Hubbard Glacier is a glacier located in eastern Alaska and part of Yukon, Canada, and named after Gardiner Hubbard.
The Kern River, originally Rio de San Felipe, later La Porciuncula, is a river in the U.S. state of California, approximately 165 miles (270 km) long. It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction.
Gannett Glacier is the largest glacier in the Rocky Mountains within the United States. The glacier is located on the east and north slopes of Gannett Peak, the highest mountain in Wyoming, on the east side of the Continental Divide in the Wind River Range. Gannett is but one of dozens of glaciers located in the Fitzpatrick Wilderness of Shoshone National Forest.
The Koshi or Kosi River drains the northern slopes of the Himalayas in Tibet and the southern slopes in Nepal. From a major confluence of tributaries north of the Chatra Gorge onwards, the Koshi River is also known as Saptakoshi for its seven upper tributaries. These include the Tamor River originating from the Kanchenjunga area in the east and Arun River and Sun Koshi from Tibet. The Sun Koshi's tributaries from east to west are Dudh Koshi, Bhote Koshi, Tamakoshi River, Likhu Khola and Indravati. The Saptakoshi crosses into northern Bihar where it branches into distributaries before joining the Ganges near Kursela in Katihar district.
A glacial lake outburst flood (GLOF) is a type of outburst flood that occurs when the dam containing a glacial lake fails. An event similar to a GLOF, where a body of water contained by a glacier melts or overflows the glacier, is called a Jökulhlaup. The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, volcanic eruptions under the ice, or if a large enough portion of a glacier breaks off and massively displaces the waters in a glacial lake at its base.
The retreat of glaciers since 1850 affects the availability of fresh water for irrigation and domestic use, mountain recreation, animals and plants that depend on glacier-melt, and, in the longer term, the level of the oceans. Studied by glaciologists, the temporal coincidence of glacier retreat with the measured increase of atmospheric greenhouse gases is often cited as an evidentiary underpinning of global warming. Mid-latitude mountain ranges such as the Himalayas, Alps, Rocky Mountains, Cascade Range, and the southern Andes, as well as isolated tropical summits such as Mount Kilimanjaro in Africa, are showing some of the largest proportionate glacial losses.
Big Wapwallopen Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 23 miles (37 km) long and flows through Bear Creek Township, Fairview Township, Rice Township, Wright Township, Dorrance Township, Hollenback Township, Nescopeck Township, and Conyngham Township. The watershed of the creek has an area of 53.2 square miles (138 km2). The creek has three named tributaries: Balliet Run, Watering Run, and Bow Creek. The creek is designated as a Coldwater Fishery and a Migratory Fishery and is also Class A Wild Trout Waters for part of its length. However, a portion is considered to be impaired by organic enrichment and/or low levels of dissolved oxygen and its pH ranges from moderately acidic to slightly alkaline.
Crooked Creek is a 26.3-mile-long (42.3 km) tributary of the Tioga River located entirely in Tioga County, Pennsylvania in the United States.
The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
Dinwoody Glacier is located in Shoshone National Forest, in the U.S. state of Wyoming on the east side of the Continental Divide in the Wind River Range. Completely within the Fitzpatrick Wilderness, Dinwoody Glacier is one of the largest glaciers in the American Rocky Mountains, and as of 1989 was ranked fourth in area. In a 1989 study which examined repeat photography and stream flow analysis, Dinwoody Glacier was determined to have retreated rapidly between 1958 and 1983, though most of the reduction has been in the thickness of the glacier rather than its surface area. In the same 25-year period, the glacier lost an average of 23.4 m (77 ft) in thickness. Radar mapping of 72 locations on the glacier resulted in an average thickness of 54 m (177 ft) and a maximum measured depth of 111 m (364 ft). The 1989 study was commenced to examine the impact on water supplies to streams and rivers from glacier retreat of both Dinwoody and Gannett Glaciers.
The glaciers of Bhutan, which covered about 10 percent of the total surface area in the 1980s, are an important renewable source of water for Bhutan's rivers. Fed by fresh snow each winter and slow melting in the summer, the glaciers bring millions of litres of fresh water to Bhutan and downriver areas each year. Glacial melt also adds to monsoon-swollen rivers which may be a contributing factor to flooding. Where glacial movement temporary blocks riverflows, downstream areas may be threatened by glacial lake outburst flood ("GLOFs"). Although GLOFs are not a new phenomenon in Bhutan, their frequency has risen in the past three decades. Significant GLOFs occurred in 1957, 1960, 1968 and 1994, devastating lives and property downstream. According to the Bhutan Department of Energy however, the majority of rivers in Bhutan are more susceptible to fluctuation with changing rainfall patterns than to flooding directly attributable to glacier or snow melt.
The lakes of Bhutan comprise its glacial lakes and its natural mountain lakes. Bhutanese territory contains some 2,674 high altitude glacial lakes and subsidiary lakes, out of which 25 pose a risk of GLOFs. There are also more than 59 natural non-glacial lakes in Bhutan, covering about 4,250 hectares (16.4 sq mi). Most are located above an altitude of 3,500 metres (11,500 ft), and most have no permanent human settlements nearby, though many are used for grazing yaks and may have scattered temporary settlements.
Little Wapwallopen Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 17 miles (27 km) long and flows through Rice Township, Dorrance Township, Conyngham Township, and Hollenback Township. The watershed of the creek has an area of 39.5 square miles (102 km2). The creek is designated as a Coldwater Fishery and a Migratory Fishery and is not considered to be impaired. It has two named tributaries: Pond Creek and Nuangola Outlet. Wild trout naturally reproduce in the creek.
Toby Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 10.5 miles (16.9 km) long and flows through Dallas Township, Dallas, Kingston Township, Courtdale, Luzerne, Pringle, Kingston, Edwardsville, and Larksville. The watershed of the creek has an area of 36.5 square miles (95 km2). The entire drainage basin is designated as a Migratory Fishery and parts are designated as either a Coldwater Fishery, a Warmwater Fishery, or a Trout Stocking Fishery. The creek has two named tributaries: Huntsville Creek and Trout Brook. It is said to show "some degraded conditions", but does not experience severe pollution and is not considered to be impaired. The creek is piped underground in Pringle, but resurfaces in Edwardsville.
Lost Creek is an unusual 3-mile (5 km) tributary of the McKenzie River in Lane County, in the U.S. state of Oregon. It is the lower section of a hydrogeological system, a losing stream, that begins at the base of Collier Glacier in the Cascade Range. This lower section rises from a spring complex north of Oregon Route 242 in the Cascade Range and flows generally northwest to meet the river near Belknap Springs. This is near the intersection of Route 242 with Oregon Route 126 and about 74 miles (119 km) upstream of the McKenzie's confluence with the Willamette River.
Furnace Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 1.0 mile (1.6 km) long and flows through Coal Township and Shamokin. The watershed of the stream has an area of 1.61 square miles (4.2 km2). It is impaired by sedimentation and siltation from urban runoff and storm sewers, but is not impacted by mine drainage. Reaches of the stream have been entirely enclosed. Furnace Run is named after a furnace that was built in the area in 1825. The stream is designated as a Coldwater Fishery and a Migratory Fishery.
Carbon Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 5.2 miles (8.4 km) long and flows through Zerbe Township, Coal Township, and Shamokin. The watershed of the stream has an area of 8.78 square miles (22.7 km2). Carbon Run is impaired due to metals from acid mine drainage, which colors the stream orange. Metals such as manganese, iron, aluminum, and others occur within its water. The watershed of the stream is in the Coal Region of Pennsylvania. Much of the area in the vicinity of the stream consists of spoil piles and abandoned mining land.
Locust Creek is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 4.0 miles (6.4 km) long and flows through East Cameron Township and Mount Carmel Township. The watershed of the creek has an area of 5.75 square miles (14.9 km2). The stream is designated as impaired due to metals from abandoned mine drainage. It also experiences a low pH. The creek flows through a water gap in Locust Mountain. Prominent land uses in its watershed include refuse areas and forested land. The creek's watershed is designated as a Coldwater Fishery and a Migratory Fishery.
Zerbe Run is a tributary of Mahanoy Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 8.3 miles (13.4 km) long and flows through Coal Township, Zerbe Township, and Little Mahanoy Township. The watershed of the stream has an area of 13.1 square miles (34 km2). Part of the stream is impaired by abandoned mine drainage, but its upper reaches are not impacted by mining. Several mine drainage discharges occur within the watershed. The stream is not far from the Western Middle Anthracite Field.
Sciota Brook is a tributary of North Branch Mehoopany Creek in Bradford County, Sullivan County, and Wyoming County, in Pennsylvania, in the United States. It is approximately 2.0 miles (3.2 km) long and flows through Wilmot Township in Bradford County, Colley Township in Sullivan County, and North Branch Township in Wyoming County. The watershed of the stream has an area of 3.23 square miles (8.4 km2). The stream itself is a moderate-gradient stream in an area consisting primarily of agricultural land and woodlots.
