The next day I ascended Le Pouce, a mountain so called from a thumb-like projection, which rises close behind the town to a height of 2600 ft. The centre of the island consists of a great platform, surrounded by old broken basaltic mountains, with their strata dipping seawards. The central platform, formed of comparatively recent streams of lava, is of an oval shape, thirteen geographical miles across, in the line of its shorter axis. The exterior bounding mountains come into that class of structures called Craters of Elevation,which are supposed to have been formed not like ordinary Craters, but by a great and sudden upheaval.
The Surveyor General of Mauritius invited me to stay at his country house and took me to see some of the island’s geological features.