Calcite Marble and Dolomite of Eastern Vermont
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The I\,Iagnetic Separation of Soi'ie Alluvial I,Iinerals in I'ialaya*
THE AMERICAN MINERAI,OGIST, VOL. 41, JULY AUGUST, 1959 THE I\,IAGNETIC SEPARATION OF SOI'IE ALLUVIAL I,IINERALS IN I'IALAYA* B. H. FnNrant, Minerals Eramination Diaision, GeologicalSurttey D epartment, F'ederotion of M al,aya. Assrnlcr This paper presents the results of a seriesof magnetic separationswhich have been in- vestigated {or a number of minerals occurring in X{alayan alluvial concentrates.The pur- pose of the investigations was to establish,by the isolation of individual mineral species,a reproducible and reliable method for the identification and quantitative estimation of minerals in alluvial concentrates examined by the Geological Survey in Malaya In par- ticular was sought the isolation of columbite from ubiquitous ilmenite. All the separations were made on the small, highly sensitive Frantz Isodynamic Model L-1 laboratory separa- tor, The minerals which have been successfully separated include ailanite, anatase, andalu- site (and chiastolite), arsenopyrite, brookite, cassiterite,columbite, epidote, gahnite, garnet (pink), ilmenite, manganeseoxide (51.6/e Mn), monazite, pyrite, rutile, scheelite,siderite, staurolite, thorite, topaz, tourmaline, uranoan monazite, wolframite, xenotime, and zircon. PnocBpunp When using an inclined feed, the Frantz Isodynamic separator (see Figs. 1(A) & (B)) hasthree inherent variables. These are the field strengLh (current used),the sideslope, and the forward slope. 5;6s $lope wdrd 511)Pe (A) (B) Irc. 1. Diagrammatic representation of side slope and forward slope. The field strength is increasedby means of a rheostat which raises the current from zero in stagesof 0.05 amps. to 1.4 amps. Early in the investigationsit was decidedthat stepsof 0.1 amp. would be sufficiently gradual. -
INCLUSIONS in AQUAMARINE from AMBATOFOTSIKELY, MADAGASCAR Fabrice Danet, Marie Schoor, Jean-Claude Boulliard, Daniel R
NEW Danet G&G Fall 2012_Layout 1 9/27/12 11:31 AM Page 205 RAPID COMMUNICATIONS INCLUSIONS IN AQUAMARINE FROM AMBATOFOTSIKELY, MADAGASCAR Fabrice Danet, Marie Schoor, Jean-Claude Boulliard, Daniel R. Neuville, Olivier Beyssac, and Vincent Bourgoin grams of translucent to transparent beryl were pro- duced, as well as several tonnes of opaque material In January 2012, aquamarine crystals containing for industrial use. While only a very small percentage interesting inclusions were extracted from the Am- was suitable for faceting, several hundred aqua- batofotsikely area northwest of Antsirabe, Mada- marines in the 1–35 ct range have been cut. In April gascar. These specimens displayed various types 2012, one of the authors (FD) traveled to the locality of eye-visible and microscopic inclusions, and and obtained representative samples. some had an unusual form. Raman microspec- troscopy identified reddish brown plate lets as Location and Geologic Setting. The workings are lo- hematite, while ilmenite was found as black cated less than 1 km north of Ambatofotsikely (a village platelets, black needles, and distinctive dark gray now locally known as Ambatofotsy Carole), 22 km dendrites. Similar inclusions are known in beryl north-northwest of Ankazomiriotra, and 74 km north- from Brazil, India, Mozambique, and Sri Lanka. west of Antsirabe. The deposit is centered at coordinates 19°27.662¢S, 46°27.450¢E, at an elevation of 1,010 m. The site is accessed by a paved road (RN 34) from ining activity near the central Malagasy village Antsirabe to a point 16 km west of Ankazomiriotra. of Ambatofotsikely was first documented nearly From there, a trail extends 15 km to Ambatofotsikely. -
Mineralogy and Origin of the Titanium
MINERALOGY AND ORIGIN OF THE TITANIUM DEPOSIT AT PLUMA HIDALGO, OAXACA, MEXICO by EDWIN G. PAULSON S. B., Massachusetts Institute of Technology (1961) SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY May 18, 1962 Signature of At r . Depardnent of loggand Geophysics, May 18, 1962 Certified by Thesis Supervisor Ab Accepted by ...... Chairman, Departmental Committee on Graduate Students M Abstract Mineralogy and Origin of the Titanium Deposit at Pluma Hidalgo, Oaxaca, Mexico by Edwin G. Paulson "Submitted to the Department of Geology and Geophysics on May 18, 1962 in partial fulfillment of the requirements for the degree of Master of Science." The Pluma Hidalgo titanium deposits are located in the southern part of the State of Oaxaca, Mexico, in an area noted for its rugged terrain, dense vegetation and high rainfall. Little is known of the general and structural geology of the region. The country rocks in the area are a series of gneisses containing quartz, feldspar, and ferromagnesians as the dominant minerals. These gneisses bear some resemblance to granulites as described in the literature. Titanium minerals, ilmenite and rutile, occur as disseminated crystals in the country rock, which seems to grade into more massive and large replacement bodies, in places controlled by faulting and fracturing. Propylitization is the main type of alteration. The mineralogy of the area is considered in some detail. It is remarkably similar to that found at the Nelson County, Virginia, titanium deposits. The main minerals are oligoclase - andesine antiperthite, oligoclase- andesine, microcline, quartz, augite, amphibole, chlorite, sericite, clinozoi- site, ilmenite, rutile, and apatite. -
The Geology of the Lyndonville Area, Vermont
THE GEOLOGY OF THE LYNDONVILLE AREA, VERMONT By JOHN G. DENNIS VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, Stale Geologist Published by VERMONT DEVELOPMENT COMMISSION MONTPELIER, VERMONT BULLETIN NO. 8 1956 Lake Willoughby, seen from its north shore. TABLE OF CONTENTS ABSTRACT ......................... 7 INTRODUCTION 8 Location 8 Geologic Setting ..................... 8 Previous Work ...................... 8 Purpose of Study ..................... 9 Method of Study 10 Acknowledgments . 11 Physiography ...................... 11 STRATIGRAPHY ....................... 16 Lithologic Descriptions .................. 16 Waits River Formation ................. 16 General Statement .................. 16 Distribution ..................... 16 Age 17 Lithological Detail .................. 17 Gile Mountain Formation ................ 19 General Statement .................. 19 Distribution ..................... 20 Lithologic Detail ................... 20 The Waits River /Gile Mountain Contact ........ 22 Age........................... 23 Preliminary Remarks .................. 23 Early Work ...................... 23 Richardson's Work in Eastern Vermont .......... 25 Recent Detailed Mapping in the Waits River Formation. 26 Detailed Work in Canada ................ 28 Relationships in the Connecticut River Valley, Vermont and New Hampshire ................... 30 Summary of Presently Held Opinions ........... 32 Discussion ....................... 32 Conclusions ...................... 33 STRUCTURE 34 Introduction and Structural Setting 34 Terminology ...................... -
Weathering of Ilmenite from Granite and Chlorite Schist in the Georgia Piedmont
American Mineralogist, Volume 87, pages 1616–1625, 2002 Weathering of ilmenite from granite and chlorite schist in the Georgia Piedmont PAUL A. SCHROEDER,* JOHN J. LE GOLVAN, AND MICHAEL F. RODEN Department of Geology, University of Georgia, Athens, Georgia 30602-2501, U.S.A. ABSTRACT Ilmenite grains from weathering profiles developed on granite and ultramafic chlorite schist in the Georgia Piedmont were studied for evidence of morphological and chemical alteration. Ilmenite- rich concentrates from the fine sand (90–150 mm) component were studied to test the assumption that there is no difference between ilmenite in the parent rock and that in colluvium delivered to primary drainage systems. Ilmenite grains in the granite profile are rounded to subhedral, and commonly contain hematite exsolution blebs. Dissolution pits are observed along the boundaries of the exsolution blebs, with goethite occurring as an alteration product. Ilmenite grains in the schist profile occur as fractured anhedral grains with uncommon lamellae of rutile. Grain fractures are filled with goethite and he- matite, particularly in the B-horizon. Ilmenite from the granite profile is Mn rich (7–15 mol% MnTiO3), whereas ilmenite from the schist profile contains only 1–2 mol% MnTiO3 and up to 8 mol% MgTiO3. Two populations of grains develop in both profiles. Grains with abundant exsolution blebs and fractures alter through a proposed two-step reaction mechanism. It is proposed that il- menite first undergoes a solid-state transformation to pseudorutile via an anodic oxidation mecha- nism. Oxidized Fe and Mn diffuse from the structure and precipitate as goethite and MnO2. Pseudorutile is ephemeral and undergoes incongruent dissolution to form anatase, hematite, and goethite. -
Okemo State Forest - Healdville Trail Forest - Healdville Okemo State B
OKEMO STATE FOREST - HEALDVILLE TRAIL North 3000 OKEMO MOUNTAIN RESORT SKI LEASEHOLD AREA OKEMO MOUNTAIN ROAD (paved) 2500 2000 Coleman Brook HEALDVILLE TRAIL 1500 to Ludlow - 5 miles STATION RD railroad tracks HEALDVILLE RD HEALDVILLE VERMONT UTTERMILK F 103 B AL LS RD to Rutland - 16 miles Buttermilk Falls 0 500 1000 2000 3000 feet 1500 LEGEND Foot trail Vista Town highway State highway Lookout tower FORESTS, PARKS & RECREATION State forest highway (not maintained Parking area (not maintained in winter) VERMONT in winter) Gate, barricade Stream AGENCY OF NATURAL RESOURCES Ski chairlift Ski area leasehold boundary 02/2013-ephelps Healdville Trail - Okemo State Forest the property in 1935. Construction projects by the CCC The Healdville Trail climbs from the base to the include the fire tower, a ranger’s cabin and an automobile summit of Okemo Mountain in Ludlow and Mount Holly. access road. The majority of Okemo Mountain Resort’s Highlights of this trail include the former fire lookout ski terrain is located within a leased portion of Okemo tower on the summit and a vista along the trail with State Forest. Okemo State Forest is managed for Okemo views to the north and west. Crews from the Vermont multiple uses under a long-term management plan; these Youth Conservation Corps constructed the trail under the uses include forest products, recreation and wildlife direction of the Vermont Department of Forests, Parks habitat. Okemo State Forest provides an important State Forest and Recreation during the summers of 1991-1993. wildlife corridor between Green Mountain National Forest lands to the south and Coolidge State Forest to the Trail Facts north. -
Southeast Region
VT Dept. of Forests, Parks and Recreation Mud Season Trail Status List is updated weekly. Please visit www.trailfinder.info for more information. Southeast Region Trail Name Parcel Trail Status Bear Hill Trail Allis State Park Closed Amity Pond Trail Amity Pond Natural Area Closed Echo Lake Vista Trail Camp Plymouth State Park Caution Curtis Hollow Road Coolidge State Forest (east) Open Slack Hill Trail Coolidge State Park Closed CCC Trail Coolidge State Park Closed Myron Dutton Trail Dutton Pines State Park Open Sunset Trail Fort Dummer State Park Open Broad Brook Trail Fort Dummer State Park Open Sunrise Trail Fort Dummer State Park Open Kent Brook Trail Gifford Woods State Park Closed Appalachian Trail Gifford Woods State Park Closed Old Growth Interpretive Trail Gifford Woods State Park Closed West River Trail Jamaica State Park Open Overlook Trail Jamaica State Park Closed Hamilton Falls Trail Jamaica State Park Closed Lowell Lake Trail Lowell Lake State Park Closed Gated Road Molly Beattie State Forest Closed Mt. Olga Trail Molly Stark State Park Closed Weathersfield Trail Mt. Ascutney State Park Closed Windsor Trail Mt. Ascutney State Park Closed Futures Trail Mt. Ascutney State Park Closed Mt. Ascutney Parkway Mt. Ascutney State Park Open Brownsville Trail Mt. Ascutney State Park Closed Gated Roads Muckross State Park Open Healdville Trail Okemo State Forest Closed Government Road Okemo State Forest Closed Mountain Road Okemo State Forest Closed Gated Roads Proctor Piper State Forest Open Quechee Gorge Trail Quechee Gorge State Park Caution VINS Nature Center Trail Quechee Gorge State Park Open Park Roads Silver Lake State Park Open Sweet Pond Trail Sweet Pond State Park Open Thetford Academy Trail Thetford Hill State Park Closed Gated Roads Thetford Hill State Park Open Bald Mt. -
Porphyry Deposits
PORPHYRY DEPOSITS W.D. SINCLAIR Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, K1A 0E8 E-mail: [email protected] Definition Au (±Ag, Cu, Mo) Mo (±W, Sn) Porphyry deposits are large, low- to medium-grade W-Mo (±Bi, Sn) deposits in which primary (hypogene) ore minerals are dom- Sn (±W, Mo, Ag, Bi, Cu, Zn, In) inantly structurally controlled and which are spatially and Sn-Ag (±W, Cu, Zn, Mo, Bi) genetically related to felsic to intermediate porphyritic intru- Ag (±Au, Zn, Pb) sions (Kirkham, 1972). The large size and structural control (e.g., veins, vein sets, stockworks, fractures, 'crackled zones' For deposits with currently subeconomic grades and and breccia pipes) serve to distinguish porphyry deposits tonnages, subtypes are based on probable coproduct and from a variety of deposits that may be peripherally associat- byproduct metals, assuming that the deposits were econom- ed, including skarns, high-temperature mantos, breccia ic. pipes, peripheral mesothermal veins, and epithermal pre- Geographical Distribution cious-metal deposits. Secondary minerals may be developed in supergene-enriched zones in porphyry Cu deposits by weathering of primary sulphides. Such zones typically have Porphyry deposits occur throughout the world in a series significantly higher Cu grades, thereby enhancing the poten- of extensive, relatively narrow, linear metallogenic tial for economic exploitation. provinces (Fig. 1). They are predominantly associated with The following subtypes of porphyry deposits are Mesozoic to Cenozoic orogenic belts in western North and defined according to the metals that are essential to the eco- South America and around the western margin of the Pacific nomics of the deposit (metals that are byproducts or poten- Basin, particularly within the South East Asian Archipelago. -
Geologic Evolution of Trail Ridge Eolian Heavy-Mineral Sand and Underlying Peat, Northern Florida
Georgia Southern University Digital Commons@Georgia Southern Geology and Geography Faculty Publications Geology and Geography, Department of 1989 Geologic Evolution of Trail Ridge Eolian Heavy-Mineral Sand and Underlying Peat, Northern Florida Eric Force U.S. Geological Survey Fredrick J. Rich Georgia Southern University, [email protected] Follow this and additional works at: https://digitalcommons.georgiasouthern.edu/geo-facpubs Part of the Geography Commons, and the Geology Commons Recommended Citation Force, Eric, Fredrick J. Rich. 1989. "Geologic Evolution of Trail Ridge Eolian Heavy-Mineral Sand and Underlying Peat, Northern Florida." U.S. Geological Survey Professional Paper 1499: 1-23 Washington, DC: United States Government Printing Office. source: https://pubs.er.usgs.gov/publication/pp1499 https://digitalcommons.georgiasouthern.edu/geo-facpubs/117 This article is brought to you for free and open access by the Geology and Geography, Department of at Digital Commons@Georgia Southern. It has been accepted for inclusion in Geology and Geography Faculty Publications by an authorized administrator of Digital Commons@Georgia Southern. For more information, please contact [email protected]. Geologic Evolution of Trail Ridge EoMmn Peat, Northern Florida AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur- rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur- vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. -
Quarterly of the Green Mountain Club Spring 2016
NEWS Quarterly of the Green Mountain Club SPRING 2016 LONG TRAIL NEWS • SPRING 2016 | 1 The mission of the Green Mountain Club is to make the Vermont mountains play a larger part in the life of the people by protecting and maintaining the Long Trail System and EBECCA FULLERTON fostering, through education, the stewardship R of Vermont’s hiking trails and mountains. ON BY I Quarterly of the ILLUSTRAT Green Mountain Club CONTENTS Michael DeBonis, Executive Director Spring 2016, Volume 76, No. 1 Jocelyn Hebert, Long Trail News Editor Richard Andrews, Volunteer Copy Editor Sly Dog Studio, Design FEATURES Green Mountain Club 4711 Waterbury-Stowe Road Waterbury Center, Vermont 05677 5 / Tribute to Sam Parisi Phone: (802) 244-7037 By Matt Wels Fax: (802) 244-5867 E-mail: [email protected] 6 / Evolution of the Trail Backpack Website: www.greenmountainclub.org TheLong Trail News is published by The Green By Mike DeBonis Mountain Club, Inc., a nonprofit organization founded in 1910. In a 1971 Joint Resolution, the Vermont 8 / Stone, Wood and Iron: A Photo Essay Legislature designated the Green Mountain Club the “founder, sponsor, defender and protector of the Long 10 / The Northern Hardwood Forest Trail System...” By Squirrel Johnson Contributions of manuscripts, photos, illustrations, and news are welcome from members and nonmembers. Copy and advertising deadlines are December 22 for the 11 / Bear Necessity spring issue; March 22 for summer; June 22 for fall; and September 22 for winter. 12 / A Collective Connection to the Land The opinions expressed byLTN contributors and By Caitlin Miller advertisers are not necessarily those of GMC. -
The Magnetite-Series and Ilmenite-Series Granitoids in Chile
MINING GEOLOGY,30(3),183•`190,1980 The Magnetite-series and Ilmenite-series Granitoids in Chile Shunso ISHIHARA*and Carlos E. ULRIKSEN** Abstract: Paleozoic and Mesozoic-Cenozoic granitoids of the Chilean Andes were studied magnetically in the area between Latitude 22-35•KS. The Paleozoic granitoids are found to be composed of the ilmenite-series and weakly magnetic magnetite-series, whereas all the Mesozoic-Cenozoic ones appear to be the magnetite-series. Lack of significant sulfide deposits in the Paleozoic terrains may have been resulted from the reducing nature of the granitic magmatism. Within the magnetite-series terrains of Mesozoic-Cenozoic age, magnetic susceptibility of the granitoids seems to increase continentward. Granitoids related to porphyry copper deposits in the Andean Cordillera have higher magnetic susceptibility than those occurring in the Coast Range which could be genetically associated with manto-type deposits. The different styles of mineralization may possibly be in consequence of the different oxidation status of the granitic magmatism. areas are shown in Figure 1. Introduction Granitoids in Chile Granitoids in the Chilean Andes are dis- tributed continuously from the Peruvian coast Granitoids of Chile occupy about 30 percent batholiths (18•KS) to the southern tip of South of the total land area and occur as large America (54•KS) for more than 4,000 km. These batholiths to small intrusive plugs which may granitoids range in composition, from quartz have brought the effusive equivalents to the diorite to granite, and show different mode of surface along the Andean orogenic belt. Their occurrence, from catazonal to epizonal. Some exposure is seen in two lanes in the northern of the epizonal granitoids are associated with half (18-38•KS); one along the coast while the well-known prophyry copper and manto-type other in the Andean Cordillera. -
Winter 2020 Long Trail News
NEWS Quarterly of the Green Mountain Club WINTER 2020 Codding Hollow Property Conserved | Managing Trails During a Global Pandemic | Winter Hiking Safety Side-to-Side in Less Than a Week | Skiing Vermont’s Highest Peaks CONTENTS Winter 2020, Volume 80, No. 3 The mission of the Green Mountain Club is to make the Vermont mountains play a larger part in the life of the people by protecting and maintaining the Long Trail System and fostering, through education, the stewardship of Vermont’s hiking trails and mountains. Quarterly of the Green Mountain Club Michael DeBonis, Executive Director Alicia DiCocco, Director of Development & Communications PHOTO BY ALICIA DICOCCO Becky Riley and Hugh DiCocco on Mt. Mansfield Ilana Copel, Communications Assistant Richard Andrews, Volunteer Copy Editor Sylvie Vidrine, Graphic Designer FEATURES Green Mountain Club 4711 Waterbury-Stowe Road ❯ Waterbury Center, Vermont 05677 6 Celebrating Success after 34 years: Phone: (802) 244-7037 Codding Hollow Property Conserved Fax: (802) 244-5867 E-mail: [email protected] by Mollie Flanigan Website: greenmountainclub.org ❯ The Long Trail News is published by The 10 Managing Trails During a Global Pandemic: Green Mountain Club, Inc., a nonprofit Field Staff Reflections of the 2020 Season organization founded in 1910. In a 1971 Joint Resolution, the Vermont Legislature by John Plummer designated the Green Mountain Club the “founder, sponsor, defender and protector of 12 ❯ Hiking Trails During a Global Pandemic: the Long Trail System...” Hiker Reflections of the 2020 Season Contributions of manuscripts, photos, illustrations, and news are welcome from by Rick Dugan members and nonmembers. ❯ The opinions expressed byLTN contributors 16 Going the Distance: are not necessarily those of GMC.