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Haruj information


Haruj
Haroudj
Haruj seen from space
Highest point
Elevation1,200 m (3,900 ft)
ListingGaret es Sebaa
Coordinates27°15′N 17°30′E / 27.25°N 17.5°E / 27.25; 17.5"Haruj". Global Volcanism Program. Smithsonian Institution.
Naming
Native nameهروج (Arabic)
Geography
Haruj is located in Libya
Haruj
Haruj
CountryLibya
DistrictJufra
Geology
Age of rockPliocene to Holocene
Mountain typeVolcanic field
Type of rockTholeiitic-alkali basalt
Last eruption2,310 ± 810 years ago

Haruj (Arabic: هروج, also known as Haroudj[1]) is a large volcanic field spread across 42,000–45,000 km2 (16,000–17,000 sq mi) in central Libya. It is one of several volcanic fields in Libya along with Tibesti, and its origin has been attributed to the effects of geologic lineaments in the crust.

It contains about 150 volcanoes, including numerous basaltic scoria cones and about 30 small shield volcanoes, along with craters and lava flows. Most of the field is covered by lava flows that originated in fissure vents; the rest of the flows originated within small shield volcanoes, stratovolcanoes and scoria cones. Some of these vents have large craters. Volcanism in Haruj blocked ancient rivers and led to the formation of Lake Megafezzan.

Volcanic activity in Haruj commenced about 6 million years ago and continued into the late Pleistocene. There are a number of individual lava flow generations that were emplaced in the Haruj volcanic field, the most recent ones in the Holocene 2,310 ± 810 years ago. There are reports of solfataric activity.

  1. ^ Klitzsch 1968, p. 587.

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in the wadis of the north and west. The northeast area is dominated by Haruj, a large and unpopulated volcanic field. Fezzan's population has grown rapidly...

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Dust storms lasting four to eight days are common during Spring. Vast Haruj volcanic field is largest geographic features, visible from space. Per the...

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