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Stratigraphy of the John Henry Member of the Straight Cliffs Formation (modified from Gooley et al. 2016). The first to third column from the left show the southwest–northeast transition from fluvial deposition in Rock House Cove and Bull Canyon to marginal marine deposition in Rogers Canyon and Left Hand Collet (locations shown in Fig. 1). DU-0 to DU-6: depositional units.

Stratigraphy of the John Henry Member of the Straight Cliffs Formation (mod... Available to Purchase

Published: 01 November 2016
Fig. 2.— Stratigraphy of the John Henry Member of the Straight Cliffs Formation (modified from Gooley et al. 2016 ). The first to third column from the left show the southwest–northeast transition from fluvial deposition in Rock House Cove and Bull Canyon to marginal marine deposition in Rogers
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Simplified stratigraphic architecture of the John Henry Member at Rock House Cove and Bull Canyon relative to Kelly Grade (Gallin et al. 2010) and Rogers Canyon (Allen and Johnson 2010). Line of section is shown on Figure 1. Dashed lines represent possible down-dip correlations for the John Henry Member. Red and blue triangles indicate apparent trends in increasing (blue) versus decreasing (red) ratio of accommodation to sediment supply (A/S), as discussed in the text.

Simplified stratigraphic architecture of the John Henry Member at Rock Hous... Available to Purchase

Published: 01 March 2016
Fig. 12.— Simplified stratigraphic architecture of the John Henry Member at Rock House Cove and Bull Canyon relative to Kelly Grade ( Gallin et al. 2010 ) and Rogers Canyon ( Allen and Johnson 2010 ). Line of section is shown on Figure 1. Dashed lines represent possible down-dip correlations
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Stratigraphic summary chart of the Turonian–Campanian Straight Cliffs Formation, including previous lithostratigraphic and sequence stratigraphic interpretations. Seven marine sandstone packages, named A–G by Peterson (1969a), pinch out landward into coal zones and coastal-plain facies. Relative shoreline movements are based on shoreface pinchouts and marginal marine facies distributions at Left Hand Collet (Dooling 2013) and Rogers Canyon (Allen and Johnson 2011).

Stratigraphic summary chart of the Turonian–Campanian Straight Cliffs Forma... Available to Purchase

Published: 01 October 2015
. Relative shoreline movements are based on shoreface pinchouts and marginal marine facies distributions at Left Hand Collet ( Dooling 2013 ) and Rogers Canyon ( Allen and Johnson 2011 ).
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Upper Cretaceous stratigraphy of south-central Utah. Columns 1–3 on left: Lithostratigraphy of the Straight Cliffs Formation showing the southwest–northeast transition from fluvial deposition (Rock House Cove and Bull Canyon) to tidal, estuarine (Kelly Grade), and marginal marine deposition (Rogers Canyon and Left Hand Collect). DU-0 to DU-6: depositional units. Column 4: Inferred trajectory of John Henry Member shoreline with time (Allen and Johnson 2011; Chentnik et al. 2015). Column 5: Sequence stratigraphy as interpreted by Shanley and McCabe (1991). Column 6: Lithostratigraphy of Kaiparowits Plateau (Peterson 1969a, 1969b; Peterson and Kirk 1977; Hettinger et al. 1993). Figure is modified from Hettinger (1995); timescale is from Gradstein et al. (2012); stratigraphic divisions are from Szwarc et al. (2015).

Upper Cretaceous stratigraphy of south-central Utah. Columns 1–3 on left: L... Available to Purchase

Published: 01 March 2016
deposition (Rogers Canyon and Left Hand Collect). DU-0 to DU-6: depositional units. Column 4: Inferred trajectory of John Henry Member shoreline with time ( Allen and Johnson 2011 ; Chentnik et al. 2015 ). Column 5: Sequence stratigraphy as interpreted by Shanley and McCabe (1991) . Column 6
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Inset map shows present day location of the Southwestern High Plateaus (SWHP) in Utah including relevant structures from Late Cretaceous to Cenozoic time. WIS—Western Interior Seaway; AZ—Arizona; CA—California; CO—Colorado; NM—New Mexico; NV—Nevada; UT—Utah; WY—Wyoming. Main map of the study area shows the locations of measured sections and relevant stratigraphy across the SWHP. Sections of the Straight Cliffs and Iron Springs Formations completed for this study are shown in orange. Generic lithologies are represented by brick (mixed limestone and sandstone) and stippled (dominantly sandstone) patterns; non-stippled is a mixture of mudstone and sandstone lithologies. Sections from this study (orange) and previous studies include: (1) Pine Valley Mountains (Cook, 1957); (2) Parowan Gap west of the SWHP; (3) Parowan Canyon; (4) Cedar Canyon (Eaton et al., 2001); (5) Orderville Gulch in the Markagunt Plateau; (6) Glendale and (7) Tenny Canyon (Tilton, 1991); (8, 9) Willis Creek and Heward Creek from the Paunsaugunt Plateau; and (10) Shakespeare Mine from the northern Kaiparowits Plateau. Previously measured sections in the Kaiparowits Plateau include: (11) Buck Hollow (Mulhern and Johnson, 2016); (12) Main Canyon (Chentnik et al., 2015); (13) Left Hand Collet (Dooling, 2013); (14) Rogers Canyon (Allen and Johnson, 2010); (15) Kelly Grade (Gallin et al., 2010); (16) Tibbet Canyon (Peterson, 1969); (17) Bull Canyon (Gooley et al., 2016); and (18) Rock House Cove (Gooley et al., 2016).

Inset map shows present day location of the Southwestern High Plateaus (SWH... Open Access

Published: 28 May 2021
, 2016 ); (12) Main Canyon ( Chentnik et al., 2015 ); (13) Left Hand Collet ( Dooling, 2013 ); (14) Rogers Canyon ( Allen and Johnson, 2010 ); (15) Kelly Grade ( Gallin et al., 2010 ); (16) Tibbet Canyon ( Peterson, 1969 ); (17) Bull Canyon ( Gooley et al., 2016 ); and (18) Rock House Cove ( Gooley et al
Journal Article

Developments in North-Central and West-Central Texas, 1938 Available to Purchase

J. J. Maucini
Journal: AAPG Bulletin
Published: 01 June 1939
AAPG Bulletin (1939) 23 (6): 844–859.
DOI: https://doi.org/10.1306/3D9330C6-16B1-11D7-8645000102C1865D
...J. J. Maucini ABSTRACT New developments and discoveries in north-central Texas during 1938 have materially increased the importance of the Strawn formations as major producing zones in the north-central district and have increased the scope of the Canyon and Cisco in the west-central. The most...
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Journal Article

Late Neogene–Quaternary tephrochronology, stratigraphy, and paleoclimate of Death Valley, California, USA Available to Purchase

Jeffrey R. Knott, Michael N. Machette, Elmira Wan, Ralph E. Klinger, Joseph C. Liddicoat, Andrei M. Sarna-Wojcicki, Robert J. Fleck, Alan L. Deino, John W. Geissman, Janet L. Slate, David B. Wahl, Brian P. Wernicke, Stephen G. Wells, John C. Tinsley, III, Jeffrey C. Hathaway, Veva M. Weamer
Journal: GSA Bulletin
Published: 02 January 2018
GSA Bulletin (2018) 130 (7-8): 1231–1255.
DOI: https://doi.org/10.1130/B31690.1
... (CH), Copper Canyon (CC), Furnace Creek Basin (FC), Kit Fox Hills (KFH), Lake Rogers (LR), Mormon Point (MP), Natural Bridge (NaB), Northern Confidence Hills (NCH), Nova Basin (NoB), and Nova Formation (NF). The box on the right shows the correlation to the lower KM-3 core in Searles Valley; unc...
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View PDF for article title, Late Neogene–Quaternary tephrochronology, stratigraphy, and paleoclimate of Death Valley, California, USA
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Journal Article

Recently Described “Bisbeeite” from the Grand Canyon is Cyanotrichite Available to Purchase

Samuel G. Gordon
Published: 01 May 1923
American Mineralogist (1923) 8 (5): 92–93.
...Samuel G. Gordon Abstract In a recent paper in this journal 1 entitled “The Optical Properties and Morphology of Bisbeeite,” Professor Austin F. Rogers described a blue mineral, occurring as minute fibrous spherulites in the Grandview mine, Grand Canyon, Arizona. His identification of the material...
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Total alkalies–silica diagram for the tuffs of Ryecroft Canyon, Pott Hole Valley, and Orange Lichen Creek. The Orange Lichen Creek includes one sample of the correlative tuff of Kiln Canyon of Quinlivan and Rogers (1974). UY and LY indicate upper and lower tuffs, respectively, of the Ryecroft Canyon; a possible correlative of the upper tuff is uy.

Total alkalies–silica diagram for the tuffs of Ryecroft Canyon, Pott Hole V... Open Access

Published: 01 December 2013
Figure 37. Total alkalies–silica diagram for the tuffs of Ryecroft Canyon, Pott Hole Valley, and Orange Lichen Creek. The Orange Lichen Creek includes one sample of the correlative tuff of Kiln Canyon of Quinlivan and Rogers (1974) . UY and LY indicate upper and lower tuffs, respectively
Journal Article

Paleozoic Stratigraphy of Part of Northwestern Arizona Available to Purchase

Andrew H. McNair
Journal: AAPG Bulletin
Published: 01 March 1951
AAPG Bulletin (1951) 35 (3): 503–541.
DOI: https://doi.org/10.1306/3D9341D5-16B1-11D7-8645000102C1865D
... limestone series across the area. In the southeast the Martin truncates the Middle Cambrian Tapeats sandstone and contains basal clastic beds. In the western Grand Canyon area the Martin limestone contains soft, argillaceous limestone beds of Temple Butte lithologic character. The Rogers Spring and Redwall...
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Late Neogene and Quaternary tephra layers of Death Valley. Solid lines mean the tephra layer was found in the section; dashed lines indicate the stratigraphic location of the tephra layer, but that the layer was not found. Ages on the magnetic polarity time scale (MPTS) are Ma (Ogg, 2012). Section locations are Artists Drive (AD), Amargosa River (AR), Confidence Hills (CH), Copper Canyon (CC), Furnace Creek Basin (FC), Kit Fox Hills (KFH), Lake Rogers (LR), Mormon Point (MP), Natural Bridge (NaB), Northern Confidence Hills (NCH), Nova Basin (NoB), and Nova Formation (NF). The box on the right shows the correlation to the lower KM-3 core in Searles Valley; unc.—unconformity.

Late Neogene and Quaternary tephra layers of Death Valley. Solid lines mean... Available to Purchase

Published: 02 January 2018
, 2012 ). Section locations are Artists Drive (AD), Amargosa River (AR), Confidence Hills (CH), Copper Canyon (CC), Furnace Creek Basin (FC), Kit Fox Hills (KFH), Lake Rogers (LR), Mormon Point (MP), Natural Bridge (NaB), Northern Confidence Hills (NCH), Nova Basin (NoB), and Nova Formation (NF). The box
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Figure 3. Generalized geologic map of the Borrego Badlands and surrounding areas. ECMF—East Coyote Mountain fault; IPF—Inspiration Point fault; SFA—San Felipe anticline; WCMF—West Coyote Mountain fault; WSDF—West Salton detachment fault (after Axen and Fletcher, 1998). Labeled dots show location of measured sections (see Figs. 4 and 7). Adapted from Rogers (1965), Dorsey (2002), Ryter (2002), Lutz (2005), Steely (2006). AO—Arroyo Otro; BW—Beckman Wash; FP—Fonts Point; FW—Fault Wash; HC—Hidden Canyon; IP—Inspiration Point; PH—Painted Hill; PV—Palo Verde Wash; VE—Valle Escondido; VM—Vista del Malpais; SST—sandstone; metasedim. rx—metasedimentary rocks.

Figure 3. Generalized geologic map of the Borrego Badlands and surrounding ... Available to Purchase

Published: 01 November 2006
of measured sections (see Figs. 4 and 7 ). Adapted from Rogers (1965) , Dorsey (2002) , Ryter (2002) , Lutz (2005) , Steely (2006) . AO—Arroyo Otro; BW—Beckman Wash; FP—Fonts Point; FW—Fault Wash; HC—Hidden Canyon; IP—Inspiration Point; PH—Painted Hill; PV—Palo Verde Wash; VE—Valle Escondido; VM—Vista
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Structure contour map of the weathered erosion surface in the San Jacinto Mountains (SJM), Little San Bernardino Mountains, and southern San Bernardino Mountains. Contour interval is 200 m. Thick dashed gray line indicates the axes of the SJM and Santa Rosa Mountains (SRM), respectively. Thin dashed lines are selected faults (Rogers, 1965) that seem to disrupt contours. Dashed line labeled “cSB edge?” marks the proposed northern limit to the tilted central Salton block at about the location of Point Happy (location shown on Figure 14) as proposed by Dorsey and Langenheim (2015). Areas 1–3 are locations discussed in the text. White dashed lines illustrate directions along which mean surface gradients have been estimated (values shown). DC—Deep Canyon; MM—Martinez Mountain; PVF—Pinyon and Vandeventer flats; SB—Salton block (Dorsey and Langenheim, 2015).

Structure contour map of the weathered erosion surface in the San Jacinto M... Open Access

Published: 19 March 2020
), respectively. Thin dashed lines are selected faults ( Rogers, 1965 ) that seem to disrupt contours. Dashed line labeled “cSB edge?” marks the proposed northern limit to the tilted central Salton block at about the location of Point Happy (location shown on Figure 14 ) as proposed by Dorsey and Langenheim
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(A) Digital elevation model of the Lake Mead region, showing distribution of late Miocene limestone and gypsum, as well as major faults (compiled from Faulds et al., 2001c; Page et al., 2005; Beard et al., 2007; Felger and Beard, 2010). Basement depth contours are shown for major basins and based on inversion of gravity data (modified slightly from Langenheim et al., 2001a, 2010). Abbreviations for physiographic features and towns (black text): BC—Black Canyon; BGL—Big Gypsum Ledges; CR—Colorado River; DS—Dolan Springs; FM—Frenchman Mountain; GM—Grapevine Mesa; ML—Mohave Lake; NM—Nevershine Mesa; SnP—Snap Point; SP—Sandy Point; WR—Wheeler Ridge. Abbreviations for faults (red text): BGf—Blind Goddess Mine fault; BHf—Bitter Ridge-Hamblin Bay fault; CMf—Cerbat Mountains fault; CWf—California Wash fault; Df—Detrital fault; Ff—Frenchman Mountain fault; HRf—Hen Springs–Rogers Springs fault; LBf—Lost Basin Range fault; LVsz—Las Vegas Valley shear zone; MMf—Mockingbird Mine fault; MSf—Meadview Slope fault; NGf—northern Grand Wash fault; Pf—Piedmont fault; SGf—southern Grand Wash fault; SIf—Saddle Island detachment fault; SWf—South Virgin–White Hills detachment fault; Wf—Wheeler Ridge fault. The Lake Mead fault system includes the Bitter Ridge–Hamblin Bay and Hen Springs–Rogers Springs faults, as well as east-northeast–striking sinistral faults to the southwest and northeast in southern Nevada. (B) Digital elevation model showing outlines of late Miocene lakes (Lakes Grand Wash, Hualapai, and Las Vegas), as adapted and in some cases modified (see discussion in text) from House et al. (2008) and Spencer et al. (2013). Each subsequent lake probably filled at least the lower parts of the older lake basins. Known thick (&gt;200 m), subsurface halite (red dashed lines) and potentially thick subsurface halite deposits (green dashed lines) are also shown.

(A) Digital elevation model of the Lake Mead region, showing distribution o... Open Access

Published: 01 June 2016
for major basins and based on inversion of gravity data (modified slightly from Langenheim et al., 2001a , 2010 ). Abbreviations for physiographic features and towns (black text): BC—Black Canyon; BGL—Big Gypsum Ledges; CR—Colorado River; DS—Dolan Springs; FM—Frenchman Mountain; GM—Grapevine Mesa; ML
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Important structural features of southern California and the nature of the basal contact of the Ocotillo Formation in the western Salton Trough. Faults of the San Felipe fault zone (SFFZ) are red. Note that the West Salton low-angle fault is folded and cut by dextral strike-slip fault zones at Yaqui Ridge. Light Green denotes a part of the West Salton detachment fault that is still active within the dextral fault system to the south. Faults are compiled and modified from Rogers (1965); Jennings (1977); Kennedy and Morton (1993); Kirby (2005); Lutz (2005); Kennedy (2000, 2003;) and this study. BB—Borrego Badlands; BM—Borrego Mountain; BRF—Buck Ridge fault; CCF—Coyote Creek fault; CF—Clark fault; EVFZ—Earthquake Valley fault zone; FCM—Fish Creek Mountains; FCMF—Fish Creek Mountains fault; GC—Grapevine Canyon; OB—Ocotillo Badlands; PR—Pinyon Ridge; SC—Sunset Conglomerate of the Ocotillo Formation (pink); SF—Sunset fault; SFF—San Felipe fault; SFBB—San Felipe-Borrego subbasin; SM—Superstition Mountain; VFCB—Vallecito–Fish Creek subbasin; VM—Vallecito Mountains; WP—Whale Peak; WSDF—West Salton detachment fault; WSFH—western San Felipe Hills; YR—Yaqui Ridge.

Important structural features of southern California and the nature of the ... Available to Purchase

Published: 01 May 2009
zones at Yaqui Ridge. Light Green denotes a part of the West Salton detachment fault that is still active within the dextral fault system to the south. Faults are compiled and modified from Rogers (1965) ; Jennings (1977) ; Kennedy and Morton (1993); Kirby (2005) ; Lutz (2005) ; Kennedy (2000
Journal Article

A New Look at Landslides of the Vermilion and Echo Cliffs, Northern Arizona Available to Purchase

Conor M. Watkins, J. David Rogers
Published: 22 April 2022
Environmental & Engineering Geoscience (2022) 28 (2): 173–192.
DOI: https://doi.org/10.2113/EEG-D-21-00063
..., and the mouth of Paria Canyon, shown in Figure 15 . The ponding of so much water against these cliffs would have saturated the Chinle Formation within just a few years, hastening loss of cohesion and triggering a successive series of slides through simple strain softening ( Trollope, 1969 , 1973 ; Rogers...
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Lapis Lazuli from San Bernardino County, California Available to Purchase

Austin F. Rogers
Published: 01 February 1938
American Mineralogist (1938) 23 (2): 111–114.
...Austin F. Rogers Abstract So far as known there is only one locality for lapis lazuli in the whole continent of North America. This locality is in San Bernardino County, California, on the north slope of the south fork of Cascade Canyon, which is a branch of San Antonio Canyon and distant about...
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Conceptual Models of Vadose Zone Flow and Transport beneath the Pajarito Plateau, Los Alamos, New Mexico Available to Purchase

Kay H. Birdsell, Brent D. Newman, David E. Broxton, Bruce A. Robinson
Published: 01 August 2005
Vadose Zone Journal (2005) 4 (3): 620–636.
DOI: https://doi.org/10.2136/vzj2004.0172
... flow and transport beneath the Pajarito Plateau identify wet canyons as being hydrologically different from dry canyons and dry mesas ( LANL, 1998a ; Rogers et al., 1996 ; Neeper and Gilkeson, 1996 ; Turin and Rosenberg, 1996 ; Birdsell et al., 2000 ). Table 1 shows a compilation of infiltration...
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Development of an Infiltration Map for the Los Alamos Area, New Mexico Available to Purchase

Edward Kwicklis, Marc Witkowski, Kay Birdsell, Brent Newman, Douglas Walther
Published: 01 August 2005
Vadose Zone Journal (2005) 4 (3): 672–693.
DOI: https://doi.org/10.2136/vzj2004.0176
... equation 2 (−0.22–2) Rogers et al. (1996a) flux is upward in 7.6–13.7 m depth POTO-4A Potrillo Canyon C Richards equation 0.12 (–) Rogers et al. (1996a) well referred to as PC-4 by Rogers et al. (1996a) MCM-5.1 Mortandad Canyon C Richards equation 1.5 (–) Rogers et al. (1996a...
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View PDF for article title, Development of an Infiltration Map for the Los Alamos Area, New Mexico
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Journal Article

Geology of Scipio Pass Quadrangle, Millard County, Utah: ABSTRACT Free

Roger Michaels
Journal: AAPG Bulletin
Published: 01 July 1984
AAPG Bulletin (1984) 68 (7): 942–943.
DOI: https://doi.org/10.1306/AD461575-16F7-11D7-8645000102C1865D
...Roger Michaels ABSTRACT The Scipio Pass quadrangle is comprised of three separate packages of stratigraphy: (1) the Canyon Range Precambrian and Cambrian allochthonous section, (2) the Pavant allochthon of Paleozoic carbonates and quartzites, and (3) a thick Cretaceous to Quaternary blanket...
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