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La Veta Pass

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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1959
AAPG Bulletin (1959) 43 (8): 1896–1939.
...Dudley W. Bolyard ABSTRACT Structurally complex Pennsylvanian and Permian strata comprise the bulk of the Sangre de Cristo Range between La Veta Pass and Westcliffe in south-central Colorado. They are at least 14,000 feet thick near Crestone in the northern part of the area, and more than 9,000...
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—Correlation of Madera formation between La Veta Pass and Whiskey Creek Pass (Brill, 1952) based on patterns of clastic ratio values.
Published: 01 August 1959
Fig. 9. —Correlation of Madera formation between La Veta Pass and Whiskey Creek Pass ( Brill, 1952 ) based on patterns of clastic ratio values.
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(a) Generalized geologic map of the northern Sangre de Cristo Mountains and surrounding region. The Sangre de Cristo Mountains are a horst block bounded by the Rio Grande rift graben of the San Luis Valley on the west and Wet Mountain Valley on the east (Lindsey et al., 1983). Note location of measured sections of the Minturn Formation discussed in the text. Measured section location abbreviations: I-70 = Interstate 70; SV = Swissvale; LVP = La Veta Pass. (b) Detailed geologic map of the Sangre de Cristo Mountains. Location of map is shown by dashed box in (a). Note the location of measured sections of the Minturn Formation discussed in the text. Measured section location abbreviations: HP = Hermit Peak; MP = Milwaukee Peak.
Published: 01 July 2003
location of measured sections of the Minturn Formation discussed in the text. Measured section location abbreviations: I-70 = Interstate 70; SV = Swissvale; LVP = La Veta Pass. (b) Detailed geologic map of the Sangre de Cristo Mountains. Location of map is shown by dashed box in (a). Note the location
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Measured stratigraphic sections of river-delta deposits of the Minturn Formation. See Figure 3a for measured section locations and Figure 2 key for lithologic patterns. Circles and arrows point to representative lithofacies as described in Table 1. Black arrows denote paleocurrent direction based on trough cross-stratification with north oriented to the top of the page. (a) Measured section of proximal river-delta deposits of the Minturn Formation at the town of Swissvale along the Arkansas River. Note the coarsening-upward packages (black triangles). (b) Measured section of proximal river-delta deposits of the Minturn Formation along Interstate 70 near the town of Minturn. Note the coarsening-upward packages (black triangles). (c) Measured section of distal river-delta deposits of the Minturn Formation at La Veta Pass in the southern part of the basin. Note that fining-upward packages (black triangles) characterize the distal deposits. Note the abundance of limestone in this section.
Published: 01 July 2003
river-delta deposits of the Minturn Formation along Interstate 70 near the town of Minturn. Note the coarsening-upward packages (black triangles). (c) Measured section of distal river-delta deposits of the Minturn Formation at La Veta Pass in the southern part of the basin. Note that fining-upward
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5402-X.357
EISBN: 9780813754086
... to the south flank of the Spanish Peaks is from Apishapa Pass, which can be reached by continuing from La Veta south on Colorado 111 about 16 mi (26 km) to Cucharas Pass. Turn left onto the Forest Service road to the northeast and drive about 6 mi (9.6 km) to the trail head at Apishapa Pass (closed...
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Figure 3. (A) Generalized geologic map of the northern Sangre de Cristo Mountains and surrounding region modified from Lindsey et al. (1983). The Sangre de Cristo Mountains are a horst bounded by the Rio Grande rift graben of the San Luis Valley on the west and by the Wet Mountain Valley on the east. The Raton basin is a Laramide basin that lay adjacent to the Laramide San Luis uplift (see text). Dashed gray boxes denote locations of Figures 3B and 14A. Circled numbers indicate locations of measured sections discussed in text. Minturn Formation measured sections: 1—Interstate 70, 2—Swissvale, 3—La Veta Pass. Sangre de Cristo Formation measured sections: 6—Badger Creek, 7—Pleasant Valley syncline, 8—Red Canyon, 9—Cuchara. (B) Detailed geologic map of the northern Sangre de Cristo Mountains modified from Lindsey et al. (1983); location is shown by dashed box in A. A–A′ marks location of cross section shown in Figure 12. B–B′ marks location of cross section shown in Figure 13. Dashed box outlines location of map shown in Figure 10. Circled numbers indicate locations of measured sections discussed in the text. Minturn Formation measured sections: 4—Hermit Peak, 5—Milwaukee Peak. Sangre de Cristo Formation measured sections: 10—Middle Taylor Creek, 11—North Fork, 12—Groundhog, 13—Humboldt Peak, 14—Blueberry Peak. Stratigraphic columns for measured sections not shown in Figures 4, 7, 8, and 9 can be found in Hoy (2000).
Published: 01 July 2002
—Swissvale, 3—La Veta Pass. Sangre de Cristo Formation measured sections: 6—Badger Creek, 7—Pleasant Valley syncline, 8—Red Canyon, 9—Cuchara. (B) Detailed geologic map of the northern Sangre de Cristo Mountains modified from Lindsey et al. (1983) ; location is shown by dashed box in A. A–A′ marks location
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Figure 6. Paleogeographic reconstructions depicting the Pennsylvanian–Permian evolution of the Central Colorado trough. (A) Middle Pennsylvanian marine-dominated deposition by fan-delta, fluvial-delta, and turbidite systems of the Minturn Formation. Measured section abbreviations: I-70—Inertate 70, SV—Swissvale, HP—Hermit Peak, MP—Milwaukee Peak, LVP—La Veta Pass. The Uncompahgre uplift provided most of the sediment along the western margin of the basin. Cross section shows the Sand Creek–Crestone thrust fault system and basin asymmetry. The Apishapa uplift is interpreted as a possible forebulge that defined the eastern margin of the basin. PC—Precambrian rocks, LPz—lower Paleozoic strata, 1Psc—Lower Sangre de Cristo Formation, 1Pm—Minturn Formation, 1Ps—undifferentianted Sangre de Cristo Formation. Triangles with double underlines represent sea level position. (B) Late Pennsylvanian–Permian deposition of the nonmarine Sangre de Cristo Formation was marked by development of an axial, north-flowing fluvial system. BC—Badger Creek, PV—Pleasant Valley syncline, MTC—Middle Taylor Creek, NF—North Fork, GH—Groundhog, HU—Humboldt Peak, RC—Red Canyon, CUC—Cuchara. Note that shortening continued on the Sand Creek–Crestone thrust fault system. The Sand Creek–Crestone thrust fault tips were near the surface by this stage and produced the growth strata documented in the footwall of the thrust system (see text for discussion). Wavy lines on cross section in the Crestone Conglomerate Member represent angular unconformities in the Gibson Peak growth syncline.
Published: 01 July 2002
, SV—Swissvale, HP—Hermit Peak, MP—Milwaukee Peak, LVP—La Veta Pass. The Uncompahgre uplift provided most of the sediment along the western margin of the basin. Cross section shows the Sand Creek–Crestone thrust fault system and basin asymmetry. The Apishapa uplift is interpreted as a possible
Journal Article
Published: 01 May 2002
The Journal of Geology (2002) 110 (3): 305–324.
... This study Castle Creek (CC) … P.-L. Pm. 7 143.0 .4 9.6 41 5.5 7.7 This study La Veta Pass (LAV) … L. Pm. 17 152.7 −13.5 4.1 75 8.1 4.6 This study Indian Creek (IC) 37.6/105.2 L. Pm. 17 168.7 −12.0 4.3 126 30.2 3.0 This study Vail, Colorado (VL) 37.4/105.1 P.-Pm...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2003
AAPG Bulletin (2003) 87 (7): 1169–1191.
... location of measured sections of the Minturn Formation discussed in the text. Measured section location abbreviations: I-70 = Interstate 70; SV = Swissvale; LVP = La Veta Pass. (b) Detailed geologic map of the Sangre de Cristo Mountains. Location of map is shown by dashed box in (a). Note the location...
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Journal Article
Published: 01 March 2005
Journal of the Geological Society (2005) 162 (2): 273–287.
...-sedimentary breccias and conglomerates, which conformably overlies the Veta Negra Formation. Unlike that formation, the Las Chilcas Formation does not exhibit a widespread metamorphic mineralogy attributable to very low-grade metamorphism, although the coarse conglomerates contain abundant very low-grade...
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Journal Article
Published: 01 January 2009
Rocky Mountain Geology (2009) 44 (1): 17–32.
... of the initiation of the Rio Grande rift, as well as the petrogenetic relationship between alkaline and sub-alkaline rocks in relatively stable cratonic areas. UW Department of Geology and Geophysics 2009 An outcrop on the Andreatta Ranch, ∼10 km east-southeast of La Veta, Colorado and north of West Spanish...
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Journal Article
Published: 01 June 2012
Earthquake Spectra (2012) 28 (1_suppl1): 75–96.
... other tailings dams constructed using the upstream method experienced varying levels of seismically induced failure (i.e., Chancón, Bellavista Dike No. 1, Veta del Agua Dike No. 5, Alhué, and Las Palmas Dam; Ramirez 2010 ). The locations of all 13 tailings dams are shown in Figure 17 . Figure 17...
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Journal Article
Published: 01 October 2020
Earth Sciences History (2020) 39 (2): 262–290.
... Betriebs-Resultate der Silberbergwerke von Veta grande in der Provinz Zacatecas in Mexico. Archiv für Mineralogie, Geognosie, Bergbau und Hüttenkunde 6: 319–342. 21 1834 Boué, Ami Résumé des progrès des sciences geologiques pendant l’année 1833. Bulletin de la Sociéte Geologique de France 5: 1–4...
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Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1432–1455.
..., the Mount Veta block has been uplifted sufficiently to expose a ca. 68–66 Ma equigranular granitic pluton. Farther to the southeast, in the Kechumstuk block, the flat-lying outflow tuff remnant in Gold Creek and a regionally extensive high terrace indicate that the landscape there has been little modified...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1933
AAPG Bulletin (1933) 17 (2): 109–168.
... is equivalent in age to the Fountain at Chimney Hollow. At La Bonte, Wyoming, typical Fountain material has been replaced by sandstones and marine limestones of the Ingleside formation (upper Casper). 1 The Sangre de Cristo conglomerate of the Sangre de Cristo Mountains, exclusive of the basal Veta Pass...
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Journal Article
Published: 18 August 2001
Canadian Journal of Earth Sciences (2001) 38 (8): 1191–1204.
... metamorphosed to augen gneiss. Corresponding author (e-mail: [email protected] ). 23 6 2000 29 1 2001 © 2001 NRC Canada 2001 Nous présentons une étude de datation de l’apatite par la méthode des traces de fission (AFT) pour cinq roches plutoniques et sept roches métamorphiques...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2002
GSA Bulletin (2002) 114 (7): 804–828.
...—Swissvale, 3—La Veta Pass. Sangre de Cristo Formation measured sections: 6—Badger Creek, 7—Pleasant Valley syncline, 8—Red Canyon, 9—Cuchara. (B) Detailed geologic map of the northern Sangre de Cristo Mountains modified from Lindsey et al. (1983) ; location is shown by dashed box in A. A–A′ marks location...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1957
AAPG Bulletin (1957) 41 (5): 953–956.
.... , AND STEPHENS , J. G. , 1954 , “ Geology of the La Veta Area, Huerfano County, Colorado ,” ibid., Map OM-146 , Oil and Gas Inv. Ser. READ , C. B. , WILPOLT , R. H. , ANDREWS , D. A. , SUMMERSON , C. H. , AND WOOD , G. H. , 1944 , “ Geologic Map and Stratigraphic Sections...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2016
GSA Bulletin (2016) 128 (3-4): 397–424.
... Mosca Pass, Blanca Peak, La Veta Pass, and the Culebra Range are consistent with this, and they indicate rapid cooling younger than ca. 27 Ma. The only thermal history model that indicates possible cooling to near-surface temperatures prior than ca. 27 Ma is sample 11, which only incorporates AHe data...
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Journal Article
Journal: Economic Geology
Published: 01 May 2018
Economic Geology (2018) 113 (3): 553–578.
... batholith. Radiometric ages gradually pass to Jurassic (174–162 Ma) at the latitude of the town of Cajamarca. In the western areas close to the crest of the Central Cordillera (La Línea ridge) the youngest ages have been found from 138 to 99 Ma. Although the Romeral fault system, with the San Jeronimo fault...
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