Global Volcanism Program | Image GVP-04025
Tecuamburro, seen here from the SE on the Pacific coastal plain, is a small lava-dome complex of mostly Pleistocene age. Tecuamburro and other lava domes forming the right-hand peaks were constructed during the late Pleistocene or early Holocene within a horseshoe-shaped, east-facing crater. The crater resulted from structural failure of the older Miraflores stratovolcano on the left.
Photo by Lee Siebert, 1988 (Smithsonian Institution).
This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.