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Geologic Map of the Midvale Hill Quadrangle, Washington County

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Geologic Map of the Midvale Hill Quadrangle, Washington County IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 184 MOSCOW AND BOISE IDAHOGEOLOGY.ORG FEENEY AND PHILLIPS GEOLOGIC MAP OF THE MIDVALE HILL QUADRANGLE, CORRELATION OF MAP UNITS deposits between volcanics flows, and zones of high silicification. indicate only flows from magnetostratigraphic unit R1 appear in Artificial Mass Wasting Alluvial Deposits Microprobe analyses obtained from three separate glass domains within a Deposits Deposits west-central Idaho (Birch Creek and Downey Gulch members), we assign ASHINGTON OUNTY, DAHO single tuff sample indicate both basalt and rhyolite glass compositions W C I this unit to R1. The majority of Grande Ronde Basalt is chemically classified m (Table 3). Unit thickness is estimated to be 76 m (250 ft). Qaw Qas Holocene as basaltic andesite (Figure 1; Table 1) and is distinguished from other Qls Qt1 regional basaltic andesites by having TiO greater than 1.6 weight percent, Qaf 0.01 ka Ash deposits—Finely laminated beds of reworked, white and off-white ash 2 Qtm Qfg QUATERNARY Ni less than 56 ppm, and V greater than 225 ppm. An exposure on the west Dennis M. Feeney and William M. Phillips surrounded by beds of arkosic sand, up to 2 m (6 ft) thick. side of hill 4033 (SW¼ sec. 7, T. 13 N., R. 4 W.) shows a thickness of 160 Pleistocene Diatom deposits—White to light-yellow blocky diatom bed, composed m (530 ft). Sedimentary interbeds are locally present between flows but not thick enough to be mapped. Aphyric flows of Grande Ronde basalt served 2018 Qafo primarily of Melosira sp. with impurities of clay and micas, ranging in thickness from 0.5 to 3 m (2 to 18 ft). Powers (1947) described three as a source of tools for indigenous peoples; one of those sites is at the diatom-bearing beds found from the southwest corner of the map to aggregate quarry on Midvale Hill (Bakewell, (2005). 2.6 Ma Thousand Springs Creek and Sage Creek, and noted primarily Aulacoseira Tgr sp.(= Melosira) and rare Stephanodiscus sp., Navicula sp., and Fragilaria sp. 1 Sedimentary Deposits ¬ Qas Pliocene 5 Qaf 15DF365 Qafo VOLCANIC ROCKS ¬ ¬ Tgr1 ¬ 5.3 Ma V o l c a n i c R o c k s Weiser volcanics 5 ? Pyroclastic Rhyolite and Basaltic Basalt 15DF366 Qaf Qafo Twaw Rocks andesite andesite Weiser andesite of Weiser River (middle Miocene?)—Medium- to dark-gray, REFERENCES TERTIARY conchoidally fractured mostly aphyric andesite (Table 1). Contains 15 Weiser volcanics Tgr1 percent microphenocrysts of plagioclase (80 percent) and augite (20 Tgr Bakewell, E.F., 2005, The Archaeopetrology of virtophyric toolstones, with 1 Twaw percent); the remaining is groundmass with approximately 25 percent glass Tsp and 5 percent opaques. The andesite of Weiser River was informally applications to archaeology in the Pacific Northwest: University of Wash- Qafo Twbm Tgr1 referred to as Twa in the Mann Creek SE quadrangle (Feeney and others, ington Ph.D. dissertation, 194 p. 3 Barry, T.L., S.P. Kelley, S.P. Reidel, V.E. Camp, S. Self, N.A. Jarboe, R.A. Duncan, V9 2014), where it emerges as a dome of stacked flows north of Concrete Twp Twb2 siding. In the Midvale Hill quadrangle, outcrops are adjacent to the modern and P.R. Renne, 2013, Eruption chronology of the Columbia River Basalt 15DF367 Group, in S.P. Reidel, V.E. Camp, M.E. Ross, J.A. Wolff, B.S. Martin, T.L. 5 Twb Weiser River and Thousand Springs Creek, suggesting that the unit filled an 1 Miocene Tolan, and R.E. Wells, eds., The Columbia River Basalt Province: Geologi- 15DF375 ancestral river channel. Unit is tentatively included in the Weiser volcanics, 5 however morphology of the unit and location in the modern Weiser River cal Society of America Special Paper 497, p. 45-66. Twba channel may indicate this unit is as young as the Pliocene. The highly Butler, R.F., 1992, Paleomagnetism: Blackwell Scientific, 317 p. Feeney, D.M., and W.M. Phillips, 2016, Geologic map of the Midvale quad- Qafo conchoidal nature of fractures in the andesite makes it a significant archaeological source of “Paiute” tool stone (Bakewell, 2002; Bakewell, rangle, Washington County, Idaho: Idaho Geological Survey Digital Web 9 Map 179, scale 1:24,000. ¬ Columbia River 2005). W Tsp Feeney, D.M., D.L. Garwood, and W.M. Phillips, 2014, Geologic map of the ¬ Basalt Group ¬ Twbm Weiser basalt of Mann Creek (middle Miocene)—Three to five flows of Mann Creek SE quadrangle, Washington County, Idaho: Idaho Geological Tgr1 dark-gray to medium bluish-gray, and dark reddish-brown, fine- to Survey Digital Web Map 169, scale 1:24,000. Qafo Tgr1 medium-grained basalt and basaltic andesite (Table 1) with normal Feeney, D.M., R.S. Lewis, W.M. Phillips, D.L. Garwood, and S.W. Cooley, 5 *40Ar/39Ar dates personal communication from R. Gaschnig, 2015. magnetic polarity as determined by ChRM analyses (Table 2). Flows range 2016, Geologic map of the Hog Creek Butte quadrangle, Washington and ¬ 15DF368 5 15DF374 from 3 to 7 m (10 to 23 ft) thick. Plagioclase abundant and as much as 2 Adams counties, Idaho: Idaho Geological Survey Digital Web Map 174, ¬ mm in length. The best exposure is a roadcut along Highway 95 (SW¼ sec. scale 1:24,000. 6, T.12 N., R. 4 W). The roadcut shows the complex relationship of the Fitzgerald, J.F., 1979, An examination of two vents in the Columbia River Tgr1 ¬ Qaf basalt of Mann Creek and the Payette Formation. This zone includes basalts, Weiser embayment, Idaho: Geological Society of America Qafo INTRODUCTION grayish-yellow palagonitic basalt, localized blocks of glassy basalt, zones Abstracts with Programs, v. 11, no. 6, p. 272. Qafo with siderite nodules, and interfingering zones of baked Payette Formation; Fitzgerald, J.F., 1981, Geology and basalt stratigraphy of the Weiser embay- Qafo all indicating these basalts interacted with water and Payette Formation as ment, west-central Idaho: University of Idaho Ph.D. dissertation, 121 p. Tsp 15DF373 The geologic map of the Midvale Hill 7.5’ quadrangle depicts the rock units Qt1 Lower terrace alluvium of Weiser River (Holocene)—Predominantly well- the flows followed the ancestral Mann Creek drainage. The top flow is Fitzgerald, J.F., 1982, Geology and basalt stratigraphy of the Weiser embay- 5 Qafo exposed at the surface or underlying a thin cover of soil or colluvium; rounded basaltic cobbles and brown silty sand and clayey sand; thickness overlying a diatom bed that is 40 to 70 cm thick. ment, west-central Idaho, in Bill Bonnichsen and R.M. Breckenridge, eds., m Tsp 515DF372 alluvial and man-made surficial deposits are also shown where they form of about 1.8 to 6 m (6 to 20 ft). Subject to flooding during spring snowmelt Cenozoic Geology of Idaho: Idaho Bureau of Mines and Geology Bulletin significant mappable units. This map is a result of fieldwork conducted in or during winter rain-on-snow events in headwaters. Twp Weiser pyroclastic rocks (middle Miocene)—Yellow-buff and light-gray to 26, p. 103-128. the summer and autumn of 2015 by the authors. Previous mapping in the olive-green tuff. Contains abundant 0.5 to 5 cm subrounded to angular, Garwood, D.L., D.M. Feeney, and W.M. Phillips, 2014, Geologic map of the 5 Qtm area includes reconnaissance mapping of Kirkham (1931), the reconnais- Terrace alluvium of Mann Creek (Late Pleistocene)—Poorly exposed clast- finely vesiculated, rusty-brown to reddish-brown clasts of basalt in a poorly Nutmeg Flat quadrangle, Washington County, Idaho: Idaho Geological 15DF371 Qaf sance geologic map of the Weiser geothermal area (McIntyre, 1976), the supported gravel and sand capped with eolian sediments and sandy collu- sorted matrix. Layers are crudely sorted and the unit is characterized by Survey Digital Web Map 168, scale 1:24,000. ¬ basalt of the Weiser embayment 1:250,000-scale map (Fitzgerald, 1981; vium. Consists of well-rounded imbricated cobbles of basalt with light- little or no soil development. Fitzgerald (1979) interprets the zone of Twp Idaho Department of Water Resources (IDWR), 2016, Water Well data. 1982), the Baker 1:250,000-scale surficial geologic map (Othberg, 1982), brown medium- to coarse-grained arkosic sand matrix. Locally interbedded mapped across secs. 25 and 36, T. 13 N., R. 4 W. as a vent. Similar Available at: http://www.idwr.idaho.gov/GeographicInfo/gisdata/gis_data. 9 Tsp and the 1:100,000-scale geologic map of the Payette National Forest (Lund, with orange-brown, coarse- to medium-grained arkosic sand. The sand pyroclastic deposits are found in abundance as interbeds with Weiser htm (accessed January 15, 2016). 9 V V 2004). The unpublished field maps, field notes, hand-held magnetometer beds are cross-bedded and form lenticular, discontinuous beds. Unit is volcanics. More work is necessary to subdivide the pyroclastic deposits in Irvine, T.N., and Baragar, W.R.A., 1971, A guide to the chemical classification data, and XRF whole rock geochemistry (which were reanalyzed in 2015 approximately 4 m (13 ft) thick. the region. Thickness ranges from 2 to 5 m (6 to 16 ft). of the common volcanic rocks, Canadian Journal of Earth Sciences, v. 8, no. Twb1 for trace elements) from James Fitzgerald’s PhD were also consulted where Qfg 5, pp. 523–548. ¬ Flood gravels (Holocene to Late Pleistocene)—Cobbles and boulders Twb Weiser basalt 2 (middle Miocene)—Two to three flows of medium- to dark-gray m appropriate. Additional references are provided in the Description of Map 2 Kessler, M.A., and B.T. Werner, 2003, Self-organization of sorted patterned ¬ Tgr1 composed of locally derived basalt, basaltic andesite, and andesite, with shades of purple, fine- to medium-grained basalt.
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