Knowledge (XXG)

Los Pinos Formation

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The formation was named the Los Pinos Gravel by E.S. Larsen and reported in 1932. It was designated the Los Pinos Member of the Hinsdale Formation, which it closely resembles, by
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The age of the formation is presently constrained by radiometric ages of interbedded flows and underlying and overlying formations. The underlying
430: 731:"Geophysical expression of elements of the Rio Grande rift in the northeast Tusas Mountains - Preliminary interpretations" 535:). Interbedded flows have been dated at 17.7 Ma and 20.7 Ma. Flows of the overlying Servilleta Formation are 4.5 Ma old. 219: 212: 729:
Drenth, Benjamin J.; Turner, Kenzie J.; Thompson, Ren A.; Grauch, V. J. S.; Cosca, Michaela A.; Lee, John P. (2011).
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Manley, Kim (1981). "Redefinition and description of the Los Pinos Formation of north-central New Mexico".
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is located along Los Pinos Creek, near the town of San Miguel in extreme northern New Mexico (
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to the north. It thins to the south, where it underlies the Cordito Member. The
57: 707:"A brief review of the geology of the San Juan region of southwestern Colorado" 424: 420: 373: 255: 102: 67: 445: 432: 234: 221: 638:"Physiogeography and Quaternary geology of the San Juan Mountains, Colorado" 532: 465: 392: 107: 51: 547:
and Larsen in 1935, and raised to formation rank by Fred Barker in 1958.
497: 97: 92: 77: 72: 62: 680:"Precambrian and Tertiary geology of Las Tablas quadrangle, New Mexico" 112: 87: 412: 653: 464: 458:). It also likely present in the subsurface of the southwestern 408: 504:
and possibly another center buried beneath basalt flows of the
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clasts, was eroded from source areas to the east, such the
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10.1130/0016-7606(1981)92<984:RADOTL>2.0.CO;2
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New Mexico Bureau of Mines and Mineral Resources Bulletin
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New Mexico Geological Society Field Conference Series
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have radiometric ages of 29.8 to 28.2 million years (
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(1932). 801:Paleogene formations of New Mexico 18:A geologic formation in New Mexico 14: 796:Neogene formations of New Mexico 469:Road cut exposing Cordito Member 350:Los Pinos Formation (New Mexico) 341: 334: 313: 306: 711:U.S. Geological Survey Bulletin 147:Esquibel & Cordito Members 23:Los Pinos Formation, Argentina 1: 325:Show map of the United States 376:. It was deposited from the 415:flows. It crops out in the 817: 20: 520:with the Cordito Member. 300: 121: 35: 584:Atwood & Mather 1932 539:History of investigation 187:500 ft (150 m) 21:Not to be confused with 705:; Larsen, E.S. (1935). 663:2027/mdp.39015086702506 608:Cross & Larsen 1935 490:San Juan volcanic field 166:Treasure Mountain Group 644:. Professional Paper. 470: 353:Show map of New Mexico 678:Barker, Fred (1958). 545:Charles Whitman Cross 496:, composed mostly of 468: 506:Servilleta Formation 502:Latir volcanic field 446:36.9614°N 106.1693°W 156:Servilleta Formation 771:1981GSAB...92..984M 475:penecontemporaneous 442: /  407:, with interbedded 366:Los Pinos Formation 231: /  37:Stratigraphic range 31:Los Pinos Formation 596:Drenth et al. 2011 529:Masonic Park Tuffs 471: 451:36.9614; -106.1693 370:geologic formation 235:36.950°N 106.124°W 525:Treasure Mountain 514:Abiquiu Formation 362: 361: 170:Masonic Park Tuff 808: 782: 753: 751: 749: 735: 725: 723: 721: 698: 696: 694: 674: 672: 670: 665: 623: 617: 611: 605: 599: 593: 587: 581: 572: 566: 457: 456: 454: 453: 452: 447: 443: 440: 439: 438: 435: 389:radiometric ages 354: 345: 344: 338: 326: 317: 316: 310: 246: 245: 243: 242: 241: 240:36.950; -106.124 236: 232: 229: 228: 227: 224: 126: 117: 54: 28: 816: 815: 811: 810: 809: 807: 806: 805: 786: 785: 756: 747: 745: 733: 728: 719: 717: 701: 692: 690: 677: 668: 666: 635: 632: 627: 626: 618: 614: 606: 602: 594: 590: 582: 575: 567: 558: 553: 541: 510:Rio Grande rift 482:Esquibel Member 450: 448: 444: 441: 436: 433: 431: 429: 428: 417:Tusas Mountains 401: 391:of interbedded 358: 357: 356: 355: 352: 351: 348: 347: 346: 329: 328: 327: 324: 323: 320: 319: 318: 280:Los Pinos Creek 239: 237: 233: 230: 225: 222: 220: 218: 217: 129: 116: 115: 110: 105: 100: 95: 90: 85: 80: 75: 70: 65: 60: 49: 48: 47: 26: 19: 12: 11: 5: 814: 812: 804: 803: 798: 788: 787: 784: 783: 754: 726: 703:Cross, Whitman 699: 675: 631: 628: 625: 624: 612: 600: 588: 573: 555: 554: 552: 549: 540: 537: 494:Cordito Member 460:San Luis basin 405:volcaniclastic 400: 397: 378:late Oligocene 360: 359: 349: 340: 339: 333: 332: 331: 330: 321: 312: 311: 305: 304: 303: 302: 301: 298: 297: 294: 290: 289: 286: 282: 281: 278: 274: 273: 269: 268: 263: 259: 258: 252: 248: 247: 215: 209: 208: 204: 203: 201:Volcaniclastic 198: 194: 193: 189: 188: 185: 181: 180: 177: 173: 172: 163: 159: 158: 153: 149: 148: 145: 141: 140: 135: 131: 130: 127: 119: 118: 111: 106: 101: 96: 91: 86: 81: 76: 71: 66: 61: 56: 55: 50:28.2–4.5  41:Late Oligocene 33: 32: 17: 13: 10: 9: 6: 4: 3: 2: 813: 802: 799: 797: 794: 793: 791: 780: 776: 772: 768: 764: 760: 755: 743: 739: 732: 727: 716: 712: 708: 704: 700: 689: 685: 681: 676: 664: 659: 655: 654:10.3133/pp166 651: 647: 643: 639: 634: 633: 629: 621: 616: 613: 609: 604: 601: 597: 592: 589: 585: 580: 578: 574: 570: 565: 563: 561: 557: 550: 548: 546: 538: 536: 534: 530: 526: 521: 519: 515: 511: 507: 503: 499: 495: 491: 487: 483: 479: 476: 467: 463: 461: 455: 426: 422: 418: 414: 410: 406: 398: 396: 394: 390: 386: 383: 379: 375: 371: 367: 337: 309: 299: 295: 291: 287: 283: 279: 275: 270: 267: 266:United States 264: 260: 257: 253: 249: 244: 216: 214: 210: 205: 202: 199: 195: 190: 186: 182: 178: 174: 171: 167: 164: 160: 157: 154: 150: 146: 142: 139: 136: 132: 125: 120: 114: 109: 104: 99: 94: 89: 84: 79: 74: 69: 64: 59: 53: 46: 42: 38: 34: 29: 24: 16: 762: 758: 746:. Retrieved 741: 737: 718:. Retrieved 714: 710: 691:. Retrieved 687: 683: 667:. Retrieved 645: 641: 630:Bibliography 615: 603: 591: 542: 522: 493: 486:intermediate 481: 472: 425:type section 402: 382:late Miocene 380:through the 372:in northern 365: 363: 293:Year defined 272:Type section 45:Late Miocene 15: 765:(12): 984. 620:Barker 1958 569:Manley 1981 449: / 437:106°10′09″W 399:Description 387:, based on 288:E.S. Larsen 238: / 226:106°07′26″W 213:Coordinates 790:Categories 551:References 434:36°57′41″N 421:New Mexico 393:lava flows 374:New Mexico 256:New Mexico 223:36°57′00″N 744:: 165–176 720:30 August 669:30 August 518:correlate 498:rhyolitic 277:Named for 254:Northern 192:Lithology 184:Thickness 152:Underlies 144:Sub-units 138:Formation 285:Named by 207:Location 162:Overlies 767:Bibcode 748:14 July 693:28 June 508:in the 478:members 262:Country 197:Primary 480:. The 423:. The 413:basalt 385:epochs 251:Region 734:(PDF) 409:tuffs 368:is a 750:2021 722:2020 695:2020 671:2020 527:and 516:may 411:and 364:The 296:1932 176:Area 134:Type 58:PreꞒ 775:doi 715:843 658:hdl 650:doi 646:166 419:of 792:: 773:. 763:92 761:. 742:62 740:. 736:. 713:. 709:. 688:45 686:. 682:. 656:. 648:. 640:. 576:^ 559:^ 533:Ma 168:, 108:Pg 52:Ma 39:: 781:. 777:: 769:: 752:. 724:. 697:. 673:. 660:: 652:: 622:. 610:. 598:. 586:. 571:. 113:N 103:K 98:J 93:T 88:P 83:C 78:D 73:S 68:O 63:Ꞓ 43:- 25:.

Index

Los Pinos Formation, Argentina
Stratigraphic range
Late Oligocene
Late Miocene
Ma
PreꞒ

O
S
D
C
P
T
J
K
Pg
N

Formation
Servilleta Formation
Treasure Mountain Group
Masonic Park Tuff
Volcaniclastic
Coordinates
36°57′00″N 106°07′26″W / 36.950°N 106.124°W / 36.950; -106.124
New Mexico
United States
Los Pinos Formation is located in the United States
Los Pinos Formation is located in New Mexico
geologic formation

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