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        <Title>Grusinnhold i sedimenter</Title>
        <Abstract>Kartlaget viser indikativ prosentandel av grus i havbunnssedimentenes øvre del (øverste ca. 10 cm av sjøbunnen). Kartet er basert på NGUs regionale kornstørrelseskart (1:100 000 – 1:250 000) og framhever variasjonen i bunnsedimenters grusinnhold fra sted til sted. Grusinnhold er basert på en indikativ prosentverdi per kornstørrelsesklasse og er delt inn i fem klasser. Variasjoner rundt de veiledende verdiene bør forventes. Det er også inkludert en uspesifisert klasse som gjelder for mindre områder hvor det ikke er mulig å fastslå grusinnhold.</Abstract>
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            <Keyword>sjø</Keyword>
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        <Name>Steininnhold_Reg</Name>
        <Title>Innhold av stein og blokk i sedimenter</Title>
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            <Keyword>Kornstørrelse</Keyword>
            <Keyword>sediment</Keyword>
            <Keyword>avsetning</Keyword>
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        <Name>Fjell_Reg</Name>
        <Title>Fjell/harde sedimenter</Title>
        <Abstract>Kartlaget viser i hvor stor grad fjell og harde sedimenter er til stede på havbunnen. Kartet er basert på NGUs regionale kornstørrelseskart (1:100 000 – 1:250 000) og fremhever variasjonen i tilstedeværelse av fjell/hard sedimenter fra sted til sted. Prosentandel av fjell/harde sedimenter er estimert av en indikativ verdi per sedimentkornstørrelsesklasse og er delt i tre klasser som viser tilstedeværelse, fravær eller flekkvis forekomst.</Abstract>
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            <Keyword>havbunn</Keyword>
            <Keyword>sjøbunn</Keyword>
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        <Abstract>Lokale miljøvariabler knyttet til Saltvannsbunnsystemer i Natur i Norge (NiN), v.3.0</Abstract>
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        <Title>Finmaterialinnhold i sedimenter (LM-FI)</Title>
        <Abstract>Kartlaget viser finmaterialinnhold (slam) i marine bunnsedimenter. Finnmaterialinnhold er en lokal miljøgradient i NiN-systemet (LM-FI) som er viktig for kartlegging av naturtyper på saltvannsbunn. Kartlaget er basert på NGUs regionale kornstørrelseskart (1:100 000 – 1:250 000). LM-FI er delt inn i trinn definert i NiN v.3.0 og som er relevante for bunnsamfunnene. Det er også inkludert en uspesifisert klasse som gjelder for mindre områder hvor det ikke er mulig å fastslå finnmaterialinnhold.</Abstract>
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        <Title>Dominerende kornstørrelse (LM-DK)</Title>
        <Abstract>Kartlaget viser den dominerende kornstørrelsen i sedimenter. Dominerende kornstørrelse er en lokal miljøfaktor i NiN-systemet (LM-DK) som er viktig for kartlegging av naturtyper på saltvannsbunn. Kartlaget er basert på NGUs regionale kornstørrelseskart (1:100 000 – 1:250 000). Klasseinndeling for LM-DK følger kategorier som er definert i NiN 3.0 og som er relevante for bunnsamfunnene. Noen klasser er slått sammen av praktiske hensyn relatert til kartleggingsmetodikk (LM-DK_AB) eller oversettelse av de opprinnelig kartlagte klasser (LM-DK_EFGY).</Abstract>
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        <Abstract>Mektighet av av sedimentdekke over bergrunn (Kvartærmektighet) og sedimenter avsatt etter siste istid (Holocen mektighet).</Abstract>
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        <Abstract>Mektighet av sedimentdekke (løsmasser) over berggrunn i Oslofjorden, basert på høyoppløselig seismikk. Målingen i millisekunder er kalkulert til meter.</Abstract>
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        <Abstract>Kartlaget viser den totale mektigheten av sedimenter som er avsatt på kontinentalmarginen sør og vest for Norge i Kvartær (de siste 2,6 millioner år). Mektigheten er angitt i millisekunder toveis gangtid (ms twt). 1 ms twt tilsvarer ca 1 m i kvartære sedimenter.</Abstract>
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            <Keyword>Norskehavet</Keyword>
            <Keyword>Nordsjøen</Keyword>
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        <Abstract>Kartlaget viser mektigheten av den øverste delen av sedimentdekket, avsatt etter slutten av siste istid for ca 11000 - 12000 år siden.</Abstract>
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        <Abstract>Mektighetskoter for kvartære sedimenter på norsk kontinentalmargin. Mektigheten er angitt i millisekunder toveis gangtid (ms twt). 1 ms twt tilsvarer ca 1 m i kvartære sedimenter.</Abstract>
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