The Cook River / Weheka is in the South Island of New Zealand. The headwaters are from the La Perouse Glacier on the western flanks of the Southern Alps / Kā Tiritiri o te Moana, and it flows west, then northeast, then northwest and into the Tasman Sea. Its tributaries include the Balfour River, fed by Balfour Glacier, and the Fox River, fed by Fox Glacier / Te Moeka o Tuawe. Much of the river lies within the Westland Tai Poutini National Park. The river was renamed from Cook River to Cook River / Weheka as a result of the Ngai Tahu Claims Settlement Act 1998.
Mount Aspiring / Tititea is New Zealand's 23rd-highest mountain. It is the country's highest outside the Aoraki / Mount Cook region.
The Sauk River is a tributary of the Skagit River, approximately 45 miles (72 km) long, in northwestern Washington in the United States. It drains an area of the high Cascade Range in the watershed of Puget Sound north of Seattle. The river is a popular destination for fly fishing. It is a National Wild and Scenic River.
The Mātukituki River is a short braided river in the Southern Alps of New Zealand's South Island. Both its West Branch and East Branch originate from the Main Divide mountain ranges near Mount Aspiring / Tititea. Their largely glacier-fed waters each flow for approximately 20 kilometres (12 mi) before joining near Camerons Flat. After this confluence, the Mātukituki River leaves the boundaries of Mount Aspiring National Park and continues for another 30 kilometres (19 mi) to exit into Lake Wānaka at the lake's southwestern edge.
Haupapa / Tasman Glacier is the largest glacier in New Zealand, and one of several large glaciers which flow south and east towards the Mackenzie Basin from the Southern Alps in New Zealand's South Island.
The Tasman River is an alpine braided river flowing through Canterbury, in New Zealand's South Island.
Hooker Glacier is one of several glaciers close to the slopes of Aoraki / Mount Cook in the Southern Alps of New Zealand. It is not as large as its neighbour, the Tasman Glacier, measuring 11 kilometres in length.
The Mueller Glacier is a 13-kilometre (8.1 mi) long glacier flowing through Aoraki / Mount Cook National Park in the South Island of New Zealand. It lies to the west of Mount Cook Village within the Southern Alps, flowing roughly north-west from its névé near Mount Montgomerie before curving around the Sealy Range as it approaches its terminus. Various other glaciers feed into the Mueller Glacier along its route, including the Frind and Huddleston Glaciers. The glacier ends at a small unnamed terminal lake, which is also fed by meltwater from the nearby Hooker Glacier. This lake is the source for the Hooker River, a small tributary of the Tasman River, which flows into Lake Pukaki.
Borchgrevink Glacier is a large glacier in the Victory Mountains, Victoria Land, draining south between Malta Plateau and Daniell Peninsula, and thence projecting into Glacier Strait, Ross Sea, as a floating glacier tongue, the Borchgrevink Glacier Tongue, just south of Cape Jones. It was named by the New Zealand Geological Survey Antarctic Expedition, 1957–58, for Carsten Borchgrevink, leader of the British Antarctic Expedition, 1898–1900. Borchgrevink visited the area in February 1900 and first observed the seaward portion of the glacier.
Abel Lake was a small lake in the Westland region of the South Island of New Zealand. It was located in the Southern Alps, 35 kilometres (22 mi) east of Franz Josef and was fed by the Abel Glacier. A short stream linked the lake with the Perth River. The lake was was likely displaced with alluvial / glacial rock or the outlet was lowered by natural erosion or manually by gold prospectors.
The Barrier River is a river in the Mount Aspiring National Park in northern Southland, New Zealand. It is a tributary of the Pyke River, which it enters about 1 kilometre (0.6 mi) south of Lake Wilmot. The Barrier River is fed by three glaciers and ice fields:
The Douglas River, formerly known as the Twain, is a river of the West Coast of New Zealand's South Island. Its source is high in the Southern Alps, five kilometres (3.1 mi) south of Mount Sefton, and its upper reaches are fed by water from the Douglas Glacier. It flows west for 18 kilometres (11 mi), joined by runoff from the Horace Walker Glacier, before joining the waters of the Karangarua River. The Douglas River's entire course is within Westland Tai Poutini National Park. The river and glacier are named after Charles Edward Douglas, a 19th-century explorer and mountaineer.
The Rees River is a headwater tributary of the Clutha River / Mata-Au that drains eastward of the main divide of the Southern Alps / Kā Tiritiri o te Moana in New Zealand. The river runs 41 km, drains an area of 406 km2, and discharges into the head of Lake Wakatipu at Glenorchy. Bound by the Richardson (Whakaari) Mountains to the east and the Forbes Mountains to the west, its snow-covered headwaters rise above 2000 m.
The Donald River is a short tributary of the Waiatoto River within Mount Aspiring National Park. It flows west for 6 kilometres (4 mi) from the Donald Glacier on the western slopes of Mount Pollux.
The Khānabād River flows in the provinces of Takhar and Kunduz in northern Afghanistan. The Khanabad River is a tributary of the Kunduz River, which is in turn a tributary of the Amu River.
Graveson Glacier is a broad north-flowing tributary to the Lillie Glacier, draining that portion of the Bowers Mountains between the Posey Range and the southern part of Explorers Range, Victoria Land, Antarctica. The geographical feature is fed by several lesser tributaries and enters Lillie Glacier via Flensing Icefall. The glacier was so named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for F. Graveson, a mining engineer who wintered at Scott Base in 1963 and was field assistant on this expedition. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
The Arrowsmith Range is a mountain range in the South Island of New Zealand. The range runs from southwest to northeast, parallel to the main ranges of the Southern Alps / Kā Tiritiri o te Moana. At the northeastern end, the range terminates at Jagged Peak, whence a ridge connects to the Jollie Range. The lower Potts Range is a continuation at the southwestern end of the range. The highest point on the range is Mount Arrowsmith.
The Agassiz Glacier is located near the west coast of New Zealand's South Island. The Agassiz Glacier is a tributary of the larger Franz Josef Glacier, and is itself fed by the Chamberlin Snowfield and the Davis Snowfield. It is named after Louis Agassiz, a Swiss-American glaciologist, and was discovered and named by the German geologist, Sir Johann "Julius" von Haast.
The Olivine Ice Plateau is a glacier in the Olivine Wilderness Area and Aspiring National Park in New Zealand's South Island. The plateau is named after the mineral olivine, which is common within the Dun Mountain Ophiolite that underlies the area. The plateau extents to the west over the Forgotten River Col. into the Forgotten River and to the north it merges with the Andy Glacier, which feeds a tributary of the Arawhata River. The Olivine Ice Plateau is one of many glaciers in the region of the Arawhata, Dart / Te Awa Whakatipu, Hollyford / Whakatipu Kā Tuka and Matukituki rivers' headwaters.
The Garden of Eden Ice Plateau is a large ice field on the western side of New Zealand's Southern Alps / Kā Tiritiri o te Moana. At over 9 km (5.6 mi) long, the Garden of Eden is one of the largest ice fields in New Zealand, along with the equally-sized Garden of Allah Ice Field which sits just to the north. The ice field is one of many geographic features in the area between the main divide of the Southern Alps and the Adams Range which share biblical names, a convention first established by the earliest explorers to the area. The Garden's remote location and difficult conditions make research difficult, especially with restrictions on helicopter landings imposed through the designation of the area as Adams Wilderness Area in 2003. Despite this, the ice plateau has been a popular destination for tramping groups for over 80 years, with access routes from both coasts and easily reachable areas once on the plateau itself.
