Applicatopn dossier for nomination as a European Geopark ...
Applicatopn dossier for nomination as a European Geopark ...
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