Unit is named the Tygh Valley Formation of the Dalles Group. Consists of interbedded basaltic, andesitic, and pumiceous sandstone and conglomerate, tuffaceous sandstone and siltstone, tuff, breccia, and agglomerate in the Tygh basin. Disconformably overlies the Frenchman Springs Member of the Wanapum Basalt and the Grande Ronde Basalt, both of the Columbia River Basalt Group; underlies Miocene and Pliocene andesite flows of the Cascade Range. Age is middle Miocene to Pliocene based on radiometric (K-Ar) ages. (B1565)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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