The Causeway, Bermuda by Hurricane Fabian, the Bermuda Government began investigating alternatives to simply repairing the causeway after each storm knocked it out. These alternatives include an underwater tunnel, a true bridge and constructing additional roadways, such as through Coney Island and Ferry Reach parks. Public meetings on these plans began in October, 2006. By February 2010, however, plans to replace the causeway had been abandoned, and the issue was a touchy subject when raised in the Senate of Bermuda. The Causeway, Bermuda The Causeway is a narrow strip of reclaimed land and bridges in the north of Bermuda linking Hamilton Parish on
Geology of Bermuda southeast indicate that Bermuda volcanoes were exposed above the water and eroding by the Oligocene. The volcano that built the island's basement is inferred to be mid-plate hotspot volcanism. Eolian limestone and hills dominates much of the surface geology of Bermuda, interbedded with layers of paleosols. Geology of Bermuda The geology of Bermuda represents an isolated limestone island in the Atlantic at the edge of the shallow Bermuda Platform. This platform is part of the larger Bermuda Pedestal (other high points include the Challenger and Plantagenet banks, separated by water 1000 feet deep. The island's volcanic basement rock is relatively