Albanus Glacier also known as Phillips Glacier, is a 25 miles (40.2 km) long glacier

Glacier

A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

 flowing west along the south side of Tapley Mountains

Tapley Mountains

The Tapley Mountains is a mountain range fronting on the eastern side of the Scott Glacier, extending eastward for between Leverett and Albanus glaciers in the Queen Maud Mountains, a part of the larger Transantarctic Mountains....

 to enter Scott Glacier

Scott Glacier (Transantarctic Mountains)

The Scott Glacier is a major glacier, 120 miles long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf...

 just north of Mount Zanuck, in the Queen Maud Mountains

Queen Maud Mountains

The Queen Maud Mountains are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the polar plateau in Antarctica...

 in Antarctica. It was discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. Byrd named it for Albanus Phillips, Jr., president of Phillips Packing in Cambridge, Maryland

Cambridge, Maryland

Cambridge is a city in Dorchester County, Maryland, United States. The population was 12,326 at the 2010 census. It is the county seat of Dorchester County and the county's largest municipality...

, a patron of, and supplier of provisions to, his Antarctic expeditions of 1928–30 and 1933–35.