An elephants' graveyard (also written elephant graveyard or elephant's graveyard) is a place where, according to legend, older elephants instinctively direct themselves when they reach a certain age. They then die there alone, far from the group.
Several theories are given about the myth's origin. One theory involves people finding groups of elephant skeletons together, or observing old elephants and skeletons in the same habitat. Others suggest the term may spring from group die-offs, such as one excavated in Saxony-Anhalt, which had 27 Palaeoloxodon antiquus skeletons. In that particular case, the tusks of the skeletons were missing, which indicated either hunters killed a group of elephants in one spot, or else opportunistic scavengers removed the tusks from a natural die-off.
Other theories focus on elephant behavior during lean times, suggesting starving elephants gather in places where finding food is easier, and subsequently die there.
The myth was popularised in films such as Trader Horn and MGM's Tarzan movies, in which groups of greedy explorers attempt to locate the elephants' graveyard, on the fictional Mutia Escarpment, in search of its riches of ivory. Osamu Tezuka's Kimba the White Lion episode "A Friend in Deed" centered around it. More recently, the 1994 Disney animated film The Lion King as well as the Broadway/West End musical adaptation referred to the motif. Also, a character from the The X-Files episode "Fearful Symmetry", which revolves around a mysterious invisible elephant, refers to the concept as fact.
In geology, "elephants' graveyard" is an informal term for a hypothetical accumulation of "large blocks of country rock stoped from the roofs of batholiths". In military settings, it is sometimes used as a slang term to describe postings or assignments for senior officers for which there is no potential for further promotion.
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- Clarke, D. Barrie; Henry, Andrew S.; White, Mary Anne (10 September 1998). "Exploding xenoliths and the absence of 'elephants' graveyards' in granite batholiths". Journal of Structural Geology 20 (9–10): 1325–1343. doi:10.1016/S0191-8141(98)00082-0.