2. Explanation the formation conditions and processes of epithermal ore deposit by reading the following model figure. VOLCANIC-HYDROTHERMAL SYSTEM GEOTHERMAL SYSTEM sQ, HCL CO Crater lake CO, HS CO,, HCLS 3>Acidic fhuid' Au cu B Saline magmatic fluid Porphyry Cu(Mo, Au Liqud flow V apor ascent Approxim ate Schematic cross-section showing shallow sub-volcanic intrusions and assoiatted stratovolcano, and nvironments deduced for formation of porphyry Cu, and high- and low-sulfidation epithermal ore deposits Active volcanic-hydrothermal systems extend from degassing magma to fumaroles and acidic springs, and rom geothermal systems characterized by neutral-pH waters that may discharge as hot springs Posits form ncorporate porphyry and/or high-sulfidation ore environments, whereas low-sulfidation are de 4. To find the possible types of ore deposits and briefly give their properties2. Explanation the formation conditions and processes of epithermol ore deposit by reading the following model figure. Schematic cross-section shouwing shallow sub-volcanic intrusions and assoiatted stratovolcano, and environments deduced for formation of porphyry Cu, and high- and low-sulfidation epithermal ore deposits. Active volcanic-hydrothermal systems extend from degassing magma to fumaroles and acidic springs, and incorporate porphyry and/or high-sulfidation ore environments, whereas low-sulfidation are deposits form from geothermal systems characterized by neutral-pH waters that may discharge as hot springs. 4. To find the possible types of ore deposits and briefly give their properties from following model figure. 1 km