Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-23T16:34:37.188Z Has data issue: false hasContentIssue false

Geological Notes on the Island of Dominica, B.W.I

Published online by Cambridge University Press:  01 May 2009

Extract

The island of Dominica is situated in lat. 15° 20′ N., and long. 62° 30′ W., and lies almost midway between the French islands of Guadeloupe (on the north) and Martinique (on the south). In the northern channel the Antillean plateau is submerged to a depth of about 2,100 feet, but in the southern a deep embayment entering from the west reaches a maximum depth of 6,600 feet. Some miles to the south-east of Dominica, however, the sea floor rises to within 270 feet of the surface, while the Madiana banks, east of Martinique and north of Barbados, are submerged only to about the dame depth. Lying as they do between the sedimentary parts of Antigua, Guadeloupe, and Barbados it would be interesting to ascertain, if possible, by boring, whether these banks are of a sedimentary nature in contrast to the volcanic nature of the main range of islands. On both the windward and leeward sides Dominica rises precipitously out of the sea, but this is more accnetuated on the leeward side where within six or seven miles of the shore the sea bottom reaches a depth of over a thousand fathoms. The preciepitous nature of the sea floor and the absence, of any sort of harbour at Roseau—the capital—render anchorage even at favourable times a very precarious matter, and one of great difficulty and danger in rough weather.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1928

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

BIBLIOGRAPHY

1882. Cleve, P. T.The North-Eastern West Indies”: Trans. Roy. Swed. Acad. Sci. Stockholm.Google Scholar
1895. Spencer, J. W.The Reconstruction of the Antillean Continent”: Geol. Soc. Amer. Bull., vol. vi.Google Scholar
1898. Spencer, J. W.The West Indian Bridge between North and South America”: Pop. Sci. Monthly, vol. lxiii.Google Scholar
1901–2. Spencer, J. W.The Windward and Leeward Islands”: Trans. Canad. Inst.Google Scholar
1902. Spencer, J. W.On the Geological and Physical Development of Dominica, etc”: Q.J.G.S., vol. lviii.Google Scholar
1903. Sapper, K. von.Ein besuch der Insel Dominica”: Centralblatt für Min., Geol. u. Pal.Google Scholar
1905. Hill, R. T.The Evolution of the Windward Archipelago”: Bull. Geol. Soc. Amer., vol. xvi.Google Scholar
1905. Hovey, E. O.The Boiling Lake of Dominica”: Bull. Geol. Soc. Amer., vol. xvi.Google Scholar
1906. Symington-Grieve, . Notes on the Island of Dominica, A. & C. Black, London.Google Scholar
1918. Vaughan, T. W.Geologic History of Central America and the West Indies during Caenozoic times”: Geol. Soc. Amer. Bull. 29.CrossRefGoogle Scholar
1922. Hardy, F.The Soils of Dominica”: West Indian Bull., vol. xix.Google Scholar
1926. Davis, William Morris. “The Lesser Antilles”: Amer. Geog. Soc. New York.Google Scholar