OpenLLM-France/wikimedia huggingface dataset:
# Gachua Union

Gachua (Bengali: গাছুয়া) is a union in Sandwip upazila of Chittagong district in Bangladesh.

## Geography

Location of Gachua Union is in the northern part of Sandwip upazila. The distance of this union from Upazila Sadar is about 10 kilometers. Santoshpur Union is in the north of this union, Amanullah Union and Kalapania Union is in the west. It is bounded on the south by Bauria Union and on the east by Sandwip Channel, Syedpur Union and Muradpur Union of Sitakunda Upazila.
The area of Gachua Union is 3463 acres (14.08 km$^2$) as of the census of 2006.
Sandwip Channel is located on the east side of Gachua Union. There are also many small canals.

## Population

According to the 2011 census, the population of Gachua Union is 16,078. Of these, 7,128 are males and 8,950 are females.

## Administrative structure

Gachua Union is No. 3 Union Parishad under Sandwip Upazila. It is part of Jatiya Sangsad Constituency No. 270 Chittagong-3. Administrative activities of the union are under Sandwip police station. It is divided into 3 mouzas.
The villages of this union are:
* Hadia Para
* Mohammadpur Para
* Latif Bhuiyan Para
* Dhaner and Abur Go Para
* Saudar Go Para
* Chobi Rahman Para
* Roushan Ali Para
* Bereer Par Para

## Education system

Gachua Union has an average literacy rate of 48.63%. The union has 1 Fazil Madrasa, 3 secondary schools, 11 primary schools and 9 Ananda schools.

## Educational institutions
### Madrashas

* Katgarh Islamia Fazil Madrasa

### Secondary schools

* Abdul Khaleq Academy High School
* Gachua Adarsh High School

### Primary schools

* North Azimpur Government Primary School
* Kashem Market Government Primary School
* Gachua AK Government Primary School
* Gachua Ghatmajhir Hat Government Primary School
* Gachua South-West Government Primary School
* Gachua South-East Government Primary School
* Gachua Madhyapara Government Primary School
* Char Hudrakhali Government Primary School
* Dadan Shaheed Belayet Bir Uttam Government Primary School
* Sandwip Gachua Banglabazar Government Primary School
* Sandwip Gachua Scouts Government Primary School

## Communication system

The main road from Upazila Sadar to Gachua Union is the Sandwip-Gachua road. There is also Sarikait-Santoshpur road. Means of communication are taxi, motorcycle, rickshaw, bicycle.

## Local markets

The main market of Gachua Union are Ghatmajhir Hat, Akbar Hat, Haq Saheb Bazar, Bangla Bazar, Kashem Market and Banir Hat and some part of Ershad Market.

## Illustrious personalities

* M Obaidul Haque –– The first Member of Parliament for Sandwip.
* Belayet Hossain –– A heroic freedom fighter with the title of Bir Uttam.
* Master Shafiqul Alam –– Bir Muktijoddha and former chairman.

## Public representative

* Current Chairman: Mohammad Shamsuddin

### List of chairmen

| Sr. No. | Chairman's name | Duration |
| 01 | Haji Abdus Sattar | |
| 02 | Master Shafiqul Haque | 1983-2003 |
| 03 | Mohammad Walidur Rahman | 2003-2011 |
| 04 | Mohammad Shamsuddin | 2011–present |
# North Branch Penobscot River

The North Branch Penobscot River is a river in Somerset County, Maine. From its source at the outlet of Little Bog (46°09′23″N 69°57′21″W﻿ / ﻿46.1563°N 69.9557°W﻿ / 46.1563; -69.9557﻿ (North Branch Penobscot River source)) about 10 miles (16 km) east of the Canada–United States border in Maine Township 6, Range 17, WELS, the river runs 27.8 miles (44.7 km) southwest and southeast to its drowned confluence with the South Branch of the Penobscot River in Seboomook Lake in Pittston Academy Grant (T.2 R.4 NBKP).
In 1939, the Great Northern Paper Company impounded Fifth St. John Pond in T.6 R.17 and dug a 2-mile-long (3.2 km) canal from the pond allowing the diversion of water from the Saint John River's Baker Branch into the Penobscot's North Branch, to sluice wood to the company mill at Millinocket. Yellow perch also used the canal to spread into the upper Penobscot River drainage.
# North Branch River

The North Branch River is an 8.2-mile-long (13.2 km) river in southeastern New Hampshire in the United States. It is a tributary of the Lamprey River, part of the Great Bay and Piscataqua River watershed leading to the Atlantic Ocean.
The river begins in Bear Brook State Park, in Deerfield, New Hampshire, at the outlet to Beaver Pond. Flowing southeast, it quickly leaves the park, then enters the town of Candia. It passes under New Hampshire Route 43 just south of the village of Candia, then reaches NH 27 just before entering the town of Raymond, where the river ends at the Lamprey River.
# North Fork American River

The North Fork American River is the longest branch of the American River in Northern California. It is 88 miles (142 km) long from its source at the crest of the Sierra Nevada, near Lake Tahoe, to its mouth at Folsom Lake northeast of Sacramento. Prior to the construction of Folsom Dam the river was about 9 miles (14 km) longer making for a total length of 97 miles (156 km).
It rises at Mountain Meadow Lake near the 9,008 ft (2,746 m) peak of Granite Chief in the Tahoe National Forest. Flowing initially northwest, the river soon swings west into a gorge, paralleling the Forest Hill Divide on the south. Big Granite Creek then joins the North Fork of the American River coming in from the right. The canyon shallows as the river turns southwest, carving through the Sierra foothills, then turning abruptly south near Colfax. About 4 miles (6.4 km) downstream, it receives Shirttail Creek from the left then is impounded in Lake Clementine (or North Fork Lake) which is formed by the North Fork Dam, built in 1939 to contain hydraulic mining debris.
Below the dam, the river bends south, passing under the Foresthill Bridge, the highest bridge in California, then receives the Middle Fork American River, its largest tributary, from the left. The valley widens as the river flows south past Auburn, soon emptying into the north arm of Folsom Lake, a reservoir formed in 1955 by the Folsom Dam. Its waters merge in the lake with those of the South Fork American River and form the American River, a tributary of the Sacramento River.
# Esther George

Esther L. George (born January 15, 1958, in Faucett, Missouri) is the former president and chief executive of the Federal Reserve Bank of Kansas City from 2011 until 2023.
George is a native of Faucett, Missouri, U.S., and received a BSBA degree in Business Administration from Missouri Western State University and an MBA degree from the University of Missouri-Kansas City. She is a graduate of the American Bankers Association's Stonier Graduate School of Banking and the Stanford Graduate School of Business.
She joined the Federal Reserve Bank of Kansas City in 1982 and held various leadership positions with the Bank, including in the Bank's research support functions, Public Affairs and Human Resources. In 2001 she became the bank's senior vice president in the Bank's Division of Supervision and Risk Management. In 2009 she was named executive vice president in charge of the unit. She is a former chair of the Federal Reserve System's Community Banking Organizations Management Group.
She was appointed to the Kansas City Fed President position on October 1, 2011. She retired on January 31, 2023, after reaching the mandatory retirement age for Federal Reserve Bank Presidents.
George was named the 2023 Harry S Truman Public Service Award Recipient, an award established in 1974 by the city of Independence, which is presented annually to an American citizen who “typifies and possesses President Truman’s qualities of dedication, industry, ability, honesty and integrity.”
# North Fork Smoky Hill River

The North Fork Smoky Hill River is a river in the central Great Plains of North America. A tributary of the Smoky Hill River, it flows from eastern Colorado into western Kansas.

## Geography

The North Fork Smoky Hill River rises in the High Plains region of the Great Plains. Its source lies in extreme northern Cheyenne County, Colorado 29 miles (47 km) west-northwest of Cheyenne Wells, the county seat. From there, the river flows east then east-northeast into Kansas. In south-central Sherman County, it has been dammed to form a small reservoir, Sherman State Fishing Lake. A few miles east of the reservoir, the river turns southeast and continues to its confluence with the Smoky Hill River in central Logan County 5 miles (8.0 km) west of Russell Springs.
The river has a total length of 195 miles (314 km) and drains an area of 759 square miles (1,970 km$^2$).

## Hydrology

The river is intermittent with water flowing only during and after rains.
# North Fork Stanislaus River

The North Fork Stanislaus River is a 31.2-mile (50.2 km) tributary of the Stanislaus River in the central Sierra Nevada and Stanislaus National Forest of eastern California.

## Geography

The river flows southwest from Alpine County, through Calaveras County, to Tuolumne County.
The river begins at the confluence of Silver Creek and Duck Creek near the western edge of the Carson-Iceberg Wilderness in the Sierra Nevada. From there it flows southwest through a canyon to its confluence with the Middle Fork Stanislaus River near Forest Meadows, which forms the Stanislaus River. The river drains a mountainous, rugged watershed of about 196 square miles (510 km$^2$).

## Hydroelectricity infrastructure

Since the 1980s, the river basin has been extensively developed for hydropower generation. Water from the North Fork is stored in Alpine, Utica, Union and New Spicer Meadows Reservoirs, which regulate the water supply for McKays Point Diversion Dam, located lower down on the North Fork. From McKays Point water is diverted to the Collierville Powerhouse, which can generate up to 253 megawatts.
# U.S. Route 10 in North Dakota

U.S. Highway 10 (US 10) in North Dakota runs 8.042 miles (12.942 km) from Interstate 94 (I-94)/US 52 near West Fargo east through Fargo before crossing the Red River of the North and entering Moorhead, Minnesota. US 10 serves as a primary east–west corridor through the Fargo–Moorhead (Main Avenue) and is concurrent with I-94 Business for its entire length in North Dakota.

## Route description

US 10 begins as a four-lane highway with a median at a trumpet interchange with I-94/US 52 (exit 343) just west of West Fargo. Once entering West Fargo, US 10 passes to the north of Bonanzaville, USA, a history museum complex before entering the downtown area of West Fargo. Continuing east, US 10 enters Fargo at its intersection with 45th Street and then intersects I-29/US 81 (exit 65) at a partial cloverleaf interchange a mile (1.6 km) later. East of this interchange, US 10 loses its median but remains two lanes each direction after intersecting 25th Street. After this intersection, US 10 curves slightly southeast and runs along the Northern Transcon railroad tracks, heading into downtown. In downtown Fargo, US 10 passes to the south of the former Fargo station, which is listed on the National Register of Historic Places. At the east end of downtown Fargo, US 10 intersects 2nd Street at a roundabout before crossing over the Red River of the North and into Moorhead, Minnesota, on the Veterans Memorial Bridge.
All of US 10 in North Dakota is part of the National Highway System, a network of highways that are considered essential to the country's economy, defense, and mobility by the Federal Highway Administration.

## History

Prior to 1986, US 10 ran along I-94 into Montana. The route was decommissioned west of Fargo in 1986.

## Major intersections

The entire route is in Cass County.
| Location | mi | km | Destinations | Notes |
| West Fargo | 0.000 | 0.000 | I-94 / US 52 – Bismarck, Fargo I-94 BL begins | Western terminus of US 10; western end of I-94 Bus. concurrency; I-94 exit 343 |
| Fargo | 5.009 | 8.061 | I-29 / US 81 – Sioux Falls, Grand Forks | I-29 exit 65 |
| Fargo | 7.025 | 11.306 | US 81 Bus. south (University Drive) | |
| Fargo | 7.221 | 11.621 | To US 81 Bus. north / 9th Street | |
| Red River of the North | 8.043 | 12.944 | Veterans Memorial Bridge; North Dakota–Minnesota line | Veterans Memorial Bridge; North Dakota–Minnesota line |
| Red River of the North | 8.043 | 12.944 | I-94 BL east / US 10 east – Moorhead | Continuation into Minnesota |
| 1.000 mi = 1.609 km; 1.000 km = 0.621 mi Concurrency terminus |||||
# North Laramie River

The North Laramie River is a tributary of the Laramie River, 86.4 miles (139.0 km) long, in southeastern Wyoming in the United States.
It rises in the Medicine Bow National Forest in the Laramie Mountains, in northern Albany County. It flows south, then east-northeast and east, emerging from the mountains and joining the Laramie River approximately 5 miles (8 km) north of Wheatland.
# Tuva'a Clifton

Tuva'a Clifton (born 29 June 1997) is a canoeist. Born in New Zealand, he represents Samoa internationally. He competed in the men's K-1 1000 metres event, K-1 200 metres event and K-2 1000 metres event at the 2020 Summer Olympics. He made the team via the quota place for Samoa after achieving a time within the limit in a qualification heat.
Clifton's family comes from New Zealand, Samoa and the Falkland Islands, with him spending his early life in New Zealand. Before becoming a kayaker, Clifton was a lifesaver at Muriwai Beach in New Zealand. Clifton has two sisters, with one of them taking part in a national kayaking programme in New Zealand.

## Radio Host at 95bfm

As well as canoeing, Clifton is currently a radio host at the Auckland alternative radio station 95bFM. He runs a weekly show every Wednesday 10am-12pm.
# North River (Missouri)

The North River is an 82-mile-long (132 km) river in northeastern Missouri, the United States. It rises in Knox County at 40°03′30″N 92°15′26″W﻿ / ﻿40.05833°N 92.25722°W﻿ / 40.05833; -92.25722 (northwest of Novelty) and flows southeast and east through Shelby and Marion counties, emptying into the Mississippi River at 39°51′21″N 91°26′41″W﻿ / ﻿39.85583°N 91.44472°W﻿ / 39.85583; -91.44472 between West Quincy and Hannibal.
The North River drainage area is 373 square miles (970 km$^2$), with a median flow of 38 cu ft/s (1.1 m$^3$/s) and a mean flow of 231 cu ft/s (6.5 m$^3$/s) based on 72 years of record at the USGS Palmyra gaging station. Record flow was on April 21, 1973 at 57,500 cu ft/s (1,630 m$^3$/s). During droughts flow sometimes drops to 1 cu ft/s (28 L/s) or less.

## Tributaries

Named tributaries of North River include Lazy Branch, Sidnor Creek (Palmyra Big Spring Branch), Lick Creek, Big Branch, Little North River, Hawkins Branch, Merrills Branch, Tiger Fork, Weldons Branch, Looney Creek, Clear Creek, Mesner Branch, Garnett Branch, and Owl Creek.

## History of name

The river is believed to be a candidate for the "River Jeffreon" that was referenced in the 1804 Treaty of St. Louis presided over by William Henry Harrison with the Sac and Fox. Zebulon Pike identified this river as the Jeffreon in his August 19 journal entry with the spelling "Jauflione", although no distinction other than "The Jauflione is about 30 yards wide at its mouth, and bears from the Mississippi about S.W." serves to distinguish it from the nearby Fabius Rivers or South River. The island across the Mississippi River from the outlet of these tributary rivers is labeled "Jeffreon" on Pike's map. The River Jeffreon marked the northern border of Sac and Fox land ceded in Missouri (extending north from the mouth of the Gasconade River on the Missouri River and then down the river to the Mississippi. In the same treaty the tribes ceded much of northern Illinois and southern Wisconsin on the east side of the Mississippi. Several legal cases stemming from the 1804 treaty have identified North River as the River Jeffreon.
It derived its current name from its position relative to Palmyra, Missouri. The North River flows north of that town and the South River flows south of it, with the outlets into the Mississippi being shared at times in the past and still within 1,500 feet (460 m) of each other. On some maps from the early 19th century, these rivers are labeled as "North Two Rivers" and "South Two Rivers".
# North River (South Fork Shenandoah River tributary)

The North River is a 55.3-mile-long (89.0km) river in the mountains and Shenandoah Valley of northern Virginia, the United States. It joins the South River at Port Republic to form the South Fork Shenandoah River.
The river rises at 4,000 feet (1,200 m) above sea level in western Augusta County, below Dyers Knob on Shenandoah Mountain along the Virginia-West Virginia border. From the man-made Elkhorn Lake it flows south and then east through the George Washington National Forest. The river breaks out of the Allegheny Mountains at North River Gap and flows into the broad Valley of Virginia. The river passes through the town of Bridgewater and flows southeast, joining the South River at Port Republic. The Middle River, a major tributary, joins the North River just west of the town of Grottoes, four miles above the juncture with the South River.
Other towns along the river include Mount Solon, Stokesville, Sangersville, Natural Chimneys, Mount Crawford, and the village of North River.
The river is popular among canoeists, rafters and inner tubers. At one point during the 19th century barges shipped goods upstream via a canal/lock system.
Typical wildlife of the North River includes the great blue heron, wood duck, Canada goose, belted kingfisher, Baltimore oriole, painted turtle, common snapping turtle, largemouth bass, sun perch, catfish, eastern cottontail rabbit, white-tailed deer, raccoon, opossum, brown bats, freshwater clams, mink, tiger swallowtail and ebony jewelwing.
Typical plant life of the North River includes the cardinal flower, joe-pye weed, purple monkeyflower, great blue lobelia, bulrush, yellow iris, American sycamore, cottonwood, box-elder, silver maple, Virginia bluebells, and spring beauty.
# Robert Elliott's Wholesale Grocery

Robert Elliott's Wholesale Grocery is a historic commercial building located at Hannibal, Marion County, Missouri. It was built about 1886, and is a two-story brick structure. It features semicircular arches with fanlight tops on the first floor, upper windows with segmental arches, and an applied cornice, possibly metal.$^{:58–59}$
It was added to the National Register of Historic Places in 1986.
# North Santiam River

The North Santiam River is a 92-mile (148 km) tributary of the Santiam River in western Oregon in the United States. It drains 766 square miles (1,980 km$^2$) of the Cascade Range on the eastern side of the Willamette Valley east of Salem.
It rises in the high Cascades in eastern Linn county, northwest of Three Fingered Jack in the Willamette National Forest. It flows north through the mountains past Marion Forks, receiving the drainage from the western slope of Mount Jefferson. Near Mount Jefferson it turns sharply west, descending through a canyon past Idanha and Detroit to Niagara County Park where the valley begins to widen and some agriculture use begins. Continuing west, the river flows past Gates, Mill City and Mehama. It emerges through the foothills into the Willamette Valley near Stayton, then flows 15 miles (24 km) southwest through the valley where it joins the South Santiam River to form the Santiam River. The confluence is approximately 10 miles (16 km) east of the confluence of the Santiam and the Willamette River.
It is impounded by Detroit Dam in the mountains west of Detroit to form Detroit Lake for flood control. Detroit Lake State Park is along the northern shore of the lake.
In the 19th century, the canyon of the North Santiam River provided a formidable obstacle to settlers. The construction of a railroad in 1887 opened up the canyon to settlement and logging of the surrounding mountains.

## Fauna

Blocked by Big Cliff Dam near Mill City, the lower North Santiam River supports spring chinook salmon and summer steelhead. In the reaches upstream of the dam, the river is managed mainly as a stocked-trout fishery. Near the stream's source at Santiam Lake in the Mount Jefferson Wilderness, native cutthroat trout, rainbow trout, and introduced brook trout are also found.
The headwaters of Marion Creek, a tributary of the North Santiam River, originate at Marion Lake, which is a location of many wildlife species. This headwaters area is a breeding location for amphibians including the rough-skinned newt.

## Watershed

Ten cities draw their drinking water from the North Santiam watershed: Detroit, Gates, Idanha, Jefferson, Lyons, Mehama, Mill City, Salem, Stayton, and Turner.
# Johann Riederer

Johann "Hans" Riederer (born 30 December 1957) is a German sports shooter and Olympic medalist. He won bronze medal in the 10 metre air rifle at the 1988 Summer Olympics in Seoul, and at the 1992 Summer Olympics in Barcelona. Riederer was born in Unterföhring, Bavaria.
# Middle Creek (Opequon Creek tributary)

Middle Creek is a 9.7-mile-long (15.6 km) tributary of Opequon Creek, belonging to the Potomac River and Chesapeake Bay watersheds, located in Berkeley County in West Virginia's Eastern Panhandle.

## Headwaters and course

Middle Creek's source is located on the eastern foothills of North Mountain (1644 feet/501 m) southwest of Martinsburg. From its headwaters, Middle Creek is a small meandering stream that curves southward paralleling Poorhouse Road until its junction with West Virginia Route 45. Throughout this stretch, Middle Creek is joined by a number of spring-fed streams off of North Mountain, most of which are used for watering animals on the area's farmlands. After it passes beneath WV 45, Middle Creek continues its course to the southeast near the community of Arden. The stream is dammed numerous times to create small lakes and ponds, as well as light rapids. Middle Creek passes under Interstate 81 and U.S. Route 11 before it meanders to the east through the town of Darkesville. From Darkesville, Middle Creek winds through a series of gorges created by rolling hills before its confluence with Opequon Creek.

## Water quality

The water quality of Middle Creek is very mixed. While the creek is in the North Mountain, its water quality is general good because of the low pollution and the low population of North Mountain. Its water quality dramatically drops once it joins the spring-fed streams because of agricultural run-off. Due to numerous dams though, this run-off doesn't always make it to the Opequon Creek. When it joins the Opequon, its water quality is good to moderate.

## Water flow

Due to water runoff during rainfall, the water flow of Middle Creek varies. In the spring, the creek's output of water is very high due to wet conditions during spring. In the summer, the water flow is usually normal, with Thunderstorms raising the water, and short-term droughts lowering the water. In the fall, the water level is usually below-normal due to dry conditions and lower rainfall. During the winter however, the creek is usually at its highest because of low evaporation caused by cold temperatures and thick cloud covers. The creek rarely freezes over, but sometimes stagnant water will freeze through.

## Flora and fauna

Middle Creek is home to many species of crayfish and minnow. Many species of turtles also inhabit the creek, most notably the eastern box turtle. Snakes are very common, with copperheads and garter snakes being the most numerous. Many species of mammals live near the creek's water, the biggest being the white-tailed deer. Plants types that live along the creek include grasses, water lilies, and aquatic plants. Sycamore trees, tulip trees, and willow trees dig their roots along the creeks banks.