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The Gable Creek Formation is a sedimentary rock formation from the Albian age of the Early Cretaceous.[1] The formation is in Wheeler County, Oregon of the United States of America and is intertongued with the similarly aged Hudspeth Formation. The formation mostly consists of fluvial-deltaic sandstones and conglomerates.[2] Marine fossils can be found throughout the formation including various species of ammonites, clams and other mollusks. The Gable Creek Formation gets its name from Gable Creek, a creek that runs through much of the formation.
^"Gable Creek Formation - John Day Fossil Beds National Monument (U.S. National Park Service)". www.nps.gov. U.S.: U.S. National Park Service. Retrieved 2020-07-04.
^"BEDROCK GEOLOGY OF THE MITCHELL QUADRANGLE, WHEELER COUNTY, OREGON" (PDF). 1971. Retrieved July 4, 2020.
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