is the volcanic mountain a site for any type of energy production?
Yes, geothermal energy
Mount Mazama
Studies of heat flow and the water chemistry in Crater Lake and the alteration of rocks older than 120,000 years ago suggest that hydrothermal areas exist in the Mazama vicinity. Most springs show similar chemistry, from the weathering of volcanic glass and clinopyroxene. These features probably formed due to processes related to residual heat from the magma chamber that produced the climactic Mazama eruption 7,700 years ago. The lake shows convective mixing that cycles every three years as thermal fluid moves into the lake through its floor, creating thermal springs that formed silica spires with heights up to
when was the last time crater lake volcano erupted Approximately 7,700 years ago what is the name of the volcano? Mount Mazama where is it located? In the state of Oregon, United States how many people live in this state? The United States Census Bureau estimates that the population of Oregon was 4,217,737 on July 1, 2019 who were the early settlers here? Paleo-Indians who were they? They were the first peoples who entered, and subsequently inhabited, the Americas during the final glacial episodes of the late Pleistocene period where did they come from? Archaeologists contend that Paleo-Indians migrated out of Beringia between and years ago how are they classified? Generally classified by lithic reduction or lithic core "styles" and by regional adaptations what are the geographical features of the volcanic mountain? It in north of the border with California, it lies in the southern portion of the Cascade Range, Crater Lake sits partly inside the volcano's caldera, with a depth of ; it is the deepest body of freshwater in the United States and the second deepest in North America after Great Slave Lake in Canada what type of plants are found near this lake? UNANSWERABLE what are the geological features of this lake? Mount Mazama, part of the Cascade Range volcanic arc, was built up mostly of andesite, dacite, and rhyodacite over a period of at least 400,000 years, lava eruptions later created a central platform, Wizard Island, Merriam Cone, and other, smaller volcanic features, including a rhyodacite dome
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Mount Mazama [SEP] Geothermal energy
Studies of heat flow and the water chemistry in Crater Lake and the alteration of rocks older than 120,000 years ago suggest that hydrothermal areas exist in the Mazama vicinity. Most springs show similar chemistry, from the weathering of volcanic glass and clinopyroxene. These features probably formed due to processes related to residual heat from the magma chamber that produced the climactic Mazama eruption 7,700 years ago. The lake shows convective mixing that cycles every three years as thermal fluid moves into the lake through its floor, creating thermal springs that formed silica spires with heights up to . As a result, the California Energy Company drilled two geothermal exploration wells: the MZI-11A with a depth of to the east of the national park barrier at the Scott Creek Drainage, and the MZII-1 with a depth of to the south of the same boundary and to the east of Annie Creek.