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Extensions of Remarks Section
December 2, 2010 CONGRESSIONAL RECORD — Extensions of Remarks E2033 EXTENSIONS OF REMARKS CELEBRATING THE LIFE AND AC- who he was. Richard Goldman was a great Scott and William Frey are the recipients of COMPLISHMENTS OF RICHARD patriot who loved our country—the diversity of the Visionary Award. In 1997, brothers Scott GOLDMAN its people, the beauty of its natural resources and William bought The Art Theatre, located in and the freedoms we all enjoy. He served our downtown Hobart. The two renovated and re- HON. NANCY PELOSI country in uniform in his youth and every day stored the theatre, which was first built in OF CALIFORNIA since. 1941. Today, the theatre attracts many visitors IN THE HOUSE OF REPRESENTATIVES I hope it is a comfort to his children John from surrounding communities. Scott and Wil- and his wife Marcia, Douglas and his wife Thursday, December 2, 2010 liam have expanded their business to include Lisa, and Susan and husband Michael the Art of Pizza restaurant, located next door Ms. PELOSI. Madam Speaker, I rise today Gelman, his eleven grandchildren and three to the theatre, which is set to open in 2011. to celebrate the life and the accomplishments great-grandchildren that so many people For their outstanding commitment to their of Richard Goldman, a great American and a mourn his loss. Thankfully this next generation community, Scott and William Frey are to be dear friend. The passing of Richard Goldman, stands ready to ensure Richard and Rhoda’s honored. an accomplished businessman, noted philan- legacy of compassion, pursuing peace and The Legacy Award recipient is People’s thropist and powerful advocate for environ- protecting our planet goes forward. -
COA Endowment Report FY2012 Table of Contents
COA Endowment Report FY2012 Table of Contents The Rachel Carson Chair in Human Ecology 3 The William H. Drury, Jr. Chair in Evolution, Ecology and Natural History 4 The Charles Eliot Chair in Ecological Planning, Policy and Design 5 The Steven K. Katona Chair in Marine Studies 6 The Elizabeth Battles Newlin Chair in Botany 7 The Partridge Chair in Food and Sustainable Agriculture Systems 8 The David Rockefeller Family Chair in Ecosystem Management and Protection 9 The Tom A. Cox Fund in Ecosystem Management and Protection The Sharpe-McNally Chair of Green and Socially Responsible Business 10 The Allan Stone Chair in the Visual Arts 11 The James Russell Wiggins Chair in Government and Polity 12 The Philip Geyelin Fund for Government and Polity Endowed Scholarships 13 The Beinecke Student Travel and Living Assistance Fund 16 The Shelby Cullom Davis Faculty International Studies Fund 17 The Shelby Cullom Davis Student International Studies Fund 18 The William H. Drury Research Fund 19 The Faculty/Staff Enrichment Fund 20 The Elizabeth A. and Henry B. Guthrie Chemistry Enhancement Fund 21 The Barbarina M. and Aaron J. Heyerdahl Beech Hill Farm Endowment Fund The Robert P. and Arlene Kogod Visiting Artist Fund 22 The McCormick Library Director Fund 23 The Rabineau Student Senior Project and Professional Development Fund The Peggy Rockefeller Farms Endowment 24 The Doug Rose GIS Enhancement Fund 25 The Maurine and Robert Rothschild Student-Faculty Collaborative Research Fund The Elizabeth Thorndike Senior Class Book Fund 26 COA’s Physical Plant Funds 27 General Unrestricted Endowment 28 New Endowment Funds Letter from the President Dear Friends of the College of the Atlantic: Before returning to COA as president, I spent a significant amount of time working in the wilds of the Peruvian Amazon. -
Current Best Practices for Vermiculite Attic Insulation
What is vermiculite insulation? What if I occasionally have to go into Vermiculite is a naturally occurring mineral that has my attic? the unusual property of expanding into worm-like EPA and ATSDR strongly recommend that accordion shaped pieces when heated. The homeowners make every effort not to disturb expanded vermiculite is a light-weight, fire- vermiculite insulation in their attics. If you resistant, absorbent, and odorless material. These occasionally have to go into your attic, current best properties allow vermiculite to be used to make practices state you should: numerous products, including attic insulation. 1. Make every effort to stay on the floored part Do I have vermiculite insulation? of your attic and to not disturb the Vermiculite can be purchased in various forms for insulation. various uses. Sizes of vermiculite products range 2. If you must perform activities that may from very fine particles to large (coarse) pieces disturb the attic insulation such as moving nearly an inch long. Vermiculite attic insulation is a boxes (or other materials), do so as gently pebble-like, pour-in product and is usually light- as possible to minimize the disturbance. brown or gold in color. The pictures in the center of What should I do if I have 3. Leave the attic immediately after the this pamphlet and on the cover show several disturbance. samples of vermiculite attic insulation. vermiculite attic insulation? 4. If you need work done in your attic such as DO NOT DISTURB IT. Any disturbance has the the installation of cable or utility lines, hire trained and certified professionals who can Is vermiculite insulation a problem? potential to release asbestos fibers into the air. -
Greensand.Pdf
www.natureswayresources.com GREENSAND Greensand is a naturallyoccurring mineral mined from ocean deposits from a sedimentary rock known as “Glauconite”. It is often an olive-green colored sandstonerock found in layers in many sedimentary rock formations. Origin of Greensand Greensand forms in anoxic (without oxygen) marine environments that are rich in organic detritus and low in sedimentary inputs. Some greensands contain marine fossils (i.e. New Jersey Greensand). Greensand has been found in deposits all over the world. The greenish color comes from the mineral glauconite and iron potassiumsilicate that weathers and breaks down releasing the stored minerals. The color may range from a dark greenish gray, green-black to blue-green dependingon the minerals and water content. It often weatherseasilyand forms nodules that have been oxidized with iron bearing minerals that has a reddish brown or rust color. +3 The major chemical description is ((K,Na)(Fe , Al, Mg)2(Si,Al)4O10(OH)2) General chemical information: Iron (Fe) 12-19% Potassium (K) 5-7 % Silicon (Si) 25.0% Oxygen (O) 45% Magnesium (Mg) 2-3 % Aluminum (Al) 1.9 % Sodium (Na) 0.27% Hydrogen (H) 0.47% Over 30 other trace minerals and many micronutrients. Types of Greensand Glauconite is the namegiven to a group of naturally occurring iron rich silica minerals that may be composed of pellets or grains. When glauconite is mined the upper layers that have weathered and become oxidizedand minerals are released.These sometimes form pyrite a iron sulfide (FeS2) when oxygen is www.natureswayresources.com absent. In the deeper layers or reduced zone pyrite crystals often form. -
The Historic New Bridge Landing State Park Commission Annual
The Historic New Bridge Landing State Park Commission Annual Report for 2016 A young visitor peers into an open window to see what is happening at the Steuben House at Historic New Bridge Landing State Park, for Calico Frolic 2016. 1 Respectfully submitted to the Governor and Legislature of New Jersey December 2016 B. Spencer Newman’s painting depicts the darkest hour of the American Revolution, when General George Washington led the outnumbered Continental garrison of Fort Lee across the Hackensack River at New Bridge on November 20, 1776. Doubtful to the last moment, this crossing preserved American hopes in the face of invasion by an army of Europe’s finest troops. Eyewitness-to-history Thomas Paine stands in the left foreground. Literally occupying the Crossroads of the American Revolution, the Zabriskie- Steuben House—the only extant house along the route of the retreat in Bergen County—went on to survive more of the war than any other home in America. The State of NJ acquired this landmark dwelling in 1928 as a perpetual memorial to the “times that try men’s souls.” 2 Dear Governor Chris Christie and Legislators: Pursuant to our responsibilities under Public Law 2009, chapter 45, the Historic New Bridge Landing Park Commission submits this annual report for 2016. 2016 has been another banner year for Historic New Bridge Landing. The key to our success is consistently exciting and innovative programming that not only attracts new audiences, but repeat visitors as well. We succeed because we understand quality programming depends not only upon having an interesting and engaging story to tell, but also on coordinating the talents of highly motivated and well educated volunteers from a variety of professions, who generously share their enthusiasm with guests, and, most importantly, who create a pervasive culture of hospitality, respect for the lessons of our history and a commitment to stewardship over a significant American Revolutionary War battleground, which gave life to our nation. -
Hawaiian Volcanoes: from Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012
AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Waikolao, Hawaii 20 - 24 August 2012 Conveners Michael Poland, USGS – Hawaiian Volcano Observatory, USA Paul Okubo, USGS – Hawaiian Volcano Observatory, USA Ken Hon, University of Hawai'i at Hilo, USA Program Committee Rebecca Carey, University of California, Berkeley, USA Simon Carn, Michigan Technological University, USA Valerie Cayol, Obs. de Physique du Globe de Clermont-Ferrand Helge Gonnermann, Rice University, USA Scott Rowland, SOEST, University of Hawai'i at M noa, USA Financial Support 2 AGU Chapman Conference on Hawaiian Volcanoes: From Source to Surface Site Meeting At A Glance Sunday, 19 August 2012 1600h – 1700h Welcome Reception 1700h – 1800h Introduction and Highlights of Kilauea’s Recent Eruption Activity Monday, 20 August 2012 0830h – 0900h Welcome and Logistics 0900h – 0945h Introduction – Hawaiian Volcano Observatory: Its First 100 Years of Advancing Volcanism 0945h – 1215h Magma Origin and Ascent I 1030h – 1045h Coffee Break 1215h – 1330h Lunch on Your Own 1330h – 1430h Magma Origin and Ascent II 1430h – 1445h Coffee Break 1445h – 1600h Magma Origin and Ascent Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Origin and Ascent III 1645h – 1900h Poster Session Tuesday, 21 August 2012 0900h – 1215h Magma Storage and Island Evolution I 1215h – 1330h Lunch on Your Own 1330h – 1445h Magma Storage and Island Evolution II 1445h – 1600h Magma Storage and Island Evolution Breakout Sessions I, II, III, IV, and V 1600h – 1645h Magma Storage -
Town of Trenton Report
JOINT RECREATION CENTER FEASIBILITY STUDY OCTOBER 7, 2009 TOWN OF TRENTON TOWN OF REMSEN TOWN OF STEUBEN Towns of Trenton, Remsen, and Steuben Joint Recreation Center Feasibility Study Final Study October 7, 2009 © 2009 Laberge Group 4 Computer Drive West Albany, New York 12205 Laberge Group Project Number 27101 Acknowledgements The Towns of Trenton, Remsen and Steuben would like to recognize and thank the many people and organizations whose assistance has made the completion of the Joint Recreation Center Feasibility Study a reality. Joint Recreation Center Steering Committee Town of Trenton Mark Scheidelman, Town Supervisor Bruce Kellogg, Town Board Member Shirley Poland, Town Board Member Stephen Godfrey, Resident Town of Remsen Clifford Hill, Town Supervisor Charlie Appleton, Town Board Member Town of Steuben Les Dean, Town Board Terry Dean, Resident This report was prepared with funds provided by the New York State Department of State under the Shared Municipal Services Incentive Grant Program. Joint Recreation Center Feasibility Study i Table of Contents Executive Summary ..................................................................................................................... vi Purpose of Feasibility Study .................................................................................................... vi The Planning Process ............................................................................................................... vi Community Overview ............................................................................................................. -
Nature of Interlayer Material in Silicate Clays of Selected Oregon Soils
AN ABSTRACT OF THE THESIS OF PAUL C, SINGLETON for the Ph.D. in Soils (Name) (Degree) (Major) Date thesis is presented July 28, 1965 Title NATURE OF INTERLAYER MATERIAL IN SILICATE CLAYS OF SELECTED OREGON SOILS - Redacted for Privacy Abstract approved = ajor professor) Ç A study was conducted to investigate the nature of hydroxy interlayers in the chlorite -like intergrade clays of three Oregon soils with respect to kind, amount, stability, and conditions of formation. The clays of the Hembre, Wren, and Lookout soils, selected to represent weathering products originating from basaltic materials under humid, subhumid, and semi -arid climatic conditions respectively, were subjected to a series of progressive treatments designed to effect a differential dissolution of the materials intimately asso- ciated with them. The treatments, chosen to represent a range of increasing severity of dissolution, were (1) distilled water plus mechanical stirring, (2) boiling 2% sodium carbonate, (3) buffered sodium citrate -dithionite, (4) boiling sodium hydroxide, and (5) preheating to 400 °C for 4 hours plus boiling sodium hydroxide. Extracts from the various steps of the dissolution procedure were chemically analyzed in order to identify the materials removed from the clays. X -ray diffraction analysis and cation exchange capacity determinations were made on the clays after each step, and any differences noted in the measured values were attributed to the removal of hydroxy interlayers from the clays. Hydroxy interlayers were found to occur more in the Hembre and Wren soils than in the Lookout soil, with the most stable interlayers occurring in the Wren. Soil reaction was one of the major differences between these soils. -
Clay Minerals Soils to Engineering Technology to Cat Litter
Clay Minerals Soils to Engineering Technology to Cat Litter USC Mineralogy Geol 215a (Anderson) Clay Minerals Clay minerals likely are the most utilized minerals … not just as the soils that grow plants for foods and garment, but a great range of applications, including oil absorbants, iron casting, animal feeds, pottery, china, pharmaceuticals, drilling fluids, waste water treatment, food preparation, paint, and … yes, cat litter! Bentonite workings, WY Clay Minerals There are three main groups of clay minerals: Kaolinite - also includes dickite and nacrite; formed by the decomposition of orthoclase feldspar (e.g. in granite); kaolin is the principal constituent in china clay. Illite - also includes glauconite (a green clay sand) and are the commonest clay minerals; formed by the decomposition of some micas and feldspars; predominant in marine clays and shales. Smectites or montmorillonites - also includes bentonite and vermiculite; formed by the alteration of mafic igneous rocks rich in Ca and Mg; weak linkage by cations (e.g. Na+, Ca++) results in high swelling/shrinking potential Clay Minerals are Phyllosilicates All have layers of Si tetrahedra SEM view of clay and layers of Al, Fe, Mg octahedra, similar to gibbsite or brucite Clay Minerals The kaolinite clays are 1:1 phyllosilicates The montmorillonite and illite clays are 2:1 phyllosilicates 1:1 and 2:1 Clay Minerals Marine Clays Clays mostly form on land but are often transported to the oceans, covering vast regions. Kaolinite Al2Si2O5(OH)2 Kaolinite clays have long been used in the ceramic industry, especially in fine porcelains, because they can be easily molded, have a fine texture, and are white when fired. -
VERMICULITE by Michael J
VERMICULITE By Michael J. Potter Domestic survey data and tables were prepared by Nicholas Muniz, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. +2 Vermiculite is a hydrated magnesium-aluminum-iron silicate, with a suggested formula of (Mg,Fe ,Al)3(Al,Si)4O10(OH)2·4H2O (Fleisher and Mandarino, 1991, p. 211). Flakes of raw vermiculite concentrate are mica-like in appearance and contain water molecules within their internal structure. When the flakes are heated rapidly at a temperature of 900º C or higher, the water flashes into steam, and the flakes expand into accordion-like particles. The color, which can range from black and various shades of brown to yellow for the raw flakes, changes upon expansion to gold or bronze. This expansion process is called exfoliation, and the resulting lightweight material is chemically inert, fire resistant, and odorless. In lightweight plaster and concrete, vermiculite provides good thermal insulation. Vermiculite can absorb such liquids as fertilizers, herbicides, and insecticides, which can then be transported as free-flowing solids (Harben and Kuzvart, 1996). Production Domestic production (sold or used) data for vermiculite were collected by the U.S. Geological Survey (USGS) from two voluntary canvasses—one for mine-mill (concentrator) operations and the other for exfoliation plants. Data were not available for the three mine-mill operations. The two U.S. producers of vermiculite concentrate were Virginia Vermiculite Ltd. with operations near Woodruff, SC, and in Louisa County, VA; and W.R. Grace & Co. from its operation at Enoree, SC. Vermiculite concentrate was shipped to exfoliating plants for conversion into lightweight material. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
A Submarine Perspective of the Honolulu Volcanics, Oahu
Journal of Volcanology and Geothermal Research 151 (2006) 279–307 www.elsevier.com/locate/jvolgeores A submarine perspective of the Honolulu Volcanics, Oahu David A. Clague a,*, Jennifer B. Paduan a, William C. McIntosh b, Brian L. Cousens c, Alice´ S. Davis a, Jennifer R. Reynolds d a Monterey Bay Aquarium Research Institute, 7700 Sandholdt Road, Moss Landing, CA 95039-9644, USA b New Mexico Geochronology Research Laboratory, N.M. Bureau of Geology, New Mexico Tech, 801 Leroy Place, Socorro, 87801-4796, USA c Ottawa-Carleton Geoscience Centre, Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada K1S 5B6 d School of Fisheries and Ocean Sciences, West Coast and Polar Regions Undersea Research Center, University of Alaska Fairbanks, P.O. Box 757220, 213 O’Neill Building, Fairbanks, AK 99775, USA Accepted 15 July 2005 Available online 27 December 2005 Abstract Lavas and volcaniclastic deposits were observed and collected from 4 submarine cones that are part of the Honolulu Volcanics on Oahu, Hawaii. The locations of these and a few additional, but unsampled, vents demonstrate that nearly all the vents are located on or very close to the shoreline of Oahu, with the most distal vent just 12 km offshore. The clastic samples and outcrops range from coarse breccias to cross-bedded ash deposits and show that explosive volcanism at depths between about 350 and 590 m depth played a part in forming these volcanic cones. The eruptive styles appear to be dominantly effusive to strombolian at greater depths, but apparently include violent phreatomagmatic explosive activity at the shallower sites along the submarine southwest extension of the Koko Rift.