👉 Highland fluids refer to a unique category of geothermal fluids found in high-elevation regions, typically above the tree line. These fluids are characterized by their low temperatures, high salinity, and often contain dissolved minerals and gases such as carbon dioxide, methane, and hydrogen sulfide. They form through the interaction of meteoric water with underlying rocks at depth, where pressure and temperature conditions allow for the dissolution of minerals. As these fluids ascend through fractures and faults, they can become superheated and pressurized, leading to the formation of geothermal systems. Highland fluids are crucial for understanding the geothermal potential of mountainous areas and can be harnessed for energy production, though their unique properties require specialized techniques for extraction and utilization.
