File:Soufriere Hills Volcano dome collapse.gif

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Original file(1,791 × 1,791 pixels, file size: 1.27 MB, MIME type: image/gif, looped, 2 frames, 4.0 s)

Summary

These false-colour <a href="//commons.wikimedia.org/w/index.php?title=Satellite&action=edit&redlink=1" class="new" title="Satellite (page does not exist)">satellite</a> images show the southern half of <a href="//commons.wikimedia.org/wiki/Montserrat" class="mw-redirect" title="Montserrat">Montserrat</a> before and after its dome collapsed. Red areas are <a href="//commons.wikimedia.org/w/index.php?title=Category:Vegetation&action=edit&redlink=1" class="new" title="Category:Vegetation (page does not exist)">vegetated</a>, <a href="//commons.wikimedia.org/wiki/Cloud" title="Cloud">clouds</a> are white, blue/black areas are ocean <a href="//commons.wikimedia.org/wiki/Water" title="Water">water</a>, and grey areas are covered by flow deposits. Fresh deposits tend to be lighter than older deposits. the drainages leading down from Soufrière Hills, including the White River Valley, the Tar River Valley, and the Belham River Valley, were filled with fresh debris.

Licensing

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File history

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Date/TimeThumbnailDimensionsUserComment
current06:39, 12 January 2017Thumbnail for version as of 06:39, 12 January 20171,791 × 1,791 (1.27 MB)127.0.0.1 (talk)These false-colour <a href="//commons.wikimedia.org/w/index.php?title=Satellite&action=edit&redlink=1" class="new" title="Satellite (page does not exist)">satellite</a> images show the southern half of <a href="//commons.wikimedia.org/wiki/Montserrat" class="mw-redirect" title="Montserrat">Montserrat</a> before and after its dome collapsed. Red areas are <a href="//commons.wikimedia.org/w/index.php?title=Category:Vegetation&action=edit&redlink=1" class="new" title="Category:Vegetation (page does not exist)">vegetated</a>, <a href="//commons.wikimedia.org/wiki/Cloud" title="Cloud">clouds</a> are white, blue/black areas are ocean <a href="//commons.wikimedia.org/wiki/Water" title="Water">water</a>, and grey areas are covered by flow deposits. Fresh deposits tend to be lighter than older deposits. the drainages leading down from Soufrière Hills, including the White River Valley, the Tar River Valley, and the Belham River Valley, were filled with fresh debris.
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