PhotosLocation


quezaltepeque+volcano Latitude and Longitude:

14°34′N 89°27′W / 14.567°N 89.450°W / 14.567; -89.450
From Wikipedia, the free encyclopedia
Quezaltepeque
Quezaltepeque is located in Guatemala
Quezaltepeque
Quezaltepeque
Highest point
Elevation1,200 m (3,900 ft) [1]
Listing Volcanoes in Guatemala
Coordinates 14°34′N 89°27′W / 14.567°N 89.450°W / 14.567; -89.450 [1]
Naming
Etymology"at the quetzal feather hill" or "at the tall upstanding hill"
Language of name Nahuatl
Geography
Location Chiquimula, Guatemala
Geology
Mountain type Volcanic field
Last eruptionUnknown [1]

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. [1]

References

  1. ^ a b c d "Quezaltepeque". Global Volcanism Program. Smithsonian Institution. Retrieved 2020-03-21.

quezaltepeque+volcano Latitude and Longitude:

14°34′N 89°27′W / 14.567°N 89.450°W / 14.567; -89.450
From Wikipedia, the free encyclopedia
Quezaltepeque
Quezaltepeque is located in Guatemala
Quezaltepeque
Quezaltepeque
Highest point
Elevation1,200 m (3,900 ft) [1]
Listing Volcanoes in Guatemala
Coordinates 14°34′N 89°27′W / 14.567°N 89.450°W / 14.567; -89.450 [1]
Naming
Etymology"at the quetzal feather hill" or "at the tall upstanding hill"
Language of name Nahuatl
Geography
Location Chiquimula, Guatemala
Geology
Mountain type Volcanic field
Last eruptionUnknown [1]

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. [1]

References

  1. ^ a b c d "Quezaltepeque". Global Volcanism Program. Smithsonian Institution. Retrieved 2020-03-21.

Videos

Youtube | Vimeo | Bing

Websites

Google | Yahoo | Bing

Encyclopedia

Google | Yahoo | Bing

Facebook