Joseph Skey

Summary

Joseph Skey On the Geology of Barbadoes (1816)

Even in the island of St. Vincent, where the quantity of rain is so much greater, failure perpetually follows the attempt; probably because we are ignorant of the successive means that have been required to produce the luxuriant vegetation which, under natural operations, springs from rocks almost bare of mould; and because too, we attempt to produce in a few years effects which have required ages to accomplish.
Source: Wikisource

Joseph Skey On the Geology of Barbadoes (1816)

The land, which when seen from the sea appears to rise uniformly from the coast, is observed on a nearer view to consist of successive terraces rising in two or three gradations one above the other; each terrace forming a plain of a quarter or half a mile in breadth, and terminated by a cliff of coral rock, varying in elevation from twelve to more than twenty feet; sometimes indeed having a considerably greater height.
Source: Wikisource

Joseph Skey On the Geology of Barbadoes (1816)

Marigalante, Antigua, and Santa Cruz also have a common structure with Barbadoes; they all agree in being of moderate elevation, have no volcanic traces, and are all formed of limestone rock; of this however I have no personal knowledge. Barbadoes is in great part composed of fossil madrepores, and traces of organic structure are to be met with in almost every part of the island.
Source: Wikisource

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