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1350-5 Geologist
POSITION DESCRIPTION 1. Position Number 2. Explanation (show any positions replaced) 3. Reason for Submission New Redescription Reestablishment Standardized PD Other 4. Service 5. Subject to Identical Addition (IA) Action HQ Field Yes (multiple use) No (single incumbent) 6. Position Specifications 7. Financial Statement Required 10. Position Sensitivity and Risk Designation Subject to Random Drug Testing Yes No Executive Personnel-OGE-278 Non-Sensitive Employment and Financial Interest-OGE-450 Non-Sensitive: Low-Risk Subject to Medical Standards/Surveillance Yes No None required Public Trust Telework Suitable Yes No 8. Miscellaneous 9. Full Performance Level Non-Sensitive: Moderate-Risk Fire Position Yes No Functional Code: -- Pay Plan: Non-Sensitive: High-Risk Law Enforcement Position Yes No BUS: - - Grade: National Security 11. Position is 12. Position Status Noncritical-Sensitive: Moderate-Risk Competitive SES Noncritical-Sensitive: High-Risk 2-Supervisory Excepted (specify in remarks) SL/ST Critical-Sensitive: High-Risk 4-Supervisor (CSRA) 13. Duty Station Special Sensitive: High-Risk 5-Management Official 6-Leader: Type I 14. Employing Office Location 15. Fair Labor Standards Act Exempt Nonexempt 7-Leader: Type II 16. Cybersecurity Code 17. Competitive Area Code: 8-Non-Supervisory #1: #2: - - #3: - - Competitive Level Code: 18. Classified/Graded by Official Title of Position Pay Plan Occupational Code Grade Initial Date a. Department, Bureau, or Office b. Second Level Review -- -- 19. Organizational Title of Position (if different from, or in addition to, official title) 20. Name of Employee (if vacant, specify) 21. Department, Agency, or Establishment c. Third Subdivision U.S. Department of the Interior a. Bureau/First Subdivision d. -
The Paleoecology and Fire History from Crater Lake
THE PALEOECOLOGY AND FIRE HISTORY FROM CRATER LAKE, COLORADO: THE LAST 1000 YEARS By Charles T. Mogen A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Environmental Science and Policy Northern Arizona University August 2018 Approved: R. Scott Anderson, Ph.D., Chair Nicholas P. McKay, Ph.D. Darrell S. Kaufman, Ph.D. Abstract High-resolution pollen, plant macrofossil, charcoal and pyrogenic Polycyclic Aromatic Hydrocarbon (PAH) records were developed from a 154 cm long sediment core collected from Crater Lake (37.39°N, 106.70°W; 3328 m asl), San Juan Mountains, Colorado. Several studies have explored Holocene paleo-vegetation and fire histories from mixed conifer and subalpine bogs and lakes in the San Juan and southern Rocky Mountains utilizing both palynological and charcoal studies, but most have been at relatively low resolution. In addition to presenting the highest resolution palynological study over the last 1000 years from the southern Rocky Mountains, this thesis also presents the first high-resolution pyrogenic PAH and charcoal paired analysis aimed at understanding both long-term fire history and the unresolved relationship between how each of these proxies depict paleofire events. Pollen assemblages, pollen ratios, and paleofire activity, indicated by charcoal and pyrogenic PAH records, were used to infer past climatic conditions. Although the ecosystem surrounding Crater Lake has remained a largely spruce (Picea) dominated forest, the proxies developed in this thesis suggest there were two distinct climate intervals between ~1035 to ~1350 CE and ~1350 to ~1850 CE in the southern Rocky Mountains, associated with the Medieval Climate Anomaly (MCA) and Little Ice Age (LIA) respectively. -
GEOLOGY What Can I Do with This Major?
GEOLOGY What can I do with this major? AREAS EMPLOYERS STRATEGIES Some employment areas follow. Many geolo- gists specialize at the graduate level. ENERGY (Oil, Coal, Gas, Other Energy Sources) Stratigraphy Petroleum industry including oil and gas explora- Geologists working in the area of energy use vari- Sedimentology tion, production, storage and waste disposal ous methods to determine where energy sources are Structural Geology facilities accumulated. They may pursue work tasks including Geophysics Coal industry including mining exploration, grade exploration, well site operations and mudlogging. Geochemistry assessment and waste disposal Seek knowledge in engineering to aid communication, Economic Geology Federal government agencies: as geologists often work closely with engineers. Geomorphology National Labs Coursework in geophysics is also advantageous Paleontology Department of Energy for this field. Fossil Energy Bureau of Land Management Gain experience with computer modeling and Global Hydrogeology Geologic Survey Positioning System (GPS). Both are used to State government locate deposits. Consulting firms Many geologists in this area of expertise work with oil Well services and drilling companies and gas and may work in the geographic areas Oil field machinery and supply companies where deposits are found including offshore sites and in overseas oil-producing countries. This industry is subject to fluctuations, so be prepared to work on a contract basis. Develop excellent writing skills to publish reports and to solicit grants from government, industry and private foundations. Obtain leadership experience through campus organi- zations and work experiences for project man- agement positions. (Geology, Page 2) AREAS EMPLOYERS STRATEGIES ENVIRONMENTAL GEOLOGY Sedimentology Federal government agencies: Geologists in this category may focus on studying, Hydrogeology National Labs protecting and reclaiming the environment. -
East-African Rift System Geological Settings of Geothermal Resources and Their Prospects
Presented at Short Course III on Exploration for Geothermal Resources, organized by UNU-GTP and KenGen, at Lake Naivasha, Kenya, October 24 - November 17, 2008. GEOTHERMAL TRAINING PROGRAMME Kenya Electricity Generating Co., Ltd. EAST-AFRICAN RIFT SYSTEM GEOLOGICAL SETTINGS OF GEOTHERMAL RESOURCES AND THEIR PROSPECTS Kristján Saemundsson ISOR – Iceland GeoSurvey Grensásvegur 9 108 Reykjavík ICELAND [email protected] 1. INTRODUCTION The geothermal areas of the East-African Rift System are not all of the same type. Even though related to the Rift the geological settings are different. Some are volcanic, others are not. Parts of the rift zones are highly volcanic but large segments of them are sediment or lake filled grabens. Extreme cases are also found where rift-related fractures produce permeability in basement rocks. In retrospect it may be useful to point out the differences and likely resource characteristics. Below seven types are described, and in which countries they occur as the dominant type. Three of those types are genuine high-temperature geothermal resources. Two may be accessible only in the off flow zone of high-temperature geothermal fields. One is of the sedimentary basin type resource of low to medium temperature, and one other of the low-temperature type is related to fractured basement rock. 2. OFF RIFT VOLCANOES Eritrea (Alid), Yemen (Al Lisi): Volcanic HT-systems suitable for back pressure turbines Main resource at rather high ground (Eritrea) Off flow probably present, perhaps suitable for binary In case of off flow temperature inversion likely Research methods: Geology/volcanology, hydrology, geochemistry, TEM/MT, airborne magnetics, seismicity, gravity 3. -
Journal of Volcanology and Geothermal Research
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH An International Journal on the Geophysical, Geochemical, Petrological, Economic and Environmental Aspects of Volcanology and Geothermal Research AUTHOR INFORMATION PACK TABLE OF CONTENTS XXX . • Description p.1 • Audience p.1 • Impact Factor p.1 • Abstracting and Indexing p.2 • Editorial Board p.2 • Guide for Authors p.4 ISSN: 0377-0273 DESCRIPTION . An international research journal with focus on volcanic and geothermal processes and their impact on the environment and society. Submission of papers covering the following aspects of volcanology and geothermal research are encouraged: (1) Geological aspects of volcanic systems: volcano stratigraphy, structure and tectonic influence; eruptive history; evolution of volcanic landforms; eruption style and progress; dispersal patterns of lava and ash; analysis of real-time eruption observations. (2) Geochemical and petrological aspects of volcanic rocks: magma genesis and evolution; crystallization; volatile compositions, solubility, and degassing; volcanic petrography and textural analysis. (3) Hydrology, geochemistry and measurement of volcanic and hydrothermal fluids: volcanic gas emissions; fumaroles and springs; crater lakes; hydrothermal mineralization. (4) Geophysical aspects of volcanic systems: physical properties of volcanic rocks and magmas; heat flow studies; volcano seismology, geodesy and remote sensing. (5) Computational modeling and experimental simulation of magmatic and hydrothermal processes: eruption dynamics; magma transport and storage; plume dynamics and ash dispersal; lava flow dynamics; hydrothermal fluid flow; thermodynamics of aqueous fluids and melts. (6) Volcano hazard and risk research: hazard zonation methodology, development of forecasting tools; assessment techniques for vulnerability and impact. The journal does not accept geothermal research papers not related to volcanism. AUDIENCE . Volcanologists, petrologists, geochemists, geothermics. -
A Possible Late Pleistocene Impact Crater in Central North America and Its Relation to the Younger Dryas Stadial
A POSSIBLE LATE PLEISTOCENE IMPACT CRATER IN CENTRAL NORTH AMERICA AND ITS RELATION TO THE YOUNGER DRYAS STADIAL SUBMITTED TO THE FACULTY OF THE UNIVERSITY OF MINNESOTA BY David Tovar Rodriguez IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE Howard Mooers, Advisor August 2020 2020 David Tovar All Rights Reserved ACKNOWLEDGEMENTS I would like to thank my advisor Dr. Howard Mooers for his permanent support, my family, and my friends. i Abstract The causes that started the Younger Dryas (YD) event remain hotly debated. Studies indicate that the drainage of Lake Agassiz into the North Atlantic Ocean and south through the Mississippi River caused a considerable change in oceanic thermal currents, thus producing a decrease in global temperature. Other studies indicate that perhaps the impact of an extraterrestrial body (asteroid fragment) could have impacted the Earth 12.9 ky BP ago, triggering a series of events that caused global temperature drop. The presence of high concentrations of iridium, charcoal, fullerenes, and molten glass, considered by-products of extraterrestrial impacts, have been reported in sediments of the same age; however, there is no impact structure identified so far. In this work, the Roseau structure's geomorphological features are analyzed in detail to determine if impacted layers with plastic deformation located between hard rocks and a thin layer of water might explain the particular shape of the studied structure. Geophysical data of the study area do not show gravimetric anomalies related to a possible impact structure. One hypothesis developed on this works is related to the structure's shape might be explained by atmospheric explosions dynamics due to the disintegration of material when it comes into contact with the atmosphere. -
19660003720.Pdf
Copy No. LUNAR NAVIGATION STUDY FINAL REPORT (June 1964 to May 1965) SUMMARY VOLUME BSR 1134 June 1965 Prepared for: George C. Marshall Space Flight Center Huntsville, Alabama under Contract No. NAS8- 11292 Authors : L. J. Abbeduto W.G. Green M. E. Amdursky T. F. King D.K. Breseke R.B. Odden J. T. Broadbent P.I. Pressel R. A. Gill T.T. Trexler H. C. Graboske C. Waite BENDIX SYSTEMS DIVISION OF THE BENDIX CORPORATION Ann Arbor, Michigan CONTENTS Page 1. INTRODUCTION 1 2. STUDY APPROACH 1 3. DEFINITIONS OF TYPICAL MISSIONS 2 4. NAVIGATION SYSTEM CONCEPTS 4 5. NAVIGATION TECHNIQUE SURVEY 4 5. 1 POSITION FIX 4 5.2 DEAD RECKONING 9 5.3 PILOTING 10 6. TYPICAL NAVIGATION REQUIREMENTS 11 7. NAVIGATION COMPONENT SURVEY 14 8. LUNAR PHYSICAL AND MISSION PARAMETERS 15 9. ERROR MODELS 18 10. POSITION FIX ERROR MODEL 19 11. INITIAL AZIMUTH ERROR MODEL 22 12. DEAD-RECKONING ERROR MODEL 23 13. ERROR MODEL DIAGRAM - CONCEPT 1 29 14. ERROR MODEL DIAGRAM - CONCEPT 2 29 15. ERROR MODEL DIAGRAM - CONCEPT 3 32 16. SUMMARY OF RESULTS 38 17. CONCLUSIONS AND RECOMMENDATIONS 36 ii ILLUSTRATIONS Figure Title Page 1 Block Diagram of Study Approach 2 2 Passive, Nongyro System Block Diagram 5 3 Inertial System Block Diagram 6 4 RF Technology System Block Diagram 7 5 Vehicle Position Error Ellipsoid 19 6 Astronomical Triangle 22 7 Star Azimuth Definition 23 8 Path Density Functions 24 9 Vehicle Path, Latitude and Longitude 26 10 Altitude vs Distance Traveled 27 11 System Error vs Time 28 12 Concept 1- Passive, Nongyro System Flow Diagram 30 13 Concept 2 - Inertial System -
Global History and the Present Time
Global History and the Present Time Wolf Schäfer There are three times: a present time of past things; a present time of present things; and a present time of future things. St. Augustine1 It makes sense to think that the present time is the container of past, present, and future things. Of course, the three branches of the present time are heavily inter- twined. Let me illustrate this with the following story. A few journalists, their minds wrapped around present things, report the clash of some politicians who are taking opposite sides in a struggle about future things. The politicians argue from histori- cal precedent, which was provided by historians. The historians have written about past things in a number of different ways. This gets out into the evening news and thus into the minds of people who are now beginning to discuss past, present, and future things. The people’s discussion returns as feedback to the journalists, politi- cians, and historians, which starts the next round and adds more twists to the en- tangled branches of the present time. I conclude that our (hi)story has no real exit doors into “the past” or “the future” but a great many mirror windows in each hu- man mind reflecting spectra of actual pasts and potential futures, all imagined in the present time. The complexity of the present (any given present) is such that no- body can hope to set the historical present straight for everybody. Yet this does not mean that a scientific exploration of history is impossible. History has a proven and robust scientific method. -
Chronology of Old Testament a Return to Basics
Chronology of the Old Testament: A Return to the Basics By FLOYD NOLEN JONES, Th.D., Ph.D. 2002 15th Edition Revised and Enlarged with Extended Appendix (First Edition 1993) KingsWord Press P. O. Box 130220 The Woodlands, Texas 77393-0220 Chronology of the Old Testament: A Return to the Basics Ó Copyright 1993 – 2002 · Floyd Nolen Jones. Floyd Jones Ministries, Inc. All Rights Reserved. This book may be freely reproduced in any form as long as it is not distributed for any material gain or profit; however, this book may not be published without written permission. ISBN 0-9700328-3-8 ii ACKNOWLEDGMENTS ... I am gratefully indebted to Dr. Alfred Cawston (d. 3/21/91), founder of two Bible Colleges in India and former Dean and past President of Continental Bible College in Brussels, Belgium, and Jack Park, former President and teacher at Sterling Bible Institute in Kansas, now serving as a minister of the gospel of the Lord Jesus Christ and President of Jesus' Missions Society in Huntsville, Texas. These Bible scholars painstakingly reviewed every Scripture reference and decision in the preparation of the Biblical time charts herewith submitted. My thanks also to: Mark Handley who entered the material into a CAD program giving us computer storage and retrieval capabilities, Paul Raybern and Barry Adkins for placing their vast computer skills at my every beckoning, my daughter Jennifer for her exhausting efforts – especially on the index, Julie Gates who tirelessly assisted and proofed most of the data, words fail – the Lord Himself shall bless and reward her for her kindness, competence and patience, and especially to my wife Shirley who for two years prior to the purchase of a drafting table put up with a dining room table constantly covered with charts and who lovingly understood my preoccupation with this project. -
SCIENCE CITATION INDEX EXPANDED - JOURNAL LIST Total Journals: 8631
SCIENCE CITATION INDEX EXPANDED - JOURNAL LIST Total journals: 8631 1. 4OR-A QUARTERLY JOURNAL OF OPERATIONS RESEARCH 2. AAPG BULLETIN 3. AAPS JOURNAL 4. AAPS PHARMSCITECH 5. AATCC REVIEW 6. ABDOMINAL IMAGING 7. ABHANDLUNGEN AUS DEM MATHEMATISCHEN SEMINAR DER UNIVERSITAT HAMBURG 8. ABSTRACT AND APPLIED ANALYSIS 9. ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY 10. ACADEMIC EMERGENCY MEDICINE 11. ACADEMIC MEDICINE 12. ACADEMIC PEDIATRICS 13. ACADEMIC RADIOLOGY 14. ACCOUNTABILITY IN RESEARCH-POLICIES AND QUALITY ASSURANCE 15. ACCOUNTS OF CHEMICAL RESEARCH 16. ACCREDITATION AND QUALITY ASSURANCE 17. ACI MATERIALS JOURNAL 18. ACI STRUCTURAL JOURNAL 19. ACM COMPUTING SURVEYS 20. ACM JOURNAL ON EMERGING TECHNOLOGIES IN COMPUTING SYSTEMS 21. ACM SIGCOMM COMPUTER COMMUNICATION REVIEW 22. ACM SIGPLAN NOTICES 23. ACM TRANSACTIONS ON ALGORITHMS 24. ACM TRANSACTIONS ON APPLIED PERCEPTION 25. ACM TRANSACTIONS ON ARCHITECTURE AND CODE OPTIMIZATION 26. ACM TRANSACTIONS ON AUTONOMOUS AND ADAPTIVE SYSTEMS 27. ACM TRANSACTIONS ON COMPUTATIONAL LOGIC 28. ACM TRANSACTIONS ON COMPUTER SYSTEMS 29. ACM TRANSACTIONS ON COMPUTER-HUMAN INTERACTION 30. ACM TRANSACTIONS ON DATABASE SYSTEMS 31. ACM TRANSACTIONS ON DESIGN AUTOMATION OF ELECTRONIC SYSTEMS 32. ACM TRANSACTIONS ON EMBEDDED COMPUTING SYSTEMS 33. ACM TRANSACTIONS ON GRAPHICS 34. ACM TRANSACTIONS ON INFORMATION AND SYSTEM SECURITY 35. ACM TRANSACTIONS ON INFORMATION SYSTEMS 36. ACM TRANSACTIONS ON INTELLIGENT SYSTEMS AND TECHNOLOGY 37. ACM TRANSACTIONS ON INTERNET TECHNOLOGY 38. ACM TRANSACTIONS ON KNOWLEDGE DISCOVERY FROM DATA 39. ACM TRANSACTIONS ON MATHEMATICAL SOFTWARE 40. ACM TRANSACTIONS ON MODELING AND COMPUTER SIMULATION 41. ACM TRANSACTIONS ON MULTIMEDIA COMPUTING COMMUNICATIONS AND APPLICATIONS 42. ACM TRANSACTIONS ON PROGRAMMING LANGUAGES AND SYSTEMS 43. ACM TRANSACTIONS ON RECONFIGURABLE TECHNOLOGY AND SYSTEMS 44. -
Climatic Variability in Western Victoria
DROUGHTS AND FLOODING RAINS: A FINE-RESOLUTION RECONSTRUCTION OF CLIMATIC VARIABILITY IN WESTERN VICTORIA, AUSTRALIA, OVER THE LAST 1500 YEARS. CAMERON BARR Thesis submitted for the degree of Doctor of Philosophy, Discipline of Geographical and Environmental Studies, University of Adelaide, Australia. 2010 CHAPTER 1 – INTRODUCTION 1.1 Introduction This thesis presents the results of a study examining the short-term (approximately 1500 year) history of climatic change from the south-eastern Australian mainland. In order to achieve this, fossil diatom assemblages from sediment cores retrieved from two crater lakes in western Victoria are examined in fine resolution and interpreted through the application of a diatom-conductivity transfer function developed specifically for use in low salinity lake systems. 1.2 Research context In early November 2006, the then Prime Minister of Australia, John Howard, called an emergency ‘water summit’ with the premiers of the south-eastern states to discuss the impact of the prevailing drought on water availability in the Murray Darling Basin, a key agricultural region for the nation. At this meeting, the attendees were informed that the drought that was afflicting the region was “the worst in 1000 years” (Shanahan and Warren, 2006). This claim proved so startling that it was widely disseminated through the local and national media and was even reported as far away as the United Kingdom (Vidal, 2006). The Prime Minister, however, remained unconvinced of the veracity of the claim because “there are no records [to verify it against]” (Shanahan and Warren, 2006). This brief exchange between the Nation’s leaders and the press highlights the problems faced by water, agricultural, environmental and social planners in Australia. -
Formal Ratification of the Subdivision of the Holocene Series/ Epoch
Article 1 by Mike Walker1*, Martin J. Head 2, Max Berkelhammer3, Svante Björck4, Hai Cheng5, Les Cwynar6, David Fisher7, Vasilios Gkinis8, Antony Long9, John Lowe10, Rewi Newnham11, Sune Olander Rasmussen8, and Harvey Weiss12 Formal ratification of the subdivision of the Holocene Series/ Epoch (Quaternary System/Period): two new Global Boundary Stratotype Sections and Points (GSSPs) and three new stages/ subseries 1 School of Archaeology, History and Anthropology, Trinity Saint David, University of Wales, Lampeter, Wales SA48 7EJ, UK; Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, Wales SY23 3DB, UK; *Corresponding author, E-mail: [email protected] 2 Department of Earth Sciences, Brock University, 1812 Sir Isaac Brock Way, St. Catharines, Ontario LS2 3A1, Canada 3 Department of Earth and Environmental Sciences, University of Illinois, Chicago, Illinois 60607, USA 4 GeoBiosphere Science Centre, Quaternary Sciences, Lund University, Sölveg 12, SE-22362, Lund, Sweden 5 Institute of Global Change, Xi’an Jiaotong University, Xian, Shaanxi 710049, China; Department of Earth Sciences, University of Minne- sota, Minneapolis, MN 55455, USA 6 Department of Biology, University of New Brunswick, Fredericton, New Brunswick E3B 5A3, Canada 7 Department of Earth Sciences, University of Ottawa, Ottawa K1N 615, Canada 8 Centre for Ice and Climate, The Niels Bohr Institute, University of Copenhagen, Julian Maries Vej 30, DK-2100, Copenhagen, Denmark 9 Department of Geography, Durham University, Durham DH1 3LE, UK 10