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Le Ceraunius Fossae sono una struttura geologica della superficie di Marte.
, The Ceraunius Fossae are a set of fracture … The Ceraunius Fossae are a set of fractures in the northern Tharsis region of Mars. They lie directly south of the large volcano Alba Mons and consist of numerous parallel faults and tension cracks that deform the ancient highland crust. In places, younger lava flows cover the fractured terrain, dividing it into several large patches or islands. They are found in the Tharsis quadrangle. The faults are mainly narrow, north-south oriented graben. Graben (the name is both singular and plural) are long, narrow troughs bound by two inward-facing normal faults that enclose a downfaulted block of crust. The graben in the Ceraunius Fossae are commonly several kilometers wide, between 100 and slightly over 1000 m deep, and very closely spaced, giving the terrain a rugged ridge and groove topography. Many of the graben are hundreds of kilometers long and have walls with complex scalloped segments. Some contain pit crater chains (catenae) at their bottoms, suggesting the presence of deep-seated tension cracks into which surface material has drained.s into which surface material has drained.
, Ceraunius Fossae é uma fossa que vai de 19.1° e 38.4° latitude norte a 104.7° e 113° longitude oeste no quadrângulo de Tharsis em Marte. Seu nome vem de uma formação de albedo clássica. Seu nome foi aprovado pela União Astronômica Internacional em 1973.
, 刻拉尼俄斯堑沟群(Ceraunius Fossae) 是火星塔尔西斯区北部的一组裂缝 … 刻拉尼俄斯堑沟群(Ceraunius Fossae) 是火星塔尔西斯区北部的一组裂缝，位于大型火山亚拔山正南，它由许多平行的断层和古代高地地壳变形时产生的张力裂缝所组成。在某些地方，年轻的熔岩流覆盖了断裂地形，将其分割成数个大区块或岛屿，它们都可在塔尔西斯区中找到。 这些断层主要为南北走向的狭窄地堑，地堑(名称既可是单数，也可为复数)是由一条狭长的沟壑，以二侧内向切面为界，附着一块下陷地壳块的正断层。刻拉尼俄斯槽沟群中的地堑通常有数公里宽，深度在100米至略高于1000米之间且间隔很近，使该地区形成崎岖的山脊和沟壑地形。许多地堑长达数百公里，岩壁带有复杂扇形段，一些底部分布有链坑状凹陷(链坑)，表明存在表面层已陷落下去的深层拉伸裂缝。杂扇形段，一些底部分布有链坑状凹陷(链坑)，表明存在表面层已陷落下去的深层拉伸裂缝。
, Ceraunius Fossae és una estructura geològi … Ceraunius Fossae és una estructura geològica del tipus fossa a la superfície de Mart, situada amb el sistema de coordenades planetocèntriques a 38.12 ° de latitud N i 255.74 ° de longitud E. Fa 1.166,63 km de diàmetre. El nom va ser fet oficial per la UAI l'any 1973 i pren el nom d'una característica d'albedo.pren el nom d'una característica d'albedo.
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MOLA colorized image of the Ceraunius Fossae region. The fractured terrain consists of two large patches of north-south trending faults surrounded by lava flows. The Alba Mons volcano is the large, circular feature at top.
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Ceraunius Fossae é uma fossa que vai de 19.1° e 38.4° latitude norte a 104.7° e 113° longitude oeste no quadrângulo de Tharsis em Marte. Seu nome vem de uma formação de albedo clássica. Seu nome foi aprovado pela União Astronômica Internacional em 1973.
, The Ceraunius Fossae are a set of fracture … The Ceraunius Fossae are a set of fractures in the northern Tharsis region of Mars. They lie directly south of the large volcano Alba Mons and consist of numerous parallel faults and tension cracks that deform the ancient highland crust. In places, younger lava flows cover the fractured terrain, dividing it into several large patches or islands. They are found in the Tharsis quadrangle. They are found in the Tharsis quadrangle.
, Le Ceraunius Fossae sono una struttura geologica della superficie di Marte.
, Ceraunius Fossae és una estructura geològi … Ceraunius Fossae és una estructura geològica del tipus fossa a la superfície de Mart, situada amb el sistema de coordenades planetocèntriques a 38.12 ° de latitud N i 255.74 ° de longitud E. Fa 1.166,63 km de diàmetre. El nom va ser fet oficial per la UAI l'any 1973 i pren el nom d'una característica d'albedo.pren el nom d'una característica d'albedo.
, 刻拉尼俄斯堑沟群(Ceraunius Fossae) 是火星塔尔西斯区北部的一组裂缝 … 刻拉尼俄斯堑沟群(Ceraunius Fossae) 是火星塔尔西斯区北部的一组裂缝，位于大型火山亚拔山正南，它由许多平行的断层和古代高地地壳变形时产生的张力裂缝所组成。在某些地方，年轻的熔岩流覆盖了断裂地形，将其分割成数个大区块或岛屿，它们都可在塔尔西斯区中找到。 这些断层主要为南北走向的狭窄地堑，地堑(名称既可是单数，也可为复数)是由一条狭长的沟壑，以二侧内向切面为界，附着一块下陷地壳块的正断层。刻拉尼俄斯槽沟群中的地堑通常有数公里宽，深度在100米至略高于1000米之间且间隔很近，使该地区形成崎岖的山脊和沟壑地形。许多地堑长达数百公里，岩壁带有复杂扇形段，一些底部分布有链坑状凹陷(链坑)，表明存在表面层已陷落下去的深层拉伸裂缝。杂扇形段，一些底部分布有链坑状凹陷(链坑)，表明存在表面层已陷落下去的深层拉伸裂缝。
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Ceraunius Fossae
, 刻拉尼俄斯槽沟群
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