Abstract
Dye-tracing tests in the region of the alps Velika planina and Mala planina have shown that the major part of the region drains towards the spring of the Lučnica at Podvolovljek where is also a small fish farm. As to the water level, the marginal and central parts also drain into the stream Lučka Bela or the springs at Volovljek. Quite interesting is the high-mountain plateau Veža, a karstified territory surrounded by the valleys Robanov kot and Podvolovljek, as well as the tributary area of the stream Kamniška Bistrica. Here there is every indication of the deep runoff into the springs above Luče, the spring Pečovski izvir, the temporary springs which are close to the stream Savinja and into the unknown springs in the gorge below the rocky needle Igla. With regard to the water level, the higher parts of the massif can drain towards the valleys Robanov kot, Podvolovljek and Kamniška Bistrica. The tributary area of the Bistrica is quite well known, too. It has been discovered that the area of the saddle Kamniško sedlo drains tovvards the springs of the Savinja. The territories of the saddle Kokrsko sedlo, the alps Dolge njive and Kalce drain into the spring Studenci below Mokrica.
Highlights
Dye-tracing tests in the region of the alps Velika planina and Mala planina have shown that the major part of the region drains towards the spring of the Lučnica at Podvolovljek where is a small fish farm
As to the water level, the marginal and central parts drain into the stream Lučka Bela or the springs at Volovljek
Quite interesting is the high-mountain plateau Veža, a karstified territory surrounded by the valleys Robanov kot and Podvolovljek, as well as the tributary area of the stream Kamniška Bistrica
Summary
Dušan Novak Geološki zavod Ljubljana Inštitut za geologijo, geotehniko in geofiziko Dimičeva 14, 1000 Ljubljana, Slovenija. Kratka vsebina Z barvanji na Veliki in Mali planini smo ugotovili, da se največji del tega območja odteka proti izviru Lučnice v Podvolovljeku, kjer je tudi manjša ribogojnica. Ob višjem vodnem stanju se podzemeljska voda z obrobja preliva tudi v Lučko Belo ali v izvire v Volovljeku. Visokogorska planota Veža oziroma Dleskovška planota med Robanovim kotom, Podvolovljekom in povirjem Kamniške Bistrice se odteka v izvire nad Lučami, v Pečovski izvir in v izvire tik ob Savinji, pa tudi v neznane izvire v soteski pod Iglo. Višji deli zakraselega masiva se lahko ob visokem vodnem stanju odtekajo tudi v Robanov kot, Podvolovljek in proti Kamniški Bistrici. Precej poznano je tudi povirje Kamniške Bistrice. Območje Kamniškega sedla se odteka proti izviru Savinje, območje Kokrskega sedla. Dolge njive in Kale pa v Studence pod Mokrico
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