What is a geyser and how does it form?

What is a geyser?
A geyser is an intermittent or semi-regularly periodic spout of geothermally heated groundwater and steam. Any subsurface encounter between water and heat produces a hydrothermal process. The heat is usually supplied by upwellings of magma from the mantle, the water by precipitation that percolates downward through surface rocks. Some oceanic water enters the mantle at subduction zones and becomes an important ingredient in upper-mantle magmas.

How does it form?
Geysers form only under special conditions. First, a system of underground channels must exist in the form of a vertical neck or series of chambers. The exact arrangement cannot be observed directly, and probably varies from geyser to geyser. This system of channels must vent at the surface. Second, water deep in the system—tens or hundreds of meters underground—must be in contact with or close proximity to magma. Third, this water must come in contact with some rock rich in silica (silicon dioxide, SiO2), usually rhyolite.