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Fig. 11. Fanglomerate facies of the Puye Formation. Top photograph shows beds of light-colored, ash-rich fluvial deposits and gray gravel and cobble deposits. Deposits are made up primarily of crystalline dacite detritus. Middle photograph shows gray, poorly sorted gravel and cobble beds overlying light-colored, ash-rich sands and gravels. Bottom photograph is mudflow deposit with crystalline dacite clasts supported in a silty to sandy matrix. Top photograph taken near Totavi. Middle and bottom photographs taken in Rendija Canyon.
