Moradi Formation

The Moradi Formation is a geological formation in Niger. It is of Late Permian age. It is informally divided into three subunits. The lower portion of the formation consists of red mudstone, with muddy calcareous sandstone and quartz-granlule conglomerate present as lenses. The middle portion consists of muddy siltstone in thick beds interbedded with red argillaceous sandstone. The lower two thirds of the upper portion of the formation consist of red siltstone intercalated with channel lag intraformational conglomerates, while the upper third consists of barchanoid shaped lenses of conglomeratic sandstone with ventifacts.^[1] These facies are indicatived of deposition under arid conditions, with less than 300 millimetres (12 in) of annual rainfall in the Central Pangean desert, with annual temperatures of 30 to 35 °C (86 to 95 °F), but with ephemeral water presence including lakes.^[2]

TypeGeological formation

Unit ofIzégouandane Group

Sub-unitsLower, Middle and Upper Units

UnderliesTeloua 1 Formation

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Moradi Formation
Stratigraphic range: Lopingian ~259–252 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Type	Geological formation
Unit of	Izégouandane Group
Sub-units	Lower, Middle and Upper Units
Underlies	Teloua 1 Formation
Overlies	Tamamaït Formation
Thickness	100 metres (330 ft)
Lithology
Primary	Mudstone, siltstone
Other	Sandstone, conglomerate
Location
Coordinates	18.8°N 7.2°E / 18.8; 7.2
Approximate paleocoordinates	16.6°S 8.2°E / -16.6; 8.2
Region	Agadez Region
Country	Niger
Extent	Iullemmeden Basin
Moradi Formation (Niger)

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