A type of spring in which hot water or steam sporadically
or episodically erupts as jets from an opening in the
surface, in some cases creating a tower of water many tens of
meters high. Geysers are often marked on the surface by a
cone of siliceous sinter and other minerals that precipitated
from the hot water, known as geyser cones. Many also have
deposits of thermophyllic (heat-loving) bacteria that can form
layers and mounds in stromatolitic buildups. Geysers form
where water in pore spaces and cracks in bedrock gets heated
by an underlying igneous intrusion or generally hot rock,
causing it to boil and erupt, then the lost water is replaced by
other water that comes in from the side of the system. In this
way, a circulation system is set up that in some cases is quite
regular with a predictable period between eruptions. The
most famous geyser in the world is Old Faithful in Yellowstone
National Park, Wyoming.
See also GEOTHERMAL ENERGY.
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