FROM PEBBLES IN THE UNDERGROUND TUNNELS “RAVNE” TO CONCRETE BLOCKS ON THE BOSNIAN PYRAMID OF THE SUN
21 January 2010
Dr.sci. Sam Semir Osmanagich
Founder of the "Archaeological Park: Bosnian Pyramid of the Sun" Foundation
Foreign Member of the Russian Academy of Natural Sciences
Under the Bosnian Valley of the Pyramids exists a huge underground network of tunnels and chambers. These tunnels had been cut in conglomerate rock. Based on density and a phase of cementation it can be concluded that this conglomerate is of rather recent geological age (tens of thousands of years). It's origin is in prehistoric glacial deposits. Conglomerate rock consists of rounded pebbles.
Huge quantities of conglomerate rocks had been extracted during the construction of underground labyrinth. This material had a potential to be used as a building material. Sure enough, blocks discovered under the layer of soil on Bosnian Pyramid of the Sun, show the presence of rounded pebbles in huge quantities. Material is exactly the same like the one present in underground tunnels.
It's logical to conclude that the ancient builders had no waste of the material: what they extracted from the underground was used in process of coating of the Bosnian Pyramid of the Sun.
Lab testing in five scientific institutions in Bosnia and Italy confirmed the artificiality of the cemented concrete on the Bosnian Pyramid of the Sun.
Very important question about the source of material is answered at this time: the source of material! Conglomerate rocks and clay were available to ancient builders in quantities.
Years in front us should give us answers on logistic: transportation, process of heating, source of labor.
Tunnels had been cut through the conglomerate. Conglomerate rock is a common sedimentary rock. Type: clastic. Color: variable. Texture: rounded pebble to cobble sized grains (finer grained matrix). Origin: river and glacial deposits. Common material: quartz, feldspars, micas, calcite, clays. Use: building material.
Age of conglomerate sedimentation: over 32.000 years. This projection is based on a piece of wood found in conglomerate (140 meters from the entrance, 5 meters below the surface, one meter above the layer of clay/marl). Radiocarbon dating of the wood performed in Germany (Christian-Albrechts University in Kiel) has shown the age of 32.000 years and dating in Poland (University of Technology in Gliwice) has shown the age of 34.000 years. The sediment has not been deposited very long time ago because of lots of visible open spaces/pores.


