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Applicatopn dossier for nomination as a European Geopark ...

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crack through which it is possible to get in a cavity. The<br />

cave is low (0,7-0,8m) and wide (up to 4m), with the<br />

plane sandy bottom, almost without detrital gypsum<br />

material. The extent of the cave is about 12m. The<br />

depth from the surface is about 7m. It w<strong>as</strong> found in<br />

1995.<br />

Cave B<strong>as</strong>kunchakskaya. It is the largest cave in<br />

Northern PriC<strong>as</strong>pian. It is situated in the small flat<br />

bottom valley Pezherskaya. It h<strong>as</strong> been known <strong>for</strong><br />

about 100 years. The c<strong>as</strong>e h<strong>as</strong> three entrances. It is<br />

laid in the Perm gypsums of Kungurian stage. It is<br />

developed on a vertical crack of submeridional<br />

direction. Its extent is about 1480m. The depth from the<br />

surface level is 32m. Its volume is about 9400 cube. M.<br />

In a cave there is a underground lake the area about 10<br />

cubic meters. The cave w<strong>as</strong> investigated by the<br />

Saratov cave explorers in details in the beginning of<br />

80th years.<br />

Cave Devjat dyr. The cave is situated in the balka<br />

Pezchernaja. It is laid in karstic rest and located in a<br />

large karst-erosive hollow. It w<strong>as</strong> a part of the cave<br />

B<strong>as</strong>kunchakskaja earlier. The total extent of the cave is<br />

about 70m. As a whole the arch of the cave closely<br />

comes to the surface. The amplitude of the cave is<br />

0,6m. The cave h<strong>as</strong> many entrances of various sizes. It<br />

is e<strong>as</strong>ily accessible, that is why it is actively visited. The<br />

cave h<strong>as</strong> been known <strong>for</strong> a long time. For the first time<br />

it w<strong>as</strong> described by the Saratov cave explorers in the<br />

beginning of 80th years.<br />

Cave Оrgannaya. It is located in the middle part of the<br />

balka Belaya. The entrance is located in the b<strong>as</strong>is of a<br />

gypsum slope (e<strong>as</strong>t exposition) of northern from the<br />

top. The general extent of the cave is 22m at the<br />

relative depth is about 1m. The height of the arch is up<br />

to 2,5m. The depth of bedding from the steppe level is<br />

about 10m. It w<strong>as</strong> found and <strong>for</strong> the first time described<br />

in the beginning of 80th years.<br />

Cave Surprise. It is located to the north of the Belaja<br />

balka. The entrance is dated to a karstic hollow and<br />

opens with a steeply inclined 16-meter manhole. It runs<br />

to the hall with the area of about 16m2 and height up to<br />

3m. From the hall a very dirty channel, which length is<br />

about 28m, runs. Earlier in the middle of a channel<br />

there w<strong>as</strong> a small lake with the area of 6m2 and depth<br />

up to 1,5m. Since 2001 it h<strong>as</strong> not present. The general<br />

depth of a cave is up to 20m. It w<strong>as</strong> found and <strong>for</strong> the<br />

first time described in the beginning of 80th years.<br />

Cave Nevidimka. This cave is situated on the north of<br />

the Belaja balka. The entrance is in the southwest part<br />

of the abrupt southern slope of karstic crater. The cave<br />

begins with the small chamber from which the manhole<br />

dives down and deduces into a vertical crack. The<br />

depth of this cave is about 10m. The entrance is usually<br />

buried with adjournment of steppe vegetation ("roll -<br />

field") and also hardly acceptable. It w<strong>as</strong> found in 1989.<br />

Cave Metro. This cave is situated in upper reachers of<br />

Belaja balka. The entrance is located in the b<strong>as</strong>is of the<br />

large karst-erosive hollow southern slope. The cave<br />

represents tailrace tunnel with the extent of about<br />

100m. The cave w<strong>as</strong> found in 1989. At the moment of<br />

detection the height of the manhole w<strong>as</strong> 1,5m. For the<br />

next years it w<strong>as</strong> buried with sandy - loam adjournment<br />

9<br />

owing to a sliding of a hollow slope. Again it w<strong>as</strong><br />

opened in 2001. The height of the manhole now is<br />

about 1m.<br />

Cave Chabanskaya. The entrance is located in a<br />

blind karstic ravine. The general extent of this cave is<br />

82m. It w<strong>as</strong> found and surveyed by cave explorers in<br />

1988. Now it is inaccessible owing to entrance failure.<br />

It w<strong>as</strong> situated in immediate proximity from a day<br />

time surface.<br />

Cave Crystalnaya. It is located on the northern co<strong>as</strong>t<br />

of B<strong>as</strong>kunchack. It is the second largest cave on the<br />

given area. The cave begins with 15m - long well,<br />

running to the hall Holodny in the height up to 3m and<br />

sizes of 4 х 2,5m. Then the low manhole deduces to<br />

the hall Teply. The sizes of this hall are 16,5 х 9m at<br />

average height of about 2,5-3m. Further the cave<br />

comes to the end with 30m – long manhole. The<br />

depth of the cave from the steppe level is 30m. The<br />

cave is plentifully decorated with a white bark of<br />

secondary gypsum crystallization. At present here<br />

there is a small cave lake with the area of up to 2 m2.<br />

The cave is interesting due to various <strong>for</strong>ms of<br />

crystallization of cave minerals. It w<strong>as</strong> found in 1986.<br />

Cave Albina. It is situated on the northern co<strong>as</strong>t of<br />

B<strong>as</strong>kunchack. The entrance is located in 2,5m above<br />

a bottom of karstic crater, in its e<strong>as</strong>t slope. The depth<br />

of the cave from the steppe level is about 7m. Its<br />

extent is about 12m. The average height is 1m, width<br />

is 3-3,5m. The cave w<strong>as</strong> found in 1995.<br />

Cave Mihajlovskaja. It is situated on the north co<strong>as</strong>t<br />

of Lake B<strong>as</strong>kunchack. The entrance is located 4m<br />

below the steppe level and 2,5m above the bottom of<br />

the karstic crater. The cave depth is about 25m from<br />

the steppe level. The extent is about 35m. It is<br />

interesting due to the presence of 6m - depth well<br />

with the diameter of 2 m. It is complex and dangerous<br />

<strong>for</strong> p<strong>as</strong>sage, there<strong>for</strong>e the entrance is immured. It<br />

w<strong>as</strong> found in 1998.<br />

Cave Bolshoy Tupic ("Blind"). It is situated on the<br />

northern co<strong>as</strong>t of Lake B<strong>as</strong>kunchack. The cave h<strong>as</strong><br />

the large arch entrance located on the b<strong>as</strong>is of a<br />

karstic crater slope. The cave is submitted by the<br />

fragment of the large channel, blindly coming to the<br />

end with the imp<strong>as</strong>se. The extent is about 13m. The<br />

cave w<strong>as</strong> found in 1986.<br />

Cave Pervomajskaja. It is situated on northe<strong>as</strong>t<br />

co<strong>as</strong>t of B<strong>as</strong>kunchack and south - west of Lake<br />

Kar<strong>as</strong>un. The entrance is located in a blind karstic

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