Sami on the Stages and in the Zoos of Europe
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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). -
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. -
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. -
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 ................................................................................. -
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 -
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. -
Working with Traditional Knowledge: Communities, Institutions, Information Systems, Law and Ethics
Dieđut 1/2011 Working with Traditional Knowledge: Communities, Institutions, Information Systems, Law and Ethics Writings from the Arbediehtu Pilot Project on Documentation and Protection of Sami Traditional Knowledge Edited by Jelena Porsanger Gunvor Guttorm Sámi allaskuvla / Sámi University College Working with Traditional Knowledge: Communities, Institutions, Information Systems, Law and Ethics Acknow ledge ments Many individuals, local Sami com mu nities and institutions have contri buted to the Árbediehtu pilot project in the period from 2008 to 2011. One of the important objectives of the project has been to listen to and take into account what Sami people expect from the work on documentation and protection of their traditional know ledge. Special gratitude is owed to communities and individuals in the Norwegian, Swedish and Finnish parts of Sápmi, who eagerly participated in community meetings and other project activities. Sami communities have been important partners in the project, which would not have been possible without their support, collabo ration and genuine interest. We are grateful to the communities and all individual árbečeahpit (tradition- bearers) in the following places: In the Coastal Sami area c/o the Sea Sami Centre of Expertise: Jáhkovuotna/Kokelv, Čuđegieddi/Kistrand, Billávuotna/Bille fjord, Cuop pogieddi/Sandvik, Jovnnanjárga/Jonsnes, Ráigešája/Igeldas, Rávt toš njárga/Stabbursnes, Leavdnja/Lakselv, Breannjá/Brenna, Keaisa/Kjæs. In the Lule Sami area c/o the Árran – Lule Sami Centre: Ájluokta/Drag, Gásluokta/Kjøps vik, Ájládde/Hellands berg, Måsske/Musken, Vuodnabahta/Hellemobotn. In the Northern Sami area c/o the museum association RiddoDuottarMuseat: Kárášjohka/Karasjok, Näkkälä järvi, Áidejávri, Guovdageaidnu/ Kauto keino. In the Southern Sami area c/o Saemien Sijte (South Sami Museum and Cultural Centre): The following reindeer herding communities: Luvlie-Nåamesjen Båatsoe/Østre Namdal, Åarjel-Njaarke/Vestre Namdal, Fovsen-Njaarke/Fosen, Låarte/Luru, and Trollheimen Sijte. -
Indigenous Internal Selfdetermination in Australia and Norway
i Indigenous internal self-determination in Australia and Norway by Pia Solberg A thesis in fulfillment of the requirements for the degree of Doctor of Philosophy School of Humanities & Languages Faculty of Arts & Social Sciences The University of New South Wales October 2016 iv Table of Contents Acknowledgments.........................................................................................................vii Language and terminology.............................................................................................ix Abstract..........................................................................................................................x Introduction.................................................................................................................11 Approaches to the problem.............................................................................13 Why compare with Norway and the Sami?.....................................................17 My approach..................................................................................................20 The structure of this thesis..............................................................................24 PART ONE: HISTORY MATTERS.............................................................................26 Chapter One. Early Colonisation...........................................................................27 Introduction........................................................................................................27 Sapmi: -
Kemin, Karungin, Simon Ja Runkauksen Kartta-Alueiden Kalliopera
WOMEN GEOLOGINEN KARTTA 1 : 100 000 GEOLOGICAL MAP OF FINLAND 1 : 100 000 KALLIOPERAKARTTOJEN SELITYKSET LEHDET 2541, 2542 + 2524, 2543 ja 2544 EXPLANATION TO THE MAPS OF SHEETS 2541, 2542+2524, 2543 and 2544 PRE-QUATERNARY ROCKS Vesa Perttunen Kemin, Karungin, Simon ja Runkauksen kartta-alueiden kalliopera Summary : Pre-Quaternary rocks of the Kemi, Karunki, Simo and Runkaus map-sheet areas GEOLOGIAN TUTKIMUSKESKUS GEOLOGICAL SURVEY OF FINLAND ESPOO 1991 SUOMEN GEOLOGINEN KARTTA - GEOLOGICAL MAP OF FINLAND 1 : 100 000 Kallioperakarttojen selitykset Lehdet 2541, 2542+2524, 2543 j a 2544 Explanation to the maps of Pre-Quaternary rocks Sheets 2541, 2542+2524, 2543 and 2544 Vesa Perttunen KEMIN, KARUNGIN, SIMON JA RUNKAUKSEN KARTTA-ALUEIDEN KALLIOPERA Summary: Pre-Quaternary rocks of the Kemi, Karunki, Simo and Runkaus map-sheet areas Geologian tutkimuskeskus - Geological Survey of Finland Espoo 1991 Perttunen, V ., 1991. Kemin, Karungin, Simon ja Runkauksen kartta-alueiden kal- liopera . Summary : Pre-Quaternary rocks of the Kemi, Karunki, Simo and Run- kaus map sheet areas . Geological map of Finland 1:100 000 . Explanation to the maps of Pre-Quaternary rocks, sheets 2541 Kemi, 2542 + 2524 Karunki, 2543 Simo and 2544 Runkaus . 80 pages, 32 figures and 11 tables . The combined area included in the Kemi, Karunki, Simo and Runkaus map sheets is located in northern Finland at the Swedish border, north of the Gulf of Bothnia . The Basement Gneiss area in the southeastern part of the map sheet area be- longs to the Archaean Pudasjarvi Granite Gneiss Complex . The gneisses are most- ly medium-grained, foliated, banded, and migmatized . According to their mineral composition, the gneisses are quartz diorites, granodiorites and oligoclase granites (trondhjemites) . -
GTK, Bulletin 412. Developments in Map Data Management And
Geological Survey of Finland 2021 Developments in map data management and geological unit nomenclature in Finland Jarmo Kohonen and Timo Tarvainen (eds) Bulletin 412 • Special Issue Geological Survey of Finland • Bulletin 412 • Special Issue Geological Survey Finland • Bulletin of Jarmo Kohonen and Timo Tarvainen (eds) and Timo Tarvainen Jarmo Kohonen 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 Dr Saku Vuori, 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 412 Developments in map data management and geological unit nomenclature in Finland by Jarmo Kohonen and Timo Tarvainen (eds) Unless otherwise indicated, the figures have been prepared by the authors of the article. https://doi.org/10.30440/bt412 Received 15.9.2020; Accepted in revised form 13.4.2021 Layout: Elvi Turtiainen Oy Espoo 2021 Kohonen, J. & Tarvainen, T. (eds) 2021. Developments in map data management and geological unit nomenclature in Finland. Geological Survey of Finland, Bulletin 412, 169 pages, 41 figures, 18 tables and 4 appendices. The ongoing transition from maps to 3D modelling of geology needs to be supported by efficient infrastructure, both within the Geological Survey of Finland (GTK) and nationally. One key com- ponent is the easy use of geological map data in forward modelling processes. -
Arkistonmuodostajan/Kokoelman Nimi Paikka Rajavuodet Hm Huomatukset
TORNIONLAAKSON MAAKUNTAMUSEON KOTISEUTUARKISTON YLEISLUETTELO 31.12.2017 I JÄRJESTETYT ARKISTOT kotiseutuarkisto Arkistonmuodostajan/Kokoelman nimi Paikka Rajavuodet Hm Huomatukset AAPAJÄRVEN SONNIOSUUSKUNTA Karunki 1940-1960 0,12 AARNI-CASTREN SUKU Tornio 1797-1954 0,40 ALATORNION HISTORIA -KOKOELMA Alatornio 1900-luku 0,85 ALATORNION NAISLIITON VÄHÄVARAISTEN Alatornio KEUHKOTAUTISTEN AVUSTUSRAHASTO ks. myös Suomalainen Naisliitto Alatornion Osasto 1933-1940 0,04 ALATORNION NUORTEN KRISTILLINEN YHDISTYS RY Alatornio 1988-2004 0,31 ALATORNION PITÄJÄN JYVÄLAINAMAKASIINI Alatornio 1847-1921 0,12 ALATORNION PITÄJÄSEURA RY Alatornio 1955-1997 0,32 ALATORNION URHEILIJOIDEN KAAKAMON Tornio KYLÄOSASTON ARKISTO sisältyy Kaakamon kylä –kokoelma 1929-1950 ARRELA, VELI Tornio 1953-1999 0,66 ENSIMMÄISEN MAAILMANSODAN Tornio SOTAINVALIDIVAIHTO -KOKOELMA 1916-1917 0,26 EVAKUOINTI 1944 -KOKOELMA Alatornio 1944 0,08 GRANROTHIN TALO Tornio 1850-1918 0,16 GRANROTH, JOHAN PETTER Tornio 1884-1903 0,06 GRANROTH, KIRSTI Tornio 1911-1922 0,04 GRANSTRÖM, KAARLO JUHO 1800-1900-luku 0,12 HANHELA, VÄINÖ Tornio 1979-1996 0,40 HUHTALO, HILDUR Tornio 1892-1908 0,08 HUMALPURO, SYLVI Tornio 1909-1969 0,12 OSMO HYVÖSEN KOKOELMA (TORNION TAISTELUT Tornio 1944 -LEHTILEIKEKOKOELMA) 1944 0,35 ISTO, EETU Alatornio 1865-1905 0,17 JAUHON SUKU Alatornio 1980-1997 0,06 KÄYTTÖRAJOITUS JAUKKURIN TALO Tornio 1840-1906 0,04 JOUSMAA, INKERI JA LASSE Tornio 1926-1952 0,06 JÄÄKÄRIPATALJOONA 27:N PERINNEYHDISTYS RY LÄNSI-POHJAN OSASTO 1993-2001 0,56 KAAKAMON KYLÄ –KOKOELMA sisältää myös -
Glacial Geology and Till Geochemistry in Ore Exploration in the Tervola Area, Southern Finnish Lapland
GLACIAL GEOLOGY AND TILL GEOCHEMISTRY IN ORE EXPLORATION IN THE TERVOLA AREA, SOUTHERN FINNISH LAPLAND PERTTI SARALA, VESA PEURANIEMI and RISTO AARIO SARALA. PERTTI, PEURANIEMI, VESA and AARIO, RISTO 1998. Glacial geology and till geochemistry in ore exploration in the Tervola area, southern Finnish Lapland. Bulletin of the Geological Society of Finland 70, Parts 1-2, 19-41. Glacial geology and till geochemistry were studied in an ore exploration project in the Palaeoproterozoic Peräpohja Schist Belt in the Tervola area of southern Finnish Lapland. The starting point for the exploration were numer- ous Au-Cu-rich erratics, the source rock of which was unknown. The mapping of the glacial landforms was based on aerial photo interpretation. The structure, texture, lithology and geochemistry of the till were studied using test pits. Three sieved fractions together with a heavy mineral fraction of the till were analyzed chemically. The glacial landforms of the area include cover and ground moraines, drum- lins, flute ridges and Rogen moraines. The ridges of the Rogen moraine were found to be composed of three different till beds. The surficial parts of the Rogen ridges showed very short transport distance, whilst the lower till was of more distant derivation. Gold and Cu contents in the till are above their regional background levels in every analyzed fraction in the two case study areas of Petäjävaara and Vam- mavaara. High metal contents in till are associated with basic volcanic rocks and their contact zones with quartzite in bedrock. Metal anomalies in till are usually very sharp-contrasted and dilute quickly with increasing distance from the source rock.