Geological observation in the eastern end of the Himalaya shows that t
he Asia/India Suture is folded. Metamorphic rocks derived from India o
ccur structurally below the suture, in the core of a regional antiform
, Isotopic and fission track dating establish cooling-exhumation of ro
cks from c.30 km depth within the last 4 Myr. We argue that exhumation
is caused by approximate to 10 mm yr(-1) erosion coeval with crustal
scale folding.