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Geologic units in Grant county, New Mexico

Permain and Pennsylvanian rocks, undivided (Phanerozoic | Paleozoic | Carboniferous Pennsylvanian Permian) at surface, covers 0.8 % of this area
Permian and Pennsylvanian rocks, undivided; includes Horquilla Limestone, Earp Formation, Epitaph and Scherrer Formations, and Concha Limestone
Lithology: medium-grained mixed clastic; carbonate
undivided, Upper Cretaceous (Phanerozoic | Mesozoic | Cretaceous) at surface, covers 0.3 % of this area
Upper Cretaceous, undivided. Includes Virden Formation in northern Hidalgo County, Ringbone Formation in Hidalgo and Luna and Grant Counties, and locally Beartooth and Sarten, Mancos in Silver City area; Cenomanian - Maastrichtian for most part, although Beartooth is pre-Cenomanian
Lithology: medium-grained mixed clastic; volcanic rock (aphanitic); limestone
Gila Group (Phanerozoic | Cenozoic | Tertiary Quaternary) at surface, covers 31 % of this area
Gila Group. Includes Mimbres Formation and several informal units in southwestern basins; Middle Pleistocene to uppermost Oligocene
Lithology: conglomerate; sandstone; basalt
Mancos Formation and Beartooth Quartzite (Phanerozoic | Mesozoic | Cretaceous) at surface, covers 1 % of this area
Mancos Formation and Beartooth Quartzite (and Sarten Sandstone); Mancos includes what was formerly referred to as Colorado Shale which in turn may include equivalents of Tres Hermanos Formation
Lithology: shale; sandstone; medium-grained mixed clastic
older piedmont alluvial deposits and shallow basin fill (Phanerozoic | Cenozoic | Tertiary Quaternary) at surface, covers 0.3 % of this area
Older piedmont alluvial deposits and shallow basin fill; includes Quemado Formation and in northeast, high level pediment gravels
Lithology: alluvium; unconsolidated deposit
sedimentary and vocaniclastic sedimentary rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers < 0.1 % of this area
Mostly Oligocene and upper Eocene sedimentary and volcaniclastic sedimentary rocks with local andesitic to intermediate volcanics; includes Espinaso, Spears, Bell Top, and Palm Park Formations
Lithology: clastic; mixed clastic/volcanic; volcanic rock (aphanitic); unconsolidated deposit
Paleozoic rocks, undivided (Phanerozoic | Paleozoic) at surface, covers 0.2 % of this area
Paleozoic rocks, undivided
Lithology: sedimentary rock
Silurian through Cambrian rocks, undivided (Phanerozoic | Paleozoic | Cambrian Ordovician(?) Silurian) at surface, covers 0.6 % of this area
Silurian through Cambrian rocks, undivided
Lithology: sedimentary rock
silicic flows and massess and associated pyroclastic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 4 % of this area
Upper Oligocene silicic (or felsic) flows and masses and associated pyroclastic rocks; includes Taylor Creek, Fanney, and Rocky Canyon Rhyolites
Lithology: felsic volcanic rock; pyroclastic; rhyolite
volcanic rocks, lower Oligocene and Eocene (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.3 % of this area
Lower Oligocene and Eocene volcanic rocks, undifferentiated; dominantly intermediate composition, with interbedded volcaniclastic rocks; (31-44 Ma)
Lithology: volcanic rock (aphanitic); intermediate volcanic rock; mixed clastic/volcanic
intrusive rocks, Paleogene and Upper Cretatceous (Phanerozoic | Mesozoic Cenozoic | Cretaceous Tertiary) at surface, covers 0.9 % of this area
Paleogene and Upper Cretaceous intrusive rocks; includes Hanover, Fierro, Tyrone, and Lordsburg granodiorite-quartz monzonite porphyries
Lithology: granodiorite; granitoid
piedmont alluvial deposits (Phanerozoic | Cenozoic | Quaternary) at surface, covers 13 % of this area
Piedmont alluvial deposits: upper and middle Quaternary; includes deposits of higher gradient tributaries bordering major stream valleys, alluvial veneers of the piedmont slope, and alluvial fans
Lithology: alluvium
silicic to intermediate intrusive rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers < 0.1 % of this area
Miocene to Oligocene silicic to intermediate intrusive rocks; dikes, stocks, plugs, and diatremes
Lithology: plutonic rock (phaneritic)
mafic intrusive rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.1 % of this area
Upper and Middle Tertiary mafic intrusive rocks
Lithology: plutonic rock (phaneritic)
intrusive rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.5 % of this area
Tertiary intrusive rocks; undifferentiated
Lithology: plutonic rock (phaneritic)
silicic to intermediate volcanic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 1 % of this area
Silicic to intermediate volcanic rocks; mainly quartz latite and rhyolite Neogene; may locally include flows interbedded with Santa Fe Group
Lithology: felsic volcanic rock; intermediate volcanic rock
basaltic andesites (Phanerozoic | Cenozoic | Tertiary) at surface, covers 9 % of this area
Lower Miocene and uppermost Oligocene basaltic andesites (22-26 Ma). Includes Bearwallow Mountain Andesite and basaltic andesite of Mangas Mountain
Lithology: andesite; basalt; intermediate volcanic rock; mafic volcanic rock
andesitic volcanics (Phanerozoic | Mesozoic Cenozoic | Cretaceous Tertiary) at surface, covers 1 % of this area
Andesitic volcanics
Lithology: andesite; intermediate volcanic rock
plutonic rocks, middle Proterozoic (Proterozoic | Mesoproterozoic) at surface, covers 5 % of this area
Middle Proterozoic plutonic rocks (younger than 1600 Ma)
Lithology: plutonic rock (phaneritic)
alluvium (Phanerozoic | Cenozoic | Quaternary) at surface, covers 3 % of this area
Alluvium; upper and middle Quaternary
Lithology: alluvium
andesites and basaltic andesites (Phanerozoic | Cenozoic | Tertiary) at surface, covers 7 % of this area
Upper Oligocene andesites and basaltic andesites (26-29 Ma); includes La Jara Peak Basaltic Andesite, Uvas Basalt, the basaltic andesite of Poverty Creek, and Squirrel Springs Andesite, the Razorback, Bear Springs Canyon, Salt Creek, Gila Flat, and Middle Mountain Formations, and the Alum Mountain Group; locally includes more silicic flows
Lithology: andesite; basalt; intermediate volcanic rock; mafic volcanic rock; felsic volcanic rock; rhyolite
quartz monzonites, intermediate intrusives, and other intermediate felsic dikes and plugs (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.5 % of this area
Quartz monzonites (Eocene) in the Silver City and Los Pinos Range, intermediate intrusives of the Cooke's Range (Oligocene), and other intermediate to felsic dikes and plugs of Oligocene and Eocene age
Lithology: quartz monzonite; granitoid
basalt and andesite flows, Neogene (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.3 % of this area
Basalt and andesite flows; Neogene. Includes flows interbedded with Santa Fe and Gila Groups
Lithology: basalt; andesite
metamorphic rocks (Proterozoic | Paleoproterozoic) at surface, covers 1.0 % of this area
Lower Proterozoic metamorphic rocks, dominantly felsic volcanic, volcaniclastic and plutonic rocks (1650-1700+ Ma); includes Vadito Group; locally includes high-grade felsic gneisses of unknown age
Lithology: felsic metavolcanic rock; plutonic rock (phaneritic); felsic gneiss
andesite and basaltic andesite flows and associated volcaniclastic units (Phanerozoic | Cenozoic | Tertiary) at surface, covers 2 % of this area
Lower Tertiary, (Lower Oligocene and Eocene) andesite and basaltic andesite flows, and associated volcaniclastic units. Includes Rubio Peak Formation, and andesite of Dry Leggett Canyon
Lithology: andesite; basalt; intermediate volcanic rock; mafic volcanic rock; mixed clastic/volcanic
Pennsylvanian rocks, undivided (Phanerozoic | Paleozoic | Carboniferous Pennsylvanian) at surface, covers < 0.1 % of this area
Pennsylvanian rocks, undivided; in Sangre de Cristo Mountains may include Sandia Formation, Madera Limestone, La Pasada, Alamitos, and Flechado Formations; elsewhere may include Bar-B, Nakaye, Red House, Oswaldo, and Syrena Formations
Lithology: sedimentary rock; medium-grained mixed clastic; carbonate
silicic flows, domes, and associated pyroclastic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 2 % of this area
Lower Oligocene silicic (or felsic) flows, domes, and associated pyroclastic rocks and intrusions; includes Mimbres Peak Formation
Lithology: lava flow; tuff; felsic volcanic rock; conglomerate; pyroclastic
Lower Cretaceous, unidivided (Phanerozoic | Mesozoic | Cretaceous) at surface, covers 0.3 % of this area
Lower Cretaceous, undivided; in northern Lea and Roosevelt Counties includes equivalents of Tucumcari Shale. In Cornudas Mountains includes Campogrande, Cox and other Washita Group formations, and the Boquillas Formation; Cenomanian. In the southwest includes Hell-To-Finish, U-Bar, and Mojado Formations which are equivalent to Bisbee Group of Arizona
Lithology: clastic; mixed clastic/carbonate
volcanic and some volcaniclastic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 0.2 % of this area
Volcanic and some volcaniclastic rocks, undifferentiated; lower Miocene and Upper Oligocene (younger than 29 Ma)
Lithology: volcanic rock (aphanitic); mixed clastic/volcanic
Abo Formation (Phanerozoic | Paleozoic | Permian) at surface, covers < 0.1 % of this area
Abo Formation; red beds, arkosic at base, finer and more mature above; Wolfcampian; may include limestone beds of Pennsylvanian age (Virgilian) in Zuni Mountains. In Robledo Mountains the Abo may be considered a member of the Hueco Formation
Lithology: sandstone; shale; conglomerate; limestone
silicic pyroclastic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 10 % of this area
Lower Oligocene silicic pyroclastic rocks (ash-flow tuffs); includes Hell's Mesa, Kneeling Nun, lower part of Bell Top Formation, Caballo Blanco, Datil Well, Leyba Well, Rock House Canyon, Blue Canyon, Sugarlump and Tadpole Ridge Tuffs, the tuffs of the Organ cauldron, Treasure Mountain Tuff (now known as Chiquito Peak Tuff), Bluff Creek Tuff, Oak Creek Tuff, tuff of Steins Mountain, tuff of Black Bill Canyon, tuff of Farr Ranch, Woodhaul Canyon, Gillespie and Box Canyon Tuffs, Cooney Tuff, and other volcanic and interbedded fluvial and pumiceous units; (31-36.5 Ma)
Lithology: pyroclastic; tuff; felsic volcanic rock; volcanic rock (aphanitic); mixed clastic/volcanic
older alluvial deposits of upland plains and piedmont areas (Phanerozoic | Cenozoic | Quaternary) at surface, covers < 0.1 % of this area
Older alluvial deposits of upland plains and piedmont areas, and calcic soils and eolian cover sediments of High Plains region; includes scattered lacustrine, playa, and alluvial deposits of the Tahoka, Double Tanks, Tule, Blanco, Blackwater Draw, and Gatuna Formations, the latter of which may be Pliocene at base; outcrops, however, are basically of Quaternary deposits; upper Quaternary to uppermost Pliocene(?)
Lithology: alluvium
Mississippian and Devonain rocks, undivided (Phanerozoic | Paleozoic | Devonian Carboniferous Mississippian) at surface, covers 0.3 % of this area
Mississippian and Devonian rocks, undivided; includes the Lake Valley Limestone, Caballero, Las Cruces, Rancheria, and Helms Formations and Escabrosa Group; Mississippian; the Onate, Sly Gap, Contadero Formations, and Percha Shale of south-central New Mexico, and Canutillo Formation of Northern Franklin Mountains and Bishops Cap area; Devonian
Lithology: carbonate; medium-grained mixed clastic
rhyolitic pyroclastic rocks (Phanerozoic | Cenozoic | Tertiary) at surface, covers 2 % of this area
Upper Oligocene rhyolitic pyroclastic rocks (ash-flow tuffs); includes Davis Canyon Tuff, South Crosby Peak Formation, La Jencia, Vick's Peak, Lemitar, South Canyon, Bloodgood Canyon, Shelley Peak Tuffs, tuff of Horseshoe Canyon, Park Tuff, Rhyolite Canyon Tuff, Apache Springs Tuff, Diamond Creek, Jordan Canyon, Garcia Camp Tuffs, the Turkey Springs Tuff, the tuff of Little Mineral Creek, the Amalia Tuff, and others. Some contain volcaniclastic and reworked volcaniclastic rocks, and eolian sandstone; (24-29 Ma)
Lithology: tuff; pyroclastic; rhyolite; andesite; mixed clastic/volcanic; eolian

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