Municipal Division is a dataset depicting the municipal division in the whole of Finland. The Municipal Division dataset is produced in scales 1:10,000, 1:100,000, 1:250,000, 1:1,000,000 and 1:4,500,000. The data included in the dataset in scale 1:10,000 are taken from the cadastral registry. Regarding other scales, municipal boundaries have been generalised to suit the scale in question. The Municipal Division dataset is available as products both in vector and raster format. The products in vector format contain the number codes of the municipalities, the names of the municipalities both in Finnish and in Swedish as well as municipal boundaries and municipal regions. In addition, the vector product includes the corresponding information about the county regions and the State Administrative Agencies. Products in raster format include municipal boundaries only. The product belongs to the open data of the National Land Survey of Finland. More information: Topographic data and how to acquire it http://www.maanmittauslaitos.fi/en/maps-and-spatial-data/expert-users/topographic-data-and-how-acquire-it .
Seabed substrate 1:1 000 000 is one of the products produced in the EMODnet (European Marine Observation and Data network) Geology EU project. Project provided seabed geological material from the European maritime areas. The EMODnet Geology project (http://www.emodnet-geology.eu/) collects and harmonizes geological data from the European sea areas to support decision-making and sustainable marine spatial planning. The EMODnet Geology partnership has included 36 marine organizations from 30 countries. This data includes the EMODnet seabed substrate map at a scale of 1:1 000 000 from the Finnish marine areas. It is based on the data produced on a scale of 1:20 000 by the Geological Survey of Finland (GTK). The data has been harmonized and reclassified into five Folk substrate classes (clay + silt (mud), sandy clays, clayey sands, coarse sediments, mixed sediments) and bedrock. The data describes the seabed substrate from the uppermost 30 cm of the sediment column. The data have been generalized into a target scale (1:1 000 000). The smallest cartographic unit within the data is 4 km2. Further information about the EMODnet-Geology project is available on the portal (http://www.emodnet-geology.eu/).
The Surface Geology Map of Finland was produced for the OneGeology-Europe Project by digitising the 1993 edition of the Quaternary map of Finland and by including data from the 2001 Geological map of the Fennoscandian Shield for those localities that were marked as an area of rock exposure on the Quaternary map. The aim of the OneGeology-Europe Project has been to create a harmonised digital map data set covering Europe. The Surface Geology Map of Finland data set includes Quaternary and bedrock units as areas and tectonic features as lines. Additionally, impact craters on the Geological Map of the Fennoscandian Shield are shown as areas. The data set has been reclassified in accordance with the data set specifications given by OneGeology-Europe. On the basis of recent radiometric age determinations, the lithological data set in the map database was re-edited and regrouped in 2009-2010. This has been done with the Geological Surveys of Sweden (SGU) and Norway (NGU) to meet the needs of the OneGeology-Europe project. The scale of use of the map data is 1:1 000 000.
The Topographic map series is a dataset depicting the terrain of all of Finland. The key elements in it are the road network, buildings and constructions, geographic names, waterways, land use and elevation. The more precise levels of the Topographic map series consist of the same map objects and map symbols depicted in the same way as in the familiar Basic map. Basic map raster is applicable to be used, for instance, as a base map for planning land use or for excursion and outdoor recreational purposes in mobile devices and in various Internet services associated with nature. When going over to the more general datasets in the Topographic map series, the number and visualisation of objects and map symbols changes. The generalised small-scale Topographic maps raster are applicable to be used as approach maps in e.g. mobile devices and Internet services. The product belongs to the open data of the National Land Survey of Finland. More information: Topographic data and how to acquire it http://www.maanmittauslaitos.fi/en/maps-and-spatial-data/expert-users/topographic-data-and-how-acquire-it
National Land Survey's Topographic map series in vector format is a dataset depicting the terrain of all of Finland. The most important elements are the road network, administrative borders, preservation areas, population centres, geographic names, waterways, land use and elevation. The largest scale level (1:100,000) of the Topographic map series in vector format is produced by generalising from the Topographic database. Topographic map series 1:250,000 is produced by generalising the dataset 1:100,000. Topographic map series 1:1,000,000 is produced by generalising the dataset 1:250,000. Topographic map series 1:4,500,000 is produced by generalising the dataset 1:1,000,000. The geographic names have been generalised from the geographic names in the Geographic Names Register to map names suited to the scale in question. The administrative borders in the Municipal Division of each scale are used as administrative borders. The Topographic map series in vector format can be used for the production of other map products, e.g. approach maps or maps on a regional or national level The product belongs to the open data of the National Land Survey of Finland. More information: Topographic data and how to acquire it http://www.maanmittauslaitos.fi/en/maps-and-spatial-data/expert-users/topographic-data-and-how-acquire-it.
The Superficial deposits of Finland 1:1 000 000 is based on 'Quaternary Deposits of Finland and Northwestern Part of Russian Federation and their Resources (Sheet 1, Western part)' mapping data. This data is also based on the 1984 map 'Quaternary Deposits of Finland' (1:1 000 000) in the “Geologia” (Geology) folio of the Atlas of Finland, 5th edition (123-126, 1990). Joint scientific and technical planning for the map of the 'Quaternary Deposits of Finland and Northwestern Part of Russian Federation and their Resources' was begun in 1987 while work on the map started in 1988. No field mapping was done for the map, rather the 1:1 000 000 Quaternary map printed in 1984 was supplemented with new data partly obtained from rock aggregate studies and partly from information on superficial deposits gathered in other superficial mapping projects. The map 'Quaternary Deposits of Finland and Northwestern Part of Russian Federation and their Resources' was printed in 1993. The map shows the superficial deposits with colours and symbols and these are classed according to their mode of geological development. The deposit classes are as follows: pre-Quaternary bedrock exposures (no Quaternary layers); boulder field, physically weathered bedrock; gravelly and sandy till; silty till; clayey till; hummocky moraine ; moraine complex; esker, delta, sandur, sorted marginal formation; interlobate formation (esker); till-covered esker / other till-covered gravel and sand deposit; gravel and sand deposit peripheral to eskers; littoral gravel and sand deposit; fluvial deposit; homogeneous clay and silt deposit; layered (varved) clay and silt deposit; peat deposit. Additionally, drumlins, end moraines, aeolian deposits, and sites of gravel, sand, clay and peat extraction as well as gold panning areas have been indicated with symbols. The data set was converted to a digital format to meet the needs of the OneGeology-Europe Project for a printed map in 2009. This data did not include drumlins, end moraines, aeolian deposits, and more important sites for the exploitation of superficial deposits (sites of gravel, sand, clay and peat extraction as well as gold panning areas). In accordance with the 1984 Quaternary map (1:1 000 000) the minimum size of the deposit polygon is generally one square kilometre. In nature the size of superficial sedimentary deposits is usually smaller than one square kilometre and therefore the most common deposit type in the area is shown in the polygon. In places, deposits smaller than a square kilometre that are significant from a superficial perspective have been noted. As a rule, the narrowest point of the deposit polygon was 0.5 km and in important cases, for example on eskers, 0.3 km. As an exception, the size of small eskers has been exaggerated. Coordinate reference system of the Superficial deposits of Finland 1:1 000 000 was transformed in October 2013. The transformation from Finnish National Grid Coordinate System (Kartastokoordinaattijärjestelmä, KKJ) Uniform Coordinate Frame to ETRS-TM35FIN projection was done by using the three-dimensional transformation in accordance with the recommendations for the public administration JHS154. The water layer which were used in the OneGeology-Europe project was replaced in 2015 with the more accurate water layer of the Topographic database 1:55 0000-1:500 000 (DVE3) from ICT Agency HALTIK.
Suomi ulottuu pohjois-etelä suunnassa läpi boreaalisen havumetsävyöhykkeen. Se jaetaan neljään alavyöhykkeeseen, joiden rajat määräytyvät lämpöilmastosta aiheutuvien kasvillisuuserojen perusteella. Alavyöhykkeet jaetaan edelleen lähinnä ilmaston mereisyydestä ja mantereisuudesta johtuvien kasvillisuuserojen määräämiin lohkoihin. Aineisto pohjautuu YM:n muistiosta nro 3/1994 Suomen metsäluonnon monimuotoisuuden kuvaaminen digitoituun aineistoon, jota on muutettu uhanalaisuusarviointiem tarpeisiin kuvaruutudigitointina eri tausta-aineistoja käyttäen. Aineisto kuuluu SYKEn avoimiin aineistoihin (CC BY 4.0)
Vuosittaiset seurantatiedot riistakannoista. Riistaeläinten runsaudenseuranta on riistantutkimuksen ja metsästäjäkunnan yhteistoimintaa. Eri seurantahankkeisiin osallistuu vuosittain lähes kymmenentuhatta metsästäjää. Eri riistaeläinryhmille on kehitetty omat seurantaohjelmansa. Metsäriistaa seurataan riistakolmiolaskennan avulla. Riistakolmiolaskennan rinnalle on kehitetty peltokolmiolaskenta alueille, joilla maatalousympäristöä ja asutusta on runsaasti. Hirvikannan kokoa arvioidaan usealla tavalla. Riistantutkimuksen tärkein työkalu hirvikannan seurannassa on hirvihavaintokortti.
Suokasvillisuuden aluejako perustuu suoyhdistymätyyppeihin. Jako on digitoitu teoksesta Suomen kartasto, vihko 141-143, Ruuhijärvi, R. 1988: Suokasvillisuus. Merialueen vyöhykerajat on digitoitu R. Ruuhijärven erikseen määritteleminä v.2002. Suomen rajat ovat peräisin Digital Chart of the World (DCW) -aineistosta, jonka rantaviivaa on korjattu SYKEssä. Tähän on sovitettu lisäksi SYKEssä luotu aluevesien ulkoraja-aineisto. Aineisto kuuluu SYKEn avoimiin aineistoihin (CC BY 4.0).