The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being 200 km (125 mi) long and having a width of 40 km (25 mi). It descends about 2,200 m (7,200 ft) from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western. Its mouth is east of the Lennox-King Glacier. It is northwest of the Ramsey Glacier.
The Nimrod Glacier is a major glacier about 85 nautical miles long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains into the Ross Ice Shelf, Antarctica.
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.
The Murchison Glacier is an 18-kilometre (11 mi) long glacier flowing through Aoraki / Mount Cook National Park in the South Island of New Zealand. Lying to the east of the Malte Brun range and west of the Liebig Range, high in the Southern Alps, it flows from the Tasman Saddle at 2,435 m mostly southwestwards to around 1,110 m. The Murchison River, which takes its meltwater, flows under the larger Tasman Glacier to the south.
The Keltie Glacier is a large Antarctic glacier, 30 nautical miles (56 km) long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the British Antarctic Expedition, 1907–09, under Ernest Shackleton, who named it for Sir John Scott Keltie, Secretary of the Royal Geographical Society, 1892–1915.
The Supporters Range is a rugged range in the Queen Maud Mountains of Antarctica. It is 25 nautical miles 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 Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because several peaks of the range are named after supporters of Ernest Shackleton's British Antarctic Expedition (1907–09).
The Priestley Glacier is a major valley glacier, about 60 nautical miles long, originating at the edge of the Polar Plateau of Victoria Land, Antarctica. The glacier drains southeast between the Deep Freeze Range and Eisenhower Range to enter the northern end of the Nansen Ice Sheet. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and named for Raymond Priestley, a geologist with the Northern Party.
Tucker Glacier is a major valley glacier of Victoria Land, Antarctica, about 90 nautical miles long, flowing southeast between the Admiralty Mountains and the Victory Mountains to the Ross Sea. There is a snow saddle at the glacier's head, just west of Homerun Range, from which the Ebbe Glacier flows northwestward.
The Usarp Mountains are a major mountain range in North Victoria Land, Antarctica. They are west of the Rennick Glacier and trend north to south for about 190 kilometres (118 mi). The mountains are bounded to the north by Pryor Glacier and the Wilson Hills. They are west of the Bowers Mountains.
The Gunn River is a river on the West Coast of New Zealand. It starts in the Price Range and flows east into the Whataroa River, which eventually drains into the Tasman Sea.
The Macaulay River is a river of the Mackenzie Country of New Zealand's South Island. It flows south from the Two Thumb Range, part of the Southern Alps, its valley merging with that of the Godley River shortly before it enters the northern end of Lake Tekapo.
The Mahitahi River is a river of the southwest of New Zealand's South Island. It flows northwest from the Hooker Range, part of the Southern Alps, reaching the Tasman Sea at Bruce Bay.
The Mistake River is a river of the Canterbury region of New Zealand's South Island. It flows south from the Hall Range to the northwest of Lake Tekapo, turning east at the southern end of the range to flow into the western edge of the lake.
The Rotokino River is a short river of the West Coast Region of New Zealand's South Island. It flows south from Lake Rotokino, draining its waters to the Whataroa River.
The Sinclair River is a river of the Canterbury region of New Zealand's South Island. It flows south from the Jollie Range and is one of the headwaters of the Clyde River, part of the upper Rangitata River system.
The South Opuha River is a river of the Canterbury region of New Zealand's South Island. It flows south down a valley between the Two Thumb Range and the Sherwood Range from its origins northwest of Mount Misery before turning southeast around the southern end of the Sherwood Range to reach the western shore of Opuha Lake, of which it is a major inflow.
The Willberg River is a river of the West Coast Region of New Zealand's South Island. It initially flows northwest before turning southwest, reaching the Poerua River 12 kilometres south of Harihari.
Slagle Ridge is a high and massive snow-covered ridge between Slone Glacier and Burnette Glacier in the Admiralty Mountains, Victoria Land, Antarctica.
The Lillie Range in Antarctica extends northward from the Prince Olav Mountains to the Ross Ice Shelf. Mounts Hall, Daniel, Krebs and Mason are in the range.
The Two Thumb Range is a range of mountains in the Canterbury Region of New Zealand's South Island. It is located to the east of Lake Tekapo and has several peaks which rise to around 2,500 metres (8,200 ft). The southern end of the range contains one of Canterbury's main skifields, Mount Dobson.
