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Abstract The Indian subcontinent today houses about one-third of the global population and is one of the most vulnerable regions to future climate variability. This region has seen changes in civilizations, kingdoms and more recently political regimes, that were intricately linked to the changing environment over the mid–late Holocene. A comparative analysis of human–environment interaction within different regions at different time scales of the Quaternary is, however, lacking. In this paper we discuss the human–environment interactions taking case studies from two diverse time periods and geographically different regions from the Indian subcontinent. First, we review and analyse the role of environmental change in the evolution of Indus civilization on the northwestern Indian subcontinent during the mid–late Holocene and secondly, we discuss the role of both the anthropogenic activities and environmental change during the Anthropocene in shaping up the Bengal Delta. Overall, during the mid–late Holocene, Indus cultural transformations were driven by natural environmental changes, whereas the anthropogenic activities in the last few centuries have modified the Bengal deltaic landscape, which has intensified the impacts of natural disasters – in both cases a change in socio-political scenarios occurred. Such studies can be used as benchmarks to understand the future response of societies to environmental changes.
Evidence of Active Quaternary Deformation on the Great Valley Fault System near Winters, Northern California
Airborne LiDAR‐Based Mapping of Surface Ruptures and Coseismic Slip of the 1955 Zheduotang Earthquake on the Xianshuihe Fault, East Tibet
ShakeMap4‐Web: Web Application for ShakeMap 4 Product Visualization
A Grand Challenge International Infrastructure for Earthquake Science
Source Parameters of the M w 5.7 Pica Crustal Earthquake in Northern Chile
Geological mapping of coastal and offshore Japan (by GSJ-AIST): collecting and utilizing the geological information
Abstract Devastating earthquakes and tsunamis capable of causing catastrophic damage to human societies and economies have frequently occurred on and around the Japanese islands. Because Japan is a long and narrow island arc in the Pacific Ocean located at the junction of four plates (the Eurasian and Philippine Sea Plates in the SW and the North America and Pacific Plates in the NE), it has probably suffered the highest number of earthquake and tsunami events anywhere in the world. Hence, geological and geoinformation investigations are supremely important, not only for understanding the geological development of Japan but also for forecasting the risks associated with geohazards and securing the safety of human lives and infrastructures. For these reasons, the Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (GSJ-AIST) has been conducting marine geological surveys since 1974 and, as of the end of 2019, produced a Marine Geology Map Series consisting of 90 geological maps. In addition, a coastal zone research project that aims to connect marine, coastal and land area geoinformation seamlessly was launched in 2008 to survey areas that have not yet been investigated, and six maps of geologically distinct areas have already been published based on that collected data.