Elephant bird The bones of these domesticated fowl have been found in subfossil sites in the island (MacPhee and Marx, 1997: 188), such as Ambolisatra (Madagascar), where "Mullerornis" sp. and "Aepyornis maximus" have been reported. Also reported by these authors, ratite remains have been found in west and south west Madagascar, at Belo-sur-Mer ("A. medius", "Mullerornis rudis"), Bemafandry ("M. agilis") and Lamboharana ("Mullerornis" sp.). Recently human tool marks have been found on elephant bird bones dating to approximately 10,000 BC. This not only vastly extends the range of human existence on Madagascar's prehistoric past, but suggests a more complex relationship between these
Elephant Spit Spit Bay to the north and west and is formed of sediments derived from the glacial erosion of volcanic material from eruptions by Big Ben which have made the seabed south-east of the island relatively shallow. Heard Island is isolated, uninhabited and rarely visited. When the island was visited in 2002 and 2003 by scientists from the Australian Antarctic Division, the spit was intact. However, a following visit in late 2008 found that a section of the eastern end of the spit had become inundated by the ocean, forming a 2-km-long island. Elephant Spit Elephant Spit is a 9 km