Mine Gap Run [SEP] mouth of the watercourse
[{"answer": "Catawissa Creek", "provenance": [{"wikipedia_id": "43822874", "title": "Mine Gap Run", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 102, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
Mine Gap Run


6.6 and the concentration of alkalinity in it is 4 milligrams per liter. The elevation near the mouth of Mine Gap Run is above sea level. The elevation of the stream's source is between and above sea level. The lower reaches of Mine Gap Run are on rock of the Mauch Chunk Formation. The middle reaches of the stream are on rock of the Spechty Kopf Formation and the Pocono Formation. The stream's upper reaches are on rock of the Buddys Run Member of the Catskill Formation. Mine Gap Run has a
20391336
Mine Gap Run


on Catawissa Mountain in Roaring Creek Township. It crosses Mine Gap Road within a few hundred feet of its source and flows northeast in a valley for some distance. The stream eventually turns north for a few tenths of a mile. It then turns northeast and enters Beaver Township. A few tenths of a mile further downstream, it reaches its confluence with Catawissa Creek. Mine Gap Run joins Catawissa Creek upstream of its mouth. Mine Gap Run experiences some form of pollution. The stream is acidic and infertile. Its pH is
20391335
Garonne


most distant point (along watercourses from the river mouth) in the drainage basin from which water runs. The Ratera-Saboredo cirque is the "most distant point (along watercourses from the river mouth) in the drainage basin from which water runs", and the source of the Garonne, according to the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution convention upon determining a stream's source. The Garonne follows the Aran Valley northwards into France, flowing via Toulouse and Agen towards Bordeaux, where
1652483
Mine Gap Run


is within and 80 percent of the length of the stream is within of a road. 90 percent of its length is within of a road. Mine Gap Run is named after mines in its vicinity. A 1992 report stated that Mine Gap Run was a poor site for angling. The Pennsylvania Department of Environmental Protection considers Mine Gap Run to be a cold water fishery. The water chemistry of the stream is suitable for brook trout and is similar to other streams with substantial populations of wild brook trout. However, no fish
20391338
Loughborough Gap


The Loughborough Gap is a missing section of the Great Central Railway to the north-east of Loughborough, England. The gap was created by the removal of embankments and bridges during the 1980s and the restoration project has been branded Bridge to the Future and Bridging the Gap. From south-to-north the route crosses the Grand Union Canal, Railway Terrace road, four-track Midland Main Line at Loughborough railway station and the A60 road. The Hermitage Brook watercourse runs parallel. During the 2010s work began to restore the
1151106
Black Creek (Nescopeck Creek tributary)


of the water gap, the creek flows through Rock Glen and picks up the tributary Falls Run. Continuing north for a few miles, it picks up tributaries Barnes Run and Scotch Run, then turns northeast for slightly over a mile, reaching its confluence with Nescopeck Creek near the community of Tank. Black Creek joins Nescopeck Creek upstream of its mouth. The entire length of Black Creek is considered by the Pennsylvania Department of Environmental Protection to be impaired by acid mine drainage, the main sources of which are the Gowen and Derringer
7762289
Mine Gap Run


Mine Gap Run is a tributary of Catawissa Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Roaring Creek Township and Beaver Township. The watershed of the stream has an area of . The stream is polluted and acidic. However, it is considered to be a coldwater fishery. The main rock formations in the stream's watershed are the Mauch Chunk Formation, the Spechty Kopf Formation, the Pocono Formation, and the Buddys Run Member of the Catskill Formation. Mine Gap Run begins
20391334
Mine Gap Run


high gradient of per kilometer (0.6 miles). The stream is wide. The watershed of Mine Gap Run has an area of . The watershed is mostly in Roaring Creek Township, but a portion of it is in Beaver Township. Part of the watershed is in Pennsylvania State Game Lands Number 58. The watershed is in the Shumans United States Geological Survey quadrangle. Mine Gap Run flows through forested land in its middle reaches. However, there is agricultural land in its upper and lower reaches. 72 percent of the stream
20391337
Tunis Run


One of these joins Tunis Run upstream of its mouth. The elevation near the mouth of Tunis Run is above sea level. The elevation of the stream's source is above sea level. Tunis Run is situated near Hough Gap. The watershed of Tunis Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Loganton. However, its source is in the quadrangle of Woodward. The mouth of the stream is located near Loganton. Tunis Run was entered into the Geographic Names Information
16500685
Rijkevoort


living at the altitude of the monastery. About 2000, the last sisters, who all reached a high age, left for Tienray. Their sober monastery building is still in Rijkevoort. The Sint Anthonisloop, a channeled side branch of the Lage Raam, runs through the center of the village. The Lage Raam flows south of the village. These watercourses take care of the drainage of the former trout areas, all of which are mined to the agricultural area on a few strips of trees along the watercourses. Football club Toxandria
16606129
Callender Gap Creek


Section 404 of the Clean Water Act and Chapter 25 of state water regulations. The borough of Jermyn once requested a permit to discharge stormwater into the creek. The elevation near the mouth of Callender Gap Creek is above sea level. The elevation of the creek's source is between above sea level. The channel of Callender Gap Creek is entirely obscured by strip mining and is culvertized. The watershed of Callender Gap Creek has an area of . is entirely within the United States Geological Survey quadrangle of Carbondale. In the early 2000s
22087602
Wild Irish Girl Mine and Battery


clad with corrugated iron. The shed contains a vertical boiler and semi- portable engine, a light three-head prospecting battery, a workshop, a living area and fireplace, and a small water tank on a recently collapsed timber stand. A caved water shaft and a stone forge are located alongside the shed. A small watercourse which runs past the battery contains three stone overshot weirs. An extensive area of early alluvial workings commences along the watercourse about south of the battery. This area, which extends for over contains diverted creek
20520347
Loudoun Valley


is approximately long. The northern section of the valley is bisected by Short Hill Mountain. The area west of the Short Hill is known as Between the Hills and is distinct from the Loudoun Valley, while the area to the east, sometimes referred to as the Catoctin Valley, is associated with it. Major watercourses include Goose Creek, Catoctin Creek, Panther Skin Run, and the Little River. The three major highways across the valley are U.S. Route 50, which runs from Aldie on the east to Ashby Gap on the
16940996
Cound Brook


Severn at Cound. The Cound rises from minor watercourses running off the Long Mynd and Caer Caradoc in the northern part of the "Stretton Gap", between the settlements of Church Stretton and All Stretton. One of the main initial tributaries is the stream that runs through the Carding Mill Valley, which is named "Ashbrook" as it flows through Church Stretton. In the village of All Stretton the Ashbrook combines with another considerable stream that comes down the Batch valley, effectively forming the beginning of the Cound, at . The
1937058
Aqueduct (bridge)


Bridges for conveying water, called aqueducts or water bridges, are constructed to convey watercourses across gaps such as valleys or ravines. The term "aqueduct" may also be used to refer to the entire watercourse, as well as the bridge. Large navigable aqueducts are used as transport links for boats or ships. Aqueducts must span a crossing at the same level as the watercourses on each end. The word is derived from the Latin ' ("water") and ' ("to lead"). A modern version
7059259
Hazle Creek


—the whole area extending over to the Lehigh Gap was heavily forested with low-lying areas generally being swampy pinewood forests. Hazle Creek's source springs originate in the terrain along the upper edge of the Lehigh River drainage basin, TBDL ft above its mouth, and TBDL above mean sea level. Hazle Creek flows from its headwaters near Hazleton to its mouth near Weatherly. Due to underground mining, most of the surface drainage in the Hazleton Basin has been destroyed. Surface water infiltrates into the underlying minepool through abandoned strip mines
1087481
Great Northern Mine


holes to obtain new lodes. The mine rarely operated thereafter. The place contains a comprehensive range of functions that exemplify historical tin mining in the Herberton district including - alluvial workings, shaft sinking, winding and pumping, maintenance and accommodation. There are four main component areas - alluvial workings, Eastern Shaft, Gully Shaft and a house. Alluvial workings extend for the length of a permanent watercourse which runs through on the boundary of the property. These workings include stone and concrete retaining walls and evidence of work areas and camp sites
21167665
Petite Rivière de Jacmel


The Petite Rivière de Jacmel is a watercourse running in Haiti through the Sud-Est department and the arrondissement of Jacmel. The Petite Rivière de Jacmel takes its source in the foothills of the mountain range called "Chaîne de la Selle", and set in Hispaniola's Tiburon Peninsula. Over approximately 10 kilometers long, the river then runs Eastwards, to meet South with the Caribbean Sea at the level of its mouth in the bay of the port-city of Jacmel. Along its path in the mountain, the river turns
2380076
Leggetts Creek


near the Pennsylvania/New York border. Thomas Meredith conceived the idea of a railroad going from the mouth of the creek at Providence to the Great Bend on the Susquehanna River, a distance of , in 1826. Names such as the "Lackawannock and Susquehanna Railroad" and the "Meredith Railroad" were considered, but eventually the name "Leggetts Gap Railroad" was settled on. The railroad was first chartered in 1832, but no progress was made until 1849. The Rockwell Mine at Leggetts Gap was opened in 1854.
17082194
Rocky Run (Susquehanna River tributary)


elevation near the mouth of Rocky Run is between above sea level. The elevation of the stream's source is between above sea level. The valley of Rocky Run is situated to the north of Lee Mountain. An abandoned anthracite mine is located in the northern part of the watershed of Rocky Run approximately upstream of its mouth. A 1911 report mentioned two tunnels leading from the mine and entering loose rocks on a hillside. The report noted that the tunnels had a low discharge and their waters were slightly acidic and stated that during
19262289
Oshawa Creek


Oshawa Creek is a watercourse that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Oshawa, Ontario. It drains a watershed of . In its lowest reaches, in Oshawa, two tributaries, Goodman's Creek and Montgomery Creek, join the watercourse. To the west it borders Lynde Creek, which also has its headwaters in the Oak Ridges Moraine, and the shorter watercourses Pringle Creek and Corbett Creek. Bowmanville Creek, to the east, also has its headwaters in the Oak Ridges Moraine
15142259
Refugio Creek


Refugio Creek (pronounced from Spanish "refugio" meaning: shelter) is a watercourse running through the Refugio Valley from the hills of western Contra Costa County, California. It runs from the hills to its mouth at San Pablo Bay through the city of Hercules and unincorporated areas, including the town of Rodeo. The creek passes through a dense suburban area in addition to Refugio Valley Park. The creek is almost entirely at the surface level and unaltered although its riparian habitat is largely destroyed in the more developed areas. "Refugio
21988878
Rausch Creek (Pine Creek tributary)


while the effluent concentration ranged from less than to . The elevation near the mouth of Rausch Creek is above sea level. The elevation near the creek's source is above sea level. Rausch Creek flows through a water gap known as Kohlers Gap (or Bear Gap), where it is flanked by steep slopes. A number of abandoned deep mine openings occur in this reach. The tributary East Branch Rausch Creek flows between Big Lick Mountain and Good Springs Mountain, while the tributary West Branch Rausch Creek flows between Big Lick Mountain
21570001
Nanticoke Creek


underground mining. Municipalities in the watershed of Nanticoke Creek include Loomis Park, Lower Askam, Hanover, Espy Gap, Truesdale Terrace, Witinski Villa, and Warrior Gap. The city of Wilkes-Barre is not far from the creek. A reservoir known as the Hanover Reservoir is located in the southwestern part of the watershed. There are also a number of silt ponds in the vicinity of the creek. The creek's mouth is half a mile to the east of Nanticoke Falls. Nanticoke Creek was entered into the Geographic Names
8894257
Drury Run


as its water supply. Coal mining and clay mining has been done in the watersheds of all four of the named tributaries of Drury Run. Underground mining of coal and clay in the Drury Run watershed began in the late 1800s and went on until 1940. Surface mining in the watershed was done between the 1940s and the 1980s. Drury Run is a high-quality trout stream from its source at Tamarack Swamp to the mouth of Woodley Draft. Downstream of Woodley Draft, it still supports fish, but is also impaired by
7212064
Nea-Nidelvvassdraget


Nea-Nidelvvassdraget is a watercourse in the municipalities of Tydal, Selbu, Klæbu, and Trondheim in Trøndelag county, Norway. The total area of the watershed is and it runs for about from the source in the Sylan mountains to its mouth in Trondheimsfjorden. Trondheim Energiverk has fourteen power stations along the water course which are highly regulated, with a total production (in 2004) of . Development of the area had already begun in 1890 with the development of the Øvre Leirfoss power station. Important rivers in the Nea-Nidelvvassdraget
1382567
Forest of Dean Coalfield


where valleys cut through the rim of the basin, carboniferous limestone and sandstone are exposed, allowing water to penetrate underground via swallow holes, cracks, and fissures. Water also enters the basin through geological faults. In an attempt to reduce the pumping requirement, many mine owners 'waterproofed' the beds of watercourses with conduits or channels, wherever water loss was thought likely to occur. These artificial drainage features can be seen, at some point or other, on almost every watercourse within the mining area. For hundreds of years
10936754
Twomile Run


Run at its mouth ranges from 291 micro-Siemens to 1091 micro-Siemens, with an average of 663 micro-Siemens. There are a number of surface mines and deep mine complexes in the Twomile Run watershed. Some of the deep mine complexes extend into adjacent watersheds. There are several rock formations in the Twomile Run watershed which are visible on the surface. These include the Huntley Mountain Formation, the Burgoon Sandstone, the Pottsville Group and the Allegheny Group. The Huntley Mountain Formation is from Devonian and Mississippian times and
15498990
Battle of the Crater


known later as the First Battle of Deep Bottom. Union soldiers filled the mine with 320 kegs of gunpowder, totaling . The explosives were approximately under the Confederate works, and the T-gap was packed shut with of earth in the side galleries. A further of packed earth in the main gallery to prevent the explosion blasting out the mouth of the mine. On July 28, the powder charges were armed. Burnside had trained a division of United States Colored Troops (USCT) under Brig. Gen. Edward Ferrero to lead
5846300
Cooum River


and Chinese coins on the banks of the river. In the late eighteenth century, Pachaiyappa Mudaliar, the renowned philanthropist, bathed in this river before offering prayers at the Komaleeswarar Temple in Komaleeswaranpet. Cooum River and the nearby Elambore River (or North River), which flows into the Cooum at its mouth, were running very close to each other near the former Central Jail area opposite Chennai Central. During floods, both the watercourses inundated the whole area. In the 1700s, the two rivers were linked by a cut to
18984612
Sepik


May 1885. But the river, in fact, did not yet have a European name. It was thus termed "Kaiserin Augustafluß" by the explorer and scientist Otto Finsch, after the German Empress Augusta. The word 'Sipik' was first reported by A. Full as one of two names for the watercourse—the other being 'Abschima'—used by the natives living at the mouth of the river. A few years later, Leonhard Schultze applied the term 'Sepik' to the entire watercourse, and it took, although Schultze
9372594
Garden Island (South Australia)


connected to a road system that runs from the above-mentioned bridge. An electric power transmission line crosses the island in an east-west direction to a termination point at the Torrens Island Power Station. Garden Island is one of the geographical features in what is now the Adelaide metropolitan area that was formed as a consequence of sea level rise at the start of the Holocene. Sea level rise had three consequences. Firstly, watercourses existing at the time were forced to create new mouths in new coastline. Secondly, currents arising
17998920
River source


definition of a river source specifically uses the most distant point (along watercourses from the river mouth) in the drainage basin from which water runs year-around (perennially), or, alternatively, as the furthest point from which water could possibly flow ephemerally. The latter definition includes sometimes-dry channels and removes any possible definitions that would have the river source "move around" from month to month depending on precipitation or ground water levels. This definition, from geographer Andrew Johnston of the Smithsonian Institution, is also used
20534038
Royal National Park


the Hawkesbury sandstone belt lies Narrabeen Shales which is mixture of shale and sandstone under which and within which are untapped coal seams which run right through Sydney and are mined extensively where they come closer to the surface south of the National Park near Wollongong. Sections of recent alluvium fringes of estuarine watercourse where the endangered ecological communities; swamp oak woodlands and swamp mahogany woodlands grow still. Running the full coastal length of the park is a coastal heathland characterised by hardy, low-growing, salt-tolerant shrubs that spread across rocky,
13377724
North Creek (Toronto)


North Creek is a mostly buried watercourse that flows into Lake Ontario on the grounds of the former Lakeshore Psychiatric Hospital now in Colonel Samuel Smith Park. Its mouth was at Kipling Avenue. Its headwaters were near the present day intersection of the Queen Elizabeth Way and Browns Line. Almost all the creek had been buried by 1960, but part of the creek remains and mouth now flows in an easterly direction instead of southerly into Lake Ontario. The mouth of Etobicoke Creek was approximately 2.5 km to the west of the mouth of North
11160504
Long Run (Nescopeck Creek tributary)


acid mine drainage. The elevation near the mouth of Long Run is above sea level. The elevation of the stream's source is approximately above sea level. Long Run is one of the major tributaries of Nescopeck Creek. Several rock formations occur in the vicinity of the watershed of Long Run. These include the Mauch Chunk Formation, the Sphechty Kopf Formation, and the Pocono Formation. The watershed of Long Run has an area of . The mouth of the creek is in the United States Geological Survey quadrangle of Sybertsville, but
9789306
Don River (Ontario)


The Don River is a watercourse in southern Ontario, that empties into Lake Ontario, at Toronto Harbour. Its mouth was just east of the street grid of the town of York, Upper Canada, the municipality that evolved into Toronto, Ontario. Of the various watercourses that drained Toronto, the Don, the Humber River, and the Rouge River have headwaters in the Oak Ridges Moraine. The Don is formed from two rivers, the East and West Branches, that meet about north of Lake Ontario while flowing southward into the
15180333
Eider Canal


. Though the new canal's western end is farther south (at the mouth of the Elbe), much of the Eider Canal's watercourse was reused for the new waterway. Many sections were deepened, and some were straightened, cutting off bends that still exist as lakes. The new canal was opened by Kaiser Wilhelm II in 1895. In 1783, as part of the canal's development, three warehouses (called "packing houses" in German) were built along the watercourse: one at the Kiel-Holtenau lock
20050281
Lucky Run


Lucky Run be restored from McDade Park downstream to its mouth. At that time, the Pennsylvania Bureau of Abandoned Mine Reclamation was near to completing a project involving sealing of the stream's streambed to prevent infiltration into a mine pool. On 45 percent of Lucky Run, an impervious surface was observed. There is substantial tree debris rerouting the stream and parts of it experience erosion. In early May 2013, the temperature in the vicinity of Lucky Run was measured to be . The watershed of Lucky Run has an area of .
13559988
Lucky Run


Run joins Keyser Creek upstream of its mouth. In 2006, the Pennsylvania Turnpike Commission either applied for or received a permit to discharge stormwater into Lucky Run for construction purposes. There is one stormwater detention facility in the watershed. The stream receives runoff from the Pennsylvania Turnpike. Lucky Run lacks any perennial flow because it loses flow to underground mine pools. For this reason, it is unlikely to attain its designated uses. In 2013, it was recommended that the stream be assessed for flow loss. The elevation near the mouth
13559985
Jackson Creek (Toronto)


Jackson Creek is a watercourse that flows into Lake Ontario near 10th Street, in the New Toronto neighbourhood of Etobicoke, a suburb of Toronto, Ontario, Canada. It is part of the Great Lakes Basin. Its headwaters were approximately five kilometers northwest—north of Bloor Street, near Highway 427. Portions of the watercourse remain above-ground today. The creek is named for Jackson Farm, the historical location of its mouth. Even though lost, for now, Jackson Creek is a strong candidate for day-lighting with
14363282
Bonar Creek


Bonar Creek was a creek in Mimico, Ontario, Canada. It was a tributary of the still-existing Mimico Creek, a watercourse that empties into Lake Ontario. Bonar Creek joined Mimico Creek north of Lake Shore Boulevard, in the marsh at the mouth of the Mimico Creek. The creek is named for Irish immigrants Bill and Letitia Bonar who lived in a pumphouse near the waterway. Almost the entire creek has been buried, except for a short stretch where the former watercourse joined Mimico Creek, and that remaining portion has
20143285
Kampen, Overijssel


, the watercourse of the river IJssel was dredged several times, but the costs were relatively high and within a few years, the river silted up again. As the IJssel had several delta-like mouths here, the main route of the river shifted several times. In the 19th century, a new strategy was put in place to counter this problem: some watercourses were dammed to allow for more water at a higher speed through one or two main routes. This had the advantage that less sand and silt were deposited and
880447
Gaps of the Allegheny


22 followed alongside the watercourse through that particular gap. Just to the north, the famous Horseshoe Curve built by the Pennsylvania Railroad crosses or utilizes no less than four gaps of the Alleghenies as it wends its way to cross the drainage divide in its two climb-saving tunnels built through the summit to its marshaling yard in Gallitzin, PA. Until around the 1920s, after newly-founded auto clubs gathered enough numbers for political clout to push for initiatives creating roads between towns, beside the railroads, the primary means of travel
21430363
Zerbe Run


Run has an area of . The mouth of the stream is in the United States Geological Survey quadrangle of Sunbury. However, its source is in the quadrangle of Shamokin. The stream also passes through the quadrangle of Trevorton. The mouth of the stream is located within of Hunter. Zerbe Run is one of major streams in the watershed of Mahanoy Creek. Its watershed occupies a total of 8.3% of the Mahanoy Creek drainage basin. Most of the abandoned mine land in the watershed occurs to the south of the stream.
11868601
Shenandoah Creek


named tributaries: Kehly Run and Lost Creek. Kehly Run joins Shenandoah Creek upstream of its mouth and drains an area of . Lost Creek joins Shenandoah Creek upstream of its mouth and drains an area of . Shenandoah Creek is impaired by abandoned mine drainage throughout its length, and also by municipal point source pollution in one reach. Shenandoah Creek's contribution to the waters of Mahanoy Creek causes the latter creek's flow to nearly double. The elevation near the mouth of Shenandoah Creek is above sea level. The watershed of Shenandoah Creek
12384633
Twomile Run


Twomile Run is a tributary of Kettle Creek in Clinton County, Pennsylvania, in the United States. It is long. Tributaries of the stream include Huling Branch and Middle Branch Twomile Run. The stream flows through Leidy Township and Noyes Township. The stream's watershed has an area of approximately 9 square miles. Coal is mined in the watershed. Most of the acid mine drainage in Kettle Creek comes from Twomile Run. The discharge of Twomile Run at its mouth ranges from 200 to 10,000 gallons per minute. There are 2.1
15498980
Birch Island Run


upper reaches of Birch Island Run, the pH is naturally low, as opposed to being low due to acid mine drainage. The alkalinity level of the upper parts of the stream is low. There are two sources of acid mine drainage in the Birch Island Run watershed. Both discharge into Little Birch Island Run within of its mouth. The Birch Island Run watershed is largely in southwestern Clinton County. However, a small area is in southeastern Cameron County. Most of the watershed is forested and far from development. In specific
5089984
Spring Run (Solomon Creek tributary)


with Solomon Creek. Spring Run joins Solomon Creek upstream of its mouth. Spring Run has no named tributaries. However, it does have an unnamed tributary which joins Spring Run at the corner of Blackman Street and New Frederick Street. It also has a tributary known locally as Sulfur Run. The entire length of Spring Run is considered by the Pennsylvania Department of Environmental Protection to be impaired. The source of the impairment is abandoned mine drainage and the cause is metals and siltation. The abandoned mine drainage in the watershed has caused
2530068
Carbon Run


of the stream ranged from 14 to 44 Nephelometric Turbidity Units. The elevation near the mouth of Carbon Run is above sea level. The elevation of the stream's source is between above sea level. Carbon Run is a relatively small stream. There is a dam known as the Bear Valley Dam located on Carbon Run. Spoil piles and abandoned mining land occupies much of the stream's watershed. In some reaches, the stream flows underground due to infiltration into mine pools, but returns to the surface in the form of a
14126231
Drury Run


of streams; it consists of acid mine water discharging from a mine pool. The Stony Run sub-watershed has an area of . The pH of Drury Run ranges from 5.3 to 5.8 at a site downstream of Tamarack Swamp. At the mouth of Stony Run, the concentration of aluminum in the water is 7.11 milligrams per liter and there is a daily load of . The iron concentration is 0.29 milligrams per liter and the load of this metal is per day. The concentration of manganese is 11.81 milligrams per liter, with
7212058
Kolan River


then flows east and then finally north by east and reaches its mouth north of . The Kolan River is joined by nineteen tributaries including the main tributary, Gin-Gin Creek, a watercourse that is long. The lower reaches of the river are surrounded by sugar cane fields. The Mouth of Kolan River Regional Park is a protected area at the river mouth. The river descends over its course. Other water storage facilities that are supplied with water from the river include the Bucca Weir and the Kolan Barrage. "Macfadyena unguis
21876707
Forest of Dean Coalfield


limb that surfaces in the area of Staple Edge and the Soudley Valley producing the steeply dipping strata. An unusual feature of the Forest of Dean Coalfield is that its edges are almost entirely exposed at the surface. Mining in the coalfield has always been hampered by the excessive amount of water encountered underground - trapped by the basin-shaped strata. Water drains into the basin by general percolation and, more directly, via surface watercourses. For much of their length, streams in the area run over impervious clay deposits, but,
10936753
Dremmen


the landscape. In some places there is sand mining. The River Rur is the largest river in the district it flows past Heinsberg into Bleckden near Dremmen. The Rur frequently floods as far as Oberbruch. The river Wurm is by the North East side of Dremmen where the industrial area is situated by Hückelhoven. A small watercourse called Geilenkirchen-Rischden today runs underground in its place. In the Middle Ages a Mühlengraben (channel for the operation of water mills) was created, at Randerath where the river Wurm branched off.
2393704
White Oak Run (Lackawanna River tributary)


and reaches its confluence with the Lackawanna River. White Oak Run joins the Lackawanna River upriver of its mouth. White Oak Run has one officially named tributary, which is known as Indian Cave Creek. Indian Cave Creek joins White Oak Run upstream of its mouth. Its watershed has an area of . White Oak Run also has a number of unnamed tributaries. Some small mine seeps contribute iron hydroxide to White Oak Run. However, their effects are localized. Urban debris, construction debris, and other litter occur in the stream
21937799
Trout Run (Shamokin Creek tributary)


part of it or any of its tributaries is designated as impaired. The elevation near the mouth of Trout Run is above sea level. The elevation of the stream's source is between above sea level. Trout Run is a relatively small stream. The watershed of Trout Run is just north of the mining region. However, the stream itself is not impacted by mining. The stream drains part of the valley between Big Mountain and Little Mountain. Red shale of the Mauch Chunk Formation occurs in this valley. The valley is
13749065
Larrys Creek


wide here. Further south, it receives Roaring Run (on the left bank). Roaring Run receives the only acid mine drainage in the watershed and enters Larrys Creek from the mouth. Larrys Creek then heads southwest back into Mifflin Township, where it passes through the borough of Salladasburg, with Pennsylvania Route 973 running parallel to the creek from the township line to the borough. At Salladasburg, Larrys Creek receives its major tributary, the Second Fork of Larrys Creek, on the right bank from the mouth. The Second Fork
20558225
Edmund Rice (Medal of Honor)


Station, Glendale, and Malvern Hill. He was promoted to the rank of major on 7 Sep 1862 and fought at Antietam later in September 1862, and the Battle of Fredericksburg December 11–13, 1862. For his actions at the battle of Gettysburg in repelling Pickett's Charge, he was presented with the Medal of Honor in 1891. Made a lieutenant colonel 28 Feb 1864, he commanded his regiment in the Rapidan Campaign, the battles of Bristoe Station, Blackburn's Ford, Robinson's Cross Roads, and the Mine Run
3519594
Kettle Creek (Pennsylvania)


of the mouth. At the southern edge of Leidy Township, Kettle Creek makes several meanders, crossing the border between Leidy Township and Noyes Township three times. The creek then meanders several miles through Noyes Township, passing strip mines and another gauging station. The creek's mouth is at the community of Westport, near Pennsylvania Route 120. Significant tributaries to Kettle Creek include Germania Branch, Little Kettle Creek, Cross Fork, Hammersley Fork, Trout Run, Beaverdam Run, Twomile Run and others. In the upper reaches of Kettle
10473366
Benwood mine disaster


28, 1924 Benwood Mine Disaster was erected at the mouth of Boggs Run along Boggs Run Road/Roosevelt Avenue in Benwood, Marshall County, West Virginia. A committee of eight Marshall County, West Virginia residents known as the Benwood Mine Disaster Memorial Committee was formed in August 2011. Fundraising for the memorial began in 2012. Construction took place between 2013 - 2014. The memorial was formally dedicated on September 27, 2014. A smaller memorial for the five (5) victims of the May 18, 1942 Hitchman Coal &
21635421
Kraken


, and following this belching comes forth much food, so that all kinds of fish that are near to hand will come to present location, then will gather together, both small and large, believing they shall obtain their food and good eating; but this great fish lets its mouth stand open the while, and the gap is no less wide than that of a great sound or bight, And nor the fish avoid running together there in their great numbers. But as soon as its stomach and mouth is full, then
740342
The Trough


on Mill Creek Mountain followed by a series of knobs separated by spring gaps. It is at the third spring gap where Wickham was once located at on the railroad. Following Wickham, Mill Creek Mountain's Long Knob (1,725 feet) flanks the Trough. Sawmill Ridge ends at the mouth of the Trough at the point where Sawmill Run descends the ridge and joins the river. The communities of Sector and Glebe are located here to the west and east, respectively. The concrete piers of the old bridge that once carried Fleming
11779557
Interstate 64 in Virginia


Interstate 64 (I-64) in the U.S. state of Virginia runs east–west through the middle of the state from West Virginia to the Hampton Roads region, for a total of . It is notable for crossing the mouth of the harbor of Hampton Roads on the Hampton Roads Bridge–Tunnel, the first bridge-tunnel to incorporate artificial islands. Also noteworthy is a section through Rockfish Gap, a wind gap in the Blue Ridge Mountains, which was equipped with an innovative system of airport-style runway lighting embedded into the
19334193
Drury Run


and the alkalinity concentration is 0.83 milligrams per liter. The daily loads of these are and , respectively. To meet the U.S. Environmental Protection Agency's maximum allowable load requirements, the acidity load would need to be reduced by 99.5%. The total daily load of acid mine drainage in the watershed is per day. The concentration of sulfates at the stream's headwaters is 5.8 milligrams per liter, but at the mouth the concentration is 67 milligrams per liter. The concentration of sulfates at the mouth of the tributary Stony Run is
7212060
Laurel Run (Lackawanna River tributary)


Restoration Priority List of the Pennsylvania Department of Environmental Protection's Bureau of Abandoned Mine Restoration. The Pennsylvania Department of Environmental Protection once created a Mine Drainage Pollution Abatement Project for the stream. The drainage basin of Laurel Run is designated as a Coldwater Fishery and a Migratory Fishery. Wild trout naturally reproduce in the creek from its headwaters downstream to its mouth. Upstream of the Laurel Run Reservoir, the riparian buffer of Laurel Run consists of native trees and understory. From the Cawley Dam downstream to the Robert Casey Highway, the stream
21500300
Sugar Notch Run


to meet its total maximum daily load requirements. The alkalinity concentration of the stream is 29.56 milligrams per liter and the daily load is . The elevation near the mouth of Sugar Notch Run is above sea level. The elevation of the stream's source is between above sea level. Sugar Notch Run loses some of its flow to subterranean mine pools. The cracks in its streambed can be up to wide. In the stream's watershed, there are some cropfalls hundreds of feet deep lead into underground mine workings. In the early
3372699
Old Adaminaby and Lake Eucumbene


in 1912. He built a weatherboard house with corrugated iron roof surrounded by a number of outbuildings. The homestead was later extended in brick. It is remembered for having a large formal garden laid out by a landscape gardener from Andersons Seeds with a small watercourse running through it and many brick and stone edged beds and paths. Most of the Kyloe mine and town was submerged but there were three main visible sites near the waters edge. In 1995/96 some concrete pillars, concrete slabs, a stone track leading in the direction of
21747285
Circular breathing


, the musician must very quickly fill the lungs by inhaling through the nose prior to running out of the air in the mouth. If done correctly, by the time the air in the mouth is nearly exhausted the musician can begin to exhale from the lungs once more, ready to repeat the process again. Essentially, circular breathing bridges the gap between exhalations with air stored in the cheeks, an extra air reserve to play with while sneaking in a breath through the nose. The usual first difficulty is to inhale through the
17362155
Saxon Mining Office


the commissionin of Simon Bogner as mining advocate ("Bergvoigt") and Hans Röhlings as the mining office manager ("Bergamtsverwalter") on St. Matthew's Day, 21 Sep 1545. This process of establishment concluded with the appointment of Hans Röhlings' son, Markus Röhlings, as the senior master miner ("Oberbergmeister") of the Albertine Electorate of Saxony in 1554. The earliest forerunners to the senior mining officials of the 17th century may be considered to be "Lorenz von Schönberg", who was appointed in 1577
10184324
Trinity River (California)


Great Pyramid of Giza. In 1884 the California legislature banned hydraulic mining as the flow of tailings from hydraulic mines in the Sierra Nevada was silting up the Sacramento River, making it unnavigable. However, the Trinity hydraulic mines escaped this ban, as the remote and swift flowing Trinity River was not considered a navigable watercourse. Nevertheless, the largest deposits had been played out by the 1920s, and the mining settlements were abandoned or fell into decline. This brought on the last stage of commercial gold mining along the Trinity, as
511976
Crab Run (Mahanoy Creek tributary)


-northwest for a few tenths of a mile, flowing alongside the base of a mountain. The stream then turns north-northeast for a short distance, passing through a pond or small lake before reaching its confluence with Mahanoy Creek. Crab Run joins Mahanoy Creek upstream of its mouth. Some stream reaches in the watershed of Crab Run are not designated as impaired waterbodies. One stream reach is listed as impaired by metals from abandoned mine drainage, but no mining has been done in the watershed. Another stream reach is impaired
12984964
Carbon Run


Ferndale. The stream flows alongside Pennsylvania Route 125 for several tenths of a mile before turning north and entering Shamokin. Several tenths of a mile further downstream, it turns northwest and reaches its confluence with Shamokin Creek. Carbon Run joins Shamokin Creek upstream of its mouth. The entire length of Carbon Run is designated as an impaired waterbody. The cause of the impairment is metals other than mercury and the source of the impairment is abandoned mine drainage. Its two unnamed tributaries are also impaired. The stream is impacted by acid mine
14126227
2010 Tour of Qatar


a final sprint to the line with Heinrich Haussler coming in second, and Juan José Haedo arriving third. Like the previous stages, breakaways occurred and most were quickly reeled in. Sep Vanmarcke from made a break from the peloton and was away for much of the stage. At the to go mark, the gap was just below two minutes as was contributing the majority of the pace setting preserving the leader’s golden jersey for Wouter Mol. For the next , the gap hovered around the 1 minute and 45 second mark with
5647912
Laurel Run (Mill Creek tributary)


elevation near the mouth of Laurel Run is above sea level. The elevation near the creek's source is between above sea level. There are outfalls on Laurel Run in several places: Trethaway Street, the Mill Street bridge, and the Scott Street bridge. It also has a retaining wall in some places. The stream flows between Wyoming Mountain and Wilkes-Barre Mountain for part of its course. It also flows through the Laurel Run Gap. The watershed of Laurel Run has an area of . The watershed encompasses much of
4811185
Tennant Creek


named after a nearby watercourse of the same name, and is the hub of the sprawling Barkly Tableland vast elevated plains of black soil with golden Mitchell grass, that cover more than 240,000 square kilometres. Tennant Creek is also near well-known attractions including the Devils Marbles, Mary Ann Dam, Battery Hill Mining Centre and the Nyinkka Nyunyu Culture Centre The Barkly Tableland runs east from Tennant Creek towards the Queensland border and is among the most important cattle grazing areas in the Northern Territory. Roughly the same size as the United Kingdom
16148442
Madagascar (software)


the Stanford Exploration Project (SEP). Generations of SEP students and researchers contributed to SEPlib. Most important contributions came from Rob Clayton, Jon Claerbout, Dave Hale, Stew Levin, Rick Ottolini, Joe Dellinger, Steve Cole, Dave Nichols, Martin Karrenbach, Biondo Biondi, and Bob Clapp. Madagascar also borrows ideas from Seismic Unix (SU), a package maintained by John Stockwell at the Center for Wave Phenomenon (CWP) at the Colorado School of Mines (Stockwell, 1997; Stockwell, 1999). Main
6337097
Mining in the Upper Harz


Pit ponies were not used in the Upper Harz. From 1905 at the Clausthal Ore Mine ("Erzbergwerk Clausthal") underground haulage was carried out using conductor engines in the gallery known as the "Tiefsten Wasserstrecke" or "Deepest Watercourse". In the Grund Ore Mine ("Erzbergwerk Grund") battery-driven locomotives were used from the 1970s and, finally, diesel engines on wheels with rubber tyres. One feature mining in the Upper Harz was the underground transportation of material in boats on the "Tiefe Wasserstrecke"
7603407
Callender Gap Creek


, the Lackawanna River Watershed Conservation Plan recommended habitat restoration at the mouth of Callender Gap Creek. A grove of maple trees, a war memorial, and several picnic tables are located at the creek's mouth. The creek's use designation is for aquatic life. Callender Gap Creek is a coldwater fishery. Callender Gap Creek was entered into the Geographic Names Information System on November 1, 1989. Its identifier in the Geographic Names Information System is 1201573. In the early 2000s, the Lackawanna River Watershed Conservation Plan recommended that the
22087603
Josiah Gregg


the mouth of a watercourse which they called the Little River. After exploring slightly to the north, they turned south along the coast and camped at Trinidad. Leaving Trinidad, they crossed a large river, but the fed-up members of the exploring party did not wish to wait for Gregg to determine the latitude of the mouth, and so pushed off without him. When he caught up with the group, his temper flared, and they named the river Mad River due to the outburst. On 20 December 1849,
19632321
King Sound


King Sound is a large gulf in northern Western Australia. It expands from the mouth of the Fitzroy River, one of Australia's largest watercourses, and opens to the Indian Ocean. It is about 120 km long, and averages about 50 km in width. The port town of Derby lies near the mouth of the Fitzroy River on the eastern shore of King Sound. King Sound has the highest tides in Australia, and amongst the highest in the world, reaching a maximum tidal range of 11.8 metres at Derby. The
309139
Zerbe Run


. The headwaters of the stream are located in springs east of Trevorton. The upper reaches of the stream's watershed are not impacted by mining. A mine drainage discharge south of Trevorton empties into the stream, causing it to be significantly polluted from Trevorton downstream to its mouth. Zerbe Run is located just outside the Western Middle Anthracite Field. The dried sediment of the stream near Trevorton is dark brown on the Munsell color system. Further downstream, the sediment is strong brown on the Munsell color system. The watershed of Zerbe
11868600
North Mahanoy Creek


Mahanoy Creek upstream of its mouth. North Mahanoy Creek has no named tributaries. However, it does have a number of unnamed tributaries. Two of these are known unofficially as "Pole Run" and "Cold Run". Their lengths are , respectively. North Mahanoy Creek is designated as an impaired waterbody. The causes of impairment are sedimentation/siltation and water/flow variation and the likely source of impairment is abandoned mine drainage. The creek loses most or all of its flow to underground mines. The lower reaches of
13741631
Red Spring Run


Its mouth is in a concrete culvert. The headwaters of Red Spring Run are at the border between the Llewellyn Formation and the Pocono Formation. The surficial geology near the lower reaches of the stream mainly consists of alluvium (which contains stratified sand, silt, and gravel, as well as some boulders) and coal dumps. Further upstream, the surficial geology mostly features land that has been surface mined for coal, with some coal dumps to the east. Near the headwaters of the stream, there is surface mining land as
9966840
Prehistory of West Virginia


reports of Native American creating stone fishing weirs in creeks to facilitate gigging. Below the mouth of Loup Creek, a salt spring was a noted buffalo lick. The remains of a stone wall, with gaps, runs along the overlooking ridgeline. Around these gaps great quantities of elk, deer, bear and other bones are still found today. Dr. Thomas S. Buster, who resided in Fayette County for around 50 years in the 19th century, wrote of the ancient wall lying immediately above Armstrong's Creek, Mount Carbon Stone Walls
6856784
Sep Lambert


the MCC, Oxford University and Cambridge University. He played once in 1903 against London County, and twice in 1904 against South Africa and Cambridge University. He played a match against HDG Leveson-Gower's XI in 1905, before another gap in appearances, this time for eleven years, returning for a match against Scotland in July 1911. Another long gap followed, though much of this can be explained by Ireland not playing between 1915 and 1919 due to the First World War. He did play three more times for Ireland
17780529
Roaring Brook (Lackawanna River tributary)


The first bridge over the stream was built in 1859. In 1870, the Scranton family constructed a mansion on the stream. In the early 1900s, the main industries in the watershed of Roaring Brook included agriculture, brick making, and coal mining. Around this time, the Delaware, Lackawanna and Western Railroad followed the stream throughout much of its length and the Erie Railroad followed the stream from Elmhurst to its mouth. The former was created by an 1852 merger of the Cobbs Gap and Delaware Railroad and the Lackawanna and Western
13856201
1st Sussex Engineers


gunfire and then by enemy demolitions. The road was cut into a cliff, overhanging a railway line, part of which ran through a tunnel whose mouth had been blown in. Calculating that a bridge was required across the gapped road, the CRE ordered up one field company and a Bailey bridge platoon. A Canadian tunnelling company was also called up to widen the approach road by removing the cliff above it, and a bomb disposal section had to check the tunnel for mines and booby-traps. Eventually, the bridge assembly
20701841
Little Cacapon, West Virginia


Little Cacapon is an unincorporated community in Hampshire County in the U.S. state of West Virginia. Little Cacapon is located at the mouth of the Little Cacapon River on the Potomac, east of Okonoko. Okonoko-Little Cacapon Road (West Virginia Secondary Route 2/7) and Spring Gap-Neals Run Road (West Virginia Secondary Route 2) converge south of Little Cacapon. Because of its key location at the mouth of the Little Cacapon and on the Baltimore and Ohio Railroad, Little Cacapon played important roles in both the French and Indian
3921816
Blair Gap


of the Allegheny Portage Railroad, which as was authorized by the enabling acts in 1824 of Pennsylvania's Main Line of Public Works as part of the Pennsylvania Canal System which originally envisioned linking Pittsburgh to Philadelphia by canals. In the early 1900s, US Route 22 followed alongside the watercourse through the gap. Until around the 1920s, after new founded auto clubs gathered enough numbers to political clout to push for initiatives creating roads between towns, off the railroads the primary means of travel town to town was on foot or where hauling was
21430007
OK Mine & Smelter


small watercourse. An intact Pooley and Sons Ltd, Birmingham and London No 524, steel weighbridge is located on a former access track on the east side of the slag dump. The mine workings southwest of the smelter comprise a large open cut containing several mine shafts. Rendered stone water tanks are located above the smelter terraces, and a limestone deposit is located to the west. OK Mine & Smelter was listed on the Queensland Heritage Register on 2 October 1996 having satisfied the following criteria. The place is important in demonstrating the
21569810
Esquel, Argentina


often a destination for "Medical Tourism" from both foreigners and Porteños (residents of Buenos Aires) alike. The townspeople have been in a long battle to prevent a gold mine being set up nearby, with concerns that the metal extraction will pollute the watercourse permanently and irreversibly. Although the mining companies were prohibited from producing mines in the area, there are still monthly street marches against the mines, and the issue never seems to feel fully settled. In May 2009, Esquel twinned with Aberystwyth in Wales; with representatives of
455935
Mutoshi Mine


, and was initially worked for gold. Between 1960 and 1987 a washing plant at the mine discharged mineralized material into the Kulumaziba watercourse. Samples of the first of the deposit indicated a resource of about 102,000 tonnes of contained copper. In November 2004, Anvil Mining agreed to pay US$12.5 million for a 70% interest in the Mutoshi copper-cobalt project from the state-owned Gécamines and the private DRC company Emiko. The property included the old Mutoshi mine, the Kulumaziba coarse rejects/tailings deposit, the Mutoshi Northwest
4574845
Mine railway


, but eventually adding protective iron, steam locomotion by fixed engines and the earliest commercial steam locomotives, all in and around the works around mines. Wagonways (or tramways) were developed in Germany in the 1550s to facilitate the transport of ore tubs to and from mines, using primitive wooden rails. Such an operation was illustrated in 1556 by Georgius Agricola of Germany (Image right). This used "Hund" carts with unflanged wheels running on wooden planks and a vertical pin on the truck fitting into the gap between the
3857313
Discovery Bay, Washington


Peninsula of Washington state. The bay enters the Strait of Juan de Fuca between the Miller and Quimper peninsulas. The bay's mouth is just south of Protection Island, a small federally protected nature preserve. Discovery Bay is in length, and wide at its mouth. Its primary inlet is Snow Creek at the south end of the bay, and other small watercourses feed the bay on its east and west sides. The community of Discovery Bay is an area near the intersection of U.S. Route 101 and State Route 20, at
9005206
Goat Rock Beach


, especially in the pupping season. The Russian River, with its mouth at the north end of Goat Rock Beach, is Sonoma County's largest watercourse, both in flow rate and lineal extent. Immediately beyond the Russian River discharge to the Pacific Ocean is the coastal town of Jenner. North of the mouth of the Russian River is Jenner Beach. Goat Rock protrudes into the Pacific at the south end of Goat Rock Beach. Visitors can access the base of Goat Rock via a low lying isthmus of land which has been
9690212
Linn (geology)


In Scotland and northern England a Linn is a geographical water feature. In Scotland it describes where a watercourse has cut through a shelf of hard rock creating a narrow (usually), steep-sided cut though which the watercourse runs. Typically there is only one named Linn on any watercourse - although obviously - there may actually be more than one feature with the necessary attributes. The photograph of the Linn of Dee illustrates the attributes of a typical 'Linn'. In "Gordon (1925)" the author describing a
13483383
Yentna-Cache Creek mining district


prospect assayed about of gold per ton. A bucketline dredge was constructed in Cache Creek in the 1920s, and used locally-abundant coal to fire the boilers. Later, a hydroelectric plant was used to run the dredge. The dredge mined the entire valley of Cache Creek as far as the mouth of Nugget Creek, then bulldozers mined what remained. Hydraulic mining was also widely used before 1942, and many ditches can be found all over the Dutch Hills today. About 115,000 ounces of placer gold was reported to have been
9754443
Furnace Run (Shamokin Creek tributary)


could experience flow augmentation. Mine seepage has contributed flow to the stream. However, in the 1950s, it was diverted into underground mines, reducing the stream's ability to carry away waste in its channel. In 1999 and 2000, the flow rate of the stream ranged from . In 1999 and 2000, the water temperature of the stream ranged from in March 2000 to in August 1999. The elevation near the mouth of Furnace Run is above sea level. The elevation of the stream's source is between above sea level
13896348
Sep Lambert


regular in the Irish side, his international career contains several large gaps between matches, and it was three years before he played his second match for Ireland, also against I Zingari in August 1899. Another three-year gap followed, before he made his first-class debut for Ireland, against London County in May 1902, in what was also Ireland's first first-class match. This was a rare period of consistent selection for Ireland, and he played three further first-class matches again that month, against
17780528
Logan/Esterly Upper Ditch


The Logan/Esterly Upper Ditch is an abandoned, artificial watercourse in the Illinois River Valley of northern California and southern Oregon, United States. Built in 1854 to supply water from the river's East Fork in California to several hydraulic mines in Oregon, it quickly returned a large profit to its investors. The ditch supplied mines worked by its own owners, as well as providing water for sale to other nearby diggings and incidentally powering at least one sawmill. Mines it served include the Waldo, Fry Gulch, and Cameron mines
18184789