Mount Danforth
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Mount Danforth
Mount Danforth () is an ice-free, pyramidal mountain over high, standing immediately east of Mount Zanuck on the south side of Albanus Glacier, in the Queen Maud Mountains. It was discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named by Richard E. Byrd for William H. Danforth of the Purina Mills, St. Louis, a contributor to the expedition. References

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Mount Zanuck
The Gothic Mountains () is a group of mountains, long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier (Transantarctic Mountains), Scott Glacier, Albanus Glacier, and Griffith Glacier. Exploration and naming The mountains were first visited in December 1934 by the Byrd Antarctic Expedition (ByrdAE) geological party led by Quin Blackburn. The name was proposed by Edmund Stump, leader of a United States Antarctic Research Program (USARP) - Arizona State University geological party which made investigations here in the 1980–81 season. The mountains are composed of granites which have weathered to produce a series of spires and peaks reminiscent of a Gothic cathedral. Location The western Gothic Mountains are just east of Scott Glacier, to the south of the point where the Albanus Glacier joins the Scott Glacier from the east. Peaks in the western section include, from west to east, Grizzly Peak, Mount Zanuck, Zanuck Ea ...
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