Global Volcanism Program | Image GVP-12267

The center of Garove Island is a lagoon likely formed through edifice collapse, with debris avalanche deposits offshore. Cones have formed across the flanks, with Peter Hafen crater along the NE coast visible in this 4 December 2019 Sentinel-2 satellite image (N is at the top; this image is approximately 15 km across). Satellite image courtesy of Copernicus Sentinel Data, 2019.

The center of Garove Island is a lagoon likely formed through edifice collapse, with debris avalanche deposits offshore. Cones have formed across the flanks, with Peter Hafen crater along the NE coast visible in this 4 December 2019 Sentinel-2 satellite image (N is at the top; this image is approximately 15 km across).

Satellite image courtesy of Copernicus Sentinel Data, 2019.

Creative Commons Icon This image is made available under the Creative Commons BY-SA 4.0 license terms.

Garove