s). “Quantitative estimation of compaction and velocity changes using 4D impedance and traveltime changes” by Landro and Stammeijer (Geophysics, 2004). “Observations and analysis of B-type earthquakes, explosions, and volcanic tremor at Pavlof volcano, Alaska” by McNutt (Bulletin of the Seismological Society of America, 1986). “Coda wave interferometric detection of seismic velocity changes ass...

The Pinacate volcanic fi eld is ~330 km SSW of Phoenix, and it is a popular destination for volcanology and planetary geology fi eld trips. The volcanic fi eld, located on the Pinacate Biosphere Reserve in Sonora, Mexico, is a 1500 km2 basaltic fi eld including a shield volcano, lava tubes, maars, a tuff cone, cinder cones, pāhoehoe and ‘a‘ā lava fl ows as young as 12 ka, and phreatomagmatic co...

Idunn Mons is a shield volcano located in the Imdr Regio large igneous rise, Venusian equivalent to hotspot geologic province on Earth. Recent studies using emissivity data from ESA's Venus Express Mission, together with experimental laboratory alteration of volcanic materials conditions, suggest that possible site for very recent or even ongoing activity. In this work we carried out mapping ch...

We examine the empirical relationship between exposure to earthquake hazard and civic capital in Italian municipalities. Drawing on National Institute of Geophysics Volcanology, we find that increases capital. exploit variation across neighboring municipalities use a neighbor-pair fixed effect estimator establish causal link accumulation decompose along four dimensions – frequency, space, magni...

Remote sensing of our planet from space currently provides data for both Earth sciences (geography, geology, volcanology, geoinformatics, cartography, climatology, meteorology, oceanology, seismology, etc.) and applied problems in many areas human activity. Already the early years age saw emergence two spacecraft use that were great interest to military circles: observation communications. It w...