Guide to Prospecting and Rock Hunting in Wyoming
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Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic Responses Are Standardized to 1/2" X 1/2" N-52 Magnet Cylinders
Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic responses are standardized to 1/2" X 1/2" N-52 magnet cylinders. Colorless and extremely pale stones of any species tend to be Inert (diamagnetic). Black opaque stones of many species are strongly magnetic and may Pick Up or Drag. Pick Up and Drag responses are weight-dependent. Direct responses on the Index apply to gems 1-4cts. Larger gems may be too heavy to Pick Up or Drag. Smaller non-Garnet gems with strong magnetism may Pick Up. Gemstone Response Range SI X 10 (-6) Range Cause of Color Actinolite Nephrite Jade (black) Strong to Drags 321-577 SI Iron Nephrite Jade (green) Moderate to Drags 91-343 Iron, Chromium Nephrite Jade (white, yellow) Inert < 0 (diamagnetic) Iron Pargasite (green) Inert < 0 (diamagnetic) Iron, Vanadium Pargasite (orangey brown) Weak 35 SI Iron Afghanite (blue) Inert < 0 (diamagnetic) Chromium, Vanadium Amber (any color) Inert < 0 (diamagnetic) Charge Transfer involving Organic Compounds Amblygonite-Montebrasite (blue, green) Inert < 0 (diamagnetic) Iron, Manganese Andalusite Inert to Weak < 0 -26 Iron-Oxygen-Titanium Charge Transfer Apatite Transparent blue, green, yellow Inert (Weak in rare cases) < 0 (diamagnetic) Mang., Rare-earth, Charge Transfer, Color Centers Cat's eye translucent yellow, yellowish brown Weak to Strong < 20 - >120 Rare-earth Metals Astrophyllite Strong 1146-1328 Iron, Manganese Axinite Drags 603-616 SI Iron Azurite (opaque) Strong 382 SI Copper Barite (pale brown, blue) Inert < 0 (diamagnetic) Color Centers Bastnasite -
Taxonomic Overview of the Greater Fritillary Genus Speyeria Scudder
INSECTA MUNDI A Journal of World Insect Systematics 0090 Taxonomic overview of the greater fritillary genus Speyeria Scudder and the atlantis hesperis species complexes, with species accounts, type images, and relevant literature (Lepidoptera: Nymphalidae) James C. Dunford McGuire Center for Lepidoptera and Biodiversity Florida Museum of Natural History, University of Florida PO Box 112710, Gainesville, FL 326112710, USA Date of Issue: September 26, 2009 CENTER FOR SYSTEMATIC ENTOMOLOGY, INC., Gainesville, FL James C. Dunford Taxonomic overview of the greater fritillary genus Speyeria Scudder and the atlantis hesperis species complexes, with species accounts, type images, and relevant literature (Lepidoptera: Nymphalidae) Insecta Mundi 0090: 174 Published in 2009 by Center for Systematic Entomology, Inc. P. O. Box 141874 Gainesville, FL 326141874 U. S. A. http://www.centerforsystematicentomology.org/ Insecta Mundi is a journal primarily devoted to insect systematics, but articles can be published on any nonmarine arthropod taxon. Manuscripts considered for publication include, but are not limited to, systematic or taxonomic studies, revisions, nomenclatural changes, faunal studies, book reviews, phylo genetic analyses, biological or behavioral studies, etc. Insecta Mundi is widely distributed, and refer- enced or abstracted by several sources including the Zoological Record, CAB Abstracts, etc. As of 2007, Insecta Mundi is published irregularly throughout the year, not as quarterly issues. As manuscripts are completed they are published and given an individual number. Manuscripts must be peer reviewed prior to submission, after which they are again reviewed by the editorial board to insure quality. One author of each submitted manuscript must be a current member of the Center for System- atic Entomology. -
An Exploration of Jade Maria Jones
Eastern Michigan University DigitalCommons@EMU Senior Honors Theses Honors College 2004 An Exploration of Jade Maria Jones Follow this and additional works at: http://commons.emich.edu/honors Recommended Citation Jones, Maria, "An Exploration of Jade" (2004). Senior Honors Theses. 85. http://commons.emich.edu/honors/85 This Open Access Senior Honors Thesis is brought to you for free and open access by the Honors College at DigitalCommons@EMU. It has been accepted for inclusion in Senior Honors Theses by an authorized administrator of DigitalCommons@EMU. For more information, please contact lib- [email protected]. An Exploration of Jade Abstract Abstract: This is a research paper studying the history of Jade carving during the Chinese Han Dynasty from 206 B.C to 220 A.D. The ap per explains the meaning of jade to the Chinese people and examines the origin of the precious stone for the Han people and other generations of dynasties. There is an accurate telling of Han beliefs followed by a descriptive passage on the history of religious influence on the Han people. There is an extensive study on the history of the Han people in general and a lengthy report on the different forms of jade and their functions for the Han people. Degree Type Open Access Senior Honors Thesis Department Art First Advisor Dr. Richard Rubenfeld Second Advisor Leslie Atzmon Keywords Jade art objects, Art objects, Chinese, Jade This open access senior honors thesis is available at DigitalCommons@EMU: http://commons.emich.edu/honors/85 AN EXPLORATION OFJ/\DL: by :'vlariaJones A St~nior ThcsIs Submitted to the !:astern tv1ichigan Umversny 1ionors Program In Partial Fulfillment of the Requiremems for Graduation With Honors in Fine Art: CcHJCcntratinnin Graphic Design 1 I I ! ~--'~""'-"""'- ,,=.. -
Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China)
minerals Article Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China) Ying Jiang 1, Guanghai Shi 1,* , Liguo Xu 2 and Xinling Li 3 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; [email protected] 2 Geological Museum of China, Beijing 100034, China; [email protected] 3 Xinjiang Uygur Autonomous Region Product Quality Supervision and Inspection Institute, Xinjiang 830004, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-8232-1836 Received: 6 April 2020; Accepted: 6 May 2020; Published: 8 May 2020 Abstract: The historic Yinggelike nephrite jade deposit in the Altyn Tagh Mountains (Xinjiang, NW China) is renowned for its gem-quality nephrite with its characteristic light-yellow to greenish-yellow hue. Despite the extraordinary gemological quality and commercial significance of the Yinggelike nephrite, little work has been done on this nephrite deposit, due to its geographic remoteness and inaccessibility. This contribution presents the first systematic mineralogical and geochemical studies on the Yinggelike nephrite deposit. Electron probe microanalysis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry (ICP-MS) and isotope ratio mass spectrometry were used to measure the mineralogy, bulk-rock chemistry and stable (O and H) isotopes characteristics of samples from Yinggelike. Field investigation shows that the Yinggelike nephrite orebody occurs in the dolomitic marble near the intruding granitoids. Petrographic studies and EMPA data indicate that the nephrite is mainly composed of fine-grained tremolite, with accessory pargasite, diopside, epidote, allanite, prehnite, andesine, titanite, zircon, and calcite. Geochemical studies show that all nephrite samples have low bulk-rock Fe/(Fe + Mg) values (0.02–0.05), as well as low Cr (0.81–34.68 ppm), Co (1.10–2.91 ppm), and Ni (0.52–20.15 ppm) contents. -
Stratigraphy and Correlation of Glacial Deposits of the Rocky Mountains, the Colorado Plateau and the Ranges of the Great Basin
STRATIGRAPHY AND CORRELATION OF GLACIAL DEPOSITS OF THE ROCKY MOUNTAINS, THE COLORADO PLATEAU AND THE RANGES OF THE GREAT BASIN Gerald M. Richmond u.s. Geological Survey, Box 25046, Federal Center, MS 913, Denver, Colorado 80225, U.S.A. INTRODUCTION glaciations (Charts lA, 1B) see Fullerton and Rich- mond, Comparison of the marine oxygen isotope The Rocky Mountains, Colorado Plateau, and Basin record, the eustatic sea level record, and the chronology and Range Provinces (Fig. 1) together occupy much of of glaciation in the United States of America (this the western interior United States. These regions volume). include approximately 140 mountain ranges that were glaciated during the Pleistocene. Most of the glaciers Historical Perspective were valley glaciers, but ice caps formed on uplands Following early recognition of deposits of two alpine locally. Discussion of the deposits of all of these ranges glaciations (Gilbert, 1890; Ball, 1908; Capps, 1909; would require monographic analysis. To avoid this, Atwood, 1909), deposits of three glaciations gradually representative ranges in each province are reviewed. became widely recognized (Alden, 1912, 1932, 1953; Atwood and Mather, 1912, 1932; Alden and Stebinger, Purpose and Scope 1913; Blackwelder, 1915; Atwood, 1915; Fryxell, 1930; This report summarizes the evidence for correlation Bradley, 1936). Subsequently drift of the intermediate of the Quaternary glacial deposits in 26 broadly glaciation was shown to represent two glacial advances distributed mountain ranges selected on the basis of (Fryxell, 1930; Horberg, 1938; Richmond, 1948, 1962a; availability of detailed information and length of glacial Moss, 1951a; Nelson, 1954; Holmes and Moss, 1955), record. and the older drift was shown to include deposits of Because the glacial deposits rarely are traceable from three glaciations (Richmond, 1957, 1962a, 1964a). -
Forest Insect and Disease Conditions in the United States 2000
United States Department Forest Insect and Of Agriculture Forest Service Disease Conditions Forest Health Protection in the United States March 2002 2000 Healthy Forests Make A World of Difference United States Department Of Agriculture Forest Insect and Forest Service Disease Conditions Forest Health Protection in the United States March 2002 2000 PREFACE This is the 50th annual report prepared by the U.S. • seed orchard insects and diseases; Department of Agriculture Forest Service (USDA • nursery insects and diseases; and Forest Service) of the insect and disease conditions of • abiotic damage. the Nation's forests. This report responds to direction in the Cooperative Forestry Assistance Act of 1978, as These categories are listed in the table of contents; amended, to conduct surveys and report annually on there is no index. insect and disease conditions of major national significance. Insect and disease conditions of local The information in this report is provided by the Forest importance are reported in regional and State reports. Health Protection Program of the USDA Forest Service. This program serves all Federal lands, The report describes the extent and nature of insect- including the National Forest System and the lands and disease-caused damage of national significance in administered by the Departments of Defense and 2000. As in the past, selected insect and disease Interior. Service is also provided to tribal lands. The conditions are highlighted in the front section of the program provides assistance to private landowners report. Maps are provided for some pests showing through the State foresters. A key part of the program affected counties in the East and affected areas in the is detecting and reporting insect and disease epidemics West. -
Aerial Survey Highlights for Colorado 2014
Aerial Survey Highlights for Colorado 2014 Aerial detection surveys of tree killing or damaging insects and diseases are conducted annually over Colorado’s forest lands. This is a cooperative effort between the US Forest Service and the Colorado State Forest Service. In 2014, 28 million acres were surveyed by 7 trained federal and state surveyors. Highlights of the survey by damage agent are reported below. In 2014, all reported agents are insects that kill and/or defoliate trees. This report includes only forest damage that is visible from the air. Spruce Beetle • Since 1996, spruce beetle has affected approximately 1,397,000 acres to varying degrees in Colorado. • Spruce beetle activity was detected on 485,000 acres in Colorado in 2014. Of these, 253,000 acres are in areas not previously mapped as having spruce beetle activity (new acres). This epidemic continues to expand rapidly (Figures 1, 2). In some areas, the outbreak has moved through entire drainages in the course of one year. In the most heavily impacted drainages, nearly every mature spruce has been killed (Figure 3). • The spruce beetle epidemic is expanding most rapidly in southern Colorado’s Forests and impacts many thousands of acres. Areas affected are found from the La Garita Wilderness Area to north of Cottonwood Pass, the Sangre de Cristo and Wet Mountains, as well as south to the Colorado border and into New Mexico. Aerial survey in south central Colorado showed spruce beetle epidemics expanded on the San Juan (26,000 new acres on 53,000 active acres), Rio Grande (78,000 new acres on 192,000 active acres), Gunnison (54,000 new acres on 79,000 active acres), and San Isabel (26,000 new acres on 31,000 active acres) National Forests. -
5-Year Review Short Form Summary
5-Year Review Short Form Summary Species Reviewed: Preble’s meadow jumping mouse (Zapus hudsonius preblei) FR Notice Announcing Initiation of This Review: March 31, 2004. 90-Day Finding for a Petition to Delist the Preble’s Meadow Jumping Mouse in Colorado and Wyoming and Initiation of a 5-Year Review (69 FR 16944-16946). Lead Region/Field Office: Region 6, Seth Willey, Recovery Coordinator, 303-236-4257. Colorado Field Office, Susan Linner, Field Supervisor, 303-236-4773. Name of Reviewer: Peter Plage, Colorado Field Office, 303-236-4750. Cooperating Field Office: Wyoming Field Office, Brian Kelly, Field Supervisor, 307-772-2374. Current Classification: Threatened rangewide. Current Recovery Priority Number: 9c. This recovery priority number is indicative of a subspecies facing a moderate degree of threat, a high recovery potential, and whose recovery may be in conflict with construction or other development projects or other forms of economic activity. Methodology used to complete the review: The 5-year review for the Preble’s meadow jumping mouse (Preble’s) was accomplished through the petition and rulemaking process. On December 23, 2003, we received two nearly identical petitions from the State of Wyoming’s Office of the Governor and from Coloradans for Water Conservation and Development, seeking to remove the Preble’s from the Federal List of Endangered and Threatened Wildlife. Both petitions were similar and maintained that the Preble’s should be delisted based on the taxonomic revision, and based on new distribution, abundance, and trends data that suggested the Preble’s was no longer threatened. On March 31, 2004, we published a notice announcing a 90-day finding that the petitions presented substantial information indicating that the petitioned action may be warranted and initiated a 5-year review (69 FR 16944-16946). -
A Publication of the Wyoming Native Plant Society
Castilleja A Publication of the Wyoming Native Plant Society October 2004, Volume 23, No. 3 www.uwyo.edu/wyndd/wnps/wnps_home.htm In this issue: Relicts and Refugia . 1 Floristic Diversity of Wyoming Counties . 3 Botanical Novitiates Find Botanical Novelty . 4 Critical Habitat for the Colorado Butterfly Plant . 5 Requiem for a Lawnmower – review. 6 Rocky Mountain Natural History – review . .7 Whitebark Pine - excerpt. 8 Cynoglossum boreale – addition to the state flora 9 Raising Livestock and Lowering Carbon Dioxide . 10 Scholarship Announcement . 11 Natives vs. Imposters. 12 Relicts and Refugia By Bonnie Heidel For all of the breath-taking alpine topography of the Medicine Bow Range, some of its heart-thumping botany lies low across rolling expanses. Three years and three stages of peatland research have documented vast Above: Eriophorum gracile (slender cotton-grass) is montane fen systems in the Medicine Bow circumboreal, with outlying distribution in northwestern Range, refugia for eleven rare Wyoming Wyoming, the Medicine Bow Range and South Park in vascular plant species of concern including five Colorado By B. Heidel relict species previously unknown from southern Wyoming. peatlands harbor close to 10% of the rare Peatland rare species are disjunct or Wyoming plant species of concern. peripheral as they are present in Wyoming, Botanists took a plunge into peatlands denizens of high latitudes, not state and with pilot site surveys on the Medicine Bow and regional endemics that are the focus of most the Shoshone national forests to compile a Wyoming Natural Diversity Database botany working list of peatland rare species, flora, and research. However, review of the Wyoming vegetation at a small number of known or plant species of concern list in 2002 compared inferred peatland study sites (Heidel and against regional peatland floras indicated that Laursen 2003 a, b; Mellmann-Brown 2004). -
Denudation History and Internal Structure of the Front Range and Wet Mountains, Colorado, Based on Apatite-Fission-Track Thermoc
NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN 160, 2004 41 Denudation history and internal structure of the Front Range and Wet Mountains, Colorado, based on apatitefissiontrack thermochronology 1 2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801Shari A. Kelley and Charles E. Chapin 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract An apatite fissiontrack (AFT) partial annealing zone (PAZ) that developed during Late Cretaceous time provides a structural datum for addressing questions concerning the timing and magnitude of denudation, as well as the structural style of Laramide deformation, in the Front Range and Wet Mountains of Colorado. AFT cooling ages are also used to estimate the magnitude and sense of dis placement across faults and to differentiate between exhumation and faultgenerated topography. AFT ages at low elevationX along the eastern margin of the southern Front Range between Golden and Colorado Springs are from 100 to 270 Ma, and the mean track lengths are short (10–12.5 µm). Old AFT ages (> 100 Ma) are also found along the western margin of the Front Range along the Elkhorn thrust fault. In contrast AFT ages of 45–75 Ma and relatively long mean track lengths (12.5–14 µm) are common in the interior of the range. The AFT ages generally decrease across northwesttrending faults toward the center of the range. The base of a fossil PAZ, which separates AFT cooling ages of 45– 70 Ma at low elevations from AFT ages > 100 Ma at higher elevations, is exposed on the south side of Pikes Peak, on Mt. -
Related Magmatism in the Upper Wind River Basin, Wyoming (USA), GEOSPHERE; V
Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE The leading wisps of Yellowstone: Post–ca. 5 Ma extension- related magmatism in the upper Wind River Basin, Wyoming (USA), GEOSPHERE; v. 14, no. 1 associated with the Yellowstone hotspot tectonic parabola doi:10.1130/GES01553.1 Matthew E. Brueseke1, Anna C. Downey1, Zachary C. Dodd1, William K. Hart2, Dave C. Adams3, and Jeff A. Benowitz4 12 figures; 2 tables; 1 supplemental file 1Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, Kansas 66506, USA 2Department of Geology and Environmental Earth Science, Miami University, 118C Shideler Hall, Oxford, Ohio 45056, USA 3Box 155, Teton Village, Wyoming 83025, USA CORRESPONDENCE: brueseke@ ksu .edu 4Geophysical Institute and Geochronology Laboratory, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA CITATION: Brueseke, M.E., Downey, A.C., Dodd, Z.C., Hart, W.K., Adams, D.C., and Benowitz, J.A., 2018, The leading wisps of Yellowstone: Post–ca. 5 Ma ABSTRACT the issue of linking volcanic events to a specific driving mechanism (Fouch, extension-related magmatism in the upper Wind River 2012; Kuehn et al., 2015). Complicating matters, magmatism often continues Basin, Wyoming (USA), associated with the Yellow- The upper Wind River Basin in northwest Wyoming (USA) is located ~80– long after (e.g., millions of years) the upper plate has been translated away stone hotspot tectonic parabola: Geosphere, v. 14, no. 1, p. 74–94, doi:10.1130/GES01553.1. 100 km southeast of the Yellowstone Plateau volcanic field. While the upper from an upwelling plume (Bercovici and Mahoney, 1994; Sleep, 2003; Shervais Wind River Basin is a manifestation of primarily Cretaceous to Eocene Lara- and Hanan, 2008; Jean et al., 2014). -
Alkalic-Type Epithermal Gold Deposit Model
Alkalic-Type Epithermal Gold Deposit Model Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S. Department of the Interior U.S. Geological Survey Cover. Photographs of alkalic-type epithermal gold deposits and ores. Upper left: Cripple Creek, Colorado—One of the largest alkalic-type epithermal gold deposits in the world showing the Cresson open pit looking southwest. Note the green funnel-shaped area along the pit wall is lamprophyre of the Cresson Pipe, a common alkaline rock type in these deposits. The Cresson Pipe was mined by historic underground methods and produced some of the richest ores in the district. The holes that are visible along several benches in the pit (bottom portion of photograph) are historic underground mine levels. (Photograph by Karen Kelley, USGS, April, 2002). Upper right: High-grade gold ore from the Porgera deposit in Papua New Guinea showing native gold intergrown with gold-silver telluride minerals (silvery) and pyrite. (Photograph by Jeremy Richards, University of Alberta, Canada, 2013, used with permission). Lower left: Mayflower Mine, Montana—High-grade hessite, petzite, benleonardite, and coloradoite in limestone. (Photograph by Paul Spry, Iowa State University, 1995, used with permission). Lower right: View of north rim of Navilawa Caldera, which hosts the Banana Creek prospect, Fiji, from the portal of the Tuvatu prospect. (Photograph by Paul Spry, Iowa State University, 2007, used with permission). Alkalic-Type Epithermal Gold Deposit Model By Karen D. Kelley, Paul G. Spry, Virginia T. McLemore, David L. Fey, and Eric D. Anderson Chapter R of Mineral Deposit Models for Resource Assessment Scientific Investigations Report 2010–5070–R U.S.