Creating a chronology of the Murrumbidgee River

Globe-combing

And now for something a little different. In June and July this year,  I found myself at a conference on paleoclimate, landscapes, vegetation, humans and ended up bumping along dirt roads in a mini bus visiting many curious locations with a very interesting bunch of researchers. How old our our rivers and landscapes? How did climate change affect that landscape? Where did all the dust and water come from and where did it go? Below are some photos of two locations where researchers such as Page, Nanson and Price (1996) gathered dates showing five phases of paleochannel activity along the  Murrumbidgee area of the Riverine Plain of southeastern Australia. The first two phases suggest greater fluvial activity and reduced dust activity followed by seasonal snow melts and increased peak flows after the last Glacial Maximum and the build up of source bordering aeolian dunes. Finally the present flow regime was established around 12,000 years ago…

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