Glacial landforms as palaeo-environmental archives in the Eastern Himalaya: A case study of Changme Khangpu glacial valley in Sikkim Himalaya, India

This study attempts to reconstruct the glacial history of the Upper Changme Khangpu Basin (CKB), an eastern tributary of the River Tista in the Eastern Himalaya, using radiocarbon ( 14 C) method, supplemented by sedimentological and mineralogical analyzes. Despite being a monsoon-dominated glaciated region, the upper reaches of the basin still contain exceptionally well-preserved glacial landforms of the recent geological past. However, there remains a critical gap in understanding due to the lack of chronological studies to clarify and correlate the roles of climate and glacial interactions in an environment where intense monsoonal precipitation rapidly alters the landscape and glacier dynamics. In order to reconstruct the past glacier fluctuations and associated palaeoclimatic conditions, this study has employed a multi-proxy approach, integrating geomorphic feature mapping, sedimentological analysis, Accelerator Mass Spectrometry (AMS) 14 C dating, alongside the Schmidt Hammer rebound data for relative age determination. The results have yielded a well-defined glacial chronology for the Late Quaternary in the CKB, identifying four distinct glacial advances of varying magnitudes. The extensive glacial phase (Phase-II) resulted in the blockage of the ablation valley, forming a ∼700 m-long proglacial lake. Subsequent glacial recession seems to have intensified the paraglacial processes which progressively reshaped and modified the earlier landforms. A new dataset of 14 C ages (3.5 ka to 31.4 ka cal BP) indicates climatic oscillations during the intervening period. Post-glacial climatic shifts, particularly between 14.29 ka and 3.5 ka cal BP, show a regional correlation with climatic patterns observed in the Eastern Himalayas. Our finding underscores the need to further refine this enquiry to develop a robust glacial chronology of the basin using multiple modern geochronological techniques.

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Journal
Progress in Physical Geography Earth and Environment
Published
2025-11-25
DOI
https://doi.org/10.1177/03091333251401113
Primary Topic
Geology and Paleoclimatology Research
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article
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article

Glacial landforms as palaeo-environmental archives in the Eastern Himalaya: A case study of Changme Khangpu glacial valley in Sikkim Himalaya, India

Manasi Debnath, Md Maroof Azam, Hiambok Jones Syiemlieh, Pankaj Kumar et al.
Progress in Physical Geography Earth and Environment
Geology and Paleoclimatology Research
article

Glacial landforms as palaeo-environmental archives in the Eastern Himalaya: A case study of Changme Khangpu glacial valley in Sikkim Himalaya, India

Manasi Debnath, Md Maroof Azam, Hiambok Jones Syiemlieh, Pankaj Kumar, Parvendra Kumar, Milap Chand Sharma, Sanjay Deswal, Sparsh Rai
article en

Abstract

This study attempts to reconstruct the glacial history of the Upper Changme Khangpu Basin (CKB), an eastern tributary of the River Tista in the Eastern Himalaya, using radiocarbon ( 14 C) method, supplemented by sedimentological and mineralogical analyzes. Despite being a monsoon-dominated glaciated region, the upper reaches of the basin still contain exceptionally well-preserved glacial landforms of the recent geological past. However, there remains a critical gap in understanding due to the lack of chronological studies to clarify and correlate the roles of climate and glacial interactions in an environment where intense monsoonal precipitation rapidly alters the landscape and glacier dynamics. In order to reconstruct the past glacier fluctuations and associated palaeoclimatic conditions, this study has employed a multi-proxy approach, integrating geomorphic feature mapping, sedimentological analysis, Accelerator Mass Spectrometry (AMS) 14 C dating, alongside the Schmidt Hammer rebound data for relative age determination. The results have yielded a well-defined glacial chronology for the Late Quaternary in the CKB, identifying four distinct glacial advances of varying magnitudes. The extensive glacial phase (Phase-II) resulted in the blockage of the ablation valley, forming a ∼700 m-long proglacial lake. Subsequent glacial recession seems to have intensified the paraglacial processes which progressively reshaped and modified the earlier landforms. A new dataset of 14 C ages (3.5 ka to 31.4 ka cal BP) indicates climatic oscillations during the intervening period. Post-glacial climatic shifts, particularly between 14.29 ka and 3.5 ka cal BP, show a regional correlation with climatic patterns observed in the Eastern Himalayas. Our finding underscores the need to further refine this enquiry to develop a robust glacial chronology of the basin using multiple modern geochronological techniques.

Progress in Physical Geography Earth and EnvironmentVol. 50(1)
Dr. Bhim Rao Ambedkar University (IN), Jawaharlal Nehru University (IN), Ambedkar University Delhi (IN), North Eastern Hill University (IN), Government of India (IN), Inter-University Accelerator Centre (IN), Government Medical College (IN), Nagaland University (IN)
Openalex Percentile: Top 59%
Geology and Paleoclimatology Research
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