@article{MTMT:25677373,
	title = {Construction of the North Head (Maungauika) tuff cone: a product of Surtseyan volcanism, rare in the Auckland Volcanic Field, New Zealand},
	url = {https://m2.mtmt.hu/api/publication/25677373},
	author = {Agustin-Flores, Javier and Németh, Károly and Cronin, Shane J and Lindsay, Jan M and Kereszturi, Gabor},
	doi = {10.1007/s00445-014-0892-9},
	journal-iso = {B VOLCANOL},
	journal = {BULLETIN OF VOLCANOLOGY},
	volume = {77},
	unique-id = {25677373},
	issn = {0258-8900},
	year = {2015},
	eissn = {1432-0819}
}

@article{MTMT:25643992,
	title = {The Al-Du'aythah volcanic cones, Al-Madinah City: implications for volcanic hazards in northern Harrat Rahat, Kingdom of Saudi Arabia},
	url = {https://m2.mtmt.hu/api/publication/25643992},
	author = {Murcia, H and Németh, Károly and El-Masry, N N and Lindsay, J M and Moufti, M R H and Wameyo, P and Cronin, S J and Smith, I E M and Kereszturi, G},
	doi = {10.1007/s00445-015-0936-9},
	journal-iso = {B VOLCANOL},
	journal = {BULLETIN OF VOLCANOLOGY},
	volume = {77},
	unique-id = {25643992},
	issn = {0258-8900},
	year = {2015},
	eissn = {1432-0819}
}

@article{MTMT:24487515,
	title = {Numerical simulation of basaltic lava flows in the Auckland Volcanic Field, New Zealand—implication for volcanic hazard assessment},
	url = {https://m2.mtmt.hu/api/publication/24487515},
	author = {Kereszturi, G and Cappello, A and Ganci, G and Procter, J and Németh, Károly and Del Negro, C and Cronin, SJ},
	doi = {10.1007/s00445-014-0879-6},
	journal-iso = {B VOLCANOL},
	journal = {BULLETIN OF VOLCANOLOGY},
	volume = {76},
	unique-id = {24487515},
	issn = {0258-8900},
	year = {2014},
	eissn = {1432-0819}
}

@article{MTMT:2707795,
	title = {Automated recognition of quasi-planar ignimbrite sheets as paleosurfaces via robust segmentation of digital elevation models: an example from the Central Andes},
	url = {https://m2.mtmt.hu/api/publication/2707795},
	author = {Székely, Balázs and Koma, Zsófia and Karátson, Dávid and Dorninger, P and Wörner, G and Brandmeier, M and Nothegger, C},
	doi = {10.1002/esp.3606},
	journal-iso = {EARTH SURF PROCESS LANDF},
	journal = {EARTH SURFACE PROCESSES AND LANDFORMS},
	volume = {39},
	unique-id = {2707795},
	issn = {0197-9337},
	keywords = {morphometry; erosion; Pattern recognition; Segmentation; Sedimentology; ignimbrite; volcanoes; Tectonics; Image segmentation; Forestry; geomorphology; digital elevation model; surveying; Tracking radar; paleosurface; Shuttle Radar Topography Mission; Andes; Geomorphometry; Surface segmentation; Gravitational movement; Automated recognition; Digital instruments; Robust segmentation; Paleosurfaces; Dissected surfaces},
	year = {2014},
	eissn = {1096-9837},
	pages = {1386-1399},
	orcid-numbers = {Székely, Balázs/0000-0002-6552-4329; Karátson, Dávid/0000-0003-0386-1239}
}

@article{MTMT:25663940,
	title = {A model for calculating eruptive volumes for monogenetic volcanoes - Implication for the Quaternary Auckland Volcanic Field, New Zealand},
	url = {https://m2.mtmt.hu/api/publication/25663940},
	author = {Kereszturi, Gabor and Németh, Károly and Cronin, Shane J and Agustin-Flores, Javier and Smith, Ian E M and Lindsay, Jan},
	doi = {10.1016/j.jvolgeores.2013.09.003},
	journal-iso = {J VOLCANOL GEOTH RES},
	journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH},
	volume = {266},
	unique-id = {25663940},
	issn = {0377-0273},
	year = {2013},
	eissn = {1872-6097},
	pages = {16-33}
}

@article{MTMT:25672806,
	title = {Evaluation of morphometry-based dating of monogenetic volcanoes-a case study from Bandas del Sur, Tenerife (Canary Islands)},
	url = {https://m2.mtmt.hu/api/publication/25672806},
	author = {Kereszturi, Gabor and Geyer, Adelina and Marti, Joan and Németh, Károly and Javier, Doniz-Paez F},
	doi = {10.1007/s00445-013-0734-1},
	journal-iso = {B VOLCANOL},
	journal = {BULLETIN OF VOLCANOLOGY},
	volume = {75},
	unique-id = {25672806},
	issn = {0258-8900},
	year = {2013},
	eissn = {1432-0819},
	orcid-numbers = {Geyer, Adelina/0000-0002-8803-6504; Marti, Joan/0000-0003-3930-8603; Németh, Károly/0000-0003-1026-0407}
}

@article{MTMT:2098670,
	title = {Morphometry of scoria cones, and their relation to geodynamic setting: A DEM-based analysis},
	url = {https://m2.mtmt.hu/api/publication/2098670},
	author = {Fornaciai,, A., and Favalli, M and Karátson, Dávid and Tarquini, S and Boschi, E},
	doi = {10.1016/j.jvolgeores.2011.12.012},
	journal-iso = {J VOLCANOL GEOTH RES},
	journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH},
	volume = {217},
	unique-id = {2098670},
	issn = {0377-0273},
	year = {2012},
	eissn = {1872-6097},
	pages = {56-72},
	orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239}
}

@article{MTMT:2083403,
	title = {LiDAR-based quantification of lava flow susceptibility in the City of Auckland (New Zealand)},
	url = {https://m2.mtmt.hu/api/publication/2083403},
	author = {Kereszturi, G and Procter, J and Cronin, SJ and Németh, Károly and Bebbington, M and Lindsay, J},
	doi = {10.1016/j.rse.2012.07.015},
	journal-iso = {REMOTE SENS ENVIRON},
	journal = {REMOTE SENSING OF ENVIRONMENT},
	volume = {125},
	unique-id = {2083403},
	issn = {0034-4257},
	abstract = {Lava flows represent one of the most significant volcanic hazards from basaltic monogenetic volcanoes, such as spatter cones, scoria cones, maars, and tuff rings. They are common features emanating from parasitic vents on the flanks of polygenetic volcanoes and in dominantly 'flat-lying' intraplate volcanic fields. The Auckland Volcanic Field (AVF) is a volcanic field that has been active for the last ca. 250ka, hosting at least 50 monogenetic volcanoes. Morphometric parameters of lava flows, such as volume, length, thickness and area, were used to quantify the potential lava-flow inundation susceptibility to New Zealand's most densely populated area, the City of Auckland based on an airborne Light Detection and Ranging (LiDAR) Digital Surface Model (DSM). The morphometric parameters of fifteen studied flows included: average length of 2.5km (range 0.7-6.5km), overall average thickness of 14.8m (range 3.4-43.8m), average of maximum thicknesses of 48.2m (range 18.3-180.5m), average area occupied of 5.1km 2 (range 0.4-25.1km 2) and average volume of 0.12km 3 (range 0.005-1km 3). Based on these parameters and a LiDAR-derived DSM, the present topography was classified into: sea, topographic depressions; low-lying areas prone to inundation by an average lava flow; buffer zones prone to inundation only by extremely thick lava flows; and peaks or ridges, which are unlikely to be overtopped. In monogenetic fields, each new vent occurs in a new location, creating uncertainty around the spatial location of the volcanic hazard. Thus, this research provides a general vent location-independent approach to describe the lava flow susceptibility for a potentially active monogenetic volcanic field. What this analysis reveals is that the City of Auckland can be divided into two distinct areas with strongly different susceptibility to lava flow inundation. The southern part of the City is predominantly flat, without hindrance to lava flow, whereas the hilly northern and central part has many ridges that can limit or channelise lavas. These contrasting properties must be accounted for in scenario-based or probabilistic hazard and risk models developed for the AVF. © 2012 Elsevier Inc.},
	keywords = {tuff ring; SCORIA CONE; volcanic hazard; MAAR; monogenetic; Slope angle; Morphometric parameters; Drainage system; Digital elevation model (DEM); Adaptive topographic classification},
	year = {2012},
	eissn = {1879-0704},
	pages = {198-213}
}

@inbook{MTMT:1330263,
	title = {Digital Terrain Analysis in a GIS Environment. Concepts and Development},
	url = {https://m2.mtmt.hu/api/publication/1330263},
	author = {Jordán, Győző},
	booktitle = {Digital Terrain Modelling},
	doi = {10.1007/978-3-540-36731-4_1},
	unique-id = {1330263},
	year = {2007},
	pages = {1-43}
}

@article{MTMT:1329287,
	title = {Extraction of morphotectonic features from DEMs: Development and applications for study areas in Hungary and NW Greece},
	url = {https://m2.mtmt.hu/api/publication/1329287},
	author = {Jordán, Győző and Meijninger, BML and van Hinsbergen, DJJ and Meulenkamp, JE and van Dijk, PM},
	doi = {10.1016/j.jag.2005.03.003},
	journal-iso = {INT J APPL EARTH OBS},
	journal = {INTERNATIONAL JOURNAL OF APPLIED EARTH OBSERVATION AND GEOINFORMATION},
	volume = {7},
	unique-id = {1329287},
	issn = {1569-8432},
	abstract = {A procedure for the consistent application of digital terrain analysis methods to identify tectonic phenomena from geomorphology is developed and presented through two case studies. Based on the study of landforms related to faults, geomorphological characteristics are translated into mathematical and numerical algorithms. Topographic features represented by digital elevation models of the test areas were extracted, described and interpreted in terms of structural geology and geomorphology. Digital terrain modelling was carried out by means of the combined use of: (1) numerical differential geometry methods, (2) digital drainage network analysis, (3) digital geomorphometry, (4) digital image processing, (5) lineament extraction and analysis, (6) spatial and statistical analysis and (7) digital elevation model-specific digital methods, such as shaded relief models, digital cross-sections and 3D surface modelling. A sequential modelling scheme was developed and implemented to analyse two selected study sites, in Hungary and NW Greece on local and regional scales. Structural information from other sources, such as geological and geophysical maps, remotely sensed images and field observations were analysed with geographic information system techniques. Digital terrain analysis methods applied in the proposed way in this study could extract morphotectonic features from DEMs along known faults and they contributed to the tectonic interpretation of the study areas. (c) 2005 Elsevier B.V. All rights reserved.},
	year = {2005},
	eissn = {1872-826X},
	pages = {163-182}
}

@article{MTMT:1329290,
	title = {Morphometric analysis and tectonic interpretation of digital terrain data: A case study},
	url = {https://m2.mtmt.hu/api/publication/1329290},
	author = {Jordán, Győző},
	doi = {10.1002/esp.469},
	journal-iso = {EARTH SURF PROCESS LANDF},
	journal = {EARTH SURFACE PROCESSES AND LANDFORMS},
	volume = {28},
	unique-id = {1329290},
	issn = {0197-9337},
	abstract = {Tectonic movement along faults is often reflected by characteristic geomorphological features such as linear valleys, ridgelines and slope-breaks, steep slopes of uniforin aspect, regional anisotropy and tilt of terrain. Analysis of digital elevation models, by means of numerical geomorphology, provides a means of recognizing fractures and characterizing the tectonics of an area in a quantitative way. The objective of this study is to investigate the use of numerical geomorphometric methods for tectonic,geomorphology through a case study. The methodology is based on general geomorphometry. In this study, the basic geometric attributes (elevation, slope, aspect and curvatures) are complemented with the automatic extraction of ridge and valley lines and surface specific points. Evans' univariate and bivariate methodology of general geomorphometry is extended with texture (spatial) analysis methods, such as trend, autocorrelation, spectral, and network analysis. Terrain modelling is implemented with the integrated use of: (1) numerical differential geometry; (2) digital drainage network analysis; (3) digital image processing; and (4) statistical and geostatistical analysis. Application of digital drainage network analysis is emphasized. A simple shear model with principal displacement zone with an NE-SW orientation can account for most of the the morphotectonic features found in the basin by geological and digital tectonic geomorphology analyses. Copyright (C) 2003 John Wiley Sons. Ltd.},
	year = {2003},
	eissn = {1096-9837},
	pages = {807-822}
}