The use of a 35 mm or similar camera set up over a theodolite is descr
ibed for surveying mountain and polar glaciers where conditions do not
allow for extensive detailed surveying or the use of heavy phototheod
olites. Though used initially by Spender and Wright in the 1930s on Mo
unt Everest and in Greenland and Arctic Canada, but apparently not by
others since then, it was again tried our by Wright in Iceland in 1999
. Modern analytical techniques have shown that heights accurate to wit
hin 2 m can be obtained from these photographs at distances up to 5 km
. In addition, five times as many points can be identified and interse
cted in the laboratory from the photographs as was possible using sket
ches in difficult field conditions. Some reasons are suggested for the
lack of use of this technique by others. The potential of existing su
rvey photographs taken in Arctic Canada for large scale surveys of hig
h polar glaciers in 1938 is described with the hope that glaciologists
and photogrammetrists might undertake their analysis.