| GATAČKO POLJE - ГАТАЧКО ПОЉЕ |
The Karstography of the DINARIC KARST IN BOSNIA AND HERZEGOVINA Part 5.3. Eastern Herzegovina. GATAČKO POLJE - ГАТАЧКО ПОЉЕ Gacko Polje, BiH-RS Trebinje Region - Gacko Municipality. Updated 20 May 2007. |
| GP
Section 6.0.2. Webpage Contents :
6.0.2.1.
Ponor "Kučine"
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Section 6.0.2. PONORS - ПОНОРИ - PONORI kod selo Bašići - код село Башићи :
Image
G(M)P1-BPM.
The observable Ponors located in the vicinity of selo Bašići are :- Ponor
"Kučine", (alternative name = Ponor
"Ćunin mlin"),
kod Kruškica,
Specific
details about some of these ponors are given below.
These
interesting ponor areas are now mostly abandoned and growing wild and there
are many other ponors no longer visible and many others still which have
become totally choked with vegetation.
Milanović.(2006)
indicates on a map of the area the locations of many ponors, some with
names;
We would like to thank our local volunteer guide, Faim Bašić for helping us locate the ponors and for information about their names and history. We questioned him in some detail about many aspects of the karstography around his village. The Austro-Hungarian heritage of Gatačko Polje was well known to him and the villagers and they have great admiration for what was achieved during this historical period in regard to controlling the water of the polje. A return visit is planned for 2007 to record further details, before all is lost. |
| Gatačko
(Malo) Polje - Гатачко (Мало) Поље
kod Selo Bašići "KUČINE"
PONOR
|
6.0.2.1...."KUČINE"
PONOR - PONOR "KUČINE" - ПОНОР "КУЧИНE"
:
GPS Co-ordinates :..43° 08' 23"N. : 018° 29' 14"E. [8 Sats]. This is located in the Malo Polje area, south-east of the village of Bašići and slightly north of the hill Kruškica, at the end of a substantial streambed leading off from the right bank of the Rijeka Mušnica. The position of the ponor and its loop-streamway are clearly indicated on the Map above. The ponor is situated at an elevation of 923m. asl. The streambed is active only when the "ponornice" Rijeka Mušnica is at medium to high flow. The water flowing into this Ponor was once used by one ponor mill, Ćunin mlin, the complex ruins of which are extant, as partly illustrated in the images below. (All photographs were recorded by B. Lewarne, 19 August 2006.)
Ćunin
mlin seems to have included a small complex of water-controlling structures.
A small "bridge" is located directly above the position indicated in Photos.6.0.2.7.
and
6.0.2.8. above.
The
ponor is overgrown but accessible. It is choked by sediment-banks at the
accessible base of the surface shaft, indicating a low absorption capacity.
We currently have no hydrological data relating to this ponor.
|
| Gatačko
Polje - Гатачко Поље
kod Selo Bašići "DJAFER'S
MILL" PONOR
|
6.0.2.2...."DJAFER'S
MILL" PONOR - PONOR "ĐAFEROV MLIN" - ПОНОР
"ЂАФEРОВ МЛИН" :
GPS Co-ordinates :..43° 08' 45"N. : 018° 29' 11"E. [6 Sats]. This is located in the Malo Polje area, north-west of the village of Bašići, at the end of an artificial streambed of Austro-Hungarian construction, leading off from the right bank of the "ponornice" Rijeka Mušnica. The position of the ponor and its short streamway are clearly indicated on the Map above. The ponor is situated at an elevation of 922m. asl. at the north-eastern foot of a large limestone cliff forming part of Mišova glav., (glavica = ridge). The Mill itself is the most complete we have seen in this area, though it is totally derelict and beyond use. The take-off point of the canal on the riverbank of the Rijeka Mušnica once had a fine control-weir and sluice-gate construction, built by the Austro-Hungarian Engineers in the late 19th century, to enable the local villagers to build a Mill using the nearby ponor as the usual hydraulic outlet for the mill turbines, (ie a ponor mill). The stonework and other materials used in the construction of the control-weir and sluice-gate were so good, that after the ponor mill itself became disused, they were scavenged and put to other uses. Although the mill is no longer used, the ponor streamway is kept permanently active and if necessary, it can be stopped off quite quickly.
During
our visit in mid-August 2006., the ponor mouth was choked with much loose
wood and branches. There was neither the time nor the opportunity on the
reconnaisance tour to unblock the entrance.
|
| Gatačko
Polje - Гатачко Поље
kod Selo Bašići "HAMZIN
MILL" PONOR
|
6.0.2.3...."HAMZIN
MILL" PONOR - PONOR "HAMZIN MLIN" - ПОНОР
"ХАМЗИН МЛИН" :
GPS Co-ordinates :..43° 08' 52"N. : 018° 29' 14"E. [6 Sats]. This is located in the Malo Polje area, north-west of the village of Bašići, a few metres in from the right bank of the "ponornice" Rijeka Mušnica. The ponor is situated at an elevation of 930m. asl. at the foot of a large limestone cliff forming part of Mišova glav. It is permanently active, although at low water levels, the water is fighting to have to get through the few metres of thickly rooted ground between the river and the ponor mouth! There is no sign of a mill structure here.
The
ponor is wide open with a considerable sized entrance chamber taking water
from the nearby Rijeka Mušnica.
There is the potential for the exploration of two different routes off
this entrance chamber.
|
| Gatačko
Polje - Гатачко Поље
"VILIN
MILL" PONOR
|
6.0.2.4...."VILIN
MILL" PONOR - PONOR "VILIN MLIN" - ПОНОР "ВИЛИН
МЛИН" :
GPS Co-ordinates :..43° 08' 55"N. : 018° 29' 14"E. [9 Sats]. This is located in the Malo Polje area, north-west of the village of Bašići, at the end of a short artificial streambed leading off from the right bank of the "ponornice" Rijeka Mušnica. The ponor is situated at an elevation of 933m. asl. at the foot of a large limestone cliff forming part of Mišova glav. It is intermittently active, although it can be controlled to flow permanently. The ponor entrance shaft is heavily overgrown at the surface, preventing further investigation during our initial fact-finding tour of the area. There are a few signs of a mill structure here. The ponor probably has a relatively low absorption capacity. We currently have no hydrological data relating to this ponor. |
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