Garajau Dyke
A feeder dyke with chilled margins in a tuff cone formed by hydrovolcanic and Strombolian eruptions on basaltic lava cliffs, Pleistocene-Holocene.
- Contributor
- dh1
- Location
- 32.63773, -16.85184
- Formation
- Upper Volcanic Comples
- Lithology
- Basalt
- Licence
- License.ALL_RIGHTS_RESERVED
- Last updated
- 2026-10-06
Tags: hydrovolcanic activity chilled margin basalt dyke strombolian eruption
Data sources
- Palaeolatitude: GPlates Web Service (EarthByte), Torsvik & Cocks (2017) (Computed output; cite the reconstruction model)