Cultural Resource Surveys Have Been Completed Within 1 Mile of the Proposed Project Area
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Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
GEOG 442 – the Great Extinctions Evolution Has Spawned An
GEOG 442 – The Great Extinctions Evolution has spawned an incredible diversity of lineages from nearly the beginning of the planet itself to the present. Speciation often results from the isolation of a population of organisms, which then evolve along their own trajectories, depending on such factors as founder effect, genetic drift, and natural selection in environments that are different to some extent from the range of environments from which they've been isolated. Speciation can be allopatric or sympatric. Once a new species forms, it is endemic to its source region. It may then be later able to escape its source region, migrating into new regions and even becoming cosmopolitan. Even a cosmopolitan species is subject to environmental change out of its environmental envelope and to competition from other species. This can then set off a process of decline and local extirpations across its range, resulting in disjunct distribution, eventually recreating an endemic distribution in its last redoubt before its final extinction. Extinction, then, is the normal fate of species. If a species is lucky, it may go extinct by dint of having evolved into one or more daughter lineages that are so divergent from the parent that we consider the parent extinct. Many species are not lucky: Their last lineage fades out. Extinction is normal. We can talk about the background extinction rate, the normal loss of species and lineages through time. The average duration of species is somewhere between 1 and 13 million years, depending on the kind of critter we're talking about. Mammal species tend to last about 1-2 million years; unicellular dinoflagellate algae are on the other end at 13 million years. -
1783-84 Laki Eruption, Iceland
1783-84 Laki eruption, Iceland Eruption History and Atmospheric Effects Thor Thordarson Faculty of Earth sciences, University of Iceland 12/8/2017 1 Atmospheric Effects of the 1783-84 Laki Eruption in Iceland Outline . Volcano-Climate interactions - background Laki eruption . Eruption history . Sulfur release and aerosol loading . Plume transport and aerosol dispersal . Environmental and climatic effects 12/8/2017. Concluding Remarks 2 Santorini, 1628 BC Tambora, 1815 Etna, 44 BC Lakagígar, 1783 Toba, 71,000 BP Famous Volcanic Eruptions Krakatau, 1883 Pinatubo, 1991 El Chichón, 1982 Agung, 1963 St. Helens, 1980 Major volcanic eruptions of the past 250 years Volcano Year VEI d.v.i/Emax IVI Lakagígar [Laki craters], Iceland 1783 4 2300 0.19 Unknown (El Chichón?) 1809 0.20 Tambora, Sumbawa, Indonesia 1815 7 3000 0.50 Cosiguina, Nicaragua 1835 5 4000 0.11 Askja, Iceland 1875 5 1000 0.01* Krakatau, Indonesia 1883 6 1000 0.12 Okataina [Tarawera], North Island, NZ 1886 5 800 0.04 Santa Maria, Guatemala 1902 6 600 0.05 Ksudach, Kamchatka, Russia 1907 5 500 0.02 Novarupta [Katmai], Alaska, US 1912 6 500 0.15 Agung, Bali, Indonesia 1963 4 800 0.06 Mt. St. Helens, Washington, US 1980 5 500 0.00 El Chichón, Chiapas, Mexico 1982 5 800 0.06 Mt. Pinatubo, Luzon, Philippines 1991 6 1000 — Volcano – Climate Interactions Key to Volcanic Forcing is: SO2 mass loading, eruption duration plume height replenishment aerosol production, residence time 12/8/2017 5 Volcanic Forcing: sulfur dioxide sulfate aerosols SO2 75%H2SO4+ 25%H2O clear sky 1991 Pinatubo aerosols -
Large Igneous Provinces and Mass Extinctions: an Update
Downloaded from specialpapers.gsapubs.org on April 29, 2015 OLD G The Geological Society of America Special Paper 505 2014 OPEN ACCESS Large igneous provinces and mass extinctions: An update David P.G. Bond* Department of Geography, Environment and Earth Science, University of Hull, Hull HU6 7RX, UK, and Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway Paul B. Wignall School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK ABSTRACT The temporal link between mass extinctions and large igneous provinces is well known. Here, we examine this link by focusing on the potential climatic effects of large igneous province eruptions during several extinction crises that show the best correlation with mass volcanism: the Frasnian-Famennian (Late Devonian), Capi- tanian (Middle Permian), end-Permian, end-Triassic, and Toarcian (Early Jurassic) extinctions. It is clear that there is no direct correlation between total volume of lava and extinction magnitude because there is always suffi cient recovery time between individual eruptions to negate any cumulative effect of successive fl ood basalt erup- tions. Instead, the environmental and climatic damage must be attributed to single- pulse gas effusions. It is notable that the best-constrained examples of death-by- volcanism record the main extinction pulse at the onset of (often explosive) volcanism (e.g., the Capitanian, end-Permian, and end-Triassic examples), suggesting that the rapid injection of vast quantities of volcanic gas (CO2 and SO2) is the trigger for a truly major biotic catastrophe. Warming and marine anoxia feature in many extinc- tion scenarios, indicating that the ability of a large igneous province to induce these proximal killers (from CO2 emissions and thermogenic greenhouse gases) is the single most important factor governing its lethality. -
Flood Basalt Hosted Palaeosols: Potential Palaeoclimatic Indicators of Global Climate Change
Geoscience Frontiers xxx (2013) 1e9 Contents lists available at ScienceDirect China University of Geosciences (Beijing) Geoscience Frontiers journal homepage: www.elsevier.com/locate/gsf Review Flood basalt hosted palaeosols: Potential palaeoclimatic indicators of global climate change M.R.G. Sayyed* Department of Geology, Poona College (University of Pune), Camp, Pune 411 001, Maharashtra, India article info abstract Article history: Since continental sediments (in addition to the marine geological record) offer important means of Received 29 December 2012 deciphering environmental changes, the sediments hosted by the successive flows of the continental Received in revised form flood basalt provinces of the world should be treasure houses in gathering the palaeoclimatic data. 27 July 2013 Palaeosols developed on top of basalt flows are potentially ideal for palaeoenvironmental reconstructions Accepted 16 August 2013 because it is easy to determine their protolith geochemistry and also they define a definite time interval. Available online xxx The present paper summarizes the nature of the basalt-hosted palaeosols formed on the flood basalts provinces from different parts of the globe having different ages. Keywords: Ó Continental flood basalts 2013, China University of Geosciences (Beijing) and Peking University. Production and hosting by Palaeosols Elsevier B.V. All rights reserved. Weathering Palaeoclimates Global change 1. Introduction across multiple time and space scales. Such palaeoclimatic records further reveal the changes in the atmospheric chemistry and the Globally distributed climate change events affect oceanic, at- response of natural systems to the climate change as these events mospheric and terrestrial environments and Earth’s history reveals are affecting the global oceanic, atmospheric and terrestrial envi- that there were periods when the climate was significantly cooler ronments. -
Historical Biogeography
click for previous page 10 The Living Marine Resources of the Western Central Atlantic The Caribbean Plate, which occupies a models and methodologies for the explanation of central position in relation to the others, provides a the distributions of organisms. As a result, useful reference point for understanding their descriptive biogeography based on ad hoc interactions and relative motions. There are two delineation of biotic units (e.g., biogeographic fundamentally different kinds of models for its realms, regions or provinces), was generally formation and evolution. Models based on the succeeded by historical biogeography based on hypothesis of in situ origin (e.g., Weyl, 1973; phylogenetic inference and the objective search Meyerhoff and Meyerhoff, 1972; Donnelly, 1989) for areas of endemism. In an independent but suggest that the anomalously thick crust that gives nearly simultaneous development, MacArthur and the plate its identity is the result of a flood basalt event Wilson (1963, 1967) developed the theory of that occurred between the two American continents island biogeography which seeks explanations as they separated in the early Mesozoic, between 200 about the composition of island biotas that are and 165 Ma. In general, these models involve independent of phylogeny and that are of interest movement of South America and Africa (which were a on much shorter time scales. Both of these two single unit at that time) to the east-south-east with trajectories in biogeography - historical and respect to North America. The movements -
I- ('A. Minor Professor
AMERICAN ARTILLERY IN THE MEXICAN WAR 1846-18^7 APPROVEDj Major Profes&ot //I- ('a. Minor Professor of the Department of History / cr*- Dean of the Graduate School AMERICAN ARTILLERY IN THE KEXICAN WAR 18^6-18^7 THESIS Presented, to the Graduate Council of the North Texas State University in Partial Fulfillment of the Requirements For the Degree of MASTER OF ARTS By Lester R. Dillon Jr., B. A. Denton, Texas Kay, 1969 TABLE OF CONTENTS Fage LIST OF TABLES iv LIST OF ILLUSTRATIONS v Chapter I. PRELUDE TO CONFLICT 1 II. CANNON AND CANNONEERS 1^ III. ARMY OF OCCUPATION 33 IV. THE HEARTLAND 60 V. ARTILLERY AND VICTORY 9° APPENDIX 102 BIBLIOGRAPHY 105 lii LIST OF TABLES Table Page 1. Organization of Scott's Army, March 18^7. ... 63 II. Organization of Scott's Army, August 18^7 ... 71 i v LIST OF ILLUSTRATIONS Figure Page 1. Theater of Operations 3 2. Field Cannon 16 3. Cannon Types and. Trajectories 19 Field Cannon and Carriage. , 21 5. Siege Cannon and Carriage . 21 6. Caisson and Limber 2^ 7. Tangent Scale 25 8. Gunner's Quadrant 25 9. Ammunition Types 28 10. Fort Brown to Point Isabel 35 11. Battle of Palo Alto. 38 12. Battle of Eecaca de la Palraa ^3 13. Battle of I-ionterey ^7 1^. Battle of Buena Vista 53 15. Siege of Vera Cruz 61 16. Vera Cruz to Mexico 66 17. Battle of Cerro Gordo . 68 18. Battle of Contreras, 7^ 19. Valley of Mexico 77 20. Kolino del Rey and Chapultepec 80 21. -
Transenergy: Transboundary Geothermal Energy Resources of Slovenia, Austria, Hungary and Slovakia
Issue N° 25 The Newsletter of the ENeRG Network May 2012 Transenergy: transboundary geothermal energy resources of Slovenia, Austria, Hungary and Slovakia The project „TRANSENERGY – which will be available to the public in Transboundary Geothermal Energy 2012. Geological, hydrogeological and Resources of Slovenia, Austria, geothermal modelling is ongoing on a Hungary and Slovakia” is implemented supra-regional scale covering the entire through the Central European Program project area. The geological model and co-financed by ERDF. It’s aim is shows the spatial distribution of the most to provide a user friendly, web-based important hydrostratigraphic units, while decision supporting tool which transfers maps of temperature distribution at various expert know-how of sustainable depths characterize the thermal field. This utilization of geothermal resources serves a basis for more detailed modelling in the western part of the Pannonian to be carried out on selected cross-border basin. pilot areas in 2012 and 2013. TRANSENERGY addresses the key geothermal energy utilization, a database Results can be downloaded from the problem of using geothermal energy of current users and utilization parameters project website (http://transenergy-eu. resources shared by different countries. from 172 users which are visualized geologie.ac. at), which provides further The main carrying medium of geothermal on 12 utilization maps and a summary information and PR material about ongoing energy is thermal groundwater. Regional report discussing the various utilization activities. flow paths are strongly linked to geological aspects, waste water treatment, monitoring Annamária Nádor structures that do not stop at state borders. practices, exploited geothermal aquifers and (project leader) Therefore only a transboundary approach their further potentials. -
Journal of Mormon History Vol. 13, 1986
Journal of Mormon History Volume 13 Issue 1 Article 1 1986 Journal of Mormon History Vol. 13, 1986 Follow this and additional works at: https://digitalcommons.usu.edu/mormonhistory Part of the Religion Commons Recommended Citation (1986) "Journal of Mormon History Vol. 13, 1986," Journal of Mormon History: Vol. 13 : Iss. 1 , Article 1. Available at: https://digitalcommons.usu.edu/mormonhistory/vol13/iss1/1 This Full Issue is brought to you for free and open access by the Journals at DigitalCommons@USU. It has been accepted for inclusion in Journal of Mormon History by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. Journal of Mormon History Vol. 13, 1986 Table of Contents • --Mormon Women, Other Women: Paradoxes and Challenges Anne Firor Scott, 3 • --Strangers in a Strange Land: Heber J. Grant and the Opening of the Japanese Mission Ronald W. Walker, 21 • --Lamanism, Lymanism, and Cornfields Richard E. Bennett, 45 • --Mormon Missionary Wives in Nineteenth Century Polynesia Carol Cornwall Madsen, 61 • --The Federal Bench and Priesthood Authority: The Rise and Fall of John Fitch Kinney's Early Relationship with the Mormons Michael W. Homer, 89 • --The 1903 Dedication of Russia for Missionary Work Kahlile Mehr, 111 • --Between Two Cultures: The Mormon Settlement of Star Valley, Wyoming Dean L.May, 125 Keywords 1986-1987 This full issue is available in Journal of Mormon History: https://digitalcommons.usu.edu/mormonhistory/vol13/iss1/ 1 Journal of Mormon History Editorial Staff LEONARD J. ARRINGTON, Editor LOWELL M. DURHAM, Jr., Assistant Editor ELEANOR KNOWLES, Assistant Editor FRANK McENTIRE, Assistant Editor MARTHA ELIZABETH BRADLEY, Assistant Editor JILL MULVAY DERR, Assistant Editor Board of Editors MARIO DE PILLIS (1988), University of Massachusetts PAUL M. -
Na Tional Register of Historic Places Inventory -- Nomination Form
- . I • Form No 10300 (Rev 10·74) UNITED ~TATES DI:PARTMI:NT O~ THE INTERIOR • FOR NPS USE•ONLY NATIONAL PARK SERVICE NA TIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS TYPE ALL ENTRIES -- COMPLETE APPLICABLE SECTIONS IINAME HISTORIC Bassett Spring ANDIOR COMMON -- ElLOCATION STREET & NUMBER Granite lake Road NOT FOR PUBLICATION CITY TOWN CONGRESSIONAL DISTRICT Four lakes -X VICINITY OF #5 - Honorable Thomas S. Foley STATE COOE COUNTY CODe Washington 53 Spokane 063 DCLASSIFICA TION CATEGORY OWNERSHIP STATUS PRESENT USE _DISTRICT _PUBLIC _OCCUPIED _ -XAGRICULTURE _MUSEUM _BUllDING(SI .!PRIVATE X.UNOCCUPIEO _COMMERCIAL _PARK _STRUCTURE _BOTH _WORK IN PROGRESS _EOUCATIONAl _PRIVATE RESIDENce ~SITE PUBLIC ACQUISITION ACCESSIBLE _ENTERTAINMENT _RELIGIOUS _OBJECT _IN PROCESS _YES RESTRICTED _GOVERNMENT _SCIENTIFIC _BEING CONSIDERED _ YES UNRESTRICTED _INDUSTRIAL _TRANSPORTATION ~NO _MILITARY _OTHER DOWNER OF PROPERTY NAME Mrs. James Owen. Sr. STREET & NUMBER CITY TOWN STATE Four lakes JL VICINITY OF Washington DLOCA TION OF LEGAL DESCRIPTION COURTHOUSE REGISTRY OF DEEDS,ETC Spokane County Courthouse STREET & NUMBER W. 1116 Broadway CITY TOWN STATE Spokane Washington DREPRESENTA TION IN EXISTING SURVEYS TITLE Spokane Metropolitan Area Transportation Study DATE October 1970 _FEDERAL -STATE )LCOUNTY -lOCAL DEPOSITORY FOR SURVEY RECOROS Spokane Ci ty Hall '" CITY TOWN STATE ) .... .:.!SP'-'o:..:.k:.::a.:..:n.::.e .:..:W.::.as:..:h:...;i~n~9.::.to:..:n-'---_ Ii'DESCRIPTION CONDITION • CHECK ONE • CHECK ONE _EXCelLENT _DETERIORATED .xUNALTERED ~ORIGINAL SITE _GOOD _RUINS -ALTERED _MOVED DATE _ .xFAIR _UNEXPOSED DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE The Bassett Spring is a very old, natural up-welling of water in a small valley south of Spokane. -
An Historical Overview of Vancouver Barracks, 1846-1898, with Suggestions for Further Research
Part I, “Our Manifest Destiny Bids Fair for Fulfillment”: An Historical Overview of Vancouver Barracks, 1846-1898, with suggestions for further research Military men and women pose for a group photo at Vancouver Barracks, circa 1880s Photo courtesy of Clark County Museum written by Donna L. Sinclair Center for Columbia River History Funded by The National Park Service, Department of the Interior Final Copy, February 2004 This document is the first in a research partnership between the Center for Columbia River History (CCRH) and the National Park Service (NPS) at Fort Vancouver National Historic Site. The Park Service contracts with CCRH to encourage and support professional historical research, study, lectures and development in higher education programs related to the Fort Vancouver National Historic Site and the Vancouver National Historic Reserve (VNHR). CCRH is a consortium of the Washington State Historical Society, Portland State University, and Washington State University Vancouver. The mission of the Center for Columbia River History is to promote study of the history of the Columbia River Basin. Introduction For more than 150 years, Vancouver Barracks has been a site of strategic importance in the Pacific Northwest. Established in 1849, the post became a supply base for troops, goods, and services to the interior northwest and the western coast. Throughout the latter half of the nineteenth century soldiers from Vancouver were deployed to explore the northwest, build regional transportation and communication systems, respond to Indian-settler conflicts, and control civil and labor unrest. A thriving community developed nearby, deeply connected economically and socially with the military base. From its inception through WWII, Vancouver was a distinctly military place, an integral part of the city’s character. -
Introduction .Of Washington Geographic Names, a Study
NOTES ON EARLY SETTLEMENTS AND ON GEOGRAPHIC NAMES OF EASTERN WASHINGTON Introduction The article which follows is a by-product of several mmor studies in the economic history of eastern Washington. Although not intended as such, it turns out to be, in some respects, an appen dix, or perhaps a series of footnotes, to Professor Meany's Origin . of Washington Geographic Names, a study published serially in this magazine and subsequently brought out as a volume by the Uni versity of Washington Press in 1923. The article contains some names not included in Professor Meany's study, elaborations of a few of his entries, and, in rare instances, slight corrections of his work. To facilitate comparison, frequent references are made to the above-mentioned volume. But the present article is conceived in a different spirit from that of Professor Meany's study. His interest centered in the origins of names; mine has consisted primarily in assembling data relating to early settlements in one area of Washington. Other entries in my article are incidental. By means of the data herein assembled the story of the occupation of the area north of the Snake River in eastern Washington during the seventies and the eighties can be traced in outline, and the principal factors which determined the sites of pioneer towns can be seen in operation. Not the least important of these factors was transportation. During the decade of the seventies the pioneers of eastern Washington were in large measure economically dependent on the Columbia River system. Down the Snake and Columbia rivers was shipped the produce of the "upper country," and up these rivers were transported immi grants and equipment needed for the economic development of the Palouse and Spokane countries.* And to some extent settlers south of the Snake River were dependent on the navigation of that stream.