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U.S. Department of the Interior Open-File Report 2014–1063 U.S. Geological Survey Sheet 2 of 2 CORRELATION OF MAP UNITS locally; upper part of unit is equivalent in age to the Cowlitz (upthrown) and D (downthrown) show vertical displacement; traps may be present in structures beneath the relatively flat-lying basalts of the doi: 10.1130/2009.fl d015(32). Formation in west half of map area (Rau, 1958); Foraminifera arrows show lateral displacement on map and vertical displace- Columbia River Group, as well as where sandstones of the Cowlitz Formation Wells, R.E., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., VOLCANIC AND INTRUSIVE and Wooden, J., 2014, Geologic history of Siletzia, a large igneous referred to Narizian Stage of Mallory (1959); equivalent to ment in cross section are faulted up-dip against impermeable strata. Stratigraphic traps also may be SEDIMENTARY ROCKS ROCKS province in the Oregon and Washington Coast Range: Correlation to the upper part of Henriksen’s (1956) Stillwater Creek Member of D Fault inferred from side-looking radar imagery (SLRI) present where sandstones of the Cowlitz or McIntosh Formations pinch out or U geomagnetic polarity time scale and implications for a long-lived the Cowlitz Formation; coccoliths from lower part of referable —Showing sense of vertical displacement; not field-checked become channelized in the western-facies deeper water siltstones. Qal Holocene Yellowstone hotspot: Geosphere, v. 10, no. 4, 28 p., # Qls QUATERNARY to CP 14a zone (R. Wells sample W92-2a,b,c; D. Bukry written # Thrust fault—Approximately located; sawteeth on upper plate doi:10.1130/GES01018.1. Qlh Pleistocene commun., 1992) REFERENCES CITED Slickenlines—On fault plane, showing azimuth and plunge Unconformity Tmus Unnamed sandstone (middle Eocene)—Massive to thick- Addicott, W.O., 1976, Neogene molluscan stages of Oregon and Washington, in bedded, plane-laminated to crossbedded, friable, fine- to Fritsche, A.E. (chairman), Ter Best, Harry, Jr., and Wornardt, W.W., eds., 123°30' 00” 123°15' 00” 123°00' 00” Tsmp S 12 Inclined medium-grained, arkosic sandstone interbedded at base of the The Neogene symposium, selected technical papers on paleontology, 46°45' 00" S sedimentology, petrology, tectonics and geologic history of the Pacific Unconformity upper member of the McIntosh Formation (Tmu) S û Horizontal—Combined with fault-dip symbol on vertical faults Coast of North America—Tomorrow's oil from today's provinces: Society Tau Tnm Tml McIntosh Formation, lower member (lower and middle Middle Folds—Showing fold crestline; showing direction of plunge where it of Economic Paleontologists and Mineralogists, Pacific Section, Proceed- DEAN DOTY RAINBOW ADNA Eocene)—Massive to thin-bedded and laminated, very fine- to CREEK FALLS Twfs Miocene can be inferred; dashed where location is inferred; dotted where ings, 51st Annual Meeting, San Francisco, Calif., April 21–24, 1976, no. Miocene coarse-grained basaltic sandstone, arkosic sandstone, and location is concealed 51, p. 95–115. Unconformity Timb laminated, tuffaceous siltstone; sandstone commonly shows Armentrout, J.M., 1975, Molluscan biostratigraphy of the Lincoln Creek 46°38' 13" graded bedding; sandstones are less common on east flank of ( Tgr F Anticline Willapa Hills; interbedded in lower part are pillow basalt flows Formation, southwest Washington, in Weaver, D.W., Hornaday, G.R., and ( Tipton, Ann., eds., Paleogene symposium and selected technical papers- Unconformity of the Crescent Formation; Foraminifera referred to upper M Syncline Middle and Ulatisian and lower Narizian Stages of Mallory (1959); equiva- Future energy horizons of the Pacific coast: American Association of Tal Early Miocene lent to lower part of Henriksen's (1956) Stillwater Creek Bedding in pillow lava—Showing up direction; shown only in Petroleum Geologists–Society of Economic Paleontologists and PLUVIUS PE ELL BOISTFORT CURTIS Oligocene cross-section within the Crescent Formation Mineralogists–Society of Economic Geologists, Pacific Sections, 50th Tlc Member of the Cowlitz Formation Tlcs Annual Meeting, Long Beach, Calif., April, 1975, p. 14–48. Tcbs Strike and dip of beds Basalt breccia and sandstone (middle and lower Eocene)— Beeson, M.H., Perttu, R., and Perttu, Janice, 1979, The origin of the Miocene Unconformity Massive to well-bedded basalt-lapilli tuff, tuff breccia, basaltic o12 Inclined—Dips along streams in unit Qal are measured on basalts of Coastal Oregon and Washington—An alternative hypothesis: 46°30' 00" Tsc sandstone, siltstone, and conglomerate; lapilli tuff consists of bedrock Oregon Geology, v. 41, no. 10, p. 159–166. palagonitic vesicular basaltic glass and altered glass shards Local Unconformity 85 Beeson, M.H., and Tolan, T.L., 2002, Basalt of Huntzinger, Asotin Member of Late TERTIARY commonly cemented by calcite and zeolite; graded bedding is s Overturned 1 Eocene Saddle Mountains Basalt, Columbia River Basalt Group (CRBG) identified BLANEY ELOCHMAN BOISTFORT WILDWOOD • 37-41 Ma1 39.6 ± 0.5 Ma • Tiqm common; forms thick sequences interbedded with the lower Tgv v Vertical—Top side of bedding shown by placement of 90° dip in western Washington [abs.]: Geological Society of America Abstracts CREEK PASS PEAK member of the McIntosh Formation (Tml) and upper part of the Unconformity value with Programs, v. 34, no. 5, p. 33. Crescent Formation Chan, C.F., Tepper, J.H., and Nelson, B.K., 2012, Petrology of the Grays River Tc Tcv Tcb Crescent Formation (lower middle lower Eocene)—Pillow flows, e Horizontal volcanics, southwest Washington—Plume-influenced slab window magma- Unconformity massive and columnar-jointed flow interiors, pillow breccia, tism in the Cascadia forearc: Geological Society of America Bulletin, v. ¦64 Strike and dip of igneous foliation—Shown only in unit Tig, Tmu Eocene lapilli-tuff breccia, and filled lava tubes of tholeiitic and alkalic 124, p. 1324–1338. Middle basalt; basalt groundmass altered to green and brown clays; gabbro and basalt intrusive rocks Eocene Henriksen, D.A., 1956, Eocene stratigraphy of the lower Cowlitz River eastern SKAMOKAWA SKAMOKAWA ELOCHMAN ABERNATHY Tmus Tib zeolite and calcite fracture fillings are ubiquitous; contains ². TD 140 PASS LAKE MOUNTAIN Tm Water well with gas show—Showing total depth (TD) of well in Willapa Hills area, southwestern Washington: Washington Division of minor amounts of mudflow breccia, basaltic sandstone, and Local Unconformity feet Mines and Geology Bulletin 43, 122 p. interbedded laminated siltstone; includes a few dikes and sills Kleibacker, D.W., 2001, Sequence stratigraphy and lithofacies of the middle Tig not differentiated on map; unit is interpreted as faulted, Eocene upper McIntosh and Cowlitz Formations—Geology of the Grays 46°15' 00" 48.7 ± 0.5 Ma1 • Tml deformed, and clockwise-rotated seamount built on oceanic River Volcanics, Castle Rock–Germany Creek area, southwest Washington: Tcsb INTRODUCTION Middle and crust (Wells and Coe, 1985), similar to the Siletz River Volca- Corvallis, Oregon State University, M.S. thesis, 219 p. Tcbs This digital map database and the PDF derived from the database were Early Eocene nics of Snavely and others (1968); Foraminifera from interbed- Tcb created from the analog geologic map: Wells, R.E. (1981), “Geologic map of the Kleinpell, R.M., 1938, Miocene stratigraphy of California: Tulsa, Okla., CATHLAMET NASSA OAK POINT COAL CREEK Tcs ded siltstones referred to upper Penutian or Ulatisian Stages of 53.6 ± 2.0 Ma1 • eastern Willapa Hills, Cowlitz, Lewis, and Wahkiakum Counties, Washington.” American Association of Petroleum Geologists Special Volume SP9, 450 p. POINT Mallory (1959); 40Ar/39Ar ages of 53.6±2.0 and 55.7±1.0 Ma are 55.7 ± 1.0 Ma1 • The geodatabase replicates the geologic mapping of the 1981 report with minor Livingston, V.E., Jr., 1966, Geology and mineral resources of the Kelso- reported from the unit in the western Willapa Hills (Moothart, exceptions along water boundaries and also along the north and south map Cathlamet area, Cowlitz and Wahkiakum Counties, Washington: 46°08' 33" 1993); locally subdivided into the following: boundaries. Slight adjustments to contacts along water boundaries were made to Washington Division of Mines and Geology Bulletin 54, 110 p. Tcsb Subaerial basalt—Massive to very vesicular, platy, plagioclase- correct differences between the topographic base map used in the 1981 compila- Magill, J., Wells, R.E., Simpson, R.W., and Cox, A.V., 1982, Post 12 m.y. INDEX MAP SHOWING MAP AREA (SHADED) IN RELATION TO U.S. phyric basalt flows and flow breccias that have weathered tops tion (analog USGS 15-minute series quadrangle maps at 1:62,500 scale) and the rotations of southwestern Washington: Journal of Geophysical Research, v. GEOLOGICAL SURVEY 7.5-MINUTE QUADRANGLES and baked and oxidized bottom contacts; interbedded with base map used for this digital compilation (scanned USGS 7.5-minute series 87, p. 3761–3776. Member of the Wanapum Basalt (Twf) by discontinuous arkosic DESCRIPTION OF MAP UNITS basalt-boulder conglomerate; basalt groundmass is in part quadrangle maps at 1:24,000 scale). These minor adjustments, however, did not Mallory, V.S., 1959, Lower Tertiary biostratigraphy of the California Coast sandstone containing carbonized logs; maximum thickness, 75 altered to clays, and vesicles are filled with calcite and zeolite materially alter the geologic map. No new field mapping was performed to Ranges: Tulsa, Okla., American Association of Petroleum Geologists VOLCANIC AND SEDIMENTARY ROCKS
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