Belfry Bulletin Number 045

Page 1

The

Belfry

Bulletin

THE JOURNAL OF THE BRISTOL EXPLORATION CLUB Volume 5 No.45

March 1951

We very much regret that this issue of the Belfry Bulletin has been seriously delayed by various changes that have taken place in the Club organization. We hope that this issue will be followed by the April number shortly, and that, things will return to normal with the May number. Club Organisation The Committee has to announce with the deepest regret the resignation of Mr. T.H. Stanbury from the position of Secretary which he has filled for so many years. Sybil Bowden-Lyle has also resigned as Assistant Secretary. The club owes these members a great debt of gratitude for the grand work they have done, much of it quite unknown to members outside the committee. A very considerable re-organisation of the Committee’s work has been called for by these resignations. The present set-up is as follows: General Secretary D.H. Hasell Caving Secretary M. Hanam Climbing Section Secretary R.W.G. Cantle Ladies Representative Miss J. Rollason Hut Warden R.A. Setterington Librarian J.W. Ifold Editor B.B. W.J. Shorthose (London section) Publisher K. Dobbs. Tackle Office G.T. Lucy In addition to the above who constitute the Committee, R. Ifold is acting as Sales Secretary. This list, with addresses, is reproduced on the back of the library list circulated with this Bulletin, and all members are asked to ensure as far as possible that they address their enquiries to the right official in the first instance. ANNUAL GENERAL MEETING Owing to the re-organisation mentioned above, we regret that no report of the Annual General Meeting is available for this issue, but we hope that it will be possible to include it next time. The Growth of Stalagmites and Stalactites PART II by R.M. WALLIS In the first part of this article we showed that the change in pressure which a water drop undergoes on appearing on a cave roof must be considered an essential part in the forming of a stalactite. This feature can only occur once to each drop, so how is it that stalagmites are formed? We have seen that the calcium carbonate appears in the drop as very small particles which are drawn into a ring round the edge. This process of course takes time and if the rate of drip is relatively fast only a small amount of carbonate will be left on the roof. The rest will fall with the drop, which will then trickle over the stalagmite and the rest of the carbonate will be deposited. The relative sizes of the –mite and –tite are thus seen to depend on the rate of drip. A slow drip will give a large stalactite and a small stalagmite; a fast drip vice versa. FLOWSTONE and other deposits covering large areas occur in the same way as stalagmites, the water appearing in some crack in the wall and the carbonate being deposited as the water trickles down.


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