434 Transactions of the South African Philosophical Society. 



On the coast near Cape Infanta there is a large cave, opening by 

 a small hole on the face of a great limestone cliff. The upper part 

 of the cliff overhangs very considerably, and long stalactites hang 

 from it. The interior of the cave must be at least 20 ft. high in 

 parts. The roof is entirely formed of stalactites from which water 

 constantly drops. The floor is of sand and guano. This cave is 

 situated near the bottom of the limestone, and at the entrance is 

 seen the boulder bed already mentioned as being probably a beach. 

 The length and breadth of the cave are not great, probably less than 

 50 yards. The general appearance of the interior is very like that 

 of the Cango cave. 



Fig 2. — Cave in Recent Limestone near Cape Infanta. 



There is no running stream of water in the cave, although one 

 may possibly have been there formerly, and would then have been 

 the cause of its formation. The cave is on Mr. Paul Dunn's farm, 

 and was discovered by him in 1847 when he tracked a leopard into it. 



On the coast near Stanford Cove there is a cave known as the 

 Kellers. It lies between the limestone above and the Table Moun- 

 tain Sandstone below, although the opening is entirely surrounded 

 by the latter rock. A stream of water issues from the opening. 

 There are other and larger streams flowing from between the lime- 

 stone and Table Mountain sandstone in the neighbourhood. 



