Thomas J Casadevall
Tom Casadevall is a Scientist Emeritus with the Geology, Geophysics, and Geochemistry Science Center.
Science and Products
Geoheritage Sites of the Nation
Geoheritage Sites of the Nation Data Release v.1
World map of volcanoes and principal aeronautical features
Evidence for a high-level porphyritic intrusion below the Sunnyside epithermal vein deposit, Colorado
High-temperature quartz veins were identified in drill core at ~600 m below the Sunnyside epithermal base and pre-cious metal deposit in southwestern Colorado. The veins consist of early anhedral quartz that shows a bluish ca-thodoluminescence emission and hosts heterogenous silicate melt inclusions. The early quartz is overgrown by a later generation of quartz that exhibits euhedral termina-tions
Progress in protecting air travel from volcanic ash clouds
Born of fire: In search of volcanoes in U.S. national parks, four striking examples
Volcanic ash and aviation–The challenges of real-time, global communication of a natural hazard
Encounters of aircraft with volcanic ash clouds: A compilation of known incidents, 1953-2009
Volcanic hazards to airports
Compilation of Disruptions to Airports by Volcanic Activity (Version 1.0, 1944-2006)
Preliminary analytical results for a mud sample collected from the LUSI Mud Volcano, Sidoarjo, East Java, Indonesia
Ground deformation at Merapi Volcano, Java, Indonesia: distance changes, June 1988-October 1995
Sulfur dioxide emission rates of Kilauea Volcano, Hawaii, 1979-1997
Monitoring so2 emission at the Soufriere Hills volcano: Implications for changes in eruptive conditions
Volcanic ash - danger to aircraft in the north Pacific
Science and Products
Geoheritage Sites of the Nation
Geoheritage Sites of the Nation Data Release v.1
World map of volcanoes and principal aeronautical features
Evidence for a high-level porphyritic intrusion below the Sunnyside epithermal vein deposit, Colorado
High-temperature quartz veins were identified in drill core at ~600 m below the Sunnyside epithermal base and pre-cious metal deposit in southwestern Colorado. The veins consist of early anhedral quartz that shows a bluish ca-thodoluminescence emission and hosts heterogenous silicate melt inclusions. The early quartz is overgrown by a later generation of quartz that exhibits euhedral termina-tions