USGS Professional Paper 1760–A
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Tc-Forty-Mile-Cheda-Dek-Guide.Pdf
Published 2011. ISBN 978-1-55362-538-4 For more information about Forty Mile, Fort Cudahy and Fort Constantine Historic Site, visit the Dänojà Zho cultural centre in Dawson or contact: Tr’ondëk Hwëch’in Heritage P. O. Box 599, Dawson City, Y0B 1G0 1242 Front Street, Dawson City Main office phone: (867) 993-7100 Dänojà Zho office phone: (867) 993-6768 Fax: (867) 993-6553 Email: [email protected] Tr’ondëk Hwëch’in website: www.trondek.ca Forty Mile web site: http://trondekheritage.com/our-places/forty-mile/ Yukon Historic Sites P. O. Box 2703, Whitehorse, Yukon Y1A 2C6 Phone: (867) 667-5386 Fax: (867) 667-8023 www.tc.gov.yk.ca/historicsites.html Cover images: Map, Yukon Archives H-1393 YG photo Yukon Archives, Alaska Historical Library #4221 Forty Mile circa 1890. Guide to Forty Mile The Forty Mile townsite is part of the Forty trading post and store established in 1893. Mile, Fort Cudahy and Fort Constantine Both of these sites are across the Fortymile Historic Site. The site is located at the River from the townsite of Forty Mile. The mouth of the Fortymile River where ground is marshy and the remains are fragile it empties into the Yukon River, 67 km so it recommended that visitors restrict their upstream from the Alaska/Yukon border activities to the Forty Mile townsite. and 88 km downriver from Dawson City. The Forty Mile, Fort Cudahy and Fort Generations of First Nation people camped Constantine Historic Site is protected under at the mouth of the Fortymile River to the Tr’ondëk Hwëch’in Final Agreement hunt and fish in the area. -
Tom Abstraktow 6B-Ost Ver Publ.Pdf
Cover photo: A euhedral, oscillatory zoned, primary monazite has been altered at the rims and along cracks to an allanite-apatite-xenotime assemblage. The host mineral is feldspar. Granite, Strzegom Massif. Workshop on accessory minerals, University of Warsaw, September 2014 Editors of Volume Bogusław BAGIŃSKI, Oliwia GRAFKA Witold MATYSZCZAK, Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa [email protected] Language correction: Ray MACDONALD Institute of Geochemistry, Mineralogy and Petrology, University of Warsaw Al. Żwirki i Wigury 93, 02-089 Warszawa [email protected] 1 Organizing committee: Bogusław BAGIŃSKI Ray MACDONALD Michał RUSZKOWSKI Financial support: Workshop on accessory minerals was financially supported by the Polish Ministry of Science and Higher Education subvention and research grant No N N307634040, Faculty of Geology University of Warsaw and PIG-PIB. 2 Workshop on accessory minerals, University of Warsaw, September 2014 Preface The progress made over the past two decades in our understanding of accessory minerals containing HFSE has been remarkable. Even when “fresh-minted”, minerals such as monazite, xenotime, allanite and zircon are compositionally and structurally complex. The complexity increases many times during low-temperature alteration processes, such as interaction with hydrothermal fluids and weathering. Progress has, of course, been expedited by the introduction of a range of exciting new technologies, especially in structure determinations. On re-reading the excellent 2002 review of accessory mineral research by Poitrasson et al., one is struck by how far the subject area has advanced in 12 years. We felt that this was an opportune time to bring together a group of Earth scientists with special expertise in accessory minerals to outline their current research interests, to share ideas and to consider productive future research directions. -
Open-File Report 2005-1235
Prepared in cooperation with the Idaho Geological Survey and the Montana Bureau of Mines and Geology Spatial databases for the geology of the Northern Rocky Mountains - Idaho, Montana, and Washington By Michael L. Zientek, Pamela Dunlap Derkey, Robert J. Miller, J. Douglas Causey, Arthur A. Bookstrom, Mary H. Carlson, Gregory N. Green, Thomas P. Frost, David E. Boleneus, Karl V. Evans, Bradley S. Van Gosen, Anna B. Wilson, Jeremy C. Larsen, Helen Z. Kayser, William N. Kelley, and Kenneth C. Assmus Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2005-1235 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2005 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Contents Abstract .......................................................................................................................................................... 1 Introduction -
Thursday, February 28, 1978
~ Property of II.IJ ~ Lounge ( . ·- Number 7 5th Session 23rd Legislature ---· -- --------- - Debates & Proceedings Thursday, February 28, 1978 Speaker: The Honourable Donald Taylor u ( ) ( ( 1 Published under author1ty of the Speaker of the Yukon Leg1slat1ve Assembly by the Queen's Prtnter for Yukon 1J;. l l!'' 1a:' Thr YoJmn Legislative Assemble Thu"sday, f1lbruary 26, 1976 Tl 1 11r~rl<ly. I l''l' II' I' !71 I J!l'ifl Hon. M.r. Taylor: :\1r. Speaker. !his morning. I would I ike to give :'--lot ice of :vtotion. ~econcled by the Honourable :vlember from WhitehorsP l~i verdale. that ll'hereas the Yukon Legislative Assembly recognizes Mr. sw· a~rr: '.1 I I::Jm ('Jprh ~ ~- I 'l• ' I ljllfll'll!ll that the Honourable Judd Buchanan. Minister of In prrsenl? dir~n and Northern Affairs. is current!~· considering the appointment of a new Commissioner for the :vtadam C!Prk : Tl. r re i ~. \1 r . Spr ;· ~r r Yukon . And whereas concern is being expressed that the custom of appointing a res ident Yukoner. fol Mr. Sp('ak!'r: 1 ll'ill now c:tllliH' l lo11· r· '" orrlrr lowed by the Minister in the past shou ld be con tinuecl. Therefore be it resolved th at the Yukon Legis ROUTINE PH0C: J:DURES lative Assembly in Session assemblecl requests that the Minister for Indian and Northern Affr~ 1r s. should DAILY IWl'TI:'-If: recommend to the governor in council. the appoint ment of a person who is a resident of the Yukon Ter Mr. Speaker: Are there any doclllllPnt!'; or cor ritor~' to be the next commiss ioner of the Territory. -
Clinton Creek Mine Waste Rock Dump
SUMMARY OF ENVIRONMENTAL MONITORING ACTIVITIES AT THE ABANDONED CLINTON CREEK ASBESTOS MINE, 2011 Looking to Hudgeon Lake from Upper Clinton Creek area, July 2011 FOR ASSESSMENT AND ABANDONED MINES ENERGY MINES AND RESOURCES BY March 2012 TABLE OF CONTENTS 1.0 BACKGROUND 1 1.1 Scope of Work 2 2.0 STUDY AREA 3 3.0 METHODS 6 3.1 Water Quality Sampling 6 3.2 Sediment Geochemistry 6 4.0 RESULTS 7 4.1 Surface Water Quality 8 4.2 Groundwater Seeps 11 4.3 Sediment Geochemistry 12 4.3.1 Stream Sediments 12 4.3.2 Tailings 14 5.0 SUMMARY 16 6.0 RECOMMENDATIONS 17 7.0 REFERENCES 19 APPENDICES Appendix A Clinton Creek Site Photographs, 2011 Appendix B Complete Field Data, July and September 2011 Appendix C Water Quality Analytical Reports, 2011 Appendix D Sediment Analytical Reports, 2011 LIST OF TABLES 1 Site Descriptions and Locations 3 2 Water Quality Summary, Surface Water Sites, 2011 9 3 Water Quality Summary of the Groundwater Seeps, September 28, 2011 12 4 Concentrations of Metals (ug/g) in Stream Sediments, 2011 13 5 Concentration of Metals in Tailings, Clinton Creek, 2011 14 6 Comparisons of Metals in 1998, 2009, 2010 and 2011 15 LIST OF FIGURES 1 Clinton Creek Water Quality Monitoring Locations in 2011 4 2 Waste Rock and Tailings Monitoring Stations in 2011 5 i Summary of Environmental Monitoring Activities at the Abandoned Clinton Creek Asbestos Mine, 2011 1.0 BACKGROUND The former Clinton Creek Asbestos Mine is located approximately 100 km northwest of Dawson City, Yukon, and nine km upstream of the confluence of Clinton Creek and the Forty Mile River. -
Inventory to Posters, Original Art and Miscellaneous Items
Inventory to POSTERS, ORIGINAL ART & MISCELLANEOUS ITEMS Held at the Yukon Archives January 1997 Libraries and Archives Inventory to POSTERS, ORIGINAL ART & MISCELLANEOUS ITEMS Held at the Yukon Archives January 1997 Yukon Archives Canadian Cataloguing in Publication Data Yukon Archives Inventory to posters, original art & miscellaneous items held at the Yukon Archives Issued by Yukon Archives. ISBN 1-55018-779-1 Includes an index. 1. Posters -- Yukon Territory -- Catalogs. 2. Art -- Yukon Territory -- Catalogs. 3. Collectibles -- Yukon Territory -- Catalogs. 4. Yukon Archives -- Catalogs. I. Yukon Territory. Yukon Education. II. Title. CD3645.Y8I68 1997 016.741.6'74 C97-980334-9 TABLE OF CONTENTS INTRODUCTION.................................................................................................................................1-1 MISCELLANEOUS ITEMS ....................................................................................................................2-1 ORIGINAL ART .................................................................................................................................3-1 POSTERS .........................................................................................................................................4-1 TITLE INDEX ....................................................................................................................................5-1 SUBJECT INDEX ................................................................................................................................6-1 -
Earth Science Chapter 6
Chapter6 Rocks Chapter Outline 1 ● Rocks and the Rock Cycle Three Major Types of Rock The Rock Cycle Properties of Rocks 2 ● Igneous Rock The Formation of Magma Textures of Igneous Rocks Composition of Igneous Rocks Intrusive Igneous Rock Extrusive Igneous Rock 3 ● Sedimentary Rock Formation of Sedimentary Rocks Chemical Sedimentary Rock Organic Sedimentary Rock Clastic Sedimentary Rock Characteristics of Clastic Sediments Sedimentary Rock Features 4 ● Metamorphic Rock Formation of Metamorphic Rocks Why It Matters Classification of The hundreds of different types of Metamorphic Rocks rocks on Earth can be classified into three main types: igneous, sedimentary, and metamorphic. This formation in Arizona is made of sedimentary rock. When you know the type of rock, you know something about how that rock formed. 132 Chapter 6 hq10sena_rxscho.indd 1 3/25/09 4:10:29 PM Inquiry Lab Sedimentary Sandwich 15 min Use slices of different types of bread to model Questions to Get You Started layers of different types of sediment deposits. Next, 1. Make a labeled diagram showing the rock layers in put your model in a plastic bag. Place a weight on the sample you observed. top of the bag to simulate the process of 2. Which factors might affect the thickness of a rock compacting sediment into rock. Then, use an empty layer in a real rock formation? film canister to obtain a core sample of the sedimentary sandwich. Trade samples with another 3. Your model has layers of different types of rocks. group and observe the other group’s sample. In a real formation, what might changes in Identify the different layers of rock and determine if rock type indicate about the rock layers are the same thickness or if some are formation’s geological history? thicker than others. -
Landslide Dams and Creek Stabilization
2005 Dawson City, Yukon Landslide Dams and Creek Stabilization at the Former Clinton Creek Asbestos Mine Gil Robinson, P.Eng., Ken Skaftfeld, P.Eng., Rolf Aslund, P.Eng., UMA Engineering, Winnipeg, Manitoba Hugh Copland, P.Eng. Government of Yukon, Whitehorse, Yukon 1.0 Abstract Risk assessment techniques were used to identify the risk associated with a breach of a landslide dam in the Clinton Creek valley at the former Clinton Creek Asbestos Mine, which is located about 100 km northwest of Dawson City, Yukon. Since closure of the mine in 1978, concerns have been raised with respect to the physical condition of the site, in particular downstream hazards associated with breaching of the landslide dam forming the Hudgeon Lake outlet. The risk was mitigated by designing a stable channel over the landslide dam, also known as the Clinton Creek waste rock dump, of which the most important design component is the gabion drop structures. The gabion drop structures act as grade control points which are connected by a nearly flat graded channel to prevent erosion of the channel fill materials. Gabions were selected because they are simple to construct yet robust and flexible enough to accommodate some lateral movement of the creeping landslide mass. The channel stabilization works consist of four gabion drop structures constructed within the first 200 m of the channel downstream of the Hudgeon lake outlet. In the fall of 2002, the first stage of these repairs was undertaken, which included the construction of Drop Structure #1 and re- grading of the Hudgeon Lake outlet. The second drop structure was built in 2003 and the last two drop structures were constructed in 2004. -
Rock Classification – Best for Coarse-Grained Rocks – Useful for Field Work Chapter 2, Pp
Basis for Classification • Minerals present in the rock Rock Classification – Best for coarse-grained rocks – Useful for field work Chapter 2, pp. 17-26 • Chemical Composition – Works for fine-grained rock – Expensive and takes time Mineralogical Classification Monomineralic Rocks • Color Index = % of dark minerals • Plagioclase Anorthosite • Felsic < 35% mafic minerals • Olivine Dunite • Mafic = 35% – 90% mafic minerals • Augite Clinopyroxenite • Ultramafic > 90% mafic mineral • Hypersthene Orthopyroxenite QAPF Chemical Classification Diagram • CIPW norm • Useful for most – Calculated minerals from Common rocks chemical analysis • Saturation concept – Si saturation • Recalculate the • Acid to basic minerals to – Al saturation 100% QAP or • Harker-Peacock index FAP – Alkalies vs calcium 1 Silica Saturation Aluminum Saturation Acid SiO2 > 66 % Based on the feldspar ratio 1:1:3 (NaAlSi3O8) Intermediate SiO2 52 to 66 % Basic SiO2 45 to 52 % Peraluminous Al2O3 > (CaO + Na2O + K2O) Ultrabasic SiO2 < 52 % Peralkaline (Na2O + K2O) > Al2O3 Classification of Igneous Rocks Classification of Igneous Rocks Figure 2-1a. Method #1 for plotting a point with the components: 70% X, 20% Y, and 10% Z on Figure 2-1b. Method #2 for plotting a point with the components: 70% X, 20% Y, and 10% Z on triangular triangular diagrams. An Introduction to Igneous and Metamorphic Petrology, John Winter, Prentice Hall. diagrams. An Introduction to Igneous and Metamorphic Petrology, John Winter, Prentice Hall. Feldspar Classification Pyroxene Classification 2 Classification -
Carbon Sources and the Graphitization of Carbonaceous Matter in Precambrian Rocks of the Keivy Terrane (Kola Peninsula, Russia)
minerals Article Carbon Sources and the Graphitization of Carbonaceous Matter in Precambrian Rocks of the Keivy Terrane (Kola Peninsula, Russia) Ekaterina Fomina 1,* , Evgeniy Kozlov 1 , Kirill Lokhov 2, Olga Lokhova 3 and Vladimir Bocharov 4 1 Geological Institute, Kola Science Centre, Russian Academy of Sciences, 14, Fersmana Street, 184209 Apatity, Russia; [email protected] 2 Institute of Earth Sciences, Saint-Petersburg State University, 7/9, Universitetskaya Emb., 199034 St. Petersburg, Russia; [email protected] 3 Institute for the History of Material Culture, Russian Academy of Sciences, 18, Dvortsovaya Emb., 191186 St.-Petersburg, Russia; [email protected] 4 Resource Center for Geo-Environmental Research and Modeling (GEOMODEL), Saint-Petersburg State University, 1, Ulyanovskaya Street, 198504 St. Petersburg, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-921-276-2996 Received: 15 December 2018; Accepted: 3 February 2019; Published: 8 February 2019 Abstract: The Precambrian rocks of the Keivy Terrane reveal five types of carbonaceous matter (CM): Fine-grained, flaky, nest, vein, and spherulitic. These types differ in their distribution character, carbon isotope composition, and graphitization temperatures calculated by the Raman spectra of carbonaceous material (RSCM) geothermometry. Supracrustal rocks of the Keivy Terrane 13 contain extremely isotopically light (δ CPDB = –43 ± 3‰) carbon. Presumably, its source was a methane–aqueous fluid. According to temperature calculations, this carbon matter and the host strata underwent at least two stages of metamorphism in the west of the Keivy Terrane and one stage in 13 the east. The CM isotope signatures of several samples of kyanite schists (δ CPDB = –33 ± 5‰) are close to those of oils and oil source rocks, and they indicate an additional carbon reservoir. -
Yukon River Restoration and Enhancment Fund 2008 Conceptual Proposal
YUKON RIVER RESTORATION AND ENHANCMENT FUND 2008 CONCEPTUAL PROPOSAL NUMBER: URE-04N-08 PROJECT TITLE: Ruby Salmon Data Collection Project PROJECT PROPONENT: Ed Sarten, Ruby Tribal Council PO box 21, Ruby, AK 99768 (907) 468-4475 [email protected] POTENTIAL PROJECT PARTNERS/ADDITIONAL PARTICIPANTS: Brandy Berkbigler, Tanana Chiefs Conference (907) 452-8251 [email protected] Lara Dehn, Alaska Department of Fish & Game (907) 459-7288 [email protected] PROJECT LOCATION: Ruby, AK PROJECT OBJECTIVES: 1.) To collect age, sex, length, weight, and girth data as well a genetic tissue samples from Chinook salmon caught with fishwheels and set nets, the two types of gear used in this area. 2.) To better understand stock biology and composition of the Ruby harvest throughout subsistence windows. Budget Priority Framework 2006: • Improve information on biological composition of run; and, • involve and educate users and non-users in communities to increase their desire to maintain and protect salmon stocks and habitat. US and Canada Yukon River Salmon Committee Joint Technical Committee Plan: • Estimate the stock biological or other composition of escapements – 1.1.2; and, • build and maintain community capacity – 3.2.3. Budget Priorities for 2008 & Near Term Priorities: 3. Determine the quality of stock escapement 4. Community Education and Stewardship PROJECT SUMMARY: Management of the Chinook salmon fishery is difficult due to the mixed stocks of salmon, commercial and subsistence fishing, the many tributaries and the vast distance that the Yukon River flows. As a result, several controversies have arisen over time. First are concerns over allocation of the fishery based on the size of salmon runs year to year. -
Structural, Petrological, and Tectonic Constraints on the Loch Borralan and Loch Ailsh Alkaline Intrusions, Moine Thrust Zone, GEOSPHERE, V
Research Paper GEOSPHERE Structural, petrological, and tectonic constraints on the Loch Borralan and Loch Ailsh alkaline intrusions, Moine thrust zone, GEOSPHERE, v. 17, no. 4 northwestern Scotland https://doi.org/10.1130/GES02330.1 Robert Fox and Michael P. Searle 24 figures Department of Earth Sciences, Oxford University, South Parks Road, Oxford OX1 3AN, UK CORRESPONDENCE: [email protected] ABSTRACT during ductile shearing. The minerals pseudomor- Grit Members of the An t-Sron Formation) and the phing leucites show signs of ductile deformation Ordovician Durness Group dolomites and lime- CITATION: Fox, R., and Searle, M.P., 2021, Structural, petrological, and tectonic constraints on the Loch Bor- During the Caledonian orogeny, the Moine indicating that high-temperature (~500 °C) defor- stones (Woodcock and Strachan, 2000; Strachan ralan and Loch Ailsh alkaline intrusions, Moine thrust thrust zone in northwestern Scotland (UK) mation acted upon pseudomorphed leucite crystals et al., 2010; British Geological Survey, 2007). zone, northwestern Scotland: Geosphere, v. 17, no. 4, emplaced Neoproterozoic Moine Supergroup rocks, that had previously undergone subsolidus break- The hinterland of the Caledonian orogenic p. 1126– 1150, https:// doi.org /10.1130 /GES02330.1. meta morphosed during the Ordovician (Grampian) down. New detailed field mapping and structural wedge comprises schists of the Moine Super- and Silurian (Scandian) orogenic periods, westward and petrological observations are used to constrain group with structural inliers of Lewisian basement Science Editor: Andrea Hampel Associate Editor: Robert S. Hildebrand over the Laurentian passive margin in the north- the geological evolution of both the Loch Ailsh gneisses and intrusive Caledonian granites (Geikie, ern highlands of Scotland.