|Elevation||4,650 ft (1,420 m)|
|Location||Lake County, Oregon, U.S.|
|Topo map||USGS Hole In The Ground|
|Last eruption||about 50,000 to 100,000 years ago|
It is about 1.0 mile (1,600 m) across, a little longer N-S than E-W. Its floor is about 150 meters (490 ft) below the surrounding ground level and has a rim that rises 35 to 65 meters (110 to 210 ft) above, the highest point on the east side. The crater formed during the late Pleistocene, between 13,500 and 18,000 years ago, at which time the Fort Rock Basin was a lake and the location was near the shore. Basaltic magma intruding near the surface flashed ground water to steam, which blew out overlying rock and soil, along with some juvenile material. As material slid into the hole formed, it closed the vent and the process repeated, eventually forming the huge hole. Blocks as large as 26 feet (8 m) in size were flung as far as 2.3 miles (3.7 km) from the crater.
To the west of Hole-in-the-Ground is an even bigger maar, 1.1 miles (1,820 m), but older and more eroded, called Big Hole.
- "Hole-in-the-Ground". Geographic Names Information System. United States Geological Survey. Retrieved 2014-12-29.
- "Deschutes & Ochoco National Forests - Hole-in-the-Ground Volcano". USDA Forest Service. 2003-12-24. Archived from the original on 2010-01-23. Retrieved 2007-05-22.
- Heiken, G. H.; R. V. Fisher and N. V. Peterson (2006-03-28). "A Field Trip to the Maar Volcanoes of the Fort Rock - Christmas Lake Valley Basin, Oregon". Geological Survey Circular 838: Guides to Some Volcanic Terrances in Washington, Idaho, Oregon, and Northern California. United States Geological Survey. Retrieved 2007-05-22.
- Wood, Charles A.; Jurgen Kienle (1993). Volcanoes of North America. Cambridge University Press. p. 205. ISBN 0-521-43811-X.
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