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A straight rille is a type of valley or trench found on the Moon. These features are typically flat-floored and relatively straight, measuring about 1–5 km wide and up to several hundred kilometers long.1

Some straight rilles are believed to be grabens, which are collapsed blocks of the lunar crust situated between parallel faults. Others appear to be tension cracks. These cracks may have formed in areas where subsurface gases caused eruptions of dark material, leading to the creation of rimless vent craters. Straight rilles are distinct from sinuous rilles, which resemble winding river valleys and are thought to be formed by ancient lava flows.1

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