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http://dbpedia.org/ontology/abstract Abalos Undae és una formació geològica de Abalos Undae és una formació geològica de tipus unda a la superfície de Mart, localitzada amb el sistema de coordenades planetocèntriques a 82.2 ° latitud N i 283.03 ° longitud E, que fa 442.74 km de diàmetre. El nom va ser aprovat per la UAI l'any 1988 i fa referència a una característica d'albedo localitzada a 72 ° latitud N i 70 ° longitud O.itzada a 72 ° latitud N i 70 ° longitud O. , Abalos Undae (Latin for "Abalos Waves") isAbalos Undae (Latin for "Abalos Waves") is a dune field on Mars in the periphery of Planum Boreum, the Martian North pole. It is one of the officially named northern circumpolar dune fields, along with Olympia, Hyperboreae, and Siton Undae, and also one of the densest of the region. Its northernmost boundary is located in the southwest channel that separates the Abalos Colles formation from the main polar ice cap, and from there the dune field extends southwest all the way to the lowlands of Vastitas Borealis. It is theorised that the dunes of the Abalos field may have resulted from erosion of Rupes Tenuis (Latin: Thin Cliff), the polar scarp. Its name was approved by the International Astronomical Union in 1988. It extends from latitude 74.94°N to 82.2°N and from longitude 261.4°E to 283.03°E (76.97°W – 98.6°W). Its origin is located at classical albedo feature with coordinates 72°N, 70°W and has a diameter of 442.74 km.2°N, 70°W and has a diameter of 442.74 km. , 阿瓦洛斯沙丘群(Abalos Undae)拉丁语意为“阿瓦洛斯波浪”,是位于火星北极阿瓦洛斯沙丘群(Abalos Undae)拉丁语意为“阿瓦洛斯波浪”,是位于火星北极高原边缘的一片沙丘场,它与奥林匹亚沙丘群、许珀耳玻瑞亚和西顿沙丘群一起,为已正式命名的绕北极沙丘区之一,也是该地区沙丘最密集的区域之一。阿瓦洛斯沙丘群的最北端边界位于将阿瓦洛斯丘群地层和主极地冰盖隔开的西南沟壑中,从那里该沙丘场一直向西南延伸至北方大平原低地。 理论上讲,阿巴洛斯地区的沙丘是特纽依斯峭壁(拉丁语:薄崖)和极地断崖被侵蚀的结果,其范围涵盖北纬74.94度到北纬82.2度、东经261.4度至东经283.03度(西经76.97度–西经98.6度)的区域,它的名称源自位于北纬72度、西经70度,直径442.74公里的古典反照率特征上,1988年,阿瓦洛斯沙丘群名称被国际天文学联合会正式接受。4公里的古典反照率特征上,1988年,阿瓦洛斯沙丘群名称被国际天文学联合会正式接受。 , Le Abalos Undae sono una struttura geologica della superficie di Marte.
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rdfs:comment Abalos Undae (Latin for "Abalos Waves") isAbalos Undae (Latin for "Abalos Waves") is a dune field on Mars in the periphery of Planum Boreum, the Martian North pole. It is one of the officially named northern circumpolar dune fields, along with Olympia, Hyperboreae, and Siton Undae, and also one of the densest of the region. Its northernmost boundary is located in the southwest channel that separates the Abalos Colles formation from the main polar ice cap, and from there the dune field extends southwest all the way to the lowlands of Vastitas Borealis. way to the lowlands of Vastitas Borealis. , Le Abalos Undae sono una struttura geologica della superficie di Marte. , 阿瓦洛斯沙丘群(Abalos Undae)拉丁语意为“阿瓦洛斯波浪”,是位于火星北极阿瓦洛斯沙丘群(Abalos Undae)拉丁语意为“阿瓦洛斯波浪”,是位于火星北极高原边缘的一片沙丘场,它与奥林匹亚沙丘群、许珀耳玻瑞亚和西顿沙丘群一起,为已正式命名的绕北极沙丘区之一,也是该地区沙丘最密集的区域之一。阿瓦洛斯沙丘群的最北端边界位于将阿瓦洛斯丘群地层和主极地冰盖隔开的西南沟壑中,从那里该沙丘场一直向西南延伸至北方大平原低地。 理论上讲,阿巴洛斯地区的沙丘是特纽依斯峭壁(拉丁语:薄崖)和极地断崖被侵蚀的结果,其范围涵盖北纬74.94度到北纬82.2度、东经261.4度至东经283.03度(西经76.97度–西经98.6度)的区域,它的名称源自位于北纬72度、西经70度,直径442.74公里的古典反照率特征上,1988年,阿瓦洛斯沙丘群名称被国际天文学联合会正式接受。4公里的古典反照率特征上,1988年,阿瓦洛斯沙丘群名称被国际天文学联合会正式接受。 , Abalos Undae és una formació geològica de Abalos Undae és una formació geològica de tipus unda a la superfície de Mart, localitzada amb el sistema de coordenades planetocèntriques a 82.2 ° latitud N i 283.03 ° longitud E, que fa 442.74 km de diàmetre. El nom va ser aprovat per la UAI l'any 1988 i fa referència a una característica d'albedo localitzada a 72 ° latitud N i 70 ° longitud O.itzada a 72 ° latitud N i 70 ° longitud O.
rdfs:label Abalos Undae , 阿瓦洛斯沙丘群
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