Íslenskum skipum eru bannaðar veiðar með botnvörpu, flotvörpu og dragnót í fiskveiðilandhelgi Íslands nema á þeim veiðisvæðum og veiðitímum sem tilgreind eru í 5. grein laga nr. 79 um veiðar í fiskveiðilandhelgi Íslands. Viðmiðunarlínan er dregin umhverfis landið á milli punkta sem eru taldir upp í lagagreininni. Vinsamlega hafið samband við Landhelgisgæslu Íslands vegna nánari upplýsinga.

Land Cover (LC) is one of 12 themes in the European Location Project (ELF). The purpose of ELF is to create harmonised cross-border, cross-theme, and cross-resolution pan-European reference data from national contributions. The goal is to provide INSPIRE-compliant data for Europe. A description of ELF (European Location Project) is here: http://www.elfproject.eu/content/overview. Encoding: INSPIRE version 4

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/.

Þekja [layer] j100v_vesturgosbelti_gigar_1utg_li: Gígar á Vesturgosbelti, línulag. [Craters of the Western Volcanic Zone, line data.] Gögn sem sýna gígaröð og útlínur. Gerður er greinarmunur á gossprungum, Holósen útlínur gíga (yngri og eldri en 7000 ára) og gígar frá Kvarter (kuldaskeið/hlýskeiðs). [Data detailing crater rows and outlines. This includes distinctions between eruptive fissure rows, Holocene crater outlines (younger and older than 7000 years), and quarternary (glacial/interglacial) craters.]

Þekja (layer) j100v_austurland_berggrunnurMork_1utg_li: Línur sýna þekkt mörk berggrunns. [Lines showing certain boundaries of bedrock.] Tilheyra flákagögn 'ni_j100v Berggrunnur á Austurlandi – 1:100.000' (j100v_austurland_berggrunnur_1utg_fl). [Follows the polygon data 'ni_j100v Berggrunnur á Austurlandi – 1:100.000' (j100v_austurland_berggrunnur_1utg_fl).]

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_austurland_strikHalli_1utg_p: Strik og hallastefna jarðlaga. [Strike and dip of the deposits.] Staðsetning mælinga á striki og hallastefnu jarðlaga á Austurlandi. [Locations of measurements of strike and dip of the deposits in Eastern Iceland.]

Þekja (layer) j100v_austurland_millilog_1utg_li:: Gjóskulög á Austfjörðum. [Tuff layers in Eastern Iceland.] Línur sýna staðsetningu stærstu gjóskulagana á Austfjörðum. Gjóskulögin eru fengin úr ýmsum kortum og kortlagningu Birgis V. Óskarssonar. Gögn eru flokkuð eftir ÍST120:2012 staðlinum, nema þrjá fitjueigindir: myndunKodi = Heiti myndunarinnar (skammstöfun) myndunIS = Heiti myndunarinnar (á íslenskuc) myndunEN = Heiti myndunarinnart (á ensku) [Lines show the location of largest tuff deposits in Eastern Iceland. The tuff layers are derived from older maps and the mapping of Birgir V. Óskarsson. 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)]

Þekja [layer] j100v_vesturgosbelti_berggrunnurNidurfoll_1utg_fl: Niðurföll í nútímahraunum. [Collapse pits in Holocene lavas.}

Þekja (layer) j100v_austurland_gigar_1utg_li: Útlínur öskjurima útkulnaðra megineldsstöðva. [Outlines of calderas of extinct volcanos.] Útlínur miða við höggun, dreifingu þursabergs og móbergsmyndana. [The lines are based on local tectonics, distribution of agglomerates and hyaloclastites.]