Geologic map of the Curlew quadrangle, Ferry County, Washington

Geology of the Bald Knob quadrangle, Ferry and Okanogan Counties, Washington

“…The longest fault in the Scatter Creek fault zone is the Long Lake fault, which has been traced from Long Lake on the northern boundry of the quadrangle to the southwest corner of the quadrangle. This Geology in the Curlew quadrangle by Calkins, Parker, and Disbrow (1959); in the Republic and Wauconda quadrangles by Muessig and Quinlan (1959) FIGUBE 7. Generalized geologic map of the Republic graben.…”

“…1); Pardee (1918, p. 33-34) considered the rocks to be probably of Mesozoic age. More recent mapping to GEOLOGY, BALD KNOB QUADRANGLE, WASHINGTON F25 the north of the reservation by Muessig and Quinlan (1959) in the Republic quadrangle and by Calkins, Parker, and Disbrow (1959) in the Curlew quadrangle indicates that some of the granitic rocks are of Tertiary age. In these two quadrangles the O'Brien Creek Formation of Eocene (?)…”

“…The west edge of the Colville batholith has been mapped along the Okanogan Valley north of Omak almost to the Canadian border (Waters and Krauskopf, 1941, pi. 1), and granitic rocks have been mapped by Muessig and Quinlan (1959) in the Republic and Wauconda quadrangles and by Calkins, Parker, and Disbrow (1959) in the central and southern part of the Curlew quadrangle.…”

“…7). The graben was mapped in detail by Calkins, Parker, and Disbrow (1959) in the Curlew quadrangle, by Muessig and Quinlan (1959) in the Wauconda and Republic quadrangles, and by me in the Bald Knob quadrangle. The north end of the graben is in the northern part of the Curlew quadrangle 2; it trends from there south-southwest for 52 miles to the southern end of the Bald Knob quadrangle.…”