davidanugraha/M4-RAG huggingface dataset:
Sōmen

Sōmen (Japanese: 素麺), somyeon (Korean: 소면; 素麵), or sùmiàn (Chinese: 素麵) is a very thin noodle made of wheat flour, less than 1.3 mm in diameter. The noodles are used extensively in East Asian cuisines. Japanese sōmen is made by stretching the dough with vegetable oil, forming thin strands that are then air dried for later use. This is distinct from a similar thin noodle, hiyamugi, which is knife-cut.
In Japan, sōmen is usually served cold with a light dipping sauce called tsuyu. South Korean somyeon may be eaten in hot or cold noodle soups. Sōmen is typically high in sodium.
Other names are nyūmen (煮麺) in Japanese, for a version served warm in soup, and the Chinese name guàmiàn (Chinese: 掛麵), which can be further classified into lóngxū (Chinese: 龍鬚; lit. 'Dragon Whiskers') for the variant with long and thin strands and fèngwei (Chinese: 鳳尾; lit. 'Phoenix Tail') for the variant with flat and broad strands.
The earliest record for what would later be sōmen dates back to the Tang dynasty in 618-907 China. Around that time, the Japanese Imperial Court in Nara brought in some knotted pastry from China which they called Sakubei/索餅 (most likely Chinese Mahua/麻花). Sakubei would later evolve into Somen first in modern day Sakurai, Nara's Miwa district during the Heian Period and would evolve to become high-class Japanese cuisine which would be served to emperors and nobles.
Sōmen are usually served cold with a light flavored dipping sauce or tsuyu. The tsuyu is usually a katsuobushi-based sauce that can be flavored with Japanese bunching onion, ginger, or myoga. In the summer, sōmen chilled with ice is a popular meal to help stay cool.
Sōmen served in hot soup is usually called nyūmen and eaten in the winter, just like soba or udon are.
Some restaurants offer nagashi-sōmen (流しそうめん flowing noodles) in the summer. The noodles are placed in a long flume of bamboo across the length of the restaurant. The flume carries clear, ice-cold water. As the sōmen pass by, diners pluck them out with their chopsticks and dip them in tsuyu. Catching the noodles requires a fair amount of dexterity, but the noodles that are not caught by the time they get to the end usually are not eaten, so diners are pressured to catch as much as they can. A few luxury establishments put their sōmen in real streams so that diners can enjoy their meal in a beautiful garden setting. Machines have been designed to simulate this experience at home.
In Korean cuisine, somyeon is used in hot and cold noodles soups such as janchi-guksu (banquet noodles) and kong-guksu (noodles in cold soybean soup), as well as soupless noodle dishes such as bibim-guksu (mixed noodles). It is often served with spicy anju (food that accompanies alcoholic drink) such as golbaengi-muchim (moon snail salad).
Third World Romance

Third World Romance is a 2023 Filipino romance film co-written and directed by Dwein Baltazar. The film stars Carlo Aquino and Charlie Dizon in the lead roles, with the supporting cast includes Ana Abad Santos, Archie Adamos, and Gardo Versoza. The film tells the story of two blue-collar workers who meet at the height of the COVID-19 pandemic and they become co-employees at a grocery store. However, their budding romance is beset by persistent economic difficulties.
Produced by Black Sheep Productions and ANIMA and distributed by Star Cinema, it was released theatrically on 16 August 2023.
The film was announced by Black Sheep Productions. Carlo Aquino and Charlie Dizon was cast to appear in the film. The trailer of the film was released on July 31, 2023. The film was screened at the 19th Cinemalaya Independent Film Festival as the closing film.
Fred Hawson, writing for ABS-CBN News, gave praise for the acting performances of Carlo Aquino and Charlie Dizon, with the former "can still pull off the youthful energy of a guy" despite being in his late thirties. However, he gave criticism for its production design which he deemed as "problematic". Le Baltar, writing for The Philippine Star, also gave praise to the lead stars where Carlo Aquino delivered "an effortless and convincing work, brimming with charm and playfulness that is simply hard to dismiss" and Charlie Dizon's mastering her acting skills in giving her character a "richer inner life" and great use of emotions in which the critic commended. Its written screenplay, Baltazar's direction, Marya Ignacio's editing, and Kara Moreno's cinematography were also praised.
In contrast, Stephanie Mayo, writing for Daily Tribune, rated the film 1.5 out of 5 stars and gave a negative review, saying that it failed "the audience for suggesting something deeper and with more substance, and failing to deliver" and was called as a "cheap romantic comedy film" that is targeted for children and felt it was staged.
Denez Abernot

Denez Abernot, ganet en arvor Bro-Leon (Bro-Bagan) e 1955, zo ur c'haner ha saver kanaouennoù brezhonek. Kanañ a rae gant Storlok e penn diwezhañ ar bloavezhioù 1970, hiziv eo livour (ha barzh) en Arvor Bro-Leon.
A bep seurt traoù en deus bet graet : pesketaer, koñversant, skolaer (skolaer kentañ Diwan e 1977), c’hoarier pezh (gant Strollad ar Vro Bagan) ha kabiten war listri an Departamant eus Konk-Leon da Eusa. Kaner eo ivez, ha saver tonioù ha sonioù, doare rock, blues pe folk. E don brudetañ a zo, hep mar ebet, Gwerz ar vezhinaerien.
Kanet en deus bet gant ar strollad Storlok, hag ur bladenn solo, Tri miz noz, a oa deuet er-maez gantañ e 1998 gant Jacques Le Guellec.
Plouneour-Traezh

Plouneour-Traezh a oa ur gumun eus Bro-Leon e kanton Lesneven, e departamant Penn-ar-Bed, e gwalarn Breizh. Emañ Plouneour-Traezh e Bro-Bagan.
Kendeuzet e oa bet gant Brignogan d'ar 1añ a viz Genver 2017 d'ober ur gumun nevez : Plouneour-Traezh-Brignogan.
Niver a annezidi
Ma c'helljen-me kanañ laouen

Ma c'helljen-me kanañ laouen a zo ur pezh-c'hoari savet ha c'hoariet gant Strollad ar Vro Bagan, ur strollad c'hoariva renet gant Goulc'han Kervella.
C'hoariet e oa bet meur a wezh er bloavezhioù 1970 ha berzh bras en doa graet neuze. Adc'hoariet eo bet e 2006.
Boued

Pep danvezenn a ya da vagañ ar vevien eo ar boued. Pa vez maget ur bev e tremen elfennoù en e gorf ken e vez pourchaset dezhañ an energiezh a laka anezhañ da chom bev. Tapet e vez ar boued e meur a doare, eus ar bev bihanañ, plantenn pe loen, betek ar valum divent. Pa vez debret ar vevien gant ar re a zo brasoc'h egeto hag un eiltro, eus ar plankton betek ar breizherien vras evel ar morviled, ar felidae vras, an olifanted hag un nebeud all ez eus ul lezenn hollek, chadenn ar bouetañ a reer eus outi. P'en deus ijinet meur a ostilh evit lazhañ al loened eus peseurt ment e ve emañ an Den e live uhelañ chadenn ar boued.
Gerioù diwar an anv boued
Kig

Kig vez graet eus forzh peseurt tamm loen ennañ danvez kigenn dreist holl met ivez druzoni, stirennoù, gwad. Ar bouzelloù hag ar flugez all a c'hell bezañ renket e-touez ar c'hig, daoust dezho bezañ stummet gant nebeut-tre pe tamm kigenn ebet.
Dont a ra ar c'hig eus ar sevel loened pe eus ar chaseal.
Savet e vez al loened a-ratozh evit o c'hig (chatal pe loened bihan) pe e c'hell ar c'hig bezañ ur produ ouzhpenn pa vez savet al loened evit un abeg all (laezh, vioù, gloan hag all). Pa vez er mod-se, al loened re gozh a vez treuzfurmet e kig memestra.
Graet e vez jiboez eus al loened chaseet evit o c'hig.
E broioù zo hag e relijionoù zo e c'hell tammoù kig, pe seurtoù kig, pe ar c'hig da vat bezañ difennet dre abegoù disheñvel.
Diwar ar ger henvrezhonek cic, kic 1339, da geñveriañ gant ar gerioù cig e kembraeg, kyk e kerneveureg, cíoch en iwerzhoneg, cico- e galianeg.
Ar ger kig a vez implijet ivez e brezhoneg evit kalz traoù liammet, kigaj, kigder, kigenn, kiger, digigañ, tric'hig hag all.
Boued a galite eo ar c'hig dre ar proteinioù a zo ennañ (Etre 20 ha 30% hervez ar seurt kig). Kavet e vez er c'hig trenkennoù amine pennañ ne c'hell ket bezañ stummet gant ar c'horf. Mineralioù a vez kavet ivez, dreist holl houarn er c'hig ruz. Vitaminoù a zo ivez dreist holl vitaminoù B. Druzoni a zo c'hoazh mui pe vui hervez an tamm kig hag ar seurt loen (tro dro 10,7 g / 100 g a geidenn).
An elfennoù boued a c'hell bezañ disheñvel-tre hervez spesad hag oad al loen, ar pezh en deus debret ha peseurt tamm kig eo.
Renket e vez alies ar seurtoù kig hervez o liv
Renket e vez ivez ar seurtoù boued hervez o orin
Posupl eo ivez renkañ ar seurtoù kig hervez ma eo bet treuzfurmet pe get
Kastell

En orin eo ur c'hastell (liester: kestell pe kistilli pe kastelloù) ur savadur e kerz un aotrou evit gwareziñ e c'halloud war e c'hladdalc'h ha chom en e c'houdor e-pad ar Grennamzer. Diwar al latin castellum eo bet deveret ar ger. Ur castellum (castrum bihan) a oa kreñvlec'h bihan al luoz roman. Meur a gastell roman e mein a zo bet adimplijet hag adsavet er Grennamzer (da skouer: kastell Brest), met muioc'h a zo bet freuzet evit sevel tiez.
Savet eo bet kestell kentañ ar Grennamzer e prenn, war ur savenn douar peurliesañ, da lavaret eo ur voudenn gastell pe voudenn gladdalc'h. Goude-se, war-dro an X kantved, e vezent savet e mein ha kastell-kreñv a reer anezho.
E-pad an Azginivelezh e klaskas ar roueed c'hall sevel pe gempenn o c'hestell-kreñv aozet evit an difenn evit ma teufent da vezañ ul lec'h plijus ha koñfortus. Evel-se e savjont kestell eus ar vravañ war riblennoù al Liger.
Hêr ar genkiz roman eo ar c'hastell europat, un atant lakaet da greñvlec'h gant mogerioù evit e wareziñ.
Kastell-Geron

Kastell-Geron a zo ur gumun eus Breizh e departamant Il-ha-Gwilen. Pennlec'h Kanton Kastell-Geron eo.
War lez ar stêr Yegn emañ Kastell-Geron.
Kastell-Jiron e brezhoneg e Geriadur brezhoneg-galleg Roparz Hemon e 1978, 1993.
Kastell Pondi

Kastell Pondivi, anvet ivez Kastell ar Roc'haned a voe savet e Pondivi er XV hag er XVI kantved gant tiegezh Roc'han.
Ur c’hastell kentañ a voe savet e Pondivi en IX kantved, war a seblant, gant noblañsoù tiegezh Porc'hoed. Gant Alan II Roc'han e voe savet war ribl ar Blavezh ur c’hastell anvet ar Sal, e 1128. Distrujet e voe ar c’hastell-se e miz Du 1342 gant soudarded saoz ar roue Edouarzh III e-pad Brezel hêrezh dugelezh Breizh. Gant mein ar rivinoù e voe savet ur gouent e-kichen. Goude ar Brezel hêrezh e teuas Pondi da vezañ kêr-benn douaroù beskonted Roc'han. Lakaet e voe sevel ur c’hastell nevez gant ar beskont Yann II Roc'han, mab-kaer d’an dug Frañsez II hag enebet outañ, pa oa savet a-du gant roue Bro-C'hall, Charlez VIII. Kroget e voe al labourioù e 1479 hag echuet e voent e 1488. En amzer-se en em astenne kêr Bondi etre ar c’hastell er biz hag an iliz-parrez er mervent.
Protestanted e teuas da vezañ aotrouien tiegezh Roc'han hag er XV kantved e voe Pondivi unan eus kreñvlec’hioù ar Brotestanted e Breizh. E-pad ar Brezelioù a Relijion e voe lakaet seziz war ar c’hastell gant soudarded Dug Mercœur, harpet gant soudarded spagnol. E 1603 e voe graet un dugelezh eus beskontelezh ar Roc’haned gant ar roue Herri IV, hag en em ziazezañ a reas Herri II Roc'han e kastell Pondivi. En XVIII kantved e voe atredet ar fozioù. E 1621 ne oa mui nemet tri zour hag e 1781 e oa un eil tour o kinnig kouezhañ en e boull. E-kerzh an Dispac'h Gall e voe lakaet ar c’hastell da vezañ ul lez-varn.
E 1940 e voe savet, e kastell Pondi, gant pennoù Strollad Broadel Breizh, Frañsez Debauvais, Olier Mordrel, Marcel Guyesse ha Célestin Lainé, Kuzul Broadel Breizh, un doare gouarnamant da c’hortoz evit ur Vreizh dizalc’h. Un 200 den bennak a gemeras perzh er vodadeg-se. Dilennet e voe Debauvais e penn Kuzul Broadel Breizh. Embannet e voe un disklêriadur awenet gant mennozhioù faskour ar gelaouenn Stur, renet gant Mordrel, Disklêriadur Pondi a ginnige sevel e Breizh ur renad kar da hini Franco e Spagn.
Emañ ar c’hastell war un dorgennig, dreist ar Blavezh, en hanternoz d’ar gêr gozh. Stumm ur c’harrez zo gantañ gant tourioù er c’hornioù ha fozioù en-dro d’ar mogerioù-kreñv. Savet e voe er bloavezhioù 1480, en un amzer ma voe kroget da ober gant kanolioù da lakaat seziz war ar c’hestell. Hiziv ez eus c’hoazh daou dour bras gant balegoù-tarzhelloù. Un hent-tro toet brav zo war ar mogerioù. Mont a reer e-barzh ar c’hastell dre ur pont diloc’h ha n’eo ket dre ur pont-gwint.
Lakaet e oa bet kastell Pondivi da vonumant istorel e 1953. Kempennet-mat e oa bet etre 1955 ha 1972. Perc’hennet eo bremañ gant 14vet dug Roc’han, Josselin de Rohan, ha feurmet e vez da gêr Bondivi. Gweladenniñ ul lodenn vat anezhañ a c’haller.
Kastell-Paol

Kastell-Paol a zo ur gumun eus Bro-Leon, e departamant Penn-ar-Bed, e gwalarn Breizh. Pennlec'h kanton Kastell-Paol eo.
Martolod e oa. Mervel a reas e-pad an Eil Brezel Bed, d'an 29 a viz Du 1940.
Niver a annezidi
Divodet eo bet ar gevelliñ gant Penarth e Kembre.
Furongian

Ar Furongian (hag a glot ouzh ar mareadoù kozh Kambrian diwezhat, Merioneth, Croixian, pe Potsdamian) a zo marevezh douarouriel diwezhañ ar c'hambrian. En em astenn a ra eus 501 ± 2 milion bloavezh'zo ha 488.3 ± 1.7 milion bloavezh'zo. Kinnig a rejod d'e zisrannañ e tri ismaread. Unan anezho, hepken, en-deus degemeret un anv ofisie, ar paiaban, tra m'eo anvet unan arall dolgellian en un douare nann-ofisiel.
Merket eo ar furongian gant donedigezh war-well an tribolitoù agnostid kentañ. E-pad ar maread-se e kemmas natur ar goueledoù. Tra ma oa fetis ha kaled e deroù ar c'hambrian, e lakaas oberiantiz ar breñved da galz lec'hidus. En abeg d'an dra-se ez eas da get organegoù evel an helioplacoided o-doa ezhomm eus ur goueled kaled.
An anevaled aet ar-wel e-pad ar c'hambrian abred hag ar c'hambrian krenn a gendalc'he da vezañ fonnus. Arvestiñ a reer ouzh donedigezh doareoù nevez evel ar graptolitoù hag ar c'honodonted gentañ. Ar re-mañ, ar Chordataed gentañ o-deus korfoù gwak hag hir, heñvel ouzh hini siliennoù a-vremañ. Kigrdbrerien vihan e oant, war a seblant. Betek penn an Triaseg e treuzvevjont.
Ar furongian war Palaeos.com
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Blasicrura interrupta

Blasicrura interrupta a zo unan eus an tri spesad a vez renket er genad Blasicrura e kerentiad an hoc'higed-mor hervez Word Register of Marine species WoRMS. Ur spesad kregin boutin a vev e reter Meurvor Indez hag e kornôg ar Meurvor Habask eus Sri Lanka d'ar Filipinez war ar resif kaled, e frailhoù reier, en dour fankek etre nebeut metroù betek 35 m donder an hini eo.
Diskrivet eo bet ar spesad gant Gray e 1824 dindan an anv genad Cypraea.
Heñvelsterioù a zo hervez an diskriverien evit ar spesad-se daoust d'an anv Blasicrura interrupta bezañ implijet un tamm muioc'h eget ar re all:
Kregin brav ha boutin a vev war ar resif kaled, e frailhoù reier, en dour fankek etre nebeut metroù betek 35 m donder an hini eo.
Mentoù boutin ar c'hregin etre-se a zo etre 19 mm ha 25 mm hirder, met e c'hell bezañ kavet hiniennoù korrig betek 14 mm pe ramz, betek 29 mm.
Blasicrura pallidula, Talostolida teres daou spesad gant livioù damheñvel.
Lec'h bevañ ar spesad a zo e reter Meurvor Indez hag e kornôg ar Meurvor Habask eus Sri Lanka d'ar Filipinez.
Basque mythology

The mythology of the ancient Basques largely did not survive the arrival of Christianity in the Basque Country between the 4th and 12th century AD. Most of what is known about elements of this original belief system is based on the analysis of legends, the study of place names and scant historical references to pagan rituals practised by the Basques.
One main figure of this belief system was the female deity Mari. According to legends collected in the area of Ataun, the other main figure was her consort Sugaar. However, due to the scarcity of the material, it is difficult to say if this would have been the "central pair" of the Basque pantheon. Based on the attributes ascribed to these mythological creatures, this would be considered a chthonic religion as all its characters dwell on earth or below it, with the sky seen mostly as an empty corridor through which the divinities pass.
The main sources for information about non-Christian Basque beliefs are:
Urtzi may have been a Basque mythological figure—a sky god—but may have been merely a word for the sky. There is evidence that can be read as either supporting or contradicting the existence of such a deity. To date, neither theory has been entirely accepted.
The Iberian Peninsula's Indo-European speaking cultures like the Lusitanians and Celtiberians seem to display a significant Basque influence on their mythologies. This includes the concept of the Enchanted Mouras, which may be based on the Mairu, and the god Endovelicus, whose name may come from proto-Basque words.
After Christianization, the Basques kept producing and importing myths.
Oberon (Seyler)

Oberon, or The Elf King (German: Oberon oder König der Elfen), or simply Oberon, originally known as Huon and Amanda (German: Hüon und Amande), is a romantic Singspiel in five acts by Friederike Sophie Seyler, inspired by the poem Oberon by Christoph Martin Wieland, which itself was based on the epic romance Huon of Bordeaux, a French medieval tale. It has been named for two of its central characters, the knight Huon and the fairy king Oberon, respectively. Musicologist Thomas Bauman describes the work as "an important impulse for the creation of a generation of popular spectacles trading in magic and the exotic. Die Zauberflöte [The Magic Flute] in particular shares many features with Oberon, musical as well as textual."
The opera was published in "Flensburg, Schleswig and Leipzig" in 1789, the year Seyler died. Seyler was married to the prominent theatre director Abel Seyler, the founder of the Seyler Theatre Company and a noted promoter of both German opera and William Shakespeare. The opera was dedicated to their common long-time friend and collaborator, the actor Friedrich Ludwig Schröder. Seyler's opera and a plagiarized version by Karl Ludwig Giesecke both enjoyed popularity from the late 18th century. The opera had a central role in the development of Emanuel Schikaneder's theatre and its focus on fairy tale operas which culminated in The Magic Flute, and was one of the influences that the latter's libretto built upon.
Seyler's libretto formed the basis of Karl Ludwig Giesecke's libretto for the opera Oberon, written for Emanuel Schikaneder's troupe and set to music by Paul Wranitzky. The play was also performed by the Weimar court theater under the direction of Goethe. As Giesecke did not credit her, he later came under much criticism for plagiarism, although it soon became evident that his work was based on Seyler's libretto. The opera The Magic Flute, with a libretto by Schikaneder, was to a significant degree based on Giesecke's version of Oberon and thus ultimately on Seyler.
According to Peter Branscombe, "it has long been recognized that Giesecke, the named author of Wranitzky's libretto, deserves little credit for what is largely a plagiarism," concluding that "Giesecke's "Oberon, König der Elfen is hardly more than a mild revision of Seyler's book." After the theatrical success of Giesecke's plagiarized version (and also after Seyler's death), Seyler's original was renamed Oberon and performed under this title. Giesecke's version of Seyler's Oberon was the first opera performed by Schikaneder's troupe at their new theater, and established a tradition within the company of fairy tale operas that was to culminate in The Magic Flute two years later.
Salar de Coipasa

El salar de Coipasa es un salar ubicado en el altiplano andino, dentro de una cuenca endorreica que abarca el oeste de Bolivia (≈98 %) y el noreste de Chile (≈2 %). En el lado boliviano, pertenece al Departamento de Oruro, mientras que en Chile se sitúa en la comuna de Colchane, Región de Tarapacá.​
El Salar se encuentra en la parte centro-occidental del altiplano andino, a 225 km al oeste de Oruro, siguiendo la ruta hacia Sabaya. Rodea enteramente al lago Coipasa y se extiende a una altitud de 3657 m s. n. m. Su superficie es de 2218 km², con dimensiones aproximadas de 70 km de largo por 50 km de acho,​ lo que lo convierte en el quinto mayor salar más grande del mundo y el segundo salar más extenso de Bolivia, después del salar de Uyuni.
El salar presenta un espesor máximo de 100 metros, compuesto por capas superpuestas de uno a dos metros de grosor. Su entorno está dominado por formaciones volcánicas, aunque en su sector occidental se encuentran afloramientos esporádicos de rocas sedimentarias.
El Salar de Coipasa está conectado al Salar de Uyuni a través de la Quebrada Negrojahuira, de alrededor de 20 km de longitud.​Su caudal proviene principalmente de los ríos Laca Jahuira y Lauca, los cuales desembocan en su superficie, contribuyendo a su dinámica hidrológica.
Salar de Tara

El Salar de Tara es un salar situado a unos 150 km al este de la localidad de San Pedro de Atacama, Provincia de El Loa, en la Región de Antofagasta, Chile, no lejos de la frontera con Argentina. El salar tiene como principal afluente al río Zapaleri que viene del norte y convierte a la cuenca del salar en una de las dos cuencas altiplánicas que tienen superficie compartida por tres países.​
El salar se encuentra sobre la caldera del volcán Vilama a una altitud de 4300 sobre el nivel del mar y forma parte de la Reserva Nacional Los Flamencos. Para acceder al salar es necesario un vehículo todoterreno.​
Las características morfométricas y climatológicas más relevantes del salar son:​
Luis Risopatrón describe su laguna en su Diccionario Jeográfico de Chile de 1924:​
El salar tiene un rico biosistema de fauna, entre los que destacan flamencos, vicuñas, chululos, zorros culpeo, cuy de la puna, caitíes, chorlos de la puna, patos jergón, gaviotas andinas o gansos guallata, entre otros. Igualmente goza de una rica flora en la que destacan bofedales, coirón, paja amarilla, tola de agua y tola amaia.​
Al acceder al Salar desde la carretera 27 se pueden apreciar los Monjes de la Pacana, gigantescas formaciones rocosas verticales repartidas por el paisaje erosionadas por el viento. El propio salar de Tara está franqueado por las Catedrales de Tara, una formación masiva de roca.​
Salar de Chalviri

El salar de Chalviri es un salar boliviano ubicado en la Reserva Nacional de Fauna Andina Eduardo Abaroa, al sur del departamento de Potosí, situado a 4369 m s.n.m.​
En el extremo oeste del salar se encuentran las termas de Polques, que son aguas termales con un alto contenido de minerales.​
La localidad más cercana es Agua Brava.
Laguna Salada (Salar de Atacama)

La laguna Salada es un cuerpo de agua superficial ubicado en la cuenca del salar de Atacama, en la comuna de San Pedro de Atacama, Provincia de El Loa, norte de Chile.
La laguna, con un espejo de agua de cerca de 0,18 km², esta conectada con la laguna Interna.​
Salar de Pedernales

El salar de Pedernales es un salar ubicado en la comuna de Diego de Almagro, cercano al límite internacional de la Región de Atacama, al este de la cordillera Claudio Gay
Es la cuenca endorreica más extensa de la III Región, con las consecuentes variaciones morfológicas, climatológicas y geológicas. El salar es una costra de yeso y halita con pocas y pequeñas lagunas generalmente pegadas a las orillas del salar. Las lagunas al nor-este son profundos “ojos” en la costra de sal. Las demás son superficiales.
Sus características morfométricas y climatológicas más relevantes son:​
Se trata de un enorme depósito de agua salobre cubierta mayormente una costra de sal que en la parte oeste y también en otros sectores permite el afloramiento del agua. La hoya hidrográfica comprende un área de 4900 km² ubicada entre los 3450 m hasta más de 5000 m de altitud y su base de equilibrio es el salar mismo, es decir, donde se concentran las sales, que tiene un área de 300 km².​ Se supone que su alimentación proviene de los dos río principales de la cuenca, el río La Ola y el río Juncalito, ambos provenientes del sur.​
Sus afluentes son el río La Ola (cuenca de 960 km²), el río Juncalito (1022 km²), el río Leoncito (244 km²) y el río Negro (Juncalito) o Salado (Juncalito) de 679 km², además de las precipitaciones directas.​
El salar no tiene efluentes naturales, es una cuenca endorreica. Sin embargo, el caudal de sus afluentes es desviado mediante cañerías para ser utilizado en la mineras Potrerillos y El Salvador. En la zona de Agua Helada existe desde 1923 un canal que comunica el río Salado (Chañaral) con la cuenca del salar de Pedernales.​​
Para satisfacer las necesidad de agua tanto humanas como industriales en la cuenca del río Salado de Chañaral, se han debido construir varias obras civiles que acumulan, transportan y tratan las aguas de la cuenca como también algunas adyacentes.
Luis Risopatrón lo describe en su Diccionario Jeográfico de Chile de 1924:
También señala la existencia de:
Salar de Carcote

El Salar de Carcote, también conocido como Salar de San Martín, es un salar situado en la Región de Antofagasta.
El salar se encuentra al suroeste de Ollagüe y tiene una superficie de aprox. 108 km² y está a una altitud de 3.690 m.​ El paisaje del área está dominado por el volcán Ollagüe al este y Aucanquilcha al norte. El ítem 020 del inventario de cuencas de Chile en que está incluida la cuenca hidrográfica del salar, limita con la cuenca del río Loa al oeste y la cuenca del salar de Ascotán al sur,​ e incluye también a los salares de Ollagüe y Ascotán.
El salar de Carcote era en su día un lago del que quedan pequeñas lagunas repartidas por el salar. Están concentradas principalmente a lo largo de su orilla occidental y comprenden una superficie de entre 3 y 4 km² aproximadamente. El principal de ellos es la laguna Verde.​
Sus principales características morfométricas y climatológicas son:​
Salar de Agua Amarga

El salar de Agua Amarga es un salar ubicado en la cordillera Andina de la Región de Atacama, al sur de los salares de Punta Negra y Pajonales.
Es una costra de yeso y de halita con "ojos" al norte y pequeñas lagunas superficiales mal definidas en las orillas este y sur. En los mapas topográficos IGM aparece una gran laguna que no existe en el terreno, sino que es una costra de yeso rugosa coloreada en marrón por partículas terrosas. El mapa geológico no presenta este error.
Las características morfométricas y climatológicas más relevantes del salar son:​
Luis Risopatrón lo describe en su s: de 1924:​
Olimpíada de Geografía de la República Argentina

La Olimpíada de Geografía de la República Argentina es un certamen que se realiza anualmente; por primera ocasión se llevó a cabo durante el año 2005. Es subsidiado por el Ministerio de Educación de la Nación (en un 70%) y organizado y financiado por la Universidad Nacional del Litoral (en un 30%) a través de la Facultad de Humanidades y Ciencias. La competencia está dirigida a jóvenes estudiantes de nivel de enseñanza media.
En el año 2014, décimo Aniversario de la Olimpíada de Geografía de la República Argentina y respondiendo a la tercera invitación de la International Geography Union (IGU/UGI) Olimpyad Task Force, se ha participado de la iGeo (Olimpiada Internacional de Geografía) realizada en Cracovia (Polonia), en calidad de Observer. Desde el año 2015 Argentina envía a su Delegación de estudiantes para participar en esta instancia internacional.
La misma se divide en tres categorías.
En el caso de las categorías A y B existen 3 instancias en las que se puede competir de manera escrita:
En la categoría C también son tres instancias:
Desde el año 2015, son seleccionados todos los años cuatro (4) estudiantes para representar al país en la iGeo (Olimpiada Internacional de Geografía), que se realiza en diferentes sedes alrededor del Mundo. Los estudiantes que formarán el equipo nacional son preseleccionados según el Orden de Mérito en la Instancia Nacional, finalmente el equipo queda conformado según un proceso evaluativo que contempla no solo conocimientos de Geografía sino también un buen manejo del idioma inglés (idioma en que se desarrolla la competencia).
Se tiene en cuenta los puntajes obtenidos por los alumnos que alcanzaron el 1º, 2º y 3º lugar.
Categoría "A": Primeros años del nivel secundario
Categoría "B": Últimos años del nivel secundario
Olimpíada Geográfica Argentina
Olimpiada Mexicana de Geografía
Lago salado

Un lago salado o lago salino es un cuerpo aislado de agua que posee una concentración de sales (principalmente cloruro sódico) y otros minerales significativamente mayor que otros lagos (la condición de lago salino suele establecerse en 25 gramos de sal por litro). En algunos casos, los lagos salados pueden llegar a tener una concentración de sal superior al agua de mar.
Los lagos salados se forman cuando las aguas que fluyen hacia el lago, que contienen sales u otros minerales, no pueden abandonarlo debido a que el lago es una cuenca endorreica terminal. Al evaporarse, el agua deja detrás cualquier sal que hubiera permanecido disuelta, aumentando así su salinidad, razón por la que los lagos salados son lugares idóneos para la producción de sal. La alta salinidad condiciona asimismo la flora y la fauna del lago en cuestión; de hecho, en ocasiones el resultado puede llegar a ser la ausencia casi total o total de vida en dicho lago.
Si el aporte de agua que fluye hacia el lago es menor que la cantidad de agua evaporada, el lago puede llegar a desaparecer y dejar un llanura salada o salar, también llamada playa.
El hecho de que sus aguas sean salinas ha hecho que se les llame popularmente mares de una manera algo errada.
Por tamaño, los tres mayores lagos salados en el mundo son el mar Caspio, el mar de Aral y el lago Baljash. El mayor lago salado de los hemisferios sur y occidental es el mar Chiquita, el cuarto en tamaño del mundo tras los tres anteriores.
El lago salado con mayor altitud es el lago Meiriqie, a una altitud de 5354 m s. n. m. y una superficie de 64 km² (el lago Namtso, habitualmente citado, es solo el más alto de los que superan los 500 km²), mientras que el lago de menor altitud es el mar Muerto, que es asimismo el punto más bajo de todas las tierras emergidas.
Desde el siglo VIII, la sal del lago Baskunchak de Rusia fue explotada y distribuida a través de la Ruta de la Seda. En la actualidad, la industria de la sal de este lago (que posee un 99,8 % de pureza de cloruro sódico) supone el 80 % de la producción total de sal de Rusia. Dependiendo de las necesidades, genera entre 1,5 y 5 millones de toneladas de sal cada año.
El Lago Enriquillo en República Dominicana se ubica en la Hoya de Enriquillo que es la mayor depresión del Caribe. Este lago de origen tectónico fue un antiguo canal marino que iba desde la bahía de Puerto Príncipe en Haití hasta la bahía de Neiba formando la actual cuenca endorreica drenando todas las escorrentías de la zona a este lago o al Lago Azuey. Este lago salado es el más grande del Caribe insular.
Volcán Antofagasta

Antofagasta es un volcán de unos 3.495 m s. n. m. de forma de cono de ceniza, se ubica a unos 8 km al sur de la localidad de Antofagasta de la Sierra, en la Provincia de Catamarca, Argentina.
Es una chimenea a 3.495 m s. n. m. con depósitos de basalto negro. Está localizado al este del Salar de Antofalla y al oeste de la caldera del Volcán Galán.
Su formación corresponde al Holoceno, la última y actual época geológica del período Cuaternario, por lo cual forma parte de las fumarolas más jóvenes de la región de la puna argentina.
En su base se encuentra el Pucará de la Alumbrera, antigua ciudadela incaica.
Complejo Sedimentario Volcánico Cortaderas Chicas

El Complejo Sedimentario Volcánico Cortaderas Chicas (CSVCC) representa una de las formaciones características del Paleozoico de la Puna Austral. Está formado por secuencias siliciclásticas y volcaniclásticas depositadas durante el Floiense, que afloran como un faja alongada en sentido NE-SO, entre el Salar de Ancahuás y el Salar de los Ratones, en la provincia de Catamarca, Argentina.
Las unidades volcaniclasticas están asociadas con flujos de lavas sin-sedimentarias de la composición riolítica y andesítica. Las unidades siliciclásticas corresponden a secuencias de plataforma marina profunda, evidenciado por las facies de turbiditas e intercalaciones de arenas y pelitas. Básicamente se trata de cuarcitas, pelitas, tobas y grauvacas. El conjunto registra metamorfismo de facies esquistos verdes.
Como se trata de una faja plegada y corrida con deformación intensa, existen superposiciones y repeticiones tectónicas que impiden determinar las relaciones estratigráficas originales. Sobre el CSVCC se apoyan las sedimentitas del Grupo Paganzo, y volcanitas y sedimentitas cenozoicas. En la parte sur está en contacto tectónico con el basamento metamórfico de la Formación Famabalasto y hacia el este se reconoce un contacto transicional con los depósitos ordovícicos de la Formación Falda Ciénega. La base del complejo aún no fue reconocida.
La unidad en general presenta escaso registro fosilífero. Se encontraron brachiopodos y graptolites, pero solo Phyllograptus sp. fue posible de identificar e indica una edad Floiense hasta Dapingiense Inferior.
Marquesado del Salar

El marquesado del Salar es un título nobiliario español creado por el rey Carlos II en favor de Juan Fernando Pérez del Pulgar y Rico de Rueda, VII señor y alcalde del Salar y su castillo, alférez mayor y regidor perpetuo del Salar de Loja, el 27 de febrero de 1693.​​ Le fue otorgada la Grandeza de España el 19 de septiembre de 1834 por Isabel II.
Su nombre hace referencia al municipio de Salar, en la provincia de Granada.
Salinella

Salinella salve is a dubious species of a very simple animal which some have named as the sole member of the phylum Monoblastozoa. It was discovered in 1892 by Johannes Frenzel in the salt pans of Córdoba Province, Argentina and cultivated in a laboratory by him. This animal has not been found since and its real existence is considered as doubtful. A project involving Michael Schrödl from the Zoological State Collection in Munich searched for Salinella in salt lakes across Argentina and Chile, but failed to find any specimens.
Salinella was discovered in soil samples from salt pans around Río Cuarto, Córdoba Province, Argentina, although the exact type locality was never specified.
According to Frenzel's description, S. salve is more organized than Protozoa, but still very primitive for a multicellular organism. They are characterised by their distinct anterior/posterior parts and being densely ciliated, especially around the "mouth" and "anus". They have only one layer of cells, and reproduce asexually by transverse fission of their bodies. Although sexual reproduction was suspected, Frenzel did not observe it.
Salt crust

A salt crust is a method of cooking by completely covering an ingredient such as fish, chicken or vegetables in salt (sometimes bound together by water or egg white) before baking. The salt layer acts as insulation and helps cook the food in an even and gentle manner. After baking, the salt crust is cracked and discarded, revealing the moist and evenly cooked food.
Typically delicate foods such as fish, chicken/poultry or vegetables are cooked using this method. In each case the aim is to lock in moisture, protect the food from drying, ensure even cooking, and maximise the flavour.
The salt crust can be created simply by adding a sufficient quantity of coarse or fine salt to cover the food item. Water may be sprayed on top, to help the salt form a hard crust. Alternatively, the salt may be mixed with egg white to form a pliable paste.
Baking typically occurs in an oven at around 200 °C (390 °F), with the salt crust acting as a cooking vessel. This slows heat transfer to the food creating a slow and low dry oven, beneficial to most proteins.
To serve, the crust is broken and carefully removed, to avoid leaving excess salt residues in the food.
Steak can also be cooked using a similar method rather than broiling it and risk the loss of its juices. Coating a pan with salt and cooking the steak, ideally approximately an inch thick or less, on top yields a more moist and flavourful cut. The pan is heated until the salt crackles and steaks cooked with this method usually involves a crispy crust made of the salt. This is a key difference to other salt crusts as usually it is discarded but in this case it is used to add texture and flavour to the steak.
The earliest recipe found for salt-baked is from the fourth century BCE in Archestratus' Life of Luxury. The recipe details for a whole, round white fish such as sea bass, snapper or sea bream that was cleaned and then gutted. The fish is seasoned with thyme being inserted into the cavity of the fish prior to the salt crust encapsulating it in two pounds of salt glued together with water and egg whites.
In a Muslim cookbook originating from the thirteenth century, a layer of salt is placed on a new terracotta tile as a base and the fish is placed on top and another layer of salt is added on, then finally being placed in an oven.
The first recorded reference in China resembling the technique of baking in a salt crust is salt-baked chicken from Dong Jing in the province of Guangdong during the Qing Dynasty (1644–1911). The chicken was cooked and preserved in the salt fields of the area giving them added flavour. A more recent traditionally recipe is building a cocoon of salt around the chicken protecting it from direct heat ensuring even cooking and the possibility of drying out the meat. The chicken is wrapped in a tight parcel concentrating all the natural flavours of the chicken resulting in a succulent and tender product. This can be seen as the combination of the salt crust method with the French en papillote style.
List of lakes by volume

This article lists lakes with a water volume of more than 100 km, ranked by volume. The volume of a lake is a difficult quantity to measure. Generally, the volume must be inferred from bathymetric data by integration. Lake volumes can also change dramatically over time and during the year, especially for salt lakes in arid climates. For these reasons, and because of changing research, information on lake volumes can vary considerably from source to source. The base data for this article are from The Water Encyclopedia (1990). Where volume data from more recent surveys or other authoritative sources have been used, that usage is referenced in the respective entry. The total volume of Earth's lakes is 199,000 km.
The volumes of the lakes below vary little by season. This list does not include reservoirs; if it did, six reservoirs would appear on the list: Lake Kariba at 26th, Bratsk Reservoir, Lake Volta, Lake Nasser, Manicouagan Reservoir, and Lake Guri.
Estuaries and lagoons are not included either. Examples: Lake Melville (estuary) and Lake Maracaibo (lagoon), comparable with Lagoa dos Patos.
In 1960, the Aral Sea was the world's twelfth-largest known lake by volume, at 1,100 km (260 cu mi). However, by 2007 it had shrunk to 10% of its original volume and was divided into three lakes, none of which are large enough to appear on this list.
Chadititan

Chadititan (meaning "titan of the salt") is an extinct genus of titanosaurian dinosaurs from the Late Cretaceous (Campanian) Anacleto Formation of Argentina. The genus contains a single species, C. calvoi, known from several fragmentary skeletons. Chadititan is characterized by its small size compared to related taxa and its particularly gracile limbs.
In 2025, Agnolín et al. reported on a diverse fossil locality in the Marín family Farm near General Roca city and the Salitral Moreno lowlands in Argentina, representing outcrops of the Anacleto Formation. Among the bones discovered were abundant titanosaur remains belonging to several individual animals, including dorsal and caudal vertebrae, a partial pubis and coracoid, and incomplete bones of the fore- and hindlimbs.
In 2025, Agnolín et al. described Chadititan calvoi as a new genus and species of titanosaurs based on these fossil remains. They established MPCN-Pv 1034—comprising nine caudal vertebrae, the top parts of both humeri and ulnae, the bottom part of the right radius, the end of the left pubis, both ends of the right femur, the top part of the left tibia and both ends of the right tibia and fibula, and indeterminate metapodials—as the holotype specimen. They further referred seven additional specimens, including a possible juvenile individual, of varying levels of completeness based on their comparable anatomy and discovery location. The generic name, Chadititan, combines the Mapudungun word chadi, meaning "salt"—in reference to the type locality being near a vast salt flat—with the word "titan", referencing the pre-Olympian gods of Greek mythology. The specific name, calvoi, honors Argentine paleontologist Jorge O. Calvo who coined the taxonomic group Rinconsauria, to which this taxon belongs.
Chadititan is a relatively small sauropod, with an estimated body length of 7 metres (23 ft). Although the known material is fragmentary, Chadititan shows several similarities to other rinconsaurian sauropods. The humerus and femur of Chadititan indicate that its limbs are gracile and relatively straight. Additionally, the anteriorly concave tail vertebrae are relatively long and narrow. No osteoderms were identified from the bonebed.
In their phylogenetic analyses, Agnolín et al. (2025) recovered Chadititan as a member of the Rinconsauria. Their results are displayed in the cladogram below:
Great Salt Lake Desert

The Great Salt Lake Desert (colloquially referred to as the West Desert) is a large dry lake in northern Utah, United States, between the Great Salt Lake and the Nevada border. It is a subregion of the larger Great Basin Desert, and noted for white evaporite Lake Bonneville salt deposits including the Bonneville Salt Flats.
Several small mountain ranges occupy the edges of the desert, such as the Cedar Mountains, Lakeside Mountains, Silver Island Mountains, Hogup Mountains, Grassy Mountains, and Newfoundland Mountains. On the western edge of the desert, just across the border in Nevada, stands Pilot Peak in the Pilot Range.
The desert is cool during the winter and includes unusual plants adapted to the dry conditions. Most of the desert receives less than 8 inches (200 mm) of annual precipitation. The salt crust covering the desert reforms yearly when the rain evaporates. The military's Utah Test and Training Range is in the northern portion of the desert. The lowest part of Juab County is located just south of the Dugway Proving Grounds, about 1.5 miles (2.4 km) northwest of the northwest corner of the Fish Springs Range.
During Jedediah Smith's 1826-27 expedition, Robert Evans nearly died while crossing the desert and in the 1840s, westward emigrants used the Hastings Cutoff through 130 miles (210 km) of Great Salt Lake desert to reduce the distance to California. The 1846 Donner Party's difficulties in making the crossing contributed to their becoming snowbound in the Sierra Nevada. Howard Stansbury explored the desert in 1849. In 1956, I-80 replaced the Wendover Cut-off across the desert, including a straight east-west section for ~50 miles (80 km) between the Cedar Mountains to the east and Wendover on the Utah/Nevada border. Following a railway completed across the desert's Bonneville Salt Flats in 1910, the flats were first used as a speedway in 1914. The world records for highest land speeds are regularly broken here.
In July 2022, archaeologists discovered about 88 footprints had been left behind by humans at least 12,000 years ago using ground-penetrating radar (GPR). In the "ghost tracks", as the archaeologists called them, the footprints absorb moisture and are only visible when it rains and disappear when dry.
The Great Salt Lake Desert experiences a desert climate with hot summers and cold winters. The desert is an excellent example of a cold desert climate. The desert's elevation, 4,250 feet above sea level, makes temperatures cooler than lower elevation deserts, such as the Mojave. Due to the high elevation and aridity, temperatures drop sharply after sunset. Summer nights are comfortably cool. Winter highs are generally above freezing, and winter nights are bitterly cold, with temperatures often dropping below freezing.
Glossary of geography terms (N–Z)

This glossary of geography terms is a list of definitions of terms and concepts used in geography and related fields, including Earth science, oceanography, cartography, and human geography, as well as those describing spatial dimension, topographical features, natural resources, and the collection, analysis, and visualization of geographic data. It is split across two articles:
Related terms may be found in Glossary of geology, Glossary of agriculture, Glossary of environmental science, and Glossary of astronomy.
Much of this material was copied from U.S. government works which are in the public domain because they are not eligible for copyright protection.
석궁

석궁(石弓, 영어: stone bow, bullet-shooting crossbow)은 서양식 쇠뇌의 일종으로, 탄알이나 돌멩이, 화살 등을 사출물로 사용하였으나, 전투용이 아닌 사냥용으로 쓰였다. 쇠뇌의 활몸으로 일반적인 활 대신 탄궁 또는 새총을 사용한 것이라고 생각할 수 있다.
최초의 석궁은 16세기에 발명되었으며, 새사냥용으로 사용되었다.
마하 수

마하 수(Mach number)란 음속에 비하여 속도가 얼마나 되는지를 나타내는 수이다. 오스트리아의 과학자 에른스트 마흐(Ernst Mach)의 이름을 따 명명되었다.
음속은 공기의 밀도 및 온도에 따라 변화하므로 속도가 일정하다고 하더라도 공기역학적인 조건에 따라 마하 수가 변화하게 된다.
마하 수의 크기에 따라 다음과 같이 분류하는데 M<0.8일 때를 아음속영역이라고 하며 특히 M<0.3 조건에서는 공기가 압축되면서 발생하는 공기역학적 효과를 무시해도 좋을정도로 압축성 효과가 약하므로 일반적인 공학적 문제를 비압축성 유동으로 고려시에는 이 영역으로 가정한다.
0.8<M<1의 영역에서는 일반적으로 이 영역의 유동장을 지나가는 물체표면에 부분적으로 충격파가 발생한다. 이러한 특성으로 이 영역은 아음속과 초음속의 특성이 혼재되어 있는 영역으로 천음속영역이라고 한다.
1<M<5의 영역에서는 물체의 앞에서 공기의 압력과 밀도가 급격히 변화하는 지점이 발생하는데 이것을 충격파이라고 부른다. 이때 충격파의 형태에 따라 활모양 충격파(Bow Shockwave)와 경사충격파(Oblique Shockwave)로 나뉜다. 또한 이 영역을 초음속영역이라 한다.
M>5인 영역에서는 충격파뿐만 아니라 유체의 점성에 의한 공력가열현상으로 화학 반응이 일어나기 시작한다. 이 영역을 극초음속영역이라 한다.
비행체가 공기 중에서 비행할 때, 마하 수 1.0을 넘는 경우(즉, 음속보다 빠른 속도로 비행하는 경우)를 초음속 비행이라고 말한다. 음속이 초당 343미터일 경우 마하 1.0은 시속 1,235km다. 이때, 비행체 주위의 공기에는 충격파가 생성되며 이 충격파를 전후하여 공기의 성질이 급격히 변화하기 때문에, 항공공학에서는 마하 수가 중요한 의미를 가진다. 또한 이러한 공기의 성질을 나타내는 중요한 무차원 수로 레이놀즈 수가 있으며 이 또한 항공공학에서 중요한 의미를 갖는다.
합성궁

합성궁(合成弓, composite bow)은 목재와 짐승의 뿔, 힘줄 따위 비목재 재료를 조합하여 만들어낸 활이다. 아시아 유목민족의 몽고궁, 한반도의 각궁이 대표적이다.
영국의 장궁, 일본의 대궁처럼 두 가지 이상의 목재를 접착하여 만든 활은 복합궁이라 하여 합성궁과 구분된다.
세계 양궁 연맹

세계 양궁 연맹(영어: World Archery 월드 아처리, WA)은 양궁 종목을 총괄하는 국제 스포츠 행정 기구이다. 1931년 9월 4일에 설립되었고, 본부는 스위스 로잔에 있다.
세계 양궁 연맹은 1931년 9월 4일 폴란드 르보프(현재의 우크라이나 리비우)에서 '국제 양궁 연맹'(프랑스어: Fédération Internationale de Tir à l'Arc, FITA)이라는 이름으로 창설되었다. 창설 당시에는 미국, 스웨덴, 이탈리아, 체코슬로바키아, 폴란드, 프랑스, 헝가리 등의 국가들이 참여하였다. 조직 설립 목적은 정기적으로 개최되는 국제 대회의 창설과, 1920년 이래로 올림픽 경기 종목에서 제외된 양궁의 올림픽 복귀였다. 이후 양궁은 1972년 하계 올림픽에서부터 정식 종목으로 다시 채택되었다.
국제 양궁 연맹은 1931년부터 세계 양궁 선수권 대회를 개최해왔다. 이 대회는 최초에는 매년 열리다가 1959년부터 2년마다 열리는 것으로 변경되었다. 1959년 연맹은 제1회 세계 필드 선수권 대회도 개최하였다.
2011년 6월에 연맹 설립 80주년을 기념하여 개최된 회의에서 투표를 통해 '국제 양궁 연맹'에서 '세계 양궁 연맹'(WA)으로 이름을 변경했다.
2021년 세계 양궁 선수권 대회

2021년 세계 양궁 선수권 대회(영어: 2021 World Archery Championships)는 2021년 9월 19일부터 9월 26일까지 미국 양크턴에서 열린 제51회 세계 양궁 선수권 대회이다.
김우진 (양궁 선수)

김우진(金優鎭, 1992년 6월 20일~)은 대한민국의 양궁 선수이다. 2016, 2020, 2024 올림픽에 참가하여 단체전에서 금메달을 획득했다. 2024년 하계올림픽에서는 양궁 혼성 단체전에서 임시현과 함께 금메달을 획득하고, 양궁 남자 개인전에서 금메달을 기록하며 대회 3관왕이 되었다.
2016년 72발 랭킹 라운드에서 700점을 기록하며 2019년 미국의 브레이디 엘리슨이 702점을 기록하며 세계 신기록을 경신하기 전까지 세계 신기록을 가지고 있었고 2024년 8월 기준, 올림픽 기록 보유자이다. 2024년 하계 올림픽에서 3관왕을 하며 개인 통산 5개의 올림픽 금메달을 획득하였으며, 이에 따라 대한민국 선수 중 가장 많은 올림픽 금메달을 획득한 선수가 되었다.
충북체육고등학교 재학 중 광저우에서 열리는 2010년 아시안 게임에 참가하였다. 예선전에서 1387점을 기록하며 오진혁 선수의 종전기록인 1386점을 넘어 세계신기록을 기록했다. 임동현, 오진혁 선수와 함께 단체전에 참가하여 금메달을 획득했다. 이후 개인전에서도 금메달을 획득하며 아시안 게임 2관왕을 달성하였다. 대회 후 인터뷰에서 그는 2011년 세계 양궁 선수권 대회와 런던 올림픽에 참가하여 금메달을 따고 싶다고 말했다. 이후 2011년 세계 양궁 선수권 대회에 참가하여 단체전과 개인전 모두 금메달을 획득했고 2011년 대한양궁협회 선정 올해의 양궁 선수에 선정되었다. 그러나 2012년 하계 올림픽 대표팀에는 합류하지 못했다.
2015년 다시 대표팀에 합류하여 세계 선수권 대회에서 개인전 및 단체전 금메달을 획득하였다. 개인전에서 한 선수 2번 우승은 1985년 이후 처음 있는 일이다. 이후 2016년 올림픽에도 대표팀에 합류하며 생애 처음으로 올림픽 대회에 출전하였다. 예선전 랭킹라운드에서 700점을 기록하며 임동현의 기존 기록인 699점을 넘어 세계신기록을 달성하였다. 구본찬, 이승윤과 함께 단체전에서 금메달을 획득하였으나 개인전에서는 32강전에서 인도네시아의 리아우 에가 아가타에게 패배하며 탈락하였다.
도쿄 올림픽에도 대표팀에 발탁되었다. 김제덕, 오진혁과 함께 단체전에서 금메달을 획득하였다. 이후 개인전 16강전에서 9발 모두 10점을 기록하여 8강전에 진출하였지만 8강전에서 중화 타이베이의 탕즈쥔 선수에게 6-4로 패배하며 결승전 진출에는 실패하였다. 도쿄 올림픽부터 양궁 종목에 심박수 중계가 도입되었는데 16강전에서 그의 심박수가 매우 낮게 나와 화제가 되었다.
2024년 하계 올림픽에 국가대표로 참가하였으며, 양궁 남자 단체전에서 김제덕, 이우석과 함께 금메달을 획득, 올림픽 3연패를 기록하였다. 양궁 혼성 단체전에서는 임시현과 함께 금메달을 획득, 양궁 남자 개인전에서 미국의 브레이디 엘리슨에게 승리해 금메달을 획득하며 대회 3관왕이 되었다. 그는 양궁 남자 개인전에서 자신의 5번째 금메달을 획득하며 김수녕, 진종오, 전이경을 넘어 올림픽 금메달을 가장 많이 획득한 대한민국 선수가 되었다.
그의 좌우명은 '계산하지 말자' 이며 2011년 8월 23일 청주야구장에서 시구자로 나와 시구를 했다. 2021년 12월 4일 심민지와 결혼했고 2022년 7월 아들 김주원이 태어났다.
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