GEOTOUR & IRSE 2012.pdf - Fakulta BERG - TUKE

More documents

Recommendations

Info

Salgótarján, 04. – 06. October 2012 Fig. 6. The Mária Adit: entrance from outside, walled entrance section, water discharge channel and the section at the steeply dipping Jószerencsét Vein Kánya Hill rockslide Silicified blocks of rhyolite and fine-grained conglomerate cover the ground of an old beechwood. Some of the blocks have a roughly rounded shape and a circular hole in the middle, as these blocks served as raw material for the millstones of the ore processing (Fig. 8). The formation of the rockslide may be attributed to an earthquake causing the historical catastrophe in 1443 at the Kánya Hill mines. Lipót Shaft The cavity of large diameter serves to demonstrate the explanation on the board about the ventilation of the mines, the means of vertical transport and the vertical zonality of the mineralization. Teréz Adit and Csengő Mine Two adits of different age can be observed here with their waste dumps. The Teréz Adit is still accessible, reaching the Lobkowitz Vein on a lower level (410 m) than in the Mária Adit. The waste comprises mainly the country rock of the veins, andesite with propilitic and potassium metasomatic alteration, serving as the demonstrative background to the explanation on the board about the rock alteration and attached mineral parageneses. Jó Hill pit field At this site several small pits show the ancient outcrop of a gold-bearing quartz vein; several quartz (vein rock) blocks can be found in the debris. The site demonstrates the extent and methods of the medieval mining activity and the formation and host rock of the epithermal gold mineralization. 12
<strong>GEOTOUR</strong> & <strong>IRSE</strong> 2012 Fig. 7 Map of the educational trail, also showing the position of the Mária Adit 13
Page 1 and 2: GEOTOUR’12 & IRSE’12 INTERNATIO
Page 3 and 4: GEOTOUR & IRSE 2012 Geoparks, Geohe
Page 5 and 6: CONDITIONS FOR IMPLEMENTATION OF TH
Page 8 and 9: Salgótarján, 04. - 06. October 20
Page 64 and 65:
Salgótarján, 04. - 06. October 20
Page 66 and 67:
Page 68 and 69:
Page 70 and 71:
Page 72 and 73:
Page 74 and 75:
Page 76 and 77:
Page 78 and 79:
Page 80 and 81:
Page 82 and 83:
Page 84 and 85:
Page 86 and 87:
Page 88 and 89:
Page 90 and 91:
Page 92 and 93:
Salgótarján, 04. - 06. 2012 THE S
Page 94 and 95:
Salgótarján, 04. - 06. 2012 Fig.
Page 96 and 97:
Salgótarján, 04. - 06. 2012 http:
Page 98 and 99:
Page 100 and 101:
Salgótarján, 04. - 06. 2012 Effec
Page 102 and 103:
Salgótarján, 04. - 06. 2012 SUMMA
Page 104 and 105:
Salgótarján, 04. - 06. 2012 of 10
Page 106 and 107:
Salgótarján, 04. - 06. 2012 the s
Page 108 and 109:
Salgótarján, 04. - 06. 2012 in Lo
Page 110 and 111:
Page 112 and 113:
Salgótarján, 04. - 06. 2012 of th
Page 114 and 115:
Salgótarján, 04. - 06. 2012 [5] F
Page 116 and 117:
Salgótarján, 04. - 06. 2012 The C
Page 118 and 119:
Salgótarján, 04. - 06. 2012 the m
Page 120 and 121:
Salgótarján, 04. - 06. 2012 some
Page 122 and 123:
Salgótarján, 04. - 06. 2012 MININ
Page 124 and 125:
Salgótarján, 04. - 06. 2012 impor
Page 126 and 127:
Page 128 and 129:
Page 130 and 131:
Salgótarján, 04. - 06. 2012 of th
Page 132 and 133:
Salgótarján, 04. - 06. 2012 MAPPI
Page 134 and 135:
Salgótarján, 04. - 06. 2012 admin
Page 136:
Salgótarján, 04. - 06. 2012 unlim
show all

GEOTOUR & IRSE 2012.pdf - Fakulta BERG - TUKE

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?