DOCSLIB.ORG

The Reutuaapa Dolomite Marble Deposit at Tervola, Northern Finland

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Reutuaapa Dolomite Marble Deposit at Tervola, Northern Finland Northern Finland Office M19/3611/2007/92 16.4.2008 Rovaniemi The Reutuaapa dolomite marble deposit at Tervola, Northern Finland Panu Lintinen, Pertti Turunen, Risto Vartiainen Reutuaapa dolomite marble l\119/361l12007/92 GEOLOGICAL SURVEY OF FINLAND DOCUMENTATION PAGE Date f RtX . no. 16.4.2008 Authors Type of report Panu Lintinen Mineral deposit report, M19 Pertti Turunen Risto Vartiainen Commissioned by Geo logical Survey ofFinland (GTK) Title or report The Reutuaapa dolomite marble deposit at Tervola, Northem Finland Abstract The Reutuaapa dolomite marble deposit is located in the municipality ofTervala in Northem Finland, about 40 km south of the city ofRovaniemi . The central part of the prospected area is covered by a sing le clai m of 50 hectares (Reutuaapa I, mining register number 8 170/ 1). During 2005-2007 the deposit was investigated with geological field mapping, a geophysical ground survey on a 2.4 km' systematic grid, and diamond drilling of 1790 meters. Systematic laboratory analysis was performed for over 550 dolomite samples, methods including both whole rock X-ray analysis and acid solution lCP-AES analysis for carbonate fraction. Flotation tests were also made for 5 representative samples. The dolomite marble of Reutuaapa is except ionally white and iron-poor. The best brightness and yellowness val- ues (ISO 2469 standard) for the dolomite concentrate were 91.0% and 1.9%, respec tively. The average Fe,O, co n- tent ofwhite marble is only 0.18%, at places <0.05%. The average total carbonate content (calculated from ana- lysed C content) of white marble is 88%, of which approximately 90% is dolomite and 10% calcite. The average Si0 2 content is 10% consisting almost exclusively of quartz. Practically all the silica was successfully removed with the flotation technique. The deposit has been intersected with 4 drilling profiles, each including a continuous 150-200 m wide section o f white dolomite marb le. On the basis of drilling and field mapping, the wbite marble forms at least a 1000 m long , 200 m wide and 100 m deep, vertically or sub-vertically dipping and E- W- trending body, surrounded by grey dolomite marbles. Thus the white dolom ite marble deposit has potential resources of over 50 million tonnes (not measured according to the N143-10 1 standards or the JORC-code). However, the deposit is still open at depth and to the east, west and south. Keywords Tervola, Reutuaapa, dolomite, marble, mapp ing, geophysical surveys, drilling, flotation Geographical area Finland, Lapland, Tervola, Reutuaapa Map sheet 3611 04 Olher information Reportser ial Archive code MI 9 M1 9/361 112007/92 Total pages Language Price Confi dentiality 38 English Confidential Unitandsection Projec t cod e Northem Finland Office, 50 I 2902000 ~;:e/nalZ: < . - ~ .L Oda~uC/naU~ Panu Lintinen Pertti Turunen Risto Vartiainen Q GTK GEOLOGIAN TUTKIMUSKESKUS • GEOLOGISKA FORS KNINGSCENTRALEN • GEO LOGICAL SURVEY OF FIN LAND Reutnaapa dolomite marble i\119/361112007/92 GEOLOGIAN TUTKIMUSKESKUS KUVAILULEHTI Paivamaara {Duro 16.4.2008 Tekija t Rapon in laji Panu Lintinen Esiintymarapo rtti, M 19 Pertt i Turunen Toimeksiantaja Risto Vartiainen Geologian tutkimuskeskus Raportin nirni The Reu tuaapa dolomite marble deposit at Tervola, Northern Finland (Reutuaa van dolomiittimannoriesiintyma Tervoktssn. Pohjois-Suomessa] Tilvlstelmf Reutuaavan dolomiittimarmoriesiintyma sijaitsee Tervolan kunnassa , noin 40 km Rovani emen kaupungin etela - puolell a. Esiintyman keskeisen tutkimusalueen kattaa 50 hehtaarin valtaus (Reutuaapa 1. kaivosrekisterinumero 8170/1). Vuosina 2005 - 2007 esiintymaa tutk ittiin geolog isen kartoituks en, systemaattisen 2.4 km':" geofysikaa- lisen mittauksen seka 1790 metrin timanttikairauksen avulla. Yli 550 dolomiittinayt teelle tehtiin systemaattiset laboratorioanalyysit , joissa kaytettiin seka XRF - rnenetelrnaa kokokivelle etta happoliuotusrnenetelmaa (ICP- AES) karbonaattifraktiolle. Ni iden lisaksi tehtiin vaahdotuskokeet 5 edustavalle naytteelle, Reutuaavan dolom iittimannori on poikkeuksellisen valkois ta ja rautako yhaa, Parhaat vaaleus- j a keltaisuusarvot (ISO 2469 - standardi) dolomiittirikasteelle ova t 9 1.0 % ja 1.9 %. Kcskimaarainen valkoisen marmorin Fe,O, - pitoisuus on ainoa staan 0.18 %, monin paikoin aile 0.05 %. Analyso idun C:n maarasta laskettu keskimaarainen totaa likarbonaattipitoisuus on valko isella mannorilla 88 %, josta noin 90 % on dolomiittia ja 10 % kalsiittia. Kes- kimaarainen 5i02 - pitoisuus on 10 % koostuen lahes yksinomaan kvartsista. Silikaatit pystyttiin poistamaan kay- tannossa kokonaan vaahdotukse lla. Esiintymii on lavistetty 4 kairausprofiililla, joista jokainen sisa ltaa yhtenaisen 150-200 metria Ievean lavistyks en valkoista dolomiittimarm oria. Kairauk sen j a geologisen kart oituksen peru steella valkoinen mannori on ainaki n 1000 metria pitka, 200 metria levea ja 100 metrin syvyydelle ulottuva pysty tai lahes pysty, itii-liintinen harmaan dolomiitt imannorin ymparc irna linssi. Esi intyma n arvioidaa n sisaltavan yli 50 miljoonaa tonnia valkoista dolo- miittimarmoria. Kuitenkin esiintyman jatkuvuus on auki syvyyssuuntaan, itaan, lanteen ja etelaan, Asiasa nat (kohdc. mcnct chuarjn c.) Tervola, Reutuaapa, dolomiitti, marmori, kartoitus, geofysikaalinen tutkimu s, kair aus, vaahdotus Maanti ctcellincn aluc (maa. llii ini,kunia. kyla. esiintymal Suomi, l appi. Tervola, Reutuaapa Karttal ehdet 36 11 04 Muur ti cdot Arkistosarjan nimi Arkistctunnus M I9 M I9/361112007/92 Kokonaissivumaara IKid; Hinta Julkisuus 38 eng lanti luottamuksellinen Yksikko ja vastuualuc Hankctunnus Pohjois-Suornen yksikko, 50 I 2902000 Allckirjoitusln imen selvcrmys ~"'A v~ ~ o i tutt-en sclvcnnys PIfM-.1 /f0L-- "L = Panu Lintinen Pertt i Turunen Risto Vartiainen - c GTK GEOtOG IAN TUTKIMUS KESKUS • GEO LOGISKA FORSKNINGSCENTRALEN •GEOLOGICA L SURVEY OF FINLAND Reutuaapa dolomite marble M19/3611/2007/92 Contents Documentation page Kuvailulehti 1 INTRODUCTION 1 2 GEOGRAPHY AND GENERAL PROPERTY DESCRIPTION 2 2.1 Location, access and infrastructure 2 2.2 Titles 3 2.3 Physiography, climate and vegetation 4 2.4 Property history 4 3 REGIONAL GEOLOGY 4 3.1 Geological setting 4 3.2 Economic geology 5 4 SURVEY DESCRIPTION 7 4.1 Current survey program 7 4.2 Research techniques and results 7 4.2.1 Geophysical surveys 7 4.2.2 Diamond drilling 8 4.2.3 Geological mapping 8 4.2.4 Chemical analyses 9 4.2.5 Mineralogical studies and flotation tests 9 4.2.6 Documentation 9 5 DOLOMITE MARBLE DEPOSIT T 10 5.1 Bedrock geology 10 5.2 Geophysics 11 5.3 Petrophysical measurements 12 5.4 Mineralogy and chemistry of dolomite 13 5.5 Flotation test results 17 6 DOLOMITE MARBLE RESOURCES 19 7 ENVIRONMENTAL ASPECTS 20 8 CONCLUDING REMARKS 21 9 REFERENCES 23 APPENDICES Reutuaapa dolomite marble 1 M19/3611/2007/92 1 INTRODUCTION The Geological Survey of Finland (GTK) is Finland’s national geoscience agency. GTK was es- tablished in 1885 and operated under the Ministry of Trade and Industry until the end of 2007. Starting in 2008, the GTK has operated under the new Ministry of Employment and the Econ- omy. GTK’s main office is located in Espoo, near Helsinki, and it has regional offices in Kuopio, Kokkola and Rovaniemi. It has a permanent staff of 720, including about 300 geologists, geo- chemists, chemists and geophysicists. GTK is responsible for the acquisition and management of geoscience information in Finland, with a particular emphasis on providing high quality data for the exploration and mining sector. Through a comprehensive mapping and research program, GTK also identifies and documents areas with mineral potential, in order to encourage follow-up exploration and exploitation by the private sector, with the aim of supporting sustainable use of both bedrock resources and surficial deposits. All GTK discoveries are offered to the private sector through an open tendering process arranged by the Ministry of Employment and the Economy. GTK offers the minerals industry expertise in Fennoscandian economic geology, as well as con- fidential, client-tailored exploration services, including geophysical surveys and modern chemi- cal, mineralogical and mineral processing laboratory services, both within Finland and world- wide. For further information see http://www.gtk.fi. The main targets of industrial mineral survey at GTK are pigment minerals, especially for paper industry (calcite, dolomite, ilmenite, kaolinite, talc) and rare elements (Li, Ta, Nb, Be). From the beginning of 2005, the industrial mineral survey in the Northern Finland office has focused on the Peräpohja Schist Belt (PSB) area of SW Lapland. The objective has been to investigate car- bonate and talc resources and the potential of the belt. The PSB is well known for widespread dolomite marbles, which have been utilized both as industrial minerals and as dimension stones. However, modern mineralogical and geochemical studies and quality assessments of the dolo- mite marbles have been few or lacking completely, especially in the eastern part of the PSB. Fur- thermore, it has been estimated that in the near future, major mining of PGE- and base metals in the south and southeast parts of the PSB will very likely require large volumes of carbonate ma- terial for environmental and/or process-related applications. After an initial review of the geographical and geological data and subsequent field evaluations, the Reutuaapa area was selected for further investigations. The survey showed that the dolomite marble deposit was of high quality and was evaluated to have considerable
Load more

Recommended publications
  • Labour Market Areas Final Technical Report of the Finnish Project September 2017
    Eurostat – Labour Market Areas – Final Technical report – Finland 1(37) Labour Market Areas Final Technical report of the Finnish project September 2017 Data collection for sub-national statistics (Labour Market Areas) Grant Agreement No. 08141.2015.001-2015.499 Yrjö Palttila, Statistics Finland, 22 September 2017 Postal address: 3rd floor, FI-00022 Statistics Finland E-mail: [email protected] Yrjö Palttila, Statistics Finland, 22 September 2017 Eurostat – Labour Market Areas – Final Technical report – Finland 2(37) Contents: 1. Overview 1.1 Objective of the work 1.2 Finland’s national travel-to-work areas 1.3 Tasks of the project 2. Results of the Finnish project 2.1 Improving IT tools to facilitate the implementation of the method (Task 2) 2.2 The finished SAS IML module (Task 2) 2.3 Define Finland’s LMAs based on the EU method (Task 4) 3. Assessing the feasibility of implementation of the EU method 3.1 Feasibility of implementation of the EU method (Task 3) 3.2 Assessing the feasibility of the adaptation of the current method of Finland’s national travel-to-work areas to the proposed method (Task 3) 4. The use and the future of the LMAs Appendix 1. Visualization of the test results (November 2016) Appendix 2. The lists of the LAU2s (test 12) (November 2016) Appendix 3. The finished SAS IML module LMAwSAS.1409 (September 2017) 1. Overview 1.1 Objective of the work In the background of the action was the need for comparable functional areas in EU-wide territorial policy analyses. The NUTS cross-national regions cover the whole EU territory, but they are usually regional administrative areas, which are the re- sult of historical circumstances.
    [Show full text]
  • Ohjausryhmän Muistio 26.9.2019
    LÄNSI-POHJAN SAIRAANHOITOPIIRIN KUNTAYHTYMÄ Perusterveydenhuollon yksikkö 2019 1(1) _____________________________________________________________________________________________________ PERUSTERVEYDENHUOLLON YKSIKÖN OHJAUSRYHMÄ Aika: 26.9.2019 klo 12.30-14.30 Paikka: Kokoustila PUHKU, keskussairaalan keuhkosairauksien pkl:n yhteydessä Ohjausryhmän jäsenet ja varajäsenet Kemi: Liisa Niiranen Keminmaa: Eila Metsävainio Simo: Vivi Marttila Tarja Leskinen Tervola: Mika Simoska Helena Hartikainen Tornio: Maarit Alalahti Pertti Sakaranaho Ylitornio: Kari Askonen Eeva Leukumaa Lapin AMK: Hannele Kauppila LPSHP: Jyri J. Taskila PTH-yksikkö: Merja Haapakorva-Kallio Kari S. Lankinen Teija Moisanen Muut kutsutut: Paavo Uusimaa, MLP Oy (skype-yhteys) Käsiteltävät asiat 1. Kokouksen avaus ja osallistujien toteaminen Puheenjohtaja Kari Askonen avasi kokouksen klo 12.30 ja todettiin läsnäolijat. 2. Työjärjestyksen hyväksyminen Hyväksyttiin. 3. Edellisen kokouksen muistion hyväksyminen Hyväksyttiin. 4. Yhteistyökysymykset Mehiläinen Länsi-Pohja OY:n kanssa Klinikkakokoukset: - Operatiiviset ryhmät Kemissä, Keminmaassa ja Torniossa, mutta Ylitorniolla, Simossa ja Tervolassa ei ole vastaavia ryhmiä - Johtavien ja vastaavien lääkäreiden kokoukseen kutsutaan erikoisaloittain ylilääkärit keskustelemaan mutta riittääkö se. Tarvitaanko moniammatillisempi foorumi? - MLP:llä 3 viikon välein Paavo Uusimaan vetämänä ylilääkäreiden, vastaavien lääkäreiden ja palvelulinjajohtajien palaveri mutta sielläkään ei ole Ylitornion, Tervolan ja Simon edustusta. - Alueellista
    [Show full text]
  • LUETTELO Kuntien Ja Seurakuntien Tuloveroprosenteista Vuonna 2021
    Dnro VH/8082/00.01.00/2020 LUETTELO kuntien ja seurakuntien tuloveroprosenteista vuonna 2021 Verohallinto on verotusmenettelystä annetun lain (1558/1995) 91 a §:n 3 momentin nojalla, sellaisena kuin se on laissa 520/2010, antanut seuraavan luettelon varainhoitovuodeksi 2021 vahvistetuista kuntien, evankelis-luterilaisen kirkon ja ortodoksisen kirkkokunnan seurakuntien tuloveroprosenteista. Kunta Kunnan Ev.lut. Ortodoks. tuloveroprosentti seurakunnan seurakunnan tuloveroprosentti tuloveroprosentti Akaa 22,25 1,70 2,00 Alajärvi 21,75 1,75 2,00 Alavieska 22,00 1,80 2,10 Alavus 21,25 1,75 2,00 Asikkala 20,75 1,75 1,80 Askola 21,50 1,75 1,80 Aura 21,50 1,35 1,75 Brändö 17,75 2,00 1,75 Eckerö 19,00 2,00 1,75 Enonkoski 21,00 1,60 1,95 Enontekiö 21,25 1,75 2,20 Espoo 18,00 1,00 1,80 Eura 21,00 1,50 1,75 Eurajoki 18,00 1,60 2,00 Evijärvi 22,50 1,75 2,00 Finström 19,50 1,95 1,75 Forssa 20,50 1,40 1,80 Föglö 17,50 2,00 1,75 Geta 18,50 1,95 1,75 Haapajärvi 22,50 1,75 2,00 Haapavesi 22,00 1,80 2,00 Hailuoto 20,50 1,80 2,10 Halsua 23,50 1,70 2,00 Hamina 21,00 1,60 1,85 Hammarland 18,00 1,80 1,75 Hankasalmi 22,00 1,95 2,00 Hanko 21,75 1,60 1,80 Harjavalta 21,50 1,75 1,75 Hartola 21,50 1,75 1,95 Hattula 20,75 1,50 1,80 Hausjärvi 21,50 1,75 1,80 Heinola 20,50 1,50 1,80 Heinävesi 21,00 1,80 1,95 Helsinki 18,00 1,00 1,80 Hirvensalmi 20,00 1,75 1,95 Hollola 21,00 1,75 1,80 Huittinen 21,00 1,60 1,75 Humppila 22,00 1,90 1,80 Hyrynsalmi 21,75 1,75 1,95 Hyvinkää 20,25 1,25 1,80 Hämeenkyrö 22,00 1,70 2,00 Hämeenlinna 21,00 1,30 1,80 Ii 21,50 1,50 2,10 Iisalmi
    [Show full text]
  • Bird-Routes-In-Lapland.Pdf
    Olli-Pekka Karlin Markus Varesvuo which is a particularly good gathering place for waders during ture for the walks: 7386462.460939, which includes Vianaapa (bird Blue Route (Tornionjoki River Route, Road E8) the spring migration period. Immediately after Niskanperä, tower, 7384330:461931). This site is provided with a fine network of Tarsiger cyanurus Tarsiger ) road no. 4 crosses Kuolajokisuu (2), another gathering place paths and lean-to shelters. The distance from Rovaniemi to this site is ( Bluetail Red-flanked The Tornionjoki River Route starts from the northernmost tip of for waders during the spring migration period. The numbers of approx. 20 km. This is a site where species such as Three-toed Woo- the Gulf of Bothnia from TORNIO and proceeds northwards along birds at Niskanperä and Kuolajokisuu is affected by the presence dpecker (Picoides tridactylus), Rustic Bunting (Emberiza rustica), along Road E8 to Skibotn in Norway. The sediment-filled Alkunkarinlah- of sediments, which are dependent on floods and the regula- with many typical wetland species, nest. In the winter, a fine site for ti Bay is at the mouth of Tornionjoki River, and it is a significant tion of the river. The delta of Ounasjoki River 1( ; Koivusaari observing White-throated Dipper (Cinclus cinclus) in its element along Snow Bunting (Plectrophenax nivalis) nesting and gathering place for aquatic birds. There are two bird floating bird tower: 7377852:4437201) is an area where 150 Raudanjoki River is east of the village of Vikajärvi and road no. 4. The towers and lean-to shelters at this location (S: 7297826:372844; bird species have been recorded, and about half of them nest easiest way to do this is from the bridge on the road joining Vikajärvi N: 7298321:372614).
    [Show full text]
  • The Emigration from the Tornio Valley (Tornedalen)
    Swedish American Genealogist Volume 26 | Number 2 Article 5 6-1-2006 The miE gration from the Tornio Valley Sture Torikka Follow this and additional works at: https://digitalcommons.augustana.edu/swensonsag Part of the Genealogy Commons, and the Scandinavian Studies Commons Recommended Citation Torikka, Sture (2006) "The miE gration from the Tornio Valley," Swedish American Genealogist: Vol. 26 : No. 2 , Article 5. Available at: https://digitalcommons.augustana.edu/swensonsag/vol26/iss2/5 This Article is brought to you for free and open access by the Swenson Swedish Immigration Research Center at Augustana Digital Commons. It has been accepted for inclusion in Swedish American Genealogist by an authorized editor of Augustana Digital Commons. For more information, please contact [email protected]. The emigration from the Tornio Valley (Tornedalen) People left Sweden from all parts of the country, even the far north BY STURE TORIKKA The emigration to North America Stranded sailors of Norrbotten have for centuries from Norrbotten, in northern-most It happened sometimes: some people walked or skied to northern Norway Sweden, started in earnest during traveled to and fro and found it dif- in times of poverty. They had open the latter half of the 1870s. In the ficult to settle in one place. As early harbors without ice there, which Tornio River Valley (Tornedalen/ as 1858 the sailor Peter Tumber arri- made life easier than at home. When Tornionlaakso) the emigration per- ved in the port of New York, where the copper works started at Kåfjord haps did not start in earnest until the he mustered out and stayed when his in Northern Norway in the 1820s this 1880s.
    [Show full text]
  • Research Highlights
    [CLIENT] IsaaksdotterIsaacson1803 LEW160651 7 December 2018 Research Highlights GOALS Locate the birth records for three of the eleven children of Isaak Mickelsson and Magdalena Johansdotter (Carlsson) born 15 December 1796: Brita Isaaksdotter, Magdalena Isaaksdotter, and Mickel Isaaksson. (Their birth dates were listed in household records, which will significantly narrow searches for these records. However, locations for those births have yet to be determined. All available records should be used to identify locations for these events, and then applicable record collections searched.) Research the ancestry of Isaak Mickelsson born 2 August 1795 in Helsingby, in Hietaniemi Parish, Västerbotten County, Sweden. His parents are Mickel Johansson and Catharina Johansdotter who lived on Heicka farm. Research the ancestry of Magdalena Johansdotter born 12 December 1796 in Nuotioranta, Hietaniemi Parish, Västerbotten County, Sweden. Her parents were Johan Metsavainio (sic) and Caisa Nilsdotter. Research two recommendations from the January 12, 2017 Project, with the objective of determining who Maria is and where she belongs in the family: Determine who the father was of the young girl named Maria in the 1859 household of Erik Isaaksson and Anna Greta Isaaksdotter. Gather more information about the 1837 marriage of Johan Johansson and Brita Caisa, as listed in Johan’s 1845 household record. This may help explain the birth of the young girl named Maria who appeared later with Anna Gretta Isaaksdotter. If you get to this third objective, I have received additional information that may or may not be of benefit in the research of Maria. We have recently received some research notes written by my wife’s mother about 1970.
    [Show full text]
  • The Preliminary Flood Risk Assessment in Tornionjoki- Muonionjoki River Basin
    In cooperation with: The preliminary flood risk assessment in Tornionjoki- Muonionjoki river basin Table of Contents 1 Background .....................................................................................................................................3 2 Description of the river basin district...........................................................................................5 2.1 Hydrology .................................................................................................................................7 2.2 Population and land use ........................................................................................................ 12 2.3 Land use planning ................................................................................................................. 15 2.4 Protected areas and cultural heritage ................................................................................... 17 2.5 Flood protection and the use of the river basin ..................................................................... 19 3 Floods in history .......................................................................................................................... 21 3.1 Observed floods .................................................................................................................... 21 3.2 Estimation of effects caused by observed floods in present situation ................................... 26 4 Possible floods in future and flood risks .................................................................................
    [Show full text]
  • Legal Protection Schemes for Free-Flowing Rivers in Europe
    Legal Protection Schemes for Free-Flowing Rivers in Europe Overview report prepared for The Nature Conservancy 1 Published December 2019 Author: Tobias Schäfer Living Rivers Foundation www.living-rivers.eu Editing, Executive Summary & Map by Henrik Österblad The Nature Conservancy nature.org Special Acknowledgment to John Zablocki The Nature Conservancy 14b Rue de la Science 1040, Brussels Belgium Image Rights © Chip Carroon 2 Legal Protection Schemes for Free-Flowing Rivers in Europe Executive Summary The research for this report was guided by the aim of compiling a catalogue of rivers in Europe that enjoy a permanent legal comparable to a designation as Wild and Scenic River under the US Wild and Scenic Rivers Act from 1968. There has been no prior study comparatively addressing the question of strict legal protection of free-flowing rivers in Europe. Results & Observations Currently, there is no EU legislation which provides strict protection for the free-flowing character of rivers. The protection schemes which exist in Europe, to date, are found within national legislation. Legal protection for rivers that specifically aim at protecting their free-flowing character can be observed in Slovenia, Finland, Sweden, and Spain. At EU legislative level, the combined legal basis and mechanisms of the WFD and the Nature Directives (including Natura 2000 areas) render the designation of free-flowing rivers as protected in theory a possibility, if implemented for the purpose. Importantly however, in reality this is rarely the case, and the legal provisions do not fully rule out dam construction and hydropower development. The reporting obligations required by the Directives, and subsequent data available on Europe’s water bodies, do in turn provide a solid basis for envisioning such a strategy for strict river protection Europe-wide.
    [Show full text]
  • FINNISH STUDIES EDITORIAL and BUSINESS OFFICE Journal of Finnish Studies, Department of English, 1901 University Avenue, Evans 458 (P.O
    JOURNAL OF INNISH TUDIES F S Volume 19 Number 1 June 2016 ISSN 1206-6516 ISBN 978-1-937875-94-7 JOURNAL OF FINNISH STUDIES EDITORIAL AND BUSINESS OFFICE Journal of Finnish Studies, Department of English, 1901 University Avenue, Evans 458 (P.O. Box 2146), Sam Houston State University, Huntsville, TX 77341-2146, USA Tel. 1.936.294.1420; Fax 1.936.294.1408 SUBSCRIPTIONS, ADVERTISING, AND INQUIRIES Contact Business Office (see above & below). EDITORIAL STAFF Helena Halmari, Editor-in-Chief, Sam Houston State University; [email protected] Hanna Snellman, Co-Editor, University of Helsinki; [email protected] Scott Kaukonen, Assoc. Editor, Sam Houston State University; [email protected] Hilary Joy Virtanen, Asst. Editor, Finlandia University; hilary.virtanen@finlandia. edu Sheila Embleton, Book Review Editor, York University; [email protected] EDITORIAL BOARD Börje Vähämäki, Founding Editor, JoFS, Professor Emeritus, University of Toronto Raimo Anttila, Professor Emeritus, University of California, Los Angeles Michael Branch, Professor Emeritus, University of London Thomas DuBois, Professor, University of Wisconsin Sheila Embleton, Distinguished Research Professor, York University Aili Flint, Emerita Senior Lecturer, Associate Research Scholar, Columbia University Titus Hjelm, Reader, University College London Daniel Karvonen, Senior Lecturer, University of Minnesota, Minneapolis Andrew Nestingen, Associate Professor, University of Washington, Seattle Jyrki Nummi, Professor, Department of Finnish Literature, University of Helsinki Juha
    [Show full text]
  • Reitit Ja Ura T Merkkien Selitykset
    ROVANIEMI MERKKIEN SELITYKSET ! ROVANIEMI RANUAN KUNNAN KEMIJÄRVI YLLÄPITÄMILLÄ REITEILLÄ LÄHELLÄ KIRKONKYLÄÄ VOI ESIINTYÄ KOIRAVALJAKKOAKTIVITEETTEJÄ. 8 SHELL RANUA KOIRAVALJAKOT LIIKKUVAT KEMI 1 REITEILLÄ: SIMO KELKKAPARKKI / AUTOPARKKI II P RANUA - SIMO - RANUA - POSIO - SYÖTE AJA MALTILLA KOHDATESSASI POSIO TEBOIL RANUA 2 KOIRAVALJAKOT. SYÖTE RUKA 3 K-MARKET HILLAMARKET KELKKAPARKKI / OTTO- PISTE AUTOPARKKI P S-MARKET RANUA AUTOILLE POSTI RANUA POSIO 4 APTEEKKI REITIT JA URAT REITIT JA MOOTTORIKELKKA RANUA MOOTTORI 1 3 KESKUSGRILLI KUUSAMO KELKOILLE 2 RANUAN RANUANJÄRVI KELKKAURAT P HOTELLI ILVESLINNA 5 RAVINTOLA RANUAN LINJA-AUTOASEMA VIRALLISET KELKKAREITIT 4 5 6 6 ARCTIC GUESTHOUSE 9 & IGLOOS PÄÄSY RANUANJÄRVELLE SINISELTÄ URALTA HONKIVAARAAN PÄIN AJETTAESSA. 7 ARCTIC FOX IGLOOS 1 KILOMETRI KOHTI HONKIVAARAA ! JA UKONSUON POIKKEAMASTA KÄÄNNÖS VOIMAKAS VIRTAUS RANUA ZOO 8 WILD ARCTIC 1 : 30 000 RESTAURANT 7 #visitranua 500 M #gatewaytolapland HONKIVAARA PUDASJÄRVI TARVIKEKESKUS POSIO 9 KORJAAMO www.visitranua.fi Junttila / Marko Zoo Ranua Kuva: HEINISUO Kartta: MML,Kartta: HERE, METI / NASA, Garmin, Esri, USGS National Land Survey of Finland, Esri, HERE, Garmin, METI/NASA, USGS KUNNAT / KAUPUNGIT AUTOILLE OULU RANUAN SISÄISIÄ REITTEJÄ MOOTTORI- YLLÄPITÄÄ RANUAN KUNTA. TERVETULOA RANUALLE RUKA KELKOILLE 2 MUIDEN KUNTIEN REITTIEN ROVANIEMI YLLÄPITÄJÄT SELVIÄT KUNTIEN / 1 RANUA Ranua - tunnettu runsaista RANUAN KAUPUNKIEN SIVUILTA. hillasoistaan loppukesästä ja KELKKAURAT syksyllä. Talvella Ranua on lumen MIKÄLI HUOMAATTE PUUTTEITA
    [Show full text]
  • KLL Länsi-Pohja 2019
    KLL Länsi-Pohja 2019 P4 Pojat 4.lk 2 km V Sija Nimi Seura Loppuaika Ero 1. Juuso Korpi Ylitornio 8.08 2. Samuel Männikkö Tervola 8.09 0.01 2. Onni Hirsivaara Tornio 8.09 0.01 4. Niko Vestenius Kemi 8.16 0.08 5. Akseli Lamsijärvi Ylitornio 8.32 0.24 6. Niklas Järvenpää Kemi 8.39 0.31 7. Joel Karppinen Simo 8.45 0.37 7. Lassi Marttala Tornio 8.45 0.37 9. Anton Keskikallio Kemi 8.49 0.41 10. Emil Männikkö Tervola 8.55 0.47 11. Oliver Alatolonen Keminmaa 9.03 0.55 12. Ante Peltola Tervola 9.11 1.03 13. Olli Marttinen Keminmaa 9.28 1.20 14. Topias Uusimäki Ylitornio 9.30 1.22 15. Noel Ronkainen Keminmaa 9.42 1.34 16. Hannes Yliniva Ylitornio 10.37 2.29 17. Veeti Posti Simo 10.50 2.42 T4 Tytöt 4.lk 2 km V Sija Nimi Seura Loppuaika Ero 1. Lotta Rossi Simo 7.28 2. Silja Pekuri Kemi 7.44 0.16 3. Lotta Ukonaho Keminmaa 9.02 1.34 4. Enni Kulju Tornio 9.03 1.35 5. Helmi Niskala Tornio 9.13 1.45 6. Anni Karisaari Kemi 9.14 1.46 7. Ella Rajala Tervola 9.30 2.02 8. Venla Karjalainen Kemi 9.45 2.17 9. Eevi Hokkanen Tornio 9.49 2.21 10. Anni-Maija Keskimaunu Keminmaa 10.02 2.34 11. Saaga Anttila Keminmaa 10.07 2.39 12. Eedit Enbuske Simo 10.55 3.27 13. Peppiina Jansson Ylitornio 12.03 4.35 14.
    [Show full text]
  • Geochemical and U-Pb and Sm-Nd Isotopic Constraints on the Evolution of the Paleoproterozoic Ylitornio Nappe Complex, Northern Fennoscandia
    Bulletin of the Geological Society of Finland, Vol. 91, 2019, pp 75–100, https://doi.org/10.17741/bgsf/91.1.003 Geochemical and U-Pb and Sm-Nd isotopic constraints on the evolution of the Paleoproterozoic Ylitornio nappe complex, northern Fennoscandia Raimo Lahtinen1*, Hannu Huhma1, Laura S. Lauri2 and Mohammad Sayab1 1 Geological Survey of Finland, P.O. Box 96, FI-02151 Espoo, Finland 2 Geological Survey of Finland, P.O. Box 77, FI-96101 Rovaniemi,, Finland Abstract The Ylitornio area in northern Finland is a typical example of a poorly outcropping, multiply deformed, complex Precambrian terrain. U–Pb, Sm-Nd and geochemical data from metavolcanic, metasedimentary and plutonic rocks combined with structural data define the lithodemic units and tectonostratigraphy of the area. The Mellajoki, Martimo, Hosiojoki, Kierovaara and Uusivirka suites form the Yli- tornio nappe complex. Although main thrust stacking had occurred between 1.92– 1.89 Ga, later reverse faulting probably continued until 1.78 Ga. The Väystäjä bimodal volcanic rocks (2.09–2.05 Ga) from the Martimo suite are plume-related EMORB-OIB rocks formed during a continent breakup. The Kaskimaa greywacke of the Martimo suite is inferred to represent sedimentation in a deepening rift basin in the continental margin. The coeval Hosiojoki felsic rocks with A-type affinity and the Kierovaara suite granites (2.00–1.98 Ga) represent dry melting of a dominantly 2.1–2.05 Ga contaminated mafic underplate, and hydrous melting of both the mafic underplate and a refractory lower crust of Archean age, respectively. The older rocks of the Uusivirka suite are early-collisional (1.92–1.91 Ga) and derived from poorly mixed local sources, whereas younger psammite-pelite associations (Ristivuoma) are syn-collisional (1.91– 1.89 Ga) and derive from multiply recycled and thoroughly mixed sources.
    [Show full text]