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dc.contributor.authorGutierrez Mozo, Ivan David
dc.contributor.authorWeibull, Wiktor Waldemar
dc.contributor.authorWatson, Lisa
dc.contributor.authorOlsen, Thomas Meldahl
dc.contributor.authorEscalona Varela, Alejandro
dc.coverage.spatialNorway, Stavangeren_US
dc.date.accessioned2023-11-10T13:08:53Z
dc.date.available2023-11-10T13:08:53Z
dc.date.created2023-06-08T18:29:58Z
dc.date.issued2023
dc.identifier.citationGutierrez, I., Weibull, W., Watson, L., Olsen, T. M., & Escalona, A. (2023). Holistic 3D Model of an Urban Area in Norway: An Integration of Geophysical, Geotechnical, Remote Sensing, and Geological Methods. Remote Sensing, 15(11), 2872.en_US
dc.identifier.issn2072-4292
dc.identifier.urihttps://hdl.handle.net/11250/3101929
dc.description.abstractUnderstanding the distribution and characterization of natural and non-natural materials on the surface and near-subsurface is important for the development of infrastructure projects. This may be a challenge in highly urbanized areas, where outcrops are scarce, and anthropogenic activities have altered the morphological expression of the landscape. This study tests the integration of ground-penetrating radar (GPR), borehole drilling, aerial imagery, geological mapping, and aerial laser scanning as complementary mapping tools for determining the stratigraphy of glacial and post-glacial Quaternary sediments, the depth to the bedrock, and the distribution of anthropogenic material in Mosvatnet, a lake in Stavanger, Norway. The integration proved to be efficient and enabled the generation of a 3D holistic model, which provided a broad understanding of the subsurface geology and the induced anthropogenic changes in the area through time. Bedrock, till, fluvioglacial, and lacustrine geological units were modeled. Accumulations of post-glacial organic matter were mapped, and the distribution of non-natural infill material was determined. The interpreted dataset suggests that the eastern shoreline of Mosvatnet has artificially prograded about one hundred meters westward since the 1930s and the elevation of the corresponding area has increased by about ten meters relative to the lake level.en_US
dc.language.isoengen_US
dc.publisherMDPIen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectgeofysikken_US
dc.subjecturbane områderen_US
dc.titleHolistic 3D Model of an Urban Area in Norway: An Integration of Geophysical, Geotechnical, Remote Sensing, and Geological Methodsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450en_US
dc.source.pagenumber1-33en_US
dc.source.volume15en_US
dc.source.journalRemote Sensingen_US
dc.source.issue11en_US
dc.identifier.doi10.3390/rs15112872
dc.identifier.cristin2153182
dc.relation.projectNorges forskningsråd: 8050en_US
dc.source.articlenumber2872en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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