNH7/GG09/GEOL4002 EARTHQUAKE SEISMOLOGY AND EARTHQUAKE HAZARD Hooke’s Law σij and εkl are second-rank tensors so Cijkl is a fourth-rank tensor. For a general, anisotropic material there are 21 independent elastic moduli. In the isotropic case this tensor reduces to just two independent elastic constants, λ and µ. -
Earth Materials Summary
GRADES 3–4 OVERVIEW EARTH MATERIALS GOALS The Earth Materials Module consists of four sequential investigations dealing with observable characteristics of solid materials from the earth—rocks and minerals. The focus is on taking materials apart to ○○○○○ find what they are made of and putting materials together to better ○○○○○○○○○○○ understand their properties. The module introduces fundamental OVERVIEW CONTENTS concepts in earth science and takes advantage of the students’ Goals 1 intrinsic interest in the subject matter and in the physical world FOSS and National Science around them. Education Standards 2 FOSS EXPECTS STUDENTS TO Science Background 3 • Develop an interest in earth materials. Working in Collaborative • Gain experiences with rocks and minerals. Groups 8 • Understand the process of taking apart and putting together Encouraging Discourse 9 to find out about materials. Guiding FOSS Investigations 10 • Use measuring tools to gather data about rocks. Assessing Progress 11 • Collect and organize data about rocks. Integrating the Curriculum 12 • Observe, describe, and record properties of minerals. FOSS for All Students 13 •Organize minerals on the basis of the property of hardness. The FOSS Teacher Guide • Investigate the effect of vinegar (acid) on a specific mineral, Organization 14 calcite. The FOSS Investigation Folio • Use evaporation to investigate rock composition. Organization 15 • Learn that rocks are composed of minerals and that minerals Scheduling the Earth cannot be physically separated into other materials. Materials Module 16 • Compare their activities to the work of a geologist. Safety in the Classroom 17 • Acquire vocabulary used in earth science. Earth Materials Module • Exercise language and math skills in the context of science. -
Earth Materials
Grade 4 Science, Quarter 1, Unit 1 Earth Materials Overview Number of instructional days: 10 (1 day = 45 minutes) Content to be learned Science processes to be integrated • Identify the four basic materials of the earth • Use physical properties to describe, compare, (water, soil, rocks, air). and sort objects. • Describe, compare, and sort rocks, soils, and • Make, record, and analyze observations and minerals by similar and different physical data. properties. • Cite evidence to support classification of • Record and analyze observations/data about objects. physical properties. • Identify and determine the uses of materials • Cite evidence to support why rocks, soils, or based on their physical properties. minerals are or are not classified together. • Support explanations using observations and • Determine and support explanations of the uses data. of earth materials. Essential questions • In what ways can we identify, describe, sort, • How can we use earth materials? and classify earth materials? Bristol-Warren, Little Compton, Portsmouth, Tiverton Public Schools, C-1 in collaboration with the Charles A. Dana Center at the University of Texas at Austin Grade 4 Science, Quarter 1, Unit 1 Earth Materials (10 days) Written Curriculum Grade-Span Expectations ESS1 - The earth and earth materials as we know them today have developed over long periods of time, through continual change processes. ESS1 (K-4) INQ –1 Given certain earth materials (soils, rocks or minerals) use physical properties to sort, classify, and describe them. ESS1 (3-4) –1 Students demonstrate an understanding of earth materials by … 1d identifying the four basic materials of the earth (water, soil, rocks, air). 1a describing, comparing, and sorting rocks, soils, and minerals by similar or different physical properties (e.g., size, shape, color, texture, smell, weight, temperature, hardness, composition). -
Geomorphic Processes
CHAPTER GEOMORPHIC PROCESSES fter learning about how the earth was forces continuously elevate or build up parts born, how it evolved its crust and other of the earth’s surface and hence the exogenic Ainner layers, how its crustal plates processes fail to even out the relief variations moved and are moving, and other information of the surface of the earth. So, variations remain on earthquakes, the forms of volcanism and as long as the opposing actions of exogenic and about the rocks and minerals the crust is endogenic forces continue. In general terms, composed of, it is time to know in detail about the endogenic forces are mainly land building the surface of the earth on which we live. Let forces and the exogenic processes are mainly us start with this question. land wearing forces. The surface of the earth is sensitive. Humans depend on it for their Why is the surface of the earth uneven? sustenance and have been using it extensively and intensively. So, it is essential to understand The earth’s crust is dynamic. You are well its nature in order to use it effectively without aware that it has moved and moves vertically disturbing its balance and diminishing its and horizontally. Of course, it moved a bit faster potential for the future. Almost all organisms in the past than the rate at which it is moving contribute to sustain the earth’s environment. now. The differences in the internal forces However, humans have caused extensive operating from within the earth which built up damage to the environment through over use the crust have been responsible for the of resources. -
Chapter 2 the Solid Materials of the Earth's Surface
CHAPTER 2 THE SOLID MATERIALS OF THE EARTH’S SURFACE 1. INTRODUCTION 1.1 To a great extent in this course, we will be dealing with processes that act on the solid materials at and near the Earth’s surface. This chapter might better be called “the ground beneath your feet”. This is the place to deal with the nature of the Earth’s surface materials, which in later sections of the chapter I will be calling regolith, sediment, and soil. 1.2 I purposely did not specify any previous knowledge of geology as a prerequisite for this course, so it is important, here in the first part of this chapter, for me to provide you with some background on Earth materials. 1.3 We will be dealing almost exclusively with the Earth’s continental surfaces. There are profound geological differences between the continents and the ocean basins, in terms of origin, age, history, and composition. Here I’ll present, very briefly, some basic things about geology. (For more depth on such matters you would need to take a course like “The Earth: What It Is, How It Works”, given in the Harvard Extension program in the fall semester of 2005– 2006 and likely to be offered again in the not-too-distant future.) 1.4 In a gross sense, the Earth is a layered body (Figure 2-1). To a first approximation, it consists of concentric shells: the core, the mantle, and the crust. Figure 2-1: Schematic cross section through the Earth. 73 The core: The core consists mostly of iron, alloyed with a small percentage of certain other chemical elements. -
NBN EN 12670 : Natural Stone
ICS: 01.040.73; 01.040.91;; 73.020 91.100.15 Geregistreerde NBN EN 12670 Belgische norm 1e uitg., februari 2002 Normklasse : B 17 Natuursteen - Terminologie Pierre naturelle - Terminologie Natural stone - Terminology Toelating tot publicatie : 12 februari 2002 Deze Europese norm EN 12670 : 2001 heeft de status van een Belgische norm. Deze Europese norm bestaat in drie officiële versies (Duits, Engels, Frans). Belgisch instituut voor normalisatie (BIN) , vereniging zonder winstoogmerk Brabançonnelaan 29 - 1000 BRUSSEL - telefoon: 02 738 01 12 - fax: 02 733 42 64 e-mail: [email protected] - BIN Online: www.bin.be - prk. 000-0063310-66 © BIN 2002 Prijsgroep : 21 EUROPEAN STANDARD EN 12670 NORME EUROPÉENNE EUROPÄISCHE NORM December 2001 ICS 01.040.73; 01.040.91; 73.020; 91.100.15 English version Natural stone - Terminology Pierre naturelle - Terminologie Naturstein - Terminologie This European Standard was approved by CEN on 20 October 2001. CEN members are bound to comply with the CEN/CENELEC Internal Regulations which stipulate the conditions for giving this European Standard the status of a national standard without any alteration. Up-to-date lists and bibliographical references concerning such national standards may be obtained on application to the Management Centre or to any CEN member. This European Standard exists in three official versions (English, French, German). A version in any other language made by translation under the responsibility of a CEN member into its own language and notified to the Management Centre has the same status as the official versions. CEN members are the national standards bodies of Austria, Belgium, Czech Republic, Denmark, Finland, France, Germany, Greece, Iceland, Ireland, Italy, Luxembourg, Netherlands, Norway, Portugal, Spain, Sweden, Switzerland and United Kingdom. -
Oregon Geologic Digital Compilation Rules for Lithology Merge Information Entry
State of Oregon Department of Geology and Mineral Industries Vicki S. McConnell, State Geologist OREGON GEOLOGIC DIGITAL COMPILATION RULES FOR LITHOLOGY MERGE INFORMATION ENTRY G E O L O G Y F A N O D T N M I E N M E T R R A A L P I E N D D U N S O T G R E I R E S O 1937 2006 Revisions: Feburary 2, 2005 January 1, 2006 NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the infor- mation furthers the mission of the Department. To facilitate timely distribution of the information, this report is published as received from the authors and has not been edited to our usual standards. Oregon Department of Geology and Mineral Industries Oregon Geologic Digital Compilation Published in conformance with ORS 516.030 For copies of this publication or other information about Oregon’s geology and natural resources, contact: Nature of the Northwest Information Center 800 NE Oregon Street #5 Portland, Oregon 97232 (971) 673-1555 http://www.naturenw.org Oregon Department of Geology and Mineral Industries - Oregon Geologic Digital Compilation i RULES FOR LITHOLOGY MERGE INFORMATION ENTRY The lithology merge unit contains 5 parts, separated by periods: Major characteristic.Lithology.Layering.Crystals/Grains.Engineering Lithology Merge Unit label (Lith_Mrg_U field in GIS polygon file): major_characteristic.LITHOLOGY.Layering.Crystals/Grains.Engineering major characteristic - lower case, places the unit into a general category .LITHOLOGY - in upper case, generally the compositional/common chemical lithologic name(s) -
Plate Tectonics and the Cycling of Earth Materials
Plate Tectonics and the cycling of Earth materials Plate tectonics drives the rock cycle: the movement of rocks (and the minerals that comprise them, and the chemical elements that comprise them) from one reservoir to another Arrows are pathways, or fluxes, the I,M.S rocks are processes that “reservoirs” - places move material from one reservoir where material is temporarily stored to another We need to be able to identify these three types of rocks. Why? They convey information about the geologic history of a region. What types of environments are characterized by the processes that produce igneous rocks? What types of environments are preserved by the accumulation of sediment? What types of environments are characterized by the tremendous heat and pressure that produces metamorphic rocks? How the rock cycle integrates into plate tectonics. In order to understand the concept that plate tectonics drives the rock cycle, we need to understand what the theory of plate tectonics says about how the earth works The major plates in today’s Earth (there have been different plates in the Earth’s past!) What is a “plate”? The “plate” of plate tectonics is short for “lithospheric plate” - - the outermost shell of the Earth that behaves as a rigid substance. What does it mean to behave as a rigid substance? The lithosphere is ~150 km thick. It consists of the crust + the uppermost mantle. Below the lithosphere the asthenosphere behaves as a ductile layer: one that flows when stressed It means that when the substance undergoes stress, it breaks (a non-rigid, or ductile, substance flows when stressed; for example, ice flows; what we call a glacier) Since the plates are rigid, brittle 150km thick slabs of the earth, there is a lot of “action”at the edges where they abut other plates We recognize 3 types of plate boundaries, or edges. -
Relative Age-Dating
Relative Age-dating -- Discovery of Important Stratigraphic Principles Roger Steinberg, Assistant Professor of Geology, Del Mar College, Corpus Christi, TX Background Physical Geology and Historical Geology are the two introductory level Geology classes taught at most colleges and universities. Physical Geology is the study of Earth materials (minerals, rocks, sediment and soil) and the processes that affect those materials, including processes associated with oceans and shorelines, rivers, glaciers, groundwater, the wind, downslope movement and tectonic forces. Historical Geology is the study of the Earth through time, emphasizing the origins of and changes in the Earth's surface and subsurface, atmosphere, biosphere, and hydrosphere (water). Historical Geology is, as the name implies, essentially a history class. As in any other history class, we wish to know what happened, and when those particular events occurred. Of equal importance to learning these facts is an understanding of how we know what we claim to know about the history of the Earth. I believe it is critically important to establish that all of our geological knowledge about the Earth and its history has a firm, scientific foundation, and is based on important principles and concepts. In piecing together the history of the Earth, geologists rely on several key principles that allow us to determine the ages of rocks and the timing of significant events. There are two very different approaches to age-dating geological materials and events. Actual age-dating is the determination of the precise, numerical age of rocks and the geologic events that have affected those rocks for a particular area. It is often considered to be synonymous with radiometric age-dating, in which the occurrence and radioactive decay of natural, radioactive isotopes within minerals and rocks can be used as a type of very accurate clock to determine their age, although not all actual age-dating methods are radiometric. -
Structural Geology –Practice Questions and Answers Revised November 2008
Structural Geology –Practice Questions and Answers Revised November 2008 1. Terms used to describe surfaces across which there has been perceptible displacement are many. However, most geologists would prefer one of the falling terms: (a) joints, (b) fractures, (c) cracks, or (d) faults. What term best describes a surface across which there has been perceptible displacement? 2. Force is a term common to physics. Its classical expression is Force = mass * acceleration. However geologists are more concerned with the intensity of force or more succinctly the stress. Stress is defined as ______________________ . 3. Stresses produce strains in Earth materials. What are strains? 4. There are two end-member varieties of faults: dip-slip and strike-slip. The displacement along a strike-slip fault is _________________ to the strike of the fault. 5. The orientation of a plane in space is expressed by its attitude; a term consisting of two components, strike and dip. Define strike. Define dip. 6. Though many beds are upright others are not. For example, an overturned bed is one that has been rotated more than __________ degrees. 7. A dip-slip fault consists of the dipping fault surface and hanging and footwall blocks. The hanging wall block lies ____________ the dipping fault surface. 8. In the following illustration what block is the White Pine located on? What block is the Maple located on? What kind of fault is illustrated? 9. The footwall block lies ___________ a dipping fault surface. 10. What do you call a three dimensional surface separating Earth material of differing aspect? 11. In a dip-slip fault, if the hanging wall block moved up relative to the footwall block, then the fault is classified as a ____________________ . -
Petrology and Provenance of the Siluro-Devonian (Old Red Sandstone Facies) Sedimentary Rocks of the Midland Valley, Scotland
Petrology and provenance of the Siluro-Devonian (Old Red Sandstone facies) sedimentary rocks of the Midland Valley, Scotland Geology and Landscape Northern Britain Programme Internal Report IR/07/040 BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE NORTHERN BRITAIN PROGRAMME INTERNAL REPORT IR/07/040 Petrology and provenance of the Siluro-Devonian (Old Red Sandstone facies) sedimentary The National Grid and other Ordnance Survey data are used with the permission of the rocks of the Midland Valley, Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2005. Scotland Keywords Provenance; petrography; Emrys Phillips Silurian and Devonian sandstones; Midland Valley; Scotland. Bibliographical reference Contributors: Richard A Smith and Michael A E Browne E.R. PHILLIPS. 2007. Petrology and provenance of the Siluro- Devonian (Old Red Sandstone facies) sedimentary rocks of the Midland Valley, Scotland. British Geological Survey Internal Report, IR/07/040. 65pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. Maps and diagrams in this book use topography based on Ordnance Survey mapping. © NERC 2007. All rights reserved Keyworth, Nottingham British Geological Survey 2007 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS British Geological Survey offices Sales Desks at Nottingham, Edinburgh and London; see contact details below or shop online at www.geologyshop.com Keyworth, Nottingham NG12 5GG The London Information Office also maintains a reference 0115-936 3241 Fax 0115-936 3488 collection of BGS publications including maps for consultation.