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What factors determine which part of the cliff will be “eaten” by salt crystals?

Numerous small pits on cliff surfaces have been noted by almost everyone who visited some of the sandstone rock cities. These pits are called honeycombs. Long ago, they were believed to form by wind erosion. For some time already, they have been understood to be shaped by a different mechanism: their origin is largely contributed by the crystallization of salts from groundwater/pore waters. A paper on this topic was released in the February issue of the Geomorphology journal: it brings additional evidence for the origin of honeycombs and, using dye experiments, documents the crucial role of the reach of hydraulic field in this process. This field, or, more exactly, its margin (i.e., the evaporation front) controls the sites of salt crystallization hence also the way the cliff surface is shaped by the salts. More information can be found in the paper, which was also contributed by scientists of the Institute of Geology: Michal Filippi as a co-author, and Jan Rohovec and Šárka Matoušková as analysts.

In memory of Jiří Fiala

This week, we learned a very sad news about the death of our colleague ing. Jiří Fiala, CSc.
Jirka graduated from University of Chemistry and Technology in Prague in 1961. His whole professional life was connected with the Academy of Sciences. He completed his post-graduate studies in the Institute of Geochemistry and Mineral Resources of the Czechoslovak Academy of Sciences. After the re-organization of the Czechoslovak Academy of Sciences, he was working in the Institute of Geology until his death. He was the Director of this institute in years 1991–1993. From the year 2008, he was an emeritus scientist of the Czech Academy of Sciences.
Jirka was a very successful scientist, measured by his publications. He specialized in geochemistry and petrology of metamorphic and magmatic rocks. In his research, he collaborated with many colleagues from abroad. Besides others, he can be credited for the foundation of the laboratories of mineral separation at the Institute of Geology.
Jirka had very open and friendly relationships with his colleagues, always willing to share his broad field experience and scientific knowledge.
With Jirkaʼs decease, the Institute of Geology as well as Czech science are losing a significant scientist and an outstanding personality. May the memory of him be honoured.
The last respect will be paid in the Church of the Most Sacred Heart of Our Lord in the main cemetery of Vimperk at 1 p.m. on Friday, February 16, 2018.

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