Earthquake
An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves.
Tsunami
A tsunami also called a tsunami wave train, and at one time incorrectly referred to as a tidal wave, is a series of water waves caused by the displacement of a large volume of a body of water, usually an ocean, though it can occur in large lakes.
Tornado
A tornado (often referred to as a twister or, erroneously, a cyclone) is a violent, dangerous, rotating column of air that is in contact with both the surface of the earth and a cumulonimbus cloud or, in rare cases, the base of a cumulus cloud.
Floods
A flood is an overflow of an expanse of water that submerges land. The EU Floods directive defines a flood as a temporary covering by water of land not normally covered by water
Volcanic Eruptions
Volcanoes can cause widespread destruction and consequent disaster through several ways. The effects include the volcanic eruption itself that may cause harm following the explosion of the volcano or the fall of rock.
Largest Volcanic Explosive Eruptions
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Posted by Disaster
In explosive eruptions, the eruption of magma is driven by the rapid release of pressure, often involving the explosion of gas previously dissolved within the material. The most famous and destructive historical eruptions are mainly of this type. An eruptive phase can consist of a single eruption, or a sequence of several eruptions spread over several days, weeks or months. Explosive eruptions usually involve thick, highly viscous felsic magma, high in volatiles like water vapor and carbon dioxide. Pyroclastic materials are the primary product, typically in the form of tuff. Eruptions the size of that at Lake Toba 74 thousand years ago (2800 km3 or more) occur worldwide every 50,000 to 100,000 years.
Volcano—Eruption | Age (Ma) | Location | Volume (km3) | Notes |
---|---|---|---|---|
Guarapuava —Tamarana—Sarusas | 132 | Paraná and Etendeka traps | 8,600 | |
Santa Maria—Fria | ~132 | Paraná and Etendeka traps | 7,800 | |
Guarapuava —Ventura | ~132 | Paraná and Etendeka traps | 7,600 | |
Sam Ignimbrite and Green Tuff | 29.5 | Yemen | 6,800 | Volume includes 5550 km³ of distal tuffs. This estimate is uncertain to a factor of 2 or 3. |
Goboboseb–Messum volcanic centre—Springbok quartz latite unit | 132 | Paraná and Etendeka traps, Brazil and Namibia | 6,340 | |
Caxias do Sul—Grootberg | ~132 | Paraná and Etendeka traps | 5,650 | |
La Garita Caldera—Fish Canyon tuff | 27.8 | San Juan volcanic field, Colorado | 5,000 | Commonly regarded as the largest tuff ever measured on Earth, or largest confidently-measured tuff on earth. It is part of at least 20 large caldera-forming eruptions in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma. |
Jacui—Goboboseb II | ~132 | Paraná and Etendeka traps | 4,350 | |
Ourinhos—Khoraseb | ~132 | Paraná and Etendeka traps | 3,900 | |
Jabal Kura'a Ignimbrite | 29.6 | Yemen | 3,800 | Volume estimate is uncertain to a factor of 2 or 3. |
Windows Butte tuff | 31.4 | William's Ridge, central Nevada | 3,500 | Part of the Mid-Tertiary ignimbrite flare-up |
Anita Garibaldi—Beacon | ~132 | Paraná and Etendeka traps | 3,450 | |
Indian Peak Caldera Complex—Wah Wah Springs tuff | 29.5 | Eastern Nevada/Western Utah | 3,200 | Indian Peak Caldera Complex total volume over 10,000 cubic km, Wah Wah Springs tuff being the largest |
Oxaya ignimbrites | 19 | Chile | 3,000 | Really a regional correlation of many ignimbrites originally thought to be distinct |
Lund Tuff | 29 | Great Basin, USA | 3,000 | Similar in composition to the Fish Canyon Tuff |
Lake Toba—Youngest Toba Tuff | 0.073 | Sunda Arc, Indonesia | 2,800 | Largest eruption on earth in at least the last 25 million years, responsible for the Toba catastrophe theory, a population bottleneck of the human species |
Pacana Caldera—Atana ignimbrite | 4 | Chile | 2,800 | Forms a resurgent caldera. |
Iftar Alkalb—Tephra 4 W | 29.5 | Afro-Arabian | 2,700 | |
Yellowstone caldera—Huckleberry Ridge Tuff | 2.059 | Yellowstone hotspot | 2,450 | Largest Yellowstone eruption on record |
Whakamaru | 0.254 | Taupo Volcanic Zone, New Zealand | 2,000 | Largest in the Southern Hemisphere in the Late Quaternary |
Palmas BRA-21—Wereldsend | 29.5 | Paraná and Etendeka traps | 1,900 | |
Kilgore tuff | 4.3 | Near Kilgore, Idaho | 1,800 | Last of the eruptions from the Heise volcanic field |
Sana'a Ignimbrite—Tephra 2W63 | 29.5 | Afro-Arabian | 1,600 | |
Millbrig eruptions—Bentonites | 454 | England, exposed in Northern Europe and Eastern US | 1,509 | One of the oldest large eruptions preserved |
Blacktail tuff | 6.5 | Blacktail, Idaho | 1,500 | First of several eruptions from the Heise volcanic field |
Emory Caldera—Kneeling Nun tuff | 33 | Southwestern New Mexico | 1,310 | |
Timber Mountain tuff | 11.6 | Southwestern Nevada | 1,200 | Also includes a 900 cubic km tuff as a second member in the tuff |
Paintbrush tuff (Topopah Spring Member) | 12.8 | Southwestern Nevada | 1,200 | Related to a 1000 cubic km tuff (Tiva Canyon Member) as another member in the Paintbrush tuff |
Bachelor—Carpenter Ridge tuff | 28 | San Juan volcanic field | 1,200 | Part of at least 20 large caldera-forming eruptions, including the world's largest, the Fish Canyon tuff in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma |
Bursum—Apache Springs Tuff | 28.5 | Southern New Mexico | 1,200 | Related to a 1050 cubic km tuff, the Bloodgood Canyon tuff |
Taupo Volcano—Oruanui eruption | 0.027 | Taupo volcanic zone, New Zealand | 1,170 | Most recent VEI 8 eruption |
Huaylillas Ignimbrite | 15 | Bolivia | 1,100 | Predates half of the uplift of the central Andes |
Bursum—Bloodgood Canyon tuff | 28.5 | Southern New Mexico | 1,050 | Related to a 1200 cubic km tuff, the Apache Springs tuff |
Yellowstone Caldera—Lava Creek Tuff | 0.639 | Yellowstone hotspot | 1,000 | Last large eruption in the Yellowstone National Park area |
Cerro Galán | 2.2 | Catamarca Province, Argentina | 1,000 | Elliptical caldera is ~35 km wide |
Paintbrush tuff (Tiva Canyon Member) | 12.7 | Southwestern Nevada | 1,000 | Related to a 1200 cubic km tuff (Topopah Spring Member) as another member in the Paintbrush tuff |
San Juan—Sapinero Mesa Tuff | 28 | San Juan volcanic field | 1,000 | Part of at least 20 large caldera-forming eruptions, including the world's largest, the Fish Canyon tuff in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma |
Uncompahgre—Dillon & Sapinero Mesa Tuffs | 28.1 | San Juan volcanic field | 1,000 | Part of at least 20 large caldera-forming eruptions, including the world's largest, the Fish Canyon tuff in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma |
Platoro—Chiquito Peak tuff | 28.2 | San Juan volcanic field | 1,000 | Part of at least 20 large caldera-forming eruptions, including the world's largest, the Fish Canyon tuff in the San Juan volcanic field and surrounding area that formed around 26 to 35 Ma |
Mount Princeton—Wall Mountain tuff | 35.3 | Thirtynine Mile volcanic area, Colorado | 1,000 | Helped cause the exceptional preservation at Florissant Fossil Beds National Monument |