To: Gib Bogle who wrote (72645 ) 2/27/2010 8:45:20 PM From: Maurice Winn 1 Recommendation Read Replies (1) | Respond to of 74559 I had assumed all the iron sand came from erosion of sub-sea old volcanoes in the Tasman sea [with the hot spots gradually migrating east, now under east Auckland [Rangitoto vicinity I suppose]. But perhaps a lot of it goes down the Wanganui River from Taupo and up the coast. It seems an extraordinary waste of effort and talent to be top in engineering then go and run noisy restaurants in New York. [I asked Google]. < In NZ my only coastal projects have been in modelling flows and transport (sediment and effluent) in the Auckland harbours. > Having grown up literally in the Manukau Harbour, I have a fondness for it. 55 years ago it was seething with marine life. 20 years ago it was totally dead, not a single worm or even bits of algae. There were presumably anaerobic bacteria festering in the ooze. Now it is coming back to life, rapidly - I have made regular visits to the mud to see how it was progressing. My 86 year old Uncle has been in recent weeks doing battle with the foreshore at the start of the old bridge causeway, clearing it of debris and making a little reclamation with some flowers and stuff. He says [and I agree] that the whole area to west of the causeway should be reclaimed for recreation purposes. The mangroves should all be removed from the harbour. A barge, hoist and tree mulcher and community services volunteers wanting a day out of gaol or off the dole could do the work. I calculated the odds of Taupo erupting in any one lifetime as being about one in ten, which is quite good odds of going up in a bang. That's quite a risk profile for a city. And, of course, the longer the time before it erupts, those odds get worse because the pressure down below keeps increasing. To avoid Taupo eruptions, stay clear when it's spring tide time, after a long dry summer, when a low pressure zone arrives. Mqurice