Uz v priekopnickych casoch prichadzali do Tatier ucenci skumajuci taje carovnej vysokohorskej prirody. Boli medzi nimi aj botanici zaujimajuci sa o bohatu kvetenu. Skutocnym botanickym rajom boli najma Belianske Tatry, kde sa na neobycajnej druhovej pestrosti podpisalo mineralne bohate vapencove podlozie. Botanicke exkurzie casto vedu najma do Doliny Siedmych pramenov zahlbenej do najvychodnejsej casti Belianskych Tatier. Dolina lezi pomerne nizko, zvacsa je skryta v lese, len najvrchnejsia cast siaha pod skaly na uboci Bujacieho vrchu, medzi ktorymi vynika pozoruhodny skalny utvar Skalne vrata. Na upati bral lezi mnozstvo skalnej sutiny, z ktorej vytekaju pramene. Ich pocet sa premietol do nazvu doliny. Dolinu v ladovych dobach nemodeloval ladovec, aj ked profesor Luknis pripusta, ze v case najvacsieho zaladnenia mohol bocny ladovcovy splaz pretiect z Doliny Kezmarskej Bielej vody cez Sedlo nad Cervenou hlinou.
Keska:
je pristupna po zltej turistickej znacke pesi alebo na horskom bicykli, ale zaverecna cast stupania je velmi narocna az zdolatelna len tlacenim. Druha moznost pristupu je po zelenej znacke na Chatu Plesnivec a potom naspat po zltej. Tretia moznost je zacat modrou turistickou znackou z Kezmarskych zlabov.
Prosim dobre zatvarat aby obsah nezmokol.
Valley seven of springs
Already in the pioneering times scholars coming in to the Tatras examining the secrets of magical mountainous nature. Among them were botanists interested in a rich flora. Real botanical paradise were mainly Belianske Tatry, where on the unusual species richness signed a mineral-rich limestone bedrock. Botanical excursion often lead mainly to the valley of seven springs recess in the easternmost part of Belianske Tatry. Valley lies rather low, mostly hidden in the woods, only the uppermost part extends below the rocks on the mountainside Bujaci hill among which stands out spectacular rock formations Skalne gate. Below the rocks lies quantity of rocks scree, from which leak out strands. Their number was reflected in the title of the valley. Valley of glacial periods does not model the glacier, although professor Luknis admits that at the time the largest glaciation could sideways glacier splaza to overflow from Valley Kezmarskej White water through the saddle above Red clay. .
Cache:
It is accessible on the yellow tourist sign walking or mountain biking, but the final part is a very difficult climb up maybe only pushing. The second approach is the use of green tourist sign in the chalet Plesnivec and down for yellow tourist sign. The third option is to begin a blue tourist signs from Kezmarske troughs.
Please close correctly so as content no wet.