THE NIILO KONSTENIUS FAMILY by Tommy Ekdahl
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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). -
Ivalojoen Kultavaltausten Työväki 1871
Maijala Erik työmies Kemi Niemi Johan työmies Rovaniemi Patokoski Matti työmies Kemi Työväki Ivalojoen Ruonala Johan työmies Kemi Ruona Olof työmies Kemi Lehtoniemi Matts työmies Kemi kultavaltauksilla Kurtti Ferdinand työmies Ylitornio Sipola Nils talonpoika Kemi Hiltunen Pehr renki Kemi 1871 Kaunisto Matts renki Tornio Tiedot on poimittu kulta-alueen virallisista Halonen Pehr renki Kemi Majala Lars renki Kemi asiakirjoista; valtauksien eli tehdaspiirien Koskela Erik renki Alajärvi omistajien piti lain mukaan tehdä tarkka Ylitalo Jakob talonpoika Lappajärvi ilmoitus jokaisesta työntekijästään, työhön Hyvönen Pehr renki Rovaniemi tulosta ja eroamisesta yms. Valtauksen 20 työväki 1871: Ruikka Thomas talonpoika Rovaniemi Klemettilä Johan Haapavesi Valtauksen 19 työväki 1871: Klemettilä Thomas Haapavesi Brunell Henrik talollinen ja työnjohtaja Hytinkoski Johan Haapavesi Kokkola Niemelä Olof itsellinen Kuolajärvi Juntikka Nils itsellinen Alatornio Körkkä Erik itsellinen Rovaniemi Juntikka Karl talonpoika Alatornio Peltovuoma Johan talonpoika Karling Johan työmies Tornio Muonionniska Huovinen Gustaf Oulu Peltovuoma Erik itsellinen Muonionniska Karling Johan Tornio Jankkila Matts irtolainen Muonionniska Juntikka Nils talonpoika Tornio Lämsä Johan Erik talonpoika Kuusamo Juntikka Karl talollinen Tornio Halvari Henrik itsellinen Rovaniemi Herranen Bertill merimies Tornio Stoorm Adam itsellinen Lohtaja Eskuri Petter ent. sotilas Oulu Rautio Anders itsellinen Lohtaja Lämsä Hans työmies Kuusamo Lampela Matts työläinen Kemi Bäckman Karl satulasepän -
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. -
Struven Ketju
‘STUOR-OIVI’ – a UNESCO World Heritage Site 68º40’57’’ north latitude and 22º44’45’’ east longitude One of the six Finnish station points forming part of the Struve Geodetic Arc protected as a UNESCO World Heritage Site is located at the summit of Stuorrahanoaivi in Enontekiö. The Struve Geodetic Arc is a triangulation chain stretching from the Black Sea to the Arctic Ocean that was laid down in the 1800s to determine the shape of the Earth. The Arc is named after the German-born astronomer F.G.W. Struve. The Struve Geodetic Arc was measured between 1816 and 1855. The measurements, which yielded surprisingly accurate results, gave rise to a chain of 265 station points stretching from Izmail on the Black Sea to Hammerfest in Norway. 83 station points were measured in Finland. Wilhelm Struve and his expedition employed triangulation and astronomical positioning as measuring methods, the objective being to measure the flatness at the poles. The measurements proved that the length of a meridian degree at the Black Sea is about 400 metres shorter than at the Arctic Ocean. UNESCO’s World Heritage Committee added the Struve Geodetic Arc to the World Heritage List in July 2005. The documentation, put together by the National Land Survey of Finland, comprised a joint application by 10 countries. In addition to being the first protected site of a scientific and technological nature, the Struve Geodetic Arc is also the first cultural site that extends across several countries. A total of 34 station points are now protected. The measurements at the summit of Stuorrahanoaivi were carried out between 1850 and 1852. -
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. -
Pests of Cultivated Plants in Finland
ANNALES AGRICULTURAE FE,NNIAE Maatalouden tutkimuskeskuksen aikakauskirja Vol. 1 1962 Supplementum 1 (English edition) Seria ANIMALIA NOCENTIA N. 5 — Sarja TUHOELÄIMET n:o 5 Reprinted from Acta Entomologica Fennica 19 PESTS OF CULTIVATED PLANTS IN FINLAND NIILO A.VAPPULA Agricultural Research Centre, Department of Pest Investigation, Tikkurila, Finland HELSINKI 1965 ANNALES AGRICULTURAE FENNIAE Maatalouden tutkimuskeskuksen aikakauskirja journal of the Agricultural Researeh Centre TOIMITUSNEUVOSTO JA TOIMITUS EDITORIAL BOARD AND STAFF E. A. jamalainen V. Kanervo K. Multamäki 0. Ring M. Salonen M. Sillanpää J. Säkö V.Vainikainen 0. Valle V. U. Mustonen Päätoimittaja Toimitussihteeri Editor-in-chief Managing editor Ilmestyy 4-6 numeroa vuodessa; ajoittain lisänidoksia Issued as 4-6 numbers yearly and occasional supplements SARJAT— SERIES Agrogeologia, -chimica et -physica — Maaperä, lannoitus ja muokkaus Agricultura — Kasvinviljely Horticultura — Puutarhanviljely Phytopathologia — Kasvitaudit Animalia domestica — Kotieläimet Animalia nocentia — Tuhoeläimet JAKELU JA VAIHTOTI LAUKS ET DISTRIBUTION AND EXCHANGE Maatalouden tutkimuskeskus, kirjasto, Tikkurila Agricultural Research Centre, Library, Tikkurila, Finland ANNALES AGRICULTURAE FENNIAE Maatalouden tutkimuskeskuksen aikakauskirja 1962 Supplementum 1 (English edition) Vol. 1 Seria ANIMALIA NOCENTIA N. 5 — Sarja TUHOELÄIMET n:o 5 Reprinted from Acta Entomologica Fennica 19 PESTS OF CULTIVATED PLANTS IN FINLAND NIILO A. VAPPULA Agricultural Research Centre, Department of Pest Investigation, -
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. -
V-Series: Help Finland and Finnish Relief, World War II
V-Series: Help Finland and Finnish Relief, World War II Title: Help Finland series Creators: Help Finland, Inc. and similar agencies Inclusive Dates: 1939-1950 Bulk dates: 1939-190 Extent: 16 linear ft. Languages: Finnish and English Acquisition: Much of the material donated by Antero Hietala, son of Ester L. Hietala, former Secretary of Help Finland, Inc. 1944-1950. Abstract: The Finnish Relief and Help Finland campaign organized to assist persons affected by the Winter, Continuation and Lapland Wars in Finland. The materials in this collection include official organizational and personal correspondences, Finnish children’s drawings of receipt of relief packages, booklets, photographs and audio records regarding the efforts of Americans and Finnish Americans to render aid to those in Finland during and after Finnish involvement in the World War II era. Biographical and Historical Notes: Prior to the beginning of World War II, Finland occupied a tenuous geopolitical position. To the east, loomed the rapidly industrializing and ascending geopolitical influence of the Soviet Union. To the southwest, the German war machine was rapidly militarizing. Finland, who had historical military ties with Germany, drew the suspicion of the Soviet war machine and on November 30, 1939, the Soviets invaded Finland. What was termed the “Winter War” was a heroic effort by Finland’s small army to repel the much larger Soviet military machine. In the end, the Soviet Red Army proved too much as the Finns fought the Soviets to a stalemate and in March 1940, Finland signed the Moscow Peace Treaty. Terms of the treaty were not favorable to Finland, which signed over the Finnish section of Karelia, the Salla/Kuusamo region, the Kalastajan saarento peninsula and 4 islands in the Gulf of Finland to the Soviets. -
Tornio Attracted Scientists the Alatornio Church and Kokkomäki Hill
The Alatornio church and Kokkomäki hill as station points The scientific fieldwork for the Struve Geodetic Arc was con- ducted in the summers of 1842–1852 in Tornio and the re- gion between the Tornio and Muonio Rivers. The elevations of the measuring points near the church were measured in the autumn of 1842, and the triangulations from the south were finished by 1844. The measurements were taken under the supervision of the Finnish Fredrik Woldstedt, who worked for the Pulkovo Astronomical Observatory of the Russian Academy of Sciences in Saint Petersburg. Woldstedt worked The structures of the church and its bell chamber are unique. At the time of the measurements, astronomy was popular closely with Struve. The walls and the large support beams feature writings outside of universities and science academies as well. dating back to the years the church was built. A view to the The Swedes measured the angles between the southern- In the Kuussaari house in Raumo was an observatory. horizon awaits beyond the large doors. Photo: Panu Pohjola. most stations of the Lapland portion of the chain in 1849. The owner of the house, Emil Broms, had several telescopes. Photo: Pia Keränen. The Alatornio church is located on the Pirkkiö island, where The southernmost triangle was formed by the Alatornio One of them was two metres long and could be used to look measurements were taken by scientists from Pulkovo, Russia church, Kaakamavaara and Perävaara station points. The at stars even in broad daylight. The ceiling of the observatory has a special opening mechanism. Photo: Reino Kainulainen, and Sweden. -
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) .