According to The World Factbook, the main natural phenomena posing a threat in Italy at a regional level are landslides, mudflows, avalanches, earthquakes, volcanic eruptions, floods and, in Venice, subsidence. [1]
According to The World Factbook, the main natural phenomena posing a threat in Italy at a regional level are landslides, mudflows, avalanches, earthquakes, volcanic eruptions, floods and, in Venice, subsidence. [1]
As released by the Italian Institute of Environmental Protection and Research (IIEPR), 2.2% of the Italian population lives in areas at high or very high risk from landslides, and 3.8% of buildings and 5.8% of cultural heritage sites are located in those places. [2]
Between 1970 and 2019, landslides caused 1085 deaths, 10 missing people, and 1454 non-fatal injuries. The regions with the highest mortality rate in that period were Aosta Valley and Trentino-Alto Adige/Südtirol. [3]
Being placed in the convergence between the Eurasian Plate and the African Plate, Italy (with the relative exception of Sardinia) suffers from seismicity, which is particularly high along the Apennine range, in Calabria, in Sicily and in some places of Northern Italy, such as Friuli, part of Veneto, and western Liguria. According to the Italian Civil Protection, the Italian seismic hazard is medium-high, while the vulnerability is very high also due to the fragility of the Italian building stock and the exposition is extremely high, as a consequence of the population density and the cultural heritage. [4]
As released by the Italian Institute of Environmental Protection and Research (IIEPR), 10.4% of the Italian population lives in areas at high or very high risk from floods, and 9.3% of buildings and 15.3% of cultural heritage sites are located in those places. [2]
Between 1970 and 2019, floods caused 585 deaths, 50 missing people, and 481 non-fatal injuries. The regions with the highest mortality rate in that period were Aosta Valley and Liguria. [3]
The Italian authorities have classified the Italian volcanoes based on the time of the last eruption; besides submarine volcanoes and those considered extinct, in Italy there are dormant (Alban Hills, Phlegraean Fields, Ischia, Vesuvius, Lipari, Vulcano, Panarea, Pantelleria) and active volcanoes (Mount Etna and Stromboli). [5]
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. The process that forms volcanoes is called volcanism.
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica, with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi).
Stromboli is an island in the Tyrrhenian Sea, off the north coast of Sicily, containing Mount Stromboli, one of the four active volcanoes in Italy. It is one of the seven Aeolian Islands, a volcanic arc north of Sicily, and the mythological home of Aeolus.
A volcano observatory is an institution that conducts research and monitoring of a volcano.
The volcanism of Italy is due chiefly to the presence, a short distance to the south, of the boundary between the Eurasian Plate and the African Plate. Italy is a volcanically active country, containing the only active volcanoes in mainland Europe. The lava erupted by Italy's volcanoes is thought to result from the subduction and melting of one plate below another.
The Hōei eruption of Mount Fuji started on December 16, 1707 and ended on February 24, 1708. It was the last confirmed eruption of Mount Fuji, with three unconfirmed eruptions reported from 1708 to 1854. The eruption took place during the reign of Emperor Higashiyama and the Shogun was Tokugawa Tsunayoshi. It is well known for the immense ash-fall it produced over eastern Japan and subsequent landslides and starvation across the country. Hokusai's One Hundred Views of Mount Fuji includes an image of the small crater at a secondary eruption site on the southwestern slope. The area where the eruption occurred is called Mount Hōei because it occurred in the fourth year of the Hōei era. Today, the crater of the main eruption can be visited from the Fujinomiya or Gotemba Trails on Mount Fuji.
Prediction of volcanic activity, and volcanic eruption forecasting, is an interdisciplinary monitoring and research effort to predict the time and severity of a volcano's eruption. Of particular importance is the prediction of hazardous eruptions that could lead to catastrophic loss of life, property, and disruption of human activities.
The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
The geology of Iceland is unique and of particular interest to geologists. Iceland lies on the divergent boundary between the Eurasian Plate and the North American Plate. It also lies above a hotspot, the Iceland plume. The plume is believed to have caused the formation of Iceland itself, the island first appearing over the ocean surface about 16 to 18 million years ago. The result is an island characterized by repeated volcanism and geothermal phenomena such as geysers.
The Cascade Volcanoes are a number of volcanoes in a volcanic arc in western North America, extending from southwestern British Columbia through Washington and Oregon to Northern California, a distance of well over 700 miles (1,100 km). The arc formed due to subduction along the Cascadia subduction zone. Although taking its name from the Cascade Range, this term is a geologic grouping rather than a geographic one, and the Cascade Volcanoes extend north into the Coast Mountains, past the Fraser River which is the northward limit of the Cascade Range proper.
The geology of the Pacific Northwest includes the composition, structure, physical properties and the processes that shape the Pacific Northwest region of North America. The region is part of the Ring of Fire: the subduction of the Pacific and Farallon Plates under the North American Plate is responsible for many of the area's scenic features as well as some of its hazards, such as volcanoes, earthquakes, and landslides.
Natural disasters in Colombia are the result of several different natural hazards that affect the country according to its particular geographic and geologic features. Human vulnerability, exacerbated by the lack of planning or lack of appropriate emergency management, and the fragility of the economy and infrastructure contribute to a high rate of financial, structural, and human losses.
The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over 350 kilometres (220 mi) northwest of the city of Vancouver and about 50 kilometres (31 mi) west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about 30 kilometres (19 mi) long (north-south) and 20 kilometres (12 mi) wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is 2,864 metres (9,396 ft) high, may be the highest volcano in Canada.
The Protezione Civile, officially Dipartimento della Protezione Civile, is the national body in Italy that deals with the prediction, prevention and management of emergency events. It was established in 1992 by legge 24 febbraio 1992, n. 225, which was updated in 2012, and it is supervised by the office of the Prime Minister. The duties of the Protezione Civile are to predict, prevent and manage at national level disasters and catastrophes, both natural and human-made. The main goal is to protect the sake of life, the properties, the settlements and the environment from damage and dangers.
The Mount Cayley volcanic field (MCVF) is a remote volcanic zone on the South Coast of British Columbia, Canada, stretching 31 km (19 mi) from the Pemberton Icefield to the Squamish River. It forms a segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia. Most of the MCVF volcanoes were formed during periods of volcanism under sheets of glacial ice throughout the last glacial period. These subglacial eruptions formed steep, flat-topped volcanoes and subglacial lava domes, most of which have been entirely exposed by deglaciation. However, at least two volcanoes predate the last glacial period and both are highly eroded. The field gets its name from Mount Cayley, a volcanic peak located at the southern end of the Powder Mountain Icefield. This icefield covers much of the central portion of the volcanic field and is one of the several glacial fields in the Pacific Ranges of the Coast Mountains.
The 2002 Mindanao earthquake struck the Philippines at 05:16 Philippine Standard Time on March 6. The world's sixth most powerful earthquake of the year, it registered a magnitude of 7.5 and was a megathrust earthquake. It originated near the Cotabato Trench, a zone of deformation situated between the Philippine Sea plate and the Sunda plate, and occurred very near to the Philippines' strongest earthquake for the 20th century, the 1918 Celebes Sea earthquake.
The Vesuvius red zone is the area designated to be quickly evacuated within a few days in the case of an eruption of Mount Vesuvius. The authorities believe that they will have two weeks' warning of an imminent eruption; the questions that arise are whether the population can be evacuated in time, despite a reluctance to leave their homes; and if there be as much as two weeks' warning in reality.
The 2002 Stromboli tsunami was a tsunami caused by a volcanic eruption on the island of Stromboli, in the Aeolian Islands of Sicily, located on the Tyrrhenian Sea. In May 2002, one of the island's two active volcanoes, called Stromboli, entered a new phase of explosive activity that was initially characterized by gas and ash emission from the summit craters. On 30 December 2002, the seismic network recorded two large collapses of a huge portion of the Sciara del Fuoco, which resulted in the tsunamis. The first landslide was around 13:15 and the second one around 13:23, which lasted for 5–7 minutes. The event caused damages on the eastern coast side of Stromboli and Panarea. These tsunamis have been considered the most violent ones to have struck Stromboli in the past 100 years.
Fabrizio Curcio is an Italian government official, who served as Head of the Civil Protection from 3 April 2015 to 8 August 2017 and again since 26 February 2021.
The Phlegraean Fields red zone is the area at greatest volcanic risk in the Phlegraean Fields, in Italy.