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your wack Barbados shares many common features with other Caribbean islands. Barbados shares in a rich Caribbean musical heritage ... especially Reggae and Calypso rhythms. Barbados also shares the distinctly Caribbean style of fine dining with blends of Creole, Indian curry, and European often centered around local fishes, fruits and vegetables. The semi tropical climate of Barbados and the cooling trade breezes blowing into the Caribbean from the Atlantic are also common to Barbados as well as to her neighbors. Barbados also shares in the dark history of slavery in the Caribbean which results in a local population that is mostly black but which also has significant white and mulatto minorities as well as Jewish, East Indian, South American, and other minorities which unite to create a people that is distinctively Bajan.
On the other hand, Barbados is at the same time unique and distinct from her Caribbean neighbors. Her uniqueness may be explained by her unique geology which in turn helps to explain her unique geography which in turn helps to explain her unique history which in turn helps to explain her unique social and economic conditions that exist at the present time.
GEOLOGY
The geology of Barbados is unique within the Caribbean.
First, a perspective on time is helpful. The island was formed around 1 million years ago, but this is just an instant when compared with the age of earth itself. On a comparative basis, earth is around 4,000 times older than the island of Barbados. Similarly, the age of the dinosaurs is 65 times older than the island of Barbados. That is, Barbados is around 1 million years old, but the last dinosaur lived around 65 million years ago! So, on a relative, comparative basis, Barbados is a mere infant.
The formation of Barbados has to do with the enormous plates that form earths outer layer. These plates sit on semi liquid, molten rock and thus float and move about. We are talking minuscule movements but which over millions of years can have earth forming consequences. Barbados is located at the junction of two monstrous plates ... the Caribbean plate and the Atlantic plate which are each part of the sea bed. As these two plates came together over time, the Atlantic plate was pushed under the Caribbean plate which was pushed up and over the Atlantic plate. In other words, the sea bed was pushed up and up until it became exposed, and the island of Barbados was formed.
At the same time, the pressure of the two plates grinding together created cracks and faults in the Caribbean plate along a line around 100 miles to the west of Barbados (toward the Caribbean), and this resulted in a series of volcanic eruptions along this fault line which produced the neighboring islands of Grenada, St. Vincent, St. Lucia, Martinique, Dominica, etc.. So, these neighboring islands are borne from the same processes as Barbados, but it is Barbados alone which is an island of sea bed pushed to the surface while the others are volcanic in origin. This explains why Barbados is relatively flat and hilly while her neighbors consist mostly of rugged mountains. And, this also accounts for the mostly arable and tillable land of Barbados which allowed her to be an agricultural leader in the region especially during the heady days when Caribbean sugar was king.
As the sea bed rose toward the surface but before becoming exposed, it first became a coral reef attracting marine life. Over the immense time this process was underway, the marine life (carbon based as are all living plants and animals on earth) moved naturally through the cycle of life and death so that the sea bed became covered with the remains of dying plants and animals. When the process finally pushed the sea bed to the surface, the exposed sea bed consisted of various types of limestone which is carbonate rock. This limestone appears everywhere in Barbados and is known locally as coral rock. You will see limestone boulders everywhere, and where roads are cut through the hills, the exposed sidewalls are limestone. The locals have used this coral rock to form building blocks for homes and other buildings, crushed it for road construction, and use it as raw material for manufactured products such as cement. The process of dying marine life falling to the sea bed also has resulted in marine fossils being present everywhere in this coral rock, so walking along rocky cliffs will reveal marine fossils in every other rock. It is also this same process of dying life being embedded in sediment that produces crude oil, and there are quite a number of oil wells on the island although the production is not significant.
The semi porous nature of the limestone coral rocks has allowed rain water to seep into the soil rather than to run off. This results in an available fresh water source reachable by wells and has also produced rain erosion manifested in many gullies and caves. Many of the caves are available for tourist inspections and tours.
Of course, the entire island did not surface at once, and the first part of the island to be exposed is the eastern part of the island known as the Scotland district. Quite understandably, this is now the highest and hilliest part of the island. Although the primeval rain forest jungle has largely been cleared on Barbados, the eastern hills still contain swatches of jungle. The eastern coastline also shows the effects of another force of nature over time, and that is the exposure to the constant easterly trade winds with the constant pounding of surf. This has produced sea erosion along the eastern coastline as the sea has carved into the exposed limestone producing cliffs and sea stacks which are oddly shaped rocks jutting up from the sea along the coastline. The sense of natures powerful forces is very evident along the east coast which many would claim is the most beautiful part of the island but also the harshest environment and thus the least habitable part of the island.
Clearly, Barbados geology is one aspect of her uniqueness and which also contributes to her unique geography, history, economy and culture.
GEOGRAPHY AND CLIMATE
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