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Examples

  • There is still plenty of ice up there, and groundwater, and the magma is moving and the craters and fissures within the calders may be lengthening and coalescing.

    ScienceBlogs Channel : Life Science Steinn Sigur 2010

  • There is still plenty of ice up there, and groundwater, and the magma is moving and the craters and fissures within the calders may be lengthening and coalescing.

    ScienceBlogs Channel : Life Science Steinn Sigur 2010

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