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Craters of the Moon National Monument & Preserve spatter cones
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Craters of the Moon National Monument & Preserve
Geologic Formations
 
Nature and Science

Blue Dragon Pahoehoe Lava Flow

The 3 young lava fields found in 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 links to some detailed geologic maps and guides to the geology of the Craters of the Moon lava field.

 
 
 
 
 
 
 
 
 

Geological Field Trips in S. Idaho, E. Oregon, and N. Nevada
Chapter 10 provides a detailed field trip guide to the Craters of the Moon flow

 

curtain of fire
Evolution of the Craters of the Moon lava field
View an animation that shows the ages of the different lava flows.
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geology map
Geology Map
USGS Geologic Map of the Craters of the Moon 30'X60' Quadrangle (Scientific Investigations Map 2969)
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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: May 30, 2011 at 14:05 MST