Labyrinth (Antarctica)

It was so named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) because the eroded dolerite of which it is formed gives an appearance of a labyrinth.

The descriptive name was suggested by the United States Antarctic Project (USAP) field party that sampled the pond in 2003-04.

Named by Advisory Committee on Antarctic Names (US-ACAN) (2004) after Scott D. Craig, United States Fish and Wildlife Service, East Orland, ME; member of a United States Antarctic Project (USAP) party that field sampled Labyrinth ponds in 2003-04.

A descriptive name suggested by the United States Antarctic Project (USAP) field party that sampled the pond in the 2003-04 season.

The pond is near the southwest extremity of Healy Trough, 0.2 nautical miles (0.37 km; 0.23 mi) east of the Wright Upper Glacier terminus.

The name was suggested by a United States Antarctic Project (USAP) field party, 2003-04, because a rock in this small pond looks like an anvil.

Named by Advisory Committee on Antarctic Names (US-ACAN) after Russell Rodriquez, United States Geological Survey, Seattle, WA; member of a United States Antarctic Project (USAP) party that sampled the pond in 2003-04.

Named by Advisory Committee on Antarctic Names (US-ACAN) (2004) after Regina Redman, United States Geological Survey, Seattle, WA; member of a United States Antarctic Project (USAP) field party in the Labyrinth in 2003-04.

The relatively level ledge rises to 1,000 metres (3,300 ft) and is bounded west and north by Healy Trough.

[13] This article incorporates public domain material from websites or documents of the United States Geological Survey.

Wright Valley south of center of mapped region. Labyrinth at west end of the range.