Field Geology
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The Rise of K–12 Blended Learning
The Rise of K–12 Blended leaRning By Michael B. Horn and Heather Staker With contributions from Alex Hernandez, Bryan Hassel, and Joe Ableidinger January 2011 NNOSIGHT NSTITUTE The Rise of K–12 Blended leaRning Online learning is sweeping across America. In the year 2000, roughly 45,000 K–12 students took an online course. In 2009, more than 3 million K–12 students did. What was originally a distance- learning phenomenon no longer is. Most of the growth is occurring in blended-learning environments, in which students learn online in an adult-supervised environment at least part of the time. As this happens, online learning has the potential to transform America’s education system by serving as the backbone of a system that offers more personalized learning approaches for all students. n Disrupting Class,1 the authors project that by 2019, 50 percent of all high school courses will be delivered online. This pattern of growth is characteristic of a disruptive innovation—an iinnovation that transforms a sector characterized by products or services that are complicated, expensive, inaccessible, and centralized into one with products or services that are simple, affordable, accessible, convenient, and often customizable. Think personal computers, the iPod and mp3s, Southwest Airlines, and TurboTax. At the beginning of any disruptive innovation, the new technology takes root in areas of nonconsumption—where the alternative is nothing at all, so the simple, new innovation is infinitely better. More users adopt it as the disruptive innovation predictably improves. Online learning fits the pattern. It started by serving students in circumstances where there is no alternative for learning—in the advanced courses that many schools struggle to offer in- house; in small, rural, and urban schools that are unable to offer a broad set of courses with highly qualified teachers in certain subject areas; in remedial courses for students who need to recover credits to graduate; and with home-schooled and homebound students. -
Strike and Dip Refer to the Orientation Or Attitude of a Geologic Feature. The
Name__________________________________ 89.325 – Geology for Engineers Faults, Folds, Outcrop Patterns and Geologic Maps I. Properties of Earth Materials When rocks are subjected to differential stress the resulting build-up in strain can cause deformation. Depending on the material properties the result can either be elastic deformation which can ultimately lead to the breaking of the rock material (faults) or ductile deformation which can lead to the development of folds. In this exercise we will look at the various types of deformation and how geologists use geologic maps to understand this deformation. II. Strike and Dip Strike and dip refer to the orientation or attitude of a geologic feature. The strike line of a bed, fault, or other planar feature, is a line representing the intersection of that feature with a horizontal plane. On a geologic map, this is represented with a short straight line segment oriented parallel to the strike line. Strike (or strike angle) can be given as either a quadrant compass bearing of the strike line (N25°E for example) or in terms of east or west of true north or south, a single three digit number representing the azimuth, where the lower number is usually given (where the example of N25°E would simply be 025), or the azimuth number followed by the degree sign (example of N25°E would be 025°). The dip gives the steepest angle of descent of a tilted bed or feature relative to a horizontal plane, and is given by the number (0°-90°) as well as a letter (N, S, E, W) with rough direction in which the bed is dipping. -
Carpe Diem – Seize the Day Blog
Carpe Diem – Seize the Day Blog Editor’s Note: Content presented in the Carpe D iem – Seize the Day Blog is for awareness and informational purposes only, and it is not meant to be a diagnostic tool. What is “Brain Fog” and what can be done about it? We all experience “Brain Fog” sometime in our lives. I know that I have. There are times when we may forget certain things on our grocery list, forget to respond to an email, misplace our keys or what we came into a room for. After all, the human brain wasn’t designed to run at its peak 24/7! Maybe we forget certain things on our grocery list, forget to respond to an email, misplace our keys or what we came into a room for. When you look up the common symptoms of “Brain Fog” on various medical websites you will discover examples such as this: • Memory problems • Inability to focus or concentrate • Difficulty processing information • Trouble problem-solving • Feelings of confusion or disorientation • Trouble finding words • lack of mental clarity “Brain Fog” is not a medical term or a medical condition itself, but rather it is a symptom that relates to other chronic medical conditions such as epilepsy, chemotherapy, and fibromyalgia. According to Tiffany Kairos, besides seizures, “Brain Fog” is one of the most difficult – and sometimes exhausting – parts of living with epilepsy. “Brain Fog” is more than just the occasional forgetfulness. “Brain Fog” is the general term used to explain a dysfunction in focus, learning, and/or memory that can cause brief episodes of confusion and disorientation. -
Nd Isotope Mapping of the Grenvillian Allochthon Boundary Thrust in Algonquin Park, Ontario
Canadian Journal of Earth Sciences Nd isotope mapping of the Grenvillian Allochthon Boundary Thrust in Algonquin Park, Ontario Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2018-0142.R1 Manuscript Type: Article Date Submitted by the 26-Sep-2018 Author: Complete List of Authors: Dickin, Alan; School of Geography and Geology Strong, Jacob; School of Geography and Geology Keyword: Nd isotopes,Draft Model ages, Grenville Province Is the invited manuscript for consideration in a Special Not applicable (regular submission) Issue? : https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 34 Canadian Journal of Earth Sciences 1 Nd isotope mapping of the Grenvillian Allochthon Boundary Thrust in Algonquin Park, 2 Ontario 3 4 A.P. Dickin and J.W.D. Strong 5 School of Geography and Earth Sciences, McMaster University, Hamilton ON, Canada 6 7 Abstract 8 Over fifty new Nd isotope analyses are presented for high-grade orthogneisses from 9 Algonquin Park and surrounding region in order to map major Grenvillian thrust boundaries. Nd 10 model ages display a consistent geographical pattern that allows detailed mapping of the 11 boundary between the Algonquin and MuskokaDraft domains, here interpreted as the local trajectory 12 of the Ottawan-age Allochthon Boundary Thrust (ABT). The ABT is underlain by a domain with 13 Paleoproterozoic Nd model ages, interpreted as a tectonic duplex entrained onto the base of the 14 main allochthon. The boundaries determined using Nd isotope mapping are consistent with field 15 mapping and with remotely sensed aeromagnetic and digital elevation data. The precise location 16 of the ABT can be observed in a road-cut on Highway 60, on the north shore of the Lake of Two 17 Rivers in the centre of Algonquin Park. -
Vol. 9 (1) 2020
Vol. 9 (1) 2020 ESMSJ ISSN: 2247 – 2479 ISSN – L: 2247 – 2479 Vol IX, Issue 1 / 2020 Econophysics, Sociophysics & Other Multidisciplinary Sciences Journal (ESMSJ) provides a resource of the most important developments in the rapidly evolving area of Econophysics, Sociophysics & other new multidisciplinary sciences. The journal contains articles from Physics, Econophysics, Sociophysics, Demographysics, Socioeconomics, Quantum Economics, Econo-operations Research, or many other transdisciplinary, multidisciplinary and modern sciences and related fundamental methods and concepts. Econophysics, Sociophysics & Other Multidisciplinary Sciences Journal (ESMSJ) Staff University of Piteşti Address: Str. Târgul din Vale, Nr.1, Piteşti 110040, Argeş, Romania Phone: +40348453102; Fax: +40349453123 Editor-in-chief Gheorghe Săvoiu Managing editor Marian Țaicu On - line edition http://www.esmsj.upit.ro/ Denis Negrea Founders Editors Gheorghe Săvoiu English version and harmonization of the Mircea Gligor scientific language Ion Iorga Simăn Georgiana Mindreci Constantin Andronache Assistant Editors Constantin Manea for English version Mihaela Gâdoiu Mariana Banuţă Editorial Board Scientific Board Benedict Oprescu Aretina David Pearson Ciprian-Ionel Turturean Doru Pogoreanu Ivana Mijatović Hans Schjær-Jacobsen Jelena Minović Mladen Čudanov Maria - Daniela Bondoc Muhittin Acar Matei Sandra Libb Thims Milica Jovanović Ondrej Jaško Mircea Bărbuceanu Radu Chişleag Slađana Barjaktarović Rakočević Ram Poudel Slavica Cicvarić Kostić Sant Sharan Mishra Vesna Tornjanski -
Building and Testing Theory on the Role of IT in the Relationship Between Power and Performance: Implementing Enterprise Performance Management in the Organization
Virginia Commonwealth University VCU Scholars Compass Theses and Dissertations Graduate School 2009 Building and Testing Theory on the Role of IT in the Relationship between Power and Performance: Implementing Enterprise Performance Management in the Organization Mitchell Wenger Virginia Commonwealth University Follow this and additional works at: https://scholarscompass.vcu.edu/etd Part of the Management Information Systems Commons © The Author Downloaded from https://scholarscompass.vcu.edu/etd/1784 This Dissertation is brought to you for free and open access by the Graduate School at VCU Scholars Compass. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of VCU Scholars Compass. For more information, please contact [email protected]. © Mitchell R. Wenger, 2009 All Rights Reserved © Mitchell R. Wenger, 2009 Page i Building and Testing Theory on the Role of IT in the Relationship between Power and Performance: Implementing Enterprise Performance Management in the Organization A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at Virginia Commonwealth University. By Mitchell R. Wenger Virginia Commonwealth University [email protected] Masters in Business Administration University of Texas at Arlington, Arlington, TX, 1984 Bachelor of Science in Accountancy University of Illinois, Urbana-Champaign, IL, 1982 Chair: Dr. Allen S. Lee Professor and Associate Dean for Research & Graduate Studies Department of Information Systems Co-Chair: Gurpreet Dhillon Professor, Department of Information Systems Virginia Commonwealth University Richmond, Virginia, USA April, 2009 © Mitchell R. Wenger, 2009 Page ii Acknowledgements This dissertation, along with the degree work leading up to it, would not have been possible without the support of my wife Deb. -
This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library
This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L. -
FM 5-410 Chapter 2
FM 5-410 CHAPTER 2 Structural Geology Structural geology describes the form, pat- secondary structural features. These secon- tern, origin, and internal structure of rock dary features include folds, faults, joints, and and soil masses. Tectonics, a closely related schistosity. These features can be identified field, deals with structural features on a and m appeal in the field through site inves- larger regional, continental, or global scale. tigation and from remote imagery. Figure 2-1, page 2-2, shows the major plates of the earth’s crust. These plates continually Section I. Structural Features undergo movement as shown by the arrows. in Sedimentary Rocks Figure 2-2, page 2-3, is a more detailed repre- sentation of plate tectonic theory. Molten material rises to the earth’s surface at BEDDING PLANES midoceanic ridges, forcing the oceanic plates Structural features are most readily recog- to diverge. These plates, in turn, collide with nized in the sedimentary rocks. They are adjacent plates, which may or may not be of normally deposited in more or less regular similar density. If the two colliding plates are horizontal layers that accumulate on top of of approximately equal density, the plates each other in an orderly sequence. Individual will crumple, forming mountain range along deposits within the sequence are separated the convergent zone. If, on the other hand, by planar contact surfaces called bedding one of the plates is more dense than the other, planes (see Figure 1-7, page 1-9). Bedding it will be subducted, or forced below, the planes are of great importance to military en- lighter plate, creating an oceanic trench along gineers. -
Wyoming-Skye Dinosaurs
Clark, N.D.L. and Brett-Surman, M.K. (2008) A comparison between dinosaur footprints from the Middle Jurassic of the Isle of Skye, Scotland, UK, and Shell, Wyoming, USA. Scottish Journal of Geology, 44 (2). pp. 139-150. ISSN 0036-9276 http://eprints.gla.ac.uk/4807/ Deposited on: 14 April 2009 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk A comparison between dinosaur footprints from the Middle Jurassic of the Isle of Skye, Scotland, UK, and Shell, Wyoming, USA N. D. L. CLARK1 & M. K. BRETT-SURMAN2 1Hunterian Museum and Art Gallery, University of Glasgow, University Avenue, Glasgow, G12 8QQ, UK (e-mail: [email protected]) 2Smithsonian Institution, Department of Paleobiology, PO Box 37012, MRC 121 Washington, DC 20013-7012, USA Synopsis Measurements of Middle Jurassic tridactyl dinosaur tracks from the Bathonian, Lealt Shale, Valtos Sandstone, Duntulm and Kilmaluag formations of the Isle of Skye, UK, are compared to the same measurements taken for dinosaur footprints from the Bajocian, Gypsum Spring and the Bathonian, Sundance Formation of the Bighorn Basin, Wyoming, USA. Principal component analysis of the data suggests that the smaller footprints from the Valtos Sandstone and Kilmaluag formations are indistinguishable from the footprints of the Sundance Formation. The single footprint from the Lealt Shale Formation is similar to the larger footprints from the Valtos Sandstone Formation. The footprints from the Duntulm and Gypsum Springs formations form distinct groupings from all other footprints. Four different groupings of dinosaur footprints can be recognized from the principal component analysis that may represent at least four different types of dinosaur. -
Wood Research Impacts of Impregnation Chemicals On
WOOD RESEARCH 54 (4): 2009 67-78 IMPACTS OF IMPREGNATION CHEMICALS ON THE FLAME SOURCE COMBUSTION LIGHT INTENSITY OF THE LAMINATED VENEER LUMBER (LVL) Hakan Keskin Gazi University, Industrial Arts Education Faculty, Department of Idustrial Technology Education, Division of Material and Manufacturing Technology, Ankara, Turkey ABSTRACT The aim of this study was to investigate the effects of impregnation chemicals on the flame source combustion light intensity of the LVL obtained from combination of Oriental beech + Lombardy poplar and European oak + Lombardy poplar woods, impregnated with boron compounds (Borax (Bx), Boric acid (Ba), Bx+Ba (wt:wt 50:50%)), Imersol-aqua (Ia) and Timbercare-aqua (Ta) according to ASTM D 1413-76-99 and directions of the manufacturer. LVL samples were prepared in the form of five layers, 3 mm thickness from the beech, oak and poplar veneers bonded with Desmodur-VTKA (DVTKA) and Poly(vinyl acetate) (PVAc) adhesives, according to TS EN 386. The flame source combustion light intensity of the LVL test samples were determined according to ASTM E 160- 50. Consequently, the flame source combustion light intensity was the highest in oak- poplar combination, Ta and PVAc and the lowest in beech-poplar combination, Bx and DVTKA adhesive. In the interaction of the impregnation chemical, types of process and adhesive, it was the highest in beech-poplar combination + (Ba+Bx) + DVTKA (763.5 lux), but the lowest in beech-poplar combination + Ba + PVAc (582.7 lux). Accordingly, boric acid showed decreasing impact on the flame source combustion light intensity of LVL. In consequence, for places which has fire risk, usage of LVL impregnated with boric acid would be advantageous. -
Best Practices for Shale Core Handling: Transportation, Sampling and Storage for Conduction of Analyses
Journal of Marine Science and Engineering Review Best Practices for Shale Core Handling: Transportation, Sampling and Storage for Conduction of Analyses Sudeshna Basu 1,2,*, Adrian Jones 1 and Pedram Mahzari 1 1 Department of Earth Sciences, University College London, London WC1E 6BS, UK; [email protected] (A.J.); [email protected] (P.M.) 2 Department of Chemical Engineering, University College London, London WC1E 7JE, UK * Correspondence: [email protected] Received: 9 January 2020; Accepted: 12 February 2020; Published: 20 February 2020 Abstract: Drill core shale samples are critical for palaeoenvironmental studies and potential hydrocarbon reservoirs. They need to be preserved carefully to maximise their retention of reservoir condition properties. However, they are susceptible to alteration due to cooling and depressurisation during retrieval to the surface, resulting in volume expansion and formation of desiccation and micro fractures. This leads to inconsistent measurements of different critical attributes, such as porosity and permeability. Best practices for core handling start during retrieval while extracting from the barrel, followed by correct procedures for transportation and storage. Appropriate preservation measures should be adopted depending on the objectives of the scientific investigation and core coherency, with respect to consolidation and weathering. It is particularly desirable to maintain a constant temperature of 1 to 4 ◦C and a consistent relative humidity of >75% to minimise any micro fracturing and internal moisture movement in the core. While core re-sampling, it should be ensured that there is no further core compaction, especially while using a hand corer. Keywords: shale; drill core instability; micro fracture; clay minerals 1. -
Meridian Lateral Files
Y Price Book Prices effective January 6, 2020 Meridian® Lateral Files Published May 2020 Introduction page 2 Meridian® Lateral Files 3 Stackable™ Lateral Files (Spec-A-File) 5 Freestanding Stackable Lateral Files (Standard Configuration) 23 Standard Pull 25 Arc Pull 30 Bar Pull 36 Bevel Pull 43 Ellipse Pull 48 Sloped Pull 54 Stackable Lateral File Cushion Tops 60 Mobile Stackable Lateral Files 62 Standard Pull 62 Bevel Pull 67 Low Credenza 72 File Tops 78 File Surrounds 82 Stackable Lateral File Accessories 91 Keyless Locks 97 Indices 101 By Name 101 By Number 103 Appendices 20-Day or Less/Assigned Lead-Time Order Information Keyed-Alike Information Vary Easy Program Stain-to-Match Program Customer’s Own Material/Customer’s Own Leather Order Information-Cushion Tops Proprietary Textiles Application Chart-Seating Proprietary Textile Colors-Seating Maharam® Application Chart-Seating Maharam Colors-Seating For the latest materials information, refer to the Materials pages on HermanMiller.com. Z Meridian® Lateral Files Price Book (5/20) 1 Introduction A Note on the Organization of This Book General Information There are a few signals that will help you understand the organization This book is effective January 6, 2020, subject to change without of this book. Once you know them, you should be able to find your way notice. Products may be purchased from authorized Herman Miller deal- around easily. ers who will quote prices upon request. For more information about our products and services or to see a list of dealers, visit www. Like a newspaper, this book is formatted with columns of text HermanMiller.com.