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Geologic units in Beaverhead county, Montana

[Additional scientific data in this geographic area]

Quartzite and biotite schist in fault contact; Middle Proterozoic metasedimentary rocks; southern Belt province (Middle Proterozoic) at surface, covers < 0.1 % of this area
Intermediate Precambrian age metasediments; dominantly quartzite with minor micaceous layers and mica schists of northern Idaho
Lithology: quartzite; mica schist; meta-argillite; calc-silicate rock; gabbro; skarn
Limestone, dolostone, shale, and arenite; Ordovician and Cambrian shallow marine inner continental-shelf deposits; southeastern Idaho (Ordovician and Cambrian) at surface, covers < 0.1 % of this area
Ordovician, commonly Lower, and Cambrian marine sediments of eastern and southern Idaho.
Lithology: limestone; dolostone (dolomite); shale; arenite
Mississippian, undifferentiated (Phanerozoic | Paleozoic | Carboniferous Mississippian) at surface, covers 5 % of this area
Mississippian, undifferentiated: sandstone, shale, and limestone, in part dolomitic, with chert nodules, some quartzite; includes Big Snowy group in central part of State, Madison group in central and southwestern parts; and Hannan and Brazer limestones in the northwestern part; may include small amounts of Pennsylvanian rocks in areas where stratigraphic studies are incomplete.
Lithology: carbonate; fine-grained mixed clastic; medium-grained mixed clastic; chert
Chert, shale, phosphorite, and carbonates; Permian restricted marine epicontinental-basin deposits; southeastern Idaho (Permian) at surface, covers < 0.1 % of this area
Permian phosphatic sandstone, mudstone and chert of east-central Idaho.
Lithology: chert; shale; phosphorite; dolostone (dolomite); arenite; limestone
Pre-Belt gneiss, schist, and related rocks (Archean Proterozoic(?) preCambrian-Proterozoic(?) preCambrian(?) Phanerozoic | Paleozoic(?) Mesozoic(?) Cenozoic | Cambrian(?) Ordovician(?) Silurian(?) Devonian(?) Carboniferous(?) Permian(?) Triassic(?) Jurassic(?) Cretaceous(?) Tertiary) at surface, covers 3 % of this area
Pre-Belt gneiss, schist, and related rocks: comprises all the rocks older than the Belt series except the Stillwater complex. These include the Cherry Creek group, consisting of interlaminated gneiss, schist, marble, and quartzite; and the Pony series of Tansley and others, consisting of gneiss and schist of both sedimentary and igneous origin. Recent work has resulted in the distinction of small masses of granitic and injected rocks now regarded as resulting from intrusion in Cretaceous or Tertiary time. Other such masses may have escaped recognition.
Lithology: metamorphic rock; plutonic rock (phaneritic)
Limestone, shale, siltstone, chert, and conglomerate; Mississippian western turbiditic flysch to eastern shallow-water carbonates; east-central Idaho (Mississippian) at surface, covers < 0.1 % of this area
Mississippian shallow-water carbonate-to-clastic sequence of east-central Idaho.
Lithology: limestone; shale; siltstone; sandstone; chert; conglomerate
Mica schist, marble, quartzite, and amphibolite; Early Middle to Early Proterozoic metasedimentary rocks; southern Belt province (Early Middle Proterozoic to Early Proterozoic) at surface, covers < 0.1 % of this area
Older Precambrian high-grade metamorphic complex of eastern Idaho.
Lithology: mica schist; marble; quartzite; amphibolite
Sandstone, siltstone, dolostone, and chert; Pennsylvanian to Mississippian shallow marine inner continental-shelf deposits; eastern east-central Idaho (Pennsylvanian and Mississippian ) at surface, covers < 0.1 % of this area
Pennsylvanian and Mississippian shallow-water carbonates of eastern Idaho.
Lithology: arenite; siltstone; dolostone (dolomite); chert
Ravalli group (Proterozoic | Mesoproterozoic) at surface, covers 3 % of this area
Ravalli group: a diverse assemblage with numerous subdivisions, only a few of which have been recognized over large enough areas to be distinguished here. Near Idaho the rocks are light colored and siliceous, ranging from pure white quartzite to siliceous shale, mostly in subdued tones of gray, green, purple, and red. Near Missoula the rocks are dark-gray quartzite and quartzitic argillite. In and near Glacier National Park the Grinnell, Appekunny, and Altyn formations are distinguished.
Lithology: meta-argillite; quartzite
Trachyandesite, latite, trachybasalt flows, dikes, and volcaniclastic debris; Eocene intermediate volcanics; central Idaho, southern Challis volcanic field (Eocene) at surface, covers < 0.1 % of this area
Eocene mixed silicic and basaltic volcanic ejecta, flows and reworked debris.
Lithology: trachyandesite; latite; trachybasalt; dacite; trachyte; lava flow; volcanic breccia (agglomerate)
Gravel, sand, and silt; Quaternary; alluvium (Quaternary) at surface, covers < 0.1 % of this area
Quaternary alluvium; may contain some glacial deposits and colluvium in uplands
Lithology: alluvium; alluvial terrace; floodplain; alluvial fan; colluvium
Pennsylvanian, undifferentiated (Phanerozoic | Paleozoic | Carboniferous Pennsylvanian) at surface, covers 3 % of this area
Pennsylvanian, undifferentiated: in western Montana is mainly the Quadrant quartzite but includes limestone and other rocks of Pennsylvanian age so far as present data permit. Farther east other formations of Pennsylvanian or possible Pennsylvanian age are included.
Lithology: sandstone; mudstone; carbonate; conglomerate; chert
Limestone, dolostone, sandstone, siltstone, and chert; Lower Permian to Lower Pennsylvanian marine continental-shelf deposits; east-central Idaho (Early Permian to Early Pennsylvanian) at surface, covers < 0.1 % of this area
Lower Permian to Lower Pennsylvanian (Carboniferous) shallow-water detritus.
Lithology: limestone; dolostone (dolomite); arenite; siltstone; chert
Jurassic, undifferentiated (Phanerozoic | Mesozoic | Jurassic) at surface, covers 0.1 % of this area
Jurassic, undifferentiated: calcareous shale and sandstone; includes the Morrison formation, the Ellis group, Sundance formation, and other rocks of Jurassic age.
Lithology: fine-grained mixed clastic; limestone; evaporite
Granodiorite, quartz monzonite, granite, alaskite, quartz monzodioirte, diorite; Tertiary to Cretaceous, intrusions, undivided; northern, west-central, and southwestern Idaho (Eocene to Cretaceous) at surface, covers < 0.1 % of this area
Eocene intrusions; Cretaceous plutons, intermediate, Cretaceous plutons, felsic; metamorphosed granitic intrusive rock
Lithology: granodiorite; quartz monzonite; granite; quartz monzodiorite; diorite; alkali-granite (alaskite)
Kootenai formation and associated rocks (Phanerozoic | Mesozoic | Jurassic Cretaceous-Early) at surface, covers 1 % of this area
Kootenai formation and associated rocks: conglomerate, sandstone, shale, and mudstone; purplish and green beds are common; mainly the Kootenai; in southern Montana includes strata that have been mapped as Cloverly formation. Includes Second Cat Creek and Third Cat Creek sands of drillers in central part of State; Sunburst sand of drillers in north-central part; and Cut Bank sand of drillers in western part. As here mapped, may locally include thin units of Jurassic age.
Lithology: medium-grained mixed clastic; mudstone; limestone
Tertiary sedimentary rocks, undifferentiated (Phanerozoic | Cenozoic | Tertiary) at surface, covers 27 % of this area
Tertiary sedimentary rocks, undifferentiated: clastic deposits in western Montana, mostly in valleys, and in most places not divided into formations; mostly poorly consolidated gravel, sand, silt, and clay; includes some tuffaceous material and locally lenses of lignite and bentonite; a little hot spring tufa; and in areas not yet mapped in detail, lava may be included. These rocks were in part laid down in lakes but a large part was formed in streams and alluvial fans. These rocks are Tertiary in age and as now mapped may even include some beds of Cretaceous age. Some late Tertiary terrace deposits may be included.
Lithology: medium-grained mixed clastic; coarse-grained mixed clastic; lava flow; ash-flow tuff; tuff; coal; bentonite; carbonate
Glacial drift (Phanerozoic | Cenozoic | Quaternary) at surface, covers 2 % of this area
Glacial drift: morainal and outwash plain deposits of mountain glaciers; mainly ill-sorted and poorly rounded boulders, cobbles, pebbles, and sand; may include alluvium in places
Lithology: glacial drift; alluvium
Clastic debris; Quaternary colluvium, fanglomerate, talus, and glacial deposits; upland-valley margins (Quaternary) at surface, covers < 0.1 % of this area
Quaternary colluvium, fanglomerate, and talus plus some glacial debris in upland valleys.
Lithology: alluvium; glacial drift; colluvium
Quartzite, siltite, argillite, and mica schist; Middle Proterozoic Lemhi Group; southern Belt province (Middle Proterozoic) at surface, covers < 0.1 % of this area
Intermediate Precambrian sediments, feldspathic quartzite and siltstone of southern Idaho.
Lithology: quartzite; siltstone; meta-argillite; exhalite; mica schist; lamprophyre
Shale, limestone, and sandstone; Triassic marine to non-marine epicontinental deposits (subunits are TRl and TRu) (Triassic) at surface, covers < 0.1 % of this area
Triassic shallow-marine to non-marine sediments of eastern Idaho; subdivisions are (TRu and TRl).
Lithology: shale; limestone; sandstone; chert; conglomerate
Gravel, sand, and clay; Quaternary-Tertiary colluvium and fanglomerate; western Idaho (Pleistocene and Pliocene) at surface, covers < 0.1 % of this area
Pleistocene and Pliocene fanglomerate, colluvium, and poorly sorted gravel deposits.
Lithology: alluvial fan; colluvium; residuum; gravel; clay or mud; sand; silt
Triassic, undifferentiated (Phanerozoic | Mesozoic | Triassic) at surface, covers 1 % of this area
Triassic, undifferentiated: conglomerate, sandstone, shale, and impure limestone belonging to the Dinwoody and Thaynes formations and other units of Triassic age, and the Chugwater of Triassic and Permian age.
Lithology: fine-grained mixed clastic; limestone; medium-grained mixed clastic
Alluvium (Phanerozoic | Cenozoic | Quaternary) at surface, covers 19 % of this area
Alluvium: mainly valley fill consisting of silt, sand, and gravel; includes some terrace deposits and glacial drift of Pleistocene age in some areas; locally includes hot spring tufa. The older part of the alluvium, where present, is probably of Pliocene age.
Lithology: alluvium; glacial drift; carbonate
Terrace deposits (Phanerozoic | Cenozoic | Tertiary Quaternary) at surface, covers 2 % of this area
Terrace deposits: gravel, sand, and silt of terrace remnants.
Lithology: alluvial terrace
Tertiary coarse-grained intrusive rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers < 0.1 % of this area
Tertiary coarse-grained rocks: Some of these rocks have the composition of quartz diorite, monzonite, and similar rocks but most are alkalic syenite, leucite-rich rocks, and other alkalic varieties. Some of the rocks that are associated areally with the Cretaceous volcanic rocks may be Cretaceous in age. Includes the larger intrusive masses in the eastern part of western Montana and the western part of eastern Montana, most of which have domed upper surfaces. Many of these masses have been regarded as laccoliths, but generally without adequate proof. The Boulder batholith and related stocks are mapped separately.
Lithology: alkalic intrusive rock
Boulder batholith and broadly related stocks (Phanerozoic | Cenozoic | Tertiary Cretaceous) at surface, covers 6 % of this area
Boulder batholith and broadly related stocks: mainly quartz monzonite, but includes diorite, aplite, and other rocks. The distinctions between masses relative to the Boulder batholith and those mapped as of other ages are locally arbitrary and tentative.
Lithology: quartz monzonite; diorite; aplite
Ordovician, undifferentiated (Phanerozoic | Paleozoic | Ordovician) at surface, covers < 0.1 % of this area
Ordovician, undifferentiated: Mainly Bighorn dolomite; near Idaho, Kinnikinic quartzite.
Lithology: dolostone (dolomite); arenite; medium-grained mixed clastic; limestone; chert
Rhyolite ot trachyte ignimbrites and flows; Pliocene felsic volcanics; eastern Snake River Plain and vicinity (Pliocene) at surface, covers < 0.1 % of this area
Pliocene silicic welded tuff, ash, and flow rock; most common in southwestern Idaho.
Lithology: rhyolite; trachyte; ignimbrite; lava flow; tuff; volcanic breccia (agglomerate)
Colorado shale (Phanerozoic | Mesozoic | Cretaceous-Early Cretaceous-Middle(?) Cretaceous-Late) at surface, covers 2 % of this area
Colorado shale: dark-gray shale and siltstone with many concretions and sandy units. Includes equivalents of Fall River, Skull Creek, Newcastle, Mowry, Belle Fourche, Greenhorn, Carlile, and Niobrara formations, and locally Telegraph Creek formation. In the less well-known areas beds of other ages may have been included.
Lithology: fine-grained mixed clastic
Open Water (Holocene) at surface, covers < 0.1 % of this area
Lakes and streams
Lithology: water
Devonian, undifferentiated (Phanerozoic | Paleozoic | Devonian) at surface, covers 0.6 % of this area
Devonian, undifferentiated: comprises Three Forks formation consisting of carbonaceous and calcareous shale with some sandstone and limestone, Jefferson limestone, and unnamed units of Devonian age.
Lithology: carbonate; fine-grained mixed clastic; conglomerate; sedimentary breccia; evaporite
Glacial debris; Late Pleistocene glacial till, outwash, and alluvium of continental glaciers; northern Idaho (Late Pleistocene ) at surface, covers < 0.1 % of this area
Pleistocene till, moraines and similar unsorted glacial debris.
Lithology: till; outwash; alluvium
Idaho batholith and associated masses (Phanerozoic | Mesozoic Cenozoic | Cretaceous-Late Tertiary) at surface, covers 3 % of this area
Idaho batholith and associated masses: faintly gneissic quartz monzonite, granodiorite, and similar rocks. The extreme eastern part of the Idaho batholith extends into Ravalli County, Mont. This and nearby masses of similar rocks are shown as associated with the Idaho batholith and designated Ki. Future studies may show that some granitoid masses further east are also allied to the Idaho batholith or that a few of the masses now grouped with that batholith are younger. Precise dating is impossible at present.
Lithology: granitoid
Montana group, undifferentiated (Phanerozoic | Mesozoic | Cretaceous-Late) at surface, covers 2 % of this area
Montana group, undifferentiated: mainly sandstone and shale, soft and in part poorly consolidated; some coal; shown undivided only in areas where detailed data are lacking and in these areas some rocks not of Montana age may have been included. In particular, rocks designated Km in southwestern Montana may include some Tertiary strata.
Lithology: fine-grained mixed clastic; coal
Quartzite, meta-conglomerate, dolostone, argillite; Middle Proterozoic Swauger quartzite; southern Belt province (Middle Proterozoic) at surface, covers < 0.1 % of this area
Intermediate Precambrian sediments, red-tinted quartzite with minor conglomeratic and dolomitic lenses of southern Idaho
Lithology: quartzite; meta-conglomerate; dolostone (dolomite); meta-argillite
Conglomerate, sandstone, and siltstone; Eocene to Late Cretaceous alluvial-fan deposits; east-central Idaho, Cordilleran fold-thrust belt, piggyback basins (Eocene to Late Cretaceous ) at surface, covers < 0.1 % of this area
Lower Tertiary to Upper Mesozoic breccia, conglomerate and sandstone; syntectonic in part.
Lithology: conglomerate; arkose; siltstone; limestone
Siltstone, shale, sandstone, and limestone; Jurassic Cordilleran retroarc-foreland-basin deposits (subunits are Jl and Ju); southeastern Idaho (Jurassic) at surface, covers < 0.1 % of this area
Jurassic shallow-marine to non-marine sediments of eastern Idaho; subdivisions are (Jl and Ju).
Lithology: siltstone; shale; sandstone; limestone
Syenite, granite, quartz syenite, and gabbro; Ordovician to Cambrian plutons; east-central Idaho (Ordovician to Cambrian) at surface, covers < 0.1 % of this area
Intrusive rock of eastern Idaho; appears older than Cretaceous; possibly Precambrian
Lithology: syenite; granite; quartz syenite; gabbro
Permian, undifferentiated (Phanerozoic | Paleozoic | Permian) at surface, covers 0.7 % of this area
Permian, undifferentiated: chert, sandstone, limestone, quartzite, and shale with rock phosphate mostly at base; mainly Phosphoria formation
Lithology: fine-grained mixed clastic; carbonate; chert; phosphorite; black shale; oil shale
Tuffaceous shale, sandstone, conglomerate, and lignite; Eocene to Pliocene alluvial and lacustrine deposits; central and southern Idaho (Tertiary) at surface, covers < 0.1 % of this area
Tertiary continental sediments; predominantly Upper Tertiary in age; subdivisions are:(Tpd, Tmd, and Ted).
Lithology: shale; sandstone; conglomerate; tuff; siltstone; lignite; bentonite; claystone; limestone
Limestone, dolostone, arenite, shale, and siltstone; Lower Paleozoic marine continental-shelf deposits; southeastern Idaho; (Early Paleozoic) at surface, covers < 0.1 % of this area
Lower Paleozoic marine carbonate and clastic units southeast of the Snake Plain.
Lithology: limestone; dolostone (dolomite); arenite; shale; siltstone
Missoula group (Proterozoic | Mesoproterozoic) at surface, covers 0.6 % of this area
Missoula group: chiefly red, maroon, or purple argillite; sandy or quartzitic argillite, and generally impure quartzite and limestone. The larger limestone masses are similar to the Siyeh limestone of the Piegan group. The Missoula group includes numerous named formations, most of which cannot be traced with confidence far from their type localities. Among these are the Marsh shale in the Helena region, the Striped Peak and Libby formations in northwestern Montana, five near Missoula, and others in and south of Glacier National Park.
Lithology: quartzite; meta-argillite; carbonate; meta-conglomerate
Tertiary volcanic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 6 % of this area
Tertiary volcanic rocks: Flows and associated pyroclastic deposits, with subordinate amounts of intercalated sedimentary beds and lignite. The volcanic material is mostly latite, quartz latite, and andesite but includes some rhyolite and basalt. The distinction between Tertiary and pre-Tertiary volcanic rocks was not made in some of the reports used in the complilation. Hence in the less well-known areas some pre-Tertiary volcanic rocks may be included.
Lithology: volcanic rock (aphanitic); mixed clastic/volcanic; coal
Dolostone, limestone, sandstone, shale, and conglomerate; Devonian marine continental-shelf deposits; east-central and southeastern Idaho (Devonian) at surface, covers < 0.1 % of this area
Devonian bedded dolomite and limestone interval of eastern and southern Idaho.
Lithology: dolostone (dolomite); limestone; sandstone; shale; conglomerate
Cambrian, undifferentiated (Phanerozoic | Paleozoic | Cambrian) at surface, covers 0.9 % of this area
Cambrian, undifferentiated: comprises Deadwood formation, in south-central Montana, and Red Lion formation, Dry Creek shale, Hasmark formation, Pilgrim limestone, Silver Hill formation, Park shale, Meagher limestone, Wolsey shale, Flathead quartzite, and other units. In a few places quartzite of Cambrian age may be mapped with the Belt series or quartzite of Belt age with the Cambrian rocks.
Lithology: carbonate; mudstone; sandstone; conglomerate
Sandstone, siltstone, shale, limestone, and coal ; Early Cretaceous Cordilleran retroarc-foreland-basin deposits; southeastern Idaho (Early Cretaceous) at surface, covers < 0.1 % of this area
Lower Cretaceous shale, siltstone, red-bed sandstone and fresh-water limestone.
Lithology: sandstone; siltstone; shale; limestone; coal
Pre-Belt gneiss, schist, and related rocks (Archean Proterozoic(?) preCambrian-Proterozoic(?) preCambrian(?) Phanerozoic | Paleozoic(?) Mesozoic(?) Cenozoic | Cambrian(?) Ordovician(?) Silurian(?) Devonian(?) Carboniferous(?) Permian(?) Triassic(?) Jurassic(?) Cretaceous(?) Tertiary) at surface, covers 0.2 % of this area
Pre-Belt gneiss, schist, and related rocks: comprises all the rocks older than the Belt series except the Stillwater complex. These include the Cherry Creek group, consisting of interlaminated gneiss, schist, marble, and quartzite; and the Pony series of Tansley and others, consisting of gneiss and schist of both sedimentary and igneous origin. Recent work has resulted in the distinction of small masses of granitic and injected rocks now regarded as resulting from intrusion in Cretaceous or Tertiary time. Other such masses may have escaped recognition.
Lithology: metamorphic rock; plutonic rock (phaneritic)
Piegan group (Proterozoic | Mesoproterozoic) at surface, covers 3 % of this area
Piegan group: most of the Piegan group is subdivided into formations that are in part equivalent to each other. Where correlations are relatively doubtful the group designation is retained. Carbonate-bearing rocks predominate in the group, but the proportions and character of the impurities in these rocks and the relations to non-carbonate-bearing rocks vary from place to place.
Lithology: carbonate; meta-argillite; quartzite
Dolostone, quartzite, shale, and limestone; Upper to Middle Ordovician marine continental-shelf deposits; east central Idaho (Late and Middle Ordovician) at surface, covers < 0.1 % of this area
Upper and Middle Ordovician dolomite and quartzite unconformably overlying (Ol).
Lithology: dolostone (dolomite); arenite; shale; limestone
Missoula group (Proterozoic | Mesoproterozoic) at surface, covers 9 % of this area
Missoula group: chiefly red, maroon, or purple argillite; sandy or quartzitic argillite, and generally impure quartzite and limestone. The larger limestone masses are similar to the Siyeh limestone of the Piegan group. The Missoula group includes numerous named formations, most of which cannot be traced with confidence far from their type localities. Among these are the Marsh shale in the Helena region, the Striped Peak and Libby formations in northwestern Montana, five near Missoula, and others in and south of Glacier National Park.
Lithology: quartzite; meta-argillite; carbonate; meta-conglomerate

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