Two synchronous members distinguished in Gualala Formation (rank herein reduced from group to formation) are (ascending) are Stewarts Point and Anchor Bay Members. [Type not designated.] Stewarts Point Member is characterized by gray-white arkose rich in potassium feldspar. Is considered Late Cretaceous age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
strata of Stewarts Point. [Name Stewarts Point "Member" not used.] Gualala Group of Weaver (1943) divided into three mappable units (ascending), informally called: strata of Stewarts Point, strata of Anchor Bay, and strata of German Rancho. Strata of Stewarts Point consist of gray-white K-feldspar arkose, gray-black mudstone, and conglomerate with exposed thickness of 4,400 feet. Interfingers with and underlies strata of Anchor Bay. In fault contact with underlying spilite near Black Point. Fossils sparse. Foraminifers diagnostic of Goudkoff's E zone (Popenoe and others, 1960) indicate age near Campanian-Maestrichtian boundary.
Source: Modified from GNU records (USGS DDS-6; Menlo GNULEX).
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