Abbey Too

The origin of the name Abbey Too remains a mystery. This particular segment of the outer reef exhibits a characteristic structure, featuring main ledges and false ledges similar to other reef sections along Broward County's coastline. Towards the east are geological formations known as spur and groove that date back to the Pleistocene Era, a period of the last Ice Age when sea levels were significantly lower, resulting in the formation of shallow fringing reefs. Presently, this part of the reef reaches its highest point at a depth of approximately 45 to 50 feet (13.5 to 15 meters), sloping off towards both the east and west. Close to the shore, a portion of the ancient reef composed of staghorn corals collapsed long ago, filling with sand over time and creating a false ledge. Many divers mistake this false ledge for the sandy gap between the middle and outer reefs. However, continuing westward reveals the true beginning of the gap just beyond the false ledge. At the southern tip of this reef section lies a distinctive formation known as Rabbit Ears Pass, representing two intact patches of the original reef. This feature offers divers a glimpse into what the reef may have appeared like 10,000 years ago. Abbey Too provides divers with the opportunity to witness a rich variety of marine life, including grouper, jacks, snapper, and vigilant barracuda. Eels, trumpetfish, drums, and jack-knifefish are commonly sighted, along with lobsters that inhabit crevices and nooks on the reef's surface and ledges.