Annals and Antiquities of Rajasthan, or the Central and Western Rajput States of India v2.c27.s7.t4.23

v2.c27.s7.t4.23

I will beg the reader to descend seventy or eighty feet with me to view the stratification of Indawar. First, three feet of good soil; five feet of red sandy earth, mixed with particles of quartz; six feet of an unctuous indurated clay; ¹ [741]—then follows a sand-rock, through which it was necessary to penetrate about sixty feet; this was succeeded by twenty feet of almost loose sand, with particles of pure quartz embedded; nodules and stalactitic concretions of sandstone, quartz, and mica, agglutinated together by a calcareous cement. The interior of the well throughout this last stratum is faced with masonry: the whole depth is more than sixty-five cubits, or forty yards. At this depth a spring of excellent water broke in upon the excavators, which supplies Indawar.