| Information | |
|---|---|
| has gloss | (noun) rock formed by the solidification of molten magma igneous rock |
| has gloss | eng: Igneous rock (derived from the Latin word "Igneus" meaning of fire, from "Ignis" meaning fire) is one of the three main rock types (the others being sedimentary and metamorphic rock). Igneous rock is formed by magma (molten rock) cooling and becoming solid. Igneous rock may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks. This magma can be derived from partial melts of pre-existing rocks in either a planets mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Over 700 types of igneous rocks have been described, most of them having formed beneath the surface of Earths crust. These have diverse properties, depending on their composition and how they were formed. |
| has gloss | eng: Igneous rocks are formed when molten rock (magma) cools down to form crystals or minerals. Examples are granite and basalt. Igneous rocks that are formed inside the Earth's crust are called intrusive rocks; rocks that are formed at the surface are called extrusive rocks. Igneous rocks are also referred to as plutonic or volcanic rocks. The word "igneous" is derived from the Latin ignis, meaning "fire"; another way to learn this is by remembering igneous as "ignite". Igneous rocks may be found near volcanoes. |
| lexicalization | eng: Igneous rocks |
| lexicalization | eng: igneous rock |
| subclass of | (noun) material consisting of the aggregate of minerals like those making up the Earth's crust; "that mountain is solid rock"; "stone is abundant in New England and there are many quarries" rock, stone |
| has subclass | (noun) a dark grey volcanic rock andesite |
| has subclass | (noun) light-colored and fine-grained granitic rock consisting chiefly of quartz and feldspars aplite |
| has subclass | (noun) (geology) the matrix of fine-grained crystalline material in which larger crystals are embedded groundmass |
| has subclass | (noun) dark greyish extrusive rock adesite |
| has subclass | (noun) large mass of intrusive igneous rock believed to have solidified deep within the earth plutonic rock, pluton, batholite, batholith |
| has subclass | (noun) a granular crystalline intrusive rock diorite |
| has subclass | (noun) one of a family of granular intrusive rocks gabbro |
| has subclass | (noun) a form of igneous rock consisting of extremely coarse granite resulting from the crystallization of magma rich in rare elements pegmatite |
| has subclass | (noun) a dark coarse-grained igneous rock consisting principally of olivine peridotite |
| has subclass | (noun) very acid volcanic rock rhyolite |
| has subclass | (noun) extrusive igneous rock solidified near or on the surface of the Earth volcanic rock |
| has subclass | (noun) any igneous rock with crystals embedded in a finer groundmass of minerals porphyry, porphyritic rock |
| has subclass | c/Igneous rocks by composition |
| has subclass | c/Igneous rocks by texture |
| Note: 196 other instance(s) ommited in the following list | |
| has instance | e/Adamellite |
| has instance | e/Benmoreite |
| has instance | e/Chromitite |
| has instance | e/Hornblende andesite porphyry |
| has instance | e/Intermediate composition |
| has instance | e/Quartz latite |
| has instance | e/Restite |
| has instance | e/Spherulite |
| has instance | e/Tezontle |
| has instance | e/Widgiemooltha Komatiite |
| has instance | e/es/Ofita |
| has instance | e/et/Basaltne andesiit |
| has instance | e/et/Leelisbasalt |
| has instance | e/et/Plagioklassporfüriit |
| has instance | e/et/Tinguaiit |
| has instance | e/fr/Série différenciée |
| has instance | e/hu/Gabbró |
| has instance | e/hu/Telérkőzet |
| has instance | e/nl/Boniniet |
| has instance | e/nl/Granitoid |
| has instance | e/nl/Kristalfractionatie |
| has instance | e/no/Drammensgranitt |
| has instance | e/pl/Alaskit |
| has instance | e/pl/Limburgit |
| has instance | e/pl/Skały efuzywne |
| has instance | e/pl/Skały hipabysalne |
| has instance | e/pl/Toleit |
| has instance | e/pl/Wehrlit |
| has instance | e/pt/Adamelito |
| has instance | e/pt/Diagrama QAPF |
| has instance | e/pt/Fonólito |
| has instance | e/sk/Absarokit |
| has instance | e/sk/Bázické horniny |
| has instance | c/sr/Базичне магматске стене |
| has instance | e/sv/Revsundsgranit |
| has instance | e/uk/Аляскит |
| has instance | e/uk/Афанітова порода |
| has instance | e/uk/Жильні гірські породи |
| has instance | e/uk/Маймечит |
| has instance | e/uk/Пехштейн |
| Meaning | |
|---|---|
| Arabic | |
| lexicalization | ara: صخر ناري |
| lexicalization | ara: علم النفط |
| Belarusian | |
| has gloss | bel: Магматычныя горныя пароды ўтварыліся з расплаўленай магмы пры яе зацвярдзеньні і крышталізацыі. У залежнасьці ад умоў зацььвярдзення магмы ў нетрах Зямлі або на яе паверхні адрозьніваюць інтрузіўныя горныя пароды і эфузіўныя горныя пароды. |
| has gloss | bel: Магматычныя горныя пароды ўтварыліся з расплаўленай магмы пры яе зацвярдзенні і крышталізацыі. У залежнасці ад умоў зацвярдзення магмы ў нетрах Зямлі або на яе паверхні адрозніваюць інтрузіўныя горныя пароды і эфузіўныя горныя пароды. |
| lexicalization | bel: Магматычныя горныя пароды |
| lexicalization | bel: магматычныя горныя пароды |
| Bosnian | |
| has gloss | bos: Magmatske stijene nastaju kada se magma hladi i skrutnjava, sa ili bez kristalizacije, ispod površine kao intruzivne stijene ili na površini kao efuzivne stijene. Magma može proizvedena parcijalnim taloženjem već postojećih stijena ili u plaštu ili u kori. Obično je taloženje uzrokovano jednim ili više sljedećih procesa - povišenjem temperature, sniženjem pritiska ili promjenom sastava. Opisano je preko 700 vrsta magmatskih stijena, većinom nastalih ispod površine Zemljine kore. |
| lexicalization | bos: magmatske stijene |
| Bulgarian | |
| has gloss | bul: Магмените скали са един от трите основни типа скали в земната кора. Образувани са от застинала и кристализирала магма. Скалите образувани при охлаждане на магмата на различна дълбочина под земната повърхност, се наричат интрузивни (плутонични), а тези образувани след изливането и изстиването на магмата върху земната повърхност - ефузивни (еруптивни; вулканични ). |
| lexicalization | bul: магмени скали |
| Catalan | |
| has gloss | cat: Les roques ígnies o magmàtiques són les roques que shan format a partir del refredament dun magma. |
| lexicalization | cat: Roques ígnies |
| Czech | |
| has gloss | ces: Magmatická nebo též vyvřelá hornina je termín z geologie. Používá se pro označení horniny, která vzniká krystalizací z magmatu. Vznik struktury magmatické horniny se řídí posloupností krystalizace, která je spojena s postupným klesáním teploty taveniny, což vyúsťuje ve vznik zárodečných krystalů pevné fáze. Následná krystalizace se řídí podle Bowenova reakčního schématu. |
| lexicalization | ces: Magmatická hornina |
| lexicalization | ces: Magmatické horniny |
| lexicalization | ces: vyvřelá hornina |
| Show unreliable ▼ | |
| lexicalization | ces: magmatická hornina |
| Mandarin Chinese | |
| lexicalization | cmn: huǒ chéng yan |
| lexicalization | cmn: 火成岩 |
| Show unreliable ▼ | |
| lexicalization | cmn: yán jiāng yan |
| lexicalization | cmn: 岩浆岩 |
| lexicalization | cmn: 岩漿岩 |
| Welsh | |
| has gloss | cym: Cerrig sy'n magma (cerrig tawdd, lafa ar wyneb y daear) wedi crisialu yw Creigiau Igneaidd. Mae magma yn casglu o dan cramen y ddaear a fel arfer yn cynnwys nwy a mwynau wedi crisialu. |
| lexicalization | cym: Craig igneaidd |
| lexicalization | cym: Creigiau igneaidd |
| lexicalization | cym: craig igneaidd |
| Danish | |
| lexicalization | dan: Magmatiske bjergarter |
| German | |
| has gloss | deu: Magmatische Gesteine oder Magmatite (nach gr. mágma „geknetete Masse“; Erstarrungsgesteine) sind Gesteine, die durch Kristallisation aus glutflüssiger Gesteinsschmelze entstanden sind. Die Magmatite sind neben den Sedimentgesteinen und den Metamorphiten eine der drei Gesteinshauptgruppen. Nach ihrer Entstehung und ihren Gefügemerkmalen werden magmatische Gesteine petrografisch in zwei Gruppen unterteilt: Plutonite (Tiefengesteine) entstehen aus erstarrendem Magma im Erdinneren, Vulkanite (Ergussgesteine) entstehen aus Lava an der Erdoberfläche. Ob die Abkühlung und Erstarrung der Gesteinsschmelze ober- oder unterirdisch erfolgt, hat einen deutlichen Einfluss auf die Kristallisation und die Textur der entstehenden Gesteine. |
| lexicalization | deu: Magmatisches Gestein |
| lexicalization | deu: Erstarrungsgestein |
| lexicalization | deu: Magmatit |
| lexicalization | deu: magmatisches Gestein |
| lexicalization | deu: Eruptivgestein |
| lexicalization | deu: Extrusivgestein |
| Modern Greek (1453-) | |
| has gloss | ell: Τα εκρηξιγενή ή πυριγενή πετρώματα αποτελούν και το μεγαλύτερο μέρος των πετρωμάτων επί των οποίων και δημιουργήθηκαν τα ιζηματογενή. Αποτελούν μια από τις τρεις κύριες ομάδες των πετρωμάτων, (η τρίτη ομάδα είναι τα μεταμορφωσιγενή πετρώματα), που παρατηρούνται στους γεωλογικούς σχηματισμούς. |
| lexicalization | ell: Εκρηξιγενές πέτρωμα |
| Esperanto | |
| has gloss | epo: Sub magmaj petroj aŭ magmatitoj (solidiĝaj ŝtonaĵoj) oni kunigas nocie en la geologio ĉiujn petrojn, kiuj ekestas per solidiĝo de magmo kaj do havas sian originon per procesoj en la terinterno. |
| lexicalization | epo: Magmaj petroj |
| lexicalization | epo: magmaj petroj |
| Estonian | |
| has gloss | est: Tardkivim ehk magmakivim on magma tardumisel (enamasti kristalliseerumisel) tekkinud kivim. |
| lexicalization | est: Tardkivimid |
| lexicalization | est: tardkivim |
| Basque | |
| has gloss | eus: Arroka igneoak magma likidotik sortutako arrokak dira. Bi motakoak daude: plutonikoak eta bolkanikoak. Plutonikoak intrusiboak dira, magmak oso geldo kristalizatzen da lurrazalen barruan, eta bolkanikoak edo estrusiboak gainazalara heltzen den magnatik sortzen dira, edo laba fragmentu aereotatik. Arroka intrusiboek milaka urte behar dituzte hozteko eta estrusiboek oso denbora gutxi, orduetatik asteetara. |
| lexicalization | eus: Arroka igneoak |
| lexicalization | eus: Arroka igneo |
| lexicalization | eus: arroka igneo |
| Persian | |
| has gloss | fas: در زمینشناسی به سنگهای حاصل از فرایندهای آتشفشانی سنگهای آذَرین گویند. سنگهای آذرین به دو بخش سنگهای آذرین درونی و سنگهای آذرین بیرونی تقسیم میشوند. سنگهای آذرین بیرونی حاصل فرآیند آتشفشانی و بیرون ریختن مواد مذاب از دهانهٔ آتشفشان است اما سنگهای آذرین درونی حاصل فرآیند ماندن ماگما در آشیانه و سرد شدن آهستهٔ آن میباشد. |
| lexicalization | fas: سنگ آذرین |
| lexicalization | fas: سنگهای آذرین |
| Finnish | |
| has gloss | fin: Magmakivet jaetaan kolmeen ryhmään muodostumistapansa perusteella. Syväkivilajit eli plutoniset kivilajit kiteytyvät kivisulasta eli magmasta hitaasti syvällä maankuoressa. Juonikivet syntyvät samalla tavoin, mutta kuoren ulkokerroksissa magmasäiliössä, kun taas tulivuoresta maan pinnalle purkautunut magma muodostaa vulkaanisia kivilajeja eli vulkaniitteja, joita kutsutaan yhteisellä nimellä myös eruptiivikiviksi tai pintakiviksi. |
| lexicalization | fin: Magmakivilajit |
| lexicalization | fin: Magmakivi |
| Show unreliable ▼ | |
| lexicalization | fin: magmakivi |
| lexicalization | fin: magmakivilaji |
| French | |
| has gloss | fra: | class="wikitable droite" |+ Roches magmatiques équivalentes ! Roche volcanique ! Roche plutonique |----- | rhyolite : | granite : |- | basalte : | gabbro : |----- | trachyte : | syénite : |- | rhyodacite : | granodiorite : |----- | andésite : | diorite : |} Les roches magmatiques, également désignées sous le vocable de roches ignées , voire comme roches éruptives , se forment quand un magma se refroidit et se solidifie, avec ou sans cristallisation complète des minéraux le composant. Cette solidification peut se produire : * en profondeur, cas des roches magmatiques plutoniques (dites « intrusives ») ; * à la surface, cas des roches magmatiques volcaniques (dites « extrusives » ou « effusives »). |
| lexicalization | fra: Roche magmatique |
| Galician | |
| has gloss | glg: As rochas ígneas (do latín igneus, lume) son aquelas rochas que se forman pola solidificación do magma ante unha redución de temperatura, sexa dentro da codia terrestre; co que se producen rochas plutónicas; ou ao agromar á superficie; producindo rochas volcánicas. Tamén existiría outro grupo de rochas ígneas que serían as filonianas ou porfíricas. |
| lexicalization | glg: Rocha magmática |
| lexicalization | glg: Rochas ígneas |
| lexicalization | glg: rocha magmática |
| Serbo-Croatian | |
| has gloss | hbs: Magmatske stene se drugačije nazivaju i eruptivne stene. Nastale su očvršćavanjem magme u zemljinoj unutrašnjosti odnosno očvršćavanjem lave na površini Zemlje. Dele se na dubinske i površinske. Prva Zemljina kora je bila sastavljena samo od magmatskih stena. |
| lexicalization | hbs: magmatske stene |
| Hebrew | |
| has gloss | heb: סלע יסוד הוא סלע שנוצר מהתגבשות של מאגמה כתוצאה מהתקררותה. נהוג לחלק את סלעי היסוד לשני סוגים, על פי אופן ההתגבשות ומיקומה, מעל או מתחת לפני קרום כדור הארץ: ;סלע פלוטוני קרוי גם "סלע תהום", "סלע מִחְדָר" או "סלע אינטרוסיבי" - Intrusive Rock– סלע שהתגבש ממאגמה בפנים כדור הארץ בתהליך איטי, ורק אחר כך, כתוצאה של תהליכי הרמה ובליה, נחשף על פני השטח. על כן הוא מורכב מגבישים גסים. לדוגמה: גרניט או גברו. ;סלע געשי קרוי גם "סלע פרץ", "סלע וולקני" או "סלע אקסטרוסיבי" - Extrusive Rock – סלע שהתגבש מלבה שפרצה אל מחוץ לקרום במהלך התפרצות געשית והתקרר במהירות, ועל כן הוא מורכב מגבישים קטנים. לדוגמה: ריוליט או בזלת. |
| lexicalization | heb: סלע יסוד |
| lexicalization | heb: סלעי יסוד |
| Croatian | |
| has gloss | hrv: Magmatske stijene nastaju kada se magma hladi i skrutnjava, s ili bez kristalizacije, ispod površine kao intruzivne stijene ili na površini kao efuzivne stijene. Magma može proizvedena parcijalnim taljenjem već postojećih stijena ili u plaštu ili u kori. Obično je taljenje uzrokovano jednim ili više sljedećih procesa - povišenjem temperature, sniženjem tlaka ili promjenom sastava. Opisano je preko 700 vrsta magmatskih stijena, većinom nastalih ispod površine Zemljine kore. |
| lexicalization | hrv: magmatske stijene |
| Hungarian | |
| has gloss | hun: A magmás kőzetek többkomponensű kőzetolvadékokból keletkező kőzetfélék, amiket összetételük és keletkezési helyük szerint és/vagy kristályosodási fokuk szerint osztályozunk. |
| lexicalization | hun: Magmás kőzetek |
| lexicalization | hun: magmás kőzet |
| Ido | |
| lexicalization | ido: Fairoza roki |
| Indonesian | |
| has gloss | ind: Batuan beku atau batuan igneus (dari Bahasa Latin: ignis, "api") adalah jenis batuan yang terbentuk dari magma yang mendingin dan mengeras, dengan atau tanpa proses kristalisasi, baik di bawah permukaan sebagai batuan intrusif (plutonik) maupun di atas permukaan sebagai batuan ekstrusif (vulkanik). Magma ini dapat berasal dari batuan setengah cair ataupun batuan yang sudah ada, baik di mantel ataupun kerak bumi. Umumnya, proses pelelehan terjadi oleh salah satu dari proses-proses berikut: kenaikan temperatur, penurunan tekanan, atau perubahan komposisi. Lebih dari 700 tipe batuan beku telah berhasil dideskripsikan, sebagian besar terbentuk di bawah permukaan kerak bumi. |
| lexicalization | ind: batuan beku |
| Show unreliable ▼ | |
| lexicalization | ind: batuan beku gunung berapi |
| Icelandic | |
| has gloss | isl: Storkuberg er bergtegund, sem myndast þegar bergkvika, sem á upptök í möttli jarðar, storknar. Storkuberg skiptist í gosberg, gangberg og djúpberg. |
| lexicalization | isl: Storkuberg |
| lexicalization | isl: storkuberg |
| Italian | |
| has gloss | ita: Le rocce magmatiche (dette anche eruttive o ignee) si formano in seguito alla solidificazione di magmi, cioè di masse silicatiche fuse contenenti vari componenti (FeO, MgO, CaO, ecc.) e sostanze volatili (acqua, anidride carbonica, idrogeno, metano, ecc.). Costituiscono quasi il 95% della crosta terrestre; ma, sulla superficie della Terra, questa abbondanza è nascosta dallo strato diffuso, sebbene molto sottile, di rocce sedimentarie e metamorfiche. |
| lexicalization | ita: Rocce magmatiche |
| lexicalization | ita: Roccia magmatica |
| lexicalization | ita: roccia magmatica |
| Lojban | |
| has gloss | jbo: nio lo dujroi goi koa cu selzba lenu lo likroi cu dunja .i suo lo dujroi cu binxo krili rokci .i lo dujroi poi kea cu zbasu tui lo tedysfe cu selcme lo spoja dujroi .ije lo dujroi poi kea cu zbasu fio cnita stuzi lo tedysfe cu selcme lo cnita dujroi |
| lexicalization | jbo: dujro'i |
| Japanese | |
| has gloss | jpn: 火成岩（かせいがん、）は、マグマが冷えて固まった岩石（若干の異物を取り込んだものを含む）。 |
| lexicalization | jpn: 火成岩 |
| Kazakh | |
| lexicalization | kaz: Магмалық тау жыныстары |
| Korean | |
| has gloss | kor: 화성암(火成岩)은 마그마가 식어서 형성된 암석이다. |
| lexicalization | kor: 화성암 |
| Lithuanian | |
| has gloss | lit: Magminės uolienos – uolienos, susidariusios iš magmos (išlydytos, daugiausia silikatinės masės), kuri šaldama sukietėjo. |
| lexicalization | lit: Magminė uoliena |
| lexicalization | lit: Magminės uolienos |
| lexicalization | lit: magminė uoliena |
| Malayalam | |
| has gloss | mal: ശിലകളുടെ മൂന്ന് തരങ്ങളിലൊന്നാണ് ആഗ്നേയ ശില (Igneous rock). മാഗ്മ തണുത്തുറഞ്ഞാണ് ഇവ രൂപം കൊള്ളുന്നത്. ക്രിസ്റ്റലീകരണം വഴിയോ അല്ലാതെയോ ഭൗമോപരിതലത്തിലോ അതിനു താഴെയോ ഇവ രൂപപ്പെടാം. ഭൂമിയുടെ പുറമ്പാളിയിലോ മാന്റിലിലോ ഉള്ള പാറകള് ഭാഗികമായി ഉരുകിയാണ് മാഗ്മ ഉണ്ടാകുന്നത്. സാധാരണയായി മൂന്ന് കാരണങ്ങളാലാണ് മാഗ്മ ഉണ്ടാകുന്നത്: താപനിലയിലെ വര്ദ്ധനവ്, മര്ദ്ദത്തിന്റെ കുറയല്, ഘടനയിലെ വ്യതിയാനം. 700-ലേറെ തരം ആഗ്നേയശിലകളുണ്ട്. ഇവയില് മിക്കതും ഭൂമിയുടെ ഉപരിതലത്തിന് താഴെയാണ്. ഘടനയും എങ്ങനെ രൂപപ്പെട്ടുവെന്നതനുസരിച്ചും ഇവ വ്യത്യസ്ത സ്വഭാവസവിശേഷതകള് കാണിക്കുന്നു. |
| lexicalization | mal: ആഗ്നേയ ശില |
| lexicalization | mal: ആഗ്നേയശില |
| Macedonian | |
| has gloss | mkd: Магматските карпи настануваат со ладењето или стврднувањето на вулканската лава или магма во самата Земјина кора или на нејзината површина. Кога ладењето е многу брзо, нема време да се создаваат кристали, но ако тоа се случува бавно, колку подолго ќе трае процесот, толку поголеми ќе бидат карпестите кристали. Овие карпи се одликуваат со голема цврстина и имаат голема примена во градежништвото. Тие немаат слоеви и не содржат фосилни остатоци. Магматските карпи се класифицираат на најразлични начини. Ако се поделат според начинот на настанувањето, има: |
| lexicalization | mkd: Магматска карпа |
| Mongolian | |
| has gloss | mon: Магмын чулуулаг (Латин: ignis- гал) нь халуун хайлмал магмаас үүсэх ба интрузив (шургамал) ба эффузив (бялхмал) гэсэн 2 үндсэн төрөлд хуваагдана. Интрузив чулуулаг нь Дэлхийн царцдаст, газрын гүнд аажим хөрж, талсжих магмаас үүсдэг бол эффузив чулуулаг нь газрын гадаргуу дээр ил гарч ирсэн халуун магмаас үүснэ. Чулуулаг үүсгэгч магм нь Дэлхийн манти, эсвэл Дэлхийн царцдасын хэсэгчилсэн хайлалтаар бий болно. Хэсэгчилсэн хайлалт нь температур ихсэх, даралт багасах, эсвэл эрдсийн найрлага өөрчлөгдөх зэрэг процесоор үүснэ. Одоогоор 700 гаруй төрлийн магмын чулуулаг тодорхойлогдоод байгаагийн ихэнхи нь газрын гүнд үүссэн байдаг. Магмын чулуулаг нь үүссэн нөхцөл ба бүрдүүлэгч эрдсийн найрлагаасаа хамааран өөр хоорондоо ялгаатай болно. |
| lexicalization | mon: магмын чулуулаг |
| Maori | |
| lexicalization | mri: toka köngotu |
| Show unreliable ▼ | |
| lexicalization | mri: toka ngiha |
| Malay (macrolanguage) | |
| has gloss | msa: Batu igneus adalah batuan yang terbentuk akibat pembekuan magma. Batu igneus ini terbahagi kepada 2 jenis, satu dipanggil "batu igneus dalam" manakala satu lagi "batu igneus luar". Batu igneus dalam terbentuk akibat pembekuan magma di lapisan dalam bumi, sehingga terbentuk padatan yang teksturnya relatif kasar. Sedangkan batu igneus luar terbentuk akibat pembekuan magma di luar permukaan bumi. |
| lexicalization | msa: Batuan igneus |
| Low German | |
| has gloss | nds: As Magmatiten oder ok magmatsch Stenen warrt in de Geologie all de Stenen tohopenfaat, de dör Fast Warrn vun Magma tostannen kommt. Jehmer Utgangspunkt liggt also binnen de Eer un hangt mit de Prozessen tosamen, de dor binnen afloopt. |
| lexicalization | nds: Magmatit |
| lexicalization | nds: magmatit |
| Dutch | |
| has gloss | nld: | |- | |} Stollingsgesteente is gesteente dat is ontstaan door stolling van lava (aan het aardoppervlak) of magma (onder het aardoppervlak). De hoofdindeling van gesteenten is in stollingsgesteenten, afzettingsgesteenten en metamorfe gesteenten. |
| lexicalization | nld: Stollingsgesteente |
| Show unreliable ▼ | |
| lexicalization | nld: magmatische gesteente |
| Norwegian Nynorsk | |
| has gloss | nno: Ein magmatisk bergart (også kalla eruptiv bergart, størkningsbergart eller vulkansk bergart) er ein bergart som er danna ved at magma har trengt seg fram frå det indre av jorda og vorte avkjølt, slik at den flytande magmaen har størkna til fast form (fjell). Det er tre typar magmatiske bergartar: djupbergartar, dagbergartar og gangbergartar. |
| lexicalization | nno: Magmatisk bergart |
| lexicalization | nno: Vulkanske bergartar |
| Norwegian | |
| has gloss | nor: Magmatisk bergart, kalles også eruptiv bergart, størkningsbergart eller vulkansk bergart, og er en bergart som er dannet ved at magma har trengt seg fram fra jordens indre, blitt avkjølt, slik at det flytende magmaet er størknet til fast form (fjell). Det er tre typer av magmatiske bergarter: dypbergarter, dagbergarter og gangbergarter. |
| lexicalization | nor: Magmatisk bergart |
| lexicalization | nor: Vulkanske bergarter |
| lexicalization | nor: magmatisk bergart |
| Polish | |
| has gloss | pol: Skały magmowe – jeden z trzech głównych typów skał (obok skał osadowych i metamorficznych) budujących skorupę ziemską, powstałych wskutek krystalizacji lub zakrzepnięcia magmy w głębi skorupy ziemskiej lub lawy na powierzchni Ziemi. |
| lexicalization | pol: Skały magmowe |
| lexicalization | pol: skały magmowe |
| Portuguese | |
| has gloss | por: As Rochas ígneas, rochas magmáticas ou rochas eruptivas (derivado do latim ignis, que significa fogo) são um dos três principais tipos de rocha (sendo que as outras são as rochas sedimentares e as rochas metamórficas). A formação das rochas ígneas vêm do resultado da consolidação devida ao resfriamento do magma derretido ou parcialmente derretido. Elas podem ser formadas com ou sem a cristalização, ou abaixo da superfície como rochas intrusivas (plutônicas) ou próximo à superfície, sendo rochas extrusivas (vulcânicas). O magma pode ser obtido a partir do derretimento parcial de rochas pré-existentes no manto ou na crosta terrestre. Normalmente, o derretimento é provocado por um ou mais dos três processos: o aumento da temperatura, diminuição da pressão ou uma mudança na composição. Já foram descritos mais de 700 tipos de rochas ígneas, sendo que a maioria delas é formada em baixo da superfície da crosta da Terra com diversas propriedades, em função de sua composição e do modo de como foram formadas. |
| lexicalization | por: Rocha ìgnea |
| lexicalization | por: rocha ígnea |
| lexicalization | por: Rochas ígneas |
| Moldavian | |
| lexicalization | ron: Roci magmatice |
| Russian | |
| has gloss | rus: Магматические горные породы — это породы, образовавшиеся непосредственно из магмы (расплавленной массы преимущественно силикатного состава), в результате её охлаждения и застывания. В зависимости от условий застывания различают интрузивные (глубинные) и эффузивные (излившиеся) горные породы. |
| lexicalization | rus: магматические горные породы |
| Slovak | |
| has gloss | slk: Vyvretá hornina alebo magmatická hornina je hornina, ktorá vznikla kryštalizáciou z chladnúcej magmy. |
| lexicalization | slk: Vyvretá hornina |
| lexicalization | slk: Vyvreté horniny |
| lexicalization | slk: vyvretá hornina |
| Slovenian | |
| has gloss | slv: Magmatske kamnine so kamnine, nastale s strjevanjem magme oziroma staljenega kamna, in sicer s kristalizacijo ali brez. Magmatske kamnine lahko nastanejo (se strdijo) pod površjem in se v tem primeru imenujejo globočnine, nasprotno pa se predornine strdijo na njem (večinoma izbruhana magma). Kamnina lahko izhaja iz Zemljinega plašča, pa tudi iz višjih plasti Zemlje, a je v slednjem primeru pred pridobitvijo magmatske strukture staljena zaradi ekstremne temperature ali pritiska. Večina od okoli 700 magmatskih kamnin, kolikor jih pozna geološka znanost, sodi v razred globočnin. |
| lexicalization | slv: Magmatska kamnina |
| lexicalization | slv: Magmatske kamnine |
| lexicalization | slv: magmatska kamnina |
| Castilian | |
| has gloss | spa: Las rocas ígneas (latín ignis, "fuego") se forman cuando el magma (roca fundida) se enfría y se solidifica. Si el enfriamiento se produce lentamente bajo la superficie se forman rocas con cristales grandes denominadas rocas plutónicas o intrusivas, mientras que si el enfriamiento se produce rápidamente sobre la superficie, por ejemplo, tras una erupción volcánica, se forman rocas con cristales invisibles conocidas como rocas volcánicas o extrusivas. La mayor parte de los 700 tipos de rocas ígneas que se han descrito se han formado bajo la superficie de la corteza terrestre. Ejemplos de rocas ígneas son la diorita, la riolita, el pórfido, el gabro, el basalto y el granito. |
| lexicalization | spa: Roca Ignea |
| lexicalization | spa: Roca Ígnea |
| lexicalization | spa: Rocas ígneas |
| Serbian | |
| has gloss | srp: Магматске стене се другачије називају и еруптивне стене. Настале су очвршћавањем магме у земљиној унутрашњости односно очвршћавањем лаве на површини Земље. Деле се на дубинске и површинске. Прва Земљина кора је била састављена само од магматских стена. |
| lexicalization | srp: Магматске стене |
| Sundanese | |
| has gloss | sun: Batu beku atawa batu igneus (tina Basa Latin: ignis, "seuneu") nyaéta wanda babatuan anu kawangun tina magma anu jadi tiis sarta jadi heuras, kalayan atawa tanpa prosés kristalisasi, boh di handapeun permukaan minangka batuan intrusif (plutonik) boh di luhur permukaan minangka batuan ékstrusif (vulkanik). Magma ieu asalna bisa tina babatuan satengah éncér atawa babatuan anu geus aya, boh dina lapisan atawa kerak bumi. Umumna, prosés ngalelehna lumangsung ku salasahiji tina prosés-prosés jiga: naékna suhu, turunna tekenan, atawa robahna komposisi. Leuwih ti 700 wanda batuan beku geus hasil didéskripsikeun, kalolobaan kawangun di handapeun beungeut kerak bumi. |
| lexicalization | sun: Batu igneus |
| lexicalization | sun: batu igneus |
| Swedish | |
| has gloss | swe: Magmatisk bergart, en bergart som bildats genom att magma som har trängt genom jordskorpan och stelnat. Extrusiva magmatiska bergarter har bildats genom vulkanism, dessa kallas också för vulkaniska bergarter. Intrusiva magmatiska bergarter har bildats genom att magma har stelnat på ett större djup eller genom att magma har trängt upp genom och stelnat i sprickor. |
| lexicalization | swe: Magmatisk bergart |
| lexicalization | swe: Magmatiska bergarter |
| lexicalization | swe: magmatisk bergart |
| Tamil | |
| has gloss | tam: தீப்பாறை, உருகிய பாறைக் குழம்பு பளிங்காக்கத்துடனோ அல்லது பளிங்காக்கம் இல்லாமலோ இறுகித் திண்மம் ஆவதால் உருவாகின்றது. இது புவி மேற்பரப்புக்கு மேலே அல்லது அதற்குக் கீழே இடம்பெறலாம். ஏற்கெனெவே புவியோட்டில் அல்லது மூடகத்தில் (mantle) உள்ள பாறைகள், பகுதியாக உருகுவதன் மூலமும் பாறைக் குழம்பு உருவாகக்கூடும். இவ்வாறு பாறைகள் உருகுவது, கீழ்க் காண்பவற்றுள் ஒன்று அல்லது அதற்கு மேற்பட்ட வழிமுறைகள் மூலம் நடைபெறக் கூடும். |
| lexicalization | tam: தீப்பாறை |
| Thai | |
| has gloss | tha: หินอัคนี (Igneous rock)คือหินที่เกิดจากการเย็นตัวและตกผลึกของหินหนืด (Magma) เมื่อหินหนืดเหล่านี้เคลื่อนที่เข้ามาใกล้ผิวโลก หินอัคนีที่เกิดจากการเย็นตัวและตกผลึกของหินหนืดใต้ผิวโลกอย่างช้า ๆ เรียกว่า หินอัคนีบาดาล (Intrusive Rocks หรือ Plutonic Rocks) หินอัคนีที่เกิดจากการเย็นตัวและตกผลึกของหินหลอมเหลว (Lava) บนผิวโลกหรือใกล้ผิวโลก เรียกว่า หินอัคนีภูเขาไฟ (Extrusive Rocks หรือ Volcanic Rocks) หินอัคนีที่เกิดจากการทับถมของเศษหินที่ได้จากการระเบิดของภูเขาไฟ เมื่อมีการเชื่อมประสานด้วยแร่ จะได้หินที่เรียกว่า หินอัคนีตะกอนภูเขาไฟ (Pyroclastic Rocks) |
| lexicalization | tha: หินอัคนี |
| Turkish | |
| has gloss | tur: Magmatik kayaçlar. Magmanın yükselerek yer kabuğunun içerisine girmesi veya derinliklerinde yeryüzünde soğuyarak katılaşması sonucu oluşan kayaç türüdür. Magmatik kayaçlar temel olarak silikat minerallerinden oluşmuşlardır. |
| lexicalization | tur: Magmatik kayaçlar |
| Ukrainian | |
| has gloss | ukr: Магмати́чні гірські́ поро́ди (, , ) — ендогенні гірські породи, первинним джерелом яких є магма. Є складовою частиною літосферної тріади. Магматичні породи складають понад 90% маси літосфери. |
| lexicalization | ukr: Магматичні гірські породи |
| lexicalization | ukr: Магматичні породи |
| lexicalization | ukr: магматичні гірські породи |
| Vietnamese | |
| has gloss | vie: :Bài này nói về đá macma như là một thuật ngữ trong địa chất học. . Đá mácma hay đá magma là những loại đá được thành tạo do sự đông nguội của những dung thể magma nóng chảy được đưa lên từ những phần sâu của vỏ Trái Đất. Quá trình đông nguội có thể tạo ra các đá có các khoáng vật kết tinh rõ ràng hoặc không kết tinh tùy thuộc vào môi trường mà khối magma đông nguội, và dựa vào đó người ta ta phân ra: đá xâm nhập và phun trào. Macma này có thể có nguồn gốc từ manti của Trái Đất hoặc từ các loại đá đã tồn tại trước đó bị nóng chảy do các thay đổi nhiệt độ áp suất cực cao. Trên 700 loại đá mácma đã được miêu tả lại, phần lớn trong chúng được tạo ra gần bề mặt lớp vỏ Trái Đất. |
| lexicalization | vie: Đá Macma |
| lexicalization | vie: Đá mácma |
| Chinese | |
| has gloss | zho: 火成岩或稱-岩}-漿岩，是指岩冷卻後（地壳裡喷出的岩浆，或者被融化的现存岩石），成形的一種岩石。现在已经发现700多种岩浆岩，大部分是在地壳裡面的岩石。常見的岩漿岩有花崗岩、安山岩及玄武岩等。 |
| lexicalization | zho: 岩浆岩 |
| lexicalization | zho: 火成岩 |
Lexvo © 2008-2024 Gerard de Melo. Contact Legal Information / Imprint
