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Geochemistry This
TORONTOTORONTO Vol. 8, No. 4 April 1998 Call for Papers GSA TODAY — page C1 A Publication of the Geological Society of America Electronic Abstracts Submission — page C3 Antarctic Neogene Landscapes—In the 1998 Registration Refrigerator or in the Deep Freeze? Annual Issue Meeting — June GSA Today Introduction The present Molly F. Miller, Department of Geology, Box 117-B, Vanderbilt Antarctic landscape undergoes very University, Nashville, TN 37235, [email protected] slow environmental change because it is almost entirely covered by a thick, slow-moving ice sheet and thus effectively locked in a Mark C. G. Mabin, Department of Tropical Environmental Studies deep freeze. The ice sheet–landscape system is essentially stable, and Geography, James Cook University, Townsville, Queensland 4811, Australia, [email protected] Antarctic—Introduction continued on p. 2 Atmospheric Transport of Diatoms in the Antarctic Sirius Group: Pliocene Deep Freeze Arjen P. Stroeven, Department of Quaternary Research, Stockholm University, S-106 91 Stockholm, Sweden Lloyd H. Burckle, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964 Johan Kleman, Department of Physical Geography, Stockholm University, S-106, 91 Stockholm, Sweden Michael L. Prentice, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824 INTRODUCTION How did young diatoms (including some with ranges from the Pliocene to the Pleistocene) get into the Sirius Group on the slopes of the Transantarctic Mountains? Dynamicists argue for emplacement by a wet-based ice sheet that advanced across East Antarctica and the Transantarctic Mountains after flooding of interior basins by relatively warm marine waters [2 to 5 °C according to Webb and Harwood (1991)]. -
Elever Ved Kristiania Katedralskole Som Begynte På Skolen I Årene (Hefte 7)
1 Elever ved Kristiania katedralskole som begynte på skolen i årene (hefte 7). 1881 – 1890 Anders Langangen Oslo 2020 2 © Anders Langangen Hallagerbakken 82 b, 1256 Oslo (dette er hefte nr. 7 med registrering av elever ved Schola Osloensis). 1. Studenter fra Christiania katedralskole og noen elever som ikke fullførte skolen- 1611-1690. I samarbeid med Einar Aas og Gunnar Birkeland. Oslo 2018 2. Elever ved Christiania katedralskole og privat dimitterte elever fra Christiania 1691-1799. I samarbeid med Einar Aas & Gunnar Birkeland. Oslo 2017. 3. Studenter og elever ved Christiania katedralskole som har begynt på skolen i årene 1800 – 1822. Oslo 2018. 4. Studenter og elever ved Christiania katedralskole som begynte på skolen i årene 1823-1847. Oslo 2019. 5. Studenter og elever ved Christiania katedralskole som begynte på skolen i årene 1847-1870. Oslo 2019 6. Elever ved Kristiania katedralskole som begynte på skolen i årene 1871 – 1880. Oslo 2019. I dette syvende heftet følger rekkefølgen av elvene elevprotokollene. Det vi si at de er ordnet etter året de begynte på skolen på samme måte som i hefte 6. For hver elev er det opplysninger om fødselsår og fødselssted, foreldre og tidspunkt for start på skolen (disse opplysningene er i elevprotokollene). Dåpsopplysninger er ikke registrert her, hvis ikke spesielle omstendigheter har gjort det ønskelig (f.eks. hvis foreldre ikke er kjent eller uklart). I tillegg har jeg med videre utdannelse der hvor det vites. Også kort om karriere (bare hovedtrekk) etter skolen og når de døde. Både skolestipendiene og de private stipendiene er registrert, dessuten den delen av skolestipendiet som ble opplagt til senere utbetaling og om de ble utbetalt eller ikke. -
Exploration of Victoria Crater by the Mars Rover Opportunity
Exploration of Victoria Crater by the Mars Rover Opportunity The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Squyres, Steven W., Andrew H. Knoll, Raymond E. Arvidson, James W. Ashley, James F. III Bell, Wendy M. Calvin, Philip R. Christensen, et al. 2009. Exploration of Victoria Crater by the Mars rover Opportunity. Science 324(5930): 1058-1061. Published Version doi:10.1126/science.1170355 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:3934552 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Open Access Policy Articles, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#OAP Exploration of Victoria Crater by the Rover Opportunity S.W. Squyres1, A.H. Knoll2, R.E. Arvidson3, J.W. Ashley4, J.F. Bell III1, W.M. Calvin5, P.R. Christensen4, B.C. Clark6, B.A. Cohen7, P.A. de Souza Jr.8, L. Edgar9, W.H. Farrand10, I. Fleischer11, R. Gellert12, M.P. Golombek13, J. Grant14, J. Grotzinger9, A. Hayes9, K.E. Herkenhoff15, J.R. Johnson15, B. Jolliff3, G. Klingelhöfer11, A. Knudson4, R. Li16, T.J. McCoy17, S.M. McLennan18, D.W. Ming19, D.W. Mittlefehldt19, R.V. Morris19, J.W. Rice Jr.4, C. Schröder11, R.J. Sullivan1, A. Yen13, R.A. Yingst20 1 Dept. of Astronomy, Space Sciences Bldg., Cornell University, Ithaca, NY 14853, USA 2 Botanical Museum, Harvard University, Cambridge MA 02138, USA 3 Dept. -
Mars Reconnaissance Orbiter and Opportunity Observations Of
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE Mars Reconnaissance Orbiter and Opportunity 10.1002/2014JE004686 observations of the Burns formation: Crater Key Point: hopping at Meridiani Planum • Hydrated Mg and Ca sulfate Burns formation minerals mapped with MRO R. E. Arvidson1, J. F. Bell III2, J. G. Catalano1, B. C. Clark3, V. K. Fox1, R. Gellert4, J. P. Grotzinger5, and MER data E. A. Guinness1, K. E. Herkenhoff6, A. H. Knoll7, M. G. A. Lapotre5, S. M. McLennan8, D. W. Ming9, R. V. Morris9, S. L. Murchie10, K. E. Powell1, M. D. Smith11, S. W. Squyres12, M. J. Wolff3, and J. J. Wray13 1 2 Correspondence to: Department of Earth and Planetary Sciences, Washington University in Saint Louis, Missouri, USA, School of Earth and Space R. E. Arvidson, Exploration, Arizona State University, Tempe, Arizona, USA, 3Space Science Institute, Boulder, Colorado, USA, 4Department of [email protected] Physics, University of Guelph, Guelph, Ontario, Canada, 5Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA, 6U.S. Geological Survey, Astrogeology Science Center, Flagstaff, Arizona, USA, 7 8 Citation: Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, USA, Department Arvidson, R. E., et al. (2015), Mars of Geosciences, Stony Brook University, Stony Brook, New York, USA, 9NASA Johnson Space Center, Houston, Texas, USA, Reconnaissance Orbiter and Opportunity 10Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland, USA, 11NASA Goddard Space Flight Center, observations of the Burns formation: Greenbelt, Maryland, USA, 12Department of Astronomy, Cornell University, Ithaca, New York, USA, 13School of Earth and Crater hopping at Meridiani Planum, J. -
"Nkw^ORKI
j 18 -f THE NEWr YORK HERALD, WEIDNESDAY, DECEMBER 28, 1921. SHIP PI NG NEWS FR<OM AL L PARIrs of The1fl ORLD f \ William A McKenney lat 38 43. Ion 74 42 Str City of St I.ouls, Johnson, Savannah nopn, 30.16 Inrhea; wind, W, light breeze; tall shaft, hut which Is now being towed tg CLOSING OF MAILS -7th. (, general).Ocean Steamship Co. weatlier, dull; temperature, 23 deg Fahr. port by str Balsam. Notice to Owners, Agents and William H t'oheny 434 E Tatnplco 27th. Str city of Savannah, Borum, Savannah The postponed auction sale of bargee STRONG MAN LIKELY Foreign mails will close promptly as ind icated below at the General Post Office and general).Ocean Steamship Co. hiictu and Congressman Scully took placeTim1at City Hall Station. Ordinary prints, samples, parcel pout packages and registered articles Ship Masters. Sir Arapahoe, Devereaux, Charleston and ICast Doeton Saturday by Deputy U S Ma^ close iwo hours earlier, except that registered articles have to be mailed between the hours PASSED CITY ISLAND. J acksonvtll" (general).Clyde Steamship Co. MARITIME MISCELLANY. rltal; they were purchased by R Savldge of of M AM and I'd I'M. At the Foreign Station (corner of Morton and West streets) foreign Str Hamilton. Nelson, Norfolk (general). 8tr Norfolk, Portland for Norfolk, put In Brooklyn for $10,100 each. mall closes half an hour later than at the Geie rul Post Office and Hall Station, The Herald publishes Id Dominion Transportation Co. here wit)i main steam pipe broken; veeeel ALIEN City daily Boston HAVANA, Doc 27.Freight is beginning to TO BEND closes at Str Osborn, BARS mall the double Bound South. -
A MTAK Kiadványai 47. Budapest, 1966
A MAGYAR TUDOMÁNYOS AKADÉMIA KÖNYVTARÁNAK KÖZLEMÉNYEI PUBLICATIONES BIBLIOTHECAE ACADEMIAE SCIENTIARUM HUNGARICAE 47. INDEX ÀCRONYMORUM SELECTORUM Institute* communicationis BUDAPEST, 1966 VOCABULARIUM ABBREVIATURARUM BIBLIOTHECARII III Index acronymorum selectorum 7. Instituta communicationis A MAGYAR TUDOMÁNYOS AKADÉMIA KÖNYVTARÁNAK KÖZLEMÉNYEI PUBLICATIONES BIBLIOTHECAE ACADEMIAE SCIENTIARUM HUNGARICAE 47. VOCABULARIUM ABBREVIATURARUM BIBLIOTHECARII Index acronymorum selectorum 7. Instituta communicationis BUDAPEST, 196 6 A MAGYAR TUDOMÁNYOS AKADÉMIA KÖNYVTARÁNAK KÖZLEMÉNYEI PUBLICATIONES BIBLIOTHECAE ACADEMIAE SCIENTIARUM HUNGARICAE 47. INDEX ACRONYMORUM SELECTORUM 7 Instituta communications. BUDAPEST, 1966 INDEX ACRONYMORUM SELECTORUM Pars. 7. Instituta communicationis. Adiuvantibus EDIT BODNÁ R-BERN ÁT H et MAGDA TULOK collegit et edidit dr. phil. ENDRE MORAVEK Lectores: Gyula Tárkányi Sámuel Papp © 1966 MTA Köynvtára F. к.: Rózsa György — Kiadja a MTA Könyvtára — Példányszám: 750 Alak A/4. - Terjedelem 47'/* A/5 ív 65395 - M.T.A. KESz sokszorosító v ELŐSZÓ "Vocabularium abbreviaturarum bibliothecarii" cimü munkánk ez ujabb füzete az "Index acronymorum selectorum" kötet részeként, a köz- lekedési és hírközlési intézmények /ilyen jellegű állami szervek, vasu- tak, légiközlekedési vállalatok, távirati irodák, sajtóügynökségek stb/ névröviditéseit tartalmazza. Az idevágó felsőbb fokú állami intézmények /pl. minisztériumok stb./ nevének acronymáit, amelyeket az "Instituta rerum publicarum" c. kötetben közöltünk, technikai okokból nem -
Cabo Verde 2.0. Marca Y Desarrollo Turístico En El Archipiélago
PASOS. Revista de Turismo y Patrimonio Cultural ISSN: 1695-7121 [email protected] Universidad de La Laguna España Cabo Verde 2.0. Marca y desarrollo turístico en el archipiélago Marcelino, Pedro F.; Oca Gonzaléz, Luzia Cabo Verde 2.0. Marca y desarrollo turístico en el archipiélago PASOS. Revista de Turismo y Patrimonio Cultural, vol. 17, no. Esp.3, 2019 Universidad de La Laguna, España Available in: https://www.redalyc.org/articulo.oa?id=88165935004 DOI: https://doi.org/10.25145/j.pasos.2019.17.037 This work is licensed under Creative Commons Attribution-NonCommercial-NoDerivs 4.0 International. PDF generated from XML JATS4R by Redalyc Project academic non-profit, developed under the open access initiative Pedro F. Marcelino, et al. Cabo Verde 2.0. Marca y desarrollo turístico en el archipiélago Artículos Cabo Verde 2.0. Marca y desarrollo turístico en el archipiélago Cabo Verde 2.0: desarrollo de marca y turismo en todo el archipiélago Pedro F. Marcelino DOI: https://doi.org/10.25145/j.pasos.2019.17.037 Longyearbyen Consulting, Canadá Redalyc: https://www.redalyc.org/articulo.oa? [email protected] id=88165935004 Luzia Oca Gonzaléz University of Trás#os#Montes, Portugal [email protected] Received: 21 January 2019 Accepted: 18 February 2019 Abstract: is article homes in on the genesis and the development process of tourism in the Cabo Verdes Islands, West Africa, from its definition as a national priority in the post#independence period, to its qualification as a strategic sector in the 1990s, to the prioritizing of the sector as a core economic pillar for the 21s Century. -
What Are Marine Ecological Time Series Telling Us About the Ocean? a Status Report
IOC-UNESCO TS129 What are Marine Ecological Time Series telling us about the ocean? A status report [ Individual Chapter (PDF) download ] The full report (all chapters and Annex) is available online at: http://igmets.net/report Chapter 01: New light for ship-based time series (Introduction) Chapter 02: Methods & Visualizations Chapter 03: Arctic Ocean Chapter 04: North Atlantic Chapter 05: South Atlantic Chapter 06: Southern Ocean Chapter 07: Indian Ocean Chapter 08: South Pacific Chapter 09: North Pacific Chapter 10: Global Overview Annex: Directory of Time-series Programmes This page intentionally left blank to preserve pagination in double-sided (booklet) printing 2 Annex Description of time-series programmes The time-series sites and programmes participating in contact information.The Annex lists only time-series the IGMETS analysis are individually described in the sites where data were shared, highlighting the important following pages. The sections of this Annex are sorted collaborative and scientific contributions made. As by major ocean basins, following the ocean conveyor IGMETS is an ongoing activity, new time series will be belt starting in the Arctic Ocean (A1), North Atlantic included and their new datasets will be added beyond (A2), South Atlantic (A3), Southern Ocean (A4), Indian this first report. Updated information is available in the Ocean (A5), South Pacific (A6), and finishing in the online IGMETS metabase (http://igmets.net/metabase). North Pacific Ocean (A7). In addition to the brief infor- Two example IGMETS time-series site summary figures mation provided within each text summary here, a are shown below. These figures indicate the geographic unique identifier/web link is provided to access detailed location and available variable classes submitted to information about each time-series site. -
Volcanoes? Analogues to Martian Plumes Feeding the Giant Shield Are Terrestrial Plumes from Motionless Plates
Downloaded from http://sp.lyellcollection.org/ by guest on February 22, 2014 Geological Society, London, Special Publications Online First Are terrestrial plumes from motionless plates analogues to Martian plumes feeding the giant shield volcanoes? Christine M. Meyzen, Matteo Massironi, Riccardo Pozzobon and Luca Dal Zilio Geological Society, London, Special Publications, first published February 21, 2014; doi 10.1144/SP401.8 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection How to cite click here for further information about Online First and how to cite articles Notes © The Geological Society of London 2014 Downloaded from http://sp.lyellcollection.org/ by guest on February 22, 2014 Are terrestrial plumes from motionless plates analogues to Martian plumes feeding the giant shield volcanoes? CHRISTINE M. MEYZEN1*, MATTEO MASSIRONI1,2, RICCARDO POZZOBON1,3 & LUCA DAL ZILIO1 1Dipartimento di Geoscienze, Universita` degli Studi di Padova, via G. Gradenigo, 6, 35131 Padova, Italy 2INAF, Osservatorio Astronomico di Padova, Vicolo dell’Osservatorio 3, 35122 Padova, Italy 3IRSPS-DISPUTer, Universita’ G. d’Annunzio, Via Vestini 31, 66013 Chieti, Italy *Corresponding author (e-mail: [email protected]) Abstract: On Earth, most tectonic plates are regenerated and recycled through convection. However, the Nubian and Antarctic plates could be considered as poorly mobile surfaces of various thicknesses that are acting as conductive lids on top of Earth’s deeper convective system. Here, volcanoes do not show any linear age progression, at least not for the last 30 myr, but constitute the sites of persistent, focused, long-term magmatic activity rather than a chain of volcanoes, as observed in fast-moving plate plume environments. -
Elever Ved Kristiania Katedralskole Som Begynte På Skolen I Årene (Hefte 6)
1 Elever ved Kristiania katedralskole som begynte på skolen i årene (hefte 6) 1871 - 1880 Anders Langangen Oslo 2019 2 © Anders Langangen Hallagerbakken 82 b, 1256 Oslo (dette er hefte nr. 6 med registrering av elever ved Schola Osloensis). 1. Studenter fra Christiania katedralskole og noen elever som ikke fullførte skolen- 1611- 1690. I samarbeid med Einar Aas og Gunnar Birkeland. Oslo 2018 2. Elever ved Christiania katedralskole og privat dimitterte elever fra Christiania 1691-1799. I samarbeid med Einar Aas & Gunnar Birkeland. Oslo 2017. 3. Studenter og elever ved Christiania katedralskole som har begynt på skolen i årene 1800 – 1822. Oslo 2018. 4. Studenter og elever ved Christiania katedralskole som begynte på skolen i årene 1823- 1847. Oslo 2019. 5. Studenter og elever ved Christiania katedralskole som begynte på skolen i årene 1847- 1870. Oslo 2019 I dette sjette heftet følger rekkefølgen av elvene elevprotokollene. Det vi si at de er ordnet etter året de begynte på skolen, og ikke året de sluttet som i de fem andre heftene. De elevene som sluttet i årene 1871-1878 er i hefte 5. For hver elev er det opplysninger om fødselsår og fødselssted, foreldre og tidspunkt for start på skolen (disse opplysningene er i elevprotokollene). I tillegg har jeg med videre utdannelse der hvor det vites. Dåpsopplysninger er ikke registrert her, hvis ikke spesielle omstendigheter har gjort det ønskelig (f.eks. hvis foreldre ikke er kjent eller uklart). Både skolestipendiene og de private stipendiene er registrert, dessuten den delen av skolestipendiet som ble opplagt til senere utbetaling og om de ble utbetalt eller ikke. -
Dark Lineae on the Equatorial Layered Deposits; Are These Recurring Slope Lineae (Rsl) Or Small Debris Flows? D
Lunar and Planetary Science XLVIII (2017) 1494.pdf DARK LINEAE ON THE EQUATORIAL LAYERED DEPOSITS; ARE THESE RECURRING SLOPE LINEAE (RSL) OR SMALL DEBRIS FLOWS? D. E. Stillman1, R. E. Grimm1, F. J. Calef2, Y. Lu2, and T. I. Michaels3, 1Dept. of Space Studies, Southwest Research Institute, 1050 Walnut St. #300, Boulder, CO 80302 ([email protected]), 2Jet Propulsion Laboratory, California Inst. of Technology, 3SETI Institute Introduction: To gain insight into the formation Aram Chaos has the only confirmed EQ site out- and recharge mechanism(s) of recurring slope lineae side of VM and on a layered deposit. At this site there (RSL), we have been using HiRISE images to search are also many dark lineae that appear to never fade. for candidate RSL sites. As of the December 2016 Meanwhile, neighboring RSL recur, incrementally HiRISE release, we have cataloged 577 candidate RSL lengthen, and fade. Non-fading dark lineae have been sites, of which 74 have been confirmed to exhibit RSL. detected in other locations (e.g., Rauna crater), but not Confirmed sites show recurrence, incremental length- at this magnitude. Further complicating the matter is ening, and fading of dark lineae, while candidate RSL that incremental lengthening of the EQ RSL sites from sites have dark lineae that look like RSL but do not 13°S to 4°N appears to occur twice a year, over two possess all three of the characteristics in available im- periods approximately centered on the equinoxes. agery. Each site is categorized by its number of RSL Overall, EQ RSL lengthen ~60% of the year, and stay characteristics and by a qualitative ranking of the like- dark and static for an additional ~15% of a Mars year. -
Pionertida for Nynorsk Kyrkjespråk. Ei Tekstsamling
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by HSN Open Archive NR 3/2016 NOTAT Per Halse PIONERTIDA FOR NYNORSK KYRKJESPRÅK. EI TEKSTSAMLING. Føreord Dette er ei samling aktstykkje, oversyn, tekstsamanlikningar og andre kjelder for soga om korleis det voks fram eit nynorsk kyrkjemål. Dei åtti fyrste tekstene var vedlegg til doktoravhandlinga Gudsord og folkemål. Framveksten av nynorsk kyrkjespråk 1859–1908, Universitetet i Oslo 2009 (ss. 513–570). Derimot er dei ikkje med i den kortare bokversjonen Gudsord og folkespråk. Då nynorsk vart kyrkjemål, Tapir Akademisk Forlag 2011. Tekstdøma gjorde eg då i staden tilgjengelege på ei tilsett-side ved Høgskulen i Volda. Gjennom endringar i vevstrukturen har den lenkja frå 2011 forsvunne. Etter råd frå gode kollegaer gjer eg no det som burde vore gjort for over fem år sidan: Dokumentet som heitte «Åtti tekster frå pionertida for nynorsk kyrkjespråk» kjem i litt utvida stand og med ny tittel her i Notat-serien. Attåt dei åtti vedlegga frå avhandlinga har eg teke med nokre utdrag som samanliknar omsetjingar av Peter Hognestad (1866–1931) med dei dansk-norske som rådde i samtida (nummera 81–83 attast i heftet). Språkutviklinga og politiske vedtak har gjennom godt over hundre år gjort skilnadene mellom nynorsk og bokmål monaleg mindre enn det dei var frå starten. Materialet i denne samlinga gjev glimt av den språklege stoda i norsk skule og kyrkje på 1800- og byrjinga av 1900-talet. For utfyllande opplysningar om tekstene og konteksten viser eg til Gudsord og folkespråk. Då nynorsk vart kyrkjemål (Trondheim: Tapir, 2011) og Peter Hognestad.