Tamazight-NLP/NLLB-Seed_Tamasheq-Latin-Script huggingface dataset:
English: From these contours, a sense of the general terrain can be determined.
Tamasheq: Ghur tigheliyen tin ,ittur n general terrain addobat ad it w aghil
English: In cartography, the contour interval is the elevation difference between adjacent contour lines.
Tamasheq: Daɣ kartografi, awa ilan jir taghelit imos tizzijrit ta tizlayat iyaka tan n taɣelit win sider
English: Two or more contour lines merging indicates a cliff.
Tamasheq: Issin megh tiɣeliyen ajjoten n iyaka olanat id adaɣ
English: Usually contour intervals are consistent throughout a map, but there are exceptions.
Tamasheq: Harkuk taqqan jir taɣelit tila alɣma fal karti mušan ille mušan
English: Whether crossing an equipotential line represents ascending or descending the potential is inferred from the labels on the charges.
Tamasheq: Jir ɣas a okayan fal taɣelit tida id ogdanat megh a issewadan meɣ ifnazan eqqal anachach ɣur label tan wi fal šarj tan
English: Acid precipitation is indicated on maps with isoplats.
Tamasheq: Asirmad n acid precipitation tiwar fal karti tan s isoplat tan
English: Contour lines are also used to display non-geographic information in economics.
Tamasheq: Taɣeliyen n iyaka sakninat har ajjudi isalan n a war n aqqel jografia daɣ ekonomi
English: Such isolines are useful for representing more than two dimensions (or quantities) on two-dimensional graphs.
Tamasheq: šund tagheliyen n iso tin daɣ aqqal nat a olaɣan i asukni n a ojjaran tahiriken sanatat (meɣ tazzayen ) fal graph tan win issin.
English: In interpreting radar images, an isodop is a line of equal Doppler velocity, and an isoecho is a line of equal radar reflectivity.
Tamasheq: Dagh afaham n taliwen tin radar tan, isodrop taqqal taɣelit n Dppler velocity togdahat d isoecho eqqal taɣelit n radar reflectivity togdahat
English: Line color is the choice of any number of pigments that suit the display.
Tamasheq: Dumu n taghelit eqqal nefran n iddikud fuk n tisilmagh ti inhajjanen id asukni
English: Line type refers to whether the basic contour line is solid, dashed, dotted or broken in some other pattern to create the desired effect.
Tamasheq: Išikil iyaka imos as taghelit tan iyaka tassohat, titbaɣtabaɣ megh tarza daɣ desin iyyan i a tijru innugh wan otasan
English: Numerical marking is the manner of denoting the arithmetical values of contour lines.
Tamasheq: Ešwal wan iddikud eqqal immik s itiwajraw arithmetic value wan iyaka wan taɣelit.
English: If the contour lines are not numerically labeled and adjacent lines have the same style (with the same weight, color and type), then the direction of the gradient cannot be determined from the contour lines alone.
Tamasheq: A fal iyaka tan win taɣelit war eššelan tolas iyaka tan win sider olahan ichikil ( olahan tazzayt , dumu d ichikil) dihen asatoɣ wan gradient war addobat ad ej ɣur iyaka tan win taɣelit ɣas
English: A properly labeled contour map helps the reader to quickly interpret the shape of the terrain.
Tamasheq: Taɣelit n karti tijjat ešwal iknan taddobat ad tidhil emaghir net i ad ifhim daɣ armud tulat n terrain
English: Then the coordinates of other places are measured from the nearest control point through surveying.
Tamasheq: Dihen coordonate tan win idagan i yadnen itkadan ɣur titbaqqet n awikkil ta tojjarat ehiz s tan akayad n iddikud
English: This phenomenon is called datum shift.
Tamasheq: Immik šund wen isim net datum shilft
English: More ambitious undertakings such as the Struve Geodetic Arc across Eastern Europe (1816-1855) and the Great Trigonometrical Survey of India (1802-1871) took much longer, but resulted in more accurate estimations of the shape of the Earth ellipsoid.
Tamasheq: Alxidmaten ti iknanen uglay šund tann Struve Geodetic Arc daɣ alqiblat tan Eroba ɣur awatay wan (1816 har 1855) d Farak n Tigonometrical maqqoran n India ɣur awatay wan (1802 har 1871) ahoj mušam ewad ittus n mirda tan n dumu wan Ellipsoid wan akal
English: An approximate definition of sea level is the datum WGS 84, an ellipsoid, whereas a more accurate definition is Earth Gravitational Model 2008 (EGM2008), using at least 2,159 spherical harmonics.
Tamasheq: Almaɣna hin ikkan iddikud wan ejarew inta s datum WGS 84, ellipsoid, as ijja awen almaɣna wa oɣadan hullan inta s Earth Gravitational Model 2008 ( EGM2008) isaxdaman 2.159.spherical harmonics
English: When used without qualification, the term latitude refers to geodetic latitude.
Tamasheq: Alwaq wa ti exdam awadim wala musnat net isim wan latitude itawan i geodetic latitude
English: The datum shift between two particular datums can vary from one place to another within one country or region, and can be anything from zero to hundreds of meters (or several kilometers for some remote islands).
Tamasheq: Datum shift jir issin datum tan izlay s edag s iyyan daɣ addawla megh rejion iyyat addobat ad eqqil harat ghur bannan har timad n metir tan ( meɣ metir tan ajjotnen i island tan wi ajjujnen)
English: For example, in Sydney there is a 200 metres (700 feet) difference between GPS coordinates configured in GDA (based on global standard WGS 84) and AGD (used for most local maps), which is an unacceptably large error for some applications, such as surveying or site location for scuba diving.
Tamasheq: Ilmital, daɣ Sidney illan ti 200 n metir (700 n atkul) izlaynen jir isalan win GPS wa ehan GDA ( iknan fal standard WGS 84 wan alɣalim) d AGD ( exaddaman hullan i karti tan tin akal) harat eqqalan tajjarzazzal maqqorat i aplikasyon tan iyyad chund win eket n iddikud meɣ ajarw n edag s alamaɣ daɣ aman
English: Since reference datums can have different radii and different center points, a specific point on Earth can have substantially different coordinates depending on the datum used to make the measurement.
Tamasheq: Alwaq wa id datum tan addoben ad ikrichan radii izlayan d titbaqqa n ammas izlaynen, titbaqqet fal akal taddobat akaraš n coordinate tan izlaynen fal datumm ijjan eket
English: The most common reference Datums in use in North America are NAD27, NAD83, and WGS 84.
Tamasheq: Datum tan oharnen axdamnen daɣ tamasna n Amrik imosan NAD27, NAD83, dWGS 84
English: This datum, designated as NAD 83 ...is based on the adjustment of 250,000 points including 600 satellite Doppler stations which constrain the system to a geocentric origin."
Tamasheq: “Datum wen itawan in i NAD 83...ijja fal aqqad n 250.000 n titbaqqet han 600 n satelit tin stasyon Doppler assibdadnen system ghur geocentric origin”””
English: It is the reference frame used by the U.S. Department of Defense (DoD) and is defined by the National Geospatial-Intelligence Agency (NGA) (formerly the Defense Mapping Agency, then the National Imagery and Mapping Agency).
Tamasheq: Awen eqqal ilan adiriš s Department of Defense wan Amrik (DoD) exdam siris tolas ikfe National Geospatial-intelligence Agency (NGA) almaɣna (a eruwan Defene Mapping Agency dihen National Imagery and Mapping Agency)
English: It was used as the reference frame for broadcast GPS Ephemerides (orbits) beginning January 23, 1987.
Tamasheq: Eqqal a fal ijja anifham i Broadcast GPS Ephemerides ( orbits) issintan ɣur ayor wan tindufan daɣ achal wan 23 n awatay wan 1987.
English: It became the reference frame for broadcast orbits on June 28, 1994.
Tamasheq: Eqqal a fal ijja anifham i Broadcast orbits ɣur ayor wan awzem wan karad n achal wan 28 n awatay 1994.
English: WGS 84 (G873) was adopted as the reference frame for broadcast orbits on January 29, 1997.
Tamasheq: WGS 84 (G873) eqqal a fal ijja anifham i broacast orbits daɣ ayor wan tindufan dag ašal wan 29 n awatay wan 1997
English: WGS 84 is the default standard datum for coordinates stored in recreational and commercial GPS units.
Tamasheq: WGS 84 eqqal Default Standard datum i coordinate tan aghzannen daɣ GPS tan win dallol d mamala
English: For example, the longitudinal difference between a point on the equator in Uganda, on the African Plate, and a point on the equator in Ecuador, on the South American Plate, increases by about 0.0014 arcseconds per year.
Tamasheq: Ilmital, uzlay n tichijrit jir tatbaqqet ghur equator s Uganda daɣ Afrikiya d titbaqqet ɣur equator daɣ achrut n Amrik wan ajala iwwid s 0.0014arcseconds dagh awatay
English: Most mapping, such as within a single country, does not span plates.
Tamasheq: Ijji n Karti tan ajjotnen šund daɣ ammas n addawla iyyat war ilsa plate tan
English: Ptolemy credited him with the full adoption of longitude and latitude, rather than measuring latitude in terms of the length of the midsummer day.
Tamasheq: Ptolemy iflas ti s atkul n tizzijrit hak id tahrike uhun eket n tahrike daɣ tizzijrit n ašrut n achal n awelan
English: Mathematical cartography resumed in Europe following Maximus Planudes' recovery of Ptolemy's text a little before 1300; the text was translated into Latin at Florence by Jacobus Angelus around 1407.
Tamasheq: Kartografi tan matematik tolas amasughal dagh Eroba ghur ajjaraw ijja Maximus Planudes i akatab wan Ptolemy ad orakan i 1300: akatab wen iffisar ti Jacobus Angelus dagh Latin dagh akal wan Florence ghur awatay wan 1407
English: They then choose the most appropriate mapping of the spherical coordinate system onto that ellipsoid, called a terrestrial reference system or geodetic datum.
Tamasheq: Dihen sannafranan ijji n karti wa ofan i sistem n coordiate tan fal ellipsoid s isim net Terrestrial Sistem meɣ Geodetuic datum
English: φ, or phi) of a point on Earth's surface is the angle between the equatorial plane and the straight line that passes through that point and through (or close to) the center of the Earth.
Tamasheq: φ, or phi) n titbaqqet fal arori n akal eqqal harat wa illan jir equatorial plane d taɣelit toghadat ta hi tikkat ɣur titbaqqet ten d tokay (meɣ tahoz in) s ammas n akal
English: All meridians are halves of great ellipses (often called great circles), which converge at the North and South Poles.
Tamasheq: Meridia tan fuk ilan tizunawen n itarmisan maqqornen ( tawaghrinen s tijjililluwa maqqornen) ahalnen siha s pole tan win tamasna d win ajala
English: The antipodal meridian of Greenwich is both 180°W and 180°E. This is not to be conflated with the International Date Line, which diverges from it in several places for political and convenience reasons, including between far eastern Russia and the far western Aleutian Islands.
Tamasheq: Antipodal meridian wan greenwich eqqal 180°W and 180°E dagh edag iyyan. Awen war oher harat n taɣelit ta s itawan International Date Line ta id tifalat s idagan ajjotnen fal iddililan n folitik d n bannan eha jir alqiblat n Russia d Aleutian Islands win ataram
English: Coordinates on a map are usually in terms northing N and easting E offsets relative to a specified origin.
Tamasheq: Coordinate tan fal karti harkuk iktaban isim tamasna wan N d E i alqiblat i asilmad n iɣinni
English: In geography, latitude is a geographic coordinate that specifies the north–south position of a point on the Earth's surface.
Tamasheq: Daɣ jografia , tahrike taqqal coordinate n jografia tisalmadat s edag n tamasna-daɣ ajala n titbaqqet fal arori n akal
English: Latitude is used together with longitude to specify the precise location of features on the surface of the Earth.
Tamasheq: Tahrike inta id tizzijrit alwaq iyyan tajinat atiwaɣir iyyan i asilmad n edag s tiditt n samalan fal arori n akal
English: The second step is to approximate the geoid by a mathematically simpler reference surface.
Tamasheq: Tikkelt tan sanatat inta s itur n ahiz wan Geoid s referens raqqisan n matematik
English: Lines of constant latitude and longitude together constitute a graticule on the reference surface.
Tamasheq: Iyaka tan win tahrike d tišijrit aqqalan fuk nasan graticule fal arori n referens
English: Since there are many different reference ellipsoids, the precise latitude of a feature on the surface is not unique: this is stressed in the ISO standard which states that "without the full specification of the coordinate reference system, coordinates (that is latitude and longitude) are ambiguous at best and meaningless at worst".
Tamasheq: “Alwaq ti illanat ellipsoid tan ajjotnen izlaynen , tahrike tan tiditt n samal fal arori war taqqel iyyat ghas. Awen itiwaɣal dagh ISO Standard allaghat nen as “a fal wadden s amasirsar imdan n system wan coordinate, coordinate tan ( taha tahrike d tišijrit) aqqanan eɣaf hullan tolas war ilen almaɣna””
English: The plane through the centre of the Earth and perpendicular to the rotation axis intersects the surface at a great circle called the Equator.
Tamasheq: Abyon wa ɣur ammas n akal eqqalan a ozɣaɣan i rotation axis azun arori ghur tajjililwayt ta maqqorat s itawan Equator
English: The time variation is discussed more fully in the article on axial tilt.
Tamasheq: Amutti n alwaq ijja fal majrad ajjen dagh artikl fal axial tilt
English: The situation is reversed at the June solstice, when the Sun is overhead at the Tropic of Cancer.
Tamasheq: Talgha timutti ɣur awzem wa darat alwaq wa id tafukt taha edes n Tropic of Cancer
English: Since latitude is defined with respect to an ellipsoid, the position of a given point is different on each ellipsoid: one cannot exactly specify the latitude and longitude of a geographical feature without specifying the ellipsoid used.
Tamasheq: Alwaq wa id tahrike tila almaɣna daɣ semɣar n ellipsoid, edag n titbaqqet iyyan izlay fal ellipsoid fuk: war ti illa i addoben ad izli tahrike d tišijrit n samal n jorgafia daɣ war imel ellipsoid war s exdam
English: Geographic latitude must be used with care.
Tamasheq: Tahrike tan jografia t inhajja id axadam iijan esawey
English: The evaluation of the meridian distance integral is central to many studies in geodesy and map projection.
Tamasheq: Aminšiš n ujjij wan meridian eqqal a ehan ammas n farak tan daɣ geodesy d asukni wan karti
English: There are two methods of proceeding.
Tamasheq: Illanat sanatat tikarsiwen i anuttif net
English: When converting from isometric or conformal to geodetic, two iterations of Newton-Raphson gives double precision accuracy.
Tamasheq: Alwaq wa id tisammaskala Isometric meɣ conformal s geodetic, illan ti issin iteration tan n Newton-Raphson hakkinen isalan oɣadnen
English: The differences shown on the plot are in arc minutes.
Tamasheq: Tamezlayt ta fal terrain tiwar tišangay tan minit tan
English: The transformation between geodetic and Cartesian coordinates may be found in Geographic coordinate conversion.
Tamasheq: Amutti n coordinate tan win geodetic Cartesian addoben ad tiwajriwan daɣ amakal n coordinate tan win jografia
English: In general the true vertical at a point on the surface does not exactly coincide with either the normal to the reference ellipsoid or the normal to the geoid.
Tamasheq: Titbaqqet ta tiknat aqqad fal arori war tijiyit id alwaq wa id ellipsoid talgha net ta tolaghat meɣ geoid net wa olaghan
English: Longitude is a geographic coordinate that specifies the east–west position of a point on the Earth's surface, or the surface of a celestial body.
Tamasheq: Tišijrit tan coordinate tan win jografia isladan alqiblat-dagh-ataram n titbaqet fal arori n akal megh fal arori n atri n išinnawan
English: The prime meridian, which passes near the Royal Observatory, Greenwich, England, is defined as 0° longitude by convention.
Tamasheq: Prime meridian wa itikiyan edes n Royal Observatory, Greenwich, England, itawaghir s 0° dagh tišijrit s anifham
English: Local time (for example from the position of the sun) varies with longitude, a difference of 15° longitude corresponding to a one-hour difference in local time.
Tamasheq: Alwaq wan akal ( ilmital ghur edag wan tafukt) izlay s tišijrit, ila tezazlit n 15° n tišijrit togdahat id alwaq iyyan izlayan n n akal
English: The principle is straightforward, but in practice finding a reliable method of determining longitude took centuries and required the effort of some of the greatest scientific minds.
Tamasheq: Mabda i raqqisan mušan s tiditt ajjaraw n tikarse n taflist i almud n tišijrit ijja timad n iwityan tolas azilzam musnaten maqqornen n ešaraj wan science
English: His prime meridian passed through Alexandria.
Tamasheq: Prime meridian itiki fal Alexandria
English: He used a prime meridian through the Canary Islands, so that all longitude values would be positive.
Tamasheq: Assaxdam prime meridian daɣ Canary Islands har id isalan win tišijrit ad alaɣan
English: Hindu and Muslim astronomers continued to develop these ideas, adding many new locations and often improving on Ptolemy's data.
Tamasheq: Falăki tan win Indu tan d inăslimăn har ăjjudi okăyăn daɣ efes n anniyăten tin, issewdan idăgăn eynaynen tolas alwăq iyyan simuttiyăn isălăn fal Ptolemy
English: In the later Middle Ages, interest in geography revived in the west, as travel increased, and Arab scholarship began to be known through contact with Spain and North Africa.
Tamasheq: Daɣ ămindi n iwityan win aru, afor daɣ jogrăfia amităkwăy ɣur Ikufăr win atărăm šund ijjit n isikilăn d răsiya tan tin teɣare ilmădan fal assănăt addinăt ɣur aratay wa ijjăn id Spania d Afrikiya tan tămăsna
English: Christopher Columbus made two attempts to use lunar eclipses to discover his longitude, the first in Saona Island, on 14 September 1494 (second voyage), and the second in Jamaica on 29 February 1504 (fourth voyage).
Tamasheq: Christopher Columbus erăm har issin ihăndagăn ad exdăm s tiseten tin akăyăd n atărmăs n tăfukt i ad is-sin tišijrit net, awa ezzăran daɣ Saona Island daɣ ayor wan sutămbăr n ašal wan 14 n awătăy wan 1494 ( asikil wan is-sin) d wan is-sin daɣ Jamaica daɣ ayor wan tindufăn n ašal wan 29 daɣ awătăy wan 1504. ( asikil wan akkoz)
English: Initially an observation device, developments over the next half century transformed it into an accurate measurement tool.
Tamasheq: s tizărăt amutăj n akăyăd, ifesăn daɣ tăzune n temede n awătăy wan ilkămăt amutti s amutăj n eket olăɣăn
English: On land, the period from the development of telescopes and pendulum clocks until the mid 18th-Century saw a steady increase in the number of places whose longitude had been determined with reasonable accuracy, often with errors of less than a degree, and nearly always within 2-3°.
Tamasheq: Fal akal, ɣur azzaman wan efes n telescope tan d muntar tan pendulum har tazune n awatay wan 1800 issewad iddikud n idagan wi s tišijrit nasan tiskat s aqqud n tiditt , alwaq iyyan ahan marsalan id oraknen i degre s harkuk illan jir 2 d 3 °
English: Making accurate observations in an ocean swell is much harder than on land, and pendulum clocks do not work well in these conditions.
Tamasheq: Ijji n ikăyădan oɣădnen dagh ejjărew wan maqqorăn hullan ojjăr wan akal assăhat d muntar tan tin pendulum ar xăddim nat hullan daɣ tălɣiwen in
English: It offered two levels of rewards, for solutions within 1° and 0.5°.
Tamasheq: Ehak issin ihăndăgan n timzal i addăbăra tan daɣ 1° har 0.5°
English: This work was supported and rewarded with thousands of pounds from the Board of Longitude, but he fought to receive money up to the top reward of £20,000, finally receiving an additional payment in 1773 after the intervention of parliament.
Tamasheq: Alxdimăt ten idhăl tat tolas tila timzăl n timăd n azruf wan pounds ghur Board of Longitude mušăm eghil d ijru azruf ewădăn a ojjăran 20,000 n dollar, as išrăy ijjraw timzăl awidnen daɣ awătăy wan 1773 darat majrăd wan dibiti tan
English: Lunar distances came into general use after 1790.
Tamasheq: Ujjij wan ayor eqqal a fal tijja alxdimăt ɣur darăt n awătăy wan 1790
English: It was quickly realised that the telegraph could be used to transmit a time signal for longitude determination.
Tamasheq: Ijran a hin addinăt daɣ armud as telegraph addobăt axădăm daɣ asissiki n sinyăl wan alwăq i musnat n tišijrit
English: The Survey established chains of mapped locations through Central and South America, and the West Indies, and as far as Japan and China in the years 1874–90.
Tamasheq: Farăk iday isassărăn n idagan wr nen kărti daɣ Amrik tan ammăs har tan agăla d West Indies har Japon d Chine daɣ iwityăn win 1874 har win 90
English: This changed when wireless telegraphy became available in the early 20th-Century.
Tamasheq: Awen ammutăy alwăq wa id telegraghy ta war n ila iɣunăn taqqăl a ti illan dagh iwityăn azzarnen n awatăy wan 2000
English: Radio navigation systems came into general use after World War II.
Tamasheq: Sistem tan win amătikwi n Radio issintăn alxidmăt darat akkinăs wan issin n alɣălim
English: With the exception of magnetic declination, all proved practicable methods.
Tamasheq: A war n imos magnetic declination, awa yadăn fuk eqqal išujjišăn iknănen
English: Longitude at a point may be determined by calculating the time difference between that at its location and Coordinated Universal Time (UTC).
Tamasheq: Tašijrit ɣur titbăqet addobaăt awădim alamăd net ɣur t issedăna azli n alwăq jir edăg wa eha d Cordinated Universal Time (UTC)
English: The word near is used because the point might not be at the centre of the time zone; also the time zones are defined politically, so their centres and boundaries often do not lie on meridians at multiples of 15°.
Tamasheq: Isim wan edes atiwăna fal as tatbăqet war n eha ammăs n alwăq wan edag: săddeq alwăq wan ihăndagăn almăɣna net folitik a ti tijjaăt, daɣ awen ammăssăn nasan d alxădudăn nasăn alwaq iyyan fal oherăn harat id meridan tan s inătfisăn n 15°
English: The international standard convention (ISO 6709)—that East is positive—is consistent with a right-handed Cartesian coordinate system, with the North Pole up.
Tamasheq: International Standard Convention (ISO6709)- n as alqiblăt toɣad - ila ujrah s aqqud n Cartesian Coordinate System id North Pole
English: They have since shifted to the standard approach.
Tamasheq: S ammutăyan ɣur alwaq wen daɣ s ašujjš wa ijlăn
English: The geoid is the shape that the ocean surface would take under the influence of the gravity of Earth, including gravitational attraction and Earth's rotation, if other influences such as winds and tides were absent.
Tamasheq: Geoid eqqăl dumu wa dar ola arori n ejarew i assăhăt tan ajjălilliwi wan amădal eha awa id erămmăs ajjălilliwi d aɣalilway n amădal fal war ti illen at assăhaten tiyyad šund adud tan d tinăzzamăren
English: It can be known only through extensive gravitational measurements and calculations.
Tamasheq: Iket tan hin inkašnen win aɣălilway n amadal d iddikudăn nasan a addobăt nen fal asilmăd net
English: Although the physical Earth has excursions of +8,848 m (Mount Everest) and −10,984 (Marianas Trench), the geoid's deviation from an ellipsoid ranges from +85 m (Iceland) to −106 m (southern India), less than 200 m total.
Tamasheq: Kuddeɣ as amădăl s taɣissa net a han ti ifruɣăn n +8,848 m (Adaɣ wan Everest) d -10,984 (Marianas Trench), afruɣ wan geoid ɣur itărtăran win ellipsoid ɣur +85m (Iceland) har -106m (India tan tamasna), a orăkan fuk i 200m
English: If the continental land masses were crisscrossed by a series of tunnels or canals, the sea level in those canals would also very nearly coincide with the geoid.
Tamasheq: A fal tikunen n idăɣan win amădal eɣlăyan tan id tijursăyen n iɣešan, iddikud n ejjărew wa maqqorăn daɣ iɣešăn win inta deɣ a izli har hin ehaz geoid
English: That means that when traveling by ship, one does not notice the undulations of the geoid; the local vertical (plumb line) is always perpendicular to the geoid and the local horizon tangential to it.
Tamasheq: Awen almăɣna net a fal issekel awădim daɣ Bato, war hin za egra a hin awădim imitikwiyan n geoid; teɣate net (iyaka wan ammas) hrkuk ozɣaɣ i geoid d edag wa id immuqăs diris
English: That is because GPS satellites, orbiting about the center of gravity of the Earth, can measure heights only relative to a geocentric reference ellipsoid.
Tamasheq: Awen fal as satelit tn win GPS tan, aqqalnen šund ebănɣ n ammas wan aɣălilwăy n amadal, adobăt eket n iddikud n izuk net daɣ as orak sa s ammăs n ellipsoid
English: Modern GPS receivers have a grid implemented in their software by which they obtain, from the current position, the height of the geoid (e.g. the EGM-96 geoid) over the World Geodetic System (WGS) ellipsoid.
Tamasheq: GPS receivers win amarăd ilan griyaj ehan software tan s karrăšan ɣur edag wan ahan iddikud n izuk n geoid (almital EGM-96 Geoid) fal World Geodetic System (GWS) ellipsoid