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Cobbles of Cave Creek, Arizona

Cobbles of Cave Creek, Arizona

There are two distinct kinds of rocks in this picture, the young faintly purple volcanic boulders are from the abundant Miocene ~ 15 million years basaltic lava beds upstream.  An exception is the light-colored one in the upper right corner which is a felsic ash-flow tuff (~23-20 million).  All the greenish hued rocks in the picture are indeed metamorphic and way older.  They are mostly volcanic, the product of a volcanic arc (like Japan) that was added to the rim of the North America continent ~1700 million years ago.  The chlorite content will vary from as low as 2-5% to 30-40% depending on what kind of volcanic rock was metamorphosed, and there are at least 12 different formations of green chloritic metamorphic volcanic and associated sedimentary rocks in that area. I can pick out at least four (Xcg: conglomerate – the lower left boulder, Xms:  green argillite – upper middle, Xma: mafic lava – upper right, and Xfv: felsic lava – right center).    The file I attach is one of the smaller of four pdfs you can download for free from our website (repository.azgs.az.gov) that cover the geology of the New River Mesa, AZGS OFR-98-12.  This, the written report has detailed descriptions of many of the formations represented by the boulders in your picture; the others area a geologic map, a set of geologic cross-sections, and an explanation.  There are several other maps in your area, including one for Cave Creek AZGS OFR-97-1, Humboldt Mountain AZGS OFR-98-11, and Bartlett Dam AZGS OFR-96-22.  

Text by Charles Ferguson.

Photographer: Thomas McGuire

Photo Date: 2018