| East Butte | |
| Elevation Ft: | 6572 |
| Elevation Ref: | [1] [2] |
| Prominence Ft: | 1542 |
| Isolation Mi: | 19.33 |
| Isolation Ref: | [3] |
| Parent Peak: | Big Southern Butte (7,550 ft) |
| Map: | Idaho#USA |
| Label Position: | bottom |
| Map Size: | 240 |
| Country: | United States of America |
| State: | Idaho |
| Region: | Bingham |
| Region Type: | County |
| Coordinates: | 43.5013°N -112.6625°W |
| Coordinates Ref: | [4] |
| Range: | Snake River Plain Rocky Mountains |
| Rock: | Rhyolite |
| Age: | 600,000 years old |
| Type: | Lava dome |
| Topo: | USGS Little Butte SW |
East Butte is a 6572adj=midNaNadj=mid summit located in Bingham County, Idaho, United States.
East Butte and line parent Big Southern Butte were major landmarks for early explorers and pioneers.[4] The remote mountain is situated over 40 miles east of Craters of the Moon National Monument and Preserve, 32 miles west of the community of Idaho Falls, and can be seen from Highway 20 midway between Idaho Falls and Arco at milepost 274. East Butte is set on land belonging to the Idaho National Laboratory so access is restricted even though a road leads to multiple radio towers at the top. Topographic relief is modest as the summit rises over 1200abbr=offNaNabbr=off above the Eastern Snake River Plain in one mile. This landform's toponym has been officially adopted by the United States Board on Geographic Names.[4]
East Butte is a lava dome composed of aphanitic rhyolite. It formed around 600,000 years ago as sialic magma flowed through a conduit in the basalt plain which surrounds the peak.[5]
East Butte is located in a cold semi-arid climate zone with warm summers and cold winters (Köppen BSk).[6] Winter temperatures can drop below 0 °F with wind chill factors below −20 °F. Precipitation is relatively sparse.