Mill Stream Glacier () is a tributary
glacier, about wide, flowing west between the
Supporters Range
The Supporters Range () is a rugged range in the Queen Maud Mountains of Antarctica.
It is long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south.
So named by the New Zealand Geolog ...
and
Otway Massif Otway Massif () is a prominent, mainly ice-free massif, about 10 nautical miles (18 km) long and 7 nautical miles (13 km) wide, standing at the northwest end of the Grosvenor Mountains at the confluence of Mill Glacier and Mill Stream Gla ...
in Antarctica to enter
Mill Glacier
Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill ...
. It was named by the
New Zealand Geological Survey Antarctic Expedition of 1961–62 in association with Mill Glacier.
[
]
References
Glaciers of Dufek Coast
{{DufekCoast-glacier-stub