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Exploration in the furthest reaches
of Poland's deepest and longest cave
- Jaskinia Wielka Śnieżna
Rafał Mateja, Marek Wierzbowski
Sekcja Grotołazów Wrocław

 


During the nineties exploration in the system of the largest and deepest cave in Poland flourished. Independent groups of cavers discovered many new passages in different areas of this vast cave system. Connecting the Wielka Snieżna with Wielka Litworowa and Wilcza gave the system two new entrances, extended its length to over 20 kilometers and its depth to 816 meters. The Śnieżna cave was discovered in 1959, and over the course of time it was connected with other caves in the area. The exploration of its main parts was already finished in the sixties, although during the seventies and eighties new sections were explored, mainly by climbing or diving.

Westward Expansion

Jaskinia Śnieżna
- one of the largest pitches

The idea of extending the system horizontally in the direction of the insufficiently explored massifs of Krzesanica and Ciemniak was born in the early 90s. A group of Wrocław cavers directed by Witold Jokiel made the first discoveries extending the system in westward direction. The extension of the Galeria Krokodyla was found and in the January 1996 Jaskinia Wielka Litworowa was connected to the Wielka Śnieżna.

The difficulties encountered in the Galeria Krokodyla and its great distance from the entrance made it the most challenging exploration project at that time. Galeria Krokodyla extensive passageways are a series of ramps and domes connected by often small, uncomfortable, slippery canyons. All that prepared us for what was to come after discovering this new extensive section of the cave called .
"If I had only known that it would be so bad I would have stayed for another year in the army instead of coming here" - these words belong to one of the cavers from Wrocław who after finishing his mandatory army service visited Przemkowe Partie.
Przemkowe Partie are a fragment of Wielka Śnieżna cave system. They start at the end of a passage called Biała Woda, and extend westwards under the metamorphic outlier of the Małołączniak massif. Its furthest reaches lie under the neighboring Litworowa valley. The majority of the passages within the Przemkowe Partie are located on W-E faults, which are similar to the ones dominating Śnieżna cave. The exploration of Przemkowe Partie is an extension of the idea of exploring the cave in the northwestern direction and is the most significant exploration project undertaken in the Tatra mountains during the last five years.

The discovery

Climbing in Partie za Kolankiem

The first discoveries in the Przemkowe Partie were made in October 1994. At that time a long dig with significant airflow yielded 100 meters of very tight passage, which led to the base of the dome. A few meters off the floor of this dome a small and uncomfortable passage was discovered. The dome itself was later used as a place to camp, and the passage lead into an extensive cave system with three independent water flows. Two of which supply more water than Śnieżna on comparable depth levels. Half year later, after a break caused by extensive snowfall, five in cave bivouacs were organized. It was the most intensive time of exploration and at the time all the easy leads were checked. Many of leads still remained, but all of them required difficult climbing or passing through very tight squeezes. An extensive set of climbing equipment had to be added to the exploration gear.

Competition

The continuous problems of accessing the cave through the snow-covered entrance drove us to areas where discovering a new entrance was possible. So in 1996 Partie za Kolankiem section became the target of our exploration. The whole project started when three consecutive trips did not reach Przemkowe Partie. Since the access to the Przemkowe Partie is very time consuming and hard all the trips there were well planed and involved long in cave camp in. However the large amounts of snow sucked into its entry sections of the cave made it often impossible to enter. Many hours of digging and constructing an igloo and tunnel system were required to reach the cave entrance itself. The suction generated by the cave was so strong that if the tunnel was left open it took only couple of hours for the cave to suck sufficient amounts of snow to block the entry passage and trap the cavers. Unfortunately this happened on a number of occasions.


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POLISH CAVING 2001
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