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Global Volcanism Program | Image GVP-11986

The elongated island of Pulau Weh is offshore from the NW tip of Sumatra. It has been interpreted as the remains of a partially-collapsed older volcanic center that now opens to the NW and is filled by the sea. Volcanism at Pulau Weh was considered to be of Pleistocene age, but fumaroles and hot springs are present along a NW-E-trending line along the summit of the island and near the western shore of Lhok Perialakot bay on the northern side of the island. Copyrighted photo by Michael Thirnbeck, 2006.

The elongated island of Pulau Weh is offshore from the NW tip of Sumatra. It has been interpreted as the remains of a partially-collapsed older volcanic center that now opens to the NW and is filled by the sea. Volcanism at Pulau Weh was considered to be of Pleistocene age, but fumaroles and hot springs are present along a NW-E-trending line along the summit of the island and near the western shore of Lhok Perialakot bay on the northern side of the island.

Copyrighted photo by Michael Thirnbeck, 2006.

Copyrighted image used with permission. All Rights Reserved. Contact photographer for any usage requests.

Keywords: island volcano


Pulau Weh