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The Economics of Mining Evolved More Favorably in Mexico Than Peru
Created by Richard L. Garner 3/9/2007 1 MINING TRENDS IN THE NEW WORLD 1500-1810 "God or Gold?" That was the discussion question on an examination that I took many years ago when I started my studies in Latin American history. I do not recall how I answered the question. But the phrase has stuck in my mind ever since. And it has worked its way into much of the history written about the conquest and post-conquest periods, especially the Spanish conquests. From the initial conquests in the Caribbean and certainly after the conquests of Mexico and Peru the search for minerals became more intensive even as the Spanish Crown and its critics argued over religious goals. In the middle of the sixteenth century after major silver discoveries in Mexico and Peru the value of the output of the colonial mines jumped significantly from a few million pesos annually (mainly from gold) to several tens of millions. Perhaps “Gold” (mineral output) had not yet trumped “God” (religious conversion) on every level and in every region, but these discoveries altered the economic and financial equation: mining while not the largest sector in terms of value or labor would become the vehicle for acquiring and consolidating wealth. Until the late seventeenth century Spanish America was the New World’s principal miner; but then the discovery of gold in Brazil accorded it the ranking gold producer in the New World while Spanish American remained the ranking silver producer. The rise of mining altered fundamentally the course of history in the New World for the natives, the settlers, and the rulers and had no less of an effect on the rest of the world. -
Lovelock-Cave-Back-Country-Byway
Back Country Byways . An Invitation to Discover There is an axiom among seasoned travelers advising that the best way to get to know a new place is to get off the highway and visit the back roads, the side trails and the hidden, out-of-the-way corners where the true qualities wait to be discovered. The same axiom holds true for America’s public lands, the vast reaches of our nation that are all too often seen only from the windows of speeding cars or the tiny portholes of airliners. The Bureau of Land Management, America’s largest land managing agency, is providing an exciting opportunity for more Americans to get to know their lands by getting off the main roads for leisurely trips on a series of roads and trails being dedicated as Back Country Byways. The Back Country Byways Program, an outgrowth of the national Scenic Byways Program, is designed to encourage greater use of these existing back roads through greater public awareness. The system is BUREAUREAU OOFF LANDLAND MANMANAGEMENTGEMENT expected to expand to 100 roads when completed. In Nevada, each byway has a character and beauty of its own, taking travelers through scenery that is uniquely Nevadan, into historic areas that helped shape our state and near areas that have been largely untouched by man. They can see the multiple uses of their lands and come to a greater awareness of the need for the conservation and wise use of these resources. And all this can be accomplished at little cost to the taxpayer. Because the roads are already in place, only interpretive signs and limited facilities are needed to better serve the public. -
Technical Report Getchell Project NI 43-101 Technical Report Premier Gold Mines Limited and I-80 Gold Corp
AMC Mining Consultants (Canada) Ltd. BC0767129 200 Granville Street, Suite 202 Vancouver BC V6C 1S4 Canada T +1 604 669 0044 E [email protected] W amcconsultants.com Technical Report Getchell Project NI 43-101 Technical Report Premier Gold Mines Limited and i-80 Gold Corp Humboldt County, Nevada, USA In accordance with the requirements of National Instrument 43-101 “Standards of Disclosure for Mineral Projects” of the Canadian Securities Administrators Qualified Persons: D Nussipakynova, P.Geo. P Greenhill, FAusIMM (CP) AMC Project 720031 Effective date 23 July 2020 Report date 22 January 2021 Unearth a smarter way Getchell Project NI 43-101 Technical Report Premier Gold Mines Limited and i-80 Gold Corp 720031 1 Summary 1.1 Introduction This Technical Report (the Report) provides an update of the Mineral Resource estimates and metallurgy of the Mineral Resources identified within the Getchell Project (Property) located in Humboldt County, Nevada, USA. The Report has been prepared by AMC Mining Consultants (Canada) Ltd. (AMC) of Vancouver, Canada on behalf of Premier Gold Mines Limited / i-80 Gold Corp (i-80 or the Companies). On 10 August 2020, Premier entered into a definitive purchase agreement with affiliates of Waterton Global Resource Management, Inc. to acquire from Waterton all of the outstanding membership interests of Osgood Mining Company LLC (OMC). The Property comprises a number of property parcels which collectively encompass 2,545 acres in the Potosi mining district. The four-square miles of land contain all areas of past gold production and the area of the currently estimated Mineral Resource. This area includes the historical Pinson Mine. -
Northern Paiute and Western Shoshone Land Use in Northern Nevada: a Class I Ethnographic/Ethnohistoric Overview
U.S. DEPARTMENT OF THE INTERIOR Bureau of Land Management NEVADA NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Ginny Bengston CULTURAL RESOURCE SERIES NO. 12 2003 SWCA ENVIROHMENTAL CON..·S:.. .U LTt;NTS . iitew.a,e.El t:ti.r B'i!lt e.a:b ~f l-amd :Nf'arat:1.iern'.~nt N~:¥G~GI Sl$i~-'®'ffl'c~. P,rceP,GJ r.ei l l§y. SWGA.,,En:v,ir.e.m"me'Y-tfol I €on's.wlf.arats NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Submitted to BUREAU OF LAND MANAGEMENT Nevada State Office 1340 Financial Boulevard Reno, Nevada 89520-0008 Submitted by SWCA, INC. Environmental Consultants 5370 Kietzke Lane, Suite 205 Reno, Nevada 89511 (775) 826-1700 Prepared by Ginny Bengston SWCA Cultural Resources Report No. 02-551 December 16, 2002 TABLE OF CONTENTS List of Figures ................................................................v List of Tables .................................................................v List of Appendixes ............................................................ vi CHAPTER 1. INTRODUCTION .................................................1 CHAPTER 2. ETHNOGRAPHIC OVERVIEW .....................................4 Northern Paiute ............................................................4 Habitation Patterns .......................................................8 Subsistence .............................................................9 Burial Practices ........................................................11 -
RESULTS CONFIRM EXTENSION to Mcdermitt RESOURCE
ASX RELEASE 5 March 2021 ASX: JRL RESULTS CONFIRM EXTENSION TO McDERMITT RESOURCE Assay results from MDRC012 confirm substantial thickness and continuity of lithium mineralisation from surface Remaining four drillhole results expected by mid-March 2021 Jindalee Resources Limited ( Jindalee , the Company ) is pleased to announce that assay results have now been received for 11 holes of the 15-hole program completed late in 2020 at the Company’s 100% owned McDermitt Lithium Project (US). The latest results for MDRC012 confirm substantial widths of lithium mineralisation from surface in the SE portion of the deposit including : 58.0m @ 1611 ppm Li from 1.5m including 12.2m @ 2617ppm Li 27.4m @ 1477 ppm Li from 88.9m Results from MDRC012, located approximately 500m SE of the nearest hole (MDRC011), support significant intercepts recently announced by Jindalee 5 with drilling successfully confirming and extending the geology and grade continuity of the lithium mineralisation at McDermitt (Figure 1). The density of drilling is expected to be adequate to extend the current Inferred Mineral Resource 1 and Exploration Target Range 1 and convert existing Inferred Mineral Resources to Indicated status ahead of a possible Scoping Study. Figure 1 – Schematic section showing significant intercepts through the McDermitt Project. McDermitt Lithium Project – Background In late 2019 Jindalee announced an Inferred Mineral Resource of 150Mt @ 2,000ppm Li (0.43% Li 2O) at 1,750ppm Li cut-off 1 had been estimated at McDermitt (refer Table 1, below): Cut Off Mass Grade Contained LCE (ppm Li) (Mt) (ppm Li) (Mt) 1,750 150 2,000 1.6 Table 1 – Summary of the maiden Inferred Mineral Resource The Mineral Resource was estimated using a cut-off grade of 1,750ppm Li, which is considered appropriate in the context of similar projects and based on an assessment of the likelihood of future economic extraction as required by the JORC (2012) Code. -
Burning Man Geology Black Rock Desert.Pdf
GEOLOGY OF THE BLACK ROCK DESERT By Cathy Busby Professor of Geology University of California Santa Barbara http://www.geol.ucsb.edu/faculty/busby BURNING MAN EARTH GUARDIANS PAVILION 2012 LEAVE NO TRACE Please come find me and Iʼll give you a personal tour of the posters! You are here! In one of the most amazing geologic wonderlands in the world! Fantastic rock exposure, spectacular geomorphic features, and a long history, including: 1. PreCambrian loss of our Australian neighbors by continental rifting, * 2. Paleozoic accretion of island volcanic chains like Japan (twice!), 3. Mesozoic compression and emplacement of a batholith, 4. Cenozoic stretching and volcanism, plus a mantle plume torching the base of the continent! Let’s start with what you can see on the playa and from the playa: the Neogene to Recent geology, which is the past ~23 million years (= Ma). Note: Recent = past 15,000 years http://www.terragalleria.com Then we’ll “build” the terrane you are standing on, beginning with a BILLION years ago, moving through the Paleozoic (old life, ~540-253 Ma), Mesozoic (age of dinosaurs, ~253-65 Ma)) and Cenozoic (age of mammals, ~65 -0 Ma). Neogene to Recent geology Black Rock Playa extends 100 miles, from Gerlach to the Jackson Mountains. The Black Rock Desert is divided into two arms by the Black Rock Range, and covers 1,000 square miles. Empire (south of Gerlach)has the U.S. Gypsum mine and drywall factory (brand name “Sheetrock”), and thereʼs an opal mine at base of Calico Mtns. Neogene to Recent geology BRP = The largest playa in North America “Playa” = a flat-bottomed depression, usually a dry lake bed 3,500ʼ asl in SW, 4,000ʼ asl in N Land speed record: 1997 - supersonic car, 766 MPH Runoff mainly from the Quinn River, which heads in Oregon ~150 miles north. -
Thacker Pass Lithium Mine Final EIS, Appendix B, Mining Plan Of
Final Environmental Impact Statement Thacker Pass Lithium Mine Project Appendix B Mining Plan of Operations This page intentionally left blank. Appendix B – Mining Plan of Operations APPENDIX B. MINING PLAN OF OPERATIONS Thacker Pass Lithium Mine Project B-1 Final Environmental Impact Statement Appendix B – Mining Plan of Operations This page intentionally left blank. B-2 Thacker Pass Lithium Mine Project Final Environmental Impact Statement Thacker Pass Project Proposed Plan of Operations and Reclamation Plan Permit Application July 2019 October 2019 - Revised Submitted to: Bureau of Land Management Nevada Division of Environmental Protection Winnemucca District Bureau of Mining Regulation and Reclamation Humboldt River Field Office 901 S Stewart Street, Suite 4001 5100 East Winnemucca Boulevard Carson City, Nevada 89701 Winnemucca, Nevada 89445 Submitted by: LithiumNevada Lithium Nevada Corp. 3685 Lakeside Drive Reno, Nevada 89509 Contact: Edward (Ted) Grandy, VP Legal and Regulatory Affairs Thacker Pass Project – Plan of Operations and Reclamation Plan LithiumNevada Summary Lithium Nevada Corp. (LNC), a wholly owned subsidiary of Lithium Americas Corp. (LAC), proposes to construct, operate, reclaim, and close an open pit lithium mining and processing operation, the Thacker Pass Project (Project), located on public lands in northern Humboldt County, Nevada. The surface and subsurface mineral estates associated with the Project are located on public lands administered by the Bureau of Land Management (BLM), Winnemucca District, and controlled by federal unpatented lode mining claims owned by LNC. LNC is submitting this Plan of Operations and Reclamation Plan (Plan) to develop the Project in accordance with BLM Surface Management Regulations under 43 Code of Federal Regulations (CFR) 3809, Surface Occupancy regulations under 43 CFR 3715, and Nevada reclamation regulations under Nevada Administrative Code (NAC) 519A. -
Biostratigraphy of the Bilk Limestone (Permian), Northwestern Nevada
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Spring 1972 Biostratigraphy of the Bilk Limestone (Permian), Northwestern Nevada Erich Thomas Western Washington University Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Thomas, Erich, "Biostratigraphy of the Bilk Limestone (Permian), Northwestern Nevada" (1972). WWU Graduate School Collection. 731. https://cedar.wwu.edu/wwuet/731 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. BIOSTRATIGRAPHY OF THE BILK LIIffiSTONE (PERMIAN), NORTHWESTERN NEVADA A Thesis Presented to The Facvilty of Western Washington State College In Partial Fxilfillment of the Requirements for the Degree Master of Science ty Erich Thomas May 1972 BIOSTRATIGRAPHY OF THE BILK LB'fESTONE (PERMIAN), NORTHWESTERN NEVADA tiy Erich Thomas Accepted in Partial Completion of the Requirements for the Degree Master of Science Advisory Committee Chairman MASTER'S THESIS In presenting thisthesis in partial fulfillment of the requirements for a master's degree at Western Washington University, I grant to Western Washington University the non-exclusive royalty-free rightto archive, reproduce, distribute, and display the thesis in any and all forms, including electronic format, via any digital library mechanisms maintained by WWU. I represent and warrant this is my original work and does not infringe or violate any rights of others. I warrant that I have obtained written permissions from the owner of any third party copyrighted material included in these files. -
Brueseke, M.E., W.K. Hart & M.T. Heizler, Diverse Mid-Miocene Silicic
Bull Volcanol DOI 10.1007/s00445-007-0142-5 RESEARCH ARTICLE Diverse mid-Miocene silicic volcanism associated with the Yellowstone–Newberry thermal anomaly Matthew E. Brueseke & William K. Hart & Matthew T. Heizler Received: 1 February 2005 /Accepted: 8 March 2007 # Springer-Verlag 2007 Abstract The Santa Rosa–Calico volcanic field (SC) of primarily focused along its eastern and western margins. At northern Nevada is a complex, multi-vent mid-Miocene least five texturally distinct silicic units are found in the eruptive complex that formed in response to regional western Santa Rosa–Calico volcanic field, including abun- lithospheric extension and flood basalt volcanism. Santa dant lava flows, near vent deposits, and shallow intrusive Rosa–Calico volcanism initiated at ∼16.7 Ma, concurrent bodies. Similar physical features are found in the eastern with regional Steens–Columbia River flood basalt activity portion of the volcanic field where four physically distinct and is characterized by a complete compositional spectrum units are present. The western and eastern Santa Rosa– of basalt through high-silica rhyolite. To better understand Calico units are characterized by abundant macro- and the relationships between upwelling mafic magmatism, microscopic disequilibrium textures, reflecting a complex coeval extension, and magmatic system development on petrogenetic history. Additionally, unlike other mid-Mio- the Oregon Plateau we have conducted the first compre- cene Oregon Plateau volcanic fields (e.g. McDermitt), the hensive study of Santa Rosa–Calico silicic volcanism. Santa Rosa–Calico volcanic field is characterized by a Detailed stratigraphic-based field sampling and mapping paucity of caldera-forming volcanism. Only the Cold illustrate that silicic activity in this volcanic field was Springs tuff, which crops out across the central portion of the volcanic field, was caldera-derived. -
Brxs R43.Pdf
MINERAL RESOURCES OF THE KUMlVA PEAK 38-BV 60"OUADRANGLE INTRODUCTION Parallel Survey. Descriptions of mines and prospects within the auadranale were made bv HI! 11 91 51. Lincoln 11 9231. The Kumiva Peak 30' by 60' Quadrangle lies about 40 ~anderburg-(1936). ~vertdn11947). onh ham i1969); miles north of Reno in western Nevada. The southern and Johnson (1977). Descriptions of the geology of the boundary is the 40th parallel and the western boundary, Washoe County portion of the quadrangle were included in the 120th meridian, lies about % mile west of the Nevada- the work by Bonham (1969); Johnson (I9771 described California state line. Portions of Washoe and Pershing the geology of the Pershing County part of the quadrangle. Counties, the northern half of Pyramid Lake, and a large During 1984-85, the Nevada Bureau of Mines and part of the Pyramid Lake Indian Reservation ail lie within Geology conducted a mineral inventory of the Sonoma- this quadrangle. Gerlach Resource Area for the Bureau of Land Management The John Fremont end Kit Carson party traveled through and, as part of that project,many mines andprospects in the central portion of this area in early January 1844. The the Kumiva Peak 30' by 60' Quadrangle were examined Fremont party discovered and named Pyramid Lake and and sampled. Field data were collected by Jack Quade, passed along its eastern shore on their way south. The J. V. Tingley, R: B. Jones, and L. J. Garside. In 1986, earliest mining activity, gold and silver prospecting, began T. L. T. Grose reported on several prospects in the about 1670 in Cottonwood Canyon in the northern Fox southern part of the quadrangle and, in 1967, J. -
Technical Report for the Rochester Mine Lovelock, Nevada, Usa
TECHNICAL REPORT FOR THE ROCHESTER MINE LOVELOCK, NEVADA, USA NI 43-101 Technical Report – Updated Project Study Effective Date: December 31, 2014 Filing Date: February 18, 2015 Prepared by: Gregory D. Robinson, P.E. Kelly Lippoth, AIME Annette McFarland, P.E. Raul Mondragon, RM SME Dana Willis, RM SME Rochester Mine Lovelock, Nevada, USA NI 43-101 Technical Report February 18, 2015 Cautionary Statement on Forward-Looking Information This Technical Report contains forward-looking statements within the meaning of the U.S. Securities Act of 1933 and the U.S. Securities Exchange Act of 1934 (and the equivalent under Canadian securities laws), that are intended to be covered by the safe harbor created by such sections. Such forward-looking statements include, without limitation, statements regarding Coeur Mining, Inc.’s (Coeur’s) expectations for the Rochester Mine, including estimated capital requirements, expected production, cash costs and rates of return; mineral reserve and resource estimates; estimates of silver and gold grades, expected financial returns and costs; and other statements that are not historical facts. We have tried to identify these forward-looking statements by using words such as “may,” “might”, “will,” “expect,” “anticipate,” “believe,” “could,” “intend,” “plan,” “estimate” and similar expressions. Forward-looking statements address activities, events or developments that Coeur expects or anticipates will or may occur in the future, and are based on information currently available. Although Coeur believes that its -
4.5 Cultural Resources
4.5 – Cultural Resources 4.5 Cultural Resources This section identifies cultural and paleontological resources along the IC Project Alignment, identifies applicable significance thresholds, assesses the IC Project’s impacts to these resources and their significance, and recommends measures to avoid or substantially reduce any effects found to be potentially significant. Cultural resources are defined as any object or specific location of past human activity, occupation, or use that is identifiable through historical documentation, inventory, or oral evidence. Cultural resources can be separated into three categories: archaeological, building/structural, and traditional resources. Archaeological resources include prehistoric and historic remains of human activity. Prehistoric resources can be composed of lithic scatters, ceramic scatters, quarries, habitation sites, temporary camps/rock rings, ceremonial sites, and trails. Historic-era resources are typically those that are 50 years or older. Historic archaeological resources can consist of structural remains (e.g., concrete foundations), historic objects (e.g., bottles and cans), features (e.g., refuse deposits or scatters), and sites (e.g., resources that contain one or more of the aforementioned categories). Built environment resources range from historic buildings to canals, historic roads and trails, bridges, ditches, cemeteries, and electrical infrastructure, such as transmission lines, substations, and generating facilities. A traditional cultural resource is a resource associated with the cultural practices, traditions, beliefs, lifeways, arts, crafts, or social institutions of a living community. They are rooted in a traditional community’s history and are important in maintaining the continuing cultural identity of the community. See Section 4.18, Tribal Cultural Resources, for a discussion on cultural resources of potential importance to California Native American tribes.