When magma comes in contact with underground water, it creates hot springs, or geysers.
Lava will cool quickly compared to underground magma.
It starts when water heats up and turns into a gas
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A magmatic quake is seismic activity caused by the movement of high pressure magma within the earth's crust. This tends to occur as the pressure within a magma chamber increases which leads to hydraulic fracturing of the surrounding rock mass. This fracturing causes the seismicity or magmatic quake. This sort of small scale seismic activity near a volcano may indicate that the pressure in the magma chamber that feeds the volcano is increasing and in turn may be a precursor to a volcanic eruption and is something that vulcanologists or geophysicists would be on the look out for!
underground aquifers
Underground water can be heated by geothermal energy as a result of the Earth's internal heat. This heat comes from the radioactive decay of minerals deep within the Earth's crust and can warm up groundwater to create geothermal reservoirs. Additionally, proximity to volcanic activity can also heat underground water.
Geothermal energy is possible where there is hot magma near the Earth's surface, which heats underground water to create steam. This steam can then be harnessed to generate electricity through geothermal power plants.
These are vents through which volcanic gases and water vapour escape to the earth's surfaec.Fumaroles are formed when magma heats underground water,it mixes with volcanic gases and the mixture is eventually released as steam.
Groundwater that comes in contact with magma or rocks heated by magma can boil into steam. If it boils quickly enough it can result in an explosion called a phreatic eruption.
An opening in the ground where hot water and gases escape from magma heated deep underground.
Geysers are natural hot springs that erupt with steam and boiling water, formed when underground water is heated by nearby magma or hot rocks. As the water heats up, it becomes pressurized and eventually forces its way to the surface, resulting in an explosive eruption. The cycle of heating and eruption can create impressive displays, making geysers a unique geological phenomenon. This process is influenced by the geological conditions and water supply in the area.
A hydrothermal system is an area where magma close to the surface heats up groundwater. This process creates geothermal features like geysers, hot springs, and fumaroles. The heat from the magma warms the water, causing it to rise to the surface and release steam and mineral-rich water.
A geyser is an underground volcano with water on the surface of it. This water is then boiled by the magma.
A magma.
When magma heats water, it transforms the water into steam. This steam can then be harnessed to drive turbines, generating electricity in geothermal power plants. The process effectively uses the Earth's internal heat to produce renewable energy.
The heating of underground water by magma is called geothermal activity. The word geothermal comes from the Greek geo meaning "Earth" and therme meaning "heat".
At the temperatures found in magma water would normally be a gas, but is trapped under pressure as long as the magma is underground. When pressure is reduced enough the water vapor can bubble out of the magma very rapidly, resulting in an explosion.