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 language | English |
|---|---|
| Pages (from-to) | 345-351 |
| Number of pages | 7 |
| Journal | Eos |
| Volume | 73 |
| Issue number | 33 |
| DOIs | |
| Publication status | Published - 18 Aug 1992 |
| Externally published | Yes |
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