Historical unrest at large calderas of the world

  title={Historical unrest at large calderas of the world},
  author={Christopher G. Newhall and Daniel Dzurisin}
This is a remarkable reference for researchers interested in volcanic hazards and silicic volcanism. Because of long repose and often obscure shapes and large size calderas are a volcanic type less obvious and less well studied. Because they represent potentially highly dangerous and highly explosive volcanos which could have large-scale and even global impact when they erupt, it is very important to understand their behavior. This new volume represents an extensive effort at compiling real… 
Monitoring super-volcanoes: geophysical and geochemical signals at Yellowstone and other large caldera systems
To prepare ourselves and society, scientists must scrutinize a spectrum of volcanic signals and assess the many factors contributing to unrest and toward diverse modes of eruption.
A Physical Model of Sill Expansion to Explain the Dynamics of Unrest at Calderas with Application to Campi Flegrei
Many calderas show remarkable unrests, which often do not culminate in eruptions (non-eruptive unrest). In this context the interpretation of the geophysical data collected by the monitoring networks
InSAR Imaging of Aleutian Volcanoes
In this chapter we discuss our InSAR observations of Aleutian volcanoes that have been active during historical time, starting with Kiska Volcano in the west and ending with Mount Wrangell in the
A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop
Abstract. Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the
An overview of recent (1988 to 2014) caldera unrest: Knowledge and perspectives
Calderas are among the most active and dangerous volcanoes. Caldera unrest is defined by enhanced seismicity, gravity changes, surface deformation, and degassing. Although much caldera unrest does
Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications
Taupō volcano, New Zealand, is a large caldera volcano that has been highly active through the Holocene. It most recently erupted ∼1,800 years ago but there have been multiple periods of historic
Response plan for volcano hazards in the Long Valley Caldera and Mono Craters Region, California
Persistent unrest in Long Valley Caldera-characterized by recurring earthquake swarms, inflation of the resurgent dome in the central sections of the caldera, and emissions of magmatic carbon dioxide
Decadal to monthly timescales of magma transfer and reservoir growth at a caldera volcano
A study of pre-eruptive magmatic processes and their timescales using chemically zoned crystals from the ‘Minoan’ caldera-forming eruption of Santorini volcano, Greece, which occurred in the late 1600s bc, to provide insights into how rapidly large silicic systems may pass from a quiescent state to one on the edge of eruption.