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Besides the ledges of coral, which are covered by the tide, that which generally prevails is the napal, as it is called by the inhabitants, forming the basis of the red cliffs, and not infrequently the beds of the rivers. Though this napal has the appearance of rock it possesses in fact so little solidity that it is difficult to pronounce whether it be a soft stone or only an indurated clay.
Napal and Bhutan were overrun, and the whole northern boundary of India pressed against by this fearful tide of life. To the west, Bokhara, and, even to the south and west, Afghanistan, were swallowed up. Persia, Turkestan, and all Central Asia felt the pressure of the flood. It was at this time that Burchaldter revised his figures. He had been mistaken.
The red napal has by much the smallest proportion of sand, and seems to possess all the qualities of the steatite or soap-earth found in Cornwall and other countries.
Sand is commonly met with at the depth of three or four fathoms, and beneath this a stratum of napal or steatite, which is considered as a sign that the metal is near; but the least fallible mark is a red stone, called batu kawi, lying in detached pieces. It is mostly found in red and white clay, and often adhering to small stones, as well as in homogeneous lumps.
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