In volcanic areas, groundwater heated by magma can be a source of hot springs, geothermal energy, and steam. This heated groundwater can also contribute to the formation of hydrothermal features such as geysers and fumaroles.
When lava is heated, it undergoes a process called crystallization, where the molten rock solidifies and forms crystals as it cools. This process is essential in the formation of igneous rocks, such as basalt and granite, as well as in the development of various volcanic landforms.
A liquid that is heated may be called a "heating medium" or simply "heated liquid."
When magma is being heated it rises. When it is cooled, it sinks.
because they are both heated by a nearby body of magma
Solid iron oxide and a poisonous called sulphur dioxide
In volcanic areas, groundwater heated by magma can be a source of hot springs, geothermal energy, and steam. This heated groundwater can also contribute to the formation of hydrothermal features such as geysers and fumaroles.
When a mixture of powdered iron and sulfur is heated, iron sulfide is formed. Iron sulfide is a compound composed of iron and sulfur atoms that have reacted together through a chemical reaction.
The balanced chemical equation for powdered quartz (SiO2) reacting with powdered magnesium (Mg) when heated is: 2Mg + SiO2 -> 2MgO + Si. This reaction produces magnesium oxide (MgO) and silicon (Si).
geothermal energy
The opening top of the volcano is called a crater. The super-heated gases and ash billows out of the mouth of hell before the magma erupts out destroying all in its path.
by hot water tapped from volcanic springs.
When lava is heated, it undergoes a process called crystallization, where the molten rock solidifies and forms crystals as it cools. This process is essential in the formation of igneous rocks, such as basalt and granite, as well as in the development of various volcanic landforms.
Rubber and glass which become softer as they are heated are examples of crystalline solids
A liquid that is heated may be called a "heating medium" or simply "heated liquid."
The change is a chemical change known as a chemical reaction. When heated, the iron and sulfur react to form a new compound called iron sulfide.
When the heated part of the mantle rises through the Earth's crust, it can create volcanic activity as magma reaches the surface. This process is known as mantle convection and is responsible for the movement of tectonic plates and the formation of volcanic hotspots.