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Hindu Springs Fault

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Journal Article
Journal: Geosphere
Published: 01 August 2014
Geosphere (2014) 10 (4): 664–679.
... include the L-shaped Milkweed-Hindu channel on the central Hualapai Plateau and Peach Springs Canyon, the trunk valley coincident with the Hurricane fault ( Young, 1966 , 1979 , 1982 , 2001a ). The paleocanyons preserve the greatest buried relief at the plateau margin, 1200 m near Truxton, Arizona...
FIGURES
First thumbnail for: Paleogene Grand Canyon incompatible with Tertiary ...
Second thumbnail for: Paleogene Grand Canyon incompatible with Tertiary ...
Third thumbnail for: Paleogene Grand Canyon incompatible with Tertiary ...
Image
Cross section through the western Grand Canyon region showing geometric relationships between various geomorphic and geologic features discussed in text (based on Young, 1982). Xg—Proterozoic crystalline basement; D—Cambrian and Devonian strata; MP—Mississippian to Permian strata; Pk—Permian Kaibab Formation; Tb—8 Ma Shivwits basalts. Vertical arrows show measurements of elevation differences discussed in text. Hindu Canyon channel depicted assuming present minimum elevation of Rim gravel deposits in Peach Springs Wash (1000 m) has not been modified by faulting (see text for discussion).
Published: 01 July 2011
—Permian Kaibab Formation; Tb—8 Ma Shivwits basalts. Vertical arrows show measurements of elevation differences discussed in text. Hindu Canyon channel depicted assuming present minimum elevation of Rim gravel deposits in Peach Springs Wash (1000 m) has not been modified by faulting (see text
Image
View of light-colored Kaibab, Toroweap, and Coconino formations capping Supai Group red beds near Toroweap overlook, east of the Hurricane fault. Dissected, light-colored alluvial fans probably were more active during the Pleistocene, and their significant dispersal distance demonstrates why the Hindu Fanglomerate contains light-colored clasts derived from the Shivwits Plateau scarp at locations well south of modern Grand Canyon on the Hualapai Plateau. Lower, light-colored ledge (L) in the center left of view is within the normally red, upper Esplanade Sandstone, which becomes locally bleached by groundwater due to increased fracturing near major fault zones and breccia pipes. The Esplanade Sandstone crops out only north of the modern gorge on the Hualapai Plateau west of Peach Springs Canyon. Scale: thickness of stratigraphic section from Layer L to top of center horizon is 425 m.
Published: 01 August 2014
locally bleached by groundwater due to increased fracturing near major fault zones and breccia pipes. The Esplanade Sandstone crops out only north of the modern gorge on the Hualapai Plateau west of Peach Springs Canyon. Scale: thickness of stratigraphic section from Layer L to top of center horizon
Journal Article
Published: 01 August 2002
Bulletin of the Seismological Society of America (2002) 92 (6): 2061–2079.
... Koyna, Maharashtra 17.398 73.767 3-4 Felt for “around 40 sec.” Sandhyanand Kuda, Gujarat 23.113 71.385 8 New springs Times of India Kumbakakonam, Tamil Nadu 10.961 79.182 4-5 People ran, strongly felt The Hindu Lahore, Punjab (Pakistan) 31.542 74.399 4-5 Reported...
FIGURES
First thumbnail for: The 26 January 2001 M 7.6 Bhuj, India, Earthquake:...
Second thumbnail for: The 26 January 2001 M 7.6 Bhuj, India, Earthquake:...
Third thumbnail for: The 26 January 2001 M 7.6 Bhuj, India, Earthquake:...
Journal Article
Published: 01 December 1989
Journal of the Geological Society (1989) 146 (6): 1003–1016.
...R. C. LEAKE; C. J. N. FLETCHER; H. W. HASLAM; B. KHAN; SHAKIRULLAH Abstract Stratabound scheelite mineralization has been discovered in the Hindu Kush range of northern Pakistan as a result of a geochemical drainage survey. The mineralization occurs predominantly in clinozoisite-bearing...
Journal Article
Published: 09 May 2022
Quarterly Journal of Engineering Geology and Hydrogeology (2022) 55 (3): qjegh2021-189.
...Norman Woods; Mohammad Karimi; Ibrahim Jafari; Richard Hinchliffe Abstract The present road over the Hindu Kush Mountain Range via the Salang Pass (termed the Salang Corridor) links the south of Afghanistan, including the capital Kabul, with northern Afghanistan and Central Asia. It is the only...
FIGURES
First thumbnail for: Geological and geotechnical investigations for the...
Second thumbnail for: Geological and geotechnical investigations for the...
Third thumbnail for: Geological and geotechnical investigations for the...
Journal Article
Journal: Geology
Published: 01 July 2001
Geology (2001) 29 (7): 651–654.
... in orogenic belts ( Edwards et al., 2000 ; Schneider et al., 1999 ). A cluster of seismicity associated with the Tato hot springs included a swarm of 26 events in a 24 h period. When relocated using cross-correlation techniques, hypocenters locate within ±50 m of each other and define a fault plane that may...
FIGURES
First thumbnail for: Seismic characterization of an active metamorphic ...
Second thumbnail for: Seismic characterization of an active metamorphic ...
Third thumbnail for: Seismic characterization of an active metamorphic ...
Journal Article
Journal: Geosphere
Published: 01 October 2014
Geosphere (2014) 10 (5): 870–891.
... the Milkweed, Hindu, and Peach Springs paleocanyons are the stratigraphic equivalent of Koons’ (1948a , 1948b ) Blue Mountain gravel, but are located on the opposite side of the Hurricane fault ( Young, 1966 , 1999 ). The upper Peach Springs Canyon (Peach Springs Wash) Tertiary section is similar...
FIGURES
First thumbnail for: Paleogene rim gravel of Arizona: Age and significa...
Second thumbnail for: Paleogene rim gravel of Arizona: Age and significa...
Third thumbnail for: Paleogene rim gravel of Arizona: Age and significa...
Journal Article
Published: 01 September 2021
Jour. Geol. Soc. India (2021) 97 (9): 975–979.
... in Himalaya are known to be triggered between January-March ( Ballesteros-Cánovas et al., 2018 ), where powder snow avalanches tend to occur due to cumulative snow precipitation. Given the unusual timing of the avalanche (spring) it is speculated that warmer snow surface temperature (0°C) with rising...
FIGURES
First thumbnail for: The 23 rd April ’21 Snow Avalanche, Girthi Ganga p...
Second thumbnail for: The 23 rd April ’21 Snow Avalanche, Girthi Ganga p...
Journal Article
Published: 01 October 2001
Russ. Geol. Geophys. (2001) 42 (10): 1453–1461.
... associated with the India/Eurasia collision and the activity of the Tibetan plume. Plume geophysical fields seismicity three-dimensional velocity structure deep structure mantle diapirism plate collision geodynamics High Asia, including Tibet, the Himalayas, Pamir-Hindu Kush, and Tien Shan...
FIGURES
First thumbnail for: THE TIBETAN PLUME AND SEISMICITY IN HIGH ASIA AS I...
Second thumbnail for: THE TIBETAN PLUME AND SEISMICITY IN HIGH ASIA AS I...
Third thumbnail for: THE TIBETAN PLUME AND SEISMICITY IN HIGH ASIA AS I...
Journal Article
Published: 01 May 2003
Seismological Research Letters (2003) 74 (3): 305–311.
... to the north-northeast-trending range in front of the Hindu Kush Mountains to the east. ERI calculated a fault strike of 191° and slip of 0.7 m along an azimuth of 111°. According to M. Kikuchi and Y. Yamanaka of ERI, the rupture area was 10 km × 5 km, the source duration was 4 sec, the average stress drop...
FIGURES
First thumbnail for: Damage from the Nahrin, Afghanistan, Earthquake of...
Second thumbnail for: Damage from the Nahrin, Afghanistan, Earthquake of...
Third thumbnail for: Damage from the Nahrin, Afghanistan, Earthquake of...
Journal Article
Published: 01 December 1996
Bulletin of the Seismological Society of America (1996) 86 (6): 1793–1803.
.... Cheatum C. E. McEuen R. B. (1978) . Elsinore fault seismicity: the September 13, 1973, Agua Caliente Springs, California, earthquake series , Bull. Seism. Soc. Am. 68 , 429 - 440...
Journal Article
Published: 04 August 2023
Geological Magazine (2023) 160 (7): 1376–1394.
... by a terminal continent–continent collision (e.g. Hatcher, 2010 ). Hindu Raj Pakistan metamorphism monazite petrochronology zircon geochronology Kohistan Himalaya Six days of vehicle-supported field mapping along the Yasin and Ishkuman valleys was carried out in the Spring of 2018...
FIGURES
First thumbnail for: Metamorphic and intrusive history of the <span cla...
Second thumbnail for: Metamorphic and intrusive history of the <span cla...
Third thumbnail for: Metamorphic and intrusive history of the <span cla...
Journal Article
Published: 01 December 1992
Journal of the Geological Society (1992) 149 (6): 1045–1047.
... to the south of the main Indus suture zone, but also active compression in the mountain ranges north of the Indus suture: the Karakoram, Hindu Kush, Pamirs, Kun Lun and Tien Shan, as well as uplift of the 5 km high Tibetan plateau. Crustal shortening has mainly been accommodated by thrusting and folding...
Journal Article
Published: 01 November 2017
Jour. Geol. Soc. India (2017) 90 (5): 602–608.
... . Chu T-C. , and Wang J-J. , (2000) Radioactive disequilibrium of Uranium and Thorium Nuclide series in hot spring and river water from peitou hot spring basin in Taipei . Jour. Nuclear Radio Chemical Sciences , v. 1 , pp. 5 – 10 . Deccan Chronicle , (2016) IAF plane with 29...
FIGURES
First thumbnail for: Source and Causes of 2015 Great Pluvial Flood of C...
Second thumbnail for: Source and Causes of 2015 Great Pluvial Flood of C...
Third thumbnail for: Source and Causes of 2015 Great Pluvial Flood of C...
Image
Geologic relations of the Grand Canyon to the Laramide Kaibab uplift bounded on the east by the East Kaibab (EKm) and Echo Cliffs (ECm) monoclines adapted after Reynolds (1989), Billingsley and Workman (2000), Sable and Hereford (2004), Biek et al. (2009), and Felger and Beard (2010). Geology across the Markagunt (MP), Paunsagunt (PP), and Kaiparowits (KoP) plateaus north of the Grand Canyon after Dickinson et al. (2012). Plateaus bordering the Grand Canyon: CP—Coconino; HP—Hualapai; KaP—Kaibab; SP—Shivwits; UP—Uinkaret. Major faults: Hf—Hurricane; Pf—Paunsagunt; Sf—Sevier. Trend (bracketed line) of Miocene Crooked Ridge (CR) paleochannel near Kaibito after Lucchitta et al. (2011a, 2011b). Paleogene–Miocene Hindu-Milkweed (HM) and Peach Springs (PS) paleovalleys (bracketed lines) on Hualapai Plateau after Young (2011). Distribution of “rim gravels” (Tse) on Coconino Plateau east of the Peach Springs paleovalley schematic after Hill and Ranney (2008). Explanation for legend: Neogene volcanics (Tvn)—San Francisco volcanic field and underlying Miocene volcanics; Oligocene–Miocene strata (Tsu)—Buck and Doe Conglomerate; Paleogene volcanics (Tvo)—Oligocene (to Lower Miocene) Marysvale Volcanics and Pine Valley laccolith (near St. George); Eocene strata (Tse)—Music Mountain and West Water Formations; Maastrichtian–Paleocene strata (KT) of the Canaan Peak and Pine Hollow Formations (preserved only along the axis of the Table Cliff syncline of the northwest Kaiparowits Plateau); Campanian strata (Kc)—Wahweap and Kaiparowits Formations; Permian strata (P)—Coconino, Toroweap, and Kaibab Formations; Precambrian to Permian rocks (PP)—Hermit Formation and older rocks including Proterozoic basement. Towns: C—Cameron; CC—Cedar City; E—Escalante; F—Flagstaff; GC—Grand Canyon village; Ka—Kanab; Ki—Kingman; Ko—Kaibito; L—Littlefield; Pa—Page; Pe—Peach Springs; Pu—Panguitch; S—Seligman; SG—St. George; W—Williams. States: AZ—Arizona; NV—Nevada; UT—Utah.
Published: 01 February 2013
—Paunsagunt; Sf—Sevier. Trend (bracketed line) of Miocene Crooked Ridge (CR) paleochannel near Kaibito after Lucchitta et al. (2011a , 2011b) . Paleogene–Miocene Hindu-Milkweed (HM) and Peach Springs (PS) paleovalleys (bracketed lines) on Hualapai Plateau after Young (2011) . Distribution of “rim gravels
Journal Article
Published: 01 October 1994
Bulletin of the Seismological Society of America (1994) 84 (5): 1571–1579.
... follows stretched exponential relations with spatial inhomogeneities in q value. Tests of a large number of synthetic sequences show that if different parts of a fault zone produced aftershocks decaying with stretched exponentials having a wide variety of q values, the combined sequence will be best fit...
Journal Article
Published: 01 March 2003
Seismological Research Letters (2003) 74 (2): 107–123.
... includes the major Ornach-Nal, Ghazaband, and Chaman strike-slip faults, which continue the left-lateral motion as far north as Kabul, where they join the Herat Fault and ultimately the Hindu Kush and Pamir Ranges. The Chaman Fault itself may accommodate as much as 19-24 mm/yr of strike-slip motion...
FIGURES
First thumbnail for: Earthquakes in Afghanistan
Second thumbnail for: Earthquakes in Afghanistan
Third thumbnail for: Earthquakes in Afghanistan
Journal Article
Published: 01 December 1987
Bulletin of the Seismological Society of America (1987) 77 (6): 2143–2151.
... P. (1980) . Microearthquake seismicity and fault plane solutions in the Hindu Kush region and their tectonic implications , J. Geophys. Res. 85 , 1365 - 1387 . Lash C. C. (1980) . Shear waves...
Journal Article
Published: 01 June 2011
Italian Journal of Geosciences (2011) 130 (2): 161–262.
... Slates on the Paleo-Mesozoic sediments of the Northern Karakoram Terrain ( Z anchi , 1993 ; Z anchi & G aetani , 1994 ). This thrust fault can be traced through the Wakhan ( K afarskyi & A bdullah , 1976 ) and across East Hindu Kush down to the Tirich Mir ( Z anchi et alii , 2000...
FIGURES
First thumbnail for: The geology of the Karakoram range, Pakistan: the ...
Second thumbnail for: The geology of the Karakoram range, Pakistan: the ...
Third thumbnail for: The geology of the Karakoram range, Pakistan: the ...