How the Continents Deform: the Evidence from Tectonic Geodesy*
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Student Handbook
A Handbook for Geology Students 1 Contents Why study Geology? ............................................................................................. 3 Job Prospects and Salaries .................................................................................. 7 Why Appalachian Geology? ................................................................................ 10 Geology Faculty and Staff ................................................................................... 13 Financial Support in the Department ................................................................... 23 Geology Department Awards and Honors .......................................................... 26 Opportunities and Requirements ........................................................................ 28 Degree Programs in Geology ............................................................................. 35 Geology Courses ................................................................................................ 44 Field Camp ......................................................................................................... 51 2 Why study Geology? Geology is the multi-disciplinary science that studies the earth and its history. We live on a dynamic planet that is constantly changing. Our ability to survive as a civilization and as a species is intricately linked to the geologic processes that shape our earth, form its natural resources and allow it to recover from the abuse that our society heaps upon it. Geology is important because -
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
Geological Sciences 1
Geological Sciences 1 GEOLOGICAL SCIENCES Certificates • Geophysics - Graduate Certificate (catalog.colorado.edu/graduate/ With one of the most successful graduate programs in the nation, colleges-schools/arts-sciences/programs-study/geological-sciences/ the Department of Geological Sciences has enjoyed a reputation of geophysics-graduate-certificate/) excellence for more than 100 years. Our doctoral program is ranked • Hydrologic Sciences - Graduate Certificate (catalog.colorado.edu/ among the top 10 percent of U.S. geology programs by the National graduate/colleges-schools/arts-sciences/programs-study/geological- Research Council, and CU Boulder is ranked as one of the top two sciences/hydrologic-sciences-graduate-certificate/) universities in the world for geosciences by U.S. News and World Report. Graduate students have an opportunity to work with over 35 tenured Faculty and tenure-track faculty who support a wide range of interdisciplinary While many faculty teach both undergraduate and graduate students, research programs in such areas as: cosmochemistry and planetary some instruct students at the undergraduate level only. For more geology; Earth science education; economic and energy resources; information, contact the faculty member's home department. geobiology and astrobiology; geochemistry; geochronology and Abbott, Lon D. (https://experts.colorado.edu/display/fisid_145044/) thermochronology; geodynamics, geophysics, and remote sensing; Senior Instructor; PhD, University of California, Santa Cruz geomorphology and cryosphere; global change; hydrology; natural hazards; paleoclimate and paleoceanography; paleontology and Anderson, Robert S. (https://experts.colorado.edu/display/fisid_130117/) paleobiology; petrology and mineralogy; sedimentology and stratigraphy; Distinguished Professor; PhD, University of Washington and structure and tectonics. Arthurs, Leilani A. (https://experts.colorado.edu/display/fisid_145087/) The graduate degrees offered include Master of Science (MS) and Doctor Assistant Professor; PhD, University of Notre Dame of Philosophy (PhD). -
Geomicrobiological Processes in Extreme Environments: a Review
202 Articles by Hailiang Dong1, 2 and Bingsong Yu1,3 Geomicrobiological processes in extreme environments: A review 1 Geomicrobiology Laboratory, China University of Geosciences, Beijing, 100083, China. 2 Department of Geology, Miami University, Oxford, OH, 45056, USA. Email: [email protected] 3 School of Earth Sciences, China University of Geosciences, Beijing, 100083, China. The last decade has seen an extraordinary growth of and Mancinelli, 2001). These unique conditions have selected Geomicrobiology. Microorganisms have been studied in unique microorganisms and novel metabolic functions. Readers are directed to recent review papers (Kieft and Phelps, 1997; Pedersen, numerous extreme environments on Earth, ranging from 1997; Krumholz, 2000; Pedersen, 2000; Rothschild and crystalline rocks from the deep subsurface, ancient Mancinelli, 2001; Amend and Teske, 2005; Fredrickson and Balk- sedimentary rocks and hypersaline lakes, to dry deserts will, 2006). A recent study suggests the importance of pressure in the origination of life and biomolecules (Sharma et al., 2002). In and deep-ocean hydrothermal vent systems. In light of this short review and in light of some most recent developments, this recent progress, we review several currently active we focus on two specific aspects: novel metabolic functions and research frontiers: deep continental subsurface micro- energy sources. biology, microbial ecology in saline lakes, microbial Some metabolic functions of continental subsurface formation of dolomite, geomicrobiology in dry deserts, microorganisms fossil DNA and its use in recovery of paleoenviron- Because of the unique geochemical, hydrological, and geological mental conditions, and geomicrobiology of oceans. conditions of the deep subsurface, microorganisms from these envi- Throughout this article we emphasize geomicrobiological ronments are different from surface organisms in their metabolic processes in these extreme environments. -
The Central Asia Collision Zone: Numerical Modelling of the Lithospheric Structure and the Present-Day Kinematics
Th e Central Asia collision zone: numerical modelling of the lithospheric structure and the present - day kinematics Lavinia Tunini A questa tesi doctoral està subjecta a l a llicència Reconeixement - NoComercial – SenseObraDerivada 3.0. Espanya de Creative Commons . Esta tesis doctoral está sujeta a la licencia Reconocimiento - NoComercial – SinObraDerivada 3.0. España de Creative Commons . Th is doctoral thesis is license d under the Creative Commons Attribution - NonCommercial - NoDerivs 3.0. Spain License . The Central Asia collision zone: numerical modelling of the lithospheric structure and the present-day kinematics Ph.D. thesis presented at the Faculty of Geology of the University of Barcelona to obtain the Degree of Doctor in Earth Sciences Ph.D. student: Lavinia Tunini 1 Supervisors: Tutor: Dra. Ivone Jiménez-Munt 1 Prof. Dr. Juan José Ledo Fernández 2 Prof. Dr. Manel Fernàndez Ortiga 1 1 Institute of Earth Sciences Jaume Almera 2 Department of Geodynamics and Geophysics of the University of Barcelona This thesis has been prepared at the Institute of Earth Sciences Jaume Almera Consejo Superior de Investigaciones Científicas (CSIC) March 2015 Alla mia famiglia La natura non ha fretta, eppure tutto si realizza. – Lao Tzu Agradecimientos En mano tenéis un trabajo de casi 4 años, 173 páginas que no hubieran podido salir a luz sin el apoyo de quienes me han ayudado durante este camino, permitiendo acabar la Tesis antes que la Tesis acabase conmigo. En primer lugar quiero agradecer mis directores de tesis, Ivone Jiménez-Munt y Manel Fernàndez. Gracias por haberme dado la oportunidad de entrar en el proyecto ATIZA, de aprender de la modelización numérica, de participar a múltiples congresos y presentaciones, y, mientras, compartir unas cervezas. -
Geodetic Position Computations
GEODETIC POSITION COMPUTATIONS E. J. KRAKIWSKY D. B. THOMSON February 1974 TECHNICALLECTURE NOTES REPORT NO.NO. 21739 PREFACE In order to make our extensive series of lecture notes more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. GEODETIC POSITION COMPUTATIONS E.J. Krakiwsky D.B. Thomson Department of Geodesy and Geomatics Engineering University of New Brunswick P.O. Box 4400 Fredericton. N .B. Canada E3B5A3 February 197 4 Latest Reprinting December 1995 PREFACE The purpose of these notes is to give the theory and use of some methods of computing the geodetic positions of points on a reference ellipsoid and on the terrain. Justification for the first three sections o{ these lecture notes, which are concerned with the classical problem of "cCDputation of geodetic positions on the surface of an ellipsoid" is not easy to come by. It can onl.y be stated that the attempt has been to produce a self contained package , cont8.i.ning the complete development of same representative methods that exist in the literature. The last section is an introduction to three dimensional computation methods , and is offered as an alternative to the classical approach. Several problems, and their respective solutions, are presented. The approach t~en herein is to perform complete derivations, thus stqing awrq f'rcm the practice of giving a list of for11111lae to use in the solution of' a problem. -
MICR 423: Geomicrobiology Fall 2018 3 Credit Hours
MICR 423: Geomicrobiology Fall 2018 3 Credit Hours Course description. This course will focus on the role that microorganisms play in fundamental geological processes. Topics will include an outline of the present understanding of microbial involvement of weathering of rocks, formation and transformation of soils and sediments, genesis and degradation of minerals. Elemental cycles will also be covered with emphasis on the interrelationships between the various geochemical cycles and the microbial trophic groups involved. Prerequisite: MICR 301 and Chemistry 210 and 21l. Recommended: GEOL 220, 221 or 222. Lecture. Life Science II, Room 430, 9:35 – 10:50 Tues and Thurs Course Goals. At the end of this course you will be able to: • Intelligently converse with microbiologists, geologists, environmental scientists and engineers about the role microorganisms play in the cycling of elements • Be familiar with a variety of techniques to identify and characterize microorganisms in any environment • Relate microbial physiology, genetics, cell structure, and metabolism to the effect, role, or signature that microbes imprint on their surroundings Instructor Office Office Hours Dr. Scott Hamilton-Brehm Life Science III, Rm 1009 M 10-12 pm or by 453-3818 appointment [email protected] Strongly suggested textbooks: • BROCK BIOLOGY OF MICROORGANISMS, 15th edition, 2017, Michael T. Madigan, Kelly S. Bender, Daniel H. Buckley, Matthew W. Sattley, and David A. Stahl (Benjamin Cummings/Pearson). • Hall BG. Phylogenetic trees made easy: a how-to manual. 2008. Final Course Grading scale Grade Points Percentage A 900 - 1000 90-100% B 800 - 899 80-89% C 700 - 799 70-79% D 600 - 699 60-69% F 0 - 599 0-59% Lecture Grades. -
GPS and the Search for Axions
GPS and the Search for Axions A. Nicolaidis1 Theoretical Physics Department Aristotle University of Thessaloniki, Greece Abstract: GPS, an excellent tool for geodesy, may serve also particle physics. In the presence of Earth’s magnetic field, a GPS photon may be transformed into an axion. The proposed experimental setup involves the transmission of a GPS signal from a satellite to another satellite, both in low orbit around the Earth. To increase the accuracy of the experiment, we evaluate the influence of Earth’s gravitational field on the whole quantum phenomenon. There is a significant advantage in our proposal. While the geomagnetic field B is low, the magnetized length L is very large, resulting into a scale (BL)2 orders of magnitude higher than existing or proposed reaches. The transformation of the GPS photons into axion particles will result in a dimming of the photons and even to a “light shining through the Earth” phenomenon. 1 Email: [email protected] 1 Introduction Quantum Chromodynamics (QCD) describes the strong interactions among quarks and gluons and offers definite predictions at the high energy-perturbative domain. At low energies the non-linear nature of the theory introduces a non-trivial vacuum which violates the CP symmetry. The CP violating term is parameterized by θ and experimental bounds indicate that θ ≤ 10–10. The smallness of θ is known as the strong CP problem. An elegant solution has been offered by Peccei – Quinn [1]. A global U(1)PQ symmetry is introduced, the spontaneous breaking of which provides the cancellation of the θ – term. As a byproduct, we obtain the axion field, the Nambu-Goldstone boson of the broken U(1)PQ symmetry. -
Need for Seismic Hydrology Research with a Geomicrobiological Focus
sustainability Communication Need for Seismic Hydrology Research with a Geomicrobiological Focus Heejung Kim Department of Geology, Kangwon National University, Chuncheon 24341, Korea; [email protected] Abstract: Earthquakes cause deformation in previously stable groundwater environments, resulting in changes to the hydrogeological characteristics. The changes to hydrological processes follow- ing large-scale earthquakes have been investigated through many physicochemical studies, but understanding of the associated geomicrobiological responses remains limited. To complement the understanding of earthquakes gathered using hydrogeochemical approaches, studies on the effects of the Earth’s deep crustal fluids on microbial community structures can be applied. These studies could help establish the degree of resilience and sustainability of the underground ecosystem following an earthquake. Furthermore, investigations on changes in the microbial community structure of the Earth’s deep crustal fluids before and after an earthquake can be used to predict an earthquake. The results derived from studies that merge hydrogeochemical and geomicrobiological changes in the deep crustal fluids due to the effect of stress on rock characteristics within a fault zone can be used to correlate these factors with earthquake occurrences. In addition, an earthquake risk evaluation method may be developed based on the observable characteristics of fault-zone aquifers. Keywords: earthquake; seismic hydrology; groundwater; hydrogeochemistry; geomicrobiology Citation: Kim, H. Need for Seismic Many studies on the reaction of the Earth’s deep crustal fluids before and after earth- Hydrology Research with a quakes have been conducted worldwide, including in countries with a high frequency Geomicrobiological Focus. of earthquakes. Seismic hydrology is the study of earthquake prediction by analyzing Sustainability 2021, 13, 8704. -
Area of Study
DEPARTMENT OF EARTHDEPARTMENT SCIENCES OF THE GRADUATE SCHOOL | MONTANA STATE UNIVERSITY AreaEarth ofSciences Study DEGREES OFFERED • M.S. in Earth Sciences FirstThe Departmentgraph of Earth Sciences at Montana State University has a faculty of 13 earth • Ph.D. in Earth Sciences scientists, geologists and geographers. The Master of Science and Doctor of Philosophy in Earth • Ph.D. in Ecology and TextSciences programs have around 45 active graduate students and stress independent thesis Environmental Science research with some supporting course work. Faculty expertise and research in the department spans a large majority of the subfields of Earth Sciences. Our geography faculty includes specialties from settlement geography to bioclimatology, from international urban geography to GIS to snow science. The interests of our geology faculty range from petrogenesis to paleobiology to structural geology, and from dinosaur taphonomy and stratigraphy to geomorphology. Our geobiology faculty have research interests in vertebrate paleontology, paleoecology, biogeography, paleoclimatology and geomicrobiology. Program strengths are in basin analysis and energy resources, dinosaur paleontology, geography of the northern Rocky Mountains, architecture and composition of the lithosphere, snow science and cryospheric processes, and climate change. ADMISSION Applicants should a GPA of 3.0 or higher, GRE scores better than the 50th percentile and a strong academic background in Earth Sciences (geography, geology or geobiology). Foreign students must have a TOEFL score better than 550 for the paper test and 231 for the computer test. The department does not accept general applicants to our graduate program. An applicant should identify a major advisor from the list of faculty, contact that individual, and Department Address: determine whether there is space available in that advisor’s program. -
Geomicrobiology: Interactions Between Microbes and Minerals, Comes at a Very Opportune Time
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Hemeroteca Cientifica Catalana INTERNATL MICROBIOL (1998) 1:241–242 241 © Springer-Verlag Ibérica 1998 BOOK REVIEWS a few chapters are devoid of typographical mistakes which Geomicrobiology: Interactions between in some case have resulted in factual errors. Nealson and Microbes and Minerals Stahl state that freshwater environments typically contain JILLIAN F. BANFIELD, KENNETH H. NEALSON (eds) 100 to 250 mM of sulfate while marine systems contain 1997. Mineralogical Society of America, Washington, DC. micromolar amounts (just the opposite is true). Bazylinski (Series: Reviews in Mineralogy, vol. 35) and Moskowitz have inadvertently created a new subgroup 448 pp. Paperback, $32. of Proteobacteria. The volume I received also included an ISBN 0-93995045-6 insert correcting a figure in chapter 11, earlier versions did not. Suffice it to say reediting would greatly enhance the The recent controversy over nanofossils in a Martian utility of this text. Despite its shortcomings, it is a good meteorite and reports of bacteria growing in basalt have once primer for the novice and an important volume for the again brought the study of geomicrobiology into the seasoned veteran. headlines. Thus, Geomicrobiology: Interactions Between Microbes and Minerals, comes at a very opportune time. The book, a byproduct of a short course of the same title hosted John F. Stolz by the Mineralogical Society of America last fall, provides Duquesne University, Pittsburgh, Pennsylvania an in depth look at a fascinating subject. Containing 13 chapters it begins with a review for non-specialists on microorganisms and biogeochemical cycles and concludes with the evolution of the carbon cycle. -
Coordinate Systems in Geodesy
COORDINATE SYSTEMS IN GEODESY E. J. KRAKIWSKY D. E. WELLS May 1971 TECHNICALLECTURE NOTES REPORT NO.NO. 21716 COORDINATE SYSTElVIS IN GEODESY E.J. Krakiwsky D.E. \Vells Department of Geodesy and Geomatics Engineering University of New Brunswick P.O. Box 4400 Fredericton, N .B. Canada E3B 5A3 May 1971 Latest Reprinting January 1998 PREFACE In order to make our extensive series of lecture notes more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. TABLE OF CONTENTS page LIST OF ILLUSTRATIONS iv LIST OF TABLES . vi l. INTRODUCTION l 1.1 Poles~ Planes and -~es 4 1.2 Universal and Sidereal Time 6 1.3 Coordinate Systems in Geodesy . 7 2. TERRESTRIAL COORDINATE SYSTEMS 9 2.1 Terrestrial Geocentric Systems • . 9 2.1.1 Polar Motion and Irregular Rotation of the Earth • . • • . • • • • . 10 2.1.2 Average and Instantaneous Terrestrial Systems • 12 2.1. 3 Geodetic Systems • • • • • • • • • • . 1 17 2.2 Relationship between Cartesian and Curvilinear Coordinates • • • • • • • . • • 19 2.2.1 Cartesian and Curvilinear Coordinates of a Point on the Reference Ellipsoid • • • • • 19 2.2.2 The Position Vector in Terms of the Geodetic Latitude • • • • • • • • • • • • • • • • • • • 22 2.2.3 Th~ Position Vector in Terms of the Geocentric and Reduced Latitudes . • • • • • • • • • • • 27 2.2.4 Relationships between Geodetic, Geocentric and Reduced Latitudes • . • • • • • • • • • • 28 2.2.5 The Position Vector of a Point Above the Reference Ellipsoid . • • . • • • • • • . .• 28 2.2.6 Transformation from Average Terrestrial Cartesian to Geodetic Coordinates • 31 2.3 Geodetic Datums 33 2.3.1 Datum Position Parameters .