(C) dalciak
SK:
Obcasny vodopad v lesiku pri Siatorskej Bukovinke vznikol niekedy v obdobi stvrtohor. V tomto case bola oblast Cerovej vrchoviny vyzdvihovana zemskymi silami a potociky sa postupne zarezavali do starsieho pieskovcoveho podlozia. V maksich pieskovcoch vznikli hlboke jarky, v tvrdsich zasa terenne stupne. Erozia postupovala v protismere toku, preto je zvana spatna. Aj v tomto udolicku je vytvoreny hlboky kanon so spadom vysokym cca 8 m. A obcas nim tecie aj voda 
.
POZOR! Cache je ulozena dole v kanone, nehladajte ju hore na nebezpecnych svahoch! Pod vodopadom je velky balvan a o neho sa opiera kus padnuteho stromu. V dutine medzi nimi je krabicka (a mame tu aj spoiler). Na GPS sa nespoliehajte, dole je biedny signal. A pri pohybe pod skalnymi stenami pozor na uvolnene balvany - erozia je tu rychla a za posledne roky ich uz zopar popadalo.
Zdroj: Geosprievodca
Datum poslednej zmeny: 28. januara 2017
EN:
The occasional waterfall in the woods of Siatorska Bukovinka came to existence during the Quaternary Period. During this era, the area of Cerova vrchovina (Cerova Highlands) was being thrusted upwards by Earth forces, while the water streams were eroding their way through underlying older sandstones. In the softer sandstones, deep ravines were created. In the harder ones, terrain steps usually developed. The erosion proceeded in the opposite direction to the flow, which is called backwards erosion. In this valley, a deep canyon with an 8 m high fall developed. And sometimes there is also water flowing .
BEWARE! The cache is down inside the canyon. Please do not search on the dangerous steep slopes! There is a large boulder right below the waterfall. The box is in a hole formed by the boulder and a piece of fallen tree leaning to it (photospoiler avaliable). Don't count on your GPS, there is weak signal down there. And watch out for falling rocks while moving close to the walls - the erosion process is quite quick here, several boulders have fallen down lately.
Last modification date: 28 January 2017
