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Geologic Map of the Magic Reservoir East Quadrangle, Blaine and Camas Counties, Idaho

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Geologic Map of the Magic Reservoir East Quadrangle, Blaine and Camas Counties, Idaho IDAHO GEOLOGICAL SURVEY DIGITAL WEB MAP 82 MOSCOW-BOISE-POCATELLO KAUFFMAN AND OTHBERG GEOLOGIC MAP OF THE MAGIC RESERVOIR EAST QUADRANGLE, Disclaimer: This Digital Web Map is an informal report and may be BLAINE AND CAMAS COUNTIES, IDAHO revised and formally published at a later time. Its content and format may not conform to agency standards. John D. Kauffman and Kurt L. Othberg 2007 CORRELATION OF MAP UNITS Qags Pdm Qags Qag2 Qam Qag 2 Unconsolidated Sedimentary and Mass Movement Deposits Volcanic Rocks Kap Qags Qag3 Artificial Basaltic Silicic Intrusive Sedimentary Alluvial Deposits Mass Movement Deposits Deposits Rocks Rocks Rocks Rocks Qam m Holocene Qam Qas Qaf Qt Qags Qag Qls Qag 2 Kgdh Qags Qaf Qag 3 ? ? Qas Kgdh QUATERNARY Qsfb Pleistocene Qags Qmb Qag2 Qam ? Qwrb QTac CENOZOIC Qas Tsma Kap Qags Kgdh Pliocene Trbt Twbr Qags Tcbb TERTIARY Qag2 Tpt Miocene Eocene Qam Tcv Qam Kap Qaf CRETACEOUS MESOZOIC Qaf Kgdh Pdm PERMIAN PALEOZOIC Qag 3 Qam m Kgdh INTRODUCTION from about 30 feet near Ditto Hill to at least 70 feet at Sheep Bridge where INTRUSIVE ROCKS Qaf the base is not exposed. Thickening is probably due to irregularities in the The geologic map of the Magic Reservoir East quadrangle depicts rock units preflow topography. Stream drainage is moderately well developed. Basalt Kap Aplite dikes (Cretaceous?)Fine-grained, light-colored granitic dikes cutting Qag 3? exposed at the surface or underlying thin surficial cover of soil and colluvium. surface covered by silt and clay (loess?) 2-4 feet thick and includes a well- Kgdh unit. More abundant than shown, based on presence of fragments in m Thicker surficial deposits are also depicted where they mask or modify the developed soil caliche (duripan). Variations in soil characteristics and the overburden. Qag 3? underlying rock units or form significant mappable units. The map is the vegetation form a patterned ground visible on aerial photographs. Qas Hornblende-biotite granodiorite (Cretaceous)Gray, medium- to coarse-grained, result of field work conducted in 2006 by the authors. Mapping by previous Kgdh Formerly divided into upper and lower units by Schmidt (1961), and equigranular to porphyritic hornblende-biotite granodiorite. Biotite is in Qag workers, noted below, was field checked and incorporated where appropriate. Qam 2 Struhsacker and others (1982) report three flows. However, we could find distinct books up to 4 mm across. Plagioclase displays oscillatory zoning Qam Soils information is from Johnson (1991, 2002). Kgdh Tcv no conclusive evidence of separate flows, although there do appear to be (An20-An40). Sphene unusually ambundant, perhaps as much as 1 percent m Previous work in the area includes that of Malde and others (1963), Schmidt several internal vesicular zones in the outcrop at Sheep Bridge. An 40Ar/39Ar locally. Equivalent to Kgdk unit of Worl and others (1991), who indicate it is a potassium-rich intrusive, having high K O content for a given SiO m m (1961), Leeman (1982), Struhsacker and others (1982), and Honjo (1986). date on the flow just west of Ditto Hill (Schmidt's upper flow) resulted in a 2 2 m content relative to other intrusives to the northwest. Also notable for the 02P020 Qas Malde and others conducted regional reconnaissance mapping, which plateau age of 1.54 ± 0.13 Ma and an inverse isochron age of 1.48 ± 0.22 relative abundance of gold-bearing quartz veins (Lewis, 1989; Worl and Qwrb Qag included the Magic Reservoir area, and established a regional stratigraphy. Ma (Idaho Geological Survey, unpublished data). For the flow at Sheep 3 m Qaf 40 39 Schmidt mapped the Bellevue area and provided a more detailed stratiagraphy Bridge (Schmidt's lower flow), an Ar/ Ar date resulted a plateau age of Lewis, 2001). Map unit includes locally derived thin gravel and sand in Qas Tpt 1.17 ± 0.21 Ma and an inverse isochron age of 1.06 ± 0.19 Ma (Idaho terrace remnants (Qsmr and Qsw of Schmidt, 1961). Qam m and description of units, although his main focus was on Quaternary units Qag Qam Qam 06JK752 Geological Survey, unpublished data). Chemical composition of samples 3 Qam and stream diversions by basalt flows. Leeman, using Schmidt's stratigraphic Tcv units, proposed a Magic Reservoir eruptive center to account for much of from the upper unit near Ditto Hill and the lowerunit at Sheep Bridge SEDIMENTARY ROCKS is indistinguishable (samples 02RB106 and 02P020; Table 1). Qag Qam Qag the volcanism in the area. Struhsacker and others worked in the northwestern 3 Tcv Dollarhide Formation, Middle Member (Lower Permian)Light-colored Qwrb 75 Qag3 part of the Magic Reservoir area and slightly modified Schmidt's stratigraphy, Pdm Andesite of Square Mountain (Pliocene)Fine-grained andesitic unit with calcareous sandstone, siliceous sandstone, sandy limestone, silty argillite, Qam 35 but concentrated on the rhyolitic units and provided little new mapping. Tsma plagioclase phenocrysts and locally common quartz and plagioclase and minor conglomerate. Kgdh Honjo essentially used the stratigraphic sequence of these previous workers. Qag3 Qls xenocrysts; also a few granitic or rhyolitic xenoliths. Forms capping unit on Our observations of several stratigraphic units in the Magic Reservoir East Clay Bank Hills east of Magic City where it is in unconformable, probably Qwrb and adjacent quadrangles do not support the stratigraphic interpretations of Qag Qaf Tpt erosional, contact with basalt of Clay Bank Hills or granitic rock of Kgdh Kgdh Tpt these previous workers. The discrepancies are noted and discussed below unit. Maximum thickness is about 100 feet. Thin erosional remnants extend SYMBOLS Qaf in the Description of Map Units. After Schmidts investigations, the extent south to just north of Rattlesnake Butte. Remanent magnetic polarity Qt Qags of field mapping by these subsequent workers may have been inadequate inconclusive, but probably reverse; both normal and reverse readings were Contact: Line showing the approximate boundary between one to identify the stratigraphic problems we observed. In addition, varying use obtained in the field. Commonly has curving, platy jointed zone 5-10 feet map unit and another. Qaf of the terms Moonstone Rhyolite, rhyolite of Magic Reservoir, and Qls Tcv thick below a stocky, crudely columnar top. The top weathers into large 02RB106 Tpt rhyolite ash-flow tuffs of Magic Reservoir for in some instances equivalent 15 subrounded blocks as much as 3 to 6 feet in diameter. One analyzed sample Tpt Tpt units and in other cases different units has confused the stratigraphic picture. Fault: Approximately located; dashed where inferred; dotted where 5 8 (sample 06JK712; Table ) plots in the upper part of the andesite field on the 18 Therefore we avoid using these terms. Instead, we use local geographic 18 total alkali-silica diagram of Le Maitre (1984). Chemical composition of our concealed; bar and ball on downthrown side; arrow indicates features or rock types for naming most units, noting correlation to the previous sample is very similar to those for the Square Mountain ferrolatite reported bearing and plunge of slickenside lineation on fault plane. units. Our mapping does not entirely resolve the stratigraphic questions, but in Honjo (1986) and Honjo and Leeman (1987), which also plot in the upper it provides additional information and alternatives that should be considered Quartz vein; dip shown by arrow. andesite field. and evaluated in future research and geologic mapping. Qwrb Qaf 3 Qaf Previously mapped as part of the Square Mountain basalt by Schmidt (1961) Tsma Strike and dip of basalt flow or volcanic layer. DESCRIPTION OF MAP UNITS who placed it stratigraphically below the basalt of Clay Bank Hills (Schmidt's Qaf Qas Clay Bank basalt). Struhsacker and others (1982) placed the Square Mountain Strike and dip of flow foliation. Kgdh ARTIFICIAL DEPOSITS basalt above their older rhyolite and below their Tuff 1 of Magic Reservoir 25 Tpt (equivalent to Schmidt's Poison Creek tuff), which they dated at 5.64 Ma. Tsma Made ground (Holocene)Artificial fills composed of excavated, transported, Tcv 5 m Honjo (1986), following Schmidt's (1961) and Struhsacker and others (1982) Kgdh and emplaced construction materials typically derived locally. Primarily stratigraphic sequence, also placed this unit below the basalt of Clay Bank Zone of lithophysal cavities. Tpt 10 includes highway fills and the fill portion of Magic Dam. Hills and below the Poison Creek tuff. However, we have found it capping and probably filling irregularities on the basalt of Clay Bank Hills and also Estimated strike and dip of basalt flow or volcanic layer. Kgdh Kgdh capping the Poison Creek tuff. On the basis of our preliminary field work Tsma Tpt SEDIMENTARY AND Tpt Tcv in the Magic Reservoir West quadrangle, we believe there is an older Tcv MASS MOVEMENT DEPOSITS xenolithic and xenocrystic unit stratigraphically lower than the basalt of 06JK717 Clay Bank Hills and above the older rhyolite of Magic Reservoir unit of Sample location and number. Kgdh Alluvial Deposits Struhsaker and others (1982) that resembles the Square Mountain unit. 06JK701 Schmidt (1961) places the Square Mountain basalt stratigraphically above Tsma 06JK712 Qam Alluvium of the Big Wood River (Holocene)Moderate- to well-sorted gray the rhyolite on Moonstone Mountain and Honjo and others (1986) report sandy pebble and cobble gravel with few boulders; stratified with gravelly Tpt an age of ~3.0-3.4 Ma for rhyolite at Moonstone Mountain. As noted below, coarse sand. Gravel clasts subrounded to rounded Paleozoic sedimentary Qls we obtained an age for the basalt of Clay Bank Hills of ~4.0 Ma. Therefore, REFERENCES Tcbb and metamorphic rocks, Cretaceous granitic rocks, and Eocene felsites. our stratigraphic position of the andesite unit above the basalt of Clay Bank 02P019 Thickness more than 10 feet. Hills is in accord with the reported ages.
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