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Crevasse Canyon Formation

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In some exposures, the Dilco Coal Member is separated from the Dalton Sandstone Member by the Mulatto Tongue of the Mancos Shale. A fourth member of the Crevasse Canyon Formation, the Borrego Pass Lentil, is found in a limited exposure area between the Dilco Coal Member and the Mulatto Tongue. The
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or ripple laminated." The Dalton Sandstone Member is described as "Gray to yellowish gray, fine- to medium-grained, cliff-forming sandstone." The Gibson Coal Member is described as "Drab mudstone, buff, brown, and greenish gray sandstone (commonly
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In the San Juan Basin, the Gibson Coal Member and the Dilco Coal Member were exploited for coal for steam locomotives from the 1940s to the 1990s. However, they constitute less than 1% of the original coal reserves of San Juan Basin.
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Estrada-Ruiz, Emilio; Upchurch, Garland R.; Wheeler, Elisabeth A.; Mack, Greg H. (May 2012). "Late Cretaceous Angiosperm Woods from the Crevasse Canyon and McRae Formations, South-Central New Mexico, USA: Part 1".
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Mack, Greg H. (1992). "Paleosols as an Indicator of Climatic Change at the Early-Late Cretaceous Boundary, Southwestern New Mexico".
898: 692: 899:"A new species of Neurankylus (Testudines; Baenidae) from the upper Cretaceous Crevasse Canyon Formation, Southern New Mexico, USA" 557: 1001: 478:
remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific
946: 763: 432:), and coal," with the coals typically less than 0.5 m thick. Thickness is 700 feet (210 m) at the type section. 982: 790: 866: 195: 812:"Borrego Pass Lentil, a new member of the Crevasse Canyon Formation, southern San Juan basin, New Mexico" 1021: 1016: 502: 548:
The formation was originally described in 1954 by Allen and Balk as part of the Mesaverde Group.
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The formation is divided into three members, in ascending stratigraphic order:
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In southern New Mexico, the Crevasse Canyon Formation contains fossil soils (
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New Mexico Bureau of Geology and Mineral Resources, Open-File Geologic Map
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O'Sullivan, R.B.; Repenning, C.A.; Beaumont, E.C.; Page, H.G. (1972).
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Weishampel, David B.; Dodson, Peter; OsmĂłlska, Halszka, eds. (2004).
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Lucas, Spencer G.; Dalman, Sebastian G.; Sullivan, Robert M. (2016).
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List of stratigraphic units with indeterminate dinosaur fossils
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Tschudy (1976) identified the Crevasse Canyon formation as
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New Mexico Bureau of Mines and Mineral Resources Circular
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New Mexico Museum of Natural History and Science Bulletin
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New Mexico Bureau of Mines and Mineral Resources Bulletin
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New Mexico Museum of Natural History and Science Bulletin
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Dilco Coal, Dalton Sandstone & Gibson Coal Members
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New Mexico Geological Society Field Conference Series
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Borrego Pass Lentil is a highly variable sandstone.
739: 727: 690: 493:turtle that is the earliest representative of its 621: 594: 346: 318: 993: 455:contains paleosols typical of an arid climate ( 326:Crevasse Canyon Formation (the United States) 892: 678: 18:Geologic formation in New Mexico and Arizona 654:10.1306/D426792E-2B26-11D7-8648000102C1865D 543: 501:have been identified in the formation near 482:. The formation is the type formation for 935: 928:U.S. Geological Survey Professional Paper 761: 588: 1012:Upper Cretaceous Series of North America 558:List of dinosaur-bearing rock formations 944: 864: 838:International Journal of Plant Sciences 745: 733: 994: 867:"Coal resources of the San Juan Basin" 809: 788: 667:Weishampel, Dodson & OsmĂłlska 2004 627: 603: 354:Crevasse Canyon Formation (New Mexico) 930:. Professional Paper. 521-E: E1–E65. 534: 511:is common in the Gibson Coal Member. 642:SEPM Journal of Sedimentary Research 639: 1007:Cretaceous formations of New Mexico 13: 762:Allen, J.E.; Balk, Robert (1954). 14: 1033: 470: 345: 338: 317: 310: 252: 37: 755: 1002:Geologic formations of Arizona 684: 633: 443:) typical of a humid climate ( 394: 1: 570: 329:Show map of the United States 7: 551: 10: 1038: 865:Fassett, James E. (1989). 415:, fine- to medium-grained 467:boundary in this region. 370:Crevasse Canyon Formation 304: 296: 288: 280: 275: 265: 247: 233: 194: 189: 171: 166: 158: 148: 138: 130: 120: 110: 28: 24:Crevasse Canyon Formation 23: 722:Estrada-Ruiz et al. 2012 679:Lichtig & Lucas 2016 544:History of investigation 503:Elephant Butte Reservoir 423:. Sandstone is commonly 162:700 ft (210 m) 789:Cather, Steven (2010). 405:Dalton Sandstone Member 143:Point Lookout Sandstone 945:Tschudy, R.H. (1976). 816:The Mountain Geologist 616:O'Sullivan et al. 1972 514: 357:Show map of New Mexico 810:Correa, A.C. (1970). 589:Allen & Balk 1954 218:35.7916°N 108.9446°W 893:Lichtig, Asher J.; 669:, pp. 517–607. 531:of coal and shale. 214: /  30:Stratigraphic range 535:Economic resources 451:). The underlying 409:Gibson Coal Member 381:geologic formation 223:35.7916; -108.9446 895:Lucas, Spencer G. 401:Dilco Coal Member 366: 365: 1029: 988: 969: 967: 965: 951: 941: 939: 918: 916: 914: 889: 887: 885: 871: 861: 831: 829: 827: 806: 804: 802: 785: 783: 781: 768: 749: 743: 737: 731: 725: 719: 713: 712: 710: 708: 688: 682: 676: 670: 664: 658: 657: 637: 631: 625: 619: 613: 607: 601: 592: 586: 499:fossil trackways 465:upper Cretaceous 461:lower Cretaceous 453:Mojado Formation 358: 349: 348: 342: 330: 321: 320: 314: 258: 256: 255: 229: 228: 226: 225: 224: 219: 215: 212: 211: 210: 207: 153:Gallup Sandstone 106: 36: 21: 20: 1037: 1036: 1032: 1031: 1030: 1028: 1027: 1026: 1022:Santonian Stage 1017:Coniacian Stage 992: 991: 985: 963: 961: 949: 912: 910: 883: 881: 869: 825: 823: 800: 798: 779: 777: 766: 758: 753: 752: 744: 740: 732: 728: 720: 716: 706: 704: 689: 685: 677: 673: 665: 661: 638: 634: 626: 622: 614: 610: 602: 595: 587: 578: 573: 554: 546: 537: 517: 497:. Two dinosaur 473: 397: 362: 361: 360: 359: 356: 355: 352: 351: 350: 333: 332: 331: 328: 327: 324: 323: 322: 284:Crevasse Canyon 253: 251: 222: 220: 216: 213: 208: 205: 203: 201: 200: 125:Mesaverde Group 105: 104: 103: 102: 97: 92: 87: 82: 77: 72: 67: 62: 57: 52: 47: 42: 34: 33: 19: 12: 11: 5: 1035: 1025: 1024: 1019: 1014: 1009: 1004: 990: 989: 983: 975:The dinosauria 970: 942: 937:10.3133/pp521E 919: 890: 862: 850:10.1086/664714 844:(4): 412–428. 832: 807: 786: 757: 754: 751: 750: 738: 726: 714: 683: 671: 659: 632: 620: 608: 593: 575: 574: 572: 569: 568: 567: 566: 565: 553: 550: 545: 542: 536: 533: 516: 513: 509:Petrified wood 472: 471:Fossil content 469: 396: 393: 364: 363: 353: 344: 343: 337: 336: 335: 334: 325: 316: 315: 309: 308: 307: 306: 305: 302: 301: 298: 294: 293: 292:Allen and Balk 290: 286: 285: 282: 278: 277: 273: 272: 270:San Juan Basin 267: 263: 262: 249: 245: 244: 235: 231: 230: 198: 192: 191: 187: 186: 173: 169: 168: 164: 163: 160: 156: 155: 150: 146: 145: 140: 136: 135: 132: 128: 127: 122: 118: 117: 112: 108: 107: 100: 99: 98: 93: 88: 83: 78: 73: 68: 63: 58: 53: 48: 43: 38: 26: 25: 17: 9: 6: 4: 3: 2: 1034: 1023: 1020: 1018: 1015: 1013: 1010: 1008: 1005: 1003: 1000: 999: 997: 986: 984:0-520-24209-2 980: 976: 971: 959: 955: 948: 943: 938: 933: 929: 925: 920: 908: 904: 900: 896: 891: 879: 875: 868: 863: 859: 855: 851: 847: 843: 839: 833: 821: 817: 813: 808: 796: 792: 787: 776: 772: 765: 760: 759: 747: 742: 735: 730: 723: 718: 702: 698: 694: 687: 680: 675: 668: 663: 655: 651: 647: 643: 636: 629: 624: 617: 612: 605: 600: 598: 590: 585: 583: 581: 576: 564: 561: 560: 559: 556: 555: 549: 541: 532: 530: 526: 522: 512: 510: 506: 504: 500: 496: 492: 488: 486: 481: 477: 468: 466: 462: 458: 454: 450: 446: 442: 437: 433: 431: 426: 422: 418: 414: 410: 406: 402: 392: 390: 386: 382: 379: 375: 371: 341: 313: 303: 299: 295: 291: 287: 283: 279: 274: 271: 268: 264: 261: 260:United States 250: 246: 243: 239: 236: 232: 227: 199: 197: 193: 188: 185: 181: 177: 174: 170: 165: 161: 157: 154: 151: 147: 144: 141: 137: 133: 129: 126: 123: 119: 116: 113: 109: 96: 91: 86: 81: 76: 71: 66: 61: 56: 51: 46: 41: 31: 27: 22: 16: 974: 964:11 September 962:. Retrieved 957: 953: 927: 911:. Retrieved 906: 902: 882:. Retrieved 877: 873: 841: 837: 824:. Retrieved 819: 815: 801:11 September 799:. Retrieved 794: 780:11 September 778:. Retrieved 774: 770: 756:Bibliography 746:Fassett 1989 741: 734:Tschudy 1976 729: 717: 705:. Retrieved 700: 696: 686: 674: 662: 645: 641: 635: 623: 611: 547: 538: 518: 507: 483: 474: 438: 434: 430:cross-bedded 408: 404: 400: 398: 369: 367: 297:Year defined 276:Type section 15: 884:1 September 822:(2): 99–102 797:. OF-GM 212 707:1 September 628:Correa 1970 604:Cather 2010 485:Neurankylus 449:inceptisols 425:crossbedded 395:Description 221: / 209:108°56′41″W 196:Coordinates 996:Categories 571:References 529:palynology 385:New Mexico 378:Cretaceous 238:New Mexico 206:35°47′30″N 913:31 August 909:: 117–119 880:: 303–307 826:31 August 703:: 151–152 525:Santonian 521:Coniacian 457:aridisols 441:paleosols 417:sandstone 376:-bearing 281:Named for 176:Sandstone 167:Lithology 159:Thickness 139:Underlies 131:Sub-units 115:Formation 35:Santonian 897:(2016). 858:83998771 552:See also 476:Dinosaur 413:mudstone 289:Named by 190:Location 180:mudstone 149:Overlies 960:: 48–55 445:alfisol 389:Arizona 248:Country 242:Arizona 172:Primary 121:Unit of 101:↓ 981:  856:  491:baenid 419:, and 407:, and 266:Extent 257:  234:Region 950:(PDF) 870:(PDF) 854:S2CID 767:(PDF) 495:genus 487:notos 480:genus 372:is a 979:ISBN 966:2020 915:2021 886:2021 828:2021 803:2020 782:2020 709:2021 523:and 489:, a 447:and 421:coal 387:and 374:coal 368:The 300:1954 184:coal 111:Type 40:Preęž’ 958:154 932:doi 846:doi 842:173 650:doi 527:by 515:Age 383:in 998:: 956:. 952:. 926:. 907:74 905:. 901:. 878:40 876:. 872:. 852:. 840:. 818:. 814:. 793:. 775:36 773:. 769:. 701:74 699:. 695:. 648:. 646:62 644:. 596:^ 579:^ 505:. 463:- 403:, 391:. 240:, 182:, 178:, 90:Pg 32:: 987:. 968:. 940:. 934:: 917:. 888:. 860:. 848:: 830:. 820:7 805:. 784:. 748:. 736:. 724:. 711:. 681:. 656:. 652:: 630:. 618:. 606:. 591:. 95:N 85:K 80:J 75:T 70:P 65:C 60:D 55:S 50:O 45:ęž’

Index

Stratigraphic range
Preęž’
ęž’
O
S
D
C
P
T
J
K
Pg
N
Formation
Mesaverde Group
Point Lookout Sandstone
Gallup Sandstone
Sandstone
mudstone
coal
Coordinates
35°47′30″N 108°56′41″W / 35.7916°N 108.9446°W / 35.7916; -108.9446
New Mexico
Arizona
United States
San Juan Basin
Crevasse Canyon Formation is located in the United States
Crevasse Canyon Formation is located in New Mexico
coal
Cretaceous

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