Bugyogó-forrás

On the sign ZO from Mánfa and Budafa on the Z sign, not far from the Baranya creek, there is a dive, spout source at the top of the Rákos valley. The source higher than the median level was occupied by Sándor Csokonay in 1942. His inscription is engraved in a larger stone. The spring water escapes from the conglomerate sandy gravel on the Miocene Carpathian floor with a bit of buzzing under its name. This phenomenon is probably due to the presence of a more constricted, contoured bench. As a repulsive effect of the bench, the phenomenon of a slight sludge swirling, sometimes with piping, can be explained. Of the three places that are breaking up, but only one of them, the biggest of the water shows are marked with stones. Strong limestone drying can be observed from the spring water on the slope. Some of the more resistant limestone benches have been formed, and 5-6 lime walls can be recognized. The height of the stairs varies from 0.3 to 1.0 m. Rapid infiltration of dead plant residues falling into the brook cage is also typical. Water yield is stable at 15-25 liters per minute. The source is older than the Radnin source.