Stop 1. The deposit panorama survey from the highest point of the open pit southern bort. The dykes exposed in the northern bort of the open pit, part of the Ermakovka stock and partially developed ore zone I (stop is outside Fig.11) are well observed.

Stop 2. Endocontact quenching zone of stock with structures of dendrite quartz and aegerine crystal transversal growth.

Stop 3. Garnet-vesuvianite scarns with relics of Pre-Mesozoic granites. Low-grade ores of south-eastern ore zone I pinching out.

Stop 4. Typical dykes of porphyry-like quartz monzonites and quartz syenites.

Stop 5. North-western termination of ore zone I, fluorite-bertrandite-fenacite ores of the highest quality.

Stop 6. The crosscutting relationships between granites of the Ermakovka stock and porphyry-like quartz syenites being similar to dykes that were observed in Point 4; schlieren pegmatites that contain large crystals of light-green fluorite with primary inclusions of late magmatic fluid.

Stop 7. Felsite dyke in granites of the Ermakovka stock.

Stop 8. Ore zone XVII of fluorite-eudidymite composition.

Stop 9. Piles of various composition massive ore large blocks.