Mgr. Ivo Baroň, PhD.

portret
I am a geoscientist with an interdisciplinary background in structural geology, geomorphology, applied geophysics and engineering geology, preferably focused on active tectonics and deep-seated landslides. I achieved my PhD degree in 2005 at Masaryk University Brno, Czech Republic, being focused on structure, dynamics and history of deep-seated slope failures in the Outer Western Carpathians. In 2013-2017, I held a postoc position at the Natural History Museum Vienna in the framework of the Austrian Science Fund (FWF) Project “Active tectonics and recent dynamics of micro-displacements along major fault systems of the Eastern Alps registered in caves (SPELEOTECT)”.

My major current research interests include present-day kinematic behavior of active faults in the Eastern Alps with respect to a seismic cycle, near-surface crustal stress variations associated with fault creep, and electromagnetic emissions due to rock deformation. I maintain the “Speleotect Network” consisting of high-resolution three-dimensional extensometers at active faults in the Eastern Alps. During my research career, I have achieved a broad experience with a variety of near-surface geophysical methods, such as ERT, GPR, airborne geophysics etc., mostly for surveying and monitoring large landslides and active faults. Besides of that, I have cooperated on several natural hazard projects, governmental programs and expeditions of the Czech Geological Survey and the Austrian Geological Survey. Scientific outcomes have been published in 33 articles in respected Scopus-indexed journals. My dissemination experience also comprises organizing international conferences, editing special issues and lecturing for the public.

I have also collaborated on development of innovative geophysical methods and devices. I published a new method of infrared thermal detection of open fractures in deep-seated rockslides and unstable cliffs. I coordinate an interdisciplinary team with the Technical University in Brno, in order to develop a geophysical sensor ADBER for registering electromagnetic emissions in caves to study the emissions with respect to tectonic strain. I also contributed to development of a novel magnetoresistive system for contactless three-dimensional fracture monitoring. A novel numerical method for present-day stress inversion from a single near-surface fault was developed in a co-supervised PhD research based on my monitoring data and demands.
Publishing Activity

Baroň, I., Sokol, Ľ., Plan, L., Melichar, R. (2019): Gravitational and tectonic stress states attributed to a deep-seated gravitational slope deformation near the seismogenic Periadriatic Line fault. Engineering Geology 261. https://doi.org/10.1016/j.enggeo.2019.105284
Baroň I., Plan L., Sokol, L., Grasemann B., Melichar, R., Mitrovic I., Stemberk J. (2019): Present-day kinematic behaviour of active faults in the Eastern Alps. – Tectonophysics 752, 1-23. https://doi.org/10.1016/j.tecto.2018.12.024
Sokol, L., Melichar, R., Baroň, I. (2018): Present-day stress inversion from a single near-surface fault: A novel mathematical approach. – Journal of Structural Geology 117, 163–167. https://doi.org/10.1016/j.jsg.2018.09.013
Blahůt, J., Baroň, I., Sokol, L., Meletlidis, S., Klimeš, J., Rowberry, M., Melichar, R., García-Cañada, L., Martí, X. (2018): Large landslide stress states calculated following extreme climatic and tectonic events on El Hierro, Canary Islands. – Landslides 15 (9), 1801-1814. https://doi.org/10.1007/s10346-018-0993-1
Baroň, I., Kernstocková, M., Melichar, R. (2017): Stress field reconstruction in an active mudslide. – Geomorphology 289, 170–178. https://doi.org/10.1016/j.geomorph.2017.04.020
Baroň, I., Plan, L., Grasemann, B., Mitrovic, I., Lenhardt, W., Hausmann, H., Stemberk, J., Can deep seated gravitational slope deformations be activated by regional tectonic strain: first insights from displacement measurements in caves from the Eastern Alps. – Geomorphology 259, 2016, 81-89. https://doi.org/10.1016/j.geomorph.2016.02.007
Baroň I., Bečkovský D., Míča L. (2014): Application of infrared thermography for mapping open fractures in deep-seated rockslides and unstable cliffs. – Landslides 11: 15–27. https://doi.org/10.1007/s10346-012-0367-z
Baroň I., Kernstocková M., Faridi M., Bubík M., Milovský R., Melichar R., Sabouri J., Babůrek J. (2013): Paleostress analysis of a gigantic gravitational mass movement in active tectonic setting: The Qoshadagh slope failure, Ahar, NW Iran. – Tectonophysics, 605, 70-87. https://dx.doi.org/10.1016/j.tecto.2013.07.020
Baroň I., Agliardi F., Ambrosi Ch., Crosta G.B. (2005): Numerical Analysis of Deep-Seated Mass Movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic). –Natural Hazards and Earth System Sciences, 5, 367-374, EGU. https://doi.org/10.5194/nhess-5-367-2005
Baroň I., Cílek V., Krejčí O., Melichar, R., Hubatka F. (2004): Structure and Dynamics of Deep-Seated Slope Failures in the Magura Flysch Nappe, Outer Western Carpathians (Czech Republic). –Natural Hazards and Earth System Sciences 4, 549-562, EGU. https://doi.org/10.5194/nhess-4-549-2004

My teaching experience comprises selected courses at Masaryk University on Structural Geology, Methods of Geological and Hydrogeological Research, Physical geology, and Slope failures. I consider forming young people as an important part of my activities since being a scout leader in the 1990s. Teaching also gives me an excellent feedback on my research, not only during the courses, but also in co-supervised bachelor, diploma and PhD theses.
Memberships

International Association for Engineering Geology and the Environment
European Geosciences Union, Czech Association of Geomorphologists
Austrian Geophysical Society
Speleological Society of Vienna and Lower Austria

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Journal / Book

Ten years of earthquake research underground

Carinthia is also a geological view of the border area. From Lesachtal in the west to the Jauntal in the east, the periadriatic seam stretches. A fault line in the rock that was formed in the course of Earth's history. Since 2014, research has been conducted in the obiro caves. The goal is the earthquake prediction. 
The pal.Idriatic seam stretches from west to east throughout the Alps, from Piedmont in Italy to the north-east of Croatia. In some cases, it is only recognizable by geologists, but in some areas it is also visible, for example in the obircad caves near Bad Eisenkappel. Ivo Baron is a geologist at the Czech Academy of Sciences and, with his research team in the rock fracture line, installed measuring instruments in the obircave to record these movements in the rock. It is a globally unique research project: “Our group is the only one in the world that can make three-dimensional measurements in the microometric field of disturbances.”

Image
Článek Ivo-baroň-ORF-Ten years of earthquake research underground
Measuring instrument TM 71

Audio

Ten years of earthquake research underground

Carinthia is a border region from a geological point of view. The Periadriatic Seam stretches from the Lesach Valley in the west to the Jaun Valley in the east. A fault line in the rock that was formed in the course of the Earth's history. Research has been carried out in the Obir Caves since 2014. The aim is to predict earthquakes. 

Radio Carinthia afternoon broadcast, programme "Experience nature" (Interview with Ivo Baron from the Department of Engineering Geology about research in the Alps, 3:16minut)

Seminar / Workshop

Taiwan-Czech republic Workshop on Slope and Active Tectonics

Taiwan-Czech Republic Workshop on Slope and Active Tectonics jointly organized by the ARDWC and National Cheng Kung University, successfully concluded. This workshop brought together geological experts from the Institute of Rock Structure and Mechanics (USMH), Masaryk University and National Cheng Kung University. Professors and students from various Taiwanese universities were also invited to participate, engaging in in-depth discussions on topics related to deep-seated landslides and active tectonics. 
During the workshop, experts shared their research findings and experiences, covering fascinating topics such as oblique thrust to strike-slip, application of magnetic susceptibility anisotropy to active faults and landslide masses, and other topics. Participants attentively listened, fostering rich intellectual exchanges that propelled advancements in the geological field.

Video

Detecting plate tectonics micromotions for potential earthquake prediction (Bewegungs Melder)

TV Report on the measurement of fault activity using the TM71 extensometer in the Vienna Basin, Austria.

ORF TV, program Mayrs Magazin - Wissen fuer alle

Journal / Book

Erdbebenforschung in Obir-Höhlen

ORF Radio Kärnten

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