Cobb River | |
---|---|
Location | |
Country | New Zealand |
Physical characteristics | |
Source | |
• location | Lake Cobb |
• coordinates | 41°01′23″S172°33′12″E / 41.023°S 172.5532°E |
• elevation | 1,090 m (3,580 ft) |
Mouth | |
• location | Tākaka River |
• coordinates | 40°52′56″S172°48′37″E / 40.8822°S 172.8102°E |
• elevation | 220 m (720 ft) |
Length | 26 km (16 mi) |
Basin features | |
Progression | Cobb River → Tākaka River → Golden Bay / Mohua → Tasman Sea |
Tributaries | |
• left | Diamond Lake Stream |
• right | Chaffey Stream, Hannah Creek, Myttons Creek, Thorns Creek, Trilobite Creek, Magnesite Creek |
The Cobb River is a river in the Tasman Region of New Zealand. It flows southeast from Lake Cobb on the northern slopes of Mount Cobb, in Kahurangi National Park, in the northwestern South Island. The river's waters are captured behind a dam to become the Cobb Reservoir; the outflow continues to join with the Tākaka River. [1] The river is named for J.W. Cobb, a local mill owner. [2]
Brown and rainbow trout are available for fishing in the river. [3] A tramping track follows the river between Lake Cobb and the reservoir and there are several backcountry huts in the river valley. New Zealand's oldest rocks are found in the Cobb River catchment.
Trout is a generic common name for numerous species of carnivorous freshwater ray-finned fishes belonging to the genera Oncorhynchus, Salmo and Salvelinus, all of which are members of the subfamily Salmoninae in the family Salmonidae. The word trout is also used for some similar-shaped but non-salmonid fish, such as the spotted seatrout/speckled trout.
The Deschutes River in central Oregon is a major tributary of the Columbia River. The river provides much of the drainage on the eastern side of the Cascade Range in Oregon, gathering many of the tributaries that descend from the drier, eastern flank of the mountains. The Deschutes provided an important route to and from the Columbia for Native Americans for thousands of years, and then in the 19th century for pioneers on the Oregon Trail. The river flows mostly through rugged and arid country, and its valley provides a cultural heart for central Oregon. Today the river supplies water for irrigation and is popular in the summer for whitewater rafting and fishing.
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The D'Urville River is in the South Island of New Zealand.
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Lake Benmore is New Zealand's largest artificial lake. Located in the South Island of New Zealand and part of the Waitaki River, it was created in the 1960s by construction of Benmore Dam.
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The Saugatuck Reservoir is a reservoir in Fairfield County, Connecticut, United States, that straddles the border between the towns of Redding, Weston, and Easton. Its completion is marked by the creation of the Samuel P. Senior dam of the Saugatuck River in January 1942, and provides water to several of the nearby towns. The reservoir is surrounded by the Centennial Watershed State Forest and a small section of the Trout Brook Valley State Park Reserve on the southeast end of the reservoir. The Saugatuck Reservoir utilizes an uncontrolled spillway adjacent to the Samuel P. Senior dam that effectively limits the maximum water level. There is also a concrete levee positioned on the southeastern side of the reservoir that prevents water from flooding Trout Brook Valley.
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.
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The Cust River is a river in the Canterbury region of New Zealand. It flows east across the upper Canterbury Plains from its source north of the town of Oxford, New Zealand, flowing into the Cam River / Ruataniwha close to the town of Rangiora. The small town of Cust lies on the banks of the river. The lower part of the river, to the south-west of Rangiora, is diverted into a channel and called the "Main Drain". The channel was built in 1862 to drain the swampy land between Rangiora and the Waimakariri River, and when it was enlarged in 1868 it accidentally captured the Cust.
The Goulter River is a river in the Marlborough region of New Zealand. It rises in the Richmond Range near Lake Chalice. The lake was formed by a landslip about 2000 years ago, which dammed the river. The lake has no outlet, but water seeps through the landslip rubble into the Goulter. The river flows counter-clockwise around Mount Patriarch to join the Wairau River.
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The Haupiri River is a river of New Zealand. It starts near Mount Dixon in the Kaimata Range of the Southern Alps and flows north-west near to Lake Haupiri, then north-east to join the Ahaura River. The Ahaura joins the Grey River which flows into the Tasman Sea at Greymouth.
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The Cobb Reservoir is a hydro storage lake fed by the Cobb River in the Tasman District of the South Island of New Zealand. The reservoir feeds the Cobb Power Station and is 819 metres (2,687 ft) above sea level but drops significantly with low rainfall. Cobb Reservoir is the highest hydro storage lake in New Zealand, and is entirely surrounded by Kahurangi National Park.