Bradyseism, the Glossary
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.[1]
Table of Contents
15 relations: Ancient Greek, Arturo Issel, Caldera, Deformation (volcanology), Earthquake, Earthquake swarm, Fumarole, Gastrochaenolites, Lithophaga, Macellum of Pozzuoli, Magma chamber, Naples, Phlegraean Fields, Pozzuoli, Solfatara (volcano).
Ancient Greek
Ancient Greek (Ἑλληνῐκή) includes the forms of the Greek language used in ancient Greece and the ancient world from around 1500 BC to 300 BC.
See Bradyseism and Ancient Greek
Arturo Issel
Arturo Issel (Genoa April 11, 1842 – Genoa November 27, 1922) was an Italian geologist, palaeontologist, malacologist and archaeologist, born in Genoa.
See Bradyseism and Arturo Issel
Caldera
A caldera is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption.
Deformation (volcanology)
In volcanology, deformation is any change in the shape of a volcano or the land surrounding it. Bradyseism and deformation (volcanology) are volcanology.
See Bradyseism and Deformation (volcanology)
Earthquake
An earthquakealso called a quake, tremor, or tembloris the shaking of the Earth's surface resulting from a sudden release of energy in the lithosphere that creates seismic waves. Bradyseism and earthquake are seismology.
Earthquake swarm
In seismology, an earthquake swarm is a sequence of seismic events occurring in a local area within a relatively short period.
See Bradyseism and Earthquake swarm
Fumarole
A fumarole (or fumerole) is a vent in the surface of the Earth or another rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids.
Gastrochaenolites
Gastrochaenolites is a trace fossil formed as a clavate (club-shaped) boring in a hard substrate such as a shell, rock or carbonate hardground.
See Bradyseism and Gastrochaenolites
Lithophaga
Lithophaga, the date mussels, are a genus of medium-sized marine bivalve molluscs in the family Mytilidae.
Macellum of Pozzuoli
The Macellum of Pozzuoli (Macellum di Pozzuoli) was the macellum or market building of the Roman colony of Puteoli, now the city of Pozzuoli in southern Italy. Bradyseism and macellum of Pozzuoli are volcanology.
See Bradyseism and Macellum of Pozzuoli
Magma chamber
A magma chamber is a large pool of liquid rock beneath the surface of the Earth. Bradyseism and magma chamber are volcanology.
See Bradyseism and Magma chamber
Naples
Naples (Napoli; Napule) is the regional capital of Campania and the third-largest city of Italy, after Rome and Milan, with a population of 909,048 within the city's administrative limits as of 2022.
Phlegraean Fields
Phlegraean Fields (Campi Flegrei,; Campe Flegree) is a large caldera volcano west of Naples, Italy.
See Bradyseism and Phlegraean Fields
Pozzuoli
Pozzuoli is a city and comune of the Metropolitan City of Naples, in the Italian region of Campania.
Solfatara (volcano)
Solfatara (Solfatara di Pozzuoli) is a shallow volcanic crater at Pozzuoli, near Naples, part of the Phlegraean Fields (Campi Flegrei) volcanic area.
See Bradyseism and Solfatara (volcano)
References
[1] https://en.wikipedia.org/wiki/Bradyseism
Also known as Bradyseismic, Bradyseismic activity.