Cinder cone in Diamond Craters, a monogenetic volcanic field southeast of Burns, Oregon. Basaltic lava flows were formed in the past 25,000 years
A cinder cone in Diamond Craters, a monogenetic volcanic field southeast of Burns, Oregon. Basaltic lava flows were formed in the past 25,000 years and resemble a flat rocky area with small hills. The craters and vents, cinder cones and spatter cones, lava tubes are near Steen's Mountain Wilderness in the northern Great Basin.”
Size: 6000px × 4054px
Location: Oregon, United States of America
Photo credit: © Melissa Farlow / Alamy / Afripics
License: Royalty Free
Model Released: No
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