Abstract
In the map appended to the ‘Report on the Geology of Trinidad,’ we find the principal Tertiary coal-bearing strata of the Island indicated by a more or less irregular band of dark colour, strectching from Chaguanas, Couva, and Savonetta, on the western or Parian coast, to Manzanilla on the eastern or Atlantic side. To the north of this band lies a sterile region of detrital matter, chiefly siliceous, marked in the map by yellow with res sponts. I wish to draw attention more particularly to that part of this latter formation which lies on the eastern coast between the River Matura and Saline Bay.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
