Bulletin 37, Inventory of Washington Minerals Part II
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Glossary Glossary
Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts. -
Summer 2015 April - October Cruises
SUMMER 2015 APRIL - OCTOBER CRUISES ALASKA • THE ARCTIC • JAPAN NORTHERN EUROPE & THE BALTIC • MEDITERRANEAN THE ARCTIC page 44 ALASKA page 34 THE ARCTIC page 44 Set sail for exceptional destinations Visit exceptional sites combining dreams as well as totally authentic experience, new cultures, and enjoy new encounters that bring you even closer to Nature - these are the privileges that the smaller size of our ships offer you. Preserved archipelagos of the Aegean Sea, crystal like water and secret inlets in the Mediterranean Sea, majestic glaciers in the Arctic, exceptional encounters in the remote lands of Alaska or sailing along the Celtic coasts… A unique experience. SUMMARY CALENDAR ................................................6 YACHT CRUISES .............................................8 SERVICE ON BOARD ........................................12 GASTRONOMY ............................................16 SPA & WELLBEING . 20 OUR COMMITMENTS ........................................24 WELCOME ABOARD LE LYRIAL .................................26 OUR SISTERSHIPS ...........................................28 LE PONANT ...............................................30 SUMMARY FIVE-STAR EXPEDITIONS ......................................32 ALASKA..................................................34 4 THE ARCTIC page 44 NORTHERN EUROPE & THE BALTIC page 66 EASTERN MEDITERRANEAN page 88 JAPAN page 58 WESTERN MEDITERRANEAN page 78 Access the World’s Treasures by Sea THE ARCTIC ....................................................................44 -
Transportation Committee Thursday, May 2, 2013, at 10:00 A.M
Sacramento Area 1415 L Street, tel: 916.321.9000 Council of Suite 300 fax: 916.321.9551 Sacramento, CA tdd: 916.321.9550 Governments 95814 www.sacog.org Transportation Committee Thursday, May 2, 2013, at 10:00 a.m. Roll Call: Directors Cabaldon, Cohn, Crews (non-voting), Griego, Hesch, Hodges, Holmes (alternate), Joiner, Ex-officio Member Jones, Krovoza, Peters, Slowey, Vice Chairs Hagen and Sander, and Chair Saylor Public Communications: Any person wishing to address the committee on any item not on the agenda may do so at this time. After ten minutes of testimony, any additional testimony will be heard following the action items. 1. Minutes of the April 4, 2013, Meeting◄ (Mr. Carpenter) 2. Funding of Transit Projects Using Federal Transit Administration Section 5307 and 5339 FFY 2013 Apportionments to the Sacramento Urbanized Area◄ (Mr. Taylor) 3. Flexible Funds Programing Round Framework and Application Process◄ Ms. DeVere-Oki 4. Regional Bicycle, Pedestrian, and Trails Master Plan Update◄ (Ms. Cacciatore) 5. Transportation Investment Generating Economic Recovery (TIGER) V Nomination Process◄ (Ms. DeVere-Oki) 6. Fiscal Year 2013-14 Provisional Budget for the Capitol Valley Regional Service Authority for Freeways and Expressways (CVRS)◄ (Mr. Heiman) 7. Call Box Maintenance Request for Proposals Release◄ (Mr. Heiman) 8. SACOG Toll Credits Policy◄ (Mr. Carpenter/Ms. Arnold) 9. Background Briefing on Blueprint and Metropolitan Transportation Plan/Sustainable Communities Strategy 2035 (Mr. McKeever) 10. May Is Bike Month 2012 Recap and 2013 Campaign Update (Mr. Tendick) 11. Transportation Committee Planning Calendar Update (Mr. Carpenter) 12. Other Matters 13. Adjournment ◄ Indicates Action Prepared by: Approved by: Mike McKeever Don Saylor Chief Executive Officer Chair Next committee meeting: Thursday, June 6, 2013 The Meridian Plaza Building is accessible to the disabled. -
Sky and Telescope
SkyandTelescope.com The Lunar 100 By Charles A. Wood Just about every telescope user is familiar with French comet hunter Charles Messier's catalog of fuzzy objects. Messier's 18th-century listing of 109 galaxies, clusters, and nebulae contains some of the largest, brightest, and most visually interesting deep-sky treasures visible from the Northern Hemisphere. Little wonder that observing all the M objects is regarded as a virtual rite of passage for amateur astronomers. But the night sky offers an object that is larger, brighter, and more visually captivating than anything on Messier's list: the Moon. Yet many backyard astronomers never go beyond the astro-tourist stage to acquire the knowledge and understanding necessary to really appreciate what they're looking at, and how magnificent and amazing it truly is. Perhaps this is because after they identify a few of the Moon's most conspicuous features, many amateurs don't know where Many Lunar 100 selections are plainly visible in this image of the full Moon, while others require to look next. a more detailed view, different illumination, or favorable libration. North is up. S&T: Gary The Lunar 100 list is an attempt to provide Moon lovers with Seronik something akin to what deep-sky observers enjoy with the Messier catalog: a selection of telescopic sights to ignite interest and enhance understanding. Presented here is a selection of the Moon's 100 most interesting regions, craters, basins, mountains, rilles, and domes. I challenge observers to find and observe them all and, more important, to consider what each feature tells us about lunar and Earth history. -
Germanium-Bearing Colusite from the Yanahara Mine, Japan, and Its Significance to Ore Genesis
RESOURCE GEOLOGY, 44(1), 33•`38, 1994 Germanium-bearing Colusite from the Yanahara Mine, Japan, and Its Significance to Ore Genesis Katsuo KASE*, Masahiro YAMAMOTO* and Chiharu MITSUNO* Abstract: Colusite, Cu26V2(As,Ge)6S32, containing up to 4.3 wt.% Ge occurs with pyrite, chalcopyrite and bomite in sphalerite-barite-rich ores of the volcanogenic massive sulfide orebody at Hinotani L-1, the Yanahara mine. Electron micro- probe analysis reveals that As and V are pentavalent and Ge is tetravalent in the mineral the same as in germanite and renierite, suggesting that the Ge-bearing colusite was precipitated under high fs2 and foe conditions. These Ge-bearing min- erals sometimes occur in the Kuroko deposits related with felsic volcanism, associated with pyrite, chalcopyrite and bomite as at Hinotani, while practically no Ge-bearing minerals occur in the Besshi-type deposits related with mafic volcanism. It is concluded that the ore solutions responsible for the Hinotani L-1 orebody and possibly for whole orebodies at Yanahara are related with felsic volcanism. ore mineralogy is similar to that of the typical 1. Introduction Besshi-type deposits. The deposit is thus ambigu- There are two major types of volcanogenic mas- ous in the classification, and sometimes called sive sulfide deposits in Japan: Kuroko deposits and Besshi-type deposits. The Kuroko deposits are genetically related with Miocene dacitic-rhy- olitic volcanism, and characterized by high Zn, Pb and Ag contents and an abundance of sulfate min- erals. The Besshi-type cupriferous iron sulfide de- posits, equivalent to Kieslager, occur in the se- quence consisting of basalts and sediments, or their metamorphic equivalents, and are very low in the Pb content and poor in sulfate minerals. -
A Classification of Riparian Wetland Plant Associations of Colorado a Users Guide to the Classification Project
A Classification of Riparian Wetland Plant Associations of Colorado A Users Guide to the Classification Project September 1, 1999 By Gwen Kittel, Erika VanWie, Mary Damm, Reneé Rondeau Steve Kettler, Amy McMullen and John Sanderson Clockwise from top: Conejos River, Conejos County, Populus angustifolia-Picea pungens/Alnus incana Riparian Woodland Flattop Wilderness, Garfield County, Carex aquatilis Riparian Herbaceous Vegetation South Platte River, Logan County, Populus deltoides/Carex lanuginosa Riparian Woodland California Park, Routt County, Salix boothii/Mesic Graminoids Riparian Shrubland Joe Wright Creek, Larimer County, Abies lasiocarpa-Picea engelmannii/Alnus incana Riparian Forest Dolores River, San Miguel County, Forestiera pubescens Riparian Shrubland Center Photo San Luis Valley, Saguache County, Juncus balticus Riparian Herbaceous Vegetation (Photography by Gwen Kittel) 2 Prepared by: Colorado Natural Heritage Program 254 General Services Bldg. Colorado State University Fort Collins, CO 80523 [email protected] This report should be cited as follows: Kittel, Gwen, Erika VanWie, Mary Damm, Reneé Rondeau, Steve Kettler, Amy McMullen, and John Sanderson. 1999. A Classification of Riparian Wetland Plant Associations of Colorado: User Guide to the Classification Project. Colorado Natural Heritage Program, Colorado State University, Fort Collins, CO. 80523 For more information please contact: Colorado Natural Heritage Program, 254 General Service Building, Colorado State University, Fort Collins, Colorado 80523. (970) -
Guide to the Identification of Precious and Semi-Precious Corals in Commercial Trade
'l'llA FFIC YvALE ,.._,..---...- guide to the identification of precious and semi-precious corals in commercial trade Ernest W.T. Cooper, Susan J. Torntore, Angela S.M. Leung, Tanya Shadbolt and Carolyn Dawe September 2011 © 2011 World Wildlife Fund and TRAFFIC. All rights reserved. ISBN 978-0-9693730-3-2 Reproduction and distribution for resale by any means photographic or mechanical, including photocopying, recording, taping or information storage and retrieval systems of any parts of this book, illustrations or texts is prohibited without prior written consent from World Wildlife Fund (WWF). Reproduction for CITES enforcement or educational and other non-commercial purposes by CITES Authorities and the CITES Secretariat is authorized without prior written permission, provided the source is fully acknowledged. Any reproduction, in full or in part, of this publication must credit WWF and TRAFFIC North America. The views of the authors expressed in this publication do not necessarily reflect those of the TRAFFIC network, WWF, or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a joint program of WWF and IUCN. Suggested citation: Cooper, E.W.T., Torntore, S.J., Leung, A.S.M, Shadbolt, T. and Dawe, C. -
Trace Elements and Minerals in Fumarolic Sulfur: the Case of Ebeko Volcano, Kuriles
Hindawi Geofluids Volume 2018, Article ID 4586363, 16 pages https://doi.org/10.1155/2018/4586363 Research Article Trace Elements and Minerals in Fumarolic Sulfur: The Case of Ebeko Volcano, Kuriles E. P. Shevko,1 S. B. Bortnikova,2 N. A. Abrosimova,2 V. S. Kamenetsky ,3,4 S. P. Bortnikova,2 G. L. Panin,2 and M. Zelenski 3 1 Sobolev Institute of Geology and Mineralogy, SBRAS, Novosibirsk 630090, Russia 2Trofmuk Institute of Petroleum Geology and Geophysics, SBRAS, No. 3, Novosibirsk 630090, Russia 3Institute of Experimental Mineralogy RAS, Chernogolovka 142432, Russia 4EarthSciencesandCODES,UniversityofTasmania,PrivateBag79,Hobart,TAS7001,Australia Correspondence should be addressed to M. Zelenski; [email protected] Received 25 June 2017; Revised 13 October 2017; Accepted 14 December 2017; Published 20 March 2018 Academic Editor: Joerg Goettlicher Copyright © 2018 E. P. Shevko et al. Tis is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Native sulfur deposits on fumarolic felds at Ebeko volcano (Northern Kuriles, Russia) are enriched in chalcophile elements (As- Sb-Se-Te-Hg-Cu) and contain rare heavy metal sulfdes (Ag2S, HgS, and CuS), native metal alloys (Au2Pd), and some other low- solubility minerals (CaWO4, BaSO4). Sulfur incrustations are impregnated with numerous particles of fresh and altered andesite groundmass and phenocrysts (pyroxene, magnetite) as well as secondary minerals, such as opal, alunite, and abundant octahedral pyrite crystals. Te comparison of elemental abundances in sulfur and unaltered rocks (andesite) demonstrated that rock-forming elements (Ca, K, Fe, Mn, and Ti) and other lithophile and chalcophile elements are mainly transported by fumarolic gas as aerosol particles, whereas semimetals (As, Sb, Se, and Te), halogens (Br and I), and Hg are likely transported as volatile species, even ∘ at temperatures slightly above 100 C. -
Southwest NM Publication List
Southwest New Mexico Publication Inventory Draft Source of Document/Search Purchase Topic Category Keywords County Title Author Date Publication/Journal/Publisher Type of Document Method Price Geology 1 Geology geology, seismic Southwestern NM Six regionally extensive upper-crustal Ackermann, H.D., L.W. 1994 U.S. Geological Survey, Open-File Report 94- Electronic file USGS publication search refraction profiles, seismic refraction profiles in Southwest New Pankratz, D.P. Klein 695 (DJVU) http://pubs.er.usgs.gov/usgspubs/ southwestern New Mexico ofr/ofr94695 Mexico, 2 Geology Geology, Southwestern NM Magmatism and metamorphism at 1.46 Ga in Amato, J.M., A.O. 2008 In New Mexico Geological Society Fall Field Paper in Book http://nmgs.nmt.edu/publications/g $45.00 magmatism, the Burro Mountains, southwestern New Boullion, and A.E. Conference Guidebook - 59, Geology of the Gila uidebooks/59/ metamorphism, Mexico Sanders Wilderness-Silver City area, 107-116. Burro Mountains, southwestern New Mexico 3 Geology Geology, mineral Catron County Geology and mineral resources of York Anderson, O.J. 1986 New Mexico Bureau of Mines and Mineral Electronic file (PDF) NMBGMR search $10.00 for resources, York Ranch SE quadrangle, Cibola and Catron Resources Open File Report 220A, 22 pages. <http://geoinfo.nmt.edu/publicatio CD Ranch, Fence Counties, New Mexico ns/openfile/details.cfml?Volume=2 Lake, Catron, 20A> Cibola 4 Geology Geology, Zuni Salt Catron County Geology of the Zuni Salt Lake 7 1/2 Minute Anderson, O.J. 1994 New Mexico Bureau of Mines and -
DESCRIPTIVE MODEL of KIPUSHI Cu-Pb-Zn
Model 32c DESCRIPTIVE MODEL OF KIPUSHI Cu-Pb-Zn By Dennis P. Cox and Lawrence R. Bernstein DESCRIPTION Massive base-metal sulfides and As-sulfosalts in dolomite breccias characterized by minor Co, Ge, Ga, U, and V. GEOLOGICAL ENVIRONMENT Rock Types Dolomite, shale. No rocks of unequivocal igneous origin are related to ore formation. [The pseudoaplite at Tsumeb is herein assumed to be a metasedimentary rock following H. D. LeRoex (1955, unpublished report).] Textures Fine-grained massive and carbonaceous, laminated, stromatolitic dolomites. Age Range Unknown; host rocks are Proterozoic in Africa, Devonian in Alaska, Pennsylvanian in Utah. Depositional Environment High fluid flow along tabular or pipe-like fault- or karst (?)-breccia zones. Tectonic Setting(s) Continental platform or shelf terrane with continental or passive margin rifting. Ore formation at Tsumeb and Ruby Creek predates folding. Associated Deposit Types Sedimentary copper, U-veins, barite veins. Sedimentary exhalative Pb-Zn may be a lateral facies. DEPOSIT DESCRIPTION Mineralogy Ruby Creek: pyrite, bornite, chalcocite, chalcopyrite, carrollite, sphalerite, tennantite. Tsumeb: galena, sphalerite, bornite, tennantite, enargite. Kipushi: sphalerite, bornite, chalcopyrite, carrollite, chalcocite, tennantite, pyrite. Less abundant minerals in these deposits are linnaeite, Co-pyrite, germanite, renierite, gallite, tungstenite, molybdenite, and native Bi. Bituminous matter in vugs. At Apex mine, marcasite. Texture/Structure Massive replacement, breccia filling, or stockwork. Replacement textures of pyrite after marcasite at Ruby Creek and Apex. Alteration Dolomitization, sideritization, and silicification may be related to mineralization. Early pyrite or arsenopyrite as breccia filling or dissemination. Ore Controls Abundant diagenetic pyrite or other source of S acts as precipitant of base metals in zones of high porosity and fluid flow. -
NI 43-101 Technical Exploration Report Billali Mine, New Mexico
NI 43-101 Technical Exploration Report Billali Mine, New Mexico Report Date: December 9, 2011 Effective Date: December 9, 2011 Report Prepared for Billali Mine, LLC P. O. Box 207 Duncan, AZ 85534 Report Prepared by Jan C. Rasmussen, Ph. D., R.G., Reg. Mem. SME P. O. Box 36971 Tucson, Arizona 85740 Signed by Qualified Persons: Jan C. Rasmussen, Ph.D., R.G., RM SME NI 43-101 Technical Exploration Report – Billali Mine, New Mexico Page i Summary (Item 1) Property Description and Ownership The Billali mine is a lode mining claim patented in 1899 and now owned by the Billali Mine LLC. The Billali mine is an advanced stage, epithermal, silver-gold quartz vein prospect with minor past production. The mine is located in the northwest end of the Steeple Rock mining district of western New Mexico and adjacent Arizona. The Billali mine project is located in westernmost New Mexico, in the Summit Mountains, Grant County. It is approximately 35 mi (55 km) east of Safford, Arizona, and is approximately 15 mi (25 km) northeast of Duncan, Arizona. The location of the Billali mine adit is approximately latitude 32º53‟04.91” N and longitude 108º59‟01.59” W, elevation 5,343 ft. The claim has a cadastral location of SE ¼ and SW ¼, Section 26, Township 16 South (T16S), Range 21 West (R21W), New Mexico Meridians. Ownership The Billali mine is a patented lode mining claim owned by the Billali Mine LLC. The three managers and owners are Mr. Leslie H. Billingsley, Mr. Richard O. Billingsley, and Mr. Joy J. -
A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores
A Deposit Model for Mississippi Valley-Type Lead-Zinc Ores Chapter A of Mineral Deposit Models for Resource Assessment 2 cm Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus marcasite) from the Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and Scientificsphalerite Investigations alnong colloform Report layers of2010–5070–A light-colored spahlerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerire and iron sulfides. Size of sample is 20x13 cm. Photo by David Leach. U.S. Department of the Interior U.S. Geological Survey COVER: Sample of spheroidal sphalerite with dendritic sphalerite, galena, and iron sulfides (pyrite plus mar- casite) from Pomorzany mine. Note the “up direction” is indicated by “snow-on-the-roof” texture of galena and sphalerite along colloform layers of light-colored sphalerite. Hydrothermal sulfide clasts in the left center of the sample are encrusted by sphalerite and iron sulfides. Size of sample is 20x13 centimeters. (Photograph by David L. Leach, U.S. Geological Survey.) A Deposit Model for Mississippi Valley- Type Lead-Zinc Ores By David L. Leach, Ryan D. Taylor, David L. Fey, Sharon F. Diehl, and Richard W. Saltus Chapter A of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–A U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S.