Alba Mons (or Alba Patera) is an immense, low-lying volcano located in the northern Tharsis region of the planet Mars. It is the largest volcano on Mars in terms of area, with volcanic flow fields that extend for at least 1350 km (839 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (4.2 mi) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet.

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dbpedia-owl:abstract
  • Alba Patera je unikátní štítová sopka na povrchu Marsu, která se nachází na severní polokouli v severní oblasti Tharsis, západně od oblasti Tempe Terra, severně od další štítové sopky Ascraeus Mons, severozápadně od sopky Uranius Patera, severovýchodně Abalos Colles, jihozápadně se nachází nejvyšší sopka sluneční soustavy Olympus Mons a na západ pohoří Aceron Fossea. Na severozápadě se pak nachází menší pohoří Arcadia Dorsa.
  • Der Alba Patera ist ein Vulkan auf dem Mars. Er ist trotz seines Volumens – sein Einzugsgebiet umfasst einen Durchmesser von ungefähr 1600 km – relativ flach. Seine Höhe wird auf 3 km geschätzt. Seine Lavaströme haben teils eine Reichweite von über 300 km.
  • Alba Mons (or Alba Patera) is an immense, low-lying volcano located in the northern Tharsis region of the planet Mars. It is the largest volcano on Mars in terms of area, with volcanic flow fields that extend for at least 1350 km (839 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (4.2 mi) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet. The flanks of Alba Mons have very gentle slopes. The average slope along the volcano's northern (and steepest) flank is 0.5°, which is over five times lower than the slopes on the other large Tharsis volcanoes. In broad profile, Alba Mons resembles a vast but barely raised welt on the planet's surface. It is a unique volcanic structure with no counterpart on Earth or elsewhere on Mars. In addition to its great size and low relief, Alba Mons has a number of other distinguishing features. The central portion of the volcano is surrounded by an incomplete ring of faults and fractures, called Alba Fossae on the volcano's western flank and Tantalus Fossae on the eastern flank. The volcano also has very long, well preserved lava flows that form a radiating pattern from the volcano's central region. The enormous lengths of some individual flows (>300 km) implies that the lavas were very fluid and of high volume. Many of the flows have distinctive morphologies, consisting of long, sinuous ridges with discontinuous central lava channels. The low areas between the ridges (particularly along the volcano's northern flank) show a branching pattern of shallow gullies and channels that likely formed by water runoff. Alba Mons has some of the oldest, extensively exposed volcanic deposits in the Tharsis region. Geologic evidence indicates that significant volcanic activity ended much earlier at Alba Mons than at Olympus Mons and the Tharsis Montes volcanoes. Volcanic deposits from Alba Mons range in age from Hesperian to early Amazonian (approximately 3600 to 3200 million years old).
  • Alba Patera es una estructura volcánica única, localizada en al norte de la región de Tharsis en el planeta Marte. Se trata de un enorme volcán en escudo de alrededor de 1.600 km de diámetro, pero sólo unos 6 km de altura en su punto más alto. Alba Patera constituye por ello el volcán más grande del Sistema Solar, en términos de área y volumen.
  • Alba Patera on valtava kilpitulivuori Marsissa, Tharsis-ylängön pohjoispuolella. Alba Patera on läpimitaltaan suunnattoman suuri, noin 1 600 kilometriä, ja se onkin pinta-alaltaan laajin tulivuori koko Aurinkokunnassa. Laajuudestaan huolimatta vuoren korkein huippu kohoaa vain 6 kilometrin korkeuteen. Alba Pateran loivat rinteet ovat täynnä pitkiä ja kapeita uomia, jotka viittaavat siihen, että tulivuoresta on purkautunut pitkän ajan kuluessa tavanomaista juoksevampaa laavaa.
  • Alba Mons (littéralement « Mont Blanc » en latin), plus connu sous le nom d'Alba Patera bien que cette appellation ne désigne stricto sensu que sa caldeira sommitale, est le plus vaste volcan bouclier de la planète Mars (et de l'ensemble du système solaire), situé par 40,5° N et 250,4° E dans le quadrangle d'Arcadia, au nord-ouest du renflement de Tharsis et exactement aux antipodes du bassin d'impact d'Hellas Planitia.
  • Alba Patera è il cratere sommitale di una formazione vulcanica situata nella zona nord della regione Tharsis, sul pianeta Marte; è un enorme vulcano a scudo, approssimativamente del diametro di 1600 chilometri, ma con un'altezza di soli 6 chilometri nel suo punto più alto. È il più largo vulcano del sistema solare, in termini di area e di volume. Esso presenta colate laviche meno spesse degli altri vulcani a scudo marziani, con formazione di sottili strati lavici e centinaia di lunghi e stretti canali sui suoi fianchi. La maggior parte di questi stretti canali sono lunghi più di 100 chilometri (alcuni anche superiori a 300) suggerendo come della lava molto fluida sia eruttata per lunghi periodi di tempo. Alba Patera si trova all'interno di un sistema di faglie che si diparte a nord di Tharsis. Alba differisce dalle altre Paterae marziane in quanto manca di depositi di ceneri, e si trova nella zona dei bassopiani invece che degli altopiani.
  • アルバ・パテラ（Alba Patera）は火星のタルシス地域、北緯40.5度、西経109.9度にある楯状火山。裾野の直径はオリンポス火山の3倍以上になる太陽系最大の1600km、しかし標高は6kmに満たない。
  • Alba Patera (breedte 40,1° N, lengte 109,8° W) is een bijzondere vulkaan ten noorden van het Tharsisgebied op Mars, een enorme schildvulkaan die omstreeks 1600 kilometer in doorsnee maar slechts ~6 kilometer hoog. Het is de grootste vulkaan in het zonnestelsel wat betreft oppervlak en inhoud - zie ook Olympus Mons. Hij heeft minder dikke lavastromen dan de andere schildvulkanen op Mars, met zowel enorme platen als honderden lange smalle kanalen op zijn flanken. De meeste smalle kanalen zijn meer dan 100 kilometer lang, met sommige langer dan 300 kilometer. Dit wijst op uitbarstingen van lava gedurende lange perioden. Alba Patera ligt in een gebied van geologische breuken die vanuit Tharsis naar het noorden lopen. Een patera is een term uit de astrogeologie voor een ondiepe krater met onregelmatige, soms geschulpte rand. Alba Patera onderscheidt zich van de andere paterae op Mars doordat hij geen asafzetting met voren heeft en ligt in laagland in plaats van hoogland.
  • Alba Mons (tidligere Alba Patera) er en unik vulkansk struktur nord for Tharsis-regionen på planeten Mars. Strukturen er en enorm skjoldvulkan omtrent  km i diameter, men bare ~6 km hly. Den er den største kjente vulkanen i solsystemet målt i areal og volum (med et areal på 5,7×10 km² dekker den 5 % av overflaten på Mars). Vulkanen har en tynnere lavastrøm enn de andre skjoldvulkanene på Mars, med både enorme platelignende lag og hundrevis av lange trange kanaler på sidene. Flesteparten av de trange kanalene er over 100 km lange; noen er så lange som over 300 km; noe som tyder på utbrudd over lang tid av lava med lav viskositet. Alba Mons ligger på et system av forkastninger som går nordover fra Tharsis. Alba Mons skiller seg fra de andre patera-formasjonene på Mars på flere måter; vulkanen mangler furete askeavsetninger og ligger i lavland og ikke høyland.
  • Alba Mons (do 2007 r. Alba Patera) – wielkich rozmiarów, lecz relatywnie niski wulkan tarczowy położony w północnej części regionu Tharsis na Marsie, na północny wschód od Olympus Mons.
  • Alba Patera é a única formação vulcânica ao norte da região de Tharsis em Marte, um enorme vulcão com aproximadamente 1600 km de diâmetro mas apenas ~6 km no ponto mais alto. É o vulcão mais amplo do sistema solar,em termos de área e volume. O Alba Ptera costuma expelir menos lava que outros vulcões marcianos, gerando grandes camadas pouco espessas de lava e canais de milhares de quilômetros em seu flanco. A maioria dos canais possui mais de 100 km de extensão, muitas chegando a mais de 300, sugerindo que lava muito fluida é expelida durante um longo tempo. O Alba Patera está localizado na falha geológica que atravessa a região de Tharsis. Alba difere de outros vulcões marcianos em vários aspectos, principalmente na falta de um depósito de cinzas e por estar localizado em uma planície, ao invés de uma área montanhosa.
  • 亞拔山（Alba Mons）是火星上塔爾西斯北方的一座巨大的盾狀火山，位於北緯40.47度，東經250.4度，海拔6770公尺。破火山口寬136公里，稱作 Alba Patera。山坡一路延伸數百公里至北方低原，不像其他火山有明顯的分界。火山周圍有很多南北向的槽溝，如亞拔槽溝（Alba Fossae）等等。
  • Alba Mons (or Alba Patera) is an immense, low-lying volcano located in the northern Tharsis region of the planet Mars. It is the largest volcano on Mars in terms of area, with volcanic flow fields that extend for at least 1,350 km (840 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (22,000 ft) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet. The flanks of Alba Mons have very gentle slopes. The average slope along the volcano's northern (and steepest) flank is 0.5°, which is over five times lower than the slopes on the other large Tharsis volcanoes. In broad profile, Alba Mons resembles a vast but barely raised welt on the planet's surface. It is a unique volcanic structure with no counterpart on Earth or elsewhere on Mars. In addition to its great size and low relief, Alba Mons has a number of other distinguishing features. The central portion of the volcano is surrounded by an incomplete ring of faults and fractures, called Alba Fossae on the volcano's western flank and Tantalus Fossae on the eastern flank. The volcano also has very long, well preserved lava flows that form a radiating pattern from the volcano's central region. The enormous lengths of some individual flows (>300 km) implies that the lavas were very fluid and of high volume. Many of the flows have distinctive morphologies, consisting of long, sinuous ridges with discontinuous central lava channels. The low areas between the ridges (particularly along the volcano's northern flank) show a branching pattern of shallow gullies and channels that likely formed by water runoff. Alba Mons has some of the oldest, extensively exposed volcanic deposits in the Tharsis region. Geologic evidence indicates that significant volcanic activity ended much earlier at Alba Mons than at Olympus Mons and the Tharsis Montes volcanoes. Volcanic deposits from Alba Mons range in age from Hesperian to early Amazonian (approximately 3600 to 3200 million years old).
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  • Viking image of Alba Mons. The volcano's relief is barely visible in orbital photographs. The broad system of fractures on the volcano's eastern side is called Tantalus Fossae. The narrower fracture system on the western flank is Alba Fossae.
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  • Alba Patera je unikátní štítová sopka na povrchu Marsu, která se nachází na severní polokouli v severní oblasti Tharsis, západně od oblasti Tempe Terra, severně od další štítové sopky Ascraeus Mons, severozápadně od sopky Uranius Patera, severovýchodně Abalos Colles, jihozápadně se nachází nejvyšší sopka sluneční soustavy Olympus Mons a na západ pohoří Aceron Fossea. Na severozápadě se pak nachází menší pohoří Arcadia Dorsa.
  • Der Alba Patera ist ein Vulkan auf dem Mars. Er ist trotz seines Volumens – sein Einzugsgebiet umfasst einen Durchmesser von ungefähr 1600 km – relativ flach. Seine Höhe wird auf 3 km geschätzt. Seine Lavaströme haben teils eine Reichweite von über 300 km.
  • Alba Mons (or Alba Patera) is an immense, low-lying volcano located in the northern Tharsis region of the planet Mars. It is the largest volcano on Mars in terms of area, with volcanic flow fields that extend for at least 1350 km (839 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (4.2 mi) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet.
  • Alba Patera es una estructura volcánica única, localizada en al norte de la región de Tharsis en el planeta Marte. Se trata de un enorme volcán en escudo de alrededor de 1.600 km de diámetro, pero sólo unos 6 km de altura en su punto más alto. Alba Patera constituye por ello el volcán más grande del Sistema Solar, en términos de área y volumen.
  • Alba Patera on valtava kilpitulivuori Marsissa, Tharsis-ylängön pohjoispuolella. Alba Patera on läpimitaltaan suunnattoman suuri, noin 1 600 kilometriä, ja se onkin pinta-alaltaan laajin tulivuori koko Aurinkokunnassa. Laajuudestaan huolimatta vuoren korkein huippu kohoaa vain 6 kilometrin korkeuteen. Alba Pateran loivat rinteet ovat täynnä pitkiä ja kapeita uomia, jotka viittaavat siihen, että tulivuoresta on purkautunut pitkän ajan kuluessa tavanomaista juoksevampaa laavaa.
  • Alba Mons (littéralement « Mont Blanc » en latin), plus connu sous le nom d'Alba Patera bien que cette appellation ne désigne stricto sensu que sa caldeira sommitale, est le plus vaste volcan bouclier de la planète Mars (et de l'ensemble du système solaire), situé par 40,5° N et 250,4° E dans le quadrangle d'Arcadia, au nord-ouest du renflement de Tharsis et exactement aux antipodes du bassin d'impact d'Hellas Planitia.
  • Alba Patera è il cratere sommitale di una formazione vulcanica situata nella zona nord della regione Tharsis, sul pianeta Marte; è un enorme vulcano a scudo, approssimativamente del diametro di 1600 chilometri, ma con un'altezza di soli 6 chilometri nel suo punto più alto. È il più largo vulcano del sistema solare, in termini di area e di volume.
  • アルバ・パテラ（Alba Patera）は火星のタルシス地域、北緯40.5度、西経109.9度にある楯状火山。裾野の直径はオリンポス火山の3倍以上になる太陽系最大の1600km、しかし標高は6kmに満たない。
  • Alba Patera (breedte 40,1° N, lengte 109,8° W) is een bijzondere vulkaan ten noorden van het Tharsisgebied op Mars, een enorme schildvulkaan die omstreeks 1600 kilometer in doorsnee maar slechts ~6 kilometer hoog. Het is de grootste vulkaan in het zonnestelsel wat betreft oppervlak en inhoud - zie ook Olympus Mons. Hij heeft minder dikke lavastromen dan de andere schildvulkanen op Mars, met zowel enorme platen als honderden lange smalle kanalen op zijn flanken.
  • Alba Mons (tidligere Alba Patera) er en unik vulkansk struktur nord for Tharsis-regionen på planeten Mars. Strukturen er en enorm skjoldvulkan omtrent  km i diameter, men bare ~6 km hly. Den er den største kjente vulkanen i solsystemet målt i areal og volum (med et areal på 5,7×10 km² dekker den 5 % av overflaten på Mars). Vulkanen har en tynnere lavastrøm enn de andre skjoldvulkanene på Mars, med både enorme platelignende lag og hundrevis av lange trange kanaler på sidene.
  • Alba Mons (do 2007 r. Alba Patera) – wielkich rozmiarów, lecz relatywnie niski wulkan tarczowy położony w północnej części regionu Tharsis na Marsie, na północny wschód od Olympus Mons.
  • Alba Patera é a única formação vulcânica ao norte da região de Tharsis em Marte, um enorme vulcão com aproximadamente 1600 km de diâmetro mas apenas ~6 km no ponto mais alto. É o vulcão mais amplo do sistema solar,em termos de área e volume. O Alba Ptera costuma expelir menos lava que outros vulcões marcianos, gerando grandes camadas pouco espessas de lava e canais de milhares de quilômetros em seu flanco.
  • 亞拔山（Alba Mons）是火星上塔爾西斯北方的一座巨大的盾狀火山，位於北緯40.47度，東經250.4度，海拔6770公尺。破火山口寬136公里，稱作 Alba Patera。山坡一路延伸數百公里至北方低原，不像其他火山有明顯的分界。火山周圍有很多南北向的槽溝，如亞拔槽溝（Alba Fossae）等等。
  • Alba Mons (or Alba Patera) is an immense, low-lying volcano located in the northern Tharsis region of the planet Mars. It is the largest volcano on Mars in terms of area, with volcanic flow fields that extend for at least 1,350 km (840 mi) from its summit. Although the volcano has a span comparable to that of the United States, it reaches an elevation of only 6.8 km (22,000 ft) at its highest point. This is about one-third the height of Olympus Mons, the tallest volcano on the planet.
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  • Alba Patera
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  • Alba Patera
  • アルバ・パテラ
  • Alba Patera
  • Alba Mons
  • Alba Mons
  • Alba Patera
  • 亞拔山
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