Geologic map of the Priest Rapids 1:100,000 quadrangle, Washington

Abstract

Commissioner of Public Lands Kaleen Cottingham-Supervisor MSTRIBUTION OF THIS DOCUMENT I S U N U M W d*' PLATE (accompanies text) Plate 1. Geologic map of the Priest Rapids 1:1oO,OOO quadrangle, Washington DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, , manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recom-' mendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.

Hanford Site National Environmental Policy Act (NEPA) characterization. Revision 10

“…There is a major thrust to high-angle reverse fault on the north side of the Umtanum Ridge structure (PSPL 1982, Reidel andFecht 1994b) that dies out as it plunges eastward past the Gable Mountain-Gable Butte segment. Gable Mountain and Gable Butte are two topographically isolated, anticlinal ridges composed of a series of northwest-trending, doubly plunging, echelon anticlines, synclines, and associated faults.…”

Geologic Data Package for the 2005 Integrated Disposal Facility Waste Performance Assessment

“…The principal geologic units exposed at the surface are fluvial and eolian sands (Reidel and Fecht 1994a, 1994b, 2005. The fluvial sands were deposited by the Missoula floods and have since been reworked by westerly winds to form a thin veneer of eolian deposits.…”