John Caldecott,
Madras Journal of Literature and Science
(1837)
“ The hill on which the observatory is erected is a solid mass of laterite, in which granite is largely disseminated, and is so hard as to be penetrated with great difficulty; but little depth was therefore required for the foundations, which are accordingly only sunk one foot below the surface, on which the granite bases for the instruments are erected—this surface is by excavation three feet below the general level of the soil outside, and three and a half feet below the floor of the observing rooms. ”
