Crater Rings

West crater, looking slightly northeast. slgwv (Atlas Obscura User)

The west crater. Looking east. slgwv (Atlas Obscura User)

Looking west across east crater, from above the channel draining into it. slgwv (Atlas Obscura User)

Northwestern edge of east crater. The edge of the west crater is barely visible beyond toward the right. slgwv (Atlas Obscura User)

East crater, looking southwesterly. slgwv (Atlas Obscura User)

Looking west across the east crater. slgwv (Atlas Obscura User)

The west crater, looking southeasterly. slgwv (Atlas Obscura User)

Flat floor of the west crater. slgwv (Atlas Obscura User)

North wall of east crater. slgwv (Atlas Obscura User)

The low, broad shield volcano where the craters occur, silhouetted on the skyline. Looking south from the primitive road leading to the craters. slgwv (Atlas Obscura User)

Excerpt from the Crater Rings USGS 7.5' topographic quadrangle map (1992), showing the topographic prominence of the craters.

East crater from a distance. Looking south. slgwv (Atlas Obscura User)

Drainage channel coming into east crater from the east. slgwv (Atlas Obscura User)

The north wall of the west crater. slgwv (Atlas Obscura User)

A volcanic subsidence crater (also called a pit crater or collapse crater) is formed when subsurface magma, supporting the rock overhead, drains away for whatever reason. The unsupported rock “ceiling” over the void left by the draining magma then collapses. (Much the same mechanism accounts for the formation of summit caldera craters, but those are typically at a larger scale.)

A subsidence crater can be distinguished from other craters, such as maars (e.g., Soda Lakes in Nevada), or impact craters, because they have no built-up rim formed by debris ejected out of the crater. They also typically have flat floors, reflecting the former presence of a lava lake.

Crater Rings are two collapse craters on a low, broad shield volcano that is thought to be geologically young (less than about two million years old). The east crater is about half a mile across and 300 feet deep, while the west one is slightly smaller and shallower (approximately 200 feet deep).

This shield volcano lies out in the Snake River Plain north of Mountain Home, Idaho, an area that has seen abundant volcanic activity in the recent geologic past. Despite the ubiquitous volcanism, however, subsidence craters like this are rare in these volcanic fields.

Know Before You Go

The Crater Rings are just off Interstate 84 north of Mountain Home, Idaho. Take Old US-30 (Old Oregon Trail Highway) 9.1 miles north from its intersection with Idaho State Route 51 (American Legion Boulevard) in downtown Mountain Home to a junction (at about 43.21878 N, 115.82268 W) with Cinder Butte Road. Turn left here and follow Cinder Butte Road (which is graded) 1.8 miles to a junction (at about 43.21506 N, 115.85748 W) with a primitive road on the left. Turn left here; the Crater Rings are in the low rise which forms the skyline. Go about 1.4 miles and park. This road will need high clearance but 4wd will probably not be necessary in dry weather. Jeep roads go around the craters, but can also be hiked.

The ground cover is all low grass and shrubs. A common component is cheat grass, a non-native species that, when dry, has annoying seeds that embed in clothing (such as socks) and also in pets' coats. It's also extremely flammable and has made wildfires both more common and more catastrophic in recent years. Be very careful with fire; in particular, don't park on dry grass as it is easily ignited by a hot catalytic converter.