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The red and gray areas on the map show where igneous rock can be found at the surface, or just beneath the soil. Igneous rock is formed when magma or lava cools. The red areas are where lava erupted onto the surface and hardened to form a category of igneous rock that geologists refer to as “volcanic” (a.k.a. extrusive). The gray areas are where the magma hardened beneath the surface, making a kind of igneous rock is called “plutonic” (a.k.a. intrusive). Basalt is the most common specific type of volcanic rock and granite is the most common specific type of plutonic rock.
Plutonic, or volcanic? How can they tell? .
. . Below: This photo was taken 25 miles southeast of Havre. The battlefield where Chief Joseph surrendered is shown in the foreground with the eastern edge of the Bear Paw Mountains (a.k.a. Bear Paws or Bear's Paw Mtns.) in the distance. Although the mountains in the photo are made up of plutonic rock, most of the Bear Paws consist of volcanic rock, which is more fine-grained than the plutonic rock that makes up the mountains between Butte and Helena. As the map at the top of this page shows, most of the mountains in central mountains are made up of plutonic and/or volcanic igneous rock.
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Terms: igneous rock, plutonic rock |
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Earth Science Teacher at Helena High School |