Abstract

With an intersection on modern technologies into the sphere of geodesy and geophysics, there increase the number of possibilities of these technologies to be used. There are also ways to make the research and measurements more attractive for general public. There can be not only interest in the way of final results but also from the processing points of view. For example the sizes of historical sites need to be measured but the semi-product of processing can be also 3D model of the object. This product can be used for increasing of object attractiveness or as a base for next research. This is also the direction needed to be selected, to make the science more attractive and interesting for the public.

Highlights

  • IntroductionThe chapel of St. Marys Assumption is placed near city Púchov, Trenčín region, Slovakia

  • The method of microgravity is one of the basic methods in geophysical research. It depends on measuring and calculation of gravity anomalies that are directly connected to the weight as well as to density, these anomalies can be interpreted as density anomalies in subsoil

  • Bought methods shows the same result of an existence of anomaly, which is represented by absence of gravity in left part of the object

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Summary

Introduction

The chapel of St. Marys Assumption is placed near city Púchov, Trenčín region, Slovakia. Marys Assumption is placed near city Púchov, Trenčín region, Slovakia It was built round 1880 in neo-Baroque style as a one-sided sacral structure with two identical towers. The construction was initialized by Florián Augustín Balogh (18211898), who acts in local church as a Roman Catholic priesthood in 1846-1898 He was known as a Slovak historian, and as promoter of a modern industry and fruit-growing. He was buried hand in hand with the parents and brother in this chapel. The measurement was focused on observation and research of the subsoil. There were no found some graves so there was supposition of being of underground cavities or tombs in subsoil

Geodetic measurements of the area
Microgravity measurements of the area
Conclusions

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