Deccan Traps, India

17-24N, 43-47E
Elevation: 4,000 feet (1,200 m)


The Deccan Traps are one of the largest volcanic provinces in the world. It consists of more than 6,500 feet (>2,000 m) of flat-lying basalt lava flows and covers an area of nearly 200,000 square miles (500,000 square km) (roughly the size of the states of Washington and Oregon combined) in west-central India. Estimates of the original area covered by the lava flows are as high as 600,000 square miles (1.5 million square km). The volume of basalt is estimated to be 12,275 cubic miles (512,000 cubic km)(the 1980 eruption of Mount St. Helens produced 1 cubic km of volcanic material). The Deccan Traps are flood basalts similar to the Columbia River basalts of the northwestern United States. This photo shows a thick stack of basalt lava flows north of Mahabaleshwar. Photograph by Lazlo Keszthelyi, January 28, 1996.


The Deccan basalts may have played a role in the extinction of the dinosaurs. Most of the basalt was erupted between 65 and 60 million years ago. Gases released by the eruption may have changed the global climate and lead to the demise of the dinosaurs 65 million years ago. This photo shows the Deccan Tarps between Mambai and Mahabaleshwar. Photograph by Lazlo Keszthelyi, January 27, 1996.


Vocanologists are also trying to understand how such great volumes of lava are erupted. Early models proposed that lava flooded across large areas at extremely rapid rates. Recently proposed models suggested that at least some of the flows are emplaced at gradual rates, lasting months to years. This photo shows the Ajunta Caves, temples carved into the basalts. Note the school group for scale. Photograph by Lazlo Keszthelyi, January 31, 1996.

More information on the Deccan

Sources of Information:

Bhattacharji, S., Chatterjee, N., Wampler, J.M., Nayak, P.N., and Deshnukh, S.S., 1996, Indian intraplate and continental margin rifting, lithospheric extension, and mantle upwelling in Deccan flood basalt volcanism near the K/T boundary: evidence from mafic dike swarms: Journal of Petrology, v. 104, p. 379-398.

Beane, J.E., Turner, C.A., Hooper, P.R., and Subbarao, K.V., and Walsh, J.N., 1986, Stratigraphy, composition and form of the Deccan Basalts, western Ghats, India.

Krishnan, M.S., 1953, The structural and tectonic history of India: Mem. Geological Survey of India, 81: 109 p.

Officer, C.B., and Drake, C.L., 1985, Terminal Cretaceous environment events: Science, v. 227, p. 1161-1167.

Rampino, M.R., and Stothers, R.B., 1988, Flood basalt volcanism during the past 250 million years: Science, v. 241, p. 663-668.

Self, S., Thordarson, T., and Keszthelyi, L., 1996, Inflation features as keys to the emplacement of pahoehoe lava flow fields in the Columbia River Basalt Group, in Conference Abstracts Long Lava Flows, Whithead, P., ed.: James Cook University, Queensland, p. 72-73.

Self, S., Finnemore, S.L., Walker, G.P.L., and Thordarson, T., 1993, How are flood basalt lavas emplaced? -- A case of the tortoise and the hare, IAVCEI Abstracts, Canberra, Australia, p. 98.

White, R.S., and McKenzie, D.P., 1989, Magmatism at rift zones: the generation of volcanic continental margins and flood basalts: Journal of Geophysical Research, v. 94, p. 7,685-7,730.



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