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Shyok River

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Journal Article

Grain Size Analysis of Dune and Bar Sediments of the Shyok River between Khalsar and Hunder Village, Karakoram Range, Ladakh, India

Rupendra Singh, Rajesh Kumar, I. M. Bahuguna, Rajesh Kumar
Published: 01 February 2020
Jour. Geol. Soc. India (2020) 95 (2): 183–189.
DOI: https://doi.org/10.1007/s12594-020-1408-1
... and ancient ( Mason and Folk, 1958 ; Friedman, 1961 ; Nordstorn, 1977; Singh et al., 2007 ; Kumar et al., 2010 ; Mir and Jeelani, 2015 ; Kanhaiya et al., 2017 ). The Shyok river basin comprises of numerous valley glaciers of size ranging from 1 km to 70 km in length and contributes water to many...
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Crossing from the Indus <span class="search-highlight">River</span> Valley to <span class="search-highlight">Shyok</span> <span class="search-highlight">River</span> Valley the over the Kha...

Crossing from the Indus River Valley to Shyok River Valley the over the Kha...

Published: 01 December 2024
Crossing from the Indus River Valley to Shyok River Valley the over the Khardung Pass, India (July 2008).
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Field photographs of the study area (a) <span class="search-highlight">Shyok</span> <span class="search-highlight">river</span> at Khalsar village (...

Field photographs of the study area (a) Shyok river at Khalsar village (...

Published: 01 February 2020
Fig.3. Field photographs of the study area (a) Shyok river at Khalsar village (b) Shyok -Nubra river confluence (c) Braided Shyok river downstream of the confluence near Diskit village (d) Sand dune deposits near Hundar village
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Sand-silt-clay ternary plot of <span class="search-highlight">Shyok</span> <span class="search-highlight">river</span> sand bars indicates sand

Sand-silt-clay ternary plot of Shyok river sand bars indicates sand

Published: 01 February 2020
Fig.6. Sand-silt-clay ternary plot of Shyok river sand bars indicates sand
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Incision history of the <span class="search-highlight">Shyok</span> <span class="search-highlight">River</span> into the valley fill. Error bars reflec...

Incision history of the Shyok River into the valley fill. Error bars reflec...

Published: 01 May 2014
Figure 12. Incision history of the Shyok River into the valley fill. Error bars reflect Monte Carlo best-fit model results for the Agham terrace age and external uncertainties from CRONUS online calculator ( Balco et al., 2008 ) for other ages. Shaded areas indicate likely incision paths. Dashed
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<span class="search-highlight">SHYOK</span> <span class="search-highlight">RIVER</span> WATER DISCHARGE

SHYOK RIVER WATER DISCHARGE

Published: 01 May 2014
TABLE 2. SHYOK RIVER WATER DISCHARGE
Journal Article

Ice dams, outburst floods, and glacial incision at the western margin of the Tibetan Plateau: A >100 k.y. chronology from the Shyok Valley, Karakoram

Dirk Scherler, Henry Munack, Jürgen Mey, Patricia Eugster, Hella Wittmann, Alexandru T. Codilean, Peter Kubik, Manfred R. Strecker
Journal: GSA Bulletin
Published: 01 May 2014
GSA Bulletin (2014) 126 (5-6): 738–758.
DOI: https://doi.org/10.1130/B30942.1
...Figure 12. Incision history of the Shyok River into the valley fill. Error bars reflect Monte Carlo best-fit model results for the Agham terrace age and external uncertainties from CRONUS online calculator ( Balco et al., 2008 ) for other ages. Shaded areas indicate likely incision paths. Dashed...
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Field photographs of fluvial-lacustrine valley fill in the upper <span class="search-highlight">Shyok</span> Vall...

Field photographs of fluvial-lacustrine valley fill in the upper Shyok Vall...

Published: 01 May 2014
Figure 4. Field photographs of fluvial-lacustrine valley fill in the upper Shyok Valley. (A) Fill terrace near Agham village. Note bright-colored lake sediments. View is southeast, upstream the Shyok River. (B) Valley fill in a tributary near Khardung. View is north, toward confluence
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Outcrop-scale structures from the upstream <span class="search-highlight">Shyok</span> Valley. (a) Marble and amp...

Outcrop-scale structures from the upstream Shyok Valley. (a) Marble and amp...

Published: 24 February 2020
Fig. 3. Outcrop-scale structures from the upstream Shyok Valley. (a) Marble and amphibolite schist of the PMC mapped along the Shyok river in the NE of the Shyok–Muglib strand of the KF. (b) Contact of the SMC with the KB. (c) Porphyritic granites with large laths of K-feldspar and plagioclase
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Stretched ASTER images, a Google Earth image, and a field photo of the trac...

Stretched ASTER images, a Google Earth image, and a field photo of the trac...

Published: 14 June 2018
Figure 7. Stretched ASTER images, a Google Earth image, and a field photo of the trace of the Longmu Co fault through the Chang Chenmo Range on the western side of the Shyok River. Location of A–C is shown in Figure 1 . (A) False color ASTER image. Imagery obtained from the U.S. Geological
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Geomorphology of the <span class="search-highlight">Shyok</span>-Nubra confluence. (A) Hillshade image with glaci...

Geomorphology of the Shyok-Nubra confluence. (A) Hillshade image with glaci...

Published: 01 May 2014
(a-a′ through h-h′). Dashed lines in profiles a-a’ through e-e’ give top of reconstructed valley fill. Elevations of Shyok and Nubra valley bottoms are colored, repeating every 20 m to highlight low gradients and alluvial fans. White arrows give flow direction of rivers. (B) Longitudinal profiles of the Shyok
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( a ) Low-resolution DEM of the Ladakh Batholith showing sample locations; ...

( a ) Low-resolution DEM of the Ladakh Batholith showing sample locations; ...

Published: 01 July 2009
) age data ± 1σ plotted against distance from the Indus River. (Note the systematic decrease of age from the south, near the Indus River, to the north towards the Shyok River, in both plots (indicated by dashed arrow).)
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Examples of spectra from ASTER images. Granite from within the Pangong Rang...

Examples of spectra from ASTER images. Granite from within the Pangong Rang...

Published: 14 June 2018
Figure 3. Examples of spectra from ASTER images. Granite from within the Pangong Range (PG) and limestone and skarn along the Shyok River (SL) were identified using ASTER and then verified in the field. We were not able to access areas of interest within parts of the Karakoram Range, part
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(A) The Digital Elevation Model with the major climate systems marked. The...

(A) The Digital Elevation Model with the major climate systems marked. The...

Published: 01 May 2021
) The Google Earth imagery showing TCN ages (yellow, Dortch et al., 2010 ), optical ages (white, Ganju et al., 2018 ) of the moraines at the confluence of Nubra and Shyok rivers. (C) The field photograph of Ganglas moraine near Leh (Ladakh Himalaya) dated to Marine Isotope Stage (MIS)-2 by Shukla et al
Journal Article

Structural relationship between the Karakoram and Longmu Co fault systems, southwestern Tibetan Plateau, revealed by ASTER remote sensing

Wendy Bohon, Kip V. Hodges, Alka Tripathy-Lang, J Ramón Arrowsmith, Christopher Edwards
Journal: Geosphere
Published: 14 June 2018
Geosphere (2018) 14 (4): 1837–1850.
DOI: https://doi.org/10.1130/GES01515.1
...Figure 7. Stretched ASTER images, a Google Earth image, and a field photo of the trace of the Longmu Co fault through the Chang Chenmo Range on the western side of the Shyok River. Location of A–C is shown in Figure 1 . (A) False color ASTER image. Imagery obtained from the U.S. Geological...
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(A) Lithologic map of the Ladakh region created from a combination of field...

(A) Lithologic map of the Ladakh region created from a combination of field...

Published: 14 June 2018
in the Bangong suture area; SL—limestone in the Shyok River area.
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Morphologic characteristics of formerly glaciated confluences along the Shy...

Morphologic characteristics of formerly glaciated confluences along the Shy...

Published: 01 May 2014
Figure 13. Morphologic characteristics of formerly glaciated confluences along the Shyok and Indus Rivers. (A) Catchments of major rivers that drain the Karakoram Mountains, along with the distribution of present-day glaciers (gray) and valley flats (yellow). RF—Raikhot fault; MKT—Main Karakoram
Journal Article

A Record of Ichnogenus Chondrites from Ladakh, Jammu and Kashmir, India and its Significance

D. K. Srivastava, A. K. Bhandari, N. Srimal, R. P. Radcliffe
Published: 01 September 1980
Jour. Geol. Soc. India (1980) 21 (9): 458–460.
DOI: https://doi.org/10.17491/jgsi/1980/210907
... - shale sequence of Tegar Formation are seen near Khalsar, Diskit and Terche in a belt along the southern side of the Shyok river. Recrystallized unidentifiable gastropods, crinoid stems and shells of bivalve are seen in the limestones near Khalsar and Skampu villages. Generally the limestones...
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Hydro-chemical Characteristics of Melt Water Draining from Glaciers of Rongdo Basin, Shyok Valley, Ladakh

Zahid Majeed, Muneer A. Mukhtar, Nadeem A. Bhat, Rakesh Misra, Anayat Ahmad Qureshi
Published: 01 April 2023
Jour. Geol. Soc. India (2023) 99 (4): 459–465.
DOI: https://doi.org/10.1007/s12594-023-2333-x
.... It is a V th order basin which is bound in the north and northeast by Shyok, and in south and southwest by Sumdo. It is a sub-basin of Indus river basin and lies in between the longitudes 77°37.40'E to 78°13.03'E and latitude 34°7.89'N to 34°37.05’N ( Fig 1 ). The main two tributaries of Rongdo basin...
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A Note on the Geology of Nubra-Shyok Area of Ladakh, Kashmir, Himalaya

V. C. Thakur, N. S. Virdi, Hakim Rai, K. R. Gupta
Published: 01 January 1981
Jour. Geol. Soc. India (1981) 22 (1): 46–50.
DOI: https://doi.org/10.17491/jgsi/1981/220106
... can be described as ophiolitic melange (Gansser, 1974). An intrusive body of tonalitic composition occurs within the Shyok Formation exposed at localities south of Tirit and junction of Nubra and Shyok rivers. Karakoram Batholith The Karakoram Bathotith is an important petrographic province...
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