Landhelgi Íslands er skilgreind í lögum nr. 41/1979 með síðari breytingum frá 15. október 2021. Heiti laganna er Lög um landhelgi, aðlægt belti, efnahagslögsögu og landgrunn. Í lögunum eru skilgreiningar og útskýringar á aðlægu belti, efnahagslögsögu og landgrunni Íslands: https://www.althingi.is/lagas/nuna/1979041.html Landhelgi Íslands skal afmörkuð af línu sem alls staðar er 12 sjómílur frá grunnlínu. Grunnlína er sett fram sem lína en einnig punktar. Línan er dregin milli punktanna. Aðlægt belti er svæði utan landhelgi (línur). Efnahagslögsaga Íslands er svæði utan landhelgi (línur). Vinsamlega hafið samband við Landhelgisgæslu Íslands vegna nánari upplýsinga.

Gagnasafn [GDB] NI_J100v_Vesturgosbelt_1.utg: Jarðfræðikort af Vesturgosbelti Íslands í mælikvarði 1:100.00, 1. útg. [Geological map of the Western Volcanic Zone of Iceland in the scale of 1:100.000, 1st ed.] Kortið sýnir jarðlög, gíga, höggun, strik og halla, framhlaup og niðurföll, steingervinga, jökulrákir, jökulgarða, jökulkembur, malarása og fornar strandlínur stöðuvatna. Jarðlög eru flokkuð eftir aldri, gerð og samsetningu. Kortið var unnin í samstarfi Náttúrufræðistofnunar Íslands og Íslensku Orkurannsoknastofa. Tilvísun: Birgir V. Óskarsson, Ögmundur Erlendsson, Robert A. Askew, Árni Hjartarson, Magnús Á. Sigurgeirsson, Skafti Brynjólfsson og Sveinn Jakobsson 2022. Jarðfræðikort af Vesturgosbelti. 1.100.000. 1. útg. Garðabær: Náttúrufræðistofnun Íslands, Íslenskar Orkurannsóknir og Umhverfis- og Auðlindaráðuneytið. [The map displays bedrock geology, volcanic craters, tectonics, strike and dips, landslides and collapse pits, fossils, glacial striations, glacial moraines, flutes, eskers and ancient lake strandlines. Bedrock is classified by age, type, and composition. The map was completed in a collaborative project between the Icelandic Institute of Natural History and the Icelandic Geosurvey. Bibliographic reference: Birgir V. Óskarsson, Ögmundur Erlendsson, Robert A. Askew, Árni Hjartarson, Magnús Á. Sigurgeirsson, Skafti Brynjólfsson og Sveinn Jakobsson 2022. Geological map of the Western Volcanic Zone, Iceland. 1:100.000. 1st edition. Garðabær: Icelandic Institute of Natural History, Iceland GeoSurvey and Ministry for the Environment and Natural Resources.]

Þekja [layer] j100v_vesturgosbelti_berggrunnur_1utg_fl: Gögn fyrir berggrunn ásamt nútímahraunum. [Data showing the bedrock geology, including Holocene lavas.] Berggrunnur er flokkaður eftir aldri, gerð og samsetningu. Gögn eru flokkuð eftir ÍST120:2012 staðlinum, nema fitjueigindir: myndunKodi = stuttur kóði sem táknar gerð bergmyndunar, myndunIS = stutt íslenskt heiti fyrir bergmyndun, myndunEN = stutt enskt nafn á bergmyndun, eldstodNafn = nafn eldstöðvakerfis, kenni = stuttur kóði fyrir hlýskeiðishraun og nútímahraun, aldur = aldursbil, Nýr kóði fyrir fitjueigindina 'Tegund storkubergs' (tegStorkubergs): dbas = dílabasalt. [Bedrock is classified by age, type, and composition. The data follows the ÍST120:2012 data standard with these additional feature attributes: myndunKodi = short code denoting the rock formation type, myndunIS = short Icelandic name for rock formation, myndunEN = short English name for rock formation, eldstodNafn = name of the volcanic system, kenni = short codename for interglacial and postglacial lavas, aldur = age range. New code for feature attribute 'Tegund storkubergs' (tegStorkubergs): dbas = porphyrytic basalt.]

Þekja (layer) j100v_austurland_hoggun_1utg_li: Sprungur og misgengi. [Cracks and faults.] Gögn með sprungum og misgengjum kortlögð í ýmsum kortlagningaverkefnum. [Data showing cracks and faults mapped in various mapping projects.]

Corine Land Cover (CLC) 2012 and CLC change 2006-2012 are two of the datasets produced within the frame of the Initial Operations of the Copernicus programme (the European Earth monitoring programme previously known as GMES) on land monitoring. Corine Land Cover (CLC) provides consistent information on land cover and land cover changes across Europe. This inventory was initiated in 1985 (reference year 1990) and established a time series of land cover information with updates in 2000, 2006 and 2012 being the last one. CLC products are based on photointerpretation of satellite images by national teams of participating countries - the EEA member and cooperating countries – following a standard methodology and nomenclature with the following base parameters: 44 classes in the hierarchical three level Corine nomenclature; minimum mapping unit (MMU) for status layers is 25 hectares; minimum width of linear elements is 100 metres; minimum mapping unit (MMU) for Land Cover Changes (LCC) for the change layers is 5 hectares. The resulting national land cover inventories are further integrated into a seamless land cover map of Europe.Land cover and land use (LCLU) information is important not only for land change research, but also more broadly for the monitoring of environmental change, policy support, the creation of environmental indicators and reporting. CLC datasets provide important datasets supporting the implementation of key priority areas of the Environment Action Programmes of the European Union as protecting ecosystems, halting the loss of biological diversity, tracking the impacts of climate change, assessing developments in agriculture and implementing the EU Water Framework Directive, among others.More about the Corine Land Cover (CLC) and Copernicus land monitoring data in general can be found at http://land.copernicus.eu/.

Corine Land Cover (CLC) 2018 and CLC change 2012-2018 are two of the datasets produced within the frame of the Initial Operations of the Copernicus programme (the European Earth monitoring programme previously known as GMES) on land monitoring.Corine Land Cover (CLC) provides consistent information on land cover and land cover changes across Europe. This inventory was initiated in 1985 (reference year 1990) and established a time series of land cover information with updates in 2000, 2006. 2012 and now 2018. CLC products are based on photointerpretation of satellite images by national teams of participating countries - the EEA member and cooperating countries – following a standard methodology and nomenclature with the following base parameters: 44 classes in the hierarchical three level Corine nomenclature; minimum mapping unit (MMU) for status layers is 25 hectares; minimum width of linear elements is 100 metres; minimum mapping unit (MMU) for Land Cover Changes (LCC) for the change layers is 5 hectares. The resulting national land cover inventories are further integrated into a seamless land cover map of Europe. Land cover and land use (LCLU) information is important not only for land change research, but also more broadly for the monitoring of environmental change, policy support, the creation of environmental indicators and reporting. CLC datasets provide important datasets supporting the implementation of key priority areas of the Environment Action Programmes of the European Union as protecting ecosystems, halting the loss of biological diversity, tracking the impacts of climate change, assessing development in agriculture and implementing the EU Water Framework Directive, among others. More about the Corine Land Cover (CLC) and Copernicus land monitoring data in general can be found at http://land.copernicus.eu/

Þekja (layer) j100v_austurland_steingervingar_1utg_p: Fundarstaðir steingervinga. [Locations with fossils.] Fundarstaðir steingervinga, einkum plöntusteingervinga eða surtabrands. [Location with fossils, exclusvely plant fossils or lignite deposits.]

Þekja (layer) j100v_austurland_berggrunnur_1utg_fl: Gögn sem sýnir bergrunn Austurlands. [Data showing the bedrock geology of Eastern Iceland.] Flákalag með bergrunn Austurlands. Flákarnir sýna mismunandi gerðir storkubergs ásamt sethulu. Gögn eru flokkuð eftir ÍST120:2012 staðlinum, nema þrjá fitjueigindir: myndunKodi = Heiti myndunarinnar (skammstöfun) myndunIS = Heiti myndunarinnar (á íslenskuc) myndunEN = Heiti myndunarinnart (á ensku) Nýr kóði fyrir fitjueigindi 'Tegund storkubergs' (tegStorkubergs): shra = samsett hraun, dbas = Dílabasalt, dobas = Díla- og olívínbasalt, and = Andesít. [Polygone layer of the bedrock geology of Eastern Iceland. The polygones show different classes of intrusive and extrusive rocks and the sediment cover. The data follows the ÍST120:2012 data standard with the three additional feature attributes: myndunKodi = Lithostratigraphic unit (abbreviation) myndunIS = Lithostratigraphic unit (in Icelandic) myndunEN = Lithostratigraphic unit (in English) New codes for feature attribute 'Tegund storkubergs' (tegStorkubergs) are: shra = composit lava, dbas = porphyritic lava, dobas = porphyritic and olivine basalt, and = andesite.]

Þekja [layer] j100v_vesturgosbelti_lindir_1utg_p: Lindir og hverir á Vesturgosbelti Íslands. [Springs and hotsprings of the Western Volcanic Zone of Iceland.] Gögnin sýna laug, hver, lindir, gufu- og leirhver. Gögn eru ekki flokkuð eftir ÍST120:2012 staðlinum. Hér er flokkun eða lýsing nýrra fitjueiginda: 'tegUppsprettuISOR': 2: 10–25°C (Laug) 3: 25–50°C (Laug) 4: 50–75°C (Laug) 5: 75–98°C (Laug) 6: 98–100°C (Hver) 20: Hrúður 30: Leir- og gufuhverir 7212: Lindir 10–100 l/s 7213: Lindir >100 l/s 7214: Lindasvæði 100–1000 l/s 7215: Lindasvæði >1000 l/s 'tegUppsprettuNI': 1: Lindir 4: Laug (10–98°C) 5: Hver (98–100°C) 6: Leir- og gufuhver 'vatnshiti': Hitastig vatnsins við lindina, mælieining: °C. 'gerdiISOR': Grágrýtislind/Grágrýtislindir: Lind/lindir í hrauni eldra en síðasta jökulskeið, Hraunalind/Hraunalindir: Lind/lindir í nútímahrauni, Móbergslind/Móbergslindir: Lind/lindir í móbergi, Sprungulind: Lind í sprungu. [This data includes cold, warm and hot springs, steam and mud springs. The data does not follow the ÍST120:2012 data standard. Explanation and classification of the new feature attributes: 'tegUppsprettuISOR': 2: 10–25°C (Warm spring) 3: 25–50°C (Warm spring) 4: 50–75°C (Warm spring) 5: 75–98°C (Warm spring) 6: 98–100°C (Boiling spring) 20: Hot spring deposits 30: Mud and steam spring 7212: Cold spring 10–100 l/s 7213: Cold spring >100 l/s 7214: Cold spring area 100–1000 l/s 7215: Cold spring area >1000 l/s 'tegUppsprettuNI': 1: Cold spring 4: Warm spring (10–98°C) 5: Boiling spring (98–100°C) 6: Mud and steam spring 'vatnshiti': Temperature of the spring in °C. 'gerdiISOR': Grágrýtislind/Grágrýtislindir: Spring(s) in 'grey basalt' lavas older than the last glacial, Hraunalind/Hraunalindir: Spring(s) in postglacial lavas, Móbergslind/Móbergslindir: Spring(s) in hyaloclastite tuff, Sprungulind: Spring in tectonic fissure.]

Skyndilokanir Upplýsingar um skyndilokanir veiðisvæða koma úr gagnagrunnum Fiskistofu. Frá árinu 2020 hefur ákvörðunartaka um skyndilokanir veiðisvæða fyrir tilteknum veiðum verið í höndum Fiskistofu en var áður hjá Hafrannsóknarstofnun. Skyndilokun varir að jafnaði í 2 vikur. Tímamörk lokunar eru alltaf tilgreind með ákvörðun skyndilokunar. Ákvörðun um skyndilokun veiðisvæðis er gerð þegar mælingar á afla stenst ekki viðmiðunarmörk Hafrannsóknarstofnunar en einnig til að loka svæðum sem hafa staðbundinn kvóta. Reglugerðalokanir Reglugerðir eru ákvarðaðar af Atvinnuvega- og nýsköpunarráðuneytinu (ANR) og skilgreina bannsvæði og tímabil, þar sem fiskveiðar eru bannaðar með tilteknum veiðarfærum. Sumar reglugerðarlokanir eru árstíðarbundnar, til dæmis friðun vegna hrygninga þar sem svæðum sem fiskur kemur til hrygninga er lokað á ákveðnum tíma ársins.