| Gabrielse Cone | |
| Elevation M: | 1600 |
| Location: | British Columbia, Canada |
| District: | Cassiar Land District |
| Range: | Stikine Ranges |
| Coordinates: | 59.4186°N -130.3972°W |
| Type: | Cinder cone |
| Age: | Holocene |
| Volcanic Arc/Belt: | Northern Cordilleran Volcanic Province |
| Last Eruption: | Holocene |
Gabrielse Cone is a remarkably fresh, clearly postglacial monogenetic cinder cone, located in the Tuya Volcanic Field in British Columbia, Canada. It is about 4000NaN0 in diameter and has a central crater about 300NaN0 deep. It is Holocene in age and to its northeast appears to be breached with the remnants of a lava flow. The cone is near the headwaters of Iverson Creek.
Gabrielse Cone is named after Hu Gabrielse, a Canadian geologist who first identified the cone.[1]