Fairy circles are circular patches of bare ground, typically 2 to 12 meters across, surrounded by a ring of taller grass, found scattered across arid grasslands. The best known examples stretch roughly 2,400 kilometers through the Namib desert from Angola through Namibia into South Africa's Northwestern Cape, and a second population was identified in Western Australia's Pilbara region in 2014, with possible occurrences reported in North Africa, the Middle East, and Madagascar. Their formation is contested: one hypothesis credits sand termites, which some researchers argue create the bare patches and improve soil moisture around their colonies, while a competing hypothesis holds that the circles arise from grasses self-organizing under competition for scarce water, an explanation recent research has emphasized as the one most consistent with field observations. The two known regions may not share a single cause, which has complicated efforts to settle on one unified explanation.
Facts
PeriodicityLife cycle of some 30 to 60 years per circle 1 ScaleCircles 2 to 12 metres in diameter; band extending some 2,400 kilometres from Angola to the Northwestern Cape 1 First DescribedFirst mentioned in technical literature in the 1920s 1 Identification
Distinguishing AppearanceCircular patches of barren land encircled by stimulated grass growth 1 Connections
Demonstrated By
Source Encyclopaedia Britannica
Sources
1. Fairy circle (arid grass formation), Wikipedia
Lifespan section
pass through a life cycle of some 30 to 60 years.
Geographic extent
The circles occur in a band lying about 160 kilometres (100 miles) inland and extending southward from Angola for some 2,400 kilometres (1,500 miles) down to the Northwestern Cape province of South Africa.
History section
first being mentioned in technical literature in the 1920s and intermittently thereafter
Opening paragraph
Fairy circles are circular patches of barren land, varying between 2 and 12 metres (7 and 39 ft) in diameter, often encircled by a stimulated growth of grass.
View the SourceEncyclopaedia Britannica
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