Showing posts with label cave. Show all posts
Showing posts with label cave. Show all posts

Fortress Valley Cave

Peştera Valea Cetăţii (the Fortress Valley Cave) is located near Râşnov, Braşov County, Southeastern Transylvania, Romania.


The cave was first opened in 1949, when a hydraulic blowup removed a rock and caused a huge flood in the Fundata valley. In 1954, a group of young from Râşnov managed to enter the cave through the opening. Margareta Dumitrescu and Traian Orghidan conducted the first study of the cave complex in 1958 and published a description and a sketch of the cave, indicating its length of 270 m. In 1981, a team from "Emil Racoviţă" speleological club in Bucharest have mapped 857 m with a 36m level difference. In 1988 and 1989 were mapped another 63 m, respectively 38 m, with a level difference of 38.5 m and a development of 958 m. The cave has undergone a continuous process of destruction due to uncontrolled access to various visitors.


Since February 2010, the protected natural area of ​​the Fortress Valley Cave is in the custody of a firm. From this time, the damage of the karstic formations was fortunately stopped, and the cave was set up using the latest technology. The cave was opened for visiting by the public in December 2010 after a titanic work of restoration. Due to the amazing acoustic of the cave, it used also for classical music concerts.



Photos from here

Buhui Cave

The Buhui Cave is situated on the left slope of the Buhui Valley in the mountains of Anina, Southwestern Romania, at an altitude of 600 m. With a length of 3217 meters, the cave Buhui is the second longest cave in Banat and owns one of the longest underground routes in Romania; the Buhui Rivulet forms inside the cave several lakes and waterfalls.


The Buhui Rivulet is a tributary of the Caraş River in Romania. The river first flows through Buhui Lake. Thereafter it flows through the Buhui Cave and, after emerging from the cave, flows through a reach of narrow gorges before joining the Caraş River.


The cave has a gallery of various sizes, with many turns and a few big rooms along. Both of the main gallery and the rooms start as short side galleries, the end is clogged with concrete or alluvial material. The Buhui Creek appears in upstream end of the main gallery, receives the tributary stream Certej next the entry with the same name, partially losses water through sinkholes and some tears. It completely disappears next the second entry (Dolina, 975 m downstream), then it reappears 108 m downstream through an intermittent spring, forming waterfalls and deep domes up the dam at Buhui entrance. The cave can be crossed from one end to another, but to avoid more difficult obstacles is recommended the use of the three successive entries.


The Buhui Cave is impressive not only in size but also by the wide variety of galleries and halls with concretions and fossils. It has a great scientific importance due to its karst hydrology and bio-speleological aspects. Therefore it was proposed in 1969 as a speleological reserve.


Photos from here

Valea Rea Cave

Peştera Valea Rea (Eng. approx. Bad Valley Cave) is located in Apuseni Mountains (Western Carpathians), in the North-West of Padiş karstic plateau, near Pietroasele village, Bihor County, at 1300 m altitude.


The karst from the area of Cârligate – Valea Rea is special because of the first poli-genetic endokarst of Romania. Valea Rea cave (21 km long) began its evolution due to post-magmatic hydrothermal substances, associated to the eruptive area of Vlădeasa. These created a mineral hydrothermal paleokarst and a relict hydrothermal karst. As a consequence of the end of post-magmatic activities and of the lifting of the northern Bihor Mountains block during the Pliocen age, the pre-conditions for the formation of a classic endokarst of cold water, which partially re-organised the previous spaces, appear.


The Valea Rea Cave, besides the fact that it is one of the most complex caves of the world, is also Romania's greatest underground mineralogical "museum". Over 37 different minerals described as components of some speleological formations - speleothemes (cave pearls, gyps, quartz, celestit, malachite, rhodochrosite, metatyuyamunit etc.), a lot of these being described for the first time in speleologic environment - place this cave among the World's top 10 caves. It is also the most complex cave system in Romania (developed on about 20 km) including mineralized hydrothermal paleo-karst (including native gold veins), relict hydrothermal but also cold water endokarst. The cave has the greatest vertical underground waterfall of Romania (the Ventilator Fall): 82 m high, 10 m diameter. It is the largest Romanian cave entirely developed in dolomite.


The Valea Rea Cave measures 21 km in length, and after the entrance (only 1 sqm) follows a system of deep ravines up to 120 m, and then continue with the galleries, shafts, vertical chimneys and spacious rooms. Unfortunately, the cave can't be visited since it was declared a scientific reserve. (Infos from Apuseni Natural Park site).

Isverna Cave

The Isverna Cave (Romanian: Peştera Isverna or Izverna; 600 m altitude) is located in Mehedinţi County, South-Western Romania. As famous as the flooded caves in Mexico, Florida or the Alps, Isverna is passed by the largest karstic spring in Romaniaa, and still retains the charm that made famous the natural wilderness of the Romanian Carpathians. That is why, from a desire to maintain it, the cave was declared a speleological reserve. Here is an ideal place for speo-scuba diving, visited every year by hundreds of divers all over the world.


The cave was first explored by the bio-speleologist C.N. Ionescu, on a length of 200 meters. In 1914 he published a description of this section, and in 1951 P.A. Chappuis and A. Winkler made a more detailed description. Between 1964-1967 V. Decou made a bio-speleological research, and in 1973, C. Goran made a cave plan published in 1976. The "Living Fire" speleological team led by S. Roată, re-mapped the cave November 1979, discovering new galleries, so that the current length was 1,500 m. The same year began the diving exploration, with promising results, and continued in 1980 when Florin Paroiu and Costel Vanau hunted, cave diving pioneers from Romania, were first that passed the Green Siphon (50 meters long), then the shorter Yellow Siphon.


It followed the exploration of a gallery with water 1.5 m deep and strong currents, ended by the Black Siphon - the longest in Romania (over 400 m and a negative bump of 40 m). In the early '90, Jacques Yves Cousteau came here with a team of cavers and divers. In January 2005, Gabor Mogyorosy and Mihai Baciu passed the Black Siphon and found hundreds of meters of galleries, of which 300 m of active galleries. So far have been explored since the beginning of Black Siphon over 1800 m of galleries. Exploration continues today due to high potential of the cave and to the discovery of new siphons at the end of the flooded gallery.


It is said that in the cave is hidden a silver treasure of the Empress Maria Theresa. In March 2010, speleologists made an amazing discovery in the cave: in an completely isolated room, they found a unique species of little birds, resembling to the bats. Those birds hadn't ever a contact with the exterior (the access gallery is flooded), but they reacted to the light and hid in the cavities of the wall. In this room the researchers found also some circular objects with a diameter of around 1 m, with strange signs, much heavier than the lead. The area of the objects is much colder.


Images from Drobeta Turnu-Severin

The 100 million years concert hall

Românești Cave is located in the south-east of the Românești village, on the left slope of Fărăşeşti Valley, in Poiana Ruscă Mountains, Timiș County, Banat, South-Western Romania. The cave is famous for its great acoustic and the concerts played here.


The Românești Cave is 1,450m long and has three different levels. The entrance is oriented north by northwest and is 9.5m wide by 2m high, allowing a diffuse illumination for 70m. The three levels have sub-fossil character, and the main rooms were formed at the intersection of several faults. The third level is accessible only for speleologists. Geographer T. Orthmayr made the first geological and natural research and exploration in 1872. He, and later researchers, found archeological artifacts from the Musterian Culture (over 15,000 years ago), from Tisa and Coțofeni Cultures, bear cave bones - that are on display in the Banat Museum in Timișoara and the Museum of Natural History in Lugoj.


On October 11, 1984, Romania had a unique and beautiful cultural event - the first symphonic concert in a cave. Three hundred and sixty visitors entered into the cave-hall lighted with candles, lamps, projectors, to hear it. Since then, every October comes with a new concert. Live concerts in caves are extremely rare, and Romania hosts the only annual speleo-concert. In Gibraltar are sometimes concerts in a small cave that can fit 30 people, while in the Românești Cave were 5,000 spectators at the concert of master Ştefan Ruha!


Images from Agenda, Speleophilately and Wikipedia.

Old Man's Cave

Peştera Bătrânului (Old Man's Cave) is located in Northwestern Romania, Bihor County, in Pădurea Craiului Mountains, on Zece Hotare (Ten Borders) karstic plateau, at 570m altitude. It was explored for the first time by G. Czaran in 1905 and between 1961-1963 was mapped by the researchers of "Emil Racoviţă" Institute of Cluj-Napoca.


Image from here

The Peştireu Valley Rivulet run through the Old Man's Cave, the Vadu Crişului Cave, then the waters surfaces and flows into Crişul Repede River. The Old Man's cave has a total length of 1633m, and develops on several levels. The Superior Complex has a total length of approx. 500m, and it is beautifully concretionated. By the down passage one can reach the underground stream, but here just after the descent of a 6 meter jump, that turns in a cascade on high waters.



All the cave, but especially the upper floors are beautiful concretionated, with stalactites, stalagmites, domes, columns, coralites, drawers, parietal flows, erosion formations. It can be visited only by those who have experience and special equipment, (a 10 m speleology ladder, protective clothing, and means of illumination). The air temperature is 9.2 °C and the water temperature is 8.6 to 10.2 °C. Here can be seen the coleoptera Duvalius redtenbacheri biroi and Pholetion (Parapholeuon) moczaryi.



Photos from Welcome to Romania

Şugău Cave

The Șugău Cave is located n the Giurgeului Mountain, 1568 metres above sea level, on Șugău Creek, flowing out from the cave. The creek is fed by the karst water gathered in the mountain. One can come close to the cave from the Voșlăbeni village, on the road Gheorgheni - Miercurea Ciuc.


Vizualizare hartă mărită

The Șugău cave was formed 65 million years ago, in the Paleocene Period, as a result of folding movements. The spatial position of the cave system is characterized by tectonic pre-formation. The multi-level passage of the cave was formed along the lithoclasses and faults of the dolomite, granular limestone, in mezo-metamorphic crystalline shale sequence of the Rebra series. The granular limestone, along which the passage was formed, requires an exact, specialized identification, as at the mouth of the creek there is no more limestone, its place was taken by crystalline shale up to the summit.


The cave is divided into 4 large galleries: dry passages 1 and 2, which were formerly seepage, the "Túlfolyó-brach", and aqueous passage, active even nowadays. The dry passage 1 is supplied with iron door, it can be visited, but it needs renovation. The first hall is the "Dressing room", it is a recess similar to a domed cellar. Here shifted their clothes the speleologists in the period before the hospice was built. The next hall is the "Conference Room", which in 1965 carrying out alluvial deposits made way for itself in the direction of the larger halls. In this hall can be seen drip-stones. On the ceiling of the hall can be seen the snow-white, mild drip-stone deposit, called lublinite (mountain milk, rock milk). Some metres further from there can be found cauldron like forms: "The Giant Owl Eye" and "The Mother-in-Law's Mouth". On the right inwards can be seen "The Fairyland Passage"; for its walls are characteristic the stalactites. The "Bastion" is the largest stalagmite of the cave; next to it is the "Mouth of the Wolf". In the stalagmite encrustation can be found the "Altar" and the "Pagoda". The stalagmites of the Șugău cave are postgenomic, that is to say they developed after the formation of the cave recess. Its base material is calcite and aragonite.


There can be found also halls and formations such as the "Whirlpool Hall", the "Connecting Passage", "Miklós Hall", the "Triumphal Arch" and the "Bat Boneyard", the "Petrified Waterfall", the "Stalactite Cemetery", the "Concert Hall". The largest hall of the cave is the "Large Hall". A sharp descent leads in the direction of its base, from there starts a low passage towards the lower levels. In the lower part of its wall calcite crystallines can be found. Downwards from this hall we find the "Crystalline chimney", which walls are covered with crystalline.


The most mysterious and the most studied passage of the cave is the "Aqueous Section". This active passage is the most difficult passable section of the cave. The average water output of the creek, which flow over the cave, is 30 l/sec. The water temperature, in comparison with other cave creeks, is very low 5-7 centigrade degrees. Leaving the mouth, one can follow the creek along 40 m inwards. On the right there are very dangerous and slippy avens. This passage is a large tectonical faultage, which walls moved away from each other, forming a joint. It is worth mentioning the "Lamp Cemetery", which is a vertical shaft, and it is the most important part of the joint. An interesting formation of the lublinite precipitate is the "Stalactite Sources".


The excavated soil and debris during the exploration aggraded the creek, so only in one passage can be followed its flow. Our pass on is obstructed by a water trap. The other by-pass passage is also blocked by water. On the left, before the water trap a stalactite flow hangs on the wall.


The atmosphere is rich in carbon dioxide. Due to the low temperature inside, the humidity level of the Șugău cave is 95%. The cave water contains a large amount of calcium carbonate. Despite the hostile conditions the cave has a small fauna, which consists of the Froglobion-family: springtails (Collembola), insects (Insecta).


The cave's only inhabitant are some species of bat: Myottis Natererri, which shoes up especially in winter time, single or in a group, settle down on the dry walls or on the ceiling of the cave; Greater mouse-eared bat (Myotis Myotis), Lesser mouse-eared bat (Myotis Blythi), Brown long-eared bat (Plecotus Auritus), Long fingered bat (Miniorterus schreibersi).

Adapted from here.

Decumarellus sarbui

Decumarellus sarbui is the first cave genus belonging to the Tyrini in the whole world; such a genus of the Tyrini tribe has never been signaled in a cave. It lives in Movile Cave, near Mangalia, Constanţa County, Southeastern Romania. The species is endemic for the chemoautotrophically based groundwater ecosystem at Mangalia and unique in the world.

Kingdom: Animalia
Subkingdom: Eumetazoa
Phylum: Arthropoda
Subphylum: Hexapoda
Class: Insecta
Order: Coleoptera
Suborder: Polyphaga
Infraorder: Staphyliniformia
Superfamily: Staphylinoidea
Family: Staphylinidae
Subfamily: Pselaphinae
Tribe: Tyrini
Genus: Decumarellus
Species: sarbui
Scientific name: Decumarellus sarbui Poggi, 1994

The genus Decumarellus is dedicated to the Romanian bio-speleologist Vasile Decu and at the same time reminds of the un-doubtful relationship with the genus Marellus. The species (sarbui) is dedicated to Romanian scientist Dr. Şerban M. Sârbu, from the Department of Biological Sciences of the Cincinnati University, USA.


Decumarellus sarbui shows the typical morphological adaptations to the live in caves. It might be the extreme result of the differentiation of a branch of the genus Marellus, which settled down in the hypogeus habitat and evolved independently, at least since the possibility of a link between the cave and the surface fauna came to a stop. According to the geological, hydrological and palaeo-geographical data, the isolation of the cave goes back to the end of Miocene (almost 5.5-5.2 millions of years ago) when the climate of the Southern Dobrogea got extremely dry in connection with the crisis of salinity from Messinian.

The Temple of the Fates

Nobody knows for sure how old the place is, no one really knows the temple’s origins. There are at least 5 different stories, from Paganism to Christianity or even Extra-Terrestrial! However some people say that it lasts 7000 years ago, some that it has Dacian origins, other say that it is of Christian origin because it has an eccentric altar and no proof that there was a cross, but the generally accepted version is that the monastery was set-up around 1742, when Orthodox churches were destroyed by the Austrian-Hungarians, bringing instead the Romano-Catholic Church or the Greek-Catholic Church. But, for sure, the place is holy, and its energy can help you - the cave monastery is known for its miraculous healing powers with people coming here every year to get healed and have their good wishes fulfilled.


The cave church is situated in Şinca Veche village, Braşov County. The abundant vegetation on the way to the temple is absolutely beautiful. The intense smell of myrrh, frankincense and burning candles came to one's awareness. There is a total calmness and stillness in the forest where the cave is located and the energy is divine.


A grotto hidden in the middle of the woods, in the heart of a block of grit stone looks like a cave dug into the mountain. The temple has large rooms cut into quartz in a technique similar to that used by the Dacians to cut huge blocks of stone at Măgura Călanului. There are several hemispherical, ellipsoidal, spiral-like or spherical diggings, connected by the huge secant, which crosses all the rooms connecting the sky and the earth, the spiritual and the material worlds. Inside are ceremonial chambers and altars with mysterious carvings, including a really strange Yin-Yang symbol within the Star of David, the Egyptian sign for "fishing rod", crosses, a Yin-Yang shaped window, a sphinx and other strange signs.


The "tower" of the church is invisible from outside and one can enjoy its beauty and the wonderful violet light it sheds only from the inside. On the pavement there are marked three places - claimed to be the energetic centers of the place. People say that if you pray over these places , your wish will be fulfilled. They say that the temple is a vortex of energy that attracts energy into an underground tunnel connecting the temple with the fortress of Râşnov. Whatever the reason, one can definitely feel some mystical, unexplained energy when is inside.





The Topolniţa Cave

Peştera Topolniţa (the Topolniţa Cave), not far from the hermitage with the same name, is situated in the central part of the Mehedinţi Plateau, in the Sohodol Valley, between the villages Marga and Păuneăti, clustered beneath the earth, have carved this picturesque cave, the 2nd longest in the country and the 17th in the world.


The Topolniţa Cave is actually a system of caves, loosing streams, and resurgences, so the plural is actually correct. The whole system is called sistemul carstic Topolniţa (Topolniţa hydrokarstic system). The main structure is a river which enters a cave, flows underground for some 600m and reappears in a spring called Gaura lui Ciocârdie (Ciocârdie's Hole), which is actually a narrow gorge or roofless cave. There are other streams entering the system and various caves.


The Topolniţa Cave was declared a natural protected monument. From the point of view of its galleries’ length (25km) this cave is the second after the Vântului Cave (the Wind’s Cave). The galleries of the cave are situated on four levels. The cave displays rich concretions (stalactites, stalagmites, curtains, stone pearls), halls, waterfalls, lakes, guano deposits. Inside the cave skeletons of cave bears (Ursus spelaeus) were found. The galleries have 12,000 m, on 5 floors, among which the gallery “Emil Racoviţă” is 1,570 m long. Inside the galleries there are spectacular shapes, called accordingly, as The Great Candle, and hosts species specific to the Southern climate. In the vicinity of Păuneăti village there is the Borovăţ Forest (56 hectares) with black pine mixed with beech and shrubs specific to the area.

An unique ecosystem

Movile Cave, located in Romania, a few kilometers from the Black Sea coast, near the city of Mangalia, Constanţa county, is probably one of the caves that have received the most attention during the last years, both from the mass media and from the scientific community.


The reason for such a high interest from such a diverse audience are various and spectacular:
* it is a peculiar, practically unique environment, until now the only cave ecosystem completely driven by chemosynthesis (chemosynthesis = production of organic molecules using chemical energy rather than light);
* it is an extremely small and fragile environment which deserves our protection;
* it is one of the richest cave ecosystems regarding the number of species;
* more than 30 new species for science were described from this cave, and all are endemic (i.e, they live only in this ecosystem);
* it can serve as a valuable model for understanding how life can thrive even in the absence of light and under extreme conditions;
* the history of its discovery and research is one of committment and dedication.


While excavating for a major construction project in 1986, engineers happened to find a cave in which extraordinary conditions prevail. Named the Movile cave, it is the site of a hitherto unknown groundwater ecosystem that is rich in hydrogen sulfide (8-12 mg/l) and in contact with an atmosphere poor in oxygen (7-10%), rich in carbon dioxide (2-3.5%), and also containing significant amounts of methane (1-2%). Its exploration began in 1990. Until research teams began exploring Movile Cave, its 12000 square meters were entirely sealed off. The cave had no natural entrance and was discovered by accident during some geological research in the area.


The entrance is represented by a shaft with a depth of 18 meters. With a total length of about 300 meters it is a relatively small cave with narrow passages covered with clay. It is developed mainly horizontal with some pits which do not exceed 3 meters. In its lower part there is a small lake which connects the cave with the groundwater table. The passages continue underwater and are forming 3 air bells where the atmosphere is very rich in carbondioxide (up to ten times more than outside) and poor in oxygen (one third of the outside atmosphere).


When Earth's climate changed 5.5 million years ago, the area went from being tropical to temperate. The only animals that survived were those living in warm caves underground. Movile Cave, is one of Earth's most unusual ecosystems, populated with invertebrates that have adapted -- through a process called troglomorphy -- to their underground prison. They have done this by losing pigmentation, learning to navigate blind, and surviving on bacteria and fungi that derive energy from the sulfide hot springs beneath the cave. The predatory leeches, rare water scorpions, and other inhabitants of Movile Cave are similar to species found in deep sea vent communities. They depend on chemoautotrophic organisms (users of chemical energy) instead of the more usual photoautotrophic organisms (users of photosynthetic energy). Forty-six species of terrestrial and aquatic invertebrates have thus far been identified to inhabit this ecosystem, of which 31 are of a previously unknown kind. The vast majority are anthropods belonging to the classes of Arachnida, Crustacea, Myriapoda, and Insecta. Eighteen aquatic species in the cave belong to the flatworms, round worms, microscopic animals related to round worms, segmented worms, etc. A blind leech, a snail, and a blind water-scorpion have also been identified. The discoveries include grazers such as four species of isopods, or pillbugs, six springtails, a millipede, and a bristletail. Among the new species of carnivores are two pseudoscorpions, a 2-inch-long centipede, a worm-sucking leech, four spiders, and a water scorpion.




Access into the cave is permitted only for research purposes with the permission of the custodians, trips into the cave are limited at two hours, twice a month while no more than 3 people can enter at the same time, clean footwear and coveralls have to be worn to avoid contamination of the cave, two gates and an airtight lid are protecting the cave from unauthorized access and influences from the outside (gas exchange, temperature fluctuations and species immigration).


The cave is declared as a protected area, both by the city council of Mangalia and by the Romanian Academy of Sciences and falls under the regulations of the Environmental Protection Law of Romania. The custody of the cave belongs to a consortium made up by representatives of the Group for Underwater and Spelological Exploration and the Local Council of Mangalia.

Ialomicioara

The upper course of Ialomiţa River was praised by famous Romanian writers; the old Ialomiţa, the axis of the settlement in this area, has is spring in the Bucegi Mountains at the foot of Omu Peak, being the cradle of life and beauty of this land, even from the Dacian times and of those before them. The supreme god of the Dacians was Zalmoxis, who withdrew for three years in a cave on the holy mountain Kogaion; after his disappearance, he was considered dead and mourned by his people, but in the fourth year he returned, episode that some considered to be a resurrection, thus it was a parallel to Jesus Christ's resurrection. It is said that the cave of Zalmoxis is the Ialomicioara Cave.



Nearby the springs, at the entrance in the Ialomicioara Cave, the faithful ones and the monks from the area have built an Orthodox monastic dwelling several times. The churches and the cells, being made from wood, have had burned out four times during the four centuries of existence. The last fire had destroyed everything in 1961. Starting from 1st August 1993, the whole complex was completely rebuilt, being now an astonishing place, charming our hearts and souls.


The Ialomicioara Cave has had a long history, being certified for the first time in 1510 when the Wallachian prince Mihnea Vodă cel Rău would had hidden here. But the cave was first described in 1793. Cezar Bolliac, Romanian writer of the 19th century, discovered in 1870 almost all the major galleries till the Bears' Hall. Formed on the direction of a fault orientated East-West, the cave had risen in the emptiness left between the two compartments. To this very main purpose had contributed the infiltration waters and the brook which dissolved and eroded the limestone. One effect of this movement is the presence of some big friction mirrors some dozens of meters high in the Bears' Hall and Hades Hall.

The Polovragi Cave

In the North of Oltenia, not far from Polovragi Monastery, the valley of Olteţ River develop in the Jurassic limestone from the South of Parâng Mountains and of Căpăţânii Mountains a very abrupt relief about 200-300 m, which shelter the beautiful Olteţ Gorges. The gorges, with parallel walls, at 3-4 m distance in the lower part and 10-20 m in the upper part, let pass only a little light, but one can see many erosion levels, with many caves, most of them inaccessible.


The biggest and the most interesting of the caves from Olteţ river is The cave of Pahomie from Polovragi, cut in the left side of the gorges at 200 m from the entrance. The name Polovragi comes from an ancient plant, called Polovraga, in the Carpathian Mountains, used by the ancient Dacians as a panacea in their medicine. Pahomie, a monk from the nearby monastery, lived here in the XVIIth century and made a few drawings on the walls.


A wall painting known as "The Death", or "The Grim Reaper".

Cornel Bălosu, a specialist from the Oltenia Museum, says that from the 5th century to the 17th century, the left side of the body was considered the devil's side, (this survives in English in the word "sinister" which derives from the latin for "left") so the image above keeps the scythe in the left hand. This image made in white on black is painted in simple colors, because in all paintings from the middle ages in churches, the colors used were white/yellow (for the bones) on a black background, the fearsome color of death. Also, the painting of Pahomie's Death keeps its head to the right, because the tradition is that if the left part of the body was evil, the right part was for the forces of good. So when someone died, the head was turned to the right, with force if necessary, when the body was placed in the coffin.


Photo by Sorin (Panoramio)

It is a long cave, over 27000 m (900m electrified), having the main gallery mostly horizontal from which starts some lateral galleries most of all clogged by alluvia. Along the gallery three sectors are distinct. First till the Gallery of the Pillar, and starts with two little side galleries the important one being the right one named Bats Gallery. The electrified gallery continues with 2-8 m height and around 10 m width. There are frequent falls, flows from the ceiling, chimneys; here are opening little secondary galleries adorned with lime.


The ogiva sector, bordered by the Pillar Gallery and the Suffocated Gallery, starts at approximately 400 m from the entrance. Have the same width, but its height vary from 0.5 to 2 m. Concretion rate is reducing. The last sector, the Suffocated Gallery at the Northern end of the gallery continues the cave till a clogged whirlpool. Here the height and the width are reduced, and the stalagmite formations are more frequent at the end of the sector. The cave is relatively warm, wet and without air currents. The biospeleology of the cave is not very interesting, having a poor fauna and single troglobiont specie: Trachysphera spelaea. The cave is interesting especially from geomorphologic and landscape point of view.