Ali Barbour's Cave is thought to be between
120,000 and 180,000 years old. Situated about 30km south of Mombasa
and 200m back from the high water mark, it compromises a series
of interlinking chambers at depths of up to 10 m below ground level.
It is part of a vast cave complex which penetrates miles
inland as far as the original coast line.
The cave is exactly as when it was discovered,
except the chamber housing the kitchen and toilets which had to be modified for
functional reasons.
In the Restaurant only the stone floor has been added
together with furniture and fittings, lighting and sound effects.
The natural holes in the roof crust are open to the sky, protected
in bad weather with sliding covers. |
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Take your time,
look around
and enjoy your meal...
Our cuisine
is typically international
and we specialize
in seafood.
We are open for dinner only
and closed
on Christmas Day.
There is also a bus available to collect clients
from anywhere
on Diani Beach.
During the season it is advisable to book tables in advance
by contacting
our office
on
Tel 254 (040) 3202033
and 254 (040) 3203003
Dress: Long trousers for men. |
A triangular makuti umbrella soars over the cocktail bar and reception
areas supported by a single blue gum pole over 50 feet high (nearly
20 m).
It is thought the cave owes its origin to a subterranean
solution beneath the water-table and was subsequently breached and then modified
by dramatic changes in the sea-level, tidal and wave action, and engulfment of
surface streams through the ages.
The cave was formed in coral reef limestone which
grew up from the sea floor in, what the geologists call, the Middle Pleistocene Period,
perhaps over 400.000 years ago.
At the time the sea level was over 100 feet (30m)
higher than it is today and the cave was submerged some 60 feet (20m) below
the surface.
The cave itself developed some 250,000
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years later in the Upper Pleistocene Period. Nothing much happened
for the next 15,000 years or so until it was converted into a restaurant
in 1983.
The interesting geological features to
be found in the cave include stalactite formations, fossil shells,
corals and flow stones.
The finest coral examples in
the cave are located in the serving area where massive corals,
stalactite flowstone drapery feature together with a beautiful
fan-shaped formation high up in the north-west corner.
The restaurant also displays many corals, particularly
on the north and west walls, including a large colony on the buttress leading
into the main dining area. In the sunken dome chamber
at the end of the restaurant, small stalactites hang from the roof and coral "twigs" appear
in the east wall together with thick calcite bends which appear to represent
cross-sections through large shells, perhaps giant clams.
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