Motion of Earth's surface caused by volcanic activity
Bradyseism is the gradual uplift (positive bradyseism) or descent (negative bradyseism) of part of the Earth's surface caused by the filling or emptying of an underground magma chamber or hydrothermal activity, particularly in volcanic calderas. It can persist for millennia in between eruptions and each uplift event is normally accompanied by thousands of small to moderate earthquakes.[1] The word derives from the ancient Greek words βραδύς bradús, meaning "slow", and σεισμός seismós meaning "movement", and was coined by Arturo Issel in 1883.[2][3][4]
^De Natale, G.; Troise, C.; Pingue, F.; Mastrolorenzo G.; Pappalardo L.; Battaglia M.; Boschi E. (2006). "The Campi Flegrei caldera: unrest mechanisms and hazards". In Troise C., De Natale G. & Kilburn C.R.J. (ed.). Mechanisms of activity and unrest at large calderas. Special Publications. Vol. 269. London: Geological Society. p. 28. ISBN 978-1-86239-211-3. Retrieved 14 July 2011.
^Cite error: The named reference Scandone was invoked but never defined (see the help page).
^Orsi, G.; Civetta L.; de Vita S.; Di Vito M.A.; Isaia R.; Petrazzuoli S.M.; Ricciardi G.P.; Ricco C. (1999). "Short-term ground deformations and seismicity in the resurgent Campi Flegrei caldera (Italy): an example of active block-resurgence in a densely populated area". Journal of Volcanology and Geothermal Research. 91 (2–4). Elsevier: 415–451. Bibcode:1999JVGR...91..415O. doi:10.1016/S0377-0273(99)00050-5.
^"Bradyseism in the Flegrea Area". UNESCO World Heritage Centre. Retrieved 19 July 2011.
Bradyseism is the gradual uplift (positive bradyseism) or descent (negative bradyseism) of part of the Earth's surface caused by the filling or emptying...
trench Phenomena associated with igneous activity Geysers and hot springs Bradyseism Volcanic eruption Earth's magnetic field Exogenic phenomena Slope phenomena...
trench Phenomena associated with igneous activity Geysers and hot springs Bradyseism Volcanic eruption Earth's magnetic field Exogenic phenomena Slope phenomena...
fifth century the breakwater of Portus Iulius became submerged due to Bradyseism. The Romans built new breakwaters near Misenum and the base was fed by...
Archived from the original on 3 December 2021. Retrieved 1 January 2022. "Bradyseism in the Flegrea Area". UNESCO World Heritage Centre. Archived from the...
molluscs when, at an earlier time, the ground level was much lower due to Bradyseism, and sea-water could flow in. Temple of Augustus (part of the cathedral)...
The lowering of the ground close to the coast below sea level, due to bradyseism, seems to have occurred in two phases: between the third and fifth centuries...
39,000 years ago. The area exhibits small localised earthquake swarms, bradyseism, and release of carbon dioxide and hydrogen sulfide into the atmosphere...
temples, theatre, numerous houses and necropoles are still buried. Due to bradyseism, which affects the entire Vesuvius region, portions of the historic city...
tuff cliffs with a semicircular gallery and is half submerged due to bradyseism. Near the theatre on the coast a large Roman villa complex has recently...
suffered several natural disasters: a first bradyseism in 1978, the 1980 Irpinia earthquake and a second bradyseism in 1983. These events dramatically highlighted...
debate in early geology, and eventually led to the identification of bradyseism in the area, showing that the Earth's crust could be subject to gradual...
roof about 24 metres above water level. Formation of cave was caused by bradyseism (tectonic upheaval of cliffs): cliffs fractured, and the cave was formed...
secondary volcanic phenomena, of which the best known is the Phlegraean bradyseism, which in the second half of the 1900s led to the evacuation of entire...
Terra was populated until 1970 when it was evacuated due to a sudden bradyseism event that raised the hill on which the district is located by 1.7 m (5...
frequent episodes of large-scale up- and downlift ground deformation (Bradyseism) do occur. In 2008 it was discovered that the Phlegraean Fields and Mount...
Julius" created by Marcus Vipsanius Agrippa in 37 BC, later sunk due to bradyseism. The sea floor elsewhere in the Mediterranean holds countless archaeological...
the Romans) became progressively silted up by the process of coastal bradyseism. During the 5th century, when the Vandals made life difficult in Ercula...
was delayed by the total evacuation of the Rione Terra in 1970 due to bradyseism and poor housing conditions, by bureaucratic delays, by difficulties in...
deterioration of the zone that already started to suffer some consequences of the bradyseism that subsequently will submerge the ancient Sinuessanus habitat. All that...