that had been in the sand under the chalk, and which by the sinking of the chalk was squeezed out like so much dough. It remained as a reef for some years, but has now totally disappeared, having been carried away by the waves.
As the great chasm was formed, the masses from the sides falling in were, as it were, mumbled and chewed up in the depths, and to the eyes of the frightened spectators sent forth flashes of light; they also supposed that an intolerable stench was emitted from the abyss. But this was no more than the odours given out by the violent attrition of the cherty sandstone and chalk grinding against each other as they descended.
Throughout the 26th the subsided masses of the great chasm continued sinking, and the elevated reef gradually rising; but by the evening of that day everything had settled very nearly into the position in which it remains at present, although edges have since lost their sharpness and minor rents have been choked.
A writer whose reminiscences have been recently published describes briefly the aspect of the place after the sinkage.
"I rode over to see this huge landslip. The greater part of a farm had subsided a hundred feet or more. Hedges and fields, with their crops of turnips, etc., were undisturbed by the fall, and broken off sharply from the ground a hundred feet above. There was a rather dislocated ridge on the shore, which formed a sort of moraine to the slip. On this part were some cottages twisted about, but still holding together, and having their gardens and even their wells attached; yet the shock of the falling mass had been so great as to cause the upheaval of an island off shore."
