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Watkins Creek Ranch Gallatin MT Property Name County State
NPS Form 10-900a OMB No. 1024-0018 (8-86) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLACES CONTINUATION SHEET Section ___ Page __ SUPPLEMENTARY LISTING RECORD NRIS Reference Number: 06001180 Date Listed: 12/27/2006 Watkins Creek Ranch Gallatin MT Property Name County State N/A Multiple Name This property is listed in the National Register of Historic Places in accordance with the attached nomination documentation subject to the following exceptions, exclusions, or amendments, notwithstanding the National Park Service certification included in the nomination documentation. / Signatu^e/cof the Keeper Da&e 6f Action / U =====7I^== Amended Items in Nomination: Description: The correct Town, Range, Section notation in the first paragraph should read: Range 4 Easf. The sawed ends of the corner logs on the Isabel & Frederick Lincoln Cabin (Building #9) are not tapered, as they are on the similar Guest Duplex Cabins (#6-8), marking the slightly different form and details of the later cabin. These clarifications were confirmed with the MT SHPO office. DISTRIBUTION: National Register property file Nominating Authority (without nomination attachment) NFS Form 10-900 0MB No. 1024-0018 (Rev. Oct. 1990) National Park Service RECEIVED 2280 NATIONAL REGISTER OF HISTORIC PLACES REGISTRATION FORM 3 NAT PF<N MATIAMAI OADl/ irK'k/rJ-" uco iiniruiiriL i nilM OLIIVILC 1. Name of Property historic name: Watkins Creek Ranch other name/site number: Firehole Ranch 2. Location street & number: 1207 Firehole Ranch Road not for publication: n/a vicinity: n/a city/town: West Yellowstone state: Montana code: MT county: Gallatin code: 031 zip code: 59758 3. -
Applicability of Siberian Placer Mining Technology to Alaska
MIRL Report No. 89 Applicability- - of Siberian Placer Mining Technology to Alaska Dr. Frank J. Skudrzyk, Project Manager E++W Engineering Consultants 461 1 Dartmouth Fairbanks, Alaska James C,Barker U.S. Bureau of Mines Alaska Field Operations Cenkr Fairbanks. Alaska Daniel E. Walsh School of Mineral Engineering University of Alaska Fairbanks Fairbanks, Alaska Rocky MacDonald American Arctic Company Fairbanks, Alaska Library of Congress Cataloging in Publication Data Library of Congress Catalog Card Number: 9 1-6 1923 ISBN 0-911043-12-8 May, 1991 Published bv Mined Industry Research Laboratory 212 ONeill Building University of Alaska Fairbanks Fairbanks, Alaska 99775-1 180 Alaska Science and Technology Foundation 550 West 7th Avenue Suite 360 Anchorage, Alaska 99501 ABSTRACT The result of Perestroyka and Glasnost has been an awakening of potential for cooperation between East and West. Nowhere has that been better demonstrated than between Alaska and Magadan Province, USSR. This report summarizes a one year effort financed by ASTF, with participation from several technical organizations, to establish contacts with the Siberian placer mining industry. The purpose of the project was to provide initial assessment of the Soviet technology for placer mining in permafrost. A ten day trip to Magadan province by an ASTF team and a similar length visit to Alaska by the Soviet mining group representing the All Union Scientific and Research Institute of Gold and Rare Metals, (VNII-I), Magadan are described. The report also reviews translated data on mining in permafrost and describes surface and underground placer mining technology developed by the Soviets. The report also lists relevant publications on Soviet mining research and state of the art Soviet mining technology and expertise. -
The Red Emerald
The Red Emerald Black Album Words by Seth William Rozendaal Photos by David Rozendaal This work is for the enjoyment of gemstone aficionados around the world and throughout time, and dedicated to the divine muse who inspires everything. This book celebrates the Red Emerald’s public debut at the 2017 Tucson Gem and Mineral Show. Graphics taken from the Mineralogical Record Volume 47 Number 1: Colombian Emeralds where noted. The two photos of the Heart matrix specimen on the top of the page in Section VI were taken by Wayne Schrimp. Seth Rozendaal is responsible for the landscape photo in Section II, the beveled heart in Section VI and Office Suite Graphics. The Suite Treasure necklace photo in Section XIII was taken at the Brent Isenberger Studio. Cover and all other interior photos in this album were taken by David Rozendaal. Without his tireless dedication, this publication would not have been possible. For additional information, please contact: Seth William Rozendaal (515) 868-7207 [email protected] Index I - Red Beryl IS Red Emerald II - Formation III - Matrix Specimens IV - Wafers V - Prisms VI - Twins VII - Clusters VIII - Bixbyite Combinations IX - Topaz Combinations X - Hourglass Patterning XI - The Scarlet Spectrum XII - Facet-Grade Red Emerald XIII - The Red Emerald Suite Treasure I ~ Red Beryl IS Red Emerald The human infatuation with Emeralds runs so deep, and our desire for them traces so far back… It's one of the only gemstones found in rank-signifying Neolithic headdresses. Yeah, you heard me: Caveman Crowns. Aja Raden - Author, Historian and Scientist Diamonds may be forever, but only Emeralds are eternal; our appreciation of Emeralds stretches from the beginning of human civilization to the very end. -
Hawaiian Volcanoes US$1225
The Geological Society of America’s Explore Hawaiian Volcanoes FIELD EXPERIENCE 27 July - 4 August 2014 Experience the wonders of active volcanism on the Earth’s most accessable and active volcano - Kilauea on the Big Island of Hawaii! This eight-day field trip on the Big Island of Hawaii will expand your knowl- edge in the field of plate tectonics, hot spot volcanism and the geologic features and hazards associated with living on an active volcano. We will discuss volcanic edifices, eruption styles, magma evolution and see various types of lava flows, lava lakes, tree molds and lava trees, fault scarps, rifts, craters and calderas. We will use our observations and new- found knowledge to discuss methods on how to effectively communicate geologic concepts. We will model inquiry in the field. US Prince does not include$1225 airfares to/from Hilo, HI. Trip ITINERARY* Sunday, July 27 - Participants arrive in Hilo, Hawaii for transfer via van to Kilauea Military Camp. No meals pro- vided. We will go to dinner as a group at Ken’s House of Pancakes (at your own expense) Monday, July 28 - Overview/logistics, Kilauea Visitor Center, Steaming Bluffs, Sulphur Banks, Kilauea Overlook, HVO, Jaggar Museum, SW Rift, Halema’uma’u Overlook (if open), Keanakako’I overlook, Devastation Trail, Pu’u Pua’i Overlook. ~ 4 miles of hiking on easy trails. BLD. Tuesday, July 29 - Chain of Craters Road including stops at Lua Manu Crater, Pauahi Crater and others, Mauna Ulu trail to Pu’u Huluhulu, Kealakomo Overlook, Alanui Kahiko, P’u Loa Petroglyphs, Holei Sea Arch, end of Chain of Craters Road. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Intergrown Emerald Specimen from Chivor Tity Was Confirmed by Raman Spectroscopy
Editor Nathan Renfro Contributing Editors Elise A. Skalwold and John I. Koivula Intergrown Emerald Specimen from Chivor tity was confirmed by Raman spectroscopy. The inclusion exhibited a well-formed hexagonal prismatic shape with Colombia’s Chivor emerald mines are located in the east- pyramid-like termination (figure 2). Although intergrowth ern zone of the Eastern Cordillera range of the Andes emerald crystals have been described and documented in Mountains. Chivor translates to “green and rich land” in the literature several times (G. Grundmann and G. Giu- Chibcha, the language of the indigenous people who were liani, “Emeralds of the world,” in G. Giuliani et al., Eds., already mining emerald more than 500 years ago, before Emeralds of the World, extraLapis English, No. 2, 2002, pp. the arrival of the Spanish conquistadors (D. Fortaleché et al., “The Colombian emerald industry: Winds of change,” Fall 2017 G&G, pp. 332–358). Chivor emeralds exhibit a bright green color with a tint of blue; they have relatively Figure 1. An emerald crystal inclusion measuring high clarity and fewer inclusions than emeralds found in ~2.67 × 2.71 × 5.43 mm is found inside this large Colombia’s western belt. emerald specimen (18.35 × 10.69 × 9.79 mm) from Colombia’s Chivor mine. Photo by John Jairo Zamora. The authors recently examined a rough emerald crystal specimen (figure 1), measuring 18.35 × 10.69 × 9.79 mm, reportedly from Chivor. This crystal weighed 3.22 g (16.10 ct) and had a prismatic hexagonal crystal shape. Standard gemological examination confirmed the gemstone to be emerald, and ultraviolet/visible/near-infrared (UV-Vis-NIR) spectroscopy showed a classic Colombian emerald absorp- tion spectrum. -
Rediscovery of the Elements — a Historical Sketch of the Discoveries
REDISCOVERY OF THE ELEMENTS — A HISTORICAL SKETCH OF THE DISCOVERIES TABLE OF CONTENTS incantations. The ancient Greeks were the first to Introduction ........................1 address the question of what these principles 1. The Ancients .....................3 might be. Water was the obvious basic 2. The Alchemists ...................9 essence, and Aristotle expanded the Greek 3. The Miners ......................14 philosophy to encompass a obscure mixture of 4. Lavoisier and Phlogiston ...........23 four elements — fire, earth, water, and air — 5. Halogens from Salts ...............30 as being responsible for the makeup of all 6. Humphry Davy and the Voltaic Pile ..35 materials of the earth. As late as 1777, scien- 7. Using Davy's Metals ..............41 tific texts embraced these four elements, even 8. Platinum and the Noble Metals ......46 though a over-whelming body of evidence 9. The Periodic Table ................52 pointed out many contradictions. It was taking 10. The Bunsen Burner Shows its Colors 57 thousands of years for mankind to evolve his 11. The Rare Earths .................61 thinking from Principles — which were 12. The Inert Gases .................68 ethereal notions describing the perceptions of 13. The Radioactive Elements .........73 this material world — to Elements — real, 14. Moseley and Atomic Numbers .....81 concrete basic stuff of this universe. 15. The Artificial Elements ...........85 The alchemists, who devoted untold Epilogue ..........................94 grueling hours to transmute metals into gold, Figs. 1-3. Mendeleev's Periodic Tables 95-97 believed that in addition to the four Aristo- Fig. 4. Brauner's 1902 Periodic Table ...98 telian elements, two principles gave rise to all Fig. 5. Periodic Table, 1925 ...........99 natural substances: mercury and sulfur. -
Garnet, Industrial 2016
2016 Minerals Yearbook GARNET, INDUSTRIAL [ADVANCE RELEASE] U.S. Department of the Interior September 2018 U.S. Geological Survey Garnet, Industrial By Robert M. Callaghan and Kenneth C. Curry Domestic survey data and table were prepared by Chanda C. Williams, statistical assistant. In 2016, U.S. production of crude garnet concentrate for combination with one or two other minerals, have reserves that industrial use was estimated to be 56,400 metric tons (t) valued can be mined at a low cost, and have the ability to react rapidly at about $12.8 million, a slight increase in tonnage and virtually to changes in market demand. The value of industrial garnet is unchanged in value from 55,200 t valued at $12.7 million in 2015. influenced by the size and grade of reserves, the type and quality U.S. production of refined garnet in 2016 was estimated to be of garnet mined, the proximity of deposits to infrastructure and 49,400 t valued at $24.4 million, a slight increase in tonnage and consumers, and the milling costs. The majority of industrial- a slight decrease in value from 48,700 t valued at $24.8 million grade garnet mined in the United States consists of almandine in 2015. U.S. exports of industrial garnet were 13,400 t, a 9% (iron-aluminum silicate) and pyrope (magnesium-aluminum decrease compared with those in 2015. Imports of garnet were silicate), although some andradite (calcium-iron silicate) also is estimated to be 150,000 t in 2016, a 38% decrease compared with mined domestically. -
Rare Earth Elements in Planetary Crusts: Insights from Chemically Evolved Igneous Suites on Earth and the Moon
minerals Article Rare Earth Elements in Planetary Crusts: Insights from Chemically Evolved Igneous Suites on Earth and the Moon Claire L. McLeod 1,* and Barry J. Shaulis 2 1 Department of Geology and Environmental Earth Sciences, 203 Shideler Hall, Miami University, Oxford, OH 45056, USA 2 Department of Geosciences, Trace Element and Radiogenic Isotope Lab (TRaIL), University of Arkansas, Fayetteville, AR 72701, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-513-529-9662 Received: 5 July 2018; Accepted: 8 October 2018; Published: 16 October 2018 Abstract: The abundance of the rare earth elements (REEs) in Earth’s crust has become the intense focus of study in recent years due to the increasing societal demand for REEs, their increasing utilization in modern-day technology, and the geopolitics associated with their global distribution. Within the context of chemically evolved igneous suites, 122 REE deposits have been identified as being associated with intrusive dike, granitic pegmatites, carbonatites, and alkaline igneous rocks, including A-type granites and undersaturated rocks. These REE resource minerals are not unlimited and with a 5–10% growth in global demand for REEs per annum, consideration of other potential REE sources and their geological and chemical associations is warranted. The Earth’s moon is a planetary object that underwent silicate-metal differentiation early during its history. Following ~99% solidification of a primordial lunar magma ocean, residual liquids were enriched in potassium, REE, and phosphorus (KREEP). While this reservoir has not been directly sampled, its chemical signature has been identified in several lunar lithologies and the Procellarum KREEP Terrane (PKT) on the lunar nearside has an estimated volume of KREEP-rich lithologies at depth of 2.2 × 108 km3. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
DOCUMENT RESUME ED 079 711 TITLE Reading Language Arts
DOCUMENT RESUME ED 079 711 CS 000 .670 TITLE Reading Language Arts Curriculum Guide, Grades 1-2-3, Book Two.. INSTITUTION Vermilion Parish School Board, Abbeville, La. PUB DATE 70 NOTE 128p.. EDRS PRICE ME -$0.65 HC-S6.58 DESCRIPTORS Beginning Reading; *Curriculiu Guides; *Developmental Reading; *Primary Grades; Reading; Reading Improvement; Reading Instruction; Reading Materials; *Reading Programs; *Reading Skills - IDENTIFIERS Elementary Secondary Education Act Title III ABSTRACT This language arts curriculum guide focuses primarily on reading instruction for students in grades one, two,and three. The topics discussed in this guide include an introduction to reading; major steps in developmental reading instruction; suggested time allotments for the Ginn Reading Program; scope and sequence charts; a checklist -for evaluating progress in reading; a guide for the use of supplementary material; grouping for effective reading instruction; experience and enrichment charts in a reading program; suggested activities and games; and the use of the overhead projector- in reading instruction..A bibliography of professional and instructional books is also included..(WR) U S DEPARTMENT OF HEALTH, EDUCATION A WELFARE NATIONAL INSTITUTE OF EDUCATION THIS DOCUMENT HAS BEEN REPRO DUCED EXACTLY AS RECEIVED FROM THE PERSON OR ORGANIZATIONORIGIN ATING IT POINTS OF VIEW OR OPINIONS STATED 00 NOT NECESSARILY REPRE SENT 01FICIAL NATIONAL INSTITUTE OF EDUCATION POSITION OR POLICY Y° READING GRADES 1-2-3 p4 'VERMILION PARISH LANGUAGE ARTS CURRICULUM GUIDE 1970 -
Exploration of Placer Gold Deposits by Geomagnetic Surveys
MTR-2 EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. EXPLORATION OF PLACER GOLD DEPOSITS BY GEOMAGNETIC SURVEYS by Eric Anderson V. P. Exploration Placer Management Group, Ltd. Exploration of Placer Gold Deposits by Geomagnetic Surveys Eric Anderson, V.P. Exploration Placer Management Group, Ltd. ABSTRACT Past attempts to explore for placer gold deposits by measuring the anomalous magnetic intensities of the magnetite normally found in the ”black sands” fraction of placer gravels were for the most part unsuccessful. Recent improvements in the sensitivity, reliability and portability of magnetometers have made it possible to cheaply and accurately delineate some types of placer gravels if they occur in a geological environment that is ”magnetically hospitable” and does not mask the signal of the overlaying gravels. The main benefit of this technique is that it can accurately delineate targets and thus dramatically reduce the overall cost of an exploration program in a given area. INTRODUCTION Whether or not this technique will work in a given area depends on three factors: 1. The amount of magnetite associated with the pay gravels. 2. The depth of the gravel deposit. 3. The nature of the underlying bedrock. In our work to date in Western Canada and United States, we have not encountered any pay gravels that did not have measurable concentrations of magnetite in the black sands. It is common to find gravel deposits with high concentrations of magnetite and no gold values whatsoever, but our experience and history have shown that gold values rarely occur without associated magnetic black sands; although the concentrates of magnetite do vary tremendously, In this regard it is important to keep two things in mind: 1.