370 THE EMPTY QUARTER by Mr. Philby as * accretions/ evidently without any knowledge of their real nature. They are fulgurites or lightning-tubes, produced when discharges of lightning strike the ground, the intense heat of the powerful spark fusing the quartz sand along the path of the electric current. The inside of such tubes of silica-glass is always smooth and glazed, and the outside is rough with adhering grains of partly fused sand. The walls are usually very thin and friable, and specimens can be collected only as fragments. Though roughly cylindrical, the tubes taper away downwards and are sometimes branched. When flattened they often have thin flanges of fused material projecting from the sides of the tube : these have been called * winged fulgurites.' The most complete specimen in the Mineral Collection of the British Museum is a portion 3 feet in length of a tube 1-1 £ inches in diameter, from Maldonado, Uruguay ; and the longest, but made up of pieced fragments, is nearly 16 feet in length, from near Dresden. A fulgurite in the sand-dunes at Drigg on the coast of Cumberland was traced for 30 feet without reaching the end. Specimens are very rarely found and are not common in collections. The specimens collected by Mr. Philby are fragments found loose on the surface of the sand. They were found in hollows between the sand-dunes, and an interesting fact is that they are taken by the Arabs as indications of the presence of water. No doubt the lightning would strike in the wetter and more conduct- ing parts of the ground. (1). From Bard Jallab (collected 9/2/32).—Narrow tubes | cm, in diameter, the longest fragment 7 cm. in length. These are cylindrical and straight and are remarkable in having very thick walls, there being only a thread-like central cavity. Nearly the whole of the fulgurite here consists of a grey silica-glass full of small bubbles. This suggests that the lightning struck dry sand, and that there was very little radial expansion of the tube caused by the pressure of water-vapour. One piece shows a division into two branches. (2). Bani Jafnan (18/2/32).—Fragments of irregular shape with spine-like projections, Here the walls are thin and the central cavity large with inside glazing. The largest fragment is 3J cm. long with a flattened cross-section of about 1'J x J cm. (3). Eibaka Qa'amiyat (24/2/32), about 40 miles west of Shanna.—Broken fragments of flattened tubes with projecting spines and wings. The walls are thick but with a well-marked central cavity, being intermediate between those in (1) and (2). The largest fragment is 4 cm. long with a cross-section of about 2x1 cm.