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Geotherm
The geothermal gradient is the rate at which temperature increases with depth in the Earth's crust, which can indicate geothermal energy potential or volcanic activity.
EAGLET
Explosions
Ash (danger to airplanes, building collapse,
lahars)
Gas (pyroclastic flows, toxic gases)
Lava (flowing molten rock)
Earthquakes
Tsunami
Pahoehoe(basaltic lava)
A type of basaltic lava that has a smooth, ropy surface and is characterized by its low viscosity, allowing it to flow easily.
Aa (basaltic lava)
A type of basaltic lava characterized by a rough, jagged surface that forms when lava cools quickly.
Modern records
studying active volcanoes and
recording phenomena, correlating with other active
volcanoes
Historical records
Documented volcanic events, their impacts on communities and environments, and observations from past civilizations and studies that aid research on volcanic activity.
Geologic history
Mapping and dating volcanic
rocks and ash deposits
Thermal conditions
refers to the temperature and heat-related factors that influence volcanic activity and magma formation.
where are the Subducting plates
Subducting plates are typically found at convergent plate boundaries, where one tectonic plate is forced under another, often leading to volcanic activity.
dome volcano
A type of volcano characterized by a steep, dome-shaped profile formed by the slow extrusion of viscous lava that is typically andesitic to rhyolitic in composition.
magnetic conditions
related to the Earth's magnetic field and its influence on geological processes.
hydrologic conditions
Refers to the various factors affecting water movement and distribution in geological environments, including groundwater flow, surface water interactions, and precipitation patterns.
USGS
The United States Geological Survey, a scientific agency of the U.S. government that studies natural resources, natural hazards, and the landscape of the U.S.
magma characteristics
Its composition can vary from basaltic (low silica, low viscosity) to andesitic (medium silica, medium viscosity) and rhyolitic (high silica, high viscosity). The temperature of magma typically ranges from 700 to 1300 degrees Celsius. Viscosity is influenced by silica content, with higher silica leading to thicker, more viscous magma. The gas content, including water vapor and carbon dioxide, affects the pressure within the magma chamber and can influence the explosiveness of a volcanic eruption.