Landforms of the lower Hushe Valley (Central Karakoram, Pakistan)

This paper presents a new geomorphological map for the lower Hushe Valley (below 3400 m asl), located to the SE of the Central Karakoram in Baltistan (North Pakistan). Fieldwork and remote sensing were combined to improve understanding of the most recent surface landforms to produce a 1:50,000 scale...

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Detalles Bibliográficos
Autores: Zabaleta Lopetegui, Ane, Álvarez González, Irantzu, Aranburu Artano, Arantza, Izagirre Estibaritz, Eñaut, Uriarte Goti, Jesús Ángel, Morales Juberías, Tomás, Antigüedad Auzmendi, Ignacio
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universidad del País Vasco
Repositorio:Addi. Archivo Digital para la Docencia y la Investigación
OAI Identifier:oai:addi.ehu.eus:10810/49910
Acceso en línea:http://hdl.handle.net/10810/49910
Access Level:acceso abierto
Palabra clave:glacial landforms
fluvial landforms
gravitational landforms
mass wasting processes
Hushe valley-Karakoram
Pakistan landscape evolution
rock avalanches
Indus river
Himalaya
inventory
incision
models
Descripción
Sumario:This paper presents a new geomorphological map for the lower Hushe Valley (below 3400 m asl), located to the SE of the Central Karakoram in Baltistan (North Pakistan). Fieldwork and remote sensing were combined to improve understanding of the most recent surface landforms to produce a 1:50,000 scale map. Thirteen landform types associated with glacial, fluvial, gravitational and mass wasting processes were identified and mapped. Particular emphasis was made on currently dynamic processes that could pose a threat to the population. The distribution of the landforms on the valley (reworked tills, alluvial fans, rockfalls, among others) differs between the eastern and the western hillslopes, and from north to south, mainly due to bedrock types, location of geological structures and distribution of lateral tributaries. This map is the first and necessary step towards a deep assessment on geological risk related to external processes in the area.