Change: Tulsequah Glacier has retreated 1.1 km since 1948. The terminus of this valley glacier is currently situated in a ice-contact lake. This lake actually extends 2.5 km upglacier. There is no crevassing present at the terminus and it is expected to disitigrate into to lake because it is quite thin.   View changes from previous version. (Word count: 380)

Change: Juneau icefield tributary and Tulsequah Glacier. This tributary was once joined to the Tulsequah glacier duiring the Little Ice Age. At the end of the 19th century the glaciers began to recede, creating the ice-dammed lake. By the 1920's, the tributary had receded by several kilometers, which increased the size   View changes from previous version. (Word count: 329)

Change: Latitude: 58º-59º, Longitude: 133º-135ºSource:Canadian Glaciers Official Name Latitude(Centre of Glacier) Longitude (Centre of Glacier) Gazetteer Map Reference Opposer Glacier 58°55'00" 133°35'30" 104K/13 Sittakanay Glacier 58°30'00" 133°20'00" 104K/6 Speel Glacier 58°20'00" 133°24'00" 104K/6 Tulsequah Glacier 58°50'00" 133°48'00" 104K/13 Twisted Pinkie Glacier 58°51'20" 133°46'50" 104K/13 Wright Glacier 58°24'00" 133°23'00"   View changes from previous version. (Word count: 207)

Change: Located in the center of this image is Tulsequah Lake. This lake is located on the ice margin of a tributary of Tulsequah Glacier and   View changes from previous version. (Word count: 196)

Change: Source:Canadian Glaciers Official Name Latitude(Centre of Glacier) Longitude (Centre of Glacier)   View changes from previous version. (Word count: 13)

Change: There were only format changes (bold, italics, etc.) in this version. See this version for details. (Word count: 0)