| Chiquimula Volcanic Field | |
|---|---|
 | |
| Highest point | |
| Elevation | 1,192 m (3,911 ft) |
| Coordinates | 14°49′48″N89°33′0″W / 14.83000°N 89.55000°W |
| Geography | |
  Chiquimula Volcanic Field Guatemala | |
| Location | Chiquimula, Guatemala |
| Geology | |
| Mountain type | Volcanic field |
| Last eruption | unknown |
The Chiquimula Volcanic Field is located in the Chiquimula valley in southern Guatemala. [1]
Santa María Volcano is a large active volcano in the western highlands of Guatemala, in the Quetzaltenango Department near the city of Quetzaltenango. It is part of the mountain range of the Sierra Madre.
Pacaya is an active complex volcano in Guatemala, which first erupted approximately 23,000 years ago and has erupted at least 23 times since the Spanish conquest of Guatemala. It rises to an elevation of 2,552 metres (8,373 ft). After being dormant for over 70 years, it began erupting vigorously in 1961 and has been erupting frequently since then. Much of its activity is Strombolian, but occasional Plinian eruptions also occur, sometimes showering the area of the nearby Departments with ash.
Volcán Atitlán is a large, conical, active stratovolcano adjacent to the caldera of Lake Atitlán in the Guatemalan Highlands of the Sierra Madre de Chiapas range. It is within the Sololá Department, in southwestern Guatemala.
Acatenango is a stratovolcano in Guatemala, close to the city of Antigua. It is part of the mountain range of the Sierra Madre. The volcano has two peaks, Pico Mayor and Yepocapa which is also known as Tres Hermanas. Acatenango is joined with Volcán de Fuego and collectively the volcano complex is known as La Horqueta.
The Almolonga volcano, also called "Cerro Quemado" or "La Muela" due to its distinct shape, is an andesitic stratovolcano in the south-western department of Quetzaltenango in Guatemala. Part of the mountain range of the Sierra Madre, the volcano is located near the town of Almolonga, just south of Quetzaltenango, Guatemala's second largest city.
The Decade Volcanoes are 16 volcanoes identified by the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) as being worthy of particular study in light of their history of large, destructive eruptions and proximity to densely populated areas. The Decade Volcanoes project encourages studies and public-awareness activities at these volcanoes, with the aim of achieving a better understanding of the volcanoes and the dangers they present, and thus being able to reduce the severity of natural disasters.
Quezaltepeque is a volcanic field in Chiquimula, Guatemala. It has erupted in the Holocene. It is an area of basaltic lava flows, which erupted from vents along a north–south trending fault without explosions, cutting through Tertiary pyroclastic rocks WNW of Ipala volcano about 5 km south of Quezaltepeque town. These basaltic flows issued passively from vents along a N-S-trending fault without accompanying explosive activity. There are mounds of lava over the vents.
Toozaza Peak is a tuya in the Stikine Ranges of the Cassiar Mountains in northern British Columbia, Canada, located in the Iverson Creek. Toozaza Peak is the summit of a north–south aligned ridge between the head of Toozaza Creek and the head of the Jennings River, just south of the Jennings' divide with the Little Rancheria River headwaters. The Little Rancheria and Toozaza Creek are part of the Liard, while the Jennings is part of the Yukon River drainage via Teslin Lake, and the peak therefore stands astride the line of the Continental Divide. It is part of the Tuya Volcanic Field, a volcanic field associated with the Stikine Volcanic Belt, part of the Northern Cordilleran Volcanic Province.
The Fort Selkirk volcanic field is a monogenetic volcanic field in the Northern Cordilleran Volcanic Province, Yukon Territory, Canada. It is the northernmost Holocene age volcanic field in Canada, located close to the connection of the Yukon and Pelly rivers. The youngest eruptions within the field are unknown. However, the youngest volcano Volcano Mountain produced lava flows that appear to be only a few hundred years old.
The volcano Tacaná is the second highest peak in Central America at 4,060 metres (13,320 ft), located in the Sierra Madre de Chiapas of northern Guatemala and southern Mexico. It is also known in Mexico as Volcán Tacina.
Cerro Santiago is one of the most prominent cinder cones of a volcanic field surrounding the city of Jutiapa in southern Guatemala. Its elevation is 1,192 m.
Volcán de Flores is the most prominent stratovolcano in a volcanic field composed of several small volcanoes in southern Guatemala. With an elevation of 1,600 m, it is located approximately 10 km west of the city of Jutiapa.
The Cuilapa-Barbarena volcanic field is a field of cinder cones in Guatemala with approximately 70 cones. At an elevation of 1,454 m, the field is located over the intersection of the local Jalpatagua fault with the Miocene Santa Rosa de Lima caldera. The youngest cones postdate the last activity phase of Tecuamburro and may be of Holocene age, but with no confirmed evidence.
The San Diego volcanic field is an extensive volcanic field on the El Salvador–Guatemala border of Central America. It consists of a group of basaltic cinder cones and lava flows, with the largest feature being Volcán de San Diego after which the volcanic field is named.
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