| dc.contributor.author | Skinner, N J | |
| dc.contributor.author | Bhatt, N V | |
| dc.contributor.author | Hastenrath, S | |
| dc.date.accessioned | 2014-04-29T09:44:30Z | |
| dc.date.available | 2014-04-29T09:44:30Z | |
| dc.date.issued | 1974-08-16 | |
| dc.identifier.citation | Nature, Volume 250, Issue 5467, pp. 561-562 (16 August 1974). (Nature Homepage) | en_US |
| dc.identifier.uri | http://adsabs.harvard.edu/abs/1974Natur.250..561S | |
| dc.identifier.uri | http://www.nature.com/nature/journal/v250/n5467/abs/250561a0.html | |
| dc.identifier.uri | http://hdl.handle.net/11295/66146 | |
| dc.description.abstract | MOUNT Kenya is a large central volcano just south of the equator in central Kenya. It rises to a height of 5,199 m above sea level. The base of the volcano covers an area of approximately 7,000 sq km, and is roughly circular in plan with an average diameter of 105 km. A detailed geological study1 indicated that some 1,500 m of the upper part of the mountain has been removed by erosion since the volcano was formed in the Plio-Pleistocene. | en_US |
| dc.language.iso | en | en_US |
| dc.title | Negative magnetic anomaly associated with Mount Kenya | en_US |
| dc.type | Article | en_US |
