Fenyves-forrás

It's not happening right now

It is located at the beginning of the valley that starts from the northern rim of the Suvor roof. It is also a source of stones with nameplate and nameplate. It comes at the juncture of the K and P signals. There is no permanent discharge at the site of the reservation building, after which there will only be water leaks after longer rainfall. At other times - in the driest months, a deeper spot is made at the time of booking, which is due to the appearance of the lower part of the Triassic Sandstone. Its yields often change, and waterlogging is also in the foreground, so its yield is sometimes significant. The source is spilled only intermittently (rarely, mostly only at snow melting) and its yields vary between 0-30 liters / minute. In dry periods, downstream of the valley you can observe water leaks, but with a dry period, you gradually fall off until you are finally in the lowest spot.

It didn't happen when we went there.