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One can see from elevation or relief maps that the submerged land to the south of Sumatra and Java are not under deep, but under relatively shallow water.
To what extent will the islands on the tongue suffer during the plate movements described? Sumatra and Java of course ride at the edge of the plate, and are land masses rather than seabed because of the subduction pressure.
Where this is causing extensive volcanic activity in Sumatra and Java, it is also finding weak places in the plate holding Indonesia, which can buckle in such a manner as to rise.
Where this is causing extensive volcanic activity in Sumatra and Java, it is also finding weak places in the plate holding Indonesia, which can buckle in such a manner as to rise.
But there has not been any evidence of a tipping up on the eastern side until buoys 56001 and 56003 below Sumatra and Java showed a rising sea flood, as outlined in Issue 218 of this newsletter on December 31, 2010, and now the eastern coastline of Sri Lanka awash.
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