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 Waimakariri River is one of the largest rivers in Canterbury, on the eastern coast of New Zealand's South Island. It flows for 151 kilometres (94 mi) in a generally southeastward direction from the Southern Alps across the Canterbury Plains to the Pacific Ocean.
The Lewis River is a river in the Canterbury region of New Zealand. The valley of this river forms the southeastern approach to Lewis Pass; the river is thus adjacent to State Highway 7. The Lewis River is a tributary of the Boyle River. The Nina River flows into the Lewis River a few kilometres upstream from the confluence with the Boyle River. Land Information New Zealand lists the name of the river as "not official", i.e. the name is not confirmed by the New Zealand Geographic Board. It was named for the surveyor Henry Lewis, who discovered the pass in 1860 alongside his colleague Christopher Maling. Later in 1860, the river was named by Julius von Haast during his own expedition; von Haast became the brother-in-law of Lewis' daughter in 1866.
The Henry River is a minor river in the South Island of New Zealand.
Crooked River is a river that flows from headwaters in the Southern Alps to Lake Brunner in the West Coast region of New Zealand's South Island. It is named for the erratic path it takes. Near Lake Brunner, it passes through reasonably flat farmland, but closer to its source, it rushes through gorges and rapids. One tributary is the Poerua River from Lake Poerua.
The Hope Fault is an active dextral strike-slip fault in the northeastern part of South Island, New Zealand. It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique convergent boundary between the Indo-Australian Plate and Pacific Plate, from the transform Alpine Fault to the Hikurangi Trench subduction zone.
Mandamus River is a river in the South Island of New Zealand.
The Doubtful River is a river in the Canterbury region of New Zealand. It rises near Mount Barron and flows south then south-east through Lake Sumner Forest Park, reaching the Boyle River 40 kilometres (25 mi) west of Hanmer Springs. The Doubtful Range lies to the south. The Doubtless River and Devilskin Stream are tributaries entering from the north.
The Empson River is a stream in the Canterbury Region of New Zealand. It arises near Grey Hill in the Hanmer Range and flows south into the Waiau Uwha River. The name is not official.
The Glencoe River is a river in the Canterbury region of New Zealand. It arises in the Organ Range near Shale Peak and flows south into the Mandamus River.
The Glenrae River is a river in the Canterbury region of New Zealand. It arises in the Glynn Wye Range near Mount Skiddaw and flows through the Lake Sumner Forest Park south and then south-east into the Hurunui River, which exits in the Pacific Ocean. Its tributaries include Devils Creek and Robyne Creek.
The Grantham River is a river in the Canterbury region of New Zealand. It arises in the Hanmer Range near Mount Miromiro, in the Hanmer Forest Park, and flows south-east into the Waiau Uwha River, which has its mouth on the Pacific Ocean.
The Hanmer River is a river in the Hurunui District of New Zealand. It originates in the Hossack Saddle between the Hanmer Range and the Amuri Range, and flows south-west into the Waiau Uwha River about 8 kilometres (5.0 mi) south-west of Hanmer Springs.
The Okuku River is a river of the north Canterbury region of New Zealand's South Island. It flows predominantly south from several sources in and close to the eastern edge of the Puketeraki Range west of Waikari, flowing through a steep gorge in the Okuku Range before flowing into the Ashley River / Rakahuri 20 kilometres (12 mi) east of Oxford.
The Otto River is a short river of the West Coast Region of New Zealand's South Island. It is one of the headwaters of the Grey River.
The Upper Grey River is a river of the West Coast Region of New Zealand's South Island. As the name suggests, it is a stretch of the Grey River, and the name is used for the section between the confluence of the Blue Grey River, Brown Grey River, and Crooked Mary Creek in the Southern Alps and the Upper Grey's confluence with the Little Grey River 25 kilometres southwest of Reefton.
The Hope River, in Canterbury, New Zealand, is a tributary of the Waiau Uwha River. It is one of three rivers by that name in the South Island.
The Stanley River is a river of the Canterbury region of New Zealand's South Island. An upper tributary of the Waiau Uwha River, it rises on the southern flanks of the St James Range and flows southwest to reach the Waiau Uwha 17 kilometres (11 mi) east of the Lewis Pass. Lake Guyon drains to the Stanley River via a swampy tributary named Stanley Vale. In its lower reaches the river passes through a gorge known as Stanley Gate. The Fowler Pass Track follows the river for much of its length.
Lake Tennyson is a glacial high-country lake in Canterbury, New Zealand. The first European settler to see the lake was Frederick Weld in 1853, who also named it. The headwaters of the Waiau Toa / Clarence River are just to the north, and the river flows through Lake Tennyson.
The Edwards River is a river located in the north of New Zealand's Canterbury region. It is the northern of the two rivers in New Zealand of this name.
