I was in Australia a couple of years ago and was very surprised to find a chain of relatively recent cinder cones on the Atherton Tableland just west of Cairns, Queensland. There was also an "explosion crater" of some type. The lava in the area appeared to be basalt. Is this a small hotspot, or is subduction responsible? Is any renewal of activity expected? Keep up your excellent work on Volcano World! Regards,
Dick Van Effen
Science writer
Midland Daily News
Midland, MI

rocky Dick Van Effen


Hi Dick,

I don't think the source of those relatively young basalts is really understood. I think it is not subduction-related, and if it is a hotspot it sure isn't a very active one. You are correct in recognizing that they are basalts, in fact some of the longest (if not THE longest) lava tubes are part of that volcanic group. As far as deciding whether future activity is probable you would have to compare the time since the most recent eruption to the average time between eruptions. Of course this only gives you a statistical answer, not a real one.
A few months ago there was a related question, and you can find the answer in the Australia section of the volcanoes of other regions section of previously-asked-questions of the ask-a-volcanologist section of VolcanoWorld.
You've asked a good question and I'm sorry I don't have a more definitive answer. There will be a workshop held at the University of North Queensland next summer that will deal with long lava flows in general, and perhaps theresomeone will have some good answers to your question.

Sincerely,

Scott Rowland


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