Sutinščica
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Sutinščica is the longest cave in
Zagorje Hrvatsko Zagorje (; Croatian Zagorje; ''zagorje'' is Croatian language, Croatian for 'backland' or 'behind the hills') is a cultural region in northern Croatia, traditionally separated from the country's capital Zagreb by the Medvednica mount ...
with of explored passage, and is located in the southern foothills of the
Ivanščica Ivanščica () or Ivančica is a mountain in northern Croatia. The highest peak is the eponymous Ivanščica at . Together with Strahinjščica it forms the Očura massif. The rivers of Bednja (river), Bednja, Lonja, Krapina (river), Krapina and ...
massif. Its depth is , but its total vertical difference is . It is a mostly horizontal cave, so its horizontal length of is close to its total length. Part of the cave is seasonally dry, while part requires specialised equipment. The opening keyhole passage opens up into a series of chambers, while the permanently submerged section further back remains unexplored.


Description

Sutinščica is a
ponor A ponor is a natural opening where surface water enters into underground passages; they may be found in Karst topography, karst landscapes where the geology and the geomorphology is typically dominated by porous limestone rock. Ponors can drain s ...
of average width and height along northward orientation from the entrance. The keyhole shape of this passage originated as the result of differential erosion between high and low water levels.
Speleothems A speleothem (; ) is a geological formation made by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depend ...
are present in the cave, but many have likely been destroyed by undocumented explorers. In wetter conditions, only are explorable without diving equipment thanks to a
siphon A siphon (; also spelled syphon) is any of a wide variety of devices that involve the flow of liquids through tubes. In a narrower sense, the word refers particularly to a tube in an inverted "U" shape, which causes a liquid to flow upward, abo ...
. from the entrance there is a sequence of two larger chambers, of dimensions 10×10×6 m and 13×9×4 m (length×width×height). Reaching these chambers is difficult because of narrow, muddy passages, the narrowest passage in the cave being the squeeze just before the entrance to the second chamber. Even at low water level, the cave typically ends in a small siphon, though its water level gradually lowers. A map of the cave as explored in 2021 has been published.


History

A cave "with two entrances" near Sutinske Toplice was first mentioned in 1889.''Narodne novine'' 1889(8). This information was relayed by in 1905. This information was repeated by Vladimir Redenšek in 1961 and by Roman Ozimec in 2011. It may or may not be the same as Sutinščica, but it is argued to be a strong possibility, and the search for that cave in 2021 is the reason the Sutinščica was discovered. Cavers from the section Kraševski Zviri first learned of the entrance to a spring cave in Mali Komor from local resident Božo Cerčić in January 2021, who told them that only miners had dared to enter it in the past. Sediment that had accumulated at the entrance had to be removed before it could be explored. The initial length explored on 14 February was , with no further exploration beyond the first siphon. It was already longer than Židovske jame, until that point the longest cave in Zagorje. The cavers returned on the 21st when conditions were drier, discovering about of new passageway, including two chambers. Topographic mapping continued on the 25th and 26th, with a new cumulative length of . This was followed by a photography expedition on 2 March. After the water level fell further, an expedition on the 11th was able to map the cave to , with little further activity carried out that year apart from a public presentation on the exploration of the cave. The main reason for abandoning further cave exploration in late 2021 and early 2022 was because in September 2021, a
CO₂ Carbon dioxide is a chemical compound with the chemical formula . It is made up of molecules that each have one carbon atom covalently double bonded to two oxygen atoms. It is found in a gas state at room temperature and at normally-encountere ...
concentration of 4% with O₂ at 17% was measured. Only after a second measurement in February 2022 showed a concentration in equilibrium with ambient levels could exploration resume, so on the 2nd a team entered the cave, mapping it to thanks to a side passage connection previously not noticed. An attempt to find a second entrance in 2023 was unsuccessful, although it did clean the area around the cave of a significant amount of waste. The water level did not permit significant further exploration that year.


Biology

Stygofauna Stygofauna are any fauna that live in groundwater systems or aquifers, such as caves, fissures and vugs. Stygofauna and troglofauna are the two types of subterranean fauna (based on life-history). Both are associated with subterranean environmen ...
include
isopods Isopoda is an Order (biology), order of crustaceans. Members of this group are called isopods and include both Aquatic animal, aquatic species and Terrestrial animal, terrestrial species such as woodlice. All have rigid, segmented exoskeletons ...
. The presence of etiolated seedlings of some plant species within the cave was also noted. A biospeleological expedition was carried out in 2023.


See also

* List of caves on Ivanščica and Strahinjčica


References


Bibliography

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Embedded video
on
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.


External links


Novosti Speleološke udruge "Kraševski zviri"
{{in lang, hr News page of its primary explorers Caves of Croatia