Bimini Road — Bimini Island, Bahama Islands - June 1998 The westernmost and closest to the United States mainland, the island of Bimini can be seen in…

MegalithFringe site

Bimini Road

The Bahamas

DatedEst. 1000 BCE–900 CE

Photo Original picture by NASA · Public domainSource file on Wikimedia Commons

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Overview

About this site

Overview

The Bimini Road, sometimes called the Bimini Wall, is an underwater rock formation near the island of North Bimini in the Bimini chain of islands, The Bahamas. It consists of a 0.8 km (0.50 mi)-long northeast-southwest linear feature composed of roughly rectangular limestone blocks.

Various claims have been made for the feature being a wall, road, pier, breakwater or other man-made structure, but credible evidence or arguments for such an origin are lacking. The consensus among geologists and archaeologists is that it is a natural feature composed of beachrock.

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Where it sits in time

The site's dated range, placed against world reference points.

The scale is logarithmic: each step to the left is about ten times older than the last.

Est. 1000 BCE–900 CEHow this date was established: Type comparisonTypical for this type

What this badge meansThe published range for this kind of monument in this region. It is not a date for this site.
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Article

Bimini Road

4 min read761 wordsRead on Wikipedia

Descriptions in various books and articles are said to exaggerate the regularity and rectangularity of the blocks.

Bimini Road

Description

Sources for this section

The Bimini Road is the largest of three linear features. It trends northeast/southwest and has a pronounced hook at its southwest end. It consists of flat-lying, tabular, roughly rectangular, polygonal and irregular stone blocks measuring as much as 3–4 metres (10–13 ft) in horizontal dimensions, with the average size being 2–3 metres (7–10 ft). The larger blocks show complementary edges, which are lacking in the smaller blocks. Two similar, narrower and shorter linear features, approximately 50 and 60 m (160 and 200 ft) long, lie parallel to and shoreward of the Road; they consist of smaller blocks only 1–2 m (3–7 ft) in maximum horizontal breadth. Descriptions in various books and articles are said to exaggerate the regularity and rectangularity of the blocks.

The blocks have rounded corners and resemble giant loaves of bread. They consist of limestone composed of carbonate-cemented shell hash called beachrock, which is native to the Bahamas. The highly rounded form of the blocks indicates that a significant thickness of their original surface has been removed by biological, physical and chemical processes, so that tool marks or inscriptions would be unlikely to have survived.

Research history

Sources for this section

On September 2, 1968, while diving in 5.5 meters (18 feet) of water off the northwest coast of North Bimini, Joseph Manson Valentine, Jacques Mayol and Robert Angove encountered what they called a pavement of rounded stones of varying size and thickness.

After a detailed examination, Gifford and Ball reported that the three features are unconnected at the southwest end, that no evidence exists of two courses of blocks or of a single block set squarely atop another, that bedrock closely underlies the whole area, and that the blocks of the inner and middle features have always rested on a layer of loose sand. They saw no regular or repeated patterns of grooves that might be interpreted as tool marks. These observations are disputed by other investigators, who claim that a second course of blocks can be seen where sand has washed away; detailed evidence for a continuous second layer has not been published in a reputable scientific venue.