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Geology of New Mexico

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resulting from rainfall onto heavy snow accumulations in southwestern and south central New Mexico on December 18–19, 1978; flooding after heavy rainfall from the remnants of Hurricane Doly between July 26–28, 2008; and widespread flooding from an unusually wet monsoon season in the summer of 2006. The state is occasionally impacted by remnants of East Pacific
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In 1863, silver was found in Magdalena, west of Socorro, followed by a large find in Grant County. Silver City, White Oaks, Ute Creek, Cerrillos, Elizabethtown, Twining, Chloride, Hondo Canyon, Red River Canyon and Socorro were soon discovered to also have silver. Rising costs and depleted ore bodies
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Holland, Mark E.; Grambling, Tyler A.; Karlstrom, Karl E.; Jones, James V.; Nagotko, Kimberly N.; Daniel, Christopher G. (September 2020). "Geochronologic and Hf-isotope framework of Proterozoic rocks from central New Mexico, USA: Formation of the Mazatzal crustal province in an extended continental
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south of Santa Fe. New deposits, along with the reopened Spanish mine in Silver City prompted a boom in copper mining in the late 19th century. Placer gold mining expanded into the Sangre de Cristo Mountains and along the Rio Grande, while lead mining got underway in Las Cruces. Coal was discovered
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Mining is still a cornerstone of the New Mexico economy, although it has largely shifted to open-pit extraction. Coal is mined in the northwest and copper, silver, gold, manganese, zinc and lead are extracted near Silver City. Molybdenum is an important resource in the Sangre de Cristo mountains,
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Flooding is one of the more common geologic hazards in New Mexico. Historically significant flooding events included extensive river flooding accompanied by local flash floods in September 1941; river flooding across the northeastern High Plains region between June 14–17, 1965; severe flooding
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in Utah. One estimate puts the probability of a large earthquake in the southern Rio Grande Rift in the next century at 5%. However, faults are concentrated along the Rio Grande Rift, with its urban centers, and while only 20 faults in the state are considered active, the consequences of an
917:. Uranium is still mined close to Grants, although production has dropped after a high point between the 1950s and the 1970s. Gypsum, limestone, potash and salt are mined out of Pennsylvanian and Permian rocks in the east. Mining accounted for 3,763 jobs by 2018. 1493:"Revised regional correlations and tectonic implications of Paleoproterozoic and Mesoproterozoic metasedimentary rocks in northern New Mexico, USA: New findings from detrital zircon studies of the Hondo Group, Vadito Group, and Marqueñas Formation" 347:. A second set of slightly younger island arcs accreted to the continented shortly after, around 1650 to 1600 Mya, during the Mazatzal orogeny. The Mazatzal beds now underlie most of southern New Mexico and the Mazatzal orogeny is recorded in the 1397:
Damiel, Christopher G.; Andronicos, Christopher L.; Aronoff, Ruth F. (2016). "Regional Al2SiO5 triple-point metamorphic rocks of northern New Mexico; A field trip to honor the career contributions od Lincoln Hollister to petrology and tectonics".
489:(about 1200 Mya). Thereafter the region experienced steady erosion, which in some cases brought rock near the surface that had been buried as deep as 10 kilometers (6.2 mi). This beveled much of New Mexico almost completely flat, forming a 1027:
earthquake could be serious. The large number of faults increases the likelihood of an earthquake even though rupture of any one fault is infrequent. The largest earthquakes in historic times were two magnitude 5.8 earthquakes in 1906 near
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Mack, Greg H. (2004). "Middle and late Cenozoic crustal extension, sedimentation, and volcanism in the southern Rio Grande rift, Basin and Range, and southern transition zone of southwestern New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
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Karlstrom, Karl E.; Amato, Jeffrey M.; Williams, Michael L.; Heizler, Matt; Shaw, Colin A.; Read, Adam S.; Bauer, Paul (2004). "Proterozoic tectonic evolution of the New Mexico region: A synthesis". In Mack, G.H.; Giles, K.A. (eds.).
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is an important geologic resource for farmers and municipal areas. In 2019, oil and gas production yielded $ 3.1 billion in oil and gas taxes and revenues for the state. Mining has historically also been important.
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to the continental margin, forming a band of new continental crust stretching from Arizona to Newfoundland and from the Wyoming-Colorado border to central New Mexico. These events are recorded in the rocks of the
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McMillan, Nancy J. (2004). "Magmatic record of Laramide subduction and the transition to Tertiary extension: Upper Cretaceous through Eocene igneous rocks of New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
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New Mexico is entirely landbound, with just 0.2% of the state covered with water, and most of the state has an arid to semiarid climate. Much of the state is mountainous, except for the easternmost
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were another interval of relative tectonic quiescence, where gradual subsidence deposited formations that preserve an impressive stratigraphic record across the state. This ended with the
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as well as block faulting and tilting in the more recent geologic past. For the most part, these rocks are exposed along the Rio Grande rift in the center of New Mexico, except in the
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across much of New Mexico, making this the most extensive Paleozoic formation exposed in the state. The subsequent retreat of the sea resulted in deposition of large deposits of
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Mack, Greg H. (2004). "The late Cambro-Ordovician Bliss and lower Ordovician El Paso Formations, southwestern New Mexico and west Texas". In Mack, G.H.; Giles, K.A. (eds.).
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of oil in 2019, yielding $ 3.1 billion in oil and gas taxes and revenues for the state. Mining has historically been important, but accounted for just 3,763 jobs by 2018.
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Heiken, G; Goff, F; Gardner, J N; Baldridge, W S; Hulen, J B; Nielson, D L; Vaniman, D (May 1990). "The Valles/Toledo Caldera Complex, Jemez Volcanic Field, New Mexico".
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Geological evolution of the Colorado Plateau of eastern Utah and western Colorado, including the San Juan River, Natural Bridges, Canyonlands, Arches, and the Book Cliffs
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Copnnel, Sean (2004). "Geology of the Albuquerque Basin and tectonic development of the Rio Grande rift in north-central New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
83:. This event transformed the New Mexico crust into mature continental crust. Over a thousand million years of tectonic quiescence followed, ending with the rise of the 2348:
Smith, Gary A. (2004). "Middle to late Cenozoic development of the Rio Grande rift and t adjacent regions in northern New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
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batholith. Following the Picuris orogeny, northern New Mexico was again tectonically quiet, while southern New Mexico experience some deformation associated with the
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Armstrong, Augustus K.; Mamet, Bernard L.; Repetski, John E. (2004). "Mississippian System of New Mexico and adjacent areas". In Mack, G.H.; Giles, K.A. (eds.).
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near gold and copper mines and potentially recoverable gold deposits grew more numerous as prospectors traced placer gold back to the veins where it originated.
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Lucas, Spencer G.; Harris, Susan K.; Spielmann, Justin A.; Berman, David S.; Henrici, Amy C.; Heckert, Andrew B.; Zeigler, Kate E.; Rinehart, Larry F. (2005).
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rocks crop out across approximately five percent of New Mexico and underlie the entire state. The rocks now exposed at the surface were uplifted during the
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The Laramide Orogeny changed the topography of New Mexico into one of high uplifts and deep basins. The basins began to fill with sediments during the
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Cather, Steven M. (2004). "Laramide Orogeny in Central and Northern New Mexico and Southern Colorado". In Mack, Greg H.; Giles, Katherine A. (eds.).
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Nummedal, Dag (2004). "Tectonikc and eustatic controls on upper Cretaceous stratigraphy of northern New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
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Barker, Fred; Friedman, Irving (1974). "PRECAMBRIAN METAVOLCANIC ROCKS OF THE TUSAS MOUNTAINS, NEW MEXICO: MAJOR ELEMENTS AND OXYGEN ISOTOPES".
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The increasing weight of the Sonoma mountains to the west drove subsidence of its foreland basin, which included most of New Mexico. During the
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Provinces in the southwestern part of the state. The presence of these four physiographic provinces gives the state great geological diversity.
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The rise of hot asthenosphere below New Mexico reversed the compression of the crust and put it into tension, resulting in the opening of the
1929: 4013: 3284: 3168: 2952: 2911: 1373:"Structural evolution and timing of deformation along the Proterozoic Spring Creek shear zone of the northern Tusas Mountains, New Mexico" 1695:
Carlson, Marvin P (May 1999). "Transcontinental Arch — a pattern formed by rejuvenation of local features across central North America".
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Kluth, C.; Schaftenaar, C. (1994). "Depth and geometry of the northern Rio Grande rift in the San Luis basin, south-central Colorado.".
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was deposited in the basin shelves, while areas receiving debris eroded off the highlands formed clastic sedimentary formations such as
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Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
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have led to widespread abandonment and ghost towns throughout the state, which remain comparatively well-preserved in the dry climate.
1170: 2246:"Stratigraphy, sediment dispersal and paleogeography of the Lower Eocene San Jose Formation, San Juan Basin, New Mexico and Colorado" 2183:
Seager, William (2004). "Laramide (late Cretaceous-Eocene) tectonics of southwestern New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
701:, when the climate become somewhat cooler and wetter, and a substantial river system developed through New Mexico that deposited the 2423: 2382: 2357: 2332: 2221: 2192: 2149: 1979: 1954: 1889: 1791: 1766: 1646: 1620: 1411: 1320: 1295: 1213:"Geology and mineral resources in the Hopewell and Bromide No. 2 districts, northern Tusas Mountains, Rio Arriba County, New Mexico" 1195: 663: 1526:"History and timing of polyphase Proterozoic deformation in the Manzano thrust belt, central New Mexico [master's thesis]" 3975: 3077: 3016: 840: 411:
facies. Geologists debate the extent of different terranes—sections of continental crust—that joined. Metavolcanic rocks in the
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McMillan, Nancy J.; McLemore, Virginia T. (2004). "Cambrian-Ordovician magmatism and extension in New Mexico and Colorado".
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Under Spanish rule turquoise and lead were mined near Cerillos and copper was found at Santa Rita in the southwest in 1798.
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Making the case for the Picuris orogeny: Evidence for a 1500 to 1400 Ma orogenic event in the southwestern United States
540:. Later in the Cambrian, the sea began to advance northeast across New Mexico, beginning in the boot heel of the state ( 2083:(Cope) from the Upper Triassic (Apachean) Whitaker quarry, New Mexico, with detailed analysis of a single quarry block" 697:. The Moenkopi represents deposition in a coastal plain by rivers running to the west. This pattern continued into the 3967: 3861: 3631: 3621: 3601: 3596: 3586: 3556: 3004: 1663: 1610: 1311:
Chapin, C.; Cather, S. (1994). "Tectonic setting of the axial basins of the northern and central Rio Grande rift.".
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Bryan, Kirk (1938). "Geology and ground-water conditions of the Rio Grande depression in Colorado and New Mexico".
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Lucas, Spencer G. (2004). "The Triassic and Jurassic systems in New Mexico". In Mack, G.H.; Giles, K.A. (eds.).
1238: 3941: 3846: 3806: 3626: 3566: 3516: 3496: 3437: 2994: 2904: 2826: 2648: 2245: 2044: 1844: 1372: 1212: 862: 207: 199: 58: 50: 1664:"Biostratigraphy and Carbonate Facies of the Mississippian Arroyo Penasco Formation, North-Central New Mexico" 2440: 2087:
New Mexico Museum of Natural History & Science, A Division of the Department of Cultural Affairs Bulletin
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that carry considerable moisture, and such storm remnants contributed to both the 1941 and the 2008 floods.
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began to develop around 15 Mya, and volcanic activity subsequently spread southwest and northeast along the
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were intruded in the early Cambrian along north–south faults, which may indicate incipient rifting of the
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deformed and metamorphosed much of the crust of New Mexico. This event is recorded in the rock of the
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on the east. It has been the focus of significant scientific research on continental rift processes.
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The Rio Grande Joint Investigation in the upper Rio Grande basin in Colorado, New Mexico, and Texas
2045:"Review of Upper Triassic stratigraphy and biostratigraphy in the Chama Basin, northern New Mexico" 1028: 960: 852: 808: 514: 482: 474: 388: 373: 335: 269: 391:. All of the rocks more than 1.65 billion years old show evidence of metamorphism ranging between 3951: 3926: 3831: 3771: 3746: 3716: 3706: 3357: 3352: 3337: 3327: 3256: 3201: 3181: 2290: 1739: 1576: 1261: 914: 825: 821: 755: 690: 580: 400: 2078: 170: 1845:"Stratigraphy and correlation of the Permo-Carboniferous Cutler Group, Chama Basin, New Mexico" 607:. The Cutler Group contain important fossil quarries that shed light on the early evolution of 3886: 3841: 3781: 3756: 3711: 3650: 3402: 3362: 3307: 3211: 3191: 2419: 2416:
The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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Baldridge, W.; Olsen, K.; Callender, J. (1984). "Rio Grande Rift: Problems and Perspectives".
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
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The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11
1166: 1008: 956: 747: 735: 639: 623: 470: 301: 261: 229: 159: 595:, marking the transition from marine to continental sedimentation. The latter is recorded by 3961: 3916: 3796: 3761: 3442: 3251: 3216: 3196: 3186: 3048: 2972: 2827:"A preliminary assessment of the seismic hazard of the southern Rio Grande Rift, New Mexico" 2529: 2494: 1840: 1712: 1568: 1504: 1468: 1353: 1253: 1141: 897: 793: 778: 774: 643: 592: 365: 241: 237: 203: 100: 69: 54: 678:, giving New Mexico an exquisitely hot and dry climate through much of the early Mesozoic. 501: 3988: 3921: 3876: 3776: 3246: 3236: 2291:"Eocene tectonics and depositional setting of west-central New Mexico and eastern Arizona" 1016: 952: 901: 873: 869: 858: 782: 686: 671: 654: 553: 454: 412: 331: 323: 300:
dating. This indicates that the material making up the island arcs was extracted from the
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The region was tectonically quiescent until around 1400 Mya, when the poorly understood
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are now among the most productive groundwater reservoirs in the western United States.
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in the northwest has active oil and gas production, along with the small extent of the
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Rocks exposed in the southern Rocky Mountains are as old as nearly 1800 million years (
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Rinehart, L.F.; Lucas, S.G.; Heckert, A.B.; Spielmann, J.A.; Celesky, M.D. (2009).
1000: 739: 702: 612: 604: 587:. Towards the end of the Pennsylvanian, fluctuations in sea level caused by global 576: 571:
broke the ancient peneplain into basins separated by uplifts. Fossiliferous marine
466: 416: 340: 309: 273: 187: 151: 79:). This was followed by 200 million years of tectonic quiescence that ended in the 46: 1491:
Jones, James V. III; Daniel, Christopher G.; Frei, Dirk; Thrane, Kristine (2011).
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and 30 percent supracrustal formed between 1.765 and 1.4 billion years ago in the
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Lucas, Spencer G.; Zeigler, Kate E.; Heckert, Andrew B.; Hunt, Adrian P. (2005).
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Keller, G. R. (1986). "Introduction to Special Section on the Rio Grande Rift".
1134:"Landforms of the conterminous United States: a digital shaded-relief portrayal" 984: 944: 888:. Small mountain glaciers formed in the Brazos and Sangre de Cristo Mountains. 881: 781:. Advances and retreats of the coastline are recorded in formations such as the 711: 675: 396: 392: 384: 354: 344: 305: 281: 280:
The crust underlying the state formed between 1.7 and 1.8 billion years ago as
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Earthquake hazards are moderate in New Mexico compared with California or the
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Geologic hazards are infrequent in New Mexico, but potential dangers include
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in the southeast. Oil and gas production in the state totalled 1,820,963,878
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in northern New Mexico. These are described as juvenile crust, because their
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Geologic hazards are infrequent in New Mexico, but potential dangers include
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Sanford, Allan R.; Lin, Kuo-wan; Tsai, I-ching; Jaksha, Lawrence H. (2002).
2744: 2498: 1357: 843:, which deposited significant ash falls across much of New Mexico. The vast 720: 608: 572: 529: 490: 462: 435: 431: 408: 358: 327: 214: 42: 2210:"Laramide orogeny in central and northern New Mexico and southern Colorado" 1257: 465:
intruded into the crust throughout the western United States, such as the
992: 940: 884:, exploding and then collapsing into its magma chamber and emplacing the 797: 727: 622:, formed in southeastern New Mexico and Texas, surrounded by the massive 549: 545: 443: 362: 225: 143: 123: 108: 96: 738:. This was followed by flooding of northern New Mexico by an arm of the 674:
orogenies pushed up mountains to the west of New Mexico that produced a
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is an important geologic resource for farmers and municipal areas. The
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barrier reef. A brief rise in sea level deposited the limestone of the
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Most of New Mexico has a semiarid to arid climate, and ground water in
92: 72: 34: 2889: 2649:"Groundwater Resources of Union County, New Mexico: A Progress Report" 880:(or Jemez Caldera) formed in the Jemez Mountains 1.25 Mya ago in the 817: 743: 716: 635: 631: 415:
may be among the oldest, which are intruded by 1.65 billion year old
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only shortly before the island arcs formed. These rocks are mostly
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The geologic history of the state began with its assembly during the
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Because of New Mexico's typically semiarid climate, ground water in
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in the west has pulled away from the interior of the North American
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As the Farallon plate disintegrated and sank into the mantle, hot
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The geology of New Mexico. A geologic history (Special Volume 11)
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Zeigler, K.E.; Podzemny, B.; Yuhas, A.; Blumenberg, V. (2019).
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When Life Nearly Died: The greatest mass extinction of all time
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Memoirs of the New Mexico Bureau of Mines and Mineral Resources
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east of the coastal mountains thrown up by the Sevier orogeny.
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New Mexico Geological Society Guidebook, 35th field conference
1974:. Salt Lake City: University of Utah Press. pp. 141–217. 524:
New Mexico at the start of the Paleozoic was dominated by the
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Towards the end of the Cretaceous, shallow subduction of the
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is recorded nowhere in the rock beds of New Mexico, but the
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New Mexico Bureau of Geology and Mineral Resources Circular
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New Mexico Bureau of Mines & Mineral Resources Circular
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New Mexico Bureau of Geology and Mineral Resources Bulletin
556:. The sea did not submerge the Transcontinental Arch until 61:
Provinces meet, giving the state great geologic diversity.
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U.S. Geological Survey Miscellaneous Investigations Series
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for placer gold took place after an 1821 discovery in the
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of the Chinle Group preserved large numbers of fossils of
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polymettalic sulfides, rich in gold, silver and tungsten,
376:. The total relief of Precambrian rocks is 11 kilometers. 796:, which uplifted the Rocky Mountains and lasted into the 2448:
New Mexico Geological Society Field Conference Guidebook
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was again a time of arid climate. A great dune sea, or
154:(such as landslides); mine hazards; oil field hazards; 2718:. U.S. National Resources Committee. pp. 197–225. 2178: 2176: 1371:
Davis, Peter; Williams, Mike; Karlstrom, Karl (2011).
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are close to the crystallization ages determined from
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rock rose to take its place. This helped trigger the
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New Mexico Bureau of Geology & Mineral Resources
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The Geological Society of America Field Guide Series
41:, with ages ranging from almost 1800 million years ( 4012: 3974: 3960: 3699: 3456: 3283: 3167: 3096: 2943: 1852:
New Mexico Geologic Society Field Conference Series
611:. Continental sedimentation began in the north and 220:An important geologic feature of New Mexico is the 2278:. New Mexico Geological Society. pp. 203–248. 1875: 1873: 1598:. Geological Society of America. pp. 228–230. 1486: 1484: 1190:. New Mexico Geological Society. pp. 95–136. 1127: 1125: 947:potential of the Santa Fe Group was recognized by 265:Map of Precambrian bedrock exposures in New Mexico 107:commenced around 30 Mya, and was followed by late 2776:. National Oceanic and Atmospheric Administration 2749:New Mexico Burea of Geology and Mineral Resources 2739: 2737: 1786:. New Mexico Geological Society. pp. 77–93. 847:was active during this time, as were the smaller 544:) and sedimentary beds were deposited during the 2441:"The Santa Fe group of north-central New Mexico" 2317: 2315: 991:or other contamination of ground water or soil; 750:. The Jurassic ended with the deposition of the 563:By the late Paleozoic, in the Pennsylvanian and 419:, but display more than one metamorphic fabric. 142:or other contamination of ground water or soil; 2793: 2791: 2557: 2555: 1313:Geological Society of America Special Paper 291 1288:Geological Society of America Special Paper 291 773:, which deposited shore formations such as the 2728: 1615:. Geological Society of America. p. 205. 1455:Whitmeyer, Steven; Karlstrom, Karl E. (2007). 3676: 2905: 2514:Annual Review of Earth and Planetary Sciences 2276:The Geology of New Mexico: A Geologic History 1609:Daniel, Christoper G. and co-authors (2013). 1077:. New Mexico State University. Archived from 742:, leading to deposition of the limestone and 252:Stratigraphy, tectonics, and geologic history 8: 1110:. New Mexico Economic Development Department 658:Map of Mesozoic exposures in New Mexico, USA 532:to northern New Mexico. Small quantities of 202:in the north-central part of the state; the 182:Map of physiographic provinces of New Mexico 206:in the northwestern part of the state; and 3683: 3669: 3661: 2912: 2898: 2890: 1132:Thelin, Gail P.; Pike, Richard J. (1991). 1508: 1472: 1450: 1448: 1436: 1145: 951:in 1938, and the Alamosa subbasin of the 2115: 2103: 2030: 2006: 505:Map of Paleozoic exposures in New Mexico 351:of the Manzano and Los Pinos mountains. 2586: 2546: 2167: 1904: 1040: 804:Cenozoic (66 million years ago-present) 288:, the Gold Hill complex, and the Pecos 284:. This is recorded in the rocks of the 2602:. New Mexico Oil Conservation Division 1186:Mack, G.H.; Giles, K.A., eds. (2004). 276:, an uplifted Mesoproterozoic batholic 194:exposures, which are assigned to four 45:) to nearly the present day. Here the 4048:Geology of the United States by state 2681:Hawley, John; Kernodle, Mike (1999). 2212:. In Mack, G.H.; Giles, K.A. (eds.). 2127: 2018: 1994: 1165:. Mountain Press Publishing Company. 820:, recorded in formations such as the 497:Paleozoic (541-251 million years ago) 190:region. The state thus has extensive 7: 2289:Cather, S.M.; Johnson, B.D. (1984). 1104:"New Mexico Climate & Geography" 618:At the same time, a deep basin, the 591:produced cyclic formations like the 322:The island arcs were carried into a 2534:10.1146/annurev.ea.18.050190.000331 769:, the region was submerged by the 650:Mesozoic (251-66 million years ago) 2621:Mundahl, Erin (January 17, 2020). 812:Bandelier Tuff in San Diego Canyon 777:and marine formations such as the 14: 1530:Earth and Planetary Sciences Etds 1055:. United States Geological Survey 1053:Water Basics Information by Topic 758:, the latter deposited in a vast 664:Permian-Triassic extinction event 3644: 2600:"Natural Gas And Oil Production" 841:Mid-Tertiary ignimbrite flare-up 407:in the vicinity of Taos reached 75:1750 to 1650 million years ago ( 2567:New Mexico Workforce Connection 2479:Journal of Geophysical Research 1924:. London: Thames & Hudson. 1573:10.1016/j.precamres.2020.105820 1338:Journal of Geophysical Research 932:of natural gas and 331,460,749 513:Pennsylvanian limestone of the 3466:List of counties in New Mexico 1662:Armstrong, Augustus K (1967). 1211:McLemore, Virginia T. (2011). 1163:Roadside geology of New Mexico 552:, beginning with the Cambrian 1: 2563:"Mining (except oil and gas)" 1717:10.1016/S0040-1951(99)00005-0 1237:Dunbar, Neila W. (May 1999). 845:Mogollon-Datil volcanic field 174:Basins of the Rio Grande Rift 3692:Geology of the United States 2825:Salyards, Steven L. (1991). 715:, one of the earliest known 662:The Mesozoic began with the 224:. This extends from central 22:A view of the Nambe Badlands 2800:"Earthquakes in New Mexico" 2798:Jochems, Andy; Love, Dave. 2690:WRRI Conference Proceedings 2473:Aldrich Jr., M. J. (1986). 1596:Precambrian: Coterminous US 689:is recorded in beds of the 240:. The rift marks where the 4064: 3262:Sangre de Cristo Mountains 2729:Hawley & Kernodle 1999 2439:Baldwin, Brewster (1956). 2208:Cather, Steven M. (2004). 1594:Reed; et al. (1993). 1007:accumulation in homes; or 955:, the central part of the 585:Sangre de Cristo Formation 528:, an elevated region from 519:Sangre de Cristo Mountains 473:. This is recorded in the 158:accumulation in homes; or 3640: 2931: 1970:Fillmore, Robert (2010). 569:Ancestral Rocky Mountains 481:(about 1250 Mya) and the 422:Precambrian rocks formed 399:grade on the sequence of 379:The rocks are 70 percent 85:Ancestral Rocky Mountains 3994:Northern Mariana Islands 2958:Census-designated places 2774:National Weather Service 2770:"Flooding in New Mexico" 2244:Smith, Larry N. (1992). 1843:; Krainer, Karl (2005). 892:Natural resource geology 308:thought to be formed by 200:southern Rocky Mountains 51:southern Rocky Mountains 3275:Southwestern New Mexico 2499:10.1029/JB091iB02p01753 1358:10.1029/JB091iB06p06142 1161:Chronic, Halka (1987). 1075:"CLIMATE OF NEW MEXICO" 771:Western Interior Seaway 646:in the Delaware Basin. 599:formations such as the 196:physiographic provinces 39:physiographic provinces 813: 695:Anton Chico Formations 659: 521: 506: 277: 266: 183: 175: 115:, particularly in the 23: 4043:Geology of New Mexico 3694:by political division 3651:New Mexico portal 2079:"The paleobiology of 1258:10.58799/NMG-v21n2.25 995:or other subsidence; 811: 657: 526:Transcontinental Arch 512: 504: 479:Tumbledown Formations 272: 264: 181: 173: 146:or other subsidence; 21: 2418:. pp. 389–406. 2377:. pp. 359–388. 2352:. pp. 331–358. 2327:. pp. 203–248. 2216:. pp. 203–248. 2187:. pp. 249–270. 2144:. pp. 169–182. 1949:. pp. 137–152. 1553:Precambrian Research 1524:Luther, Amy (2006). 870:Jemez volcanic field 849:Latir volcanic field 707:Rock Point Formation 628:San Andres Formation 538:New Mexico aulacogen 487:Los Animas Formation 326:along the margin of 117:Jemez volcanic field 111:volcanism along the 4004:U.S. Virgin Islands 3222:Northern New Mexico 3083:Tourist attractions 2526:1990AREPS..18...27H 2491:1986JGR....91.1753A 2130:, pp. 143–147. 2118:, pp. 203–218. 2106:, pp. 201–203. 2033:, pp. 160–176. 2021:, pp. 138–142. 2009:, pp. 142–158. 1884:. pp. 95–136. 1761:. pp. 95–136. 1709:1999Tectp.305..225C 1641:. pp. 95–136. 1565:2020PreR..34705820H 1350:1986JGR....91.6142K 959:, and the southern 853:Ortiz porphyry belt 756:Morrison Formations 515:La Pasada Formation 430:, copper veins and 389:uranium-lead dating 374:Big Burro Mountains 91:time, 300 Mya. The 3257:Shortgrass prairie 3202:Eastern New Mexico 3182:Central New Mexico 3066:Pueblos and Tribes 2745:"Geologic Hazards" 1510:10.1130/GES00614.1 1474:10.1130/GES00055.1 1290:. pp. 27–37. 1246:New Mexico Geology 1009:volcanic eruptions 826:Galisteo Formation 822:San Jose Formation 814: 660: 581:Flechado Formation 567:, the rise of the 522: 507: 401:metamorphic facies 278: 267: 184: 176: 160:volcanic eruptions 37:exposures of four 24: 4030: 4029: 3658: 3657: 3302:Metropolitan Area 3212:Manzano Mountains 3192:Chihuahuan Desert 2806:. New Mexico Tech 2485:(B2): 1753–1762. 2081:Coelophysis bauri 1931:978-0-500-28573-2 1841:Lucas, Spencer G. 957:Albuquerque Basin 748:Todilto Formation 736:Entrada Formation 644:Salado Formations 471:Grenville orogeny 461:and in extensive 403:. An area in the 4055: 4014:Outlying islands 3968:Washington, D.C. 3962:Federal district 3685: 3678: 3671: 3662: 3649: 3648: 3647: 3252:Sandia Mountains 3217:Mogollon Plateau 3197:Colorado Plateau 3187:Chicoma Mountain 3049:New Mexico music 2914: 2907: 2900: 2891: 2884: 2883: 2881: 2879: 2865: 2856: 2850: 2849: 2847: 2845: 2831: 2822: 2816: 2815: 2813: 2811: 2795: 2786: 2785: 2783: 2781: 2766: 2760: 2759: 2757: 2755: 2741: 2732: 2726: 2720: 2719: 2711: 2705: 2704: 2702: 2700: 2687: 2678: 2672: 2671: 2669: 2667: 2653: 2644: 2638: 2637: 2635: 2633: 2618: 2612: 2611: 2609: 2607: 2596: 2590: 2589:, p. 24-27. 2584: 2578: 2577: 2575: 2573: 2559: 2550: 2549:, p. 30-31. 2544: 2538: 2537: 2509: 2503: 2502: 2470: 2464: 2463: 2461: 2459: 2445: 2436: 2430: 2429: 2410: 2404: 2403: 2402:. pp. 1–11. 2395: 2389: 2388: 2370: 2364: 2363: 2345: 2339: 2338: 2319: 2310: 2309: 2307: 2305: 2286: 2280: 2279: 2271: 2265: 2264: 2262: 2260: 2250: 2241: 2235: 2234: 2232: 2230: 2205: 2199: 2198: 2180: 2171: 2170:, p. 29-30. 2165: 2156: 2155: 2137: 2131: 2125: 2119: 2113: 2107: 2101: 2095: 2094: 2074: 2068: 2067: 2065: 2063: 2049: 2040: 2034: 2028: 2022: 2016: 2010: 2004: 1998: 1992: 1986: 1985: 1967: 1961: 1960: 1942: 1936: 1935: 1914: 1908: 1907:, p. 27-28. 1902: 1896: 1895: 1877: 1868: 1867: 1865: 1863: 1849: 1837: 1831: 1830: 1828: 1826: 1813: 1804: 1798: 1797: 1779: 1773: 1772: 1754: 1748: 1747: 1727: 1721: 1720: 1703:(1–3): 225–233. 1692: 1686: 1685: 1683: 1681: 1668: 1659: 1653: 1652: 1633: 1627: 1626: 1606: 1600: 1599: 1591: 1585: 1584: 1547: 1541: 1540: 1538: 1536: 1521: 1515: 1514: 1512: 1488: 1479: 1478: 1476: 1452: 1443: 1442: 1440: 1424: 1418: 1417: 1394: 1388: 1387: 1377: 1368: 1362: 1361: 1333: 1327: 1326: 1315:. pp. 1–3. 1308: 1302: 1301: 1283: 1277: 1276: 1274: 1272: 1243: 1234: 1228: 1227: 1217: 1208: 1202: 1201: 1183: 1177: 1176: 1158: 1152: 1151: 1149: 1129: 1120: 1119: 1117: 1115: 1100: 1091: 1090: 1088: 1086: 1071: 1065: 1064: 1062: 1060: 1045: 975:Geologic hazards 898:Artisanal mining 794:Laramide orogeny 779:Mancos Formation 775:Dakota Formation 638:and salt of the 593:Bursum Formation 366:Laramide orogeny 242:Colorado Plateau 238:Rio Grande River 204:Colorado Plateau 101:Laramide orogeny 95:and most of the 55:Colorado Plateau 4063: 4062: 4058: 4057: 4056: 4054: 4053: 4052: 4033: 4032: 4031: 4026: 4008: 3970: 3956: 3695: 3689: 3659: 3654: 3645: 3643: 3636: 3452: 3279: 3269:(highest point) 3247:San Luis Valley 3237:Rocky Mountains 3163: 3092: 2939: 2927: 2918: 2888: 2887: 2877: 2875: 2863: 2858: 2857: 2853: 2843: 2841: 2829: 2824: 2823: 2819: 2809: 2807: 2797: 2796: 2789: 2779: 2777: 2768: 2767: 2763: 2753: 2751: 2743: 2742: 2735: 2727: 2723: 2713: 2712: 2708: 2698: 2696: 2685: 2680: 2679: 2675: 2665: 2663: 2651: 2646: 2645: 2641: 2631: 2629: 2620: 2619: 2615: 2605: 2603: 2598: 2597: 2593: 2585: 2581: 2571: 2569: 2561: 2560: 2553: 2545: 2541: 2511: 2510: 2506: 2472: 2471: 2467: 2457: 2455: 2443: 2438: 2437: 2433: 2426: 2412: 2411: 2407: 2397: 2396: 2392: 2385: 2372: 2371: 2367: 2360: 2347: 2346: 2342: 2335: 2321: 2320: 2313: 2303: 2301: 2288: 2287: 2283: 2273: 2272: 2268: 2258: 2256: 2248: 2243: 2242: 2238: 2228: 2226: 2224: 2207: 2206: 2202: 2195: 2182: 2181: 2174: 2166: 2159: 2152: 2139: 2138: 2134: 2126: 2122: 2114: 2110: 2102: 2098: 2076: 2075: 2071: 2061: 2059: 2047: 2042: 2041: 2037: 2029: 2025: 2017: 2013: 2005: 2001: 1993: 1989: 1982: 1969: 1968: 1964: 1957: 1944: 1943: 1939: 1932: 1916: 1915: 1911: 1903: 1899: 1892: 1879: 1878: 1871: 1861: 1859: 1847: 1839: 1838: 1834: 1824: 1822: 1811: 1806: 1805: 1801: 1794: 1781: 1780: 1776: 1769: 1756: 1755: 1751: 1729: 1728: 1724: 1694: 1693: 1689: 1679: 1677: 1666: 1661: 1660: 1656: 1649: 1635: 1634: 1630: 1623: 1608: 1607: 1603: 1593: 1592: 1588: 1549: 1548: 1544: 1534: 1532: 1523: 1522: 1518: 1490: 1489: 1482: 1454: 1453: 1446: 1438:10.1.1.505.5407 1431:(25): 115–117. 1426: 1425: 1421: 1414: 1396: 1395: 1391: 1375: 1370: 1369: 1365: 1335: 1334: 1330: 1323: 1310: 1309: 1305: 1298: 1285: 1284: 1280: 1270: 1268: 1241: 1236: 1235: 1231: 1215: 1210: 1209: 1205: 1198: 1185: 1184: 1180: 1173: 1160: 1159: 1155: 1131: 1130: 1123: 1113: 1111: 1102: 1101: 1094: 1084: 1082: 1081:on July 8, 2004 1073: 1072: 1068: 1058: 1056: 1047: 1046: 1042: 1037: 1017:tropical storms 977: 953:San Luis Valley 902:Ortiz Mountains 894: 874:Jemez Lineament 859:Rio Grande rift 806: 783:Mesaverde Group 687:middle Triassic 652: 554:Bliss Formation 499: 455:Picuris orogeny 413:Tusas Mountains 332:Yavapai orogeny 324:subduction zone 290:greenstone belt 259: 254: 222:Rio Grande Rift 208:Basin and Range 168: 113:Jemez Lineament 105:Rio Grande rift 81:Picuris orogeny 59:Basin and Range 12: 11: 5: 4061: 4059: 4051: 4050: 4045: 4035: 4034: 4028: 4027: 4025: 4024: 4022:Howland Island 4018: 4016: 4010: 4009: 4007: 4006: 4001: 3996: 3991: 3986: 3984:American Samoa 3980: 3978: 3972: 3971: 3966: 3964: 3958: 3957: 3955: 3954: 3949: 3944: 3939: 3934: 3929: 3924: 3919: 3914: 3909: 3904: 3902:South Carolina 3899: 3894: 3889: 3884: 3879: 3874: 3869: 3867:North Carolina 3864: 3859: 3854: 3849: 3844: 3839: 3834: 3829: 3824: 3819: 3814: 3809: 3804: 3799: 3794: 3789: 3784: 3779: 3774: 3769: 3764: 3759: 3754: 3749: 3744: 3739: 3734: 3729: 3724: 3719: 3714: 3709: 3703: 3701: 3697: 3696: 3690: 3688: 3687: 3680: 3673: 3665: 3656: 3655: 3641: 3638: 3637: 3635: 3634: 3629: 3624: 3619: 3614: 3609: 3604: 3599: 3594: 3589: 3584: 3579: 3574: 3569: 3564: 3559: 3554: 3549: 3544: 3539: 3534: 3529: 3524: 3519: 3514: 3509: 3504: 3499: 3494: 3489: 3484: 3479: 3474: 3462: 3460: 3454: 3453: 3451: 3450: 3445: 3440: 3435: 3430: 3425: 3420: 3415: 3410: 3405: 3400: 3395: 3390: 3385: 3380: 3375: 3370: 3365: 3360: 3355: 3350: 3345: 3340: 3335: 3330: 3325: 3320: 3315: 3310: 3305: 3295: 3289: 3287: 3281: 3280: 3278: 3277: 3272: 3271: 3270: 3259: 3254: 3249: 3244: 3242:San Juan Basin 3239: 3234: 3229: 3224: 3219: 3214: 3209: 3207:Llano Estacado 3204: 3199: 3194: 3189: 3184: 3179: 3173: 3171: 3165: 3164: 3162: 3161: 3156: 3151: 3146: 3141: 3136: 3131: 3126: 3121: 3116: 3111: 3109:Climate change 3106: 3100: 3098: 3094: 3093: 3091: 3090: 3088:Transportation 3085: 3080: 3075: 3070: 3069: 3068: 3063: 3053: 3052: 3051: 3041: 3040: 3039: 3034: 3029: 3027:National Guard 3019: 3014: 3013: 3012: 3007: 2997: 2992: 2987: 2982: 2977: 2976: 2975: 2970: 2960: 2955: 2949: 2947: 2941: 2940: 2932: 2929: 2928: 2919: 2917: 2916: 2909: 2902: 2894: 2886: 2885: 2851: 2817: 2787: 2761: 2733: 2721: 2706: 2673: 2639: 2613: 2591: 2579: 2551: 2539: 2504: 2465: 2431: 2424: 2405: 2390: 2383: 2365: 2358: 2340: 2333: 2311: 2281: 2266: 2236: 2222: 2200: 2193: 2172: 2157: 2150: 2132: 2120: 2108: 2096: 2069: 2035: 2023: 2011: 1999: 1997:, p. 137. 1987: 1980: 1962: 1955: 1937: 1930: 1909: 1897: 1890: 1869: 1832: 1799: 1792: 1774: 1767: 1749: 1722: 1697:Tectonophysics 1687: 1654: 1647: 1628: 1621: 1601: 1586: 1542: 1516: 1503:(4): 974–991. 1480: 1444: 1419: 1412: 1389: 1363: 1328: 1321: 1303: 1296: 1278: 1229: 1203: 1196: 1178: 1172:978-0878422098 1171: 1153: 1140:. MAP I-2206. 1121: 1108:Why New Mexico 1092: 1066: 1039: 1038: 1036: 1033: 985:flash flooding 976: 973: 922:San Juan Basin 913:including the 893: 890: 886:Bandelier Tuff 878:Valles Caldera 863:Santa Fe Group 830:Baca Formation 805: 802: 790:Farallon plate 760:foreland basin 683:lower Triassic 651: 648: 620:Delaware Basin 615:to the south. 534:alkaline magma 498: 495: 405:Cimarron Range 370:Zuni Mountains 302:Earth's mantle 286:Moppin Complex 258: 255: 253: 250: 167: 164: 136:flash flooding 13: 10: 9: 6: 4: 3: 2: 4060: 4049: 4046: 4044: 4041: 4040: 4038: 4023: 4020: 4019: 4017: 4015: 4011: 4005: 4002: 4000: 3997: 3995: 3992: 3990: 3987: 3985: 3982: 3981: 3979: 3977: 3973: 3969: 3965: 3963: 3959: 3953: 3950: 3948: 3945: 3943: 3942:West Virginia 3940: 3938: 3935: 3933: 3930: 3928: 3925: 3923: 3920: 3918: 3915: 3913: 3910: 3908: 3905: 3903: 3900: 3898: 3895: 3893: 3890: 3888: 3885: 3883: 3880: 3878: 3875: 3873: 3870: 3868: 3865: 3863: 3860: 3858: 3855: 3853: 3850: 3848: 3847:New Hampshire 3845: 3843: 3840: 3838: 3835: 3833: 3830: 3828: 3825: 3823: 3820: 3818: 3815: 3813: 3810: 3808: 3807:Massachusetts 3805: 3803: 3800: 3798: 3795: 3793: 3790: 3788: 3785: 3783: 3780: 3778: 3775: 3773: 3770: 3768: 3765: 3763: 3760: 3758: 3755: 3753: 3750: 3748: 3745: 3743: 3740: 3738: 3735: 3733: 3730: 3728: 3725: 3723: 3720: 3718: 3715: 3713: 3710: 3708: 3705: 3704: 3702: 3698: 3693: 3686: 3681: 3679: 3674: 3672: 3667: 3666: 3663: 3653: 3652: 3639: 3633: 3630: 3628: 3625: 3623: 3620: 3618: 3615: 3613: 3610: 3608: 3605: 3603: 3600: 3598: 3595: 3593: 3590: 3588: 3585: 3583: 3580: 3578: 3575: 3573: 3570: 3568: 3565: 3563: 3560: 3558: 3555: 3553: 3550: 3548: 3545: 3543: 3540: 3538: 3535: 3533: 3530: 3528: 3525: 3523: 3520: 3518: 3515: 3513: 3510: 3508: 3505: 3503: 3500: 3498: 3495: 3493: 3490: 3488: 3485: 3483: 3480: 3478: 3475: 3473: 3470: 3469: 3468: 3467: 3461: 3459: 3455: 3449: 3446: 3444: 3441: 3439: 3436: 3434: 3431: 3429: 3426: 3424: 3421: 3419: 3416: 3414: 3411: 3409: 3406: 3404: 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2318: 2316: 2312: 2300: 2296: 2292: 2285: 2282: 2277: 2270: 2267: 2255:(43): 297–310 2254: 2247: 2240: 2237: 2225: 2223:9781585460106 2219: 2215: 2211: 2204: 2201: 2196: 2194:9781585460106 2190: 2186: 2179: 2177: 2173: 2169: 2164: 2162: 2158: 2153: 2151:9781585460106 2147: 2143: 2136: 2133: 2129: 2124: 2121: 2117: 2116:Fillmore 2010 2112: 2109: 2105: 2104:Fillmore 2010 2100: 2097: 2092: 2088: 2084: 2082: 2073: 2070: 2057: 2053: 2046: 2039: 2036: 2032: 2031:Fillmore 2010 2027: 2024: 2020: 2015: 2012: 2008: 2007:Fillmore 2010 2003: 2000: 1996: 1991: 1988: 1983: 1981:9781607810049 1977: 1973: 1966: 1963: 1958: 1956:9781585460106 1952: 1948: 1941: 1938: 1933: 1927: 1923: 1919: 1913: 1910: 1906: 1901: 1898: 1893: 1891:9781585460106 1887: 1883: 1876: 1874: 1870: 1857: 1853: 1846: 1842: 1836: 1833: 1821: 1817: 1810: 1803: 1800: 1795: 1793:9781585460106 1789: 1785: 1778: 1775: 1770: 1768:9781585460106 1764: 1760: 1753: 1750: 1745: 1741: 1737: 1733: 1726: 1723: 1718: 1714: 1710: 1706: 1702: 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349:Manzano Group 346: 342: 337: 333: 329: 325: 320: 318: 315: 311: 307: 303: 299: 295: 294:Nd model ages 291: 287: 283: 275: 271: 263: 256: 251: 249: 247: 243: 239: 235: 231: 227: 223: 218: 216: 211: 209: 205: 201: 197: 193: 189: 180: 172: 165: 163: 161: 157: 153: 149: 145: 141: 137: 133: 128: 125: 120: 118: 114: 110: 106: 102: 98: 94: 90: 89:Pennsylvanian 86: 82: 78: 74: 71: 67: 62: 60: 56: 52: 48: 44: 40: 36: 32: 31: 20: 16: 3999:Puerto Rico 3907:South Dakota 3897:Rhode Island 3892:Pennsylvania 3872:North Dakota 3856: 3642: 3463: 3438:Sunland Park 3267:Wheeler Peak 3144:Homelessness 3119:Demographics 3073:Paleontology 3056:New Mexicans 3037:World War II 3005:Nuevo México 2933: 2876:. 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Retrieved 1052: 1043: 1021: 1013: 1001:mass wasting 987:in arroyos; 978: 938: 919: 911: 907: 895: 867: 856: 834: 815: 787: 764: 746:beds of the 740:Sundance Sea 725: 710: 703:Chinle Group 680: 661: 617: 605:Cutler Group 577:Madera Group 575:such as the 562: 523: 467:Sandia Crest 452: 424:volcanogenic 421: 417:trondhjemite 378: 361:, the early 353: 341:Vadito Group 321: 310:metamorphism 306:amphibolites 279: 274:Sandia Crest 228:to northern 219: 212: 188:Great Plains 185: 166:Physiography 152:mass wasting 138:in arroyos; 129: 121: 63: 47:Great Plains 27: 25: 15: 3976:Territories 3822:Mississippi 3737:Connecticut 3428:Silver City 3298:Albuquerque 3149:LGBT rights 2985:Delegations 1406:: 201–229. 997:earthquakes 963:basin from 945:groundwater 915:Questa Mine 882:Pleistocene 752:Summerville 712:Coelophysis 676:rain shadow 438:, lithium, 397:amphibolite 393:greenschist 387:, based on 385:Proterozoic 355:Precambrian 345:Hondo Group 334:. The arcs 282:island arcs 257:Proterozoic 148:earthquakes 28:geology of 4037:Categories 3937:Washington 3857:New Mexico 3852:New Jersey 3727:California 3592:San Miguel 3577:Rio Arriba 3547:Los Alamos 3472:Bernalillo 3408:Rio Rancho 3383:Los Alamos 3373:Las Cruces 3348:Farmington 3318:Bloomfield 3293:Alamogordo 3232:Rio Grande 3154:Literature 2995:Government 2968:Bizcochito 2925:New Mexico 2128:Lucas 2004 2019:Lucas 2004 1995:Lucas 2004 1918:Benton M J 1559:: 105820. 1535:August 27, 1467:(4): 220. 1386:: 177–190. 1226:: 379–388. 1035:References 965:Las Cruces 949:Kirk Bryan 828:, and the 792:drove the 767:Cretaceous 589:glaciation 463:batholiths 314:tholeiitic 30:New Mexico 3947:Wisconsin 3912:Tennessee 3817:Minnesota 3792:Louisiana 3582:Roosevelt 3522:Guadalupe 3448:Tucumcari 3393:Lovington 3388:Los Lunas 3378:Las Vegas 3134:Elections 3129:Education 3032:Civil War 3017:Landmarks 3010:Territory 2990:Geography 2938:(capital) 2662:: 127–137 2454:: 115–121 2229:April 28, 2062:April 29, 2058:: 170–181 1858:: 145–159 1744:130142252 1581:225308346 1497:Geosphere 1461:Geosphere 1433:CiteSeerX 1266:259456553 1085:March 20, 993:sinkholes 721:dinosaurs 613:prograded 609:tetrapods 573:limestone 530:Minnesota 491:peneplain 475:Allamoore 436:beryllium 432:pegmatite 409:granulite 359:Paleozoic 328:Laurentia 230:Chihuahua 144:sinkholes 73:orogenies 33:includes 3932:Virginia 3882:Oklahoma 3862:New York 3837:Nebraska 3827:Missouri 3812:Michigan 3802:Maryland 3787:Kentucky 3767:Illinois 3742:Delaware 3732:Colorado 3722:Arkansas 3632:Valencia 3622:Torrance 3602:Santa Fe 3597:Sandoval 3587:San Juan 3557:McKinley 3507:Doña Ana 3458:Counties 3423:Santa Fe 3398:Portales 3368:Kirtland 3343:Española 3333:Corrales 3323:Carlsbad 3159:Politics 3139:Gun laws 3104:Abortion 3061:Hispanos 3022:Military 2935:Santa Fe 2878:June 15, 2844:June 15, 2810:June 15, 2304:June 24, 1920:(2005). 1825:July 11, 941:aquifers 851:and the 798:Cenozoic 728:Jurassic 691:Moenkopi 550:Devonian 548:through 546:Cambrian 444:tantalum 363:Cenozoic 336:accreted 226:Colorado 124:aquifers 109:Cenozoic 97:Mesozoic 70:Mazatzal 3952:Wyoming 3927:Vermont 3832:Montana 3772:Indiana 3752:Georgia 3747:Florida 3717:Arizona 3707:Alabama 3612:Socorro 3542:Lincoln 3532:Hidalgo 3527:Harding 3502:De Baca 3433:Socorro 3418:Ruidoso 3413:Roswell 3313:Artesia 3169:Regions 3124:Economy 3097:Society 3078:Symbols 3000:History 2980:Culture 2963:Cuisine 2780:June 9, 2699:May 13, 2522:Bibcode 2487:Bibcode 1862:July 9, 1705:Bibcode 1680:May 21, 1561:Bibcode 1346:Bibcode 1114:June 9, 1059:June 9, 1029:Socorro 989:arsenic 981:erosion 969:El Paso 961:Mesilla 934:barrels 824:, the 672:Nevadan 640:Castile 624:Capitan 603:or the 597:red bed 565:Permian 517:in the 440:niobium 428:kyanite 381:plutons 192:bedrock 140:arsenic 132:erosion 93:Permian 66:Yavapai 35:bedrock 3887:Oregon 3842:Nevada 3782:Kansas 3757:Hawaii 3712:Alaska 3700:States 3607:Sierra 3492:Colfax 3487:Cibola 3482:Chaves 3477:Catron 3358:Grants 3353:Gallup 3338:Deming 3328:Clovis 3285:Cities 2945:Topics 2422:  2381:  2356:  2331:  2259:May 7, 2220:  2191:  2148:  2093:: 260. 1978:  1953:  1928:  1888:  1790:  1765:  1742:  1645:  1619:  1579:  1435:  1410:  1319:  1294:  1264:  1194:  1169:  876:. The 818:Eocene 744:gypsum 717:genera 705:. The 668:Sevier 666:. The 636:potash 632:gypsum 560:time. 317:basalt 246:craton 234:Mexico 57:, and 3917:Texas 3797:Maine 3762:Idaho 3627:Union 3567:Otero 3517:Grant 3497:Curry 3464:See: 3403:Raton 3363:Hobbs 3308:Aztec 3114:Crime 3044:Music 2973:Chile 2953:Index 2921:State 2864:(PDF) 2840:: 199 2830:(PDF) 2686:(PDF) 2652:(PDF) 2444:(PDF) 2249:(PDF) 2048:(PDF) 1848:(PDF) 1812:(PDF) 1740:S2CID 1667:(PDF) 1577:S2CID 1376:(PDF) 1262:S2CID 1242:(PDF) 1216:(PDF) 1005:radon 434:with 156:radon 3989:Guam 3922:Utah 3877:Ohio 3777:Iowa 3617:Taos 3572:Quay 3562:Mora 3552:Luna 3512:Eddy 3443:Taos 2880:2021 2846:2021 2812:2021 2782:2021 2756:2020 2701:2020 2668:2020 2634:2020 2608:2020 2574:2020 2460:2020 2420:ISBN 2379:ISBN 2354:ISBN 2329:ISBN 2306:2021 2261:2020 2231:2022 2218:ISBN 2189:ISBN 2146:ISBN 2064:2020 1976:ISBN 1951:ISBN 1926:ISBN 1886:ISBN 1864:2020 1827:2020 1788:ISBN 1763:ISBN 1682:2019 1643:ISBN 1617:ISBN 1537:2020 1408:ISBN 1317:ISBN 1292:ISBN 1273:2020 1192:ISBN 1167:ISBN 1116:2021 1087:2010 1061:2021 920:The 868:The 754:and 726:The 693:and 681:The 670:and 642:and 485:and 477:and 448:mica 446:and 395:and 372:and 343:and 298:U-Pb 68:and 26:The 3537:Lea 2923:of 2874:: 5 2872:210 2530:doi 2495:doi 2299:192 1736:160 1713:doi 1701:305 1569:doi 1557:347 1505:doi 1469:doi 1354:doi 1254:doi 1142:doi 983:or 967:to 930:MCF 800:. 732:erg 719:of 583:or 312:of 134:or 87:in 77:Mya 4039:: 2870:. 2866:. 2838:42 2836:. 2832:. 2802:. 2790:^ 2772:. 2747:. 2736:^ 2694:44 2692:. 2688:. 2660:70 2658:. 2654:. 2625:. 2565:. 2554:^ 2528:. 2518:18 2516:. 2493:. 2483:91 2481:. 2477:. 2450:. 2446:. 2314:^ 2297:. 2293:. 2251:. 2175:^ 2160:^ 2091:45 2089:. 2085:. 2056:56 2054:. 2050:. 1872:^ 1856:56 1854:. 1850:. 1820:56 1818:. 1814:. 1738:. 1734:. 1711:. 1699:. 1675:20 1673:. 1669:. 1575:. 1567:. 1555:. 1528:. 1499:. 1495:. 1483:^ 1463:. 1459:. 1447:^ 1404:44 1402:. 1384:62 1382:. 1378:. 1352:. 1342:91 1340:. 1260:. 1250:21 1248:. 1244:. 1224:62 1222:. 1218:. 1136:. 1124:^ 1106:. 1095:^ 1051:. 1011:. 999:; 865:. 832:. 785:. 723:. 634:, 493:. 450:. 442:, 319:. 232:, 215:Ma 162:. 150:; 119:. 53:, 49:, 43:Ma 3684:e 3677:t 3670:v 3304:) 3300:( 2913:e 2906:t 2899:v 2882:. 2848:. 2814:. 2784:. 2758:. 2703:. 2670:. 2636:. 2610:. 2576:. 2536:. 2532:: 2524:: 2501:. 2497:: 2489:: 2462:. 2452:7 2428:. 2387:. 2362:. 2337:. 2308:. 2263:. 2233:. 2197:. 2154:. 2066:. 1984:. 1959:. 1934:. 1894:. 1866:. 1829:. 1796:. 1771:. 1746:. 1719:. 1715:: 1707:: 1684:. 1651:. 1625:. 1583:. 1571:: 1563:: 1539:. 1513:. 1507:: 1501:7 1477:. 1471:: 1465:3 1441:. 1416:. 1360:. 1356:: 1348:: 1325:. 1300:. 1275:. 1256:: 1200:. 1175:. 1150:. 1144:: 1118:. 1089:. 1063:.

Index


New Mexico
bedrock
physiographic provinces
Ma
Great Plains
southern Rocky Mountains
Colorado Plateau
Basin and Range
Yavapai
Mazatzal
orogenies
Mya
Picuris orogeny
Ancestral Rocky Mountains
Pennsylvanian
Permian
Mesozoic
Laramide orogeny
Rio Grande rift
Cenozoic
Jemez Lineament
Jemez volcanic field
aquifers
erosion
flash flooding
arsenic
sinkholes
earthquakes
mass wasting

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