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Khumbu Himalayas

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Journal Article
Journal: Geology
Published: 01 November 2014
Geology (2014) 42 (11): 1019–1022.
...Dirk Scherler Abstract Ice-free bedrock headwalls are widespread landforms of many glacial landscapes, but their formation and evolution are not well understood. Here, I present observations from the Khumbu Himalaya, eastern Nepal, of a distinct elevation zone that aligns the base of many steep...
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First thumbnail for: Climatic limits to headwall retreat in the <span c...
Second thumbnail for: Climatic limits to headwall retreat in the <span c...
Third thumbnail for: Climatic limits to headwall retreat in the <span c...
Journal Article
Published: 01 January 1999
The Journal of Geology (1999) 107 (1): 27–48.
...Roberto F. Weinberg; Mike P. Searle Abstract Leucogranite crops out in the upper Imja Khola, Khumbu Himalaya, Nepal, where it makes up approximately 50% of the exposed bedrock. Leucogranites and their associated aplite-pegmatites typically intruded as concordant sills, millimeters- to kilometers...
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First thumbnail for: Volatile-Assisted Intrusion and Autometasomatism o...
Second thumbnail for: Volatile-Assisted Intrusion and Autometasomatism o...
Third thumbnail for: Volatile-Assisted Intrusion and Autometasomatism o...
Journal Article
Published: 01 April 1999
Journal of the Geological Society (1999) 156 (2): 227–240.
... in the Khumbu Himalaya, Nepal Journal of Geology in press Wu C. Nelson K.D. Wortman G. Samson S. Yue Y. Li J. Ktdd W.S.F. Edwards M.A. Yadong cross-structure and South Tibetan Detachment in the east central Himalaya (89°–90°E) Tectonics 1998 17 28 45 Yin...
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 (a) Map of the Khumbu Himalaya showing localities of samples used for thermobarometry. (b) Profiles of temperature derived from conventional thermometry, and pressure calculated by THERMOCALC, against map distance north of the MCT zone for samples from the Khumbu valley.
Published: 01 May 2003
Fig. 8.  ( a ) Map of the Khumbu Himalaya showing localities of samples used for thermobarometry. ( b ) Profiles of temperature derived from conventional thermometry, and pressure calculated by THERMOCALC, against map distance north of the MCT zone for samples from the Khumbu valley.
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Published: 01 October 2000
TABLE 1. RELATIVE CHRONOLOGIES FOR KHUMBU HIMALAYA AND TENTATIVE CORRELATIONS, SHOWING THE SAMPLE COLLECTED AND AGES OBTAINED IN THIS PROJECT
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Glaciated landscape in the Khumbu Himalaya, eastern Nepal. A: Hillshade map draped over digital elevation model with elevations increasing toward lighter hues. Ice cover after Arendt et al. (2012). Black points are locations of automatic weather stations at Lukla (L), Syangboche (S), Namche Bazar (N), Pheriche (P), Pyramid (Py), Kala Patthar (KP), and South Col (SC). Black line with white points indicates ridgeline and analysis extent; points are spaced at 2 km. White star indicates Pokalde Glacier (PG) with mass-balance data (Wagnon et al., 2013). Inset map gives geographic position of study area; elevations &gt;3 km in dark gray. B: Geological map showing same area as in A, based on Schelling (1992) and Lombardo and Rolfo (2000): ts—Tethyan Series sedimentary rocks; rg—Rolwaling-Khumbu Granite; rp—Rolwaling-Khumbu Paragneiss; rm—Rolwaling-Khumbu Migmatite; jp—Junbesi Paragneiss. Black line gives ridgeline for reference. C: Topographic profiles along the steepest descents from white points on ridgeline in A.
Published: 01 November 2014
Figure 1. Glaciated landscape in the Khumbu Himalaya, eastern Nepal. A: Hillshade map draped over digital elevation model with elevations increasing toward lighter hues. Ice cover after Arendt et al. (2012) . Black points are locations of automatic weather stations at Lukla (L), Syangboche (S
Image
Figure 1. Simplified geologic map of Khumbu Himalaya (after Searle, 1999a) showing outcrop locations of U-Pb and thermobarometry samples analyzed in this paper. Inset shows location of Zanskar (Z) and Garwhal (G).
Published: 01 May 2000
Figure 1. Simplified geologic map of Khumbu Himalaya (after Searle, 1999a ) showing outcrop locations of U-Pb and thermobarometry samples analyzed in this paper. Inset shows location of Zanskar (Z) and Garwhal (G).
Image
Photograph of Lingtren, west of Everest, showing the Everest leucogranite sill above the sheeted leucogranite sill complex intruding sillimanite gneisses, Khumbu Himalaya. Photo: Mike Searle.
Published: 01 December 2024
Photograph of Lingtren, west of Everest, showing the Everest leucogranite sill above the sheeted leucogranite sill complex intruding sillimanite gneisses, Khumbu Himalaya. P hoto : M ike S earle .
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Published: 01 June 2003
TABLE 1. TENTATIVE CORRELATIONS, RELATIVE CHRONOLOGIES, AND NUMERICAL DATES FOR THE GLACIAL SUCCESSIONS IN THE KHUMBU HIMALAYA SOUTH OF MOUNT EVEREST
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(A) South face of Lingtren (6749 m), west of Everest showing horizontal sheeted sill complex with leucogranites intruding sillimanite gneisses, with a massive sill above containing several large xenoliths. (B) Early, layered leucogranite sills (set 1) with fabrics intruded into gneisses cut by later granite melts with sills (set 2), Manaslu leucogranite. (C) Syn-kinematic in situ melting in migmatite, cut by later post-kinematic lecuogranite dykes, Manaslu leucogranite. (D) Thick leucogranite sills intruding sillimanite gneisses, with dykes bent toward the north beneath the South Tibetan Detachment (STD) low-angle normal fault, North face of Ama Dablam (6828 m) south of Everest, Khumbu Himalaya.
Published: 01 December 2013
Tibetan Detachment (STD) low-angle normal fault, North face of Ama Dablam (6828 m) south of Everest, Khumbu Himalaya.
Journal Article
Journal: Geology
Published: 01 May 2000
Geology (2000) 28 (5): 403–406.
...Figure 1. Simplified geologic map of Khumbu Himalaya (after Searle, 1999a ) showing outcrop locations of U-Pb and thermobarometry samples analyzed in this paper. Inset shows location of Zanskar (Z) and Garwhal (G). ...
FIGURES
First thumbnail for: Two episodes of monazite crystallization during me...
Second thumbnail for: Two episodes of monazite crystallization during me...
Third thumbnail for: Two episodes of monazite crystallization during me...
Journal Article
Journal: Geology
Published: 01 June 2003
Geology (2003) 31 (6): 561–564.
...TABLE 1. TENTATIVE CORRELATIONS, RELATIVE CHRONOLOGIES, AND NUMERICAL DATES FOR THE GLACIAL SUCCESSIONS IN THE KHUMBU HIMALAYA SOUTH OF MOUNT EVEREST ...
FIGURES
First thumbnail for: Beryllium-10 dating of Mount Everest moraines indi...
Second thumbnail for: Beryllium-10 dating of Mount Everest moraines indi...
Third thumbnail for: Beryllium-10 dating of Mount Everest moraines indi...
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 09 October 2024
Lithosphere (2024) 2024 (4): lithosphere_2023_299.
... Structure in the Higher Himalaya of the Khumbu Region, Eastern Nepal , Bozeman , Montana State University , 2019 . 29 A. Yin , “Mode of cenozoic East‐West extension in Tibet suggesting a common origin of rifts in Asia during the Indo‐Asian collision,” Journal of Geophysical Research...
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First thumbnail for: The Benkar Fault Zone: An Orogen-Scale Cross Fault...
Second thumbnail for: The Benkar Fault Zone: An Orogen-Scale Cross Fault...
Third thumbnail for: The Benkar Fault Zone: An Orogen-Scale Cross Fault...
Journal Article
Published: 01 May 2003
Journal of the Geological Society (2003) 160 (3): 345–366.
...Fig. 8.  ( a ) Map of the Khumbu Himalaya showing localities of samples used for thermobarometry. ( b ) Profiles of temperature derived from conventional thermometry, and pressure calculated by THERMOCALC, against map distance north of the MCT zone for samples from the Khumbu valley. ...
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First thumbnail for: The structural geometry, metamorphic and magmatic ...
Second thumbnail for: The structural geometry, metamorphic and magmatic ...
Third thumbnail for: The structural geometry, metamorphic and magmatic ...
Journal Article
Published: 01 March 2006
Journal of the Geological Society (2006) 163 (2): 383–399.
... is largely restricted to the western Himalaya ( Benn & Owen 1998 ). At present, most snowfall in the study area accumulates during the summer when moisture is advected north from the Indian Ocean. Fig. 2.  Geomorphological map of the upper Imja Khola Valley, Khumbu Himal. Boxes define study areas...
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First thumbnail for: Quaternary fans and terraces in the <span class="s...
Second thumbnail for: Quaternary fans and terraces in the <span class="s...
Third thumbnail for: Quaternary fans and terraces in the <span class="s...
Journal Article
Journal: GSA Bulletin
Published: 01 October 2000
GSA Bulletin (2000) 112 (10): 1621–1632.
...TABLE 1. RELATIVE CHRONOLOGIES FOR KHUMBU HIMALAYA AND TENTATIVE CORRELATIONS, SHOWING THE SAMPLE COLLECTED AND AGES OBTAINED IN THIS PROJECT ...
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First thumbnail for: Timing of late Quaternary glaciations south of Mou...
Second thumbnail for: Timing of late Quaternary glaciations south of Mou...
Third thumbnail for: Timing of late Quaternary glaciations south of Mou...
Journal Article
Published: 13 November 2024
Journal of the Geological Society (2025) 182 (1): jgs2024-118.
..., northwards to the Khumbu glacier, representing one of the thickest sillimanite-grade migmatite sections in the Himalaya. Evolution of the GHS rocks includes early prograde metamorphism during crustal thickening, resulting in kyanite-grade assemblages ( c. 680–550°C, 10–8 kbar) and later decompression...
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First thumbnail for: The making of Mt Everest: channel flow and low-ang...
Second thumbnail for: The making of Mt Everest: channel flow and low-ang...
Third thumbnail for: The making of Mt Everest: channel flow and low-ang...
Journal Article
Journal: Geology
Published: 01 June 2015
Geology (2015) 43 (6): 523–526.
... and subsequent rockfall activity in the Khumbu Himalaya operates most efficiently in a narrow elevation band above 5500 m ( Scherler, 2014 ). Another physical explanation for the observed pattern of low-lying landslides involves the adjustment of rock slopes to postglacial stress redistribution focused on lower...
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First thumbnail for: Large landslides lie low: Excess topography in the...
Second thumbnail for: Large landslides lie low: Excess topography in the...
Third thumbnail for: Large landslides lie low: Excess topography in the...
Journal Article
Published: 27 November 2024
Seismological Research Letters (2025) 96 (3): 1733–1746.
... environmental microtremors and earthquakes in the Himalayas and worldwide. Khumbu Valley (Mount Everest) is one of the Himalayan regions that has not been struck by significant earthquakes ( M w > 7.8) in living memory. Although the analysis of microseismicity deserves further investigation, this article...
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First thumbnail for: The Seismic Station IO.EVN at Pyramid EvK2cnr (Eve...
Second thumbnail for: The Seismic Station IO.EVN at Pyramid EvK2cnr (Eve...
Third thumbnail for: The Seismic Station IO.EVN at Pyramid EvK2cnr (Eve...
Journal Article
Journal: Elements
Published: 01 December 2024
Elements (2024) 20 (6): 373–380.
...Photograph of Lingtren, west of Everest, showing the Everest leucogranite sill above the sheeted leucogranite sill complex intruding sillimanite gneisses, Khumbu Himalaya. P hoto : M ike S earle . ...
FIGURES
First thumbnail for: Himalayan Leucogranites: Field Relationships and T...
Second thumbnail for: Himalayan Leucogranites: Field Relationships and T...
Third thumbnail for: Himalayan Leucogranites: Field Relationships and T...