Tibet and High Asia: 8 Glaciogeomorphology and former glaciation in the Himalaya and Karakorum
Gespeichert in:
| Weitere Verfasser: | |
|---|---|
| Format: | Buch |
| Sprache: | English |
| Veröffentlicht: |
Aachen
Shaker
2013
|
| Schriftenreihe: | Geography international
3 |
| Online-Zugang: | Inhaltsverzeichnis |
| Beschreibung: | 360 S. Ill., graph. Darst., Kt. 1 DVD (12 cm) |
| ISBN: | 9783844023879 |
Internformat
MARC
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| 008 | 141009s2013 gw abd| |||| 00||| eng d | ||
| 020 | |a 9783844023879 |9 978-3-8440-2387-9 | ||
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| 245 | 1 | 0 | |a Tibet and High Asia |n 8 |p Glaciogeomorphology and former glaciation in the Himalaya and Karakorum |c Matthias Kuhle (ed.) |
| 264 | 1 | |a Aachen |b Shaker |c 2013 | |
| 300 | |a 360 S. |b Ill., graph. Darst., Kt. |e 1 DVD (12 cm) | ||
| 336 | |b txt |2 rdacontent | ||
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| 338 | |b nc |2 rdacarrier | ||
| 490 | 1 | |a Geography international |v 3 | |
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Datensatz im Suchindex
| _version_ | 1804152579211395072 |
|---|---|
| adam_text | TABLE OF CONTENTS
ABSTRACT:. 1
KEY WORDS: 2
1. INTRODUCTION, METHODS OF EVIDENCE AND CHARACTERISTICS OF THE
INVESTIGATION AREA 3
1.1. METHODS 4
1.2. DATINGS 6
1.2.1. PROBABILITY OF INHERITANCE G
1.2.2. CHRONOLOGY BY MEANS OF SNOWLINE-DEPRESSIONS (AELA) (TAB. 1) 9
1J. AREA OF INVESTIGATION 11
2. THE MUSTANG-THAK KHOLA OUTLET GLACIER 19
2.1. THE HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE
MUSTANG-THAK KHOLA OUTLET GLACIER ON
THE BORDER OF S-TIBET (TSANGPO VALLEY AND KORE LA) AND IN THE UPPER
VALLEY CHAMBER BETWEEN KORE LA
AND THE POSITIONS OF THE LOMATHANG- AND MARAN SETTLEMENTS (FIG. 5 AND
3)....................... .................19
2.1.1. THE LATE GLACIAL LATERAL- AND GROUND MORAINES AND THE
GLACIOFLUVIAL TERRACES OF THE UPPER MUSTANG-THAK
KHOLA
AND THEIR CONTINUATION INTO THE
MIDDLE MUSTANG-THAK
KHOLA (FIG. 5 AND 2) 27
2.2. THE HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE
MUSTANG-THAK KHOLA IN THE VALLEY
CHAMBER
BETWEEN
THE
POSITIONS
OF THE
MARAN-
AND
CHAILE
SETTLEMENTS
(FIG.
5) ***
23. THE DEPOSIT OF MORAINES AND THE HIGHEST FORMER TRIM-LINES AND
GLACIER THICKNESSES OF THE MUSTANG-
THAK KHOLA IN THE VALLEY CHAMBER BETWEEN THE POSITIONS OF THE CHAILE-
AND THINI SETTLEMENTS (FIG. 5) 62
2.4. THE REMNANTS OF THE GROUND MORAINE PEDESTAL IN THE THAK KHOLA
BETWEEN THE JUNCTIONS OF THE
THINI- (LONGPOGHYUN-) AND MYAGDI (MAYANGDI-)KHOLA (FIG. 5 AND 3), MAINLY
IN THE VALLEY CHAMBER
BETWEEN THE POSITIONS OF TUKUCHE- (TUKCHE-) AND BENI SETTLEMENTS, I.E.
IN THE HIMALAYA BREACH BETWEEN
ANNAPURNA AND DHAULAGIRI 85
2.4.1. RECONSTRUCTION OF THE HEIGHT OF THE LOWEST TERMINUS OF THE
GLACIER TONGUE OF THE MUSTANG-THAK KHOLA OUTLET
GLACIER S OF THE BREACH OF THE MAIN HIMALAYAN CHAIN (FIG. 3) 101
2.4.2. FINDINGS CONCERNING A LATE GLACIAL THAK-KHOLA ICE-DAMMED LAKE AND
THE ACCOMPANYING (GLOF) MEGA FLOOD
SEDIMENTS IN THE LOWEST THAK KHOLA (FIG. 2) 101
2.5. SUMMARY OF THE RECONSTRUCTION OF THE ICE AGE (LGP, MIS 3-2)
MUSTANG-THAK KHOLA GLACIER AS AN
EXEMPLARY SOUTHERN OUTLET GLACIER FROM THE TIBETAN INLAND ICE THROUGH
MUSTANG INTO THE THAK KHOLA
THROUGH THE HIMALAYA MAIN CREST UP TO THE HIMALAYA S-SLOPE
.................................................................104
3. THE HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE MIDDLE
MARSYANDI NADI (KHOLA)
GLACIER OF THE
VALLEY CHAMBERS BETWEEN BHRAKA AND THE INFLOWS OF THE SABJE KHOLA (SAPSE
LUNGPA)
ANDJULU KHOLA UP TO THE INFLOW OF THE NAR KHOLA DOWN-VALLEY (FIG. 167A,
B) 120
3.1. THE VALLEY CHAMBER BETWEEN BHRAKA AND NAWAL (FIG. 167A) ..........
..120
3.2. THE
VALLEY CHAMBER BETWEEN NAWAL AND PISAN (FIG. 167A) ..................
..143
3J. THE VALLEY CHAMBERS BETWEEN PISAN AND THE JUNCTION OF THE NAR KHOLA
(FIG. 167A, B).......... 163
4. THE HIGHEST
FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE NAR (NAUR) KHOLA, ITS
SIDE VALLEYS
AND UPPERMOST CATCHMENT AREAS UP TO ITS INFLOW INTO THE MARSYANDI NADI
(KHOLA)-MAIN VALLEY (FIG.
167A, B) 179
4.1. THE
LGP (LGM) GLACIATION OF THE LAYJU KHOLA IN THE LUGULA- AND PERI
HIMAL-S-SLOPE (FIG. 167A)
179
4 .2. THE
CURRENT UP TO LGP (LGM)-GLACIATION OF THE UPPER PHU- PANGRI KHOLA (FIG.
167A).. ...........195
43. THE LGP (LGM) GLACIATION OF THE MIDDLE PHU KHOLA BETWEEN THE VALLEY
CHAMBER OF PHUGAU AND
KYAN (FIG.
167A)............................................................................................................................................202
HTTP://D-NB.INFO/1052211143
4.4. THE LGP
(LGM) GLACIATION OF THE PHU KHOLA BETWEEN THE VALLEY CHAMBER OF KYAN AND
CHYAKO
AND THE JUNCTION OF THE LAPSE- AND GHATTE KHOLA (LOWER KANLA- OR KANG LA
KHOLA) NEAR METAGAU (FIG.
167A) 217
4.5. THE MAXIMUM PAST, I.E. LGP (LGM) GLACIATION OF THE KANLA (KANG LA)
OR GHATTE KHOLA UP TO ITS
INFLOW INTO THE PHU KHOLA SE OF NAR (NARGAU) (FIG. 167A) 223
4.6. THE MAXIMUM PAST, I.E. LGP (LGM) GLACIATION OF THE LAPSE KHOLA UP
TO ITS INFLOW INTO THE PHU
KHOLA E OF NAR
(FIG. 167A) 226
4.7. THE MAXIMUM PAST, I.E. LGP (LGM) GLACIATION OF THE NAR (NAUR) KHOLA
GLACIER, WHICH BUNDLES UP
THE ICESTREAM NETWORK OF THE DAMODAR HIMALA AS FAR AS TO ITS INFLOW INTO
THE MARSYANDI MAIN GLACIER
(FIG. 167A, B) 227
5. THE HIGHEST
FORMER GLACIER LEVELS AND GLACIER THICKNESSES OF THE MARSYANDI NADI
(KHOLA)-MAIN
VALLEY AND ITS
SIDE VALLEYS BETWEEN THE INFLOWS OF NAR (NAUR) KHOLA AND DUDH KHOLA
(FIG. 167B). 230
5.1. GLACIAL-GEOLOGICAL AND -GEOMORPHOLOGICAL DETAILED FINDINGS IN THE
SYARKYU KHOLA, A SMALL
REPRESENTATIVE OROGRAPHIC RIGHT SIDE
VALLEY OF THE MARSYANDI NADI (KHOLA)-MAIN VALLEY (FIG. 167B)...232
5.2. CONTINUATION OF:
THE HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE MARSYANDI
NADI
(KHOLA)-MAIN VALLEY
AND ITS SIDE VALLEYS BETWEEN THE INFLOWS OF THE NAR (NAUR) KHOLA AND THE
DUDH
KHOLA (FIG. 167B) 233
6. THE HIGHESTFORMER TRIM-LINES AND GLACIER THICKNESSES OF THE DUDH
KHOLA AND ITS SIDE-VALLEYS AND
UPPERMOST CATCHMENT AREAS UP TO ITS INFLOW INTO THE MARSYANDI NADI
(KHOLA)-MAIN VALLEY (FIG. 167A,
B) 235
6.1. THE LGP (LGM) GLACIATION OF THE BHIMDAN KHOLA IN THE PERI HIMAL-S-
AND CHO HIMAL-SW SLOPE
(FIG. 167A).. 235
6.2. THE LGP (LGM)
GLACIATION BETWEEN THE JUNCTION OF THE DOBHAN KHOLA AND THE SUTI KHOLA
INTO THE
MIDDLE DUDH KHOLA (FIG. 167A) .237
6.2.1. INSERTION: THE WALL FOOT PEDESTAL IN THE N W-FLANK OF MANASLU AS
A
CHARACTERISTIC INDICATION OF PLEISTOCENE
(QUATERNARY) GLACIATION (FIG. 167A, B) 238
6.2.2. CONTINUATION OF: THE LGP (LGM) GLACIATION BETWEEN
THE INFLOW OF DOBHAN KHOLA AND SUTI KHOLA INTO THE
MIDDLE DUDH KHOLA (FIG. 167A) 239
6 .3. THE PAST
AND LGP (LGM) GLACIATION OF THE LOWER DUDH KHOLA FROM THE JUNCTION OF
THE SIDE VALLEY
OF THE SUTI KHOLA UP TO THE JUNCTION OF THE LOWER DUDH KHOLA INTO THE
MARSYANDI KHOLA (FIG. 167A, B)
241
7.
THE HIGHEST FORMER
TRIM-LINES AND GLACIER THICKNESSES OF THE MARSYANDI NADI (KHOLA)-MAIN
VALLEY
FROM THE INFLOW
OF THE DUDH KHOLA UP TO BELOW THAT ONE OF THE DANA KHOLA HANGING VALLEY
(FIG.
167B) 244
8. THE HIGHEST
FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE DANA KHOLA AS FAR AS
ITS INFLOW INTO
THE MARSYANDI NADI (KHOLA)-MAIN VALLEY
(FIG. 167B) 253
8.1. THE
LGP (LGM)-GLACIATION OF THE UPPER DANA KHOLA BETWEEN
TULAGI-GLACIER-MORAINE-LAKE AND
6865 M-PEAK
(MANSIRI-HIMAL-SOUTH PEAK: MANASLU SW-SATELLITE) AND ONGRE
KHOLA-JUNCTION (FIG.
167B) 253
8
J2.
THE
LGP (LGM = STAGE 0) GLACIATION OF THE LOWER DANA KHOLA BETWEEN ONGRE
KHOLA-JUNCTION AND
MARSYANDI MAIN VALLEY (FIG. 167B)
..............................................................................................................254
9. THE
HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE MARSYANDI NADI
(KHOLA)-MAIN VALLEY
FROM THE INFLOW OF THE DANA KHOLA UP TO BELOW THE INFLOW OF THE MYARDI
KHOLA (FIG. 167B). .....
255
10. THE HIGHEST
FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE MARSYANDI NADI
(KHOLA)-MAIN
VALLEY FROM
THE JUNCTION
OF THE MYARDI KHOLA UP TO THE JUNCTION OF THE NADI KHOLA (FIG.L67B).....
258
11. THE HIGH GLACIAL
NADI (NGADI) KHOLA SIDE GLACIER, ITS HIGHEST FORMER GLACIER LEVELS AND
ICE
THICKNESSES (FIG. 167B) 267
12. THE HIGHEST FORMER TRIM-LINES AND GLACIER THICKNESSES OF THE
MARSYANDI NADI (KHOLA)-MAIN
VALLEY FROM
THE JUNCTION OF THE NADI (NGADI) KHOLA UP TO THE VALLEY CHAMBER OF THE
BESI SHAHAR
(FIG. 167B, C) 270
13. EVIDENCES AND COURSE OF THE HIGH GLACIAL MARSYANDI NADI GLACIER
TONGUE BETWEEN THE VALLEY
CHAMBER NEAR THE BESI SHAHAR SETTLEMENT AND THE LOWEST ICE MARGIN NEAR
THE DUMRE SETTLEMENT (FIG.
167C) 284
14. ACKNOWLEDGEMENT AND DISCUSSION OF THE EMPIRICAL RESEARCH RESULTS
FROM THE AREA OF THE
MARSYANDI NADI (KHOLA) ALREADY IN HAND (FIG. 167B) 295
15. SUMMARY OF THE RECONSTRUCTION OF THE GLACIAL (LGP, MIS 3-2)
MARSYANDI NADI ICE-STREAM-
NETWORK AS COMPOSEDFROM DENDRITIC VALLEY GLACIERS FROM S-TIBET UP TO S
OF
THE HIMALAYA (FIG.
167A, B, C) 296
16. THE NUMBER OF THE EMPIRICAL, POST-GLACIAL GLACIER STAGES MARKED IN
THE FIELD, AS FAR AS TO THE
CURRENT GLACIER TERMINI IN THE MARSYANDI NADI AND ITS SIDE VALLEYS AS
WELL AS THE ACCOMPANYING
MAXIMUM ICE MARGIN POSITIONS (FIG. 167A, B AND TAB. 1) 297
17. THE GLACIAL SNOWLINE ALTITUDE (ELA) AND ITS DEPRESSION (BJLLA)
AGAINST
TODAY 299
17.1. THE ELA-DEPRESSION IN THE MARSYANDI NADI CATCHMENT AREA 299
17.2. THE ELA-DEPRESSION IN THE MUSTANG-THAK KHOLA CATCHMENT AREA 300
17 J. THE GLACIAL COURSE OF THE SNOWLINE IN THE MUSTANG-THAK KHOLA AND
MARSYANDI KHOLA (FIG. 176)
300
18. MAIN-SUMMARY: THE GLACIAL MUSTANG-THAK KHOLA OUTLET GLACIER OF THE
TIBETAN ICE SHEET AND
THE MARSYANDI KHOLA (NADI)-ICESTREAM NETWORK AND ITS PALEOCLIMATIC
INDICATOR VALUE (FIGS. 3 AND
176) 301
ACKNOWLEDGEMENTS 302
REFERENCES. 303
MAPS. 308
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| illustrated | Illustrated |
| indexdate | 2024-07-10T01:12:57Z |
| institution | BVB |
| isbn | 9783844023879 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-027550536 |
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| physical | 360 S. Ill., graph. Darst., Kt. 1 DVD (12 cm) |
| publishDate | 2013 |
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| publisher | Shaker |
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| series | Geography international |
| series2 | Geography international |
| spelling | Tibet and High Asia 8 Glaciogeomorphology and former glaciation in the Himalaya and Karakorum Matthias Kuhle (ed.) Aachen Shaker 2013 360 S. Ill., graph. Darst., Kt. 1 DVD (12 cm) txt rdacontent n rdamedia nc rdacarrier Geography international 3 Geography international ... Kuhle, Matthias 1948-2015 (DE-588)138869677 edt (DE-604)BV042110071 8 Geography international 3 (DE-604)BV023311159 3 DNB Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=027550536&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
| spellingShingle | Tibet and High Asia Geography international |
| title | Tibet and High Asia |
| title_auth | Tibet and High Asia |
| title_exact_search | Tibet and High Asia |
| title_full | Tibet and High Asia 8 Glaciogeomorphology and former glaciation in the Himalaya and Karakorum Matthias Kuhle (ed.) |
| title_fullStr | Tibet and High Asia 8 Glaciogeomorphology and former glaciation in the Himalaya and Karakorum Matthias Kuhle (ed.) |
| title_full_unstemmed | Tibet and High Asia 8 Glaciogeomorphology and former glaciation in the Himalaya and Karakorum Matthias Kuhle (ed.) |
| title_short | Tibet and High Asia |
| title_sort | tibet and high asia glaciogeomorphology and former glaciation in the himalaya and karakorum |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=027550536&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |
| volume_link | (DE-604)BV042110071 (DE-604)BV023311159 |
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