Quezaltepeque is a volcanic field in Chiquimula, Guatemala. It has erupted in the Holocene. It is an area of basaltic lava flows was 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]
Quezaltepeque | |
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Highest point | |
Elevation | 1,200 m (3,900 ft)[1] |
Listing | Volcanoes in Guatemala |
Coordinates | 14°34′N 89°27′W[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 eruption | Unknown[1] |
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