35Th IGC - It’S Over
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1991 ADMINISTRATION BOARD of DIRECTORS President Dr
FEB 91 THE GEOLOGICAL NEWSLETTER I GEOLOGICAL SOCIETY OF THE OREGON COUNTRY I .. GEOLOGICAL SOCIETY Non-Profit Org. OF THE OREGON COUNTRY U.S. POSTAGE P.O. BOX 907 PAID Portland, Oregon PORTLAND, OR 97207 Permit No. 999 \ 1Ett£ 13" .\. J!l CIJ" \ \. GEOLOGICAL SOCIETY OF THE OREGON COUNTRY 1990-1991 ADMINISTRATION BOARD OF DIRECTORS President Dr. Ruth Keen 222-1430 Directors 4138 SW 4th Ave Donald Barr (3 years) 246-2785 Portland, OR 97201 Peter E. Baer (2 years) 661-7995 Vice President Charlene Holzwarth (1 year) 284-3444 Dr. Walter Sunderland 625-6840 Immediate Past Presidents 7610 NE Earlwood Rd. Rosemary Kenney 221-0757 Newberg, OR 97132. Joline Robustelli 223-2852 Secretary Cecelia Crater 235-5158 THE GEOLOGICAL NEWSLETTER 3823 SE lOth Editor: Sandra Anderson 775-5538 Portland, OR 97202 Calendar: Joline Robustelli 223-2852 Treasurer Business Mgr. Joline Robustelli 223-2852 Archie Strong 244-1488 Assist: Cecelia Crater 235-5158 6923 SW 2nd Ave Portland, OR 97219 ACTIVITIES CHAIRS Calligrapher Properties and PA System .. Wallace R. McClung 637-3834 (Luncheon) Donald Botteron 245-6251 Field Trips (Evening) Walter A. Sunderland 625-6840 Alta B. Fosback 641-6323 Publications Charlene Holzwarth 284-3444 Margaret Steere 246-1670 Geology Seminars Publicity Margaret Steere 246-1670 Roberta L. Walter 235 -3579 Historian Refreshments Phyllis G. Bonebrake 289-8597 (Friday Evening) Hospitality Donald and Betty Turner 246-3192 (Luncheon) Margaret Fink 289-0188 (Geology Seminars) (Evening) Gale Rankin and Freda and Virgil Scott 771-3646 Manuel Boyes 223-6784 Telephone Library: Frances Rusche 6_54-5975 Cecelia Crater 235-5158 Esther Kennedy -287-3091 Volunteer Speakers Bureau Lois Sato 654-7671 Robert Richmond 282-3817 Past Presidents Panel Annual Banquet Rosemary Kenney 221-0757 Esther Kennedy 287-3091 Programs Gale Rankin 223-6784 (Luncheon) Helen E. -
Read and Understand These Archi- Ves
IAS Newsletter 203 April 2006 SUPER SEDIMENTOLOGICAL EXPOSURES The extensional Corinth-Patras basin evolution from Pliocene to present and the different coarse-grained fan-delta types along Corinth sub-basin Introduction to 30 km and 20 km wide, respectively) due to a NE-trending rifted sub-basin (Rion sub-basin, 15 The Corinth–Patras basin is a late km long and up to 3 km wide; Fig. Pliocene to Quaternary WNW 1B). Both sub-basins (Corinth and trending extensional basin that Patras) show high rates of subsidence extends for 130km across the Greek along the southern, more active mainland. It formed by late Cenozoic margins. Changes in predominant back-arc extension behind the stress directions at this time led to Hellenic trench (Fig. 1A; Zelilidis, the Rion sub-basin acting as a transfer 2000). During the Pliocene, zone between the extending Patras extension formed the Corinth– and Corinth sub-basins. Due to the Patras basin, and the resulting WNW- above-mentioned different fault directed basin was relatively uniform trends in the area of the Rion sub- in width and depth along its axis (Fig. basin, the Corinth–Patras basin 1B). locally became very narrow and The Corinth–Patras basin was shallow, forming the Rion Strait separated into two WNW-trending which influences sedimentological sub-basins (Corinth and Patras sub- evolution of the whole basin (Figs 2 basins, 90 km and 30 km long and up and 3). 3 IAS Newsletter 203 April 2006 Figure 1. (A) Sketch map of Greece: black area indicates the studied area (shown in B and C). -
Development Team
Paper No. : 03 Archaeological Anthropology Module : 24 Geological Time Scale Development Team Principal Investigator Prof. Anup Kumar Kapoor Department of Anthropology, University of Delhi Paper Coordinator Dr. Manoj Kumar Singh Department of Anthropology, University of Delhi Prof. Mani Babu, Content Writer Department of Anthropology, Manipur University Content Reviewer Prof. Anup Kumar Kapoor Department of Anthropology, University of Delhi 1 Archaeological Anthropology Anthropology Geological Time Scale Description of Module Subject Name Anthropology Paper Name 03 Archaeological Anthropology Module Name/Title Geological Time Scale Module Id 24 2 Archaeological Anthropology Anthropology Geological Time Scale Table of contents: 1. Introduction 2. Early Principles Behind Geologic Time 3. Construction Of Geologic Time Scale (GTS) 4. The Time Scale Creator 5. Recognizing Geologic Stages 6. Divisions Of Geologic Time 6.1 Proterozoic Or Precambrian Eon 6.2 The Palaozoic Era 6.3 The Mesozoic Era 6.4 The Cenozoic Era Learning outcomes To know about the geological time scale To understand the early Principles Behind Geologic Time To know about the construction Of Geologic Time Scale (GTS) To know and understand its divisions 3 Archaeological Anthropology Anthropology Geological Time Scale 1. Introduction The geography and landscape of a region are always changing. Geological research works reveal that the mountains and valleys that surround us or the position of the coastline today have not always been as we know them now. The land that we -
A Template for an Improved Rock-Based Subdivision of the Pre-Cryogenian Timescale
Downloaded from http://jgs.lyellcollection.org/ by guest on September 28, 2021 Perspective Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2020-222 A template for an improved rock-based subdivision of the pre-Cryogenian timescale Graham A. Shields1*, Robin A. Strachan2, Susannah M. Porter3, Galen P. Halverson4, Francis A. Macdonald3, Kenneth A. Plumb5, Carlos J. de Alvarenga6, Dhiraj M. Banerjee7, Andrey Bekker8, Wouter Bleeker9, Alexander Brasier10, Partha P. Chakraborty7, Alan S. Collins11, Kent Condie12, Kaushik Das13, David A. D. Evans14, Richard Ernst15,16, Anthony E. Fallick17, Hartwig Frimmel18, Reinhardt Fuck6, Paul F. Hoffman19,20, Balz S. Kamber21, Anton B. Kuznetsov22, Ross N. Mitchell23, Daniel G. Poiré24, Simon W. Poulton25, Robert Riding26, Mukund Sharma27, Craig Storey2, Eva Stueeken28, Rosalie Tostevin29, Elizabeth Turner30, Shuhai Xiao31, Shuanhong Zhang32, Ying Zhou1 and Maoyan Zhu33 1 Department of Earth Sciences, University College London, London, UK 2 School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, UK 3 Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA, USA 4 Department of Earth and Planetary Sciences, McGill University, Montreal, Canada 5 Geoscience Australia (retired), Canberra, Australia 6 Instituto de Geociências, Universidade de Brasília, Brasilia, Brazil 7 Department of Geology, University of Delhi, Delhi, India 8 Department of Earth and Planetary Sciences, University of California, Riverside, -
The Geological Origins of the Oracle at Delphi, Greece1 J.Z
The Geological Origins of the Oracle at Delphi, Greece1 J.Z. DE BOER Department of Earth & Environmental Sciences, Wesleyan University, Middletown, Connecticut, USA J.R. HALE College of Arts & Sciences, University of Louisville, Louisville, Kentucky, USA ncient authors from Plato to Pausanias geological setting of the sanctuary. According have left descriptions of Delphi’s to a number of Greek and Roman authorities, Aoracle and its mantic sessions. The the women who spoke the prophecies at latter were interpreted as events in which the Delphi sat on a tripod that spanned a cleft Pythia (priestess) placed herself on a tripod over or fissure in the rock within the temple of a cleft (fissure) in the ground below the Apollo Apollo. Vapours rose from this chasm into temple. Here she inhaled a vapour rising from the inner sanctum or adyton, where they the cleft, and became inspired with the power of intoxicated the priestess and inspired her prophecy. French archaeologists who excavated prophecies. The ancient testimonies have the oracle site at the turn of the century reported been challenged during the past half- no evidence of either fissures or gaseous emissions century, as modern archaeologists failed to and concluded that the ancient accounts were locate any cleft or source of vapours within myths. As a result, modern classical scholars the foundations of the ruined temple and and many archaeologists reject the ancient therefore concluded that the ancient sources testimonies concerning the mantic sessions and must have been in error. However, a recent their geological origin. geological study of the sanctuary and adjacent However, the geological conditions at the areas has shown that the preconditions for oracle site do not a priori exclude the early the emission of intoxicating fumes are indeed accounts. -
Rock Falls in Delphi Archaeological Site, in Greece
Rockfalls occurred in the archaeological site of Delphi, Greece B. Christaras Aristotle University of Thessaloniki, School of Geology, Lab. of Engineering Geology and Hydrogeology, e-mail: [email protected] K. Vouvalidis Aristotle University of Thessaloniki, School of Geology, Dept. of Physical & Environmental Geography, e-mail: [email protected] M. - F. Papakonstantinou Ministry of Culture, Chief Archaeologist of I’ Ephorate of Prehistoric and Classical Antiquities, Delphi, e-mail: [email protected] ABSTRACT: In the present investigation, the safety of the northern slope of Delphi’s archaeological site in Greece was investigated against rockfalls. The area consists of limestone lying over flysch. Three possible rockfall rebound tracks, passing through the ancient stadium, and the theatre, were studied for different rock dimensions and tracks resulting that the more dangerous and difficult in retention rockfall track is that which crosses the stadium. The use of barriers was investigated accepting, finally, that a 2.5m-high metallic barrier could be installed along the northern steep slope for the protection of the archaeological site. KEY WORDS: ROCKFALLS, DELPHI, SLOP STABILITY, RESTRAINING BARRIERES 1. INTRODUCTION In the middle of September 2009, prolonged rainfall activated rockfalls from the upper sections of the archaeological site’s northern slope and fall downslope, out of the enclosure wall of the Sanctuary of Apollo, north of the Portico of Attalus. Rockfalls also occur in the stadium from 2003 onwards (Figure 1). The slope, consisting of limestone, is steep and heavily broken as a result of the existing tectonics. The rockfalls created dangerous conditions in the archaeological site regarding the safety of tourists, the staff of the ephorate and the protection of the monuments. -
Engineering Geology of Dam Foundations in North - Western Greece
Durham E-Theses Engineering geology of dam foundations in north - Western Greece Papageorgiou, Sotiris A. How to cite: Papageorgiou, Sotiris A. (1983) Engineering geology of dam foundations in north - Western Greece, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/9361/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk ENGINEERING GEOLOGY OF DAM FOUNDATIONS IN NORTH - WESTERN GREECE by Sotiris A. Papageorgiou B.Sc.Athens, M.Sc.Durham (Graduate Society) The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. A thesis submitted to the University of Durham for the Degree of Doctor of Philosophy 1983 MAIN VOLUME i WALLS AS MUCH AS YOU CAN Without consideration, without pity, without shame And if you cannot make your life as you want it, they have built big and high walls around me. -
Thickness of the Lithosphere Beneath Turkey and Surroundings from S-Receiver Functions
Solid Earth, 6, 971–984, 2015 www.solid-earth.net/6/971/2015/ doi:10.5194/se-6-971-2015 © Author(s) 2015. CC Attribution 3.0 License. Thickness of the lithosphere beneath Turkey and surroundings from S-receiver functions R. Kind1,2, T. Eken3, F. Tilmann1,2, F. Sodoudi1, T. Taymaz3, F. Bulut4, X. Yuan1, B. Can5, and F. Schneider1 1Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany 2Freie Universität, Fachrichtung Geophysik, Berlin, Germany 3Department of Geophysical Engineering, The Faculty of Mines, Istanbul Technical University, 34469 Maslak, Istanbul, Turkey 4Istanbul Aydın University, AFAM D. A. E. Research Centre, Istanbul, Turkey 5Bogaziçi University, Kandilli Observatory and Earthquake Research Institute (KOERI), Istanbul, Turkey Correspondence to: R. Kind ([email protected]) Received: 9 March 2015 – Published in Solid Earth Discuss.: 10 April 2015 Revised: 8 July 2015 – Accepted: 15 July 2015 – Published: 31 July 2015 Abstract. We analyze S-receiver functions to investigate lies on studies that examined the data from several temporary variations of lithospheric thickness below the entire region and permanent seismic networks (e.g., Angus et al., 2006; of Turkey and surrounding areas. The teleseismic data used Sodoudi et al., 2006, 2015; Gök et al., 2007, 2015; Vanacore here have been compiled combining all permanent seismic et al., 2013; Vinnik et al., 2014). Interpretations from these stations which are open to public access. We obtained almost studies are either confined to a limited region or to a limited 12 000 S-receiver function traces characterizing the seismic depth extent, i.e., to crustal depths only. Thus, the variations discontinuities between the Moho and the discontinuity at of lithospheric thickness have not yet been homogeneously 410 km depth. -
54. Mesozoic–Tertiary Tectonic Evolution of the Easternmost Mediterranean Area: Integration of Marine and Land Evidence1
Robertson, A.H.F., Emeis, K.-C., Richter, C., and Camerlenghi, A. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 160 54. MESOZOIC–TERTIARY TECTONIC EVOLUTION OF THE EASTERNMOST MEDITERRANEAN AREA: INTEGRATION OF MARINE AND LAND EVIDENCE1 Alastair H.F. Robertson2 ABSTRACT This paper presents a synthesis of Holocene to Late Paleozoic marine and land evidence from the easternmost Mediterra- nean area, in the light of recent ODP Leg 160 drilling results from the Eratosthenes Seamount. The synthesis is founded on three key conclusions derived from marine- and land-based study over the last decade. First, the North African and Levant coastal and offshore areas represent a Mesozoic rifted continental margin of Triassic age, with the Levantine Basin being under- lain by oceanic crust. Second, Mesozoic ophiolites and related continental margin units in southern Turkey and Cyprus repre- sent tectonically emplaced remnants of a southerly Neotethyan oceanic basin and are not far-travelled units derived from a single Neotethys far to the north. Third, the present boundary of the African and Eurasian plates runs approximately east-west across the easternmost Mediterranean and is located between Cyprus and the Eratosthenes Seamount. The marine and land geology of the easternmost Mediterranean is discussed utilizing four north-south segments, followed by presentation of a plate tectonic reconstruction for the Late Permian to Holocene time. INTRODUCTION ocean (Figs. 2, 3; Le Pichon, 1982). The easternmost Mediterranean is defined as that part of the Eastern Mediterranean Sea located east ° The objective here is to integrate marine- and land-based geolog- of the Aegean (east of 28 E longitude). -
U Tech Glossary
URGLOSSARY used without permission revised the Ides of March 2014 glos·sa·ry Pronunciation: primarystressglässchwaremacron, -ri also primarystressglodots- Function: noun Inflected Form(s): -es Etymology: Medieval Latin glossarium, from Latin glossa difficult word requiring explanation + -arium -ary : a collection of textual glosses <an edition of Shakespeare with a good glossary> or of terms limited to a special area of knowledge <a glossary of technical terms> or usage <a glossary of dialectal words> Merriam Webster Unabridged tangent, adj. and n. [ad. L. tangens, tangent-em, pr. pple. of tangĕre to touch; used by Th. Fincke, 1583, as n. in sense = L. līnea tangens tangent or touching line. In F. tangent, -e adj., tangente n. (Geom.), Ger. tangente n.] c. In general use, chiefly fig. from b, esp. in phrases (off) at, in, upon a tangent, ie off or away with sudden divergence, from the course or direction previously followed; abruptly from one course of action, subject, thought, etc, to another. (http://dictionary.oed.com) As in off on a tangent. “Practice, repetition, and repetition of the repeated with ever increasing intensity are…the way.” Zen in the Art of Archery by Eugen Herrigel. For many terms, this glossary contains definitions from multiple sources, each with their own nuance, each authors variation emphasized. Reading the repeated definitions, with their slight variations, helps create a fuller, more overall understanding of the meaning of these terms. The etymology of the entries reinforces and may repeat the repetitions. Wax on, wax off. Sand da floor. For sometime, when I encounter a term I don’t understand (and there are very many), I have been looking them up in the oed and copying the definition into a Word document. -
Tectonics and Magmatism in Turkey and the Surrounding Area Geological Society Special Publications Series Editors
Tectonics and Magmatism in Turkey and the Surrounding Area Geological Society Special Publications Series Editors A. J. HARTLEY R. E. HOLDSWORTH A. C. MORTON M. S. STOKER Special Publication reviewing procedures The Society makes every effort to ensure that the scientific and production quality of its books matches that of its journals. Since 1997, all book proposals have been refereed by specialist reviewers as well as by the Society's Publications Committee. If the referees identify weaknesses in the proposal, these must be addressed before the proposal is accepted. Once the book is accepted, the Society has a team of series editors (listed above) who ensure that the volume editors follow strict guidelines on refereeing and quality control. We insist that individual papers can only be accepted after satisfactory review by two independent referees. The questions on the review forms are similar to those for Journal of the Geological Society. The referees' forms and comments must be available to the Society's series editors on request. Although many of the books result from meetings, the editors are expected to commission papers that were not presented at the meeting to ensure that the book provides a balanced coverage of the subject. Being accepted for presentation at the meeting does not guarantee inclusion in the book. Geological Society Special Publications are included in the ISI Science Citation Index, but they do not have an impact factor, the latter being applicable only to journals. More information about submitting a proposal and producing a Special Publication can be found on the Society's web site: www.geolsoc.org.uk. -
Slab Segmentation and Late Cenozoic Disruption of the Hellenic Arc Leigh H
Slab segmentation and late Cenozoic disruption of the Hellenic arc Leigh H. Royden, Dimitrios J. Papanikolaou To cite this version: Leigh H. Royden, Dimitrios J. Papanikolaou. Slab segmentation and late Cenozoic disruption of the Hellenic arc. Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2011, 12 (3), 10.1029/2010GC003280. hal-01438679 HAL Id: hal-01438679 https://hal.archives-ouvertes.fr/hal-01438679 Submitted on 17 Jan 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Article Volume 12, Number 3 29 March 2011 Q03010, doi:10.1029/2010GC003280 ISSN: 1525‐2027 Slab segmentation and late Cenozoic disruption of the Hellenic arc Leigh H. Royden Department of Earth, Atmospheric and Planetary Sciences, MIT, 54‐826 Green Building, Cambridge, Massachusetts, 02139 USA ([email protected]) Dimitrios J. Papanikolaou Department of Geology, University of Athens, Panepistimioupoli Zografou, 15784 Athens, Greece ([email protected]) [1] The Hellenic subduction zone displays well‐defined temporal and spatial variations in subduction rate and offers an excellent natural laboratory for studying the interaction among slab buoyancy, subduction rate, and tectonic deformation. In space, the active Hellenic subduction front is dextrally offset by 100– 120 km across the Kephalonia Transform Zone, coinciding with the junction of a slowly subducting Adria- tic continental lithosphere in the north (5–10 mm/yr) and a rapidly subducting Ionian oceanic lithosphere in the south (∼35 mm/yr).