Highlights • Funda Volcanic System produced at least 3 eruptions over a period of <200 years. • Volcanism was longer and more recurrent than previously reported. • Eruptive styles range from Strombolian (mild and violent) to phreatomagmatic. • Magma/groundwater interactions may have led to rapid changes in eruptive style. • Future hazard assessment need to effectively consider magma/groundwater interactions. Monogenetic volcanoes occur in many different geotectonic settings and are usually small and short-lived. They can experience a variety of eruptive styles, even during the same eruption. In monogenetic volcanic fields, volcanism usually migrates to different locations over time, making volcanic hazard assessment very...
Abstract Small intra-plate volcanic islands (total height above seafloor <2500 m) have been consider...
Lacustrine sequences from active volcanic settings usually hold a rich and continuous record of teph...
The Auckland field has been active for over 140,000 years, during this time eruptions have formed 49...
Monogenetic volcanoes occur in many different geotectonic settings and are usually small and short-l...
From the study and interpretation of the volcanic products and structures of Flores Island, we infer...
Lacustrine sequences from active volcanic settings usually hold a rich and continuous record of teph...
The activity of the three stratovolcanoes on the island of Sao Miguel is documented by tephrochronol...
The AD 1761 eruption on Terceira was the only historical subaerial event on the island and one of th...
It is well known that explosive volcanic eruptions pose serious hazards to local communities and may...
The interaction between magmatic and tectonic processes in ocean intraplate volcanism yields insight...
Pico, the youngest island of the Azores Archipelago (Portugal), is characterized by a central volcan...
Santa Maria Island constitutes the oldest volcanic island within the Azores Archipelago, with no ons...
The Croscat pyroclastic succession has been analysed to investigate the transition between different...
The central islands of the Azores archipelago exhibit significant volcanic and seismic activity. The...
Abstract Small intra-plate volcanic islands (total height above seafloor <2500 m) have been consider...
Lacustrine sequences from active volcanic settings usually hold a rich and continuous record of teph...
The Auckland field has been active for over 140,000 years, during this time eruptions have formed 49...
Monogenetic volcanoes occur in many different geotectonic settings and are usually small and short-l...
From the study and interpretation of the volcanic products and structures of Flores Island, we infer...
Lacustrine sequences from active volcanic settings usually hold a rich and continuous record of teph...
The activity of the three stratovolcanoes on the island of Sao Miguel is documented by tephrochronol...
The AD 1761 eruption on Terceira was the only historical subaerial event on the island and one of th...
It is well known that explosive volcanic eruptions pose serious hazards to local communities and may...
The interaction between magmatic and tectonic processes in ocean intraplate volcanism yields insight...
Pico, the youngest island of the Azores Archipelago (Portugal), is characterized by a central volcan...
Santa Maria Island constitutes the oldest volcanic island within the Azores Archipelago, with no ons...
The Croscat pyroclastic succession has been analysed to investigate the transition between different...
The central islands of the Azores archipelago exhibit significant volcanic and seismic activity. The...
Abstract Small intra-plate volcanic islands (total height above seafloor <2500 m) have been consider...
Lacustrine sequences from active volcanic settings usually hold a rich and continuous record of teph...
The Auckland field has been active for over 140,000 years, during this time eruptions have formed 49...