The Olomučany chert outcrops are located NNE of Brno in a relic of Jurassic sediments in the vicinity of Olomučany village. The layered chert intercalates in Callovian-Kimmeridgian limestones  . The chert has dark grey color and microscopically is formed by microfossils and opaque material partly by organic origin. The opaque material is colored rusty-brown due to the presence of iron oxides. Sponge spicules and bryozoans dominate the microfossils. The transparent material is formed by chalcedony and scarce crystals of macro quartz. The chalcedony forms the 0.2 mm spherulites and cryptocrystalline matrix. The spherulites are probably replaced microfossils  . The coarser grain size is typical for Olomučany chert that helps to macroscopically recognize from erratic flints encountered in Silesian and North-Moravian territory. A rare component of the Olomučany chert is glauconitic grains. A healed fissure acts as planes of weakness during flint-knapping of the chert. However, a heat-treatment of the rock improves the flaking properties.
The majority of flintstone sources at the North Moravia lies north of Nový Jičín towards the border of the Czech Republic and continues to Poland. The southernmost sediments that were probably used in Magdalenian era were transported during the Saale glaciation  . The flint is derived from Scandinavian chalk sediments of Maastrichtian to Danian age. The Campanian flints were not detected in the area. The macroscopic observation shows milky-white, yellow, brown, reddish-brown or grey colors with glossy luster. The microscopic investigation proves mostly pelagic origin with micritic primary texture. The Daanian flints are rich in Briozoas, while Mastrichtian flints are richer in remnants of shells, brachiopods and echinoderms  .
Heat-treatment of cherts and flints expands flaking quality and edge sharpness. This technique was used by prehistoric people throughout the world. Its oldest evidence in Europe comes from 24 to 17 thousand years old Solutrean archaeological sites at France and Iberian Peninsula. The following gap in using the technique took more than 6 thousand years before it was used in the Mesolithic around 9 500 years BP.
Similar technique could be identified in the Magdalenian (15,000 - 11,500 uncal BP) of Moravia (Czech Republic) where local Jurassic chert (Olomučany type) was used. Combination the Fourier-transform infrared spectroscopy (FTIR), mass magnetic susceptibility (MSmass) and measurement of isothermal remanent magnetism (IRM). FTIR is suitable to identify heat-treated chert above 300˚C. However, temperatures around 250˚C, are usually sufficient to improve flaking qualities of fine-grained quarzitic materials   .
The magnetic properties of flint in natural state are caused predominantly by magnetite, that is hydrated and oxidized during heat treatment. Majority of flints in the cave Balcarka contain also mainly magnetite, and only one contains also mineral with higher coercivity according to the Kruiver et al.  method is Goethite.
The iron oxide content of Olomucany chert is much more heterogeneous. The magnetic properties show mixture of magnetite and hematite. The pilot measurement shows that hematite is during heating transformed to a mixture of magnetite and goethite.
The results imply that the majority of flint artifacts were not heat-treated before clipping. Olomucany chert artifacts contain more magnetite than the control rock-samples, which could be interpreted as a heat treatment before the knapping, later non-intentional heating or quarrying different layers for tool making than are exposed today. The pilot results show that the heat treatment method was not used in the Moravian Magdalenian regularly, the method was not absolutely unknown.
FTIR and MS mass methods generally agree with the IRM acquisition method. Magnetic methods are therefore recommended to be applied in order to identify intentional and unintentional past heat-treatment of cherts and flints.
The research was founded by Czech Science Foundation project “Non-destructive determination of heated artifacts in Upper Palaeolithic assemblages”, number: 18-02606S. This is a contribution to UNESCO/IUGS/IGCP 679 project.