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Quaternary Geologic Map of the Shelby 1° × 2

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Quaternary Geologic Map of the Shelby 1° × 2 U.S. Department of the Interior Prepared in cooperation with the OPEN-FILE REPORT 2012–1170 U.S. Geological Survey Montana Bureau of Mines and Geology 112°00' 110°00' 49°00' 111°30' 111° 110°30' 49°00' % % LATE WISCONSIN % % lse % %% % Wild Horse Lake LIST OF MAP UNITS DESCRIPTION OF MAP UNITS SOURCES OF INFORMATION % B % % % lu % % % k e % % a % % e IT tlx al % lca [Map unit thickness is typical range; in some areas the map units may be thicker or LOAMY TILL—Sediment deposited chiefly by ice of a Laurentide continental ice Alden, W.C., 1924, Physiographic development of the northern Great Plains: Geological re r lca % C % % C % IT re tlx R thinner than the given range] sheet. Informal Fort Assiniboine till of Fullerton and Colton (1986). The till in the Society of America Bulletin, v. 35, p. 385–423. % jea ard e HOLOCENE AND LATE WISCONSIN % ch k IT % i % % r % % % % %% P tlx % northwestern part of the quadrangle was deposited by the Shelby glacial lobe; the Alden, W.C., 1932, Physiography and glacial geology of eastern Montana and adjacent areas: % lss % % R % al % % cly % FLOOD-PLAIN AND CHANNEL ALLUVIUM % % % % till in the northeastern part of the quadrangle was deposited by the Havre glacial % lu % % % U.S. Geological Survey Professional Paper 174, 133 p. % % 150 % Wild Horse Lake HOLOCENE AND LATE WISCONSIN % 0 lss % % lobe; the till in the southeastern part of the quadrangle was deposited by the Loma Calhoun, F.H.H., 1906, The Montana lobe of the Keewatin ice sheet: U.S. Geological Survey % crr % al FLOOD-PLAIN AND CHANNEL ALLUVIUM—Yellowish-brown, olive-brown, % % % % %% % % % afj % % gg % % ALLUVIAL-FAN DEPOSITS % %% % glacial sublobe (fig. 1). Regional ice flow patterns are recorded by ice-molded or Professional Paper 50, 62 p. %% % % % %% al % grayish-brown, brown, olive, yellowish-gray, brownish-gray, olive-gray, gray, % tlx % % % % % % % % % West ice-scoured landforms (shown by a symbol) and by the orientations of till ridges Christiansen, E.A., 1979, The Wisconsinan deglaciation of southern Saskatchewan and adjacent % % wla k La LOAMY AND CLAYEY SHEETWASH ALLUVIUM black, or mottled clay, silt, sand, and gravel. Calcareous or noncalcareous; partly % %% e ird Cree tlx % cly Butte e k % and meltwater channels (also shown by symbols). Typical till is pale-yellow, % areas: Canadian Journal of Earth Sciences, v. 16, p. 913–938. tlx r lu % or completely oxidized. Clasts angular to well rounded. Clast composition %% lse % al C % % % tlx % grayish-yellow, yellowish-brown, olive-brown, grayish-brown, brown, % tlx(s) er ek % lca LAKE CLAY AND SILT reflects composition of other surficial materials and bedrock in the drainage basin. Clayton, Lee, and Moran, S.R., 1982, Chronology of late Wisconsinan glaciation in middle % e % % cad e Cr % lss D Sage brownish-olive, olive, yellowish-gray, brownish-gray, olive-gray, bluish-gray, gray, North America: Quaternary Science Reviews, v. 1, p. 55–82. % % % S R % Fossiliferous (gastropod, pelecypod, and vertebrate remains; wood fragments and % % % W % tlx(e) % jea % lss or mottled, calcareous clay loam and loam; in some areas it is clay, silty clay, silty % % Colton, R.B., Lemke, R.W., and Lindvall, R.M., 1961, Glacial map of Montana east of the % % LAKE SILT AND SAND % % EET % plant detritus) in some places. Included in other map units in many areas. % % % ke % tlx M clay loam, silt loam, sandy clay, or sandy loam. Very gravelly in some places; Rocky Mountains: U.S. Geological Survey Miscellaneous Geologic Investigations % jea il % Includes some sheetwash alluvium, alluvial-fan deposits, alluvium beneath low % G k % R R lu where till directly overlies shale bedrock, the matrix commonly is >90 percent lca % i LAKE CLAY, SILT, SAND, AND GRAVEL Map I-327, scale 1:500,000. tlx(e) A pgd tlx(e) v terraces, outwash and ice-contact sand and gravel, lake deposits, and bedrock S lca e lu r % % lss %% % S tlx % shale fragments. In some places, till is interbedded with, intercalated with, or De Young, William, Youngs, F.O., and Glassey, T.W., 1932, Soil survey of the Milk River area, Sunburst lu HIL lu tlx(e) outcrops. Alluvium in some areas is dominantly redeposited outwash, ice-contact gg tlx( lse LAKE AND EOLIAN SAND AND SILT contains lenses, pods, and stringers of clay, silt, sand, or gravel. Generally Montana: U.S. Department of Agriculture, Bureau of Chemistry and Soils, Series 1928, % % % % gg deposits, and lake deposits. East and northeast of Big Sandy, alluvium overlies a % tlx % e) % % % % LS % % nonstratified; nonsorted or very poorly sorted. Local weak horizontal layering no. 22, 35 p. % % % % % % thick fill of older fluvial, glaciofluvial, and glaciolacustrine deposits and till (see % % 1 cad % % ls cly 000 ke s COLLUVIUM, SHEETWASH ALLUVIUM, LAKE DEPOSITS, AND where the ice margin fluctuated in a lake. Commonly massive; cohesive to friable. Dyke, A.S., 2004, An outline of North American deglaciation with emphasis on central and % crr crr % description of till deposits associated with “Buried bedrock valleys of the ancestral % tlx(e) % % R % % % % % In some areas, gritty or mealy; crude fissility. Generally loosely compact or northern Canada, in Ehlers, Juergen and Gibbard, P.L., eds., Quaternary % cad % GLACIOFLUVIAL-FILL DEPOSITS % IT pgd % Marias and Missouri Rivers” in the Explanation of map symbols). Thickness 1–6 % % % % % % crr % tlx % %% Gold k caa compact, but not hard. Sandy till is loose to firm; silty till is firm. Clayey till is glaciations—Extent and chronology, Part 2, North America: Amsterdam, Elsevier, p. % % ee COLLUVIUM, SHEETWASH ALLUVIUM, AND LANDSLIDE DEPOSITS m, locally >15 m % % tlx(e) pgd r % C East % % % % Butte ry al % soft, slightly sticky to sticky, and slightly plastic to plastic when moist; hard when 373–430. %% % % r Flood-plain alluvium—Chiefly poorly-sorted to well-sorted clay, silty clay, silty clay % e % % % % % 1 b Butte tlx 500 w lss R dry. Dry till in some places breaks into small angular flakes and plates that have Fox, P.P., 1946, Buried Pleistocene gorge of the Marias River, Montana [abs.]: Geological % % % % % jea % % cad a % r jea L tlx HOLOCENE, LATE PLEISTOCENE, AND MIDDLE PLEISTOCENE loam, clayey silt, and silt with scattered granules and pebbles; locally, loam, sandy % % caa t % % lca % S pgd it % sharp edges; blocky structure in some other places. Parting typically is irregular or Society of America Bulletin, v. 57, no. 12, p. 1194. % tl tlx(e) clay loam, sandy loam, or fine sand. Moderately to well stratified. Commonly has % % % % e % % % % % % % lu % cly Sa cly LOAMY COLLUVIUM prismatic. Clay minerals are dominantly montmorillonite. Widely spaced, Fullerton, D.S., Christiansen, E.A., Schreiner, B.T., Colton, R.B., and Clayton, Lee, 2007, % caa % afj ge gg either obscure bedding or pronounced horizontal bedding; weakly laminated in % % C % R % lca ree tlx weakly-developed joints are common; in some places, joint surfaces are coated by Quaternary geologic map of the Regina 4° × 6° quadrangle, United States and Canada: % pgd k Frank Jurenka’s % some places. Clay, silt, sand, or gravel lenses or small channel fills of sand and % % % % % pgd Reservoir % crr % tlx % FROST-RUBBLE AND TALUS-RUBBLE DEPOSITS powdery calcium carbonate or gypsum, or both. Joint or parting surfaces are U.S. Geological Survey Miscellaneous Investigations Series Map I–1420 (NM–13), 37 % % % % % % % gravel are common. Dense and compact in most places. Clayey alluvium is % lu % % lca % locally weakly stained by iron or manganese oxides. Selenite (gypsum) crystals p., map scale 1:1,000,000. % % % % moderately plastic, soft, and sticky where moist and hard where dry. Textures may %% % % % % % % % al % % % % 1–3 mm long are present on joint surfaces in some places. Fragments of lignite Fullerton, D.S., and Colton, R.B., 1986, Stratigraphy and correlation of the glacial deposits on % % % caa % HOLOCENE AND PLEISTOCENE vary abruptly, laterally and vertically. Local thin buried soils (humic horizons). % % lu R % % (bedrock) are ubiquitous in till. Nearly pebble free to very pebbly; cobbles and the Montana Plains, in Richmond, G.M., and Fullerton, D.S., eds., Quaternary % % % R jea Concentrations of detrital lignite (bedrock) fragments as large as 1 cm are common % % % gg al al SLUMP-BLOCK LANDSLIDE DEPOSITS AND ROCKSLIDE DEPOSITS % % % % boulders are rare to abundant. Largest erratic boulders are >2 m in diameter. glaciations in the United States of America: Quaternary Science Reviews, v. 5, p. % lu % kg % % in crossbedded sand. Where flood-plain alluvium directly overlies lake clay, silt, % %% lu % %% % % lu % % lu and sand or sheetwash alluvium, in some places it is difficult to distinguish the Clasts of older till and clasts of lignite (bedrock) as large as 2 m in diameter locally 69–82. % lu % L % % cad i lss % % lca ttl LATE WISCONSIN are included in the till. Glaciotectonic blocks or rafts of shale or sandstone tens of Fullerton, D.S., Colton, R.B., and Bush, C.A., 2004, Limits of mountain and continental % % e % % % % S %% ag lse deposits % % % gg % k e % % % % % % C tlx % % lu ee reek meters in length locally are included in the till. Pebbles in typical till are chiefly glaciations east of the Continental Divide in northern Montana and north-western North % % % % r lss LOAMY TILL Channel alluvium—Chiefly loose, stratified, poorly-sorted to well-sorted, pebbly, fine % % % C tlx % % % % % % % Kevin %% % ep lu tlx subangular to rounded erratic limestone and dolomite and erratic igneous and Dakota, U.S.A., in Ehlers, Juergen, and Gibbard, P.L., eds., Quaternary % % e tlx to medium sand and (or) coarse sand and gravel; locally very poorly sorted sandy % Sh lss Ground-moraine deposits % % % % tlx(e) % lu metamorphic rocks from the Canadian Shield; where till is derived primarily from glaciations—Extent and chronology; Part 2, North America: Amsterdam, Elsevier, p. % % % % lu shale gravel. Cobbles and boulders are common to abundant in some areas. % % % % k tlx(e) local bedrock, pebbles are chiefly angular to subrounded shale, siltstone, and soft 131–150.
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