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hypothesized that these dunes were created by the action of winds (aeolian) lifting the fine silt fraction from further east. These dunes are oriented along the axis running parallel to the coast and between the latitudes of 8°00′ to 9°30′ N and longitudes 77°18′ to 79°00′ E. The soils also have
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Kurian, N.P.; T.N. Prakash; F. Jose; K.P. Black (2001). "Hydrodynamic
Processes and Heavy Mineral Deposits of the Southwest Coast, India".
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Hendry, D.A. (1987). "Silica and calcium carbonate replacement of plant roots in tropical dune sands, SE India".
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and characteristic red sand and silt dunes. These red soils are thought to have originated in the
Pleistocene.
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Alappat, Linto; Palaniandy
Seralathan, Anil D. Shukla, Kyth Pillai Thrivikramji, Ashok Kumar Singhvi (2013).
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Geological map of southeastern India showing teri zone (marked in blue caret patterning)
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Jayangondaperumal, R. (2014). "Teri Red Sands, Tamil Nadu". In
Vishwas S. Kale (ed.).
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mainly in southeastern India. The landscape consists of sediments dating to the
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calcium deposits replacing the old roots of vegetation. The soil is rich in
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Landscapes and
Landforms of India. World Geomorphological Landscapes
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207:(1981). "Reddening of dune sands—evidence from southeast India".
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and the red colour is derived from haematite originating from
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265:. pp. 211–216.
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