Characteristics, Extent and Origin of Hydrothermal Alteration at Mount Rainier Volcano, Cascades Arc, USA: Implications for Debris-flow Hazards and Mineral Deposits
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Hypersthene Syenite and Related Rocks of the Blue Ridge Region, Virginia1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA V o l. 27, pp. 193-234 June 1, 1916 HYPERSTHENE SYENITE AND RELATED ROCKS OF THE BLUE RIDGE REGION, VIRGINIA1 BY THOMAS L. WATSON AND JUSTUS H. CLINE (Presented before the Society December 29, 191k) CONTENTS Page Introduction.................................................................................................................. 194 Previous geologic work............................................................................................. 196 Quartz-bearing hypersthene-andesine syenite...................................................... 197 Distribution.......................................................................................................... 197 Megascopic character......................................................................................... 198 Microscopic character........................................................................................ 199 Chemical composition and classification...................................................... 202 Comparison with quartz monzonite.............................................................. 204 Origin and application of name............................................................. 204 Chemical composition................................................................................ 205 Comparison with akerite.................................................................................. 206 Comparison with syenite (andesine anorthosite) of Nelson County, Virginia............................................................................................................. -
Chapter 8 - Natural Environment 8 - Natural Chapter B
• Preserved open spaces This chapter identifies Enumclaw’s environmental • Important wildlife habitat conditions and issues and describes the link between • Unmeasured social and ecological benefits the natural environment and the community’s future. • A sense of community pride and well-being The Washington State Growth Management Act (GMA) requires all towns, cities, and counties adopt Goal NE – 1: To maintain networks of open space development regulations to protect critical areas within the City including wildlife habitat corridors, (aquifer recharge areas, sensitive fish and wildlife stormwater management, trails, and critical areas. habitat, frequently flooded areas, geologically hazardous areas, and wetlands) and resource lands Policies of long-term significance (agricultural, forest, and mineral lands) and that they incorporate “best 1.1 Increase public awareness of the City’s open available science” in those regulations. The City space system. believes these areas are valuable assets for the a. Create a program for education of natural ecological balance they provide and also for the systems and the open spaces of the city. aesthetics and quality of life expected by community b. Standardize signing and other visual residents. The intent is to provide (but not exceed) components typical in park development for critical solid policy foundation for the Critical Area Ordinance areas. (CAO). This chapter illustrates previously-identified 1.2 Encourage corridor development for pedestrian critical areas and resource lands. Continuing and wildlife routes. inventory will clarify critical area boundaries and a. Keep the City’s Parks and Recreation Plan provide additional information on the application of comprehensive and updated, outlining current and policy and regulations. -
Enstatite and Bronzite
On Gem Or'thopyroxenes: Enstatite and Bronzite BY PETE J. DUNN, M.A., F.G.A. Department of Mineral Sciences Smithsonian Institution Washington, D.C. 20560 Introduction 1963). Although petrologists have sub- Enstatite and hypersthene are mem- divided this series into 6· subspecies bers of an isomorphous series of ortho- (Table I), the practicing gemologist is rhombic pyroxenes. The pure end primarily concerned with only the members of the series are enstatite, magnesium-rich members which yield MgSi03 and orthoferrosilite, Fe+2 some attractive gems. Adopting the Si03. Iron and magnesium substitute classification used by Deer et at. mutually between Mg100Fe+20 and (1963), enstatite is designated as a about Mg10Fe+290 (Deer et al., member of the series having 88% to TABLE I NOMENCLATURE OF THE ORTHOPYROXENES enstatite EnlOOFsO to En88Fs12 FeO < 6.50% bronzite En88Fs12 to En70Fs30 FeO> 6.50% hypersthene En70Fs30 to En50Fs50 FeO> 16.32% ferrohypersthene En50Fs50 to En30Fs70 FeO > 27.23% eolite En30Fs70 to En12Fs88 FeO > 38.12% orthoferrosil ite En12Fs88 to EnOFslOO FeO >47.92% En-Enstatite member Fs-Orthoferrosilite member 118 GEMS & GEMOLOGY 100% of the magnesium end member; rences include the noted Ceylon green- bronzite having 70% to 88% of the ish enstatite, and the dark green mate- magnesium end member and hypers- rial from the San Carlos Indian Reser- thene between 50% and 70% of the vation in Arizona (Sinkankas, 1959). magnesium end member. Members of All numbered specimens are from the series with Fe > Mg are usually the U.S. National Mineral Collection at opaque and of little gemological in- the Smithsonian Institution, Washing- terest. -
Mineralogy and Paragenesis of Amphiboles from Gibson Peak Pluton
THE AIVIERICAN MINERALOGIST, VOL. 49, SEPTEMBER-OCTOBER. 1964 MINERALOGY AND PARAGENESIS OF AMPHIBOLES FROM GIBSON PEAK PLUTON. NORTHERN CALIFORNIA PBrBn W. Lrelrlx, U. S. Geotogi,calSurvey, Denaer,Colorad,o. Ansrnacr Ixrnooucrrow Gibson Peak pluton, a 3-squaremile compositeintrusion in the Trin- itv Aips of northern california, is particularly suitablefor investigation of relations between amphibole paragenesisand igneouscrystallization becauseseveral distinctive amphiboles are important constituents of geneticallyrelated rocks that range from gabbro to trondhjemitic tona- lite. This paper describesthe sequenceof amphibole crystallization in difierent parts of the intrusion and reiates the compositionsof three newly analyzedamphiboles to crystallizationsequence and composition of the enclosingrock. The main conclusionis that compositionsof the investigatedamphiboles are as dependenton time of crystallizationwithin their respectiverocks as on bulk rock composition. Pnrnocn.q.pnrcrNtrnpnBTATroN oF THE Alrpnrsolr panecnNpsrs The generalstructural and petrologicfeatures of Gibson peak pluton are describedelsewhere (Lipman, 1963),and onl1-relations bearing on the origin of the amphibolesare summarizedhere. The pluton is com- posite,and five discreteintrusive units have beenrecognized on the basis of field relations.rn order of intrusion theseare hypersthene-hornblende gabbro, (augite-)hornblendegabbro, hornblende diorite, porphyritic quartz-bearingdiorite, and trondhjemitic biotite tonalite. All units show intrusive contacts with the preceding rocks, are petrographically dis- tinctive, and contain at least one amphibole. An interpretation of th" peak complex paragenesisof the Gibson amphiboles,based mainly on the textural featuresdescribed below, is presentedin Fig. 1. The evi- denceis clear orr the occurrenceof the indicated reactions,but the rela- 1321 PETER W. LIPMAN I I I F I I F I 1 I I cd d l :d d9 z z t.i r F-] {Fl z z.zt- z .=l il. -
Minerals of the San Luis Valley and Adjacent Areas of Colorado Charles F
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/22 Minerals of the San Luis Valley and adjacent areas of Colorado Charles F. Bauer, 1971, pp. 231-234 in: San Luis Basin (Colorado), James, H. L.; [ed.], New Mexico Geological Society 22nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 1971 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Owyhee River, Southeastern Oregon
CHARACTERIZATION OF MASS WASTING THROUGH THE SPECTRAL ANALYSIS OF LiDAR IMAGERY: OWYHEE RIVER, SOUTHEASTERN OREGON __________________________________ A Thesis Presented to The Graduate Faculty Central Washington University __________________________________ In Partial Fulfillment of the Requirements for the Degree Master of Science Geology __________________________________ by Christopher Earl Markley November 2013 CENTRAL WASHINGTON UNIVERSITY Graduate Studies We hereby approve the thesis of Christopher Earl Markley Candidate for the degree of Master of Science APPROVED FOR THE GRADUATE FACULTY ______________ _________________________________________ Dr. Lisa Ely, Committee Chair ______________ _________________________________________ Dr. Elizabeth Safran ______________ _________________________________________ Dr. Audrey Huerta ______________ _________________________________________ Dean of Graduate Studies ii ABSTRACT CHARACTERIZATION OF MASS WASTING THROUGH THE SPECTRAL ANALYSIS OF LiDAR IMAGERY: OWYHEE RIVER, SOUTHEASTERN OREGON by Christopher Earl Markley November 2013 Quantifying landslide character is an important aspect of understanding hillslope- channel interactions. Spectral analysis of high-resolution, LiDAR derived, DEMs was carried out following methods described by Booth et al. (2009) to determine the characteristic spectral signature inherent in different styles of landslides in the Owyhee River Canyon in southeastern Oregon. The main factor in landslide generation in this location is a lithologic contact in which a -
The Significance of Cordierite-Hypersthene Assemblages from the Beitbridge Region of the Central Limpopo Belt; Evidence for Rapid Decompression in the Archaean?
American Mineralogist, Volume 69, pages 1036-/049, /984 The significance of cordierite-hypersthene assemblages from the Beitbridge region of the Central Limpopo Belt; evidence for rapid decompression in the Archaean? N. B. W. HARRIS Department of Earth Sciences Open University Milton Keynes, England MK7 6AA AND T. J. B. HOLLAND Department of Earth Sciences University of Cambridge Cambridge, England CB23EQ Abstract The following model equilibria have been observed in metapelites from the Diti Formation of the Central Limpopo belt. (Mg,Fe)zSi206 + 2 AhSiOs + Si02 = (Mg,Fe)zAI4SisOI8 Orthopyroxene Sillimanite Quartz Cordierite 2 (Mg,FehAhShOI2 + 4 AhSiOs + 5 Si02 = 3 (Mg,Fe)zAI4SisO'8 Garnet Sillimanite Quartz Cordierite 2 (Mg,FehAhSi30I2 + 3 Si02 = (Mg,Fe)zAI4SisO'8 + 2 (Mg,Fe)zSi206 Garnet Quartz Cordierite Orthopyroxene 5 (Mg,Fe)zSi206 + 10 Al2SiOs = 4 (Mg,Fe)zAI4Sis018 + 2 (Mg,Fe)Ah04 Orthopyroxene Sillimanite Cordierite Spinel An internally consistent thermodynamic data set in the MAS system for constituent phases has been derived which is also consistent with both calorimetric data and experimental equilibria. Microprobe analyses of the phases present in the Limpopo metapelites have been applied to equilibrium equations derived from this data set, and conditions of P = 4-5 kbar, T> 670°C are implied assuming aH,o = O. Application of published cordierite-free thermobarometers both from the pelites and interlayered mafic granulites, provides similar P-T conditions (P = 3.5-5 kbar, T = 750:<:50°C) indicating that metamorphism was virtually dry. Conditions of aH,O< 0.5 are also implied by analysis of equilibria involving hydrous phases. Decompression reactions are observed both in this and in earlier studies of supracrustal rocks from the Central Limpopo Belt, and a period of essentially isothermal uplift is suggested, which raised crustal blocks from depths of about 40 km to 15 km. -
Redalyc.PETROGRAPHY of EXOTIC CLASTS in the SOEBI BLANCO
Boletín de Ciencias de la Tierra ISSN: 0120-3630 [email protected] Universidad Nacional de Colombia Colombia URBANI, FRANCO; GRANDE, SEBASTIÁN; MÉNDEZ BAAMONDE, JOSÉ PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES Boletín de Ciencias de la Tierra, núm. 33, enero-junio, 2013, pp. 59-70 Universidad Nacional de Colombia Medellín, Colombia Available in: http://www.redalyc.org/articulo.oa?id=169528792004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative PETROGRAPHY OF EXOTIC CLASTS IN THE SOEBI BLANCO FORMATION, BONAIRE, NETHERLANDS ANTILLES “PETROGRAFÍA DE LOS CLASTOS EXOTICOS DE LA FORMACIÓN SOEBI BLANCO, BONAIRE, ANTILLAS HOLANDESAS FRANCO URBANI Fundación Venezolana de Investigaciones Sismológicas, Caracas - Universidad Central de Venezuela, Facultad de Ingeniería, Escuela de Geología, Minas y Geofísica SEBASTIÁN GRANDE Universidad Central de Venezuela, Facultad de Ingeniería, Escuela de Geología, Minas y Geofísica. JOSÉ MÉNDEZ BAAMONDE Universidad Central de Venezuela, Facultad de Ciencias. Instituto de Ciencias de la Tierra. Ciudad Universitaria. Caracas. Email: [email protected]. Recibido para evaluación: 10 de marzo de 2013 / Aceptación: 19 de Junio de 2013 / Recibida versión fi nal: 02 de Julio de 2013 ABSTRACT: The Paleocen e Soebi Blanco Formation in the island of Bonaire in Southeastern Caribbean has attracted the attention of geologists since 1931 when P. J. Pijpers pointed out the presence of a wide range of “foreign pebbles” in conglomerate beds. Interest was further boosted in 1986 with a Grenvillian age determined in a granulitic pebble (ca. -
Nördlingen 2010: the Ries Crater, the Moon, and the Future of Human Space Exploration, P
Program and Abstract Volume LPI Contribution No. 1559 The Ries Crater, the Moon, and the Future of Human Space Exploration June 25–27, 2010 Nördlingen, Germany Sponsors Museum für Naturkunde – Leibniz-Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Germany Institut für Planetologie, University of Münster, Germany Deutsches Zentrum für Luft- und Raumfahrt DLR (German Aerospace Center) at Berlin, Germany Institute of Geoscience, University of Freiburg, Germany Lunar and Planetary Institute (LPI), Houston, USA Deutsche Forschungsgemeinschaft (German Science Foundation), Bonn, Germany Barringer Crater Company, Decatur, USA Meteoritical Society, USA City of Nördlingen, Germany Ries Crater Museum, Nördlingen, Germany Community of Otting, Ries, Germany Märker Cement Factory, Harburg, Germany Local Organization City of Nördlingen Museum für Naturkunde – Leibniz- Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin Ries Crater Museum, Nördlingen Center of Ries Crater and Impact Research (ZERIN), Nördlingen Society Friends of the Ries Crater Museum, Nördlingen Community of Otting, Ries Märker Cement Factory, Harburg Organizing and Program Committee Prof. Dieter Stöffler, Museum für Naturkunde, Berlin Prof. Wolf Uwe Reimold, Museum für Naturkunde, Berlin Dr. Kai Wünnemann, Museum für Naturkunde, Berlin Hermann Faul, First Major of Nördlingen Prof. Thomas Kenkmann, Freiburg Prof. Harald Hiesinger, Münster Prof. Tilman Spohn, DLR, Berlin Dr. Ulrich Köhler, DLR, Berlin Dr. David Kring, LPI, Houston Dr. Axel Wittmann, LPI, Houston Gisela Pösges, Ries Crater Museum, Nördlingen Ralf Barfeld, Chair, Society Friends of the Ries Crater Museum Lunar and Planetary Institute LPI Contribution No. 1559 Compiled in 2010 by LUNAR AND PLANETARY INSTITUTE The Lunar and Planetary Institute is operated by the Universities Space Research Association under a cooperative agreement with the Science Mission Directorate of the National Aeronautics and Space Administration. -
Volcanic Hazards • Washington State Is Home to Five Active Volcanoes Located in the Cascade Range, East of Seattle: Mt
CITY OF SEATTLE CEMP – SHIVA GEOLOGIC HAZARDS Volcanic Hazards • Washington State is home to five active volcanoes located in the Cascade Range, east of Seattle: Mt. Baker, Glacier Peak, Mt. Rainier, Mt. Adams and Mt. St. Helens (see figure [Cascades volcanoes]). Washington and California are the only states in the lower 48 to experience a major volcanic eruption in the past 150 years. • Major hazards caused by eruptions are blast, pyroclastic flows, lahars, post-lahar sedimentation, and ashfall. Seattle is too far from any volcanoes to receive damage from blast and pyroclastic flows. o Ash falls could reach Seattle from any of the Cascades volcanoes, but prevailing weather patterns would typically blow ash away from Seattle, to the east side of the state. However, to underscore this uncertainty, ash deposits from multiple pre-historic eruptions have been found in Seattle, including Glacier Peak (less than 1 inch) and Mt. Mazama/Crater Lake (amount unknown) ash. o The City of Seattle depends on power, water, and transportation resources located in the Cascades and Eastern Washington where ash is more likely to fall. Seattle City Light operates dams directly east of Mt. Baker and in Pend Oreille County in eastern Washington. Seattle’s water comes from two reservoirs located on the western slopes of the Central Cascades, so they are outside the probable path of ashfall. o If heavy ash were to fall over Seattle it would create health problems, paralyze the transportation system, destroy many mechanical objects, endanger the utility networks and cost millions of dollars to clean up. Ash can be very dangerous to aviation. -
South Prairie Creek Activity
Geomonpr¡c EvtlumoN aND Gx¡trer Mrcnmor Zo¡¡e Annlvsls Sourr Pnrun¡¡ CRETK H¡RcE CouNw, WASHINGToN Apnlzg,2005 Fon PtERcE Cou¡¡w W¡reR PRooRAilE DIvIsIoN GroEne rn ÊEasJ/ FileNo. 2998-M7-00 Geomorphic Evaluation and Channel Migration Zone Analysis FilE No. 2998-002-00 Aprll 29, 200ö Prepared for: Pierce Co¡rnty Water Programs Divlsíon 9850 - 64¡n Street West University Place, Washlngton 9g467 Altentlon: Dennis Dixon Prepared by: GeoÊngineers, lnc. 600 Dupont Street Bellingham, Washlngton 98225 (360) 647-1510 Mclnelly, LG, LEG, LHG Clvfi{:MÂ&D!ijr RcdndslllrFn¡ l¡\29911007ff)R.rlr x Dirchrmrr chelrunir fonn. f¡c¡iailu rr '{ny h¡ld rtpy uf tlu orígíæl rlonrileil ($Ì¡i[ lÉrt. tdrlc. ent/or tlgun[ jf uü anv !¡R onl¡ acqryoftlrc origíml ,lrrunrcrt"nruoritdn¡lrbc;;cnr ¡mrilstl ¡r¡¡(hnrcnts bsroili iy tìætinginccrs. hc. urd wilt*r- o" r¡*oni"¡rl d.w,-l of rôsilnl C'u¡r¡rl¡gr!È IIt5 h,v (ìcot:ntiils. lns ,lll rlghu rÉscnsL lìk No. J918.007.0t) Tnele or Corure¡¡rs Paqe No. PROJECT OBJECTIVE ........ 1 PROJECT APPROACH AND SCOPE ............... 1 REPORT ORGAN|ZAT|ON.............. ..................2 GEOMORPHTC EVALUATTON ............. .......................2 |NTRODUCT|ON.............. ...............2 REGTONAL SETTTNG ....................3 Location ............3 Basin Topography .......... ...........................3 Climate........ ........................... 3 Basin Hydrology............. ...........................3 GEOLOGTC HTSTORY ...................5 lntroduction. ...........................5 Cascades Mountain Range and the Puget Sound -
WTU Herbarium Specimen Label Data
WTU Herbarium Specimen Label Data Generated from the WTU Herbarium Database September 24, 2021 at 3:25 am http://biology.burke.washington.edu/herbarium/collections/search.php Specimen records: 2570 Images: 445 Search Parameters: Label Query: Genus = "Eriogonum" Polygonaceae Polygonaceae Eriogonum umbellatum Torr. Eriogonum flavum Nutt. var. piperi (Greene) M.E. Jones U.S.A., OREGON, JOSEPHINE COUNTY: U.S.A., OREGON, WALLOWA COUNTY: Siskiyou Mountains: On road 4402, 3 miles south east of junction Wallowa-Whitman National Forest, Wallowa Valley Ranger District. with Forest Road 112. Mount Howard, above tramway buildings. Elev. 3250 ft. Elev. 8220 ft. 41° 59' 52" N, 123° 48' 8" W; T41S R9W S18; WGS 84, 45° 15' 42" N, 117° 10' 33" W; T3S R45E S34; NAD 27 uncertainty: 500 m., Source: Digital map, Georef'd by John Open subalpine meadow with scattered Pinus albicaulis, understory Bassett mostly graminoids. Sulfury yellow, forms clumps. Phenology: Open, young forest of Ponderosa pine, Calocedrus, with Flowers. Origin: Native. Arctostaphylos shrub layer. In mats to 1 meter diameter; head of yellow flowers. Phenology: Flowers. Origin: Native. Tracy Fuentes 421 20 Jul 2002 with Sharon Rodman and Peter Zika Roger Fuller 98-36 28 Jun 1998 WTU-360560 WTU-406048 Polygonaceae Polygonaceae Eriogonum ovalifolium Nutt. var. nivale (Canby ex Coville) M.E. Jones Eriogonum pyrolifolium Hook. U.S.A., OREGON, WALLOWA COUNTY: U.S.A., WASHINGTON, PIERCE COUNTY: Wallowa-Whitman National Forest, Wallowa Valley Ranger District. Mount Rainier National Park, NE side; at small basin above The Mount Howard, above tramway buildings. Palisades Rock, around perimeter of small pond.