Abstract

Ever since Gregory's work at the turn of the century, the extensional structures extending through central Kenya have been recognized as the classic example of a continental rift zone. Because of the scale and variety of rift features present, this locality has fascinated geologists and geophysicists since its discovery.

Original languageEnglish
Pages (from-to)345-351
Number of pages7
JournalEos
Volume73
Issue number33
DOIs
Publication statusPublished - 18 Aug 1992
Externally publishedYes

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