Type of Metamorphism

There are two types of metamorphism, regional and contact:

a) Regional: As the name implies regional metamorphism involves a large area.

b) Contact: Highly localized (small area) where rock was changed by contact with molten magma. Contact metamorphism is the result of heat alone (not pressure).

The shaded area in the bedrock map to the right (ESRT page 3) shows a large area of regional metamorphism in New York State. Most of this region is comprised of the Adirondack and the Taconic Mountains. The Adirondacks were formed about a billion years ago as heat and pressure created the metamorphic rock found in the region today. The Taconic mountains formed as a result of tectonic events during the Ordovician period (page 9 ESRT 'Important Geologic Events in NYS').

Large area = regional metamorphism = heat and pressure. 

Hint: When a regents question asks about metamorphic rock in New York State you should immediately think of the Adirondack Mountains. Know where they are!

 

The two illustrations on the right are from NYS regents exam. The red-shaded areas are igneous rock which intruded into the surrounding rock as molten magma. Because it was so hot, thousands of degrees, it changed the rock it contacted (highlighted in yellow). This is contact metamorphism and is the result of heat alone (no pressure). Also notice that the zone of contact metamorphism is quite small compared to the vast areas of the Adirondacks.

Small area = contact metamorphism = heat alone (no pressure).

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