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Craters Of The Moon National Monument & Preserveblazing star flowers
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Craters Of The Moon National Monument & Preserve
Geologic Formations
 
Nature and Science
Folded Blue Dragon Pahoehoe Lava Flow

 

The 3 young lava fields that compose Craters of the Moon National Monument and Preserve range in age from 15,000 years to 2000 years. Craters of the Moon lava field, the largest of the three fields found along the Great Rift, is made up of about 60 lava flows and 25 volcanic cones that cover 618 square miles. It provides outstanding examples of how molten basaltic rock can solidify into various types of lava. The basic types include block lava (very dense and formed into angular blocks), aa lava (a rough, jagged, clinkery surface), and pahoehoe lava (a smooth, ropy, or billowy surface). Visitors can also see vents, fissures, cinder cones, lava tubes, lava bombs, spatter cones, tree molds, rafted blocks, and many other volcanic features and structures. Below are some detailed geologic maps and guides to the geology of the Craters of the Moon lava field.

 
 
 
 
 
 
spatter cone
Geology of Craters of the Moon
Learn more about our geologic features
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kipuka  

Did You Know?
Searing lava flows that initially destroyed everything in their path today protect the last refuges of intact sagebrush steppe communities on the Snake River Plain. These islands of vegetation, known as kipukas, provide important examples of what is "natural".

Last Updated: April 30, 2009 at 14:16 EST