GEOTOUR & IRSE 2012.pdf - Fakulta BERG - TUKE
GEOTOUR & IRSE 2012.pdf - Fakulta BERG - TUKE GEOTOUR & IRSE 2012.pdf - Fakulta BERG - TUKE
Salgótarján, 04. – 06. October 2012 approached from Telkibánya village by car and with 20 minutes walk from the paved road up the Kánya Hill, or with a hike on the red marked trail. Fig. 4 Educational Centre equipment The adit starts on the 517 m level, on the western slope of the Kánya Hill. After leaving the walling of the entrance, at 20 m it reaches the Lobkowitz Vein, one of the veins richest in gold, having a limonitic, ochreous and kaolinitic vein filling here. The vein itself is 1-2 dm thick only, but it is surrounded by a brecciated and hydrothermally altered host rock. Along the vein a drift was driven to the north. At 200 m the adit traverses the 0.3–1.2 m thick Jószerencsét Vein, striking to 30°, dipping to SE. The main tunnel reaches the along-strike drift at a „blind shaft‟ (reaching the level of the Veresvíz drainage tunnel), which is secured with a steel net and a barrier. The clayey hydrothermal breccia of the vein can be observed in the drift. The main tunnel leads further to the 2- 6 dm thick Jupiter Vein, following this to S in about 300 m length to the ventilation shaft. (Data of the veins: Zelenka & Horváth 2009; Sasvári & Kondela 2009). The visit is very popular also for civilian (non-geoscientist or student) groups. Walking into the nearly horizontal adit requires no special effort or equipment. As there are no chambers or any rooms inside, the optimal visitor group has to be maximum 20 persons with one or two leaders. There is no need to go further than the Jószerencsét Vein, as the drift becomes increasingly muddy inwards. The tour takes 30-45 minutes, depending on the interest of the group. 10
GEOTOUR & IRSE 2012 Fig. 5.Demonstrators of the first courses at the Educational Centre, left to right: Julián Kondela (TUKE), János Földessy (UM), Tamás Ormos (UM, geophysics), Éva Hartai (UM), Tibor Sasvári (TUKE), Norbert Németh (UM), Blaņej Pandula (TUKE) WAY OF THE GOLD-DIGGERS: THE EDUCATIONAL TRAIL This trail (Fig. 7) was designed to introduce several aspects – geology, mineralogy, mining and processing – to the tourists without personal professional guiding. Information is provided at 6 demonstration sites on boards with figures and explanations in 4 languages (Hungarian, Slovakian, English and German). General information and maps are given on a double board at the base site; GPS coordinates of the sites are also provided. The trail starts from the Mátyás király kútja (King Mathias Spring), a public rest area at the road to Sátoraljaújhely, and it also ends there as a ring. The site is known by its „ice cave‟, in fact a small adit containing ice also during the summer months, but this is not accessible for visitors. The trail is marked by miner figures. To walk around the whole trail means an 8.5 km long hike on the hills, but there is a possible marked shortening with the omission of 4 demonstration sites. The demonstration sites and the key pieces of information are listed below. Konczfalva and Veres-víz heritage adit The lowest site of the mining area is the entrance of the adit serving the water discharge and transport of the ore. The ore was milled and jigged here, using the power of the water. The ruins of the processing plants and the adit (not accessible) with outflow in a reddish channel (precipitation after weathered pyrite, hence the name Veres-víz, „Red Water‟) can be observed. The visitors are introduced into the history of mining and ore processing here. Fehér Hill Quarry The quarry explores vesicular rhyolite with spectacular, 1-2 cm long quartz prisms, barite and other minerals in the vesicles. This is a favorite site of mineral collectors, demonstrating the most frequent volcanic rock type and some minerals in the surroundings of Telkibánya. 11
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Salgótarján, 04. – 06. October 2012<br />
approached from Telkibánya village by car and with 20 minutes walk from the paved road up the<br />
Kánya Hill, or with a hike on the red marked trail.<br />
Fig. 4 Educational Centre equipment<br />
The adit starts on the 517 m level, on the western slope of the Kánya Hill. After leaving the walling<br />
of the entrance, at 20 m it reaches the Lobkowitz Vein, one of the veins richest in gold, having a<br />
limonitic, ochreous and kaolinitic vein filling here. The vein itself is 1-2 dm thick only, but it is<br />
surrounded by a brecciated and hydrothermally altered host rock. Along the vein a drift was driven<br />
to the north. At 200 m the adit traverses the 0.3–1.2 m thick Jószerencsét Vein, striking to 30°,<br />
dipping to SE. The main tunnel reaches the along-strike drift at a „blind shaft‟ (reaching the level of<br />
the Veresvíz drainage tunnel), which is secured with a steel net and a barrier. The clayey<br />
hydrothermal breccia of the vein can be observed in the drift. The main tunnel leads further to the 2-<br />
6 dm thick Jupiter Vein, following this to S in about 300 m length to the ventilation shaft. (Data of<br />
the veins: Zelenka & Horváth 2009; Sasvári & Kondela 2009).<br />
The visit is very popular also for civilian (non-geoscientist or student) groups. Walking into the<br />
nearly horizontal adit requires no special effort or equipment. As there are no chambers or any<br />
rooms inside, the optimal visitor group has to be maximum 20 persons with one or two leaders.<br />
There is no need to go further than the Jószerencsét Vein, as the drift becomes increasingly muddy<br />
inwards. The tour takes 30-45 minutes, depending on the interest of the group.<br />
10