Earthquake‐induced chains of geologic hazards: Patterns, mechanisms, and impacts

X Fan, G Scaringi, O Korup, AJ West… - Reviews of …, 2019 - Wiley Online Library
Large earthquakes initiate chains of surface processes that last much longer than the brief
moments of strong shaking. Most moderate‐and large‐magnitude earthquakes trigger …

Changes in permeability caused by transient stresses: Field observations, experiments, and mechanisms

M Manga, I Beresnev, EE Brodsky… - Reviews of …, 2012 - Wiley Online Library
Oscillations in stress, such as those created by earthquakes, can increase permeability and
fluid mobility in geologic media. In natural systems, strain amplitudes as small as 10− 6 can …

Temporal characteristics of groundwater chemistry affected by the 2016 Kumamoto earthquake using self-organizing maps

K Nakagawa, ZQ Yu, R Berndtsson, T Hosono - Journal of Hydrology, 2020 - Elsevier
Possibilities to perform pre-and post-seismic groundwater chemical comparisons on
regional groundwater flow systems are rare due to lack of data and observations. The …

Coseismic Groundwater Drawdown Along Crustal Ruptures During the 2016 Mw 7.0 Kumamoto Earthquake

T Hosono, C Yamada, T Shibata… - Water Resources …, 2019 - Wiley Online Library
Groundwater‐level changes after earthquakes provide insight into changes in
hydrogeological properties such as permeability and pore pressure. Quantifying such …

[PDF][PDF] Earthquake hydrology

M Manga, CY Wang - 2007 - scholar.archive.org
Coseismic static stress changes and dynamic stresses generated by seismic waves cause
changes in water level in wells and in stream flow and alter hydrogeologic properties such …

The 2010–2011 Canterbury earthquake sequence: Environmental effects, seismic triggering thresholds and geologic legacy

MC Quigley, MW Hughes, BA Bradley, S van Ballegooy… - Tectonophysics, 2016 - Elsevier
Seismic shaking and tectonic deformation during strong earthquakes can trigger widespread
environmental effects. The severity and extent of a given effect relates to the characteristics …

Mechanism of co-seismic water level change following four great earthquakes–insights from co-seismic responses throughout the Chinese mainland

Z Shi, G Wang, M Manga, CY Wang - Earth and Planetary Science Letters, 2015 - Elsevier
We analyze the co-seismic groundwater level responses to four great earthquakes recorded
by China's network of groundwater monitoring wells. The large number of operational wells …

[HTML][HTML] Fault-controlled springs: A review

R Keegan-Treloar, DJ Irvine, SC Solórzano-Rivas… - Earth-Science …, 2022 - Elsevier
Springs sustain groundwater-dependent ecosystems and provide freshwater for human use.
Springs often occur because faults modify groundwater flow pathways leading to discharge …

Water-table and discharge changes associated with the 2016–2017 seismic sequence in central Italy: hydrogeological data and a conceptual model for fractured …

M Petitta, L Mastrorillo, E Preziosi, F Banzato… - Hydrogeology …, 2018 - earth-prints.org
A seismic sequence in central Italy from August 2016 to January 2017 affected groundwater
dynamics in fractured carbonate aquifers. Changes in spring discharge, water-table position …

Regional changes in streamflow after a megathrust earthquake

CH Mohr, M Manga, CY Wang, O Korup - Earth and Planetary Science …, 2017 - Elsevier
Moderate to large earthquakes can increase the amount of water feeding stream flows,
mobilizing excess water from deep groundwater, shallow groundwater, or the vadose zone …