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Now showing items 451-460 of 3041
(Doctoral thesis / Doktoravhandling, 2011)
The velocity of glaciers is important for many aspects in glaciology. Mass accumulated in the accumulation area is transported down to the ablation area by deformation and sliding due to the gravitational force, and hence ...
(Master thesis / Masteroppgave, 2017)
Målet med dette studiet var å finne den naturlige miljøtilstanden i dypassenget i Lurefjorden på Vestlandet, endringer i miljøstatus gjennom tid og akkumulasjonsraten til organisk karbon i Lurefjorden ble også kalkulert. ...
(Master thesis / Masteroppgave, 2017)
The Cambrian-Ordovician boundary interval within Alum Shale at Krekling, Norway, is for the first time investigated for biostratigraphy. Samples were taken from the Alum Shale levels, within the almost continuous succession ...
(Master thesis / Masteroppgave, 2017)
(Master thesis / Masteroppgave, 2017)
Shallow landslides in soils, such as debris flows and debris avalanches, are expected to increase in frequency and intensity in large parts of Norway. The simulation, characterization and statistical analysis of such events ...
(Master thesis / Masteroppgave, 2017)
(Doctoral thesis / Doktoravhandling, 2011)
Glaciers, ice caps and ice sheets constitute a large reservoir in the global hydrological cycle and provide a coupling between climate and sea-level. Observations of glacial change is important for constraining their ...
(Master thesis / Masteroppgave, 2016)
Med utgangspunkt i NVEs 59 registrerte sørpeskred i Noreg i perioden 2010 til 2016 er denne masteroppgåva eit terskelstudie med formål å avdekke tersklar for regional varsling av sørpeskred. Oppgåva har teke føre seg NVEs ...
(Journal article / Tidsskriftartikkel / PublishedVersion; Peer reviewed, 2017)
Molecular tracers in secondary organic aerosols (SOAs) can provide information on origin of SOA, as well as regional scale processes involved in their formation. In this study 9 carboxylic acids, 11 organosulfates (OSs) ...
(Journal article / Tidsskriftartikkel / AcceptedVersion; Peer reviewed, 2017)
The Early Eocene continental breakup was magma-rich and formed part of the North Atlantic Igneous Province. Extrusive and intrusive magmatism was abundant on the continental side, and a thick oceanic crust was produced up ...