A geyser is best described as a fountain of superheated steam. This natural phenomenon occurs when water that is trapped beneath the Earth's surface is heated by geothermal activity, such as volcanic activity, deep underground. As the water is heated, it turns into steam and builds up pressure. This pressure eventually forces the steam and hot water to be expelled violently from the ground in a dramatic outburst, creating a fountain-like effect.
Let's break this down a bit more:
A geyser consists of a network of underground channels filled with water. The heat from molten rock (magma) heats the water in these channels.
As the water heats, it expands and turns into steam. However, due to the depths, the water above creates pressure that allows the water below to reach temperatures above the normal boiling point.
When this pressure is released, often when bubbles of steam rise to a narrow section of the channel nearest the surface, the superheated water violently boils, pushes through the surface, and escapes as steam and hot water – hence, a fountain of superheated steam.
This distinct eruption is what characterizes a geyser and differentiates it from other geothermal features like hot springs or thermal pools, which do not erupt but simply release heat gradually into the water.