The source of the iron in the Washington beaches is probably from the extensive basalt lava flows in the northwestern USA. Basalt is a mafic rock composed mostly of iron and magnesium silicates. There are many fewer mafic rocks inland from Santa Cruz. At 03:27 PM 9/27/99 -0700, you wrote: >In working with my kids at SVJH in Gilroy, I had one student ask the >following: > >He was doing an experiment to determine the amount of iron in the sand >at various beaches. He noted that sand from a beach in the state of >Washington had about 5 times as much iron as one from Santa Cruz, CA. >His conclusion was that the closer you get to the N or S pole, the >stronger the magnetic field, and that's why there is more iron in the >sand the further north you go. > >So what do I tell him..... Thanks Jan > > >_____________________________________________________________________ > >Public Seismic Network Mailing List (PSN-L) > >To leave this list email listserver@.............. with the body of the >message: leave PSN-L > Robert Mathieson Culver-Stockton College Canton, MO 63435 (217)231-6000 rmathieson@.......... _____________________________________________________________________ Public Seismic Network Mailing List (PSN-L)
Larry Cochrane <cochrane@..............>