Geologic Guide to Stone Mountain Park
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
History of Geology
FEBRUARY 2007 PRIMEFACT 563 (REPLACES MINFACT 60) History of geology Mineral Resources Early humans needed a knowledge of simple geology to enable them to select the most suitable rock types both for axe-heads and knives and for the ornamental stones they used in worship. In the Neolithic and Bronze Ages, about 5000 to 2500 BC, flint was mined in the areas which are now Belgium, Sweden, France, Portugal and Britain. While Stone Age cultures persisted in Britain until after 2000 BC, in the Middle East people began to mine useful minerals such as iron ore, tin, clay, gold and copper as early as 4000 BC. Smelting techniques were developed to make the manufacture of metal tools possible. Copper was probably the earliest metal to be smelted, that is, extracted from its ore by melting. Copper is obtained easily by reducing the green copper carbonate mineral malachite, itself regarded as a precious stone. From 4000 BC on, the use of clay for brick-making became widespread. The Reverend William Branwhite Clarke (1798-1878), smelting of iron ore for making of tools and the ‘father’ of geology in New South Wales weapons began in Asia Minor at about 1300 BC but did not become common in Western Europe until Aristotle believed volcanic eruptions and nearly 500 BC. earthquakes were caused by violent winds escaping from the interior of the earth. Since earlier writers had ascribed these phenomena to The classical period supernatural causes, Aristotle's belief was a By recognising important surface processes at marked step forward. Eratosthenes, a librarian at work, the Greek, Arabic and Roman civilisations Alexandria at about 200 BC, made surprisingly contributed to the growth of knowledge about the accurate measurements of the circumference of earth. -
Geochemistry of Granitic Aplite-Pegmatite Veins and Sills and Their Minerals from the Sabugal Area, Central Portugal
N. Jb. Miner. Abh. 188/3, 297 – 316 Fast Track Article PublishedStuttgart, Augustonline November2011 2011 Geochemistry of granitic aplite-pegmatite veins and sills and their minerals from the Sabugal area, central Portugal Ana M. R. Neiva, Paulo B. Silva and João M. F. Ramos With 19 fi gures and 12 tables Abstract: Granitic beryl-columbite-phosphate subtype aplite-pegmatite veins and sills from the Sabugal area intruded a biotite > muscovite granite which is related to another two-mica granite. Variation diagrams of major and trace elements of whole rocks δ18 show fractionation trends. REE patterns and O of whole rocks, BaO and P2O5 contents of K-feldspar, anorthite and P2O5 contents of plagioclase, major element and Li contents of muscovite and lithian muscovite support this series. Least squares analysis of ma- jor elements indicate that the biotite > muscovite granite and aplite-pegmatite veins and sills are derived from the earlier two-mica granite magma by fractional crystallization of quartz, plagioclase, K-feldspar, biotite and ilmenite. Modelling of trace elements shows that magmatic fl uxes and fl uids controlled the Rb, Sr and Ba contents of aplite-pegmatites,Paper probably also lithium micas (zin- nwaldite, polylithionite and rare lepidolite), cassiterite, columbite-tantalite, fl uorapatite and triplite. In aplite-pegmatites, lithian muscovite replaces primary muscovite and late lithium micas replace lithian muscovite. Complexely zoned columbite crystals are chemically characterized and attributed to disequilibrium conditions. Relations of granites and aplite-pegmatites and pegmatites from other Portuguese and Spanish areas are compared. The granitic aplite-pegmatites from Sabugal are moderately fractionated and the granitic complex type aplite-pegmatites from Gonçalo are the richest in Li and Sn, derived from a higher degree of frac- tional crystallization and fl uxes and fl uids control the Ba and Rb behaviours and Li, Sn, F and Ta concentrations. -
Decrepitation Characteristics of Igneous
DECREPITATIONCHARACTERISTICS OF IGNEOUSROCKS F. G. SMITH Unfuersi,tyof Toronto, Toronto, Canada Ansrnect ._lecrepitation during heating of igneous intrusive rocks is complex, but one stage (D2) appears to be due to misfit of solid inclusions. This stage begins at 6rb + g0'-b in simple granite pegmatite and aplite, Z0S * 80" C in ganiie, Z6E + 50" C in granodiorite and quartz norite, and 1010 + 60o C in gabbro and related rocks. The p2-sQS! of pegmatite and aplite in an area of migmatitic gneiss, with no exposed batholiths, starts at a lower temperature than the corresponding stage of decrepitation of the country gneiss. Introd,wction The rationale of decrepitation due to misfit of solid inclusions in minerals, when heated above the temperature of crystallization, was outlined previously (smith, L952a).A stage of decrepitation of several types of garnet was interpreted to be due to solid inclusions, becausethe frequency of decrepitation was found to be directly related to the abundanceof solid inclusions (smith, lg52b). A similar stage of decrepi- tation of high grade metamorphic rocks was found (Smith, lgb8). The measuredtemperatures of the beginning of this stage of decrepitation of metamorphic minerals are internally consistent, and are not at variance with the small amount of synthetic data. As a further test of the rationale. a few rocks representing several igneous rock clans were heated in the decrepitation apparatus. The results can be interpreted in an analogous manner to give the temperature of crystallization of the constituent minerals. These data, which should be considered as only tentative becauseof the small number in each clan tested, are given below, uncor- rected for the effect of pressiure. -
Lloyd Shoals
Southern Company Generation. 241 Ralph McGill Boulevard, NE BIN 10193 Atlanta, GA 30308-3374 404 506 7219 tel July 3, 2018 FERC Project No. 2336 Lloyd Shoals Project Notice of Intent to Relicense Lloyd Shoals Dam, Preliminary Application Document, Request for Designation under Section 7 of the Endangered Species Act and Request for Authorization to Initiate Consultation under Section 106 of the National Historic Preservation Act Ms. Kimberly D. Bose, Secretary Federal Energy Regulatory Commission 888 First Street, N.E. Washington, D.C. 20426 Dear Ms. Bose: On behalf of Georgia Power Company, Southern Company is filing this letter to indicate our intent to relicense the Lloyd Shoals Hydroelectric Project, FERC Project No. 2336 (Lloyd Shoals Project). We will file a complete application for a new license for Lloyd Shoals Project utilizing the Integrated Licensing Process (ILP) in accordance with the Federal Energy Regulatory Commission’s (Commission) regulations found at 18 CFR Part 5. The proposed Process, Plan and Schedule for the ILP proceeding is provided in Table 1 of the Preliminary Application Document included with this filing. We are also requesting through this filing designation as the Commission’s non-federal representative for consultation under Section 7 of the Endangered Species Act and authorization to initiate consultation under Section 106 of the National Historic Preservation Act. There are four components to this filing: 1) Cover Letter (Public) 2) Notification of Intent (Public) 3) Preliminary Application Document (Public) 4) Preliminary Application Document – Appendix C (CEII) If you require further information, please contact me at 404.506.7219. Sincerely, Courtenay R. -
“Tricks of the Trade” Revealed at 13Th
In This Issue Electronics Recycling News pg. 5,7 Georgia Recycles Spotlight on Programs pg. 8 SciTrek Program pg. 10 Volume 11 Issue 3 The Georgia Recycling Coalition Newsletter Spring 2004 “Tricks of the Trade” Revealed at 13th Annual Conference Dust off your top hat and polish that magic wand as GRC gears up for its 13th Annual Conference, Trade Show and Membership Meeting from September 12-15, 2004 at the Ocean Plaza Beach Resort on Tybee Island, GA. For our lucky 13th year gathering the theme is “Recycling Magic-Tricks of the Trade”. The agenda will include training sessions, project updates, educational programs, tours, industry vendors, the now infamous “Trash to Treasures” annual auction, and the latest information on markets and technology. There is always fun, recreation, relaxation, history, and great food on Tybee, one of Georgia’s most unique beach communities. So, Mark Your Calendar and look for registration information soon in the mail and on our website at www.georgiarecycles.org. See Call for Presentations on Page 2 for information on submitting proposals to be a speaker/presenter at this conference. Semi Annual Meeting Promotes Action on Initiatives At the March 2004 semi-annual meeting in Athens, speakers, discussions and round table sessions resulted in action steps on several GRC initiatives. The Communications Committee will be taking the “Why Is Recycling Important?” message to a Power Point presentation to be posted on our website and made available for member use. The Electronics Recycling round table discussions motivated local vendors to promote and participate in more residential collection of computers and computer peripherals via drop off sites and events handled by local program managers and KAB affiliates. -
Petrographic Study of a Quartz Diorite Stock Near Superior, Pinal County, Arizona
Petrographic study of a quartz diorite stock near Superior, Pinal County, Arizona Item Type text; Thesis-Reproduction (electronic); maps Authors Puckett, James Carl, 1940- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 23/09/2021 23:40:37 Link to Item http://hdl.handle.net/10150/554062 PETROGRAPHIC STUDY OF A QUARTZ DIORITE STOCK NEAR SUPERIOR, PINAL COUNTY, ARIZONA by James Carl Puckett, Jr. A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 0 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg ment the proposed use of the material is in the interests of scholar ship. In all other instances, however, permission must be obtained from the author. -
August 2005 Stone Mountain Park Master Plan
MASTER PLAN AMENDMENT REPORT August 15, 2005 GEORGIA’S STONE MOUNTAIN PARK MASTER PLAN AMENDMENT REPORT August 15, 2005 GEORGIA’S STONE MOUNTAIN PARK Robert and Company Engineers Architects Planners 96 Poplar Street, N.W. Atlanta, Georgia 30303 GEORGIA’S STONE MOUNTAIN PARK MASTER PLAN AMENDMENT REPORT TABLE OF CONTENTS SECTION PAGE INTRODUCTION i 1. HISTORY OF PLANNING AND DEVELOPMENT IN STONE MOUNTAIN PARK 1-1 2. KEY ELEMENTS OF THE 1992 MASTER PLAN 2-1 3. PRIVATIZATION AND THE LONG RANGE DEVELOPMENT PLAN 3-1 4. MASTER PLAN REFINEMENTS A. Park Center District 4-1 B. Natural District 4-3 C. Recreation District 4-4 D. Events District 4-4 5. TRANSPORTATION AND CIRCULATION 5-1 6. MANAGEMENT OF NATURAL AND HISTORICAL RESOURCES A. Summary Management Statement 6-1 B. Summary Management Recommendations 6-1 C. Vegetation Management Recommendations 6-2 D. Vegetation Inventory: Summary Field Survey 6-6 E. Natural District 6-9 7. LONG RANGE CAPITAL IMPROVEMENTS 7-1 GRAPHICS PAGE EXISTING LAND USE MAP ii PARK DISTRICT MAP 2-2 LONG RANGE PLAN 4-2 TRAFFIC CIRCULATION AND PARKING IMPROVEMENTS 5-3 NATURAL RESOURCES MAP 6-3 INTRODUCTION Georgia’s Stone Mountain Park is located 16 miles east of downtown Atlanta. The Park is comprised of approximately 3,200 acres of woodlands and features as its centerpiece, Stone Mountain, one of the world’s largest exposed granite monoliths. Within the Park’s boundaries there are also several lakes that cover a total of approximately 362 acres – Stone Mountain Lake is the largest at 323 acres. Often considered to be the State’s greatest natural tourist attraction, several million people visit Stone Mountain Park every year, making it one of the highest attendance attractions in the United States. -
Mineral Mania
The Rock Factory A Pre-Visit Information Guide for Teachers Meets Next Generation Science Standards: 5-PS1-3; MS LS4-1,2; MS ESS1-4; MS-ESS2-1 How does our Earth create so many different types of rocks? Learn about the different processes that form and reform rocks as you identify many types of rocks, minerals and fossils. Students will learn to think like geologists as they move through interactive investigation stations packed with specimens from the Museum’s collections. OBJECTIVES The Rock Cycle: Students will examine the three types of rocks - igneous, metamorphic and sedimentary – and discover the processes that create them. Tracing the connections between shale and slate, limestone and marble, students will discover how the rock cycle changes the very ground beneath our feet! Characteristics of Rocks Students will learn how to observe and identify rocks through their unique characteristics, looking for telling clues such as layering, crystal size, fossils, magnetism, and more. Students will practice their observational skills as they describe the Museum’s unique rock and mineral specimens. Investigation Stations: Students will explore Museum geology specimens up close at investigation stations to answer such questions as: “Why do fossils form only in certain rocks?” “How do rocks form from volcanic eruptions?” “How can I recognize different types of rocks?”. ACTIVITIES Teachers are encouraged to conduct pre-visit and post-visit classroom discussions and activities with their classes to make the most of their experience. Encourage your students to start a classroom rock collection, and create an exhibit with the rocks organized by type – igneous, sedimentary and metamorphic. -
Geologic Boulder Map of Campus Has Been Created As an Educational Educational an As Created Been Has Campus of Map Boulder Geologic The
Adam Larsen, Kevin Ansdell and Tim Prokopiuk Tim and Ansdell Kevin Larsen, Adam What is Geology? Igneous Geo-walk ing of marine creatures when the limestone was deposited. It also contains by edited and Written Geology is the study of the Earth, from the highest mountains to the core of The root of “igneous” is from the Latin word ignis meaning fire. Outlined in red, numerous fossils including gastropods, brachiopods, receptaculita and rugose the planet, and has traditionally been divided into physical geology and his- this path takes you across campus looking at these ancient “fire” rocks, some coral. The best example of these are in the Geology Building where the stone torical geology. Physical geology concentrates on the materials that compose of which may have been formed at great depths in the Earth’s crust. Created was hand-picked for its fossil display. Campus of the Earth and the natural processes that take place within the earth to shape by the cooling of magma or lava, they can widely vary in both grain size and Granite is another common building stone used on campus. When compa- its surface. Historical geology focuses on Earth history from its fiery begin- mineral composition. This walk stops at examples showing this variety to help nies sell granite, they do not use the same classification system as geologists. nings to the present. Geology also explores the interactions between the you understand what the change in circumstances will do to the appearance Granite is sold in many different colours and mineral compositions that a Map Boulder Geologic lithosphere (the solid Earth), the atmosphere, the biosphere (plants, animals of the rock. -
University of Nevada, Reno Igneous and Hydrothermal Geology of The
University of Nevada, Reno Igneous and Hydrothermal Geology of the Central Cherry Creek Range, White Pine County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by David J. Freedman Dr. Michael W. Ressel, Thesis Advisor May, 2018 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by DAVID JOSEPH FREEDMAN entitled Igneous and Hydrothermal Geology of the Central Cherry Creek Range, White Pine County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Michael W. Ressel, PhD, Advisor John L. Muntean, PhD, Committee Member Douglas P. Boyle, PhD, Graduate School Representative David W. Zeh, PhD, Dean, Graduate School May, 2018 i Abstract The central Cherry Creek Range exposes a nearly intact, 8-km thick crustal section of Precambrian through Eocene rocks in a west-dipping homocline. Similar tilts between Eocene volcanic rocks and underlying Paleozoic carbonates demonstrate that tilting and exhumation largely occurred during post-Eocene extensional faulting, thus allowing for relatively simple paleo-depth determinations of Eocene intrusions and mineral deposits. The study area is cored by the Cherry Creek quartz monzonite pluton (35 km2 exposure; ~132 km2 coincident magnetic anomaly), which was emplaced into Precambrian and Cambrian meta-sedimentary strata between 37.9-36.2 Ma and is exposed along the east side of the range. The pluton and overlying Paleozoic strata are cut by abundant 35.9-35.1 Ma porphyritic silicic dikes. A range of polymetallic mineralization styles are hosted by the intrusive rocks along two deeply-penetrating, high-angle faults and their intersections with favorable Paleozoic units. -
LAYERED PEGMATITE-APLITE Division of Earth Sciences, The
MINERALOGICAL SOCIETY OF AMERICA, SPECIAL PAPER 1, 1963 INTERNATIONALMINERALOGICALASSOCIATION,PAPERS, THIRD GENERAL MEETING LAYERED PEGMATITE-APLITE INTRUSIVES 1 RICHARD H. JAHNS AND O. FRANK TUTTLE Division of Earth Sciences, The Pennsylvania State University, University Park, Pennsylvania ABSTRACT Intrusive bodies of granitic pegmatite and aplite with simple or complex layering include those representing multiple injections of magma from external sources and those representing single injections of magma followed by segregation dur- ing crystallization. Those of the latter category can be subdivided into four classes, intergradations among which are not uncommon: 1. Bodies of aplite or fine-grained pegmatite with very large phenocrysts, or megacrysts. 2. Aplite bodies with mar- ginal or interior pegmatite masses generally formed in situ. 3. Pegmatite bodies with marginal or interior aplite masses formed in situ or by autoinjection. 4. Highly asymmetric bodies whose upper parts consist mainly or wholly of pegmatite and whose lower parts consist mainly or wholly of aplite. Zonal structure defines a gross layering within many pegmatite bodies, and a layer-like distribution of pegmatite and aplite also is common over a wide range of scales. Some of the aplites are faintly to distinctly flow layered, and others are featured by rhythmic layering in which adjacent thin and regular units differ from each other in composition. None of the observed types of layering is regarded as a result of crystal accumulation. The bulk composition of the layered intrusive bodies falls in the thermal valley of petrogeny's residua system at an average composition corresponding to a parent magma saturated with water at high pressures (e.g. -
(FP)-Rich Aplite-Pegmatites in the Central Iberian Zone Geologic
Ore Geology Reviews 95 (2018) 408–430 Contents lists available at ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev Petrogenetic relationships between Variscan granitoids and Li-(F-P)-rich T aplite-pegmatites in the Central Iberian Zone: Geological and geochemical constraints and implications for other regions from the European Variscides ⁎ E. Roda-Roblesa, , C. Villasecab, A. Pesqueraa, P.P. Gil-Crespoa, R. Vieirac, A. Limac, I. Garate-Olavea a Dpto. Mineralogía y Petrología, Universidad del País Vasco UPV/EHU, Barrio Sarriena s/n, 48940 Leioa, Spain b Dpto. Petrología y Geoquímica, Universidad Complutense, IGEO (UCM, CSIC), 28040 Madrid, Spain c Instituto de Ciências da Terra, Universidade do Porto/DGAOT, Rua do Campo Alegre 687, 4169-007 Porto, Portugal ARTICLE INFO ABSTRACT Keywords: The Central Iberian Zone (CIZ) is characterised by a large volume of Variscan granitic intrusions, which can be Li-rich aplite-pegmatites grouped into five types: (1) two-mica peraluminous leucogranites (S1); (2) P-rich highly peraluminous granites Granite batholiths (S2); (3) P-poor moderately peraluminous granites (S3); (4) moderately to low peraluminous granites (S4); and Geochemistry (5) I-type low peraluminous granites (I). Though not as abundant as granites, aplite-pegmatite rocks are Central Iberian Zone nonetheless widespread in this region, occurring either as fields of aplite-pegmatite dykes or as leucogranitic European Variscan Belt cupolas. They are commonly enriched in Li-(F-P) minerals such as spodumene, petalite, micas, and phosphates of the amblygonite-montebrasite and triphylite-lithiophilite series. Many of the Li-rich bodies show an aplitic texture, frequently with the development of layered units.