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geoscientificInformation

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    Þekja (layer) j100v_austurland_skridur_1utg_li: Lagið sýnir útlínur stærstu framhlaupa á svæðinu. [The layer shows the outlines of the largest landslides of the area.]

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    Þekja [layer] j100v_vesturgosbelti_gigar_1utg_p: Gervigígar, punktalag. [Rootless cones, point data.]

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    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.]

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

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    Average near-Up crustal velocities between summer 2015 and summer 2018. These velocities indicate velocities in the Up direction. However, they could be slightly influence by velocities along the East and North directions and are therefore called near-Up. Near-Up velocities were derived by decomposing the line-of-sight velocities of six Sentinel-1 interferometric time-series covering Iceland. These time-series used a single master approach and Sentinel-1 images from the following summers (mid-June to end of September): 2015, 2016, 2017, and 2018. The near-Up velocity grid has a 50 m resolution.

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    Þekja (layer) j100v_austurland_anomaliaC5n_1utg_li: Neðri mörk segulanomalíunar Chron 5. [Lower limits of magnetic anomaly Chron 5.] Útlínan fylgir efstu hraunum Grjótárólivínbasaltsyrpunnar. [The line follows the uppermost lava flows of Grjótá olivine basalt group.]

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    Gagnasafn (GDB) NI_J600v_berg_2.utg: Jarðfræðikorti af Íslandi – Berggrunnur – 1:600.000 [Geological Map of Iceland – Bedrock geology – 1:600.000]. Berggrunnskort af Íslandi sýnir stærstu drættina í jarðfræði landsins. Jarðlög eru flokkuð eftir aldri, gerð og samsetningu. Kortið sýnir vel gosbelti landsins og dreifingu gossstöðva frá nútíma. Nútímahraunum er skipt í forsöguleg og söguleg hraun (yngri en 871 e. Kr. ). [The Geological Map of Iceland shows the main features of the bedrock geology. Formation are classified by age, type, and composition. The map clearly shows the island's volcanic zones and the distribution of the recent eruption sites. Lava fields of the Holocene are shown as pre-historic or historic (younger than AD 871].]

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    Þekja [layer] j100v_vesturgosbelti_berggrunnur_1utg_p: Steingervingar og strik og halli. [Fossils and strike and dip.] Gögnin innihalda halli, strík og hallaáttir ásamt þekktum steingervingum. Stríkstefna (fitjueigindi 'strikstefna'): 0-359° - fylgir 'right-hand rule'. Hallastefnu eru +90° frá stríksetfna. [The data includes dip, strike and dip directions along with known fossil locations. Strike direction (feature attribute 'strikstefna') follows the right-hand rule where dip direction is +90° from strike.]

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    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.]

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    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.]