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Applicatopn dossier for nomination as a European Geopark ...

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The cave is situated in gypsum and represents the<br />

large landslide underground hall complicated with large<br />

blocks. Be<strong>for</strong>e the creation of the state reserve it had<br />

been actively visited by tourists.<br />

Cave Natechnaya. This cave is situated in the same<br />

crater <strong>as</strong> Cherep but on the opposite slope. It<br />

represents a large vertical crack (max. height up is to<br />

5m, width is up to 2,5m), with one small entrance -<br />

manhole, decorated with a white gypsum bark of<br />

secondary crystallization. Be<strong>for</strong>e the creation of the<br />

state reserve it had been actively visited by tourists. It<br />

h<strong>as</strong> been known since 1969.<br />

Cave November, 8. It is situated in the natural hale<br />

Sharbulack. It w<strong>as</strong> found in 1985. The entrance to the<br />

cave is located in a slope of karstic crater. The cave<br />

represents a descending crack in gypsum rock.<br />

General extent is about 30m. The depth from the<br />

steppe level is 13,3m.<br />

Cave March, 8. The entrance is the horizontal channel<br />

of roundish section leaving under the b<strong>as</strong>is of a gypsum<br />

exposure in the western slope of karstic crater. Further<br />

the cave runs along cracks deep into the m<strong>as</strong>sive <strong>as</strong> a<br />

narrow horizontal way. It is narrow, difficultly p<strong>as</strong>sable<br />

and short. It is seldom visited. It w<strong>as</strong> found in 1968.<br />

Cave Familnaja. It is located in the natural hole<br />

Sharbulack. It represents a large vertical crack (max.<br />

height up is to 5m, width is up to 2,5m), with one small<br />

entrance - manhole, decorated with a white gypsum<br />

bark of secondary crystallization. The height of the<br />

manhole is about 8m. The extent is about 20m. The<br />

width is 0,6-0,8m. It is very seldom visited. The<br />

entrance is obstructed. The cave is found in 1968.<br />

Cave Vodjanaja - 1. It is located in the natural hole<br />

Sharbulack in the b<strong>as</strong>is of a slope karstic crater. The<br />

extent of the cave is about 10-12m, the width is 1-1,5m<br />

and the height is 2,5m. The cave obliquely runs to the<br />

bottom and tooks to the small lake with the area of<br />

about 4m and the depth up to 2,5m. It w<strong>as</strong> found in<br />

60th years.<br />

Cave Vodjanaja - 2. It is located in the natural hole<br />

Sharbulack. The entrance represents a narrow<br />

extended window following to a cavity. The extent of a<br />

cave is about 38m. In the cave there are two small<br />

lakes with the area of 10m and 6,7m, the depth is up to<br />

1,5m and up to 3,5m accordingly. It w<strong>as</strong> found in 1989.<br />

Cave Dlinny razlomchick. It is situated in the natural<br />

hole Sharbulack. The entrance is located on the slope<br />

8<br />

of a karstic crater. The cave represents a vertical<br />

crack with the inclined sandy floor and blindly coming<br />

to the end in the distant part. The extent is about<br />

16m. The height is up to 3,5m, width is 0,5-0,6m. The<br />

cave w<strong>as</strong> found in 1989.<br />

Cave Gluboky razlomchik. It is situated in the<br />

natural hole Sharbulack. The entrance is located in a<br />

karstic well. The cave represents a vertical<br />

descending crack in gypsums, the depth is up to 10m<br />

and its width is about 0,5m. The cave w<strong>as</strong> found in<br />

2002.<br />

Cave Аstrahanka. It is situated in the southwest part<br />

of the natural hole Sharbulack. The entrance is<br />

located on the slope of a karstic hollow, in the b<strong>as</strong>is<br />

of a gypsum exposure. The extent is about 20m. The<br />

average height of the manhole is about 2-2,5m. It<br />

w<strong>as</strong> found in 2000.<br />

Cave Obmanka. It is situated in the southwest part of<br />

the natural hole Sharbulack. The entrance is located<br />

on the slope of a karstic hole, in the b<strong>as</strong>is of gypsum<br />

exposure. The maximal depth of the cave bedding<br />

from the steppe level is 21,3m. The extent is about<br />

16m. The average height of the manhole is about 1-<br />

1,3m. The width of it is about 2-2,5m. The size of the<br />

cave entrance is 2,7 X 2,1m. It blindly comes to a low<br />

manhole. It w<strong>as</strong> found in 2000.<br />

Cave Sharovskaya - 1. It is situated on the western<br />

co<strong>as</strong>t of B<strong>as</strong>kunchack. The entrance is located in a<br />

gypsum exposure (e<strong>as</strong>t exposition) and represents a<br />

narrow vertical crack running to the cavity. The b<strong>as</strong>ic<br />

part of this cave is submitted by the underground hall<br />

of a landslide origin. The hall h<strong>as</strong> sizes of 8-5,5m.<br />

Height of a hall is up to 4,5m. The floor of a cave is<br />

filled up with blocks and pieces of gypsum. It is<br />

located in immediate proximity from a day time<br />

surface. It w<strong>as</strong> found in 1995.<br />

Cave Sharovskaya - 2. It is situated on the western<br />

co<strong>as</strong>t of B<strong>as</strong>kunchack. The entrance is located in a<br />

gypsum exposure of karstic crater southern slope.<br />

The cave is submitted by bursi<strong>for</strong>m poorly<br />

descending cavity, in distant bottom part of which<br />

there is a small lake with the area of about 15m2,<br />

with the depth of 1,5m. The extent of the cave is<br />

about 11m. The depth from the surface level is 10m.<br />

It w<strong>as</strong> found in 1995.<br />

Cave Sharovskaya - 3. It is situated on the western<br />

co<strong>as</strong>t of B<strong>as</strong>kunchack. The entrance is located in a<br />

gypsum exposure and represents a narrow horizontal

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