Back in August of 2007, Linda & her husband took one of their many trips to Michigan’s Upper Peninsula & visiting Grand Marais, Ishpeming and Copper Harbor. She visited the Jasper Knob just outside of Ishpeming & writes:
It is a banded iron formation. The layers consist of jasper (the red rock) and hematite (the silvery rock). I’m delighted to tell you that some biogeologists believe that banded iron formations were formed by my old pals, the iron bacteria.
Head over to her photo blog for a lot more pictures and for sure check out her book They Breathe Iron for more about iron bacteria.