The  role  of  plate  tectonics
 
As the Caribbean plate broke away from the South American plate and slowly  moved northwards pressure within and beneath the mantel caused deformations  to occur on the ocean floor. This intense build up of pressure caused faults to  develop. The continued movement of the plate forced parts of the earth`s crust  between  fault-lines  to  be  pushed  upwards .
 
This upward movement of the ocean floor was also accompanied by folding of the  rocks into synclines, anticlines and recumbent folds. Over millions of years this  combination of folding and faulting eventually lead to an emergent block of land  which became Barbados.
 
The  role  of  corals
 
Barbados` geology consists entirely of limestone and the reason for this can be  found in its geologic history. In the tropical waters of the Caribbean ideal  conditions for coral growth existed. The ocean currents that circulated the  equator are warm which provided the corals on the ocean floor with suitable  temperatures as well as nutrients.
 
Over time the coral colony gradually grew extending itself several kilometers  across the ocean floor and several kilometers thick. These coral limestone were  important because they not only gave rise to Barbados` unique shape, but also  the physical characteristics of the island. As the ocean floor continued to rise the  hard coral limestone became emerged to form the island of Barbados.
 
Surface  geology  of  Barbados
 
Many of the Caribbean islands of the island arc such as Martinique,  Grenada and  St. Vincent display very high mountain ranges due to their volcanic origin . Barbados, on the other hand, is almost flat except for some very small hills. This is  because during its formation the entire block of coral limestone was uplifted to  form a flat surface.
 
In addition to this,  years of chemical, biological and mechanical weathering of the  limestone ensured that the landsurface was flat. One very unique feature of  Barbados is that there are no surface rivers on the  island. This is because  limestone is  very porous and eaisly eroded away.
 
There are, however, an abundance of subterranean features such as sinkhole , underground caves and subterranean streams. The underlying layers of Barbados  consists of complex networks of these features.
 
IF BARBADOS HAS NO SURFACE RIVERS THEN WHERE DOES THE  COUNTRY GET ITS WATER SUPPLY  FROM ?  All of the country`s drinking water is obtained from  underground sources. There are many aquifers located across the island that  provide what is considered to be among the purest supplies of water in the world.
 
The island is dotted with many caves which are among the most popular tourist  attractions to visit. Harrisons cave is a good example of these physical forces that  continue to shape the  island. Within the cave pools, stalgamites, stalactites, pillars  and flow stones {formed thousands of years ago} show the effects of weathering  and erosion.
 
Did  Dinosaurs  Inhabit  Barbados ?
 
Unlike Trinidad, dinosaurs did not inhabit Barbados. There are several reasons for  this. The island is relatively young when compared to the age of the continents. There are, however, fossils of marine organisms such as mollusc, fishes and coral  that can be found.The old raised beach terraces which can be found on coastal  areas are a good place to start looking for fossil remains.
 
Because Trinidad was once connected to Venezuela on the South American  continent, dinosaurs fossils will be present on this island. In fact the leg bone of a  GIANT  SLOTH was found in south Trinidad. The fossil is now on exhibit at the  National History Museum in Trinidad.
 

 
 
 
 

 
 
 
 

The geology of Barbados
 
Barbados  is  part  of  the  Caribbean 
plate  and  exhibits  a  unique  geologic 
history . Unlike  most  of  the  small 
islands  that  make  up  the  island  arc 
in  the  Caribbean , Barbados  is  not 
volcanic . Its  origin  can  be  traced  to 
plate  tectonic  movement  {of  the 
Caribbean  plate}  and  the  physical 
and  mechanical  activities  associated 
with  it  and  coral  formation .
 
  

 
 
Above is a geological map of Barbados.
 
This map is free to use.
 
 
This page last updated August 2004.
Welcome to The Geology of Barbados....

Geo Facts
The Scotland series sandstones
and clays were laid down under the sea 60-70 million years ago
The Oceanic series rocks are fine white clays ,locally known as chalk which were laid down in deep sea conditions
The coral limestone cap was
formed as the island was uplifted by earth movements over the past 600,000 years. It has been arched upwards to form to form 2 broad anticlines ,one in the centre of the island and one in the south
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