The wreck of RMS Titanic lies at a depth of about 12,500 feet (3,800 metres; 2,100 fathoms), about 370 nautical miles (690 kilometres) south-southeast off the coast of Newfoundland. It lies in two main pieces about 2,000 feet (600 m) apart. The bow is still recognisable with many preserved interiors, despite deterioration and damage sustained hitting the sea floor. In contrast, the stern is heavily damaged. A debris field around the wreck contains hundreds of thousands of items spilled from the ship as she sank. The bodies of the passengers and crew would also be distributed across the seabed, but have since been consumed by other organisms.
The Titanic sank in 1912, when she collided with an iceberg during her maiden voyage. Numerous expeditions unsuccessfully tried using sonar to map the seabed in the hope of finding the wreckage. In 1985, the wreck was finally located by a joint French–American expedition led by Jean-Louis Michel of IFREMER and Robert Ballard of the Woods Hole Oceanographic Institution, originally on a mission to find two nuclear cold war submarines
Detached rusticles below port side anchor indicating that the rusticles pass through a cycle of growth, maturation and then fall away. This particular "crop" probably was in a five to ten year cycle. Image courtesy of Lori Johnston, RMS Titanic Expedition 2003, NOAA-OE. Rusticle hanging from the stern section of the RMS Titanic showing secondary growths during maturation. Image courtesy of Lori Johnston, RMS Titanic Expedition 2003, NOAA-OE.