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Posledice vetroloma: izjava Andrej Avsenik, vodja enote Zavoda za gozdove Bled, Marko Gašperin, Zavod za gozdove Bled, razdejanje in polomljene smreke in jelke.
The consequences of a strong wind in Jelovica; statements by Andrej Avsenik, head of the Institute of Forest Bled and Marko Gašperin.
Information:
Windbreaks in Jelovica; a storm with a strong wind left an irreparable damage and path of destruction, destroying more than 150 hectares of forest lands.
Original language summary:
Vetrolom na Jelovici; neurje pustilo nepopravljivo škodo, uničenega je 150 ha gozda.
Eastern part of highly karstified plateau of Jelovica (west Slovenia) that represents big fissured and karstified aquifer is drained by the group of Kroparica springs that are positioned ...approximately 1 km in the south of the city Kropa. Kroparica is represented by several springs that mainly flow out from the triasic Ba~a dolomite. Some of them are positioned in the hill slope sediments. In the article litostratigraphical and structural conditions in the background of the springs are represented together with simple hydrogeologicalbalance of Kroparica aquifer recharge. It was determined that the recharge area is between 3,8 and 6,5 km2 and that the average yearly outflow is between 224 and 386 l/s. Maximum outflows are much larger and are higher than some m3/s. High fluctuation of discharges are the consequence of high karstification level of Kroparica aquifer.
Eastern part of highly karstified plateau of Jelovica (west Slovenia) that represents big fissured and karstified aquifer is drained by the group of Kroparica springs that are positioned ...approximately 1 km in the south of the city Kropa. Kroparica is represented by several springs that mainly flow out from the triasic Ba~a dolomite. Some of them are positioned in the hill slope sediments. In the article litostratigraphical and structural conditions in the background of the springs are represented together with simple hydrogeologicalbalance of Kroparica aquifer recharge. It was determined that the recharge area is between 3,8 and 6,5 km2 and that the average yearly outflow is between 224 and 386 l/s. Maximum outflows are much larger and are higher than some m3/s. High fluctuation of discharges are the consequence of high karstification level of Kroparica aquifer.
