Hebes Mensa is a large mensa that rises from the floor of Hebes Chasma, one of the chasmata of the Valles Marineris network on Mars. Some researchers have identified this mesa to be an interior layered deposit (ILD), similar to Ganges Mensa, and are named for alternating light-toned and dark-toned layers forming a stair-stepped stratigraphy. The faces of Hebes Mensa are sometimes fluted. It is 7.5 kilometres (4.7 mi) tall and 120 by 43 kilometres (75 by 27 mi) wide.
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| - Hebes Mensa (en)
- Hebes Mensa (it)
- 赫柏桌山 (zh)
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| - Hebes Mensa is a large mensa that rises from the floor of Hebes Chasma, one of the chasmata of the Valles Marineris network on Mars. Some researchers have identified this mesa to be an interior layered deposit (ILD), similar to Ganges Mensa, and are named for alternating light-toned and dark-toned layers forming a stair-stepped stratigraphy. The faces of Hebes Mensa are sometimes fluted. It is 7.5 kilometres (4.7 mi) tall and 120 by 43 kilometres (75 by 27 mi) wide. (en)
- L'Hebes Mensa è una formazione geologica della superficie di Marte. Prende il nome da Ebe, dea della giovinezza nella mitologia greca. (it)
- 赫柏桌山(Hebes Mensa)是一座大型桌山,它隆起于火星水手谷的分支峡谷-赫柏峡谷谷底。一些研究人员已将该桌山确定为类似恒河桌山的内部层状沉积物(ILD),并对这一色泽深浅交替的阶梯状地层进行了命名。赫柏桌山表面有时呈现出凹槽,它高约7.5公里(4.7英里),占地面积120×43公里(75×27英里)。 (zh)
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| - Hebes Chasma, seen on daytime IR THEMIS. Hebes Mensa is the feature in the center of the chasm. (en)
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| - Hebes Mensa is a large mensa that rises from the floor of Hebes Chasma, one of the chasmata of the Valles Marineris network on Mars. Some researchers have identified this mesa to be an interior layered deposit (ILD), similar to Ganges Mensa, and are named for alternating light-toned and dark-toned layers forming a stair-stepped stratigraphy. The faces of Hebes Mensa are sometimes fluted. It is 7.5 kilometres (4.7 mi) tall and 120 by 43 kilometres (75 by 27 mi) wide. (en)
- L'Hebes Mensa è una formazione geologica della superficie di Marte. Prende il nome da Ebe, dea della giovinezza nella mitologia greca. (it)
- 赫柏桌山(Hebes Mensa)是一座大型桌山,它隆起于火星水手谷的分支峡谷-赫柏峡谷谷底。一些研究人员已将该桌山确定为类似恒河桌山的内部层状沉积物(ILD),并对这一色泽深浅交替的阶梯状地层进行了命名。赫柏桌山表面有时呈现出凹槽,它高约7.5公里(4.7英里),占地面积120×43公里(75×27英里)。 (zh)
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| - POINT(76.779998779297 -1.0199999809265)
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