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
2026-08-20

Tags: hydrovolcanic activity chilled margin basalt dyke strombolian eruption

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