prvi hrvatski speleološki kongres - KARST underground protection

Along the line they also built several tunnels. One of them, located about 1 km SW of
village Godoviĉ remain unfinished.
Tunnel is strait and about 400 m long. They start to dig it from both sides.On
the southern entrance to tunnel there are preserved different stages of the tunnel
construction. In the height of the tunnel floor small service tunnel for transport of
excavated rock was made. Above it higher segments of the tunnel were excavated.
They are connected with the service tunnel by vertical shafts trough which the
excavated rock was poured into the small wagons below. The digging was propagated
in three step-like height segments. In segments was done also scaffolding and
cementing of the walls. Because the work was not finished there are all digging and
building phases preserved. Some of them were already panelled and cemented.
On the N side the digging was completely finished and the tunnel
circumference was cemented, but later, between WW I and WW II Italian army build
in it a bunker, one of many in the system Vallo Alpino. The bunker build in the tunnel
is concrete cube, with staircase and a shaft that leads to surface outpost covered with
steel cupola. Access to the bunker is from the tunnel from south or staircase from the
surface above the tunnel. To hide the bunker the N entrance to the tunnel was filled
and disguised.
Speleologija Crne Gore - istraţenost, mogućnosti, perspective
Speleology of Montenegro – level of exploration, possibilities and
prospective
Goran Barović 1
1
Asocijacija speleoloških društava Crne Gore, Danila Bojovića br.4, Nikšić, Crna Gora
Ključne riječi: speleologija, istraţivanje, spiljski “nakit” - sige, turizam, zaštita
Key words: Speleology, Research, Speleothems, Tourism, Protection
Prostor Crne Gore prema svom geološkom sastavu, klimatskim i hidrološkim
karakteristikama je veoma pogodno tlo za nastanak speleoloških objekata. Kreĉnjaĉka
osnova i velika koliĉina padavina omogućili su da se na ovom prostoru razvije vrlo
intenzivna kraška erozija koja je glavni ĉinilac u formiranju ovih objekata. Dejstvom
kraške erozije došlo je do formiranja velikog broja podzemnih kraških oblika.
Najpoznatiji istraţivaĉi koji su ispitivali prostor Crne Gore bili su A.Grund,
A.Penk i K. Absolon, J.Cvijić. Kompletnija i obuhvatnija istraţivanja spleoloških
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