DOCSLIB.ORG

Till Geochemical Research in the Savukoski- Pelkosenniemi Region

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Till Geochemical Research in the Savukoski- Pelkosenniemi Region GEOLOGICAL SURVEY OF FINLAND Northern Finland Office Rovaniemi 7.5.2014 58/2014 Till geochemical research in the Savukoski- Pelkosenniemi region Pertti Sarala GEOLOGIAN TUTKIMUSKESKUS 58/2014 7.5.2014 GEOLOGICAL SURVEY OF FINLAND DESCRIPTION Date/ Dnro 7.5.2014 Author Report type Pertti Sarala Final report Ordered by GTK Name Till geochemical research in the Savukoski-Pelkosenniemi region Abstract The Geological Survey of Finland (GTK) in co-operation with the NATI Research Oy carried out Quaternary geological re- search in the Savukoski-Pelkosenniemi region in eastern Finnish Lapland in 2012-2013. The aim of the project was to test the CROCS technology of NATI in a regional mineral potential mapping when the glacial till samples were used. 102 till samples with about 3-5 km sampling interval were collected as a part of GTK’s own sampling programme. Test pits and soil drilling were used to collect the till samples from a basal part of the glaciogenic overburden, near the bedrock surface. In this report, the results of conventional till geochemistry (<0.06 mm sieved size fraction analysed by ICP-OES after aqua regia digestion) made by GTK is presented. The results prove the study area to be potential for several base metals like chromium and nickel together with gold and PGE. Results of the CROCS technology application by NATI were presented in the sepa- rate, appended report (http://www.natires.com/rrs2013-1.htm, referred 7th May 2014). Keywords Geochemistry, till, heavy minerals, exploration, CROCS technology Geography (country, province, municipality, village, occurrence etc.) Finland, Lapland, Pelkosenniemi, Savukoski Map sheet Other information Name of the report serie Archive code Archive report 58/2014 Page numbers Language Price Publicity 10 p. English - Public Unit and department Project code Northern Office, Bedrock geology and Resources 7780031 Signature Signature Pertti Sarala GEOLOGICAL SURVEY OF FINLAND 58/2014 7.5.2014 Content DESCRIPTION 1 INTRODUCTION 1 2 BEDROCK 2 3 QUATERNARY GEOLOGY 2 4 METHODS 2 5 RESULTS 3 6 DISCUSSION AND CONCLUSIONS 9 7 REFERENCES 9 GEOLOGICAL SURVEY OF FINLAND 58/2014 1 1 INTRODUCTION Geological Survey of Finland (GTK) and NATI Research Ltd. carried out a small methodological testing of the CROCS technology in Häme region, southern Finland in 2011 (Knauf 2012). The test was related to gold potential mapping of the area nearby Tammela. That project rose up an idea to continue method- ology testing in a regional scale in some other study area of GTK. The area in Savukoski-Pelkosenniemi, eastern Finnish Lapland was chosen for a new project area. This project included both a conventional till geochemical research done by GTK and the methodological testing of the CROCS technology done by NATI Research Oy. For the sample material of the research GTK collected 102 basal till samples from the whole study area (Fig. 1) as a part of GTK’s own sampling programme. The sampling was carried out in 2012-2013. The aim of the GTK’s own programme was to collect till and bedrock samples from the area to study geochemical and lithological features of the area to estimate mineral exploration potential of the area. GTK’s sampling point network was planned based on earlier geological knowledge and Quaternary maps of the study area. Analyse and interpretation results were not applied to verify during this project. Fig. 1. Location of the Savukoski-Pelkosenniemi study area in eastern Finland. Till sampling points used for collecting samples in this study are also presented on the bedrock map 1:200 000 after GTK. GEOLOGICAL SURVEY OF FINLAND 58/2014 2 2 BEDROCK Bedrock in the study area consists of both Achaean and Proterotzoic rocks and the contact zone between them (Fig. 1). Archaean rocks in the eastern part are mainly composed of granite gneiss and some mafic volcanic rocks (Juopperi 1986). They are a part of 2.5-3.0 Ga old the Tuntsa Suite that are existing in eastern Lapland. In the western part of the study area, quartzites, mica schicts, diabase veins and some mafic rocks of the 2.0-2.4 Ga old Savukoski Group exist. The narrow chain of komatites and mafic vol- canic rocks with some mica schists are following the contact of Archaean and Proterotzoic rocks almost in north-south orientation through the area. In south-eastern corner of the study area situates the Akan- vaara layered intrusion of 2.44 Ga in age. It includes chromium mineralization that was studied in many phases over decades (Mutanen 1997). Rocks in the whole study area are strongly deformed and faulted, and metamorphosed in the amphibolite facies. The bedrock is largely pre-glacially weathered having sev- eral metres thick partly or totally softened saprolite of saprock surface. In places weathering has been ef- fective and as a consequence of it kaolinite is found in the bedrock. 3 QUATERNARY GEOLOGY The study area locates on southern side of the last ice-divide zone of the Late Weichselian glaciation (Jo- hansson et al. 2011). Ice flow direction has been mainly from north-west to south-east. After strong gla- cial events, glaciogenic overburden composed mainly on sandy till covers the bedrock dominantly in the area. Only the tops of the highest hills are covered by the block fields of frost-weathered bedrock. In low land areas peat deposits are common and cover till layers. There is one glaciofluvial esker system that crosses the area in northwest-southeast direction in the central part of the study area. Post-glacial river sands and silts are common in the Kemijoki River valley. Based on test pit, soil and percussion drilling data the thickness of overburden varies generally 2-5 m, but in topographic depressions and in the river valleys it can reached up to 50 m. 4 METHODS Till samples were collected using the test pits and soil drillings (Table 1). Totally 102 sampling points were used to collect basal till samples. The samples were stratigraphy controlled and the sampling depth has been about one meter above bedrock surface from the bottommost till bed. This sampling strategy was supposed to produce most homogeneous sampling material where the till samples represents most uniform glacial transport and deposition processes. In this project two types of till samples were used: a) c. 250-350 g for conventional till geochemistry (used in GTK) and b) c. 5 litres, i.e. 7-10 kg that were sent to NATI for the CROCS technology applica- tion. Conventional till samples were dried (70°C) and sieved (<0.063 mm) before digesting subsample (5 g) using aqua regia. After that they were analysed by ICP-OES and ICP-MS for 41 elements (method 515PM) and GFAAS for gold and palladium (method 521U) in the Labtium laboratory (Labtium order 47506). The 5 litres samples were sent to NATI’s laboratory and they were processed as described in the appended report (http://www.natires.com/rrs2013-1.htm, referred 7th May 2014). Analysis includes both geochemical and mineralogical component of the concentrated till samples. Furthermore, two concentrate GEOLOGICAL SURVEY OF FINLAND 58/2014 3 fractions processed by NATI (so called heavy fraction, HF, and fine fraction, FF)) were analysed in the Labtium laboratory (ordered by GTK) using the same methods as were used for the conventional geo- chemistry (Labtium orders 47526, 47527, 47559, 47560). Table 1. List of the test pits (POS$) and soil drilling points (JOV$, HAH1) in the study area. ID X Y ID X Y ID X Y POS$-2012-32 7482752 3543117 POS$-2012-69 7467269 3537423 POS$-2012-101 7457560 3530477 POS$-2012-33 7480340 3540302 POS$-2012-70 7465661 3537083 POS$-2012-102 7457315 3528891 POS$-2012-34 7479798 3542003 POS$-2012-71 7467479 3535087 JOV$-2012-6 7472347 3546733 POS$-2012-35 7476389 3541291 POS$-2012-72 7464888 3535453 JOV$-2012-11 7465610 3558102 POS$-2012-36 7473123 3544537 POS$-2012-73 7463151 3536255 JOV$-2012-12 7466073 3559059 POS$-2012-37 7470752 3546907 POS$-2012-74 7459880 3545694 JOV$-2012-13 7465452 3546656 POS$-2012-38 7484402 3543362 POS$-2012-75 7463166 3543380 JOV$-2012-15 7463763 3549852 POS$-2012-39 7483518 3557411 POS$-2012-76 7461597 3539822 JOV$-2012-20 7460850 3547449 POS$-2012-41 7479072 3555644 POS$-2012-77 7455512 3556675 JOV$-2013-1 7451950 3524536 POS$-2012-42 7478984 3558074 POS$-2012-77 7455512 3556675 JOV$-2013-2 7452523 3526181 POS$-2012-43 7476607 3554298 POS$-2012-78 7457812 3557228 JOV$-2013-9 7456037 3528345 POS$-2012-44 7476817 3556085 POS$-2012-79 7458614 3556922 JOV$-2013-10 7455004 3529072 POS$-2012-45 7476980 3559272 POS$-2012-80 7455262 3558193 JOV$-2013-11 7455062 3531218 POS$-2012-46 7472567 3558748 POS$-2012-81 7451960 3557399 JOV$-2013-12 7456647 3531851 POS$-2012-47 7470007 3557788 POS$-2012-82 7451133 3558767 JOV$-2013-13 7458829 3532873 POS$-2012-48 7471499 3553502 POS$-2012-83 7451331 3549586 JOV$-2013-14 7458762 3536063 POS$-2012-49 7473784 3552914 POS$-2012-84 7452163 3548697 JOV$-2013-15 7459714 3537561 POS$-2012-50 7476593 3552171 POS$-2012-85 7457505 3550868 JOV$-2013-16 7456389 3541663 POS$-2012-51 7480740 3552881 POS$-2012-86 7458087 3546217 JOV$-2013-17 7455285 3541079 POS$-2012-52 7469263 3545549 POS$-2012-87 7455518 3544999 JOV$-2013-19 7451074 3533182 POS$-2012-53 7486541 3552752 POS$-2012-88 7455115 3543679 JOV$-2012-25 7458680 3547760 POS$-2012-54 7482638 3550369 POS$-2012-89 7453487 3541931 JOV$-2012-27 7458118 3553907 POS$-2012-55 7481187 3550502 POS$-2012-89 7453487 3541931 JOV$-2012-28 7459784 3554270 POS$-2012-56 7486329 3544600 POS$-2012-90 7452456 3540935 JOV$-2012-34 7466725 3542437 POS$-2012-57 7485124 3548940 POS$-2012-91 7455549 3533589 JOV$-2012-40
Load more

Recommended publications
  • Discover Pyhä-Luosto
    DISCOVER PYHÄ-LUOSTO AND SURROUNDINGS SODANKYLÄ PELKOSENNIEMI 1 THE OLD CHURCH 22 SUVANTO VILLAGE 2 THE CHURCH OF SODANKYLÄ 23 THE ANDY MCCOY STATUE 3 LOCAL HERITAGE MUSEUM 24 JAAKKOLA LOG HOUSE CAFÉ 4 MUSEUM-GALLERY ALARIESTO 25 LUCKY RANCH 5 PAPPILANNIEMI NATURE PATH 26 KAIRANKUTSU – CALL OF THE WILDERNESS 6 KOMMATTI DISCGOLFPARK 7 AURORA HOUSE – THE HOUSE KEMIJÄRVI OF THE NORTHERN LIGHTS 27 ART STUDIO PMH 8 NILIMELLA – BEACH 28 KEMIJÄRVI CHURCH, THE OLD BELL TOWER AND 9 SAVIKANGAS – BEACH PINE-FLOGGING SPOT 29 ART CENTER PUUSTELLI PYHÄ-LUOSTO 30 KEMIJÄRVI REGIONAL MUSEUM 10 LUOSTO DISCGOLFPARK 31 SPA – SWIMMING POOL POUKAMA 11 AHVENLAMPI, LUOSTO 32 BEACH 12 BEACH – AARNILAMPI 33 KEMIJÄRVI DISC GOLF RANGE 13 THE AMETHYST MINE, LUOSTO 34 KOTAVAARA OBSERVATION TOWER 14 OUTINEN RIDING CENTRE 15 THE CHAPEL OF THE NORTHERN LIGHTS, PYHÄ 16 AITTAKURU GORGE, PYHÄ 17 VISITOR CENTRE NAAVA, PYHÄ 18 ISOKURU GORGE, PYHÄ 19 PYHÄ SCENIC CHAIR LIFT 20 PYHÄ DISC GOLF RANGE 21 BEACH - ASTELINRANTA 2 4 80 SODANKYLÄ 7 1-6, 8-9 5 Välisuvanto E63 10,11 Kitinen Torvinen 24 22 Luosto PYHÄ-LUOSTO NATIONAL PARK Suvanto 23 Kemijoki Luosto changes. reserve the rights to make We 13 PELKOSENNIEMI Vuojärvi 25 < TO ROVANIEMI Pyhätunturi Pyhätunturi 4 19,20 E75 18 15-17 Kemijoki Javarusjoki 5 14 27-33 82 TO SALLA > 5 E63 34 < TO ROVANIEMI KEMIJÄRVI TO KUUSAMO > Vikajärvi Kemijärvi 3 DESTINATIONS IN 2 THE CHURCH OF SODANKYLÄ The main church of Sodankylä was built in 1859, SODANKYLÄ: and it was built out of locally-sourced stone. The SODANKYLÄ TOURIST INFORMATION altarpiece of ”Christ the comforter” was painted Jäämerentie 3 by Artturi Heickel in 1912.
    [Show full text]
  • The Dispersal and Acclimatization of the Muskrat, Ondatra Zibethicus (L.), in Finland
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Wildlife Damage Management, Internet Center Other Publications in Wildlife Management for 1960 The dispersal and acclimatization of the muskrat, Ondatra zibethicus (L.), in Finland Atso Artimo Suomen Riistanhoito-Saatio (Finnish Game Foundation) Follow this and additional works at: https://digitalcommons.unl.edu/icwdmother Part of the Environmental Sciences Commons Artimo, Atso, "The dispersal and acclimatization of the muskrat, Ondatra zibethicus (L.), in Finland" (1960). Other Publications in Wildlife Management. 65. https://digitalcommons.unl.edu/icwdmother/65 This Article is brought to you for free and open access by the Wildlife Damage Management, Internet Center for at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Other Publications in Wildlife Management by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. R I 1ST A TIE T L .~1 U ( K A I S U J A ,>""'liSt I " e'e 'I >~ ~··21' \. • ; I .. '. .' . .,~., . <)/ ." , ., Thedi$perscdQnd.a~C:li"'dti~otlin. of ,the , , :n~skret, Ond~trq ~ib.t~i~',{(.h in. Firtland , 8y: ATSO ARTIMO . RllSTATIETEELLISljX JULKAISUJA PAPERS ON GAME RESEARCH 21 The dispersal and acclimatization of the muskrat, Ondatra zibethicus (l.), in Finland By ATSO ARTIMO Helsinki 1960 SUOMEN FIN LANDS R I 1ST A N HOI T O-S A A T I b ] AK TV ARDSSTI FTELSE Riistantutkimuslaitos Viltforskningsinstitutet Helsinki, Unionink. 45 B Helsingfors, Unionsg. 45 B FINNISH GAME FOUNDATION Game Research Institute Helsinki, Unionink. 45 B Helsinki 1960 . K. F. Puromichen Kirjapaino O.-Y. The dispersal and acclimatization of the muskrat, Ondatra zibethicus (L.), in Finland By Atso Artimo CONTENTS I.
    [Show full text]
  • Sm–Nd and U–Pb Isotope Geochemistry of the Palaeoproterozoic Mafic Magmatism in Eastern and Northern Finland
    Geological Survey of Finland GeologicalGeological SurveySurvey ofof FinlandFinland 2018 Sm–Nd and U–Pb isotope geochemistry of the Palaeoproterozoic mafic magmatism in eastern and northern Finland Hannu Huhma, Eero Hanski, Asko Kontinen, Jouni Vuollo, Irmeli Mänttäri and Yann Lahaye Bulletin 405 • Monograph Geological Survey of Finland, Bulletin The Bulletin of the Geological Survey of Finland publishes the results of scientific research that is thematically or geographically connected to Finnish or Fennoscandian geology, or otherwise related to research and innovation at GTK. Articles by researchers outside GTK are also welcome. All manuscripts are peer reviewed. Editorial Board Prof. Pekka Nurmi, GTK, Chair Dr Stefan Bergman, SGU Dr Asko Käpyaho, GTK Dr Antti Ojala, GTK Dr Timo Tarvainen, GTK, Scientific Editor Instructions for authors available from the Scientific Editor. GEOLOGICAL SURVEY OF FINLAND Bulletin 405 Sm–Nd and U–Pb isotope geochemistry of the Palaeoproterozoic mafic magmatism in eastern and northern Finland by Hannu Huhma, Eero Hanski, Asko Kontinen, Jouni Vuollo, Irmeli Mänttäri and Yann Lahaye Unless otherwise indicated, the figures have been prepared by the authors of the publication. Layout: Elvi Turtiainen Oy Espoo 2018 Huhma, H.1) , Hanski, E.2), Kontinen, A.3), Vuollo, J.4), Mänttäri, I.1) & Lahaye, Y.1) 2018. Sm–Nd and U–Pb isotope geochemistry of the Palaeoproterozoic mafic magmatism in eastern and northern Finland. Geological Survey of Finland, Bulletin 405, 150 pages, 128 figures, 1 table and 11 appendices. The extensive isotopic studies performed at the Geological Survey of Finland (GTK) since the early 1970s have shown that mafic magmas in the Karelia province of the Fennoscandian Shield were emplaced in several stages, including ca.
    [Show full text]
  • ELY-Keskuksen Lappiin Myöntämä Rahoitus
    1 (19) ELY-keskuksen myöntämä rahoitus Lapin maakuntaan 1.1.–30.6.2017 Strateginen valinta: Kilpailukykyä ja työtä avoimessa ja arktisessa Lapissa Hakija Kunta Rahoitus / tukimuoto Hankkeen nimi Tukimäärä, Tuki- € prosentti, % GTK, Luonnonvarakeskus, Kolari, Kittilä, Sodankylä, EAKR TL 2 Tutkimus-, Biohiilen hyödyntäminen 597 739 80 Oulun yliopisto Rovaniemi osaamis- ja kaivannaisjätteiden innovaatiokeskittymien peittomateriaaleissa ja kehittäminen alueellisten viherrakentamisessa - Biopeitto vahvuuksien pohjalta Kemi-Torniolaakson EAKR TL 2 Tutkimus-, Maatilat biokaasun tuottajina Lapissa 217 150 80 koulutuskuntayhtymä Lappia osaamis- ja innovaatiokeskittymien kehittäminen alueellisten vahvuuksien pohjalta LUKE, Arctic Warrioirs Oy, Rovaniemi EAKR TL 2 Tutkimus-, Laatusormenjälki arktiselle luonnon 362 726 80 Detria Oy osaamis- ja raaka-aineelle (Arctic FingerPrint) innovaatiokeskittymien kehittäminen alueellisten vahvuuksien pohjalta Luonnonvarakeskus Oulu, Kempele, Tyrnävä, EAKR TL 2 Tutkimus-, Taimistopohjoinen, Pohjois-Suomen 216 952 80 Oulun yliopisto Raahe, Kittilä, Tervola, osaamis- ja taimistotuotannon kehittäminen Oulun seudun Kemi, Sodankylä, Simo innovaatiokeskittymien koulutuskuntayhtymä kehittäminen alueellisten 2 (19) Kemi-Tornionlaakson vahvuuksien pohjalta koulutuskuntayhtymä Lappia, Ammattiopisto Lappia Oulun yliopisto Geologian Rovaniemi, Oulu, Sotkamo, EAKR TL 2 Tutkimus-, DROMINÄ - Dronet mittauksessa ja 43 359 80 tutkimuskeskus Kajaani osaamis- ja näytteenotossa Suomen ympäristökeskus innovaatiokeskittymien kehittäminen
    [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]
  • Lapin Maakunnallisesti Tärkeät Lintualueet
    LAPIN MAAKUNNALLISESTI TÄRKEÄT LINTUALUEET MAALI-hankkeen loppuraportti Lapin Lintutieteellinen Yhdistys ry 2016 LAPIN MAAKUNNALLISESTI TÄRKEÄT LINTUALUEET Lapin maakunnallisesti tärkeät lintualueet MAALI-hankkeen loppuraportti Lapin lintutieteellinen yhdistys LLY ry www.lly.fi 2016 Raportin laatija: Veikko Isomursu Taitto ja kuvat: Olli-Pekka Karlin Alueiden rajaukset: Olli-Pekka Karlin, Antti Ruonakoski Pohjakartat © Maanmittauslaitos 2013 2 LAPIN MAAKUNNALLISESTI TÄRKEÄT LINTUALUEET Yhteistyössä 3 LAPIN MAAKUNNALLISESTI TÄRKEÄT LINTUALUEET Sisällysluettelo 6 1 Johdanto 60 920280 Kittilä, Nälkäjärvi 6 2 Toteutus Lapissa 61 920284 Kolari, Kurtakkojärvi 7 3 Kohteiden valinta 62 920367 Kolari, Rautuvaaran altaat 7 4 Kiitokset 63 920368 Kolari, Ylläslompolo 8 5 Kohteiden valintakriteerit 64 920477 Kolari, Äkäslompolo 9 6 Kohdeluettelo 65 920373 Muonio, Jerisjärvi 10 7 Lintualueet 66 920372 Muonio, Muonionjärvi 7.1 Kulttuuriympäristöt 67 920345 Pelkosenniemi, Arvosjoki 10 920461 Kemijärvi, Kostamo 68 920346 Pelkosenniemi, Säynäjäjärvi 11 920462 Kemijärvi, Oinas 69 920364 Pello, Orajärvi 12 920434 Kemijärvi, Räisälä 70 920230 Pello, Paamajärvi 13 920369 Kolari, Myllymaan pellot 71 920010 Pellojärvi-Säynäjäjärvi 14 920366 Pello, Turtolan pellot 72 920291 Posio, Kynsijärven Alaperä- 15 920365 Pello, Yliranta-Poikkihaka Kynsilampi-Kynsijoki 16 920330 Ranua, Marikkosuo 73 920289 Ranua, Kuhajärvi 17 920456 Rovaniemi, Niskanperän pellot 74 920157 Ranua, Portimojärvi 18 920315 Rovaniemi, Matinmikonperän pellot 75 920290 Ranua, Roosinginjärvi 19 920327
    [Show full text]
  • Late Weichselian and Holocene Shore Displacement History of the Baltic Sea in Finland
    Late Weichselian and Holocene shore displacement history of the Baltic Sea in Finland MATTI TIKKANEN AND JUHA OKSANEN Tikkanen, Matti & Juha Oksanen (2002). Late Weichselian and Holocene shore displacement history of the Baltic Sea in Finland. Fennia 180: 1–2, pp. 9–20. Helsinki. ISSN 0015-0010. About 62 percent of Finland’s current surface area has been covered by the waters of the Baltic basin at some stage. The highest shorelines are located at a present altitude of about 220 metres above sea level in the north and 100 metres above sea level in the south-east. The nature of the Baltic Sea has alter- nated in the course of its four main postglacial stages between a freshwater lake and a brackish water basin connected to the outside ocean by narrow straits. This article provides a general overview of the principal stages in the history of the Baltic Sea and examines the regional influence of the associated shore displacement phenomena within Finland. The maps depicting the vari- ous stages have been generated digitally by GIS techniques. Following deglaciation, the freshwater Baltic Ice Lake (12,600–10,300 BP) built up against the ice margin to reach a level 25 metres above that of the ocean, with an outflow through the straits of Öresund. At this stage the only substantial land areas in Finland were in the east and south-east. Around 10,300 BP this ice lake discharged through a number of channels that opened up in central Sweden until it reached the ocean level, marking the beginning of the mildly saline Yoldia Sea stage (10,300–9500 BP).
    [Show full text]
  • Lomakuljetusten Aikataulut
    LOMAKULJETUSTEN AIKATAULUT ASEVELVOLLISTEN LOMAMATKAKULJETUKSET JÄÄKÄRIPRIKAATI SODANKYLÄ (LÄHTÖAIKA KLO 14:00) AIKATAULU REITTI N:O 2 Sodankylä - Savukoski - Salla - Hautajärvi - Ruka - Kuusamo klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 22.30 15.00 Savukoski Samperin Sav. la-pys. 21.00 15.55 Salla Torin laita 19.50 17.30 Hautajärvi tienhaara 19.10 18.00 Ruka vt 5 pysäkki 18.40 18.30 Kuusamo las 18.20 2 (7) AIKATAULU REITTI N:O 3 Sodankylä - Pelkosenniemi - Kemijärvi - Posio - Taivalkoski klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 22.30 14.50 Pelkosenniemi SEO 21.40 15.30 Kemijärvi ABC-asema 21.00 15.55 Joutsijärvi Sallan tienhaara 20.20 17.30 Posio ST1-asema 19.10 18.30 Taivalkoski TB-Koillistie 18.00 3 (7) AIKATAULU REITTI N:O 4 Sodankylä - Kittilä - Ylläs - Kolari - Pello - Ylitornio -Tornio klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 22.30 14.50 Tepsa 21.40 15.20 Kittilä Neste 21.00 15.50 Ylläs, Eelin kaupan pysäkki 20.20 16.20 Kolari, Neste 19.50 17.30 Pello, SEO-huoltamo 19.00 18.20 Ylitornio SEO-asema 18.10 19.10 Tornio Green Line 17.20 4 (7) AIKATAULU REITTI NRO 5 Sodankylä - Kittilä - Muonio - Palojoensuu - Enontekiö klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 22.30 16.30 Muonio SEO 19.40 17.25 Palojoensuu vt pysäkki 19.00 17.45 Hetta Grilli 18.40 5 (7) AIKATAULU REITTI NRO 6 Sodankylä - Ivalo klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 20.00 Ivalo Las 6 (7) AIKATAULU REITTI N:O 7 Sodankylä - Rovaniemi - Keminmaa - Kemi klo km Kohdepaikkakunta Paluuaika 14.00 VK kas 6 piha 22.30 Roi lento-as n.
    [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]
  • Muuttajan Opas
    1 22.3.2018 MOVER’S GUIDE Kemijärven kaupunki PL 5 FI-98100 Kemijärvi FINLAND KEMIJARVI.FI 2 22.3.2018 Contents NORTHERNMOST CITY OF FINLAND................................................................................................................................. 3 KEMIJÄRVI BUSINESS SERVICES ...................................................................................................................................... 4 DISTANCES......................................................................................................................................................................................... 5 CUSTOMER SERVICE COUNTER SORTTEERI ............................................................................................................ 7 KEMIJÄRVI TOURIST INFO ....................................................................................................................................................... 7 KEMIJÄRVI CITY ADMINISTRATIVE COURT .................................................................................................................. 8 POST OFFICE K-SUPERMARKET KEMIJÄRVI .............................................................................................................. 8 KOILLIS-LAPIN SÄHKÖ (ELECTRICITY PLANT) ........................................................................................................... 8 KEMIJÄRVEN LÄMPÖ- JA VESI (HEAT AND WATER) .............................................................................................. 9 WASTE MANAGEMENT
    [Show full text]
  • DRAINAGE BASIN of the BALTIC SEA Chapter 8
    216 DRAINAGE BASIN OF THE BALTIC SEA Chapter 8 BALTIC SEA 217 219 TORNE RIVER BASIN 221 KEMIJOKI RIVER BASIN 222 OULUJOKI RIVER BASIN 223 JÄNISJOKI RIVER BASIN 224 KITEENJOKI-TOHMAJOKI RIVER BASINS 224 HIITOLANJOKI RIVER BASIN 226 VUOKSI RIVER BASIN 228 LAKE PYHÄJÄRVI 230 LAKE SAIMAA 232 JUUSTILANJOKI RIVER BASIN 232 LAKE NUIJAMAANJÄRVI 233 RAKKOLANJOKI RIVER BASIN 235 URPALANJOKI RIVER BASIN 235 NARVA RIVER BASIN 237 NARVA RESERVOIR 237 LAKE PEIPSI 238 GAUJA/KOIVA RIVER BASIN 239 DAUGAVA RIVER BASIN 241 LAKE DRISVYATY/ DRUKSHIAI 242 LIELUPE RIVER BASIN 245 VENTA, BARTA/BARTUVA AND SVENTOJI RIVER BASINS 248 NEMAN RIVER BASIN 251 LAKE GALADUS 251 PREGEL RIVER BASIN 254 VISTULA RIVER BASIN 260 ODER RIVER BASIN Chapter 8 218 BALTIC SEA This chapter deals with major transboundary rivers discharging into the Baltic Sea and some of their transboundary tributaries. It also includes lakes located within the basin of the Baltic Sea. TRANSBOUNDARY WATERS IN THE BASIN OF THE BALTIC SEA1 Basin/sub-basin(s) Total area (km²) Recipient Riparian countries Lakes in the basin Torne 40,157 Baltic Sea FI, NO, SE Kemijoki 51,127 Baltic Sea FI, NO, RU Oulujoki 22,841 Baltic Sea FI, RU Jänisjoki 3,861 Lake Ladoga FI, RU Kiteenjoki-Tohmajoki 1,595 Lake Ladoga FI, RU Hiitolanjoki 1,415 Lake Ladoga FI, RU Lake Pyhäjärvi and Vuoksi 68,501 Lake Ladoga FI, RU Lake Saimaa Juustilanjoki 296 Baltic Sea FI, RU Lake Nuijamaanjärvi Rakkonlanjoki 215 Baltic Sea FI, RU Urpanlanjoki 557 Baltic Sea FI, RU Saimaa Canal including 174 Baltic Sea FI, RU Soskuanjoki Tervajoki 204
    [Show full text]
  • The Fourth Periodic Report of Finland on the Application of the European Charter for Regional Or Minority Languages
    THE FOURTH PERIODIC REPORT OF FINLAND ON THE APPLICATION OF THE EUROPEAN CHARTER FOR REGIONAL OR MINORITY LANGUAGES SEPTEMBER 2010 Table of Contents INTRODUCTION .................................................................................................................................................. 1 GENERAL PART ................................................................................................................................................... 3 1. BASIC INFORMATION ON FINLAND ................................................................................................................................. 3 Population, religion and languages ........................................................................................................................................ 3 Special status of the Åland Islands ......................................................................................................................................... 3 2. REGIONAL OR MINORITY LANGUAGES IN FINLAND ........................................................................................................ 4 Swedish .................................................................................................................................................................................. 4 Sámi ....................................................................................................................................................................................... 4 3. NUMBERS OF PERSONS SPEAKING REGIONAL
    [Show full text]