Fenyves-forrás

It's not happening right now

It didn't happen when we went there.

At the beginning of the valley, which starts from the northern edge of the Szadó-roof, there is an immersion spring with a stone-paved reservation and a nameplate. It occurs at the junction of the K and P signs. There is no permanent outflow at the site of the reservation, as it only drains after longer periods of rain. Other times - in the drier months, the water appears at a deeper location than the reservation, which originates from the Lower Triassic sandstone distribution area. Its yields change frequently accordingly, and water application also occurs in the foreground, so the yield of its stream is sometimes significant. The source has an outflow only intermittently (rarely, mostly only during snowmelt), its yields vary between 0-30 liters / minute. In dry periods, water leaks can be observed in the valley below it, but with the onset of the dry period, they gradually subside, until eventually only those at the lowest surface area have runoff.