A long chain of mountains extends generally somewhat north of west from Mount Everest whose west ridge descends to the col of
Lho La () before rising to
Khumbutse (). The ridge drops to an unnamed col at and then ascends to Lingtren from where it continues to another unnamed col at and then to
Pumori (). Bounded on the north by this chain of mountains is the
Khumbu Glacier, which descends to the northwest over the
Icefall before it turns sharply southwest. Lingtren lies at the apex of this right-angled bend. North of the mountain chain in Tibet the West Rongbuk Glacier flows east to join the main
Rongbuk Glacier. Near Lingtren, the Khumbu glacier is at about whereas the West Rongbuk glacier is at about . Geologically the south face of the mountain is of black
gneiss overlain by a thick
sill of massive
granite. The gneiss has been
intruded with many thinner granite sills. The summit elevation is alternatively stated to be and using different
elevation models. Lingtren's
prominence is about above its key col, which is between it and its nearest higher neighbour Pumori. == Discovery ==