Research paperThe morphology and formation of flow-lobe tumuli on Icelandic shield volcanoes
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Geomorphological characterization of the 2014–2015 Holuhraun lava flow-field in Iceland
2021, Journal of Volcanology and Geothermal ResearchCharacterization, origin, and evolution of one of the most eroded mafic monogenetic fields within the central Andes: The case of El País lava flow field, northern Chile
2021, Journal of South American Earth SciencesEmplacement and inflation of the Al-Halaq al Kabir lava flow field, central part of the Al Haruj Volcanic Province, Central Libya
2019, Journal of Volcanology and Geothermal ResearchCitation Excerpt :In the present study we treated this mappable unit as an individual flow field and remapped it as unit II (Fig. 3a, b). The terminology used in this paper to describe inflated pahoehoe lavas is revised from Walker (1991), Hon et al. (1994), Self et al. (1998), Rossi and Gudmundsson (1996) and Thordarson and Self (1993). The lava flow field is defined as a complex body that contains several lava flows (eruptive episodes) produced by individual volcanic eruptions and identified in the field on the basis of field relations (Thordarson and Self, 1993; Thordarson and Höskuldsson, 2008; Fig. 4a).
Estimate of depths of source fluids related to mound fields on Mars
2018, Planetary and Space ScienceUsing satellite imagery to identify and analyze tumuli on Earth and Mars
2018, Earth and Planetary Science LettersCitation Excerpt :While a full analysis of this type of relationship between tumuli characteristics and the tumuli population's location within the flow is beyond the scope of this study, the results presented from these two lava flow fields supports the idea that such studies can connect these relict surface features to the larger-scale lava flow emplacement structure, thus enabling some interpretation of a flow's emplacement history. Using detailed descriptions of the morphologies of different types of terrestrial lava flow features (Baloga et al., 2007; Duncan et al., 2004; Duraiswami et al., 2001; Hon et al., 1994; Rossi and Gudmundsson, 1996; Walker, 1991) along with hypotheses about the tumulus formation mechanism (Anderson et al., 2012; Rossi and Gudmundsson, 1996), a flowchart of specific planform morphological types (Supplemental Fig. 1/S1) was designed to differentiate between tumuli and other topographic features commonly found on inflated lava flows, such as lava rises. This flowchart focused only on planform morphology of the features, making it appropriate for use with satellite imagery.
Plateaus and sinuous ridges as the fingerprints of lava flow inflation in the Eastern Tharsis Plains of Mars
2017, Journal of Volcanology and Geothermal Research
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Present address: Department of Geography, University of Turku, FIN-20014 Turku, Finland.