Global InformationIgwisi Hills information
| Igwisi Hills | |
|---|---|
| Highest point | |
| Elevation | 1,146 m (3,760 ft)[1] |
| Coordinates | 4°53′13.18″S 31°56′4.46″E / 4.8869944°S 31.9345722°E[2] |
| Geography | |
| Location | Tanzania |
| Geology | |
| Age of rock | Pleistocene? |
| Mountain type | Pyroclastic Cone |
| Last eruption | 10450 BC |
The Igwisi Hills are a volcanic field in Kaliua District of Tabora Region of Tanzania. Three tuff cones are found there, one of which is associated with a lava flow. They are one of the few locations of possibly kimberlitic lava flows on Earth.
The volcanoes are located in the middle of the Tanzania craton, away from other Tanzanian volcanoes. There have been prior episodes of kimberlitic volcanism in the craton, however.
The age of the Igwisi Hills is poorly known but may be early Holocene-late Pleistocene in age. Some rainfall-induced chemical modification is found, and the hills have a unique vegetation profile.
- ^ Cite error: The named reference
GVPwas invoked but never defined (see the help page). - ^ Brown, R.J.; Sparks, R.S.J. "Mapping the Igwisi Hills kimberlite volcanoes, Tanzania: understanding how deep-sourced mantle magmas behave at the Earth's surface" (PDF). GEF Scientific Reports. Natural Environment Research Council. Retrieved 20 March 2016.