Kissanga, when it encounters a body of salt water filling this deep gully. It then runs over this denser water with decreased depth and increased velocity, the layer of fresh water being deeper with the ebb tide and shallower... Sessional Papers - Page 14by Great Britain. Parliament. House of Commons - 1900Full view - About this book
| Geography - 1900 - 816 pages
...of the undercurrents and a comparison with that at the surface. The results are summarized thus : *' The observations appear to show that the fresh water...to the bottom until reaching the head of the Congo cailon just below Eissanga, when it encounters a body of salt water filling this deep gully. It then... | |
| |